1.
Outcrop
–
An outcrop or rocky outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth. However, in places where the cover is removed through erosion or tectonic uplift. In Finland, glacial erosion during the last glacial maximum, followed by scouring by sea waves, bedrock and superficial deposits may also be exposed at the Earths surface due to human excavations such as quarrying and building of transport routes. Outcrops allow direct observation and sampling of the bedrock in situ for geologic analysis, in situ measurements are critical for proper analysis of geological history and outcrops are therefore extremely important for understanding the geologic time scale of earth history. Outcrops are also important for understanding fossil assemblages, paleo-environment. An outcrop example in California is the Vasquez Rocks, familiar from location shooting use in many films, list of rock formations Geological formation Geologic time scale Media related to Outcrops at Wikimedia Commons
Outcrop
–
View of a bedrock outcrop near
San Carlos Water,
Falkland Islands
Outcrop
–
Granite outcrops at
Silesian Stones Mountain in southwestern
Poland.
Outcrop
–
Serrote Branco's outcrop.
Caicó,
Brazil.
Outcrop
–
A typical shore outcrop scoured by ancient glaciers in
Espoo,
Finland.
2.
Bucegi Mountains
–
The Bucegi Mountains (Romanian, Munții Bucegi, are located in central Romania, south of the city Brașov. They are part of the Southern Carpathians group of the Carpathian Mountains, to the east, the Bucegi Mountains have a very steep slope towards the popular tourist destination Prahova Valley. At a higher elevation is the Bucegi Plateau, where wind and rain have turned the rocks into spectacular figures such as the Sphinx, the Bucegi is believed to be the Dacian holy mountain Kogainon, on which the God Zalmoxis resided in a cave. The exact origin of the name Bucegi is disputed by philologists, buceag or bugeac seems to be the source of the name, a word designating in the language of mountain people both the moss in the forest and the wilderness or the junipers. Archaic version of the name Bucegi is Buceci, name used today by elders in the mountains. And Bucur is a genuine Dacian name, in Iorgu Iordans work, Toponimia romînească, the name of the mountains is derived from Slavic buk, meaning beech. Bucegi Mountains are bordered by Prahova Valley, area with the most ski resorts in Romania, moreover, since 1935, a part of Bucegi Mountains has been included in the list of protected areas in Romania, with national park status. Among the most popular ski resorts within the Bucegi Mountains are Sinaia, nicknamed the Pearl of the Carpathians, Sinaia offers the possibility of performing winter sports. Ski slopes within the resort are serviced by ski lift, accessible by cable car, the main tourist attractions are Peleș Castle, Pelișor, Royal Station, Sinaia Monastery, Casino and George Enescu Memorial House. Bușteni, located at an altitude of 800–900 m, features a base of accommodation. A cable car links Silva Hotel and Babele Chalet, on the mountaintops and this area has unusual rock formations, such as the Sphinx and Babele. Bușteni is the point of trekking on some of the most attractive routes in Bucegi Massif. In the winter months, Bușteni offers the possibility of practicing skiing and sleighing, there are ski slopes with varying degrees of difficulty. Bușteni is also a point, featuring Cantacuzino Castle and Cezar Petrescu Memorial Museum. Likewise, there is a trout farm, the Rucăr-Bran Corridor is a mountain pass that has the Bucegi Mountains on one side and the Piatra Craiului Mountains and Iezer-Păpușa Mountains on the other side. Bucegi Mountains area, whereof exist references since the 15th century, has proposed for protection in 1936, due to peerless landscapes and great diversity of plant. This proposal was taken up only in 1990, when materialized through the Ministers order no, Bucegi Natural Park covers an area of 32,663 hectares across three counties, having more than 60% of the territory covered with forests. Photo gallery of Bucegi Mountains Bucegi Natural Park
Bucegi Mountains
–
Bucegi Mountains
Bucegi Mountains
–
Podu Dâmboviţei village, in the
Dâmbovicioara commune, in the Rucăr-Bran Corridor
Bucegi Mountains
–
Omu Peak, 2505 m asl.
Bucegi Mountains
–
Ascending Bucsoiu peak
3.
Romania
–
Romania is a sovereign state located in Southeastern Europe. It borders the Black Sea, Bulgaria, Ukraine, Hungary, Serbia and it has an area of 238,391 square kilometres and a temperate-continental climate. With over 19 million inhabitants, the country is the member state of the European Union. Its capital and largest city, Bucharest, is the sixth-largest city in the EU, the River Danube, Europes second-longest river, rises in Germany and flows in a general southeast direction for 2,857 km, coursing through ten countries before emptying into Romanias Danube Delta. The Carpathian Mountains, which cross Romania from the north to the southwest are marked by one of their tallest peaks, Moldoveanu, modern Romania was formed in 1859 through a personal union of the Danubian Principalities of Moldavia and Wallachia. The new state, officially named Romania since 1866, gained independence from the Ottoman Empire in 1877, at the end of World War I, Transylvania, Bukovina and Bessarabia united with the sovereign Kingdom of Romania. Romania lost several territories, of which Northern Transylvania was regained after the war, following the war, Romania became a socialist republic and member of the Warsaw Pact. After the 1989 Revolution, Romania began a transition towards democracy and it has been a member of NATO since 2004, and part of the European Union since 2007. A strong majority of the population identify themselves as Eastern Orthodox Christians and are speakers of Romanian. The cultural history of Romania is often referred to when dealing with artists, musicians, inventors. For similar reasons, Romania has been the subject of notable tourist attractions, Romania derives from the Latin romanus, meaning citizen of Rome. The first known use of the appellation was attested in the 16th century by Italian humanists travelling in Transylvania, Moldavia, after the abolition of serfdom in 1746, the word rumân gradually fell out of use and the spelling stabilised to the form român. Tudor Vladimirescu, a leader of the early 19th century. The use of the name Romania to refer to the homeland of all Romanians—its modern-day meaning—was first documented in the early 19th century. The name has been officially in use since 11 December 1861, in English, the name of the country was formerly spelt Rumania or Roumania. Romania became the predominant spelling around 1975, Romania is also the official English-language spelling used by the Romanian government. The Neolithic-Age Cucuteni area in northeastern Romania was the region of the earliest European civilization. Evidence from this and other sites indicates that the Cucuteni-Trypillian culture extracted salt from salt-laden spring water through the process of briquetage
Romania
–
Neacșu's letter from 1521, the oldest surviving document written in
Romanian.
Romania
–
Flag
Romania
–
Writ issued on 14 October 1465 by
Radu cel Frumos, from his residence in
Bucharest, indicating
Ottoman victory.
Romania
–
A 1917 British map showing territories with majority Romanian populations.
4.
Quartz
–
Quartz is the second most abundant mineral in Earths continental crust, behind feldspar. There are many different varieties of quartz, several of which are semi-precious gemstones, since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. The word quartz is derived from the German word Quarz and its Middle High German ancestor twarc, the Ancient Greeks referred to quartz as κρύσταλλος derived from the Ancient Greek κρύος meaning icy cold, because some philosophers apparently believed the mineral to be a form of supercooled ice. Today, the rock crystal is sometimes used as an alternative name for the purest form of quartz. Quartz belongs to the crystal system. The ideal crystal shape is a six-sided prism terminating with six-sided pyramids at each end, well-formed crystals typically form in a bed that has unconstrained growth into a void, usually the crystals are attached at the other end to a matrix and only one termination pyramid is present. However, doubly terminated crystals do occur where they develop freely without attachment, a quartz geode is such a situation where the void is approximately spherical in shape, lined with a bed of crystals pointing inward. α-quartz crystallizes in the crystal system, space group P3121 and P3221 respectively. β-quartz belongs to the system, space group P6222 and P6422. These space groups are truly chiral, both α-quartz and β-quartz are examples of chiral crystal structures composed of achiral building blocks. The transformation between α- and β-quartz only involves a comparatively minor rotation of the tetrahedra with respect to one another, although many of the varietal names historically arose from the color of the mineral, current scientific naming schemes refer primarily to the microstructure of the mineral. Color is an identifier for the cryptocrystalline minerals, although it is a primary identifier for the macrocrystalline varieties. Pure quartz, traditionally called rock crystal or clear quartz, is colorless and transparent or translucent, common colored varieties include citrine, rose quartz, amethyst, smoky quartz, milky quartz, and others. The most important distinction between types of quartz is that of macrocrystalline and the microcrystalline or cryptocrystalline varieties, the cryptocrystalline varieties are either translucent or mostly opaque, while the transparent varieties tend to be macrocrystalline. Chalcedony is a form of silica consisting of fine intergrowths of both quartz, and its monoclinic polymorph moganite. Other opaque gemstone varieties of quartz, or mixed rocks including quartz, often including contrasting bands or patterns of color, are agate, carnelian or sard, onyx, heliotrope, amethyst is a form of quartz that ranges from a bright to dark or dull purple color. The worlds largest deposits of amethysts can be found in Brazil, Mexico, Uruguay, Russia, France, Namibia, sometimes amethyst and citrine are found growing in the same crystal. It is then referred to as ametrine, an amethyst is formed when there is iron in the area where it was formed
Quartz
–
Quartz
crystal cluster from
Tibet
Quartz
–
Clear rock crystals on a white base
Quartz
–
Amethyst crystals on matrix
Quartz
–
Citrine from Brazil
5.
Chalcedony
–
Chalcedony is a cryptocrystalline form of silica, composed of very fine intergrowths of quartz and moganite. These are both silica minerals, but they differ in that quartz has a crystal structure, while moganite is monoclinic. Chalcedonys standard chemical structure is SiO2, Chalcedony has a waxy luster, and may be semitransparent or translucent. It can assume a range of colors, but those most commonly seen are white to gray. The color of chalcedony sold commercially is often enhanced by dyeing or heating, the name chalcedony comes from the Latin chalcedonius. The name appears in Pliny the Elders Naturalis Historia as a term for a kind of Jaspis. The name is derived from the town Chalcedon in Asia Minor. The Greek word khalkedon also appears in the Book of Revelation and it is a hapax legomenon so it is hard to tell whether the precious gem mentioned in the Bible is the same mineral known by this name today. Chalcedony occurs in a range of varieties. Many semi-precious gemstones are in forms of chalcedony. The more notable varieties of chalcedony are as follows, Agate is a variety of chalcedony characterized by either transparency or color patterns, opaque varieties are sometimes referred to as jasper. Fire agate shows iridescent phenomena on a background, iris agate shows exceptional iridescence when light is shone through the stone. Landscape agate is chalcedony with a number of different mineral impurities making the stone resemble landscapes, aventurine is a form of quartz, characterised by its translucency and the presence of platy mineral inclusions that give a shimmering or glistening effect termed aventurescence. Chrome-bearing fuchsite is the inclusion, and gives a silvery green or blue sheen. Oranges and browns are attributed to hematite or goethite, carnelian is a clear-to-translucent reddish-brown variety of chalcedony. Its hue may vary from an orange, to an intense almost-black coloration. Similar to carnelian is sard, which is rather than red. Chrysoprase is a variety of chalcedony, which has been colored by nickel oxide
Chalcedony
–
A cut and polished Chalcedony
geode
Chalcedony
–
Agate
Chalcedony
–
Aventurine (Unknown scale)
Chalcedony
–
Carnelian
6.
Red
–
Red is the color at the longer-wavelengths end of the spectrum of visible light next to orange, at the opposite end from violet. Red color has a predominant light wavelength of roughly 620–740 nanometers, light with a longer wavelength than red but shorter than terahertz radiation and microwave is called infrared. Red is one of the secondary colors, resulting from the combination of yellow. Traditionally, it was viewed as a primary colour, along with yellow and blue, in the RYB color space and traditional color wheel formerly used by painters. Reds can vary in shade from light pink to very dark maroon or burgundy. Red is the color of cyan. In nature, the red color of blood comes from hemoglobin, the red color of the Grand Canyon and other geological features is caused by hematite or red ochre, both forms of iron oxide. It also causes the red color of the planet Mars, the color of autumn leaves is caused by pigments called anthocyanins, which are produced towards the end of summer, when the green chlorophyll is no longer produced. One to two percent of the population has red hair, the color is produced by high levels of the reddish pigment pheomelanin. Since red is the color of blood, it has historically been associated with sacrifice, danger, modern surveys in the United States and Europe show red is also the color most commonly associated with heat, activity, passion, sexuality, anger, love and joy. In China, India and many other Asian countries it is the color of symbolizing happiness, since the 19th century, red has also been associated with socialism and communism. The word red is derived from the Old English rēad, the word can be further traced to the Proto-Germanic rauthaz and the Proto-Indo European root rewdʰ-. In Sanskrit, the word means red or blood. In the Akkadian language of Ancient Mesopotamia and in the modern Inuit language of Inuit, the words for colored in Latin and Spanish both also mean red. In Portuguese the word for red is vermelho, which comes from Latin vermiculus, in the Russian language, the word for red, Кра́сный, comes from the same old Slavic root as the words for beautiful—красивый and excellent—прекрасный. Thus Red Square in Moscow, named long before the Russian Revolution, in heraldry, the word gules is used for red. Red can vary in hue from orange-red to violet-red, and for each hue there is a variety of shades and tints. Red hematite powder was found scattered around the remains at a grave site in a Zhoukoudian cave complex near Beijing
Red
–
Pure, or solid red, the color of most ripe
strawberries.
Red
–
Red
Red
–
Scarlet is one quarter of the way between the colors red and orange. It is the color worn by a
cardinal of the
Roman Catholic Church..
Red
–
The
cardinal takes its name from the color worn by Roman Catholic
cardinals.
7.
Yellow
–
Yellow is the color between green and orange on the spectrum of visible light. It is evoked by light with a predominant wavelength of roughly 570–590 nm, in traditional color theory, used in painting, and in the subtractive color system, used in color printing, yellow is a primary color. In the RGB color model, used to create colors on television and computer screens, yellow is made by combining red, the word yellow comes from the Old English geolu, geolwe, meaning yellow, yellowish, derived from the Proto-Germanic word gelwaz yellow. It has the same Indo-European base, gʰel-, as the gold and yell. In Iran it has connotations of pallor/sickness, but also wisdom and it plays an important role in Asian culture, particularly in China, where it is seen as the color of happiness, glory, wisdom, harmony, and culture. The word yellow comes from the Old English geolu, geolwe, meaning yellow, yellowish and it has the same Indo-European base, gʰel-, as the words gold and yell, gʰel- means both bright and gleaming, and to cry out. The English term is related to other Germanic words for yellow, namely Scots yella, East Frisian jeel, West Frisian giel, Dutch geel, German gelb, and Swedish and Norwegian gul. According to the Oxford English Dictionary, the oldest known use of word in English is from The Epinal Glossary in 700. Yellow, in the form of yellow pigment made from clay, was one of the first colors used in prehistoric cave art. The cave of Lascaux has an image of a horse colored with yellow estimated to be 17,300 years old, in Ancient Egypt, yellow was associated with gold, which was considered to be imperishable, eternal and indestructible. The skin and bones of the gods were believed to be made of gold, the Egyptians used yellow extensively in tomb paintings, they usually used either yellow ochre or the brilliant orpiment, though it was made of arsenic and was highly toxic. A small paintbox with orpiment pigment was found in the tomb of King Tutankhamun, men were always shown with brown faces, women with yellow ochre or gold faces. The ancient Romans used yellow in their paintings to represent gold and it is found frequently in the murals of Pompeii. During the Post-Classical period, yellow became firmly established as the color of Judas Iscariot, from this connection, yellow also took on associations with envy, jealousy and duplicity. The tradition started in the Renaissance of marking non-Christian outsiders, such as Jews, in 16th century Spain, those accused of heresy and who refused to renounce their views were compelled to come before the Spanish Inquisition dressed in a yellow cape. The color yellow has been associated with moneylenders and finance. The National Pawnbrokers Associations logo depicts three golden spheres hanging from a bar, referencing the three bags of gold that the saint of pawnbroking, St. Nicholas, holds in his hands. Additionally, the symbol of three golden orbs is found in the coat of arms of the House of Medici, a fifteenth century Italian dynasty of bankers and lenders
Yellow
–
Yellow is the color of
gold,
butter, and ripe
lemons.
Yellow
–
Yellow
Yellow
–
Image of a horse colored with
yellow ochre. from
Lascaux cave.
Yellow
–
Paintings in the Tomb of Nakht in
ancient Egypt (15th century BC).
8.
Brown
–
In the CMYK color model used in printing or painting, brown is made by combining red, black, and yellow, or red, yellow, and blue. In the RGB color model used to project colors onto television screens and computer monitors, brown is made by combining red and green, the brown color is seen widely in nature, in wood, soil, human hair color, eye color and skin pigmentation. Brown is the color of wood or rich soil. According to public opinion surveys in Europe and the United States, brown is the least favorite color of the public, the color most often associated with plainness, the rustic, the term is from Old English brún, in origin for any dusky or dark shade of color. The first recorded use of brown as a name in English was in 1000. The Common Germanic adjective *brûnoz, *brûnâ meant both dark colors and a glistening or shining quality, whence burnish, the current meaning developed in Middle English from the 14th century. In Southeast Asia, the name often comes from chocolate, coklat in Malay. In Japan, the word means the color of tea. Brown has been used in art since prehistoric times, paintings using umber, a natural clay pigment composed of iron oxide and manganese oxide, have been dated to 40,000 BC. Paintings of brown horses and other animals have found on the walls of the Lascaux cave dating back about 17,300 years. The female figures in ancient Egyptian tomb paintings have brown skin, light tan was often used on painted Greek amphorae and vases, either as a background for black figures, or the reverse. The Ancient Greeks and Romans produced a fine reddish-brown ink, of a color called sepia and this ink was used by Leonardo da Vinci, Raphael and other artists during the Renaissance, and by artists up until the present time. In Ancient Rome, brown clothing was associated with the classes or barbarians. The term for the plebeians, or urban poor, was pullati, in the Middle Ages brown robes were worn by monks of the Franciscan order, as a sign of their humility and poverty. Each social class was expected to wear a color suitable to their station, russet was a coarse homespun cloth made of wool and dyed with woad and madder to give it a subdued grey or brown shade. By the statute of 1363, poor English people were required to wear russet, the medieval poem Piers Plowman describes the virtuous Christian, And is gladde of a goune of a graye russet As of a tunicle of Tarse or of trye scarlet. The umbers were not widely used in Europe before the end of the fifteenth century, artists began using far greater use of browns when oil painting arrived in the late fifteenth century. In Northern Europe, Jan van Eyck featured rich earth browns in his portraits to set off the brighter colors, the 17th and 18th century saw the greatest use of brown
Brown
–
The
Sahara Desert around Kufra Oasis,
Libya, seen from space
Brown
–
Brown
Brown
–
Chocolate. A
sachertorte in a Vienna cafe.
Brown
–
Espresso-roasted
coffee beans.
9.
Green
–
Green is the color between blue and yellow on the spectrum of visible light. It is evoked by light with a predominant wavelength of roughly 495–570 nm, the modern English word green comes from the Middle English and Anglo-Saxon word grene, from the same Germanic root as the words grass and grow. It is the color of living grass and leaves and as a result is the color most associated with springtime, growth, by far the largest contributor to green in nature is chlorophyll, the chemical by which plants photosynthesize and convert sunlight into chemical energy. Many creatures have adapted to their environments by taking on a green hue themselves as camouflage. Several minerals have a color, including the emerald, which is colored green by its chromium content. In surveys made in Europe and the United States, green is the color most commonly associated with nature, life, health, youth, spring, hope and envy. In Europe and the U. S. green is associated with death, sickness, or the devil. In the Middle Ages and Renaissance, when the color of clothing showed the social status, green was worn by merchants, bankers. The Mona Lisa by Leonardo da Vinci wears green, showing she is not from a noble family, Green is also the traditional color of safety and permission, a green light means go ahead, a green card permits permanent residence in the United States. It is the most important color in Islam and it was the color of the banner of Muhammad, and is found in the flags of nearly all Islamic countries, and represents the lush vegetation of Paradise. It is also associated with the culture of Gaelic Ireland. Because of its association with nature, it is the color of the environmental movement, political groups advocating environmental protection and social justice describe themselves as part of the Green movement, some naming themselves Green parties. This has led to campaigns in advertising, as companies have sold green, or environmentally friendly. The word green comes from the Middle English and Old English word grene, which, like the German word grün, has the same root as the words grass and grow. It is from a Common Germanic *gronja-, which is reflected in Old Norse grænn, Old High German gruoni, ultimately from a PIE root *ghre- to grow. The first recorded use of the word as a term in Old English dates to ca. Latin with viridis also has a genuine and widely used term for green, related to virere to grow and ver spring, it gave rise to words in several Romance languages, French vert, Italian verde. Likewise the Slavic languages with zelenъ, Ancient Greek also had a term for yellowish, pale green – χλωρός, chloros, cognate with χλοερός verdant and χλόη the green of new growth
Green
–
The word green has the same Germanic root as the words for grass and grow.
Green
–
Green
Green
–
Emerald green. The
Gachala Emerald from the
National Museum of Natural History, Washington.
Green
–
Jade. A jade dragon from the
Han Dynasty, China. Jade can be many different shades of green.
10.
Blue
–
Blue is the colour between violet and green on the optical spectrum of visible light. Human eyes perceive blue when observing light with a wavelength between 450 and 495 nanometres, which is between 4500 and 4950 ångströms. Blues with a frequency and thus a shorter wavelength gradually look more violet, while those with a lower frequency. Pure blue, in the middle, has a wavelength of 470 nanometers, in painting and traditional colour theory, blue is one of the three primary colours of pigments, along with red and yellow, which can be mixed to form a wide gamut of colours. Red and blue mixed together form violet, blue and yellow together form green, Blue is also a primary colour in the RGB colour model, used to create all the colours on the screen of a television or computer monitor. The clear sky and the sea appear blue because of an optical effect known as Rayleigh scattering. When sunlight passes through the atmosphere, the wavelengths are scattered more widely by the oxygen and nitrogen molecules. An optical effect called Tyndall scattering, similar to Rayleigh scattering, explains blue eyes, distant objects appear more blue because of another optical effect called atmospheric perspective. Blue has been used for art and decoration since ancient times and it is the most important color in Judaism. In the Middle Ages, cobalt blue was used to colour the stained glass windows of cathedrals, beginning in the 9th century, Chinese artists used cobalt to make fine blue and white porcelain. Blue dyes for clothing were made from woad in Europe and indigo in Asia, in 1828 a synthetic ultramarine pigment was developed, and synthetic blue dyes and pigments gradually replaced mineral pigments and vegetable dyes. Pierre-Auguste Renoir, Vincent van Gogh and other late 19th century painters used ultramarine and cobalt blue not just to depict nature, in the late 18th century and 19th century, blue became a popular colour for military uniforms and police uniforms. In the 20th century, because blue was associated with harmony, it was chosen as the colour of the flags of the United Nations. Surveys in the US and Europe show that blue is the colour most commonly associated with harmony, faithfulness, confidence, distance, infinity, the imagination, cold, and sometimes with sadness. In US and European public opinion polls it is the most popular colour, Blue is the colour of light between violet and green on the visible spectrum. Blues also vary in shade or tint, darker shades of blue contain black or grey, darker shades of blue include ultramarine, cobalt blue, navy blue, and Prussian blue, while lighter tints include sky blue, azure, and Egyptian blue. Today most blue pigments and dyes are made by a chemical process, the modern English word blue comes from Middle English bleu or blewe, from the Old French bleu, a word of Germanic origin, related to the Old High German word blao. In heraldry, the azure is used for blue
Blue
–
Sky blue or pale
azure, mid-way on the RBG colour wheel between blue and cyan.
Blue
–
Blue
Blue
–
Extract of natural
indigo, the most popular blue dye before the invention of synthetic dyes. It was the colour of the first
blue jeans.
Blue
–
A block of
lapis lazuli, originally used to make ultramarine.
11.
Iron
–
Iron is a chemical element with symbol Fe and atomic number 26. It is a metal in the first transition series and it is by mass the most common element on Earth, forming much of Earths outer and inner core. It is the fourth most common element in the Earths crust, like the other group 8 elements, ruthenium and osmium, iron exists in a wide range of oxidation states, −2 to +6, although +2 and +3 are the most common. Elemental iron occurs in meteoroids and other low oxygen environments, but is reactive to oxygen, fresh iron surfaces appear lustrous silvery-gray, but oxidize in normal air to give hydrated iron oxides, commonly known as rust. Unlike the metals that form passivating oxide layers, iron oxides occupy more volume than the metal and thus flake off, Iron metal has been used since ancient times, although copper alloys, which have lower melting temperatures, were used even earlier in human history. Pure iron is soft, but is unobtainable by smelting because it is significantly hardened and strengthened by impurities, in particular carbon. A certain proportion of carbon steel, which may be up to 1000 times harder than pure iron. Crude iron metal is produced in blast furnaces, where ore is reduced by coke to pig iron, further refinement with oxygen reduces the carbon content to the correct proportion to make steel. Steels and iron alloys formed with metals are by far the most common industrial metals because they have a great range of desirable properties. Iron chemical compounds have many uses, Iron oxide mixed with aluminium powder can be ignited to create a thermite reaction, used in welding and purifying ores. Iron forms binary compounds with the halogens and the chalcogens, among its organometallic compounds is ferrocene, the first sandwich compound discovered. Iron plays an important role in biology, forming complexes with oxygen in hemoglobin and myoglobin. Iron is also the metal at the site of many important redox enzymes dealing with cellular respiration and oxidation and reduction in plants. A human male of average height has about 4 grams of iron in his body and this iron is distributed throughout the body in hemoglobin, tissues, muscles, bone marrow, blood proteins, enzymes, ferritin, hemosiderin, and transport in plasma. The mechanical properties of iron and its alloys can be evaluated using a variety of tests, including the Brinell test, Rockwell test, the data on iron is so consistent that it is often used to calibrate measurements or to compare tests. An increase in the content will cause a significant increase in the hardness. Maximum hardness of 65 Rc is achieved with a 0. 6% carbon content, because of the softness of iron, it is much easier to work with than its heavier congeners ruthenium and osmium. Because of its significance for planetary cores, the properties of iron at high pressures and temperatures have also been studied extensively
Iron
–
Iron, 26 Fe
Iron
–
Spectral lines of iron
Iron
–
Iron meteorites, similar in composition to the Earth's inner- and outer core
Iron
–
Hydrated
iron(III) chloride, also known as ferric chloride
12.
Inclusion (mineral)
–
In mineralogy, an inclusion is any material that is trapped inside a mineral during its formation. In gemology, an inclusion is a characteristic enclosed within a gemstone, according to Huttons law of inclusions, fragments included in a host rock are older than the host rock itself. Inclusions are usually other minerals or rocks, but may also be water, liquid or vapor inclusions are known as fluid inclusions. In the case of amber it is possible to find insects and plants as inclusions, the analysis of atmospheric gas bubbles as inclusions in ice cores is an important tool in the study of climate change. A xenolith is a rock which has been picked up by a lava flow. Melt inclusions form when bits of melt become trapped inside crystals as they form in the melt, inclusions are one of the most important factors when it comes to gem valuation. In many gemstones, such as diamonds, inclusions affect the clarity of the gem, in some gems, however, such as star sapphires, the inclusion actually increases the value of the gem. Many colored gemstones, such as amethyst, emerald, and sapphire, are expected to have inclusions, colored gemstones are categorized into three types as follows, Type I colored gems include gems with very little or no inclusions. They include aquamarines, topaz and zircon, Type II colored gems include those that often have a few inclusions. They include sapphire, ruby, garnet and spinel, Type III colored gems include those that almost always have inclusions. Gems in this category include emerald and tourmaline, the term inclusion is also used in the context of metallurgy and metals processing. During the melt stage of processing hard particles such as oxides can enter or form in the metal which are subsequently trapped when the melt solidifies. The term is used negatively such as when the particle could act as a fatigue crack nucleator or as an area of high stress intensity
Inclusion (mineral)
–
Quartz crystal with
chlorite inclusion.
Inclusion (mineral)
–
Clear gemstone with metallic inclusion.
Inclusion (mineral)
–
Peridot with milky inclusion.
Inclusion (mineral)
–
Natural Ruby with inclusions.
13.
Gemstone
–
A gemstone is a piece of mineral crystal which, in cut and polished form, is used to make jewelry or other adornments. However, certain rocks or organic materials that are not minerals are used for jewelry and are therefore often considered to be gemstones as well. Most gemstones are hard, but some soft minerals are used in jewelry because of their luster or other properties that have aesthetic value. Rarity is another characteristic that lends value to a gemstone, apart from jewelry, from earliest antiquity engraved gems and hardstone carvings, such as cups, were major luxury art forms. A gem maker is called a lapidary or gemcutter, a worker is a diamantaire. The carvings of Carl Fabergé are significant works in this tradition, the traditional classification in the West, which goes back to the ancient Greeks, begins with a distinction between precious and semi-precious, similar distinctions are made in other cultures. In modern usage the precious stones are diamond, ruby, sapphire, other stones are classified by their color, translucency and hardness. Another unscientific term for semi-precious gemstones used in art history and archaeology is hardstone, in modern times gemstones are identified by gemologists, who describe gems and their characteristics using technical terminology specific to the field of gemology. The first characteristic a gemologist uses to identify a gemstone is its chemical composition, for example, diamonds are made of carbon and rubies of aluminium oxide. Next, many gems are crystals which are classified by their crystal system such as cubic or trigonal or monoclinic, another term used is habit, the form the gem is usually found in. For example, diamonds, which have a crystal system, are often found as octahedrons. Gemstones are classified into different groups, species, and varieties, for example, ruby is the red variety of the species corundum, while any other color of corundum is considered sapphire. Other examples are the Emerald, aquamarine, red beryl, goshenite, heliodor, and morganite, gems are characterized in terms of refractive index, dispersion, specific gravity, hardness, cleavage, fracture, and luster. They may exhibit pleochroism or double refraction and they may have luminescence and a distinctive absorption spectrum. Material or flaws within a stone may be present as inclusions, gemstones may also be classified in terms of their water. This is a grading of the gems luster, transparency. Very transparent gems are considered first water, while second or third water gems are those of a lesser transparency, there is no universally accepted grading system for gemstones. Diamonds are graded using a system developed by the Gemological Institute of America in the early 1950s, historically, all gemstones were graded using the naked eye
Gemstone
–
A selection of gemstone pebbles made by tumbling rough rock with abrasive grit, in a rotating drum. The biggest pebble here is 40 mm long (1.6 inches).
Gemstone
–
Group of precious and semiprecious stones —both uncut and faceted— including (clockwise from top left)
diamond, uncut synthetic
sapphire,
ruby, uncut
emerald, and
amethyst crystal cluster.
Gemstone
–
Spanish emerald and gold pendant at
Victoria and Albert Museum
Gemstone
–
Enamelled gold, amethyst and pearl pendant, about 1880, Pasquale Novissimo (1844–1914), V&A Museum number M.36-1928
14.
Seal (emblem)
–
A seal is a device for making an impression in wax, clay, paper, or some other medium, including an embossment on paper, and is also the impression thus made. The original purpose was to authenticate a document, a wrapper for one such as a modern envelope, the seal-making device is also referred to as the seal matrix or die, the imprint it creates as the seal impression. In most traditional forms of dry seal the design on the matrix is in intaglio. The design on the impression will reverse that of the matrix and this will not be the case if paper is embossed from behind, where the matrix and impression read the same way, and both matrix and impression are in relief. However engraved gems were carved in relief, called cameo in this context. The process is essentially that of a mould and these pendent seal impressions dangled below the documents they authenticated, to which the attachment tag was sewn or otherwise attached. Some jurisdictions consider rubber stamps or specified signature-accompanying words such as seal or L. S. to be the equivalent of, i. e. an equally effective substitute for. In Europe, although coats of arms and heraldic badges may well feature in such contexts as well as on seals, the study of seals is known as sigillography or sphragistics. Seals were used in the earliest civilizations and are of importance in archaeology. In ancient Mesopotamia carved or engraved cylinder seals in stone or other materials were used and these could be rolled along to create an impression on clay, and used as labels on consignments of trade goods, or for other purposes. They are normally hollow and it is presumed that they were worn on a string or chain round the neck, many have only images, often very finely carved, with no writing, while others have both. From Ancient Egypt seals in the form of signet-rings, including some with the names of kings, have been found, recently, seals have come to light in South Arabia datable to the Himyarite age. One example shows a name written in Aramaic engraved in reverse so as to read correctly in the impression, from the beginning of the 3rd millennium BC until the Middle Ages, seals of various kinds were in production in the Aegean islands and mainland Greece. In the Early Minoan age these were formed of stone and ivory. By the Middle Minoan age a new set for seal forms, motifs, hard stone requires new rotary carving techniques. The Late Bronze Age is the par excellence of the lens-shaped seal and the seal ring. These were a luxury art form and became keenly collected. His collection fell as booty to Pompey the Great, who deposited it in a temple in Rome, engraved gems continued to be produced and collected until the 19th century
Seal (emblem)
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Present-day impression of a Late Bronze Age seal
Seal (emblem)
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Town seal (matrix) of
Náchod from 1570
Seal (emblem)
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Mesopotamian limestone
cylinder seal and impression—worship of
Shamash
Seal (emblem)
–
A Baiwen name seal, read up-down-right-left: Ye Hao Min Yin (lit. "Seal of Ye Haomin")
15.
Decorative box
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A decorative box is a form of packaging that is generally more than just functional, but also intended to be decorative and artistic. Many such boxes are used for packaging, both commercially and privately. Historical objects are usually called caskets if larger than a few inches in more than one dimension, traditionally gift boxes used for promotional and seasonal gifts are made from sturdy paperboard or corrugated fiberboard. These boxes normally consist of a base and detachable lid and are made by using a die cutting process to cut the board, the box is then covered with decorative paper. Gift boxes can be dressed with other gift packaging material, such as decorative ribbons, the most common type of decorative box is the feminine work box. It is usually fitted with a divided into many small compartments for needles, reels of silk and cotton. The date of its origin is unclear, but 17th-century examples exist, covered with silk and adorned with beads, no lady would have been without her work box in the 18th century. In the second half of century, elaborate pains were taken to make these boxes dainty. Work boxes are portable, but at times they form the top of a stationary table. A jewelry box, also known as a casket, is a receptacle for trinkets, snuff boxes are made in two sizes, ones for the pocket and communal boxes made for table use. Pocket boxes are made to hold a small amount of snuff for immediate consumption. High-quality boxes have tightly-sealed lids to ensure that air does not penetrate the box, pocket boxes are intended keep a day or twos supply. Table boxes are still to be found in the mess of certain old regiments - often in the rams head style -. Boxes made for the poorer snuff taker were more ordinary, popular and cheap boxes were made in papier-mâché and even potato-pulp, alloys that resembled gold or silver were developed in the 18th and 19th centuries such as the ersatz gold Pinchbeck and the silver look-alike, Sheffield Plate. The lids were often adorned with a portrait, a vignette, portrait miniature, hardstone inlays. Some of the most expensive just used subtly different colours of gold, perhaps the most widely used semi-precious metal was silver and snuffs of all shapes and sizes were made in that metal during snuffs great popularity. Monarchs retained the habit of bestowing snuff-boxes upon ambassadors and other intermediaries as a form of honor, as Talleyrand explained, the diplomatic corps found a ceremonious pinch to be a useful aid to reflection in a business interview. At the coronation of George IV of England, Messrs, rundell and Bridge, the court jewellers, were paid £8,205 for snuff-boxes for gifts to foreign representatives
Decorative box
–
18th century German gold and
mother of pearl snuffbox
Decorative box
–
Chinese mother of pearl lacquer box with
peony decor
Ming Dynasty
Decorative box
–
Elizabeth E Copeland (1866–1957) covered Box, circa 1915 metalwork, silver and
cloisonné,
Los Angeles County Museum of Art
Decorative box
–
A jewel box lined with red velvet
16.
Specific gravity
–
This page is about the measurement using water as a reference. For a general use of gravity, see relative density. See intensive property for the property implied by specific, Apparent specific gravity is the ratio of the weight of a volume of the substance to the weight of an equal volume of the reference substance. The reference substance is always water at its densest for liquids. Nonetheless, the temperature and pressure must be specified for both the sample and the reference, pressure is nearly always 1 atm. Temperatures for both sample and reference vary from industry to industry, in British beer brewing, the practice for specific gravity as specified above is to multiply it by 1000. Being a ratio of densities, specific gravity is a dimensionless quantity, Specific gravity varies with temperature and pressure, reference and sample must be compared at the same temperature and pressure or be corrected to a standard reference temperature and pressure. Substances with a gravity of 1 are neutrally buoyant in water. Those with SG greater than 1 are denser than water and will, disregarding surface tension effects and those with an SG less than 1 are less dense than water and will float on it. In scientific work, the relationship of mass to volume is expressed directly in terms of the density of the substance under study. It is in industry where specific gravity finds wide application, often for historical reasons. True specific gravity can be expressed mathematically as, S G true = ρ sample ρ H2 O where ρ sample is the density of the sample, the density of water varies with temperature and pressure as does the density of the sample. So it is necessary to specify the temperatures and pressures at which the densities or weights were determined and it is nearly always the case that measurements are made at 1 nominal atmosphere. For true specific gravity calculations, air pressure must be considered, temperatures are specified by the notation with T s representing the temperature at which the samples density was determined and T r the temperature at which the reference density is specified. For example, SG would be understood to mean that the density of the sample was determined at 20°C and of the water at 4°C. Taking into account different sample and reference temperatures, we note that, while S G H2 O =1.000000, it is also the case that S G H2 O =0.998203 /0.999840 =0.998363. Here, temperature is being specified using the current ITS-90 scale, on the previous IPTS-68 scale, the densities at 20 °C and 4 °C are 0.9982071 and 0.9999720 respectively, resulting in an SG value for water of 0.9982343. For example, in the industry, the Plato table lists sucrose concentration by weight against true SG
Specific gravity
–
Testing specific gravity of fuel.
17.
Heliotrope (mineral)
–
The mineral aggregate heliotrope, also known as bloodstone, is a variety of jasper or chalcedony. The classic bloodstone is green jasper with red inclusions of hematite, the red inclusions are supposed to resemble spots of blood, hence the name bloodstone. The name heliotrope derives from ancient notions about the manner in which the mineral reflects light. These are described, e. g. by Pliny the Elder, heliotrope was called stone of Babylon by Albert the Great and he referred to several magical properties, which were attributed to it from Late Antiquity. Pliny the Elder mentioned first that the magicians used it as a stone of invisibility, damigeron wrote about its property to make rain, solar eclipse and its special virtue in divination and preserving health and youth. Heliotrope features as an invisibility stone in one of Boccaccios stories in the Decameron, heliotrope is sometimes used in carved signet rings and is the traditional birthstone for March. The primary source of the stone is India and it is also found in Armenia, Azerbaijan, Brazil, Bulgaria, China, Australia, and the United States. There is also an outcrop of bloodstone on the Isle of Rum, media related to Heliotrop at Wikimedia Commons
Heliotrope (mineral)
–
A heliotrope, also known as a bloodstone.
18.
Banded iron formation
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Banded iron formations are distinctive units of sedimentary rock that are almost always of Precambrian age. Some of the oldest known rock formations, formed over 3,700 million years ago, Banded layers rich in iron were mostly deposited between 2,400 and 1,900 mya. Phanerozoic ironstones generally have a different genesis, Banded iron beds are an important commercial source of iron ore, such as the Pilbara region of Western Australia and the Animikie Group in Minnesota. The formations are abundant around the time of the great event,2,400 million years ago. The conventional concept is that the banded iron layers were formed in sea water as the result of oxygen released by photosynthetic cyanobacteria. The oxygen then combined with dissolved iron in Earths oceans to form insoluble iron oxides, which precipitated out, forming a layer on the ocean floor. Each band is similar to a varve, to the extent that the banding is assumed to result from variations in available oxygen. It is unclear whether these banded ironstone formations were seasonal, followed some feedback oscillation in the complex system or followed some other cycle. It is assumed that initially the Earth started with vast amounts of iron, as photosynthetic organisms generated oxygen, the available iron in the Earths oceans precipitated out as iron oxides. An alternative explanation of these deposits has undergone much discussion as part of the Snowball Earth hypothesis. Several hypotheses exist for the initiation of the Snowball Earths, in a Snowball Earth state the earths continents, and possibly seas at low latitudes, were subject to an ice age. If this was the case, Earths free oxygen may have nearly or totally depleted during a severe ice age circa 750 to 580 million years ago. Dissolved iron then accumulated in the oxygen-poor oceans, following the thawing of the Earth, the seas became oxygenated once more causing the precipitation of the iron. Another mechanism for BIFs, also proposed in the context of the Snowball Earth discussion, is by deposition from metal-rich brines in the vicinity of hydrothermally active rift zones, alternatively, some geochemists suggest that BIFs could form by direct oxidation of iron by microbial anoxygenic phototrophs. Northern Minnesotas banded iron formations lie directly underneath a layer of material only recently recognized as ejecta from the Sudbury Basin impact. At the time of formation Earth had a single supercontinent called Columbia with substantial continental shelves, an asteroid slammed into waters about 1,000 m deep some 1.85 billion years ago. Computer models suggest that the tsunami would have been at least 1,000 m at the epicentre and those immense waves and large underwater landslides triggered by the impact stirred the ocean, bringing oxygenated waters from the surface down to the ocean floor. Sediments deposited on the seafloor before the impact, including BIFs contained little if any oxidized iron and this Fe to Fe ratio suggests that most parts of the ocean were relatively devoid of oxygen
Banded iron formation
–
Banded iron formation,
Karijini National Park,
Western Australia
Banded iron formation
–
2.1 billion year old rock showing banded iron formation
Banded iron formation
–
Close-up of banded iron formation specimen from Upper Michigan. Scale bar is 5.0 mm.
Banded iron formation
–
An ashtray carved out of a soft form of banded ironstone from the 3.5 billion year old
Barbeton Supergroup in South Africa. The red layers were laid down during the daylight hours when Archaean photosynthesizing cyanobacteria produced oxygen that immediately reacted with dissolved iron compounds in the water, to form insoluble iron oxide (rust). The white layers are sediments that settled during the night when there was no oxygen in the water.
19.
Walters Art Museum
–
The Walters Art Museum, located in Mount Vernon-Belvedere, Baltimore, Maryland, is a public art museum founded and opened in 1934. It holds collections established during the mid-19th Century, located across the back alley, a block south of the Walters mansion on West Monument Street/Mount Vernon Place, on the northwest corner of North Charles Street at West Centre Street. The following year, The Walters reopened its original building after a dramatic three-year physical renovation and replacement of internal utilities. The Archimedes Palimpsest was on loan to the Walters Art Museum from a collector for conservation. This was one of the largest and most comprehensive such releases made by any museum, the Walters collection of ancient art includes examples from Egypt, Nubia, Greece, Rome, Etruria and the Near East. In 1911, Henry Walters purchased almost 100 gold artifacts from the Chiriqui region of western Panama in Central America, the museum owns the oldest surviving Chinese wood-and-lacquer image of the Buddha. It is exhibited in a gallery dedicated solely to this work, the Museum holds one of the largest and finest collections of Thai bronze, scrolls, and banner paintings in the world. Islamic art in all media is represented at the Walters, the Walters Museum owns an array of Islamic manuscripts. Walters Art Museum, MS W.613 contains five Mughal miniatures from a very important Khamsa of Nizami made for the Emperor Akbar, Henry Walters assembled a collection of art produced during the Middle Ages in all the major artistic media of the period. This forms the basis of the Walters medieval collection, for which the Museum is best known internationally. Considered one of the best collections of art in the United States, the Museums holdings include examples of metalwork, sculpture, stained glass, textiles, icons. Sculpted heads from the royal Abbey of St. Denis are rare surviving examples of sculptures that are directly connected with the origins of Gothic art in 12th Century France. An ivory casket covered with scenes of jousting knights is one of about a dozen such objects to survive in the world, many of these works are on display in the Museums galleries. Works in the collection are the subject of active research by the curatorial and conservation departments of the museum. The collection of European Renaissance and Baroque art features holdings of paintings, sculpture, furniture, ceramics, metal work, arms, the museum has one of ten surviving examples of the Sèvres pot-pourri vase in the shape of a ship from the 1750s and 1760s. William and Henry Walters collected works by late 19th Century French academic masters, Henry Walters was particularly interested in the courtly arts of 18th Century France. The museum’s collection of Sèvres porcelain includes a number of pieces that were made for members of the Royal Bourbon Court at Versailles Palace outside of Paris. Portrait miniatures and the examples of works, especially snuffboxes and watches, are displayed in the Treasury, along with some exceptional 19th-
Walters Art Museum
–
North Charles Street original main entrance to the Walters Art Museum
Walters Art Museum
–
Sculpture Garden (central "Great Hall") of the Walters Art Gallery (now Walters Art Museum) in the original Main Building of 1905-1909
Walters Art Museum
–
Sumerian male worshiper, c.2300 BC
Walters Art Museum
–
"
Padiiset's Statue ", illustrates
Canaan -
Ancient Egypt trade, c.1700 B.C. (inscription c.900 B.C.)
20.
Kremlin Armoury
–
The Kremlin Armoury or Armoury Chamber is one of the oldest museums of Moscow, established in 1851 and located in the Moscow Kremlin. The name Armoury Chamber is officially used by the museum of the Moscow Kremlin. The Kremlin Armoury originated as the arsenal in 1508. Until the transfer of the court to St Petersburg, the Armoury was in charge of producing, purchasing and storing weapons, jewelry, the finest Muscovite gunsmiths, jewelers, and painters used to work there. In 1640 and 1683, they opened the iconography and pictorial studios, in 1700, the Armoury was enriched with the treasures of the Golden and Silver chambers of the Russian tsars. In 1711, Peter the Great had the majority of masters transferred to his new capital,15 years later, the Armoury was merged with the Fiscal Yard, Stables Treasury and the Master Chamber. After that, the Armoury was renamed into the Arms and Master Chamber, Alexander I of Russia nominated the Armoury as the first public museum in Moscow in 1806, but the collections were not opened to the public until seven years later. The current Armoury building was erected in 1844-1851 by the imperial architect Konstantin Ton, the director of the museum from 1852 to 1870 was the writer Alexander Veltman. After the Bolshevik Revolution, the Armoury collection was enriched with treasures taken from the Patriarch sacristy, Kremlin cathedrals, monasteries, some of these were sold abroad on behest of Joseph Stalin in the 1930s. In 1960, the Armoury became the museum of the Kremlin. Two years later, the Patriarch chambers and the Cathedral of the Twelve Apostles were assigned to the Armoury in order to house the Applied Arts Museum, the Kremlin Armoury is currently home to the Russian Diamond Fund. It boasts unique collections of the Russian, Western European and Eastern applied arts spanning the period from the 5th to the 20th centuries, the ten Fabergé eggs in the Armoury collection are the most Imperial eggs, and the second-most overall Fabergé eggs, owned by a single owner
Kremlin Armoury
–
Moscow Armoury
Kremlin Armoury
–
Kremlin Wall and
Towers
21.
Old French
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Old French was the Gallo-Romance dialect continuum spoken from the 9th century to the 14th century. In the 14th century, these came to be collectively known as the langues doïl. The mid-14th century is taken as the period to Middle French. The areal of Old French in contemporary terms corresponded to the parts of the Kingdom of France, Upper Burgundy. As part of the emerging Gallo-Romance dialect continuum, the langues doïl were contrasted with the langue doc, in these examples, we notice a clear consequence of bilingualism, that sometimes even changed the first syllable of the Latin words. Pope estimated that perhaps still 15% of the vocabulary of modern French derives from Germanic sources, at the third Council of Tours in 813, priests were ordered to preach in the vernacular language, since the common people could no longer understand formal Latin. The second-oldest document in Old French is the Eulalia sequence, which is important for reconstruction of Old French pronunciation due to its consistent spelling. The Capetians langue doïl, the forerunner of modern standard French, did not begin to become the common speech of all of France, however, until after the French Revolution. In the Late Middle Ages, the Old French dialects diverged into a number of distinct langues doïl, during the Early Modern period, French now becomes established as the official language of the Kingdom of France throughout the realm, also including the langue doc-speaking territories in the south. Old French gives way to Middle French in the mid-14th century, the earliest extant French literary texts date from the ninth century, but very few texts before the 11th century have survived. The first literary works written in Old French were saints lives, the Canticle of Saint Eulalie, written in the second half of the 9th century, is generally accepted as the first such text. The first of these is the area of the chansons de geste. More than one hundred chansons de geste have survived in three hundred manuscripts. The oldest and most celebrated of the chansons de geste is The Song of Roland, a fourth grouping, not listed by Bertrand, is the Crusade cycle, dealing with the First Crusade and its immediate aftermath. Jean Bodels other two categories—the Matter of Rome and the Matter of Britain—concern the French romance or roman, around a hundred verse romances survive from the period 1150–1220. From around 1200 on, the tendency was increasingly to write the romances in prose, the most important romance of the 13th century is the Romance of the Rose which breaks considerably from the conventions of the chivalric adventure story. The Occitan or Provençal poets were called troubadours, from the word trobar to find, lyric poets in Old French are called trouvères. By the late 13th century, the tradition in France had begun to develop in ways that differed significantly from the troubadour poets
Old French
–
Map of France in 1180, at the height of the
feudal system. The
possessions of the French king are in light blue, vassals to the French king in green,
Angevin possessions in red. Shown in white is the
Holy Roman Empire to the east, the western fringes of which, including
Upper Burgundy and
Lorraine were also part of the Old French areal.
22.
Anglo-Norman language
–
Anglo-Norman, also known as Anglo-Norman French, is a variety of the Norman language that was used in England and, to a lesser extent, elsewhere in the British Isles during the Anglo-Norman period. One of these was Old Norman, also known as Old Northern French, other followers spoke varieties of the Picard language or western French. It was spoken in the law courts, schools, and universities and, in due course, in at least some sections of the gentry and the growing bourgeoisie. Private and commercial correspondence was carried out in Anglo-Norman or Anglo-French from the 13th to the 15th century though its spelling forms were often displaced by continental spellings. Social classes other than the nobility became keen to learn French, manuscripts containing materials for instructing non-native speakers still exist, although Anglo-Norman and Anglo-French were eventually eclipsed by modern English, they had been used widely enough to influence English vocabulary permanently. Thus, many original Germanic words, cognates of which can still be found in Nordic, German, other such examples are heir apparent, court martial, and body politic. The Royal coat of arms of the United Kingdom still features in French the mottos of both the British Monarch, Dieu et mon droit and the Order of the Garter, Honi soit qui mal y pense. Dieu et mon droit was first used by Richard I in 1198, the motto appears below the shield of the Royal Coat of Arms. Anglo-Norman was never the administrative language of England, Latin was the major language of record in legal. There is evidence, too, that foreign words often entered English via Anglo-Norman, by the late 15th century, however, what remained of insular French had become heavily anglicised, see Law French. It continued to be known as Norman French until the end of the 19th century even though, philologically, among important writers of the Anglo-Norman cultural commonwealth is Marie de France. Much of the earliest recorded French is in fact Anglo-Norman French, Latin did not disappear in medieval England either, it was used by the Church, the royal government and much local administration, as it had been before 1066, in parallel with Middle English. The early adoption of Anglo-Norman as a written and literary language probably owes something to this history of bilingualism in writing, thus, typically, local records are rather different from continental French, with diplomatic and international trade documents closest to the emerging continental norm. English remained the vernacular of the people throughout this period. The resulting virtual trilinguism in spoken and written language was one of medieval Latin, diverse French varieties, from the conquest until the end of the 14th century, French was the language of the king and his court. During this period, marriages with French princesses reinforced the French status in the royal family, nevertheless, during the 13th century, intermarriages with English nobility became more frequent. French became progressively a second language among the upper classes, moreover, with the Hundred Years War and the growing spirit of English nationalism, the status of French diminished. French was the tongue of every English king from William the Conqueror until Henry IV
Anglo-Norman language
–
About 28% of English
vocabulary comes from French, including the Anglo-French language (green)
23.
Latin
–
Latin is a classical language belonging to the Italic branch of the Indo-European languages. The Latin alphabet is derived from the Etruscan and Greek alphabets, Latin was originally spoken in Latium, in the Italian Peninsula. Through the power of the Roman Republic, it became the dominant language, Vulgar Latin developed into the Romance languages, such as Italian, Portuguese, Spanish, French, and Romanian. Latin, Italian and French have contributed many words to the English language, Latin and Ancient Greek roots are used in theology, biology, and medicine. By the late Roman Republic, Old Latin had been standardised into Classical Latin, Vulgar Latin was the colloquial form spoken during the same time and attested in inscriptions and the works of comic playwrights like Plautus and Terence. Late Latin is the language from the 3rd century. Later, Early Modern Latin and Modern Latin evolved, Latin was used as the language of international communication, scholarship, and science until well into the 18th century, when it began to be supplanted by vernaculars. Ecclesiastical Latin remains the language of the Holy See and the Roman Rite of the Catholic Church. Today, many students, scholars and members of the Catholic clergy speak Latin fluently and it is taught in primary, secondary and postsecondary educational institutions around the world. The language has been passed down through various forms, some inscriptions have been published in an internationally agreed, monumental, multivolume series, the Corpus Inscriptionum Latinarum. Authors and publishers vary, but the format is about the same, volumes detailing inscriptions with a critical apparatus stating the provenance, the reading and interpretation of these inscriptions is the subject matter of the field of epigraphy. The works of several hundred ancient authors who wrote in Latin have survived in whole or in part and they are in part the subject matter of the field of classics. The Cat in the Hat, and a book of fairy tales, additional resources include phrasebooks and resources for rendering everyday phrases and concepts into Latin, such as Meissners Latin Phrasebook. The Latin influence in English has been significant at all stages of its insular development. From the 16th to the 18th centuries, English writers cobbled together huge numbers of new words from Latin and Greek words, dubbed inkhorn terms, as if they had spilled from a pot of ink. Many of these words were used once by the author and then forgotten, many of the most common polysyllabic English words are of Latin origin through the medium of Old French. Romance words make respectively 59%, 20% and 14% of English, German and those figures can rise dramatically when only non-compound and non-derived words are included. Accordingly, Romance words make roughly 35% of the vocabulary of Dutch, Roman engineering had the same effect on scientific terminology as a whole
Latin
–
Latin inscription, in the
Colosseum
Latin
–
Julius Caesar 's
Commentarii de Bello Gallico is one of the most famous classical Latin texts of the Golden Age of Latin. The unvarnished, journalistic style of this
patrician general has long been taught as a model of the urbane Latin officially spoken and written in the floruit of the
Roman republic.
Latin
–
A multi-volume Latin dictionary in the
University Library of Graz
Latin
–
Latin and Ancient Greek Language - Culture - Linguistics at
Duke University in 2014.
24.
Greek language
–
Greek is an independent branch of the Indo-European family of languages, native to Greece and other parts of the Eastern Mediterranean. It has the longest documented history of any living language, spanning 34 centuries of written records and its writing system has been the Greek alphabet for the major part of its history, other systems, such as Linear B and the Cypriot syllabary, were used previously. The alphabet arose from the Phoenician script and was in turn the basis of the Latin, Cyrillic, Armenian, Coptic, Gothic and many other writing systems. Together with the Latin texts and traditions of the Roman world, during antiquity, Greek was a widely spoken lingua franca in the Mediterranean world and many places beyond. It would eventually become the official parlance of the Byzantine Empire, the language is spoken by at least 13.2 million people today in Greece, Cyprus, Italy, Albania, Turkey, and the Greek diaspora. Greek roots are used to coin new words for other languages, Greek. Greek has been spoken in the Balkan peninsula since around the 3rd millennium BC, the earliest written evidence is a Linear B clay tablet found in Messenia that dates to between 1450 and 1350 BC, making Greek the worlds oldest recorded living language. Among the Indo-European languages, its date of earliest written attestation is matched only by the now extinct Anatolian languages, the Greek language is conventionally divided into the following periods, Proto-Greek, the unrecorded but assumed last ancestor of all known varieties of Greek. The unity of Proto-Greek would have ended as Hellenic migrants entered the Greek peninsula sometime in the Neolithic era or the Bronze Age, Mycenaean Greek, the language of the Mycenaean civilisation. It is recorded in the Linear B script on tablets dating from the 15th century BC onwards, Ancient Greek, in its various dialects, the language of the Archaic and Classical periods of the ancient Greek civilisation. It was widely known throughout the Roman Empire, after the Roman conquest of Greece, an unofficial bilingualism of Greek and Latin was established in the city of Rome and Koine Greek became a first or second language in the Roman Empire. The origin of Christianity can also be traced through Koine Greek, Medieval Greek, also known as Byzantine Greek, the continuation of Koine Greek in Byzantine Greece, up to the demise of the Byzantine Empire in the 15th century. Much of the written Greek that was used as the language of the Byzantine Empire was an eclectic middle-ground variety based on the tradition of written Koine. Modern Greek, Stemming from Medieval Greek, Modern Greek usages can be traced in the Byzantine period and it is the language used by the modern Greeks, and, apart from Standard Modern Greek, there are several dialects of it. In the modern era, the Greek language entered a state of diglossia, the historical unity and continuing identity between the various stages of the Greek language is often emphasised. Greek speakers today still tend to regard literary works of ancient Greek as part of their own rather than a foreign language and it is also often stated that the historical changes have been relatively slight compared with some other languages. According to one estimation, Homeric Greek is probably closer to demotic than 12-century Middle English is to modern spoken English, Greek is spoken by about 13 million people, mainly in Greece, Albania and Cyprus, but also worldwide by the large Greek diaspora. Greek is the language of Greece, where it is spoken by almost the entire population
Greek language
–
Idealized portrayal of
Homer
Greek language
–
regions where Greek is the official language
Greek language
–
Greek language road sign, A27 Motorway, Greece
25.
Hebrew language
–
Hebrew is a language native to Israel, spoken by over 9 million people worldwide, of whom over 5 million are in Israel. Historically, it is regarded as the language of the Israelites and their ancestors, the earliest examples of written Paleo-Hebrew date from the 10th century BCE. Hebrew belongs to the West Semitic branch of the Afroasiatic language family, Hebrew is the only living Canaanite language left, and the only truly successful example of a revived dead language. Hebrew had ceased to be a spoken language somewhere between 200 and 400 CE, declining since the aftermath of the Bar Kokhba revolt. Aramaic and to a lesser extent Greek were already in use as international languages, especially among elites and it survived into the medieval period as the language of Jewish liturgy, rabbinic literature, intra-Jewish commerce, and poetry. Then, in the 19th century, it was revived as a spoken and literary language, and, according to Ethnologue, had become, as of 1998, the language of 5 million people worldwide. After Israel, the United States has the second largest Hebrew-speaking population, with 220,000 fluent speakers, Modern Hebrew is one of the two official languages of the State of Israel, while premodern Hebrew is used for prayer or study in Jewish communities around the world today. Ancient Hebrew is also the tongue of the Samaritans, while modern Hebrew or Arabic is their vernacular. For this reason, Hebrew has been referred to by Jews as Leshon Hakodesh, the modern word Hebrew is derived from the word Ivri, one of several names for the Israelite people. It is traditionally understood to be a based on the name of Abrahams ancestor, Eber. This name is based upon the root ʕ-b-r meaning to cross over. Interpretations of the term ʕibrim link it to this verb, cross over, in the Bible, the Hebrew language is called Yәhudit because Judah was the surviving kingdom at the time of the quotation. In Isaiah 19,18 it is called the Language of Canaan, Hebrew belongs to the Canaanite group of languages. In turn, the Canaanite languages are a branch of the Northwest Semitic family of languages, according to Avraham ben-Yosef, Hebrew flourished as a spoken language in the Kingdoms of Israel and Judah during about 1200 to 586 BCE. Scholars debate the degree to which Hebrew was a vernacular in ancient times following the Babylonian exile. In July 2008 Israeli archaeologist Yossi Garfinkel discovered a ceramic shard at Khirbet Qeiyafa which he claimed may be the earliest Hebrew writing yet discovered, dating around 3000 years ago. The Gezer calendar also dates back to the 10th century BCE at the beginning of the Monarchic Period, classified as Archaic Biblical Hebrew, the calendar presents a list of seasons and related agricultural activities. The Gezer calendar is written in an old Semitic script, akin to the Phoenician one that through the Greeks, the Gezer calendar is written without any vowels, and it does not use consonants to imply vowels even in the places where later Hebrew spelling requires it
Hebrew language
–
Hebrew street sign, above in
Hebrew alphabet, below in
Latin transliteration. Aluf Batslut veAluf Shum (he) ("The Onion Champion and the Garlic Champion") is a
play by
Hayim Nahman Bialik.
Hebrew language
–
Portion of the
Temple Scroll, one of the longest of the
Dead Sea Scrolls discovered at
Qumran
Hebrew language
–
The
Shebna Inscription, from the tomb of a royal steward found in
Siloam, dates to the 7th century BCE.
Hebrew language
–
Hebrew script used in writing a Torah scroll. Note ornamental "crowns" on tops of certain letters.
26.
Akkadian language
–
Akkadian is an extinct East Semitic language that was spoken in ancient Mesopotamia. The earliest attested Semitic language, it used the writing system, which was originally used to write the unrelated Ancient Sumerian. The language was named after the city of Akkad, a centre of Mesopotamian civilization during the Akkadian Empire. The mutual influence between Sumerian and Akkadian had led scholars to describe the languages as a sprachbund, Akkadian proper names were first attested in Sumerian texts from around the mid 3rd-millennium BC. From the second half of the third millennium BC, texts written in Akkadian begin to appear. By the second millennium BC, two variant forms of the language were in use in Assyria and Babylonia, known as Assyrian and Babylonian respectively, for centuries, Akkadian was the native language in Mesopotamian nations such as Assyria and Babylonia. However, it began to decline during the Neo-Assyrian Empire around the 8th century BC, by the Hellenistic period, the language was largely confined to scholars and priests working in temples in Assyria and Babylonia. The last known Akkadian cuneiform document dates from the 1st century AD, Akkadian belongs with the other Semitic languages in the Near Eastern branch of the Afroasiatic languages, a family native to East Africa, which then spread to West, Northwest and Northeast Africa. Within the Near Eastern Semitic languages, Akkadian forms an East Semitic subgroup and this novel word order is due to the influence of the Sumerian substratum, which has an SOV order. Additionally Akkadian is the only Semitic language to use the prepositions ina and ana, other Semitic languages like Arabic and Aramaic have the prepositions bi/bə and li/lə. The origin of the Akkadian spatial prepositions is unknown, in contrast to most other Semitic languages, Akkadian has only one non-sibilant fricative, ḫ. Akkadian lost both the glottal and pharyngeal fricatives, which are characteristic of the other Semitic languages, until the Old Babylonian period, the Akkadian sibilants were exclusively affricated. Old Akkadian is preserved on clay tablets dating back to c.2500 BC and it was written using cuneiform, a script adopted from the Sumerians using wedge-shaped symbols pressed in wet clay. As employed by Akkadian scribes, the cuneiform script could represent either Sumerian logograms, Sumerian syllables, Akkadian syllables. For this reason, the sign AN can on the one hand be a logogram for the word ilum, additionally, this sign was used as a determinative for divine names. Another peculiarity of Akkadian cuneiform is that many signs do not have a phonetic value. Certain signs, such as AḪ, do not distinguish between the different vowel qualities, nor is there any coordination in the other direction, the syllable -ša-, for example, is rendered by the sign ŠA, but also by the sign NĪĜ. Both of these are used for the same syllable in the same text
Akkadian language
–
An Akkadian inscription
Akkadian language
–
Cuneiform writing (Neoassyrian script) (1 = Logogram (LG) "mix"/syllabogram (SG) ḫi, 2 = LG "moat", 3 = SG aʾ, 4 = SG aḫ, eḫ, iḫ, uḫ, 5 = SG kam, 6 = SG im, 7 = SG bir)
Akkadian language
–
The
Deluge tablet of the
Gilgamesh epic in Akkadian.
Akkadian language
–
Geography
27.
Bow drill
–
The bow drill is a prehistoric form of drilling tool. It commonly was used to make fire, and in this function it also was called a fire drill. However, the principle also was used widely in drilling for purposes of woodworking. Bow drills were used in Mehrgarh between the 4th and 5th millennium BC and this bow drill—used to drill holes into lapis lazuli and carnelian—was made of green jasper. Similar drills were found in parts of the Indus Valley Civilization. The bow drill consists of a block or handhold, a spindle or drill, a hearth or fireboard. Other early versions of mechanical drills include the drill and the hand drill. The drill offers an ancient method of starting fire without matches or a lighter, the heat eventually produces an ember in the burnt sawdust. The ember is tiny, smaller than the head of a cigarette, once the ember is formed it is carefully placed into a tinder bundle. Once the ember is in the tinder bundle it is then carefully nurtured and coaxed into flame, once the tinder bundle bursts into flame, it is placed into the fuel that has been assembled ready for ignition. The spindle, carved to reduce friction at one end and maximize it at the other, is held in a hole in the bottom of the bearing block, and at the other by the base board. The string of the bow is wrapped once around it, so that it is tight enough not to slip during operation. The usual position that a person assumes whilst operating the bow drill is as follows, the knee is placed on the ground. The heat of the friction between the hearth and the spindle both creates charred, fuzzy dust and causes it to ignite - forming a coal or ember, the handhold is lubricated and the spindle is carved to about thumb thickness, usually 6 to 8 inches long. Another option to practice is to make the handhold into a piece, so its held down by pressure from the chin/mouth. An indentation and a v notch into the center of the dent is made into the fireboard, the notch allows a place for the dust collect while it is being abraded off the spindle and the hearth. Eventually, the friction generates heat to ignite the dust, which can be used to light tinder, whilst a v is most common, other methods to create a cavity to contain the dust whilst it is being ignited can be used. For example, drilling part-way into a made by lashing two sticks together from one side, and then drilling from the other side to meet this hole
Bow drill
–
A Bow drill is used to get an ember (left), the ember makes tinder smoke (center), until a fire is lit (right).
Bow drill
–
Diagram of a bow drill designed for fire starting
Bow drill
–
A pump drill
28.
Mehrgarh
–
Mehrgarh, sometimes anglicized as Mehergarh or Mehrgar, is a Neolithic site located near the Bolan Pass on the Kacchi Plain of Balochistan, Pakistan, to the west of the Indus River valley. The earliest settlement at Mehrgarh, in the northeast corner of the 495-acre site, was a farming village which was inhabited from circa 6500 BCE. It is one of the earliest sites with evidence of farming and herding in South Asia, archaeological material has been found in six mounds, and about 32,000 artifacts have been collected. Mehrgarh is now seen as a precursor to the Indus Valley Civilization, displaying the whole sequence from earliest settlement, jean-Francois Jarrige argues for an independent origin of Mehrgarh. But given the originality of Mehrgarh, Jarrige concludes that Mehrgarh has a local background. Gallego Romero notes that Indians who are lactose-tolerant show a genetic pattern regarding this tolerance which is characteristic of the common European mutation. According to Romero, this suggests that the most common lactose tolerance mutation made a migration out of the Middle East less than 10,000 years ago. They further note that he earliest evidence of cattle herding in south Asia comes from the Indus River Valley site of Mehrgarh and is dated to 7,000 YBP, Archaeologists divide the occupation at the site into eight periods. The Mehrgarh Period I was Neolithic and aceramic, without the use of pottery, the earliest farming in the area was developed by semi-nomadic people using plants such as wheat and barley and animals such as sheep, goats and cattle. The settlement was established with simple mud buildings and most of them had four internal subdivisions, ornaments of sea shell, limestone, turquoise, lapis lazuli and sandstone have been found, along with simple figurines of women and animals. Sea shells from far sea shore and lapis lazuli found as far away as present-day Badakshan, Afghanistan shows good contact with those areas, a single ground stone axe was discovered in a burial, and several more were obtained from the surface. These ground stone axes are the earliest to come from a context in the South Asia. Periods I, II and III are contemporaneous with another site called Kili Gul Mohammed, in April 2006, it was announced in the scientific journal Nature that the oldest evidence for the drilling of human teeth in vivo was found in Mehrgarh. According to the authors, their discoveries point to a tradition of proto-dentistry in the farming cultures of that region. Here we describe eleven drilled molar crowns from nine adults discovered in a Neolithic graveyard in Pakistan that dates from 7,500 to 9,000 years ago and these findings provide evidence for a long tradition of a type of proto-dentistry in an early farming culture. The Mehrgarh Period II and Merhgarh Period III were ceramic Neolithic, using pottery, Period II is at site MR4 and Period III is at MR2. Much evidence of manufacturing activity has been found and more advanced techniques were used, glazed faience beads were produced and terracotta figurines became more detailed. Figurines of females were decorated with paint and had diverse hairstyles, two flexed burials were found in Period II with a red ochre cover on the body
Mehrgarh
–
Map of Pakistan showing Mehrgarh in relation to the cities of Quetta, Kalat, and Sibi and the Kachi Plain of Balochistan.
Mehrgarh
Mehrgarh
–
A figurine from Mehrgarh, similar to the
Venus figurines
29.
Arabic language
–
Arabic is a Central Semitic language that was first spoken in Iron Age northwestern Arabia and is now the lingua franca of the Arab world. Arabic is also the language of 1.7 billion Muslims. It is one of six languages of the United Nations. The modern written language is derived from the language of the Quran and it is widely taught in schools and universities, and is used to varying degrees in workplaces, government, and the media. The two formal varieties are grouped together as Literary Arabic, which is the language of 26 states. Modern Standard Arabic largely follows the standards of Quranic Arabic. Much of the new vocabulary is used to denote concepts that have arisen in the post-Quranic era, Arabic has influenced many languages around the globe throughout its history. During the Middle Ages, Literary Arabic was a vehicle of culture in Europe, especially in science, mathematics. As a result, many European languages have borrowed many words from it. Many words of Arabic origin are found in ancient languages like Latin. Balkan languages, including Greek, have acquired a significant number of Arabic words through contact with Ottoman Turkish. Arabic has also borrowed words from languages including Greek and Persian in medieval times. Arabic is a Central Semitic language, closely related to the Northwest Semitic languages, the Ancient South Arabian languages, the Semitic languages changed a great deal between Proto-Semitic and the establishment of the Central Semitic languages, particularly in grammar. Innovations of the Central Semitic languages—all maintained in Arabic—include, The conversion of the suffix-conjugated stative formation into a past tense, the conversion of the prefix-conjugated preterite-tense formation into a present tense. The elimination of other prefix-conjugated mood/aspect forms in favor of new moods formed by endings attached to the prefix-conjugation forms, the development of an internal passive. These features are evidence of descent from a hypothetical ancestor. In the southwest, various Central Semitic languages both belonging to and outside of the Ancient South Arabian family were spoken and it is also believed that the ancestors of the Modern South Arabian languages were also spoken in southern Arabia at this time. To the north, in the oases of northern Hijaz, Dadanitic and Taymanitic held some prestige as inscriptional languages, in Najd and parts of western Arabia, a language known to scholars as Thamudic C is attested
Arabic language
–
The Galland Manuscript of
One Thousand and One Nights, 14th century
Arabic language
–
al-ʿArabiyyah in written Arabic (
Naskh script)
Arabic language
–
Bilingual traffic sign in
Qatar.
Arabic language
–
Examples of how the Arabic root and form system works.
30.
Azerbaijani language
–
The language has official status in Azerbaijan and Dagestan but it does not have official status in Iranian Azerbaijan, where the majority of Azerbaijanis live. It is also spoken to varying degrees in Azerbaijani communities of Georgia and Turkey and by diaspora communities, primarily in Europe. Azerbaijani is a member of the Oghuz branch of the Turkic languages, modern literature in Azerbaijan is based on the Shirvani dialect mainly, while in Iranian Azerbaijan region it is based on the Tabrizi one. Azerbaijani evolved from the Eastern branch of Oghuz Turkic which spread to the Caucasus, in Eastern Europe, Persian and Arabic influenced the language, but Arabic words were mainly transmitted through the intermediary of literary Persian. By the beginning of the 16th century, it had become the dominant language of the region, the historical development of Azerbaijani can be divided into two major periods, early and modern. Early Azerbaijani differs from its descendant in that it contained a larger number of Persian. Early writings in Azerbaijani also demonstrate linguistic interchangeability between Oghuz and Kypchak elements in many aspects, despite major differences, they all aimed primarily at making it easy for semi-literate masses to read and understand literature. They all criticized the overuse of Persian, Arabic, and European elements in both colloquial and literary language and called for a simpler and more popular style. Despite the wide use of Azerbaijani in the Azerbaijan Soviet Socialist Republic, after independence, Azerbaijan republic decided to switch back to the Latin script. The first examples of Azerbaijani literature date to the late 1200s following the Mongol conquest and were written in Arabic script, in the 1300s Kadi Burhan al-Din, Hesenoghlu, and Imadaddin Nasimi helped to establish Azerbaiijani as a language through poetry and other literary works. In 1875 Akinchi became the first Azerbaijani newspaper to be published in the Russian Empire and it was started by Hasan bey Zardabi, a journalist and education advocate. Following the rule of the Qajar dynasty Iran was ruled by Reza Shah who banned the publication of texts in Azerbaijani, modern literature in the Republic of Azerbaijan is based on the Shirvani dialect mainly, while in Iranian Azerbaijan it is based on the Tabrizi dialect. Mohammad-Hossein Shahriar is an important figure in Azerbaijani poetry and his most important work is Heydar Babaya Salam and it is considered to be a pinnacle of Azerbaijani literature and gained popularity in the Turkic-speaking world. It was translated more than 30 languages. In the mid-19th century Azerbaijani literature was taught at schools in Baku, Ganja, Shaki, Tbilisi, since 1845, it has also been taught in the Saint Petersburg State University in Russia. Per the 1829 Caucasus School Statute, Azerbaijani was to be taught in all schools of Ganja, Shusha, Nukha, Shamakhi, Quba, Baku, Derbent, Yerevan, Nakhchivan, Akhaltsikhe. Beginning in 1834, it was introduced as a language of study in Kutaisi instead of Armenian, in 1853, Azerbaijani became a compulsory language for students of all backgrounds in all of Transcaucasia with the exception of the Tiflis Governorate. Azerbaijani is one of the Oghuz languages within the Turkic language family, the International Organization for Standardization encodes North Azerbaijani and South Azerbaijani as distinct languages
Azerbaijani language
–
Garden of Pleasures by
Fuzûlî in Azerbaijani. Early 19th century. There is Shaki khan's seal on it. Museum of History of Azerbaijan
Azerbaijani language
–
Location of Azerbaijani speakers in the
Caucasus
Azerbaijani language
–
Azerbaijani-language road sign.
31.
Persian language
–
Persian, also known by its endonym Farsi, is one of the Western Iranian languages within the Indo-Iranian branch of the Indo-European language family. It is primarily spoken in Iran, Afghanistan, and Tajikistan and it is mostly written in the Persian alphabet, a modified variant of the Arabic script. Its grammar is similar to that of many contemporary European languages, Persian gets its name from its origin at the capital of the Achaemenid Empire, Persis, hence the name Persian. A Persian-speaking person may be referred to as Persophone, there are approximately 110 million Persian speakers worldwide, with the language holding official status in Iran, Afghanistan, and Tajikistan. For centuries, Persian has also been a cultural language in other regions of Western Asia, Central Asia. It also exerted influence on Arabic, particularly Bahrani Arabic. Persian is one of the Western Iranian languages within the Indo-European family, other Western Iranian languages are the Kurdish languages, Gilaki, Mazanderani, Talysh, and Balochi. Persian is classified as a member of the Southwestern subgroup within Western Iranian along with Lari, Kumzari, in Persian, the language is known by several names, Western Persian, Parsi or Farsi has been the name used by all native speakers until the 20th century. Since the latter decades of the 20th century, for reasons, in English. Tajiki is the variety of Persian spoken in Tajikistan and Uzbekistan by the Tajiks, according to the Oxford English Dictionary, the term Persian as a language name is first attested in English in the mid-16th century. Native Iranian Persian speakers call it Fārsi, Farsi is the Arabicized form of Pārsi, subsequent to Muslim conquest of Persia, due to a lack of the phoneme /p/ in Standard Arabic. The origin of the name Farsi and the place of origin of the language which is Fars Province is the Arabicized form of Pārs, in English, this language has historically been known as Persian, though Farsi has also gained some currency. Farsi is encountered in some literature as a name for the language. In modern English the word Farsi refers to the language while Parsi describes Zoroastrians, some Persian language scholars such as Ehsan Yarshater, editor of Encyclopædia Iranica, and University of Arizona professor Kamran Talattof, have also rejected the usage of Farsi in their articles. The international language-encoding standard ISO 639-1 uses the code fa, as its system is mostly based on the local names. The more detailed standard ISO 639-3 uses the name Persian for the dialect continuum spoken across Iran and Afghanistan and this consists of the individual languages Dari and Iranian Persian. Currently, Voice of America, BBC World Service, Deutsche Welle, Radio Free Europe/Radio Liberty also includes a Tajik service and an Afghan service. This is also the case for the American Association of Teachers of Persian, The Centre for Promotion of Persian Language and Literature, Persian is an Iranian language belonging to the Indo-Iranian branch of the Indo-European family of languages
Persian language
–
Old Persian
Persian language
–
Ferdowsi 's
Shahnameh
Persian language
–
Kalilah va Dimna, an influential work in Persian literature.
32.
Minoan civilization
–
The Minoan civilization was an Aegean Bronze Age civilization on the island of Crete and other Aegean islands which flourished from about 2600 to 1100 BC. It preceded the Mycenaean civilization of Ancient Greece, the civilization was rediscovered at the beginning of the 20th century through the work of British archaeologist Arthur Evans. It has been described as the earliest of its kind in Europe, the term Minoan, which refers to the mythical King Minos, originally described the pottery of the period. Minos was associated in Greek mythology with the labyrinth and the Minotaur, according to Homer, Crete once had 90 cities. The Minoan period saw trade between Crete and Aegean and Mediterranean settlements, particularly the Near East, traders and artists, the Minoan cultural influence reached beyond Crete to the Cyclades, Egypts Old Kingdom, copper-bearing Cyprus, Canaan and the Levantine coast, and Anatolia. Some of its best art is preserved in the city of Akrotiri on the island of Santorini, although the Minoan language and writing systems remain undecipherable and are subjects of academic dispute, they apparently conveyed a language entirely different from the later Greek. The reason for the end of the Minoan period is unclear, theories include Mycenaean invasions from mainland Greece, the term Minoan refers to the mythical King Minos of Knossos. Its origin is debated, but it is attributed to archeologist Arthur Evans. Minos was associated in Greek mythology with the labyrinth, which Evans identified with the site at Knossos. However, Karl Hoeck had already used the title Das Minoische Kreta in 1825 for volume two of his Kreta, this appears to be the first known use of the word Minoan to mean ancient Cretan, Evans said that applied it, not invented it. Hoeck, with no idea that the archaeological Crete had existed, had in mind the Crete of mythology, although Evans 1931 claim that the term was unminted before he used it was called a brazen suggestion by Karadimas and Momigliano, he coined its archaeological meaning. Instead of dating the Minoan period, archaeologists use two systems of relative chronology, the first, created by Evans and modified by later archaeologists, is based on pottery styles and imported Egyptian artifacts. Evans system divides the Minoan period into three eras, early, middle and late. These eras are subdivided—for example, Early Minoan I, II and III, another dating system, proposed by Greek archaeologist Nicolas Platon, is based on the development of architectural complexes known as palaces at Knossos, Phaistos, Malia and Kato Zakros. Platon divides the Minoan period into pre-, proto-, neo-, the relationship between the systems in the table includes approximate calendar dates from Warren and Hankey. The Thera eruption occurred during a phase of the LM IA period. Efforts to establish the volcanic eruptions date have been controversial, the eruption is identified as a natural event catastrophic for the culture, leading to its rapid collapse. Although stone-tool evidence exists that hominins may have reached Crete as early as 130,000 years ago, evidence for the first anatomically-modern human presence dates to 10, the oldest evidence of modern human habitation on Crete are pre-ceramic Neolithic farming-community remains which date to about 7000 BC
Minoan civilization
–
Minoan civilization
Minoan civilization
–
Minoan
copper ingot.
Minoan civilization
–
Fresco showing three women who were possibly
queens. [
citation needed]
33.
Crete
–
Crete is the largest and most populous of the Greek islands, 88th-largest island in the world and the fifth-largest island in the Mediterranean Sea, after Sicily, Sardinia, Cyprus, and Corsica. Crete and a number of surrounding islands and islets constitute the region of Crete, the capital and the largest city is Heraklion. As of 2011, the region had a population of 623,065, Crete forms a significant part of the economy and cultural heritage of Greece, while retaining its own local cultural traits. It was once the centre of the Minoan civilization, which is regarded as the earliest recorded civilization in Europe. The island is first referred to as Kaptara in texts from the Syrian city of Mari dating from the 18th century BC, repeated later in Neo-Assyrian records and it was also known in ancient Egyptian as Keftiu, strongly suggesting a similar Minoan name for the island. The current name of Crete is thought to be first attested in Mycenaean Greek texts written in Linear B, through the words
Crete
–
NASA photograph of Crete
Crete
–
Lefka Ori
Crete
–
Port of Heraklion
Crete
–
Lefka Ori (White mountains).
34.
Knossos
–
Knossos is the largest Bronze Age archaeological site on Crete and is considered Europes oldest city. The name Knossos survives from ancient Greek references to the city of Crete. The coins came from the Roman settlement of Colonia Julia Nobilis Cnossus, a Roman colony placed just to the north of, the Romans believed they had colonized Knossos. The second palace was built on a grander scale over the old Palace after an earthquake destroyed it. The structure and ruins we see today are from the second Palace, during the Bronze Age, the town surrounded the hill on which the palace was built. The site was discovered in 1878 by Minos Kalokairinos, the excavations in Knossos began in AD1900 by the English archaeologist Sir Arthur Evans and his team, and they continued for 35 years. The palace was excavated and partially restored under the direction of Arthur Evans in the earliest years of the 20th century. Its size far exceeded his expectations, as did the discovery of two ancient scripts, which he termed Linear A and Linear B, to distinguish their writing from the pictographs also present. The palace of Knossos was undoubtedly the ceremonial and political centre of the Minoan civilization and it appears as a maze of workrooms, living spaces, and storerooms close to a central square. The palace was abandoned at some time at the end of the Late Bronze Age. The occasion is not known for certain, but one of the disasters that befell the palace is generally put forward. The hill was never again a settlement or civic site, although squatters may have used it for a time, however, fieldwork in 2015 revealed that during the early Iron Age, Knossos was rich in imports and was nearly three times larger than indicated by earlier excavations. Except for periods of abandonment, other cities were founded in the vicinity, such as the Roman colony. The population shifted to the new town of Chandax during the 9th century AD, by the 13th century, it was called Makruteikhos Long Wall, the bishops of Gortyn continued to call themselves Bishops of Knossos until the 19th century. Today, the name is used only for the site now situated in the expanding suburbs of Heraklion. In the first palace period around 2000 BC the urban area reached a size of up to 18,000 people, in its peak the Palace and the surrounding city boasted a population of 100,000 people shortly after 1700 BC. The name Knossos was formerly Latinized as Cnossus or Cnossos, and occasionally Knossus, Gnossus and this site history is to be distinguished from the ancient. In Greek mythology, King Minos dwelt in a palace at Knossos and he had Daedalus construct a labyrinth, a very large maze in which to retain his son, the Minotaur
Knossos
–
Restored North Entrance with charging bull fresco
Knossos
–
A
labrys from
Messara.
Knossos
–
View to the east from the northwest corner. In the foreground is the west wall of the Lustral Basin.
Knossos
–
View to the south. The hill in the background is Gypsades. Between it and Knossos is the Vlychia. The South Entrance is on the left.
35.
Nephrite
–
Nephrite is a variety of the calcium, magnesium, and iron-rich amphibole minerals tremolite or actinolite. The chemical formula for nephrite is Ca25Si8O222 and it is one of two different mineral species called jade. The other mineral species known as jade is jadeite, which is a variety of pyroxene, while nephrite jade possess mainly grays and greens, jadeite jade, which is rarer, can also contain blacks, reds, pinks and violets. Nephrite jade is a stone used in carvings, beads. Western Canada is the source of modern lapidary nephrite. Nephrite jade was used mostly in pre-1800 China as well as in New Zealand, the Pacific Coast and Atlantic Coasts of North America, Neolithic Europe, accordingly, nephrite jade was once believed to be a cure for kidney stones. Tomb jade or grave jade are names given to ancient burial nephrite pieces that have a brown or chalky white texture as a surface treatment. A lot of tools and amulets are known since the Early Neolithic to the Late Chalcolithic on the Balkans from two or more unknown sources - Balkan nephrite culture. Such tools are found in the Later Neolithic of Poland, Sardinia, single or just a few finds of nephrite artifacts are reported also from some other European countries. Jade was used to create many utilitarian and ceremonial objects, ranging from indoor decorative items to jade burial suits, Jade was considered the imperial gem. From about the earliest Chinese dynasties until present, the deposits in most use were from the region of Khotan in the Western Chinese province of Xinjiang. There, white and greenish nephrite jade is found in quarries and as pebbles. River jade collection was concentrated in the Yarkand, and the White Jade, Nephrite jade in New Zealand is known as pounamu in the Māori language, and is highly valued, playing an important role in Māori culture. It is considered a taonga, or treasure, and therefore protected under the Treaty of Waitangi, the South Island of New Zealand is Te Wai Pounamu in Māori — The Greenstone Water — because that is where it occurs. Weapons and ornaments were made of it, in particular the mere, and these were believed to have their own mana, were handed down as valuable heirlooms, and often given as gifts to seal important agreements. It was also used for a range of such as adzes. Commonly called greenstone, jade jewellery in Māori designs is widely popular with tourists – although much of the jade itself is now imported from British Columbia, bale, Martin T. and Ko, Min-jung. Craft Production and Social Change in Mumun Pottery Period Korea, gemmological significance of the prehistoric Balkan nephrite culture
Nephrite
–
Nephrite from Jordanów Śląski (Poland)
Nephrite
–
"Mutton fat" jade for sale at
Hotan Jade Market
Nephrite
–
Large "mutton fat" nephrite jade displayed in
Hotan Cultural Museum lobby.
Nephrite
–
Nephrite from
Wyoming
36.
Emerald
–
Emerald is a gemstone and a variety of the mineral beryl colored green by trace amounts of chromium and sometimes vanadium. Beryl has a hardness of 7. 5–8 on the Mohs scale, most emeralds are highly included, so their toughness is classified as generally poor. The word emerald is derived, from Vulgar Latin, esmaralda/esmaraldus, a variant of Latin smaragdus, emeralds, like all colored gemstones, are graded using four basic parameters–the four Cs of Connoisseurship, Color, Clarity, Cut and Carat weight. Before the 20th century, jewelers used the water, as in a gem of the finest water. Normally, in the grading of colored gemstones, color is by far the most important criterion, however, in the grading of emeralds, clarity is considered a close second. A fine emerald must possess not only a pure verdant green hue as described below, in the 1960s, the American jewelry industry changed the definition of emerald to include the green vanadium-bearing beryl as emerald. As a result, vanadium emeralds purchased as emeralds in the United States are not recognized as such in the UK, in America, the distinction between traditional emeralds and the new vanadium kind is often reflected in the use of terms such as Colombian Emerald. In gemology, color is divided into three components, hue, saturation, and tone, emeralds occur in hues ranging from yellow-green to blue-green, with the primary hue necessarily being green. Yellow and blue are the normal secondary hues found in emeralds, only gems that are medium to dark in tone are considered emerald, light-toned gems are known instead by the species name green beryl. The finest emerald are approximately 75% tone on a scale where 0% tone would be colorless, in addition, a fine emerald should be well saturated and have a hue that is bright. Gray is the normal saturation modifier or mask found in emerald, Emerald tends to have numerous inclusions and surface breaking fissures. Unlike diamond, where the standard, i. e. 10× magnification, is used to grade clarity. Thus, if an emerald has no visible inclusions to the eye it is considered flawless, stones that lack surface breaking fissures are extremely rare and therefore almost all emeralds are treated to enhance the apparent clarity. The inclusions and fissures within an emerald are sometime described as jardin, imperfections are unique for each emerald and can be used to identify a particular stone. Eye-clean stones of a vivid primary green hue, with no more than 15% of any hue or combination of a medium-dark tone. The relative non-uniformity motivates the cutting of emeralds in cabochon form, faceted emeralds are most commonly given an oval cut, or the signature emerald cut, a rectangular cut with facets around the top edge. Most emeralds are oiled as part of the process, in order to fill in surface-reaching cracks so that clarity and stability are improved. Cedar oil, having a refractive index, is often used in this widely adopted practice
Emerald
–
Emerald crystal from
Muzo,
Colombia
Emerald
–
Cut emeralds
Emerald
–
Brazilian emerald (grass-green variety of the mineral beryl) in a quartz-pegmatite matrix with typical hexagonal, prismatic crystals.
Emerald
–
Spanish-made emerald and gold pendant exhibited at
Victoria and Albert Museum.
37.
Nibelungenlied
–
The Nibelungenlied, translated as The Song of the Nibelungs, is an epic poem in Middle High German. The story tells of dragon-slayer Siegfried at the court of the Burgundians, how he was murdered, the Nibelungenlied is based on pre-Christian Germanic heroic motifs, which include oral traditions and reports based on historic events and individuals of the 5th and 6th centuries. Old Norse parallels of the legend survive in the Völsunga saga, the Prose Edda, the Poetic Edda, the Legend of Norna-Gest, in 2009, the three main manuscripts of the Nibelungenlied were inscribed in UNESCOs Memory of the World Register in recognition of their historical significance. The poem in its various forms was lost by the end of the 16th century. There are thirty-five known manuscripts of the Nibelungenlied and its variant versions, eleven of these manuscripts are essentially complete. The oldest version seems to be the one preserved in manuscript B, twenty-four manuscripts are in various fragmentary states of completion, including one version in Dutch. The text contains approximately 2,400 stanzas in 39 Aventiuren, the title under which the poem has been known since its discovery is derived from the final line of one of the three main versions, hie hât daz mære ein ende, daz ist der Nibelunge liet. Liet here means lay, tale or epic rather than simply song, the manuscripts sources deviate considerably from one another. This categorization derives from the signatures on the *A, *B, the Nibelungs lament, a sort of appendix to the poem proper, mentions a Meister Konrad who was charged by a bishop Pilgrim of Passau with the copying of the text. This is taken as a reference to Saint Pilgrim, bishop of Passau from 971–991, the search for the author of the Nibelungenlied in German studies has a long and intense history. Among the names suggested were Konrad von Fußesbrunnen, Bligger von Steinach, none of these hypotheses has wide acceptance, and mainstream scholarship today accepts that the authors name cannot be established. The original version began with the introduction of Kriemhild, the protagonist of the work. The second part deals with Kriemhilds marriage to Etzel, her plans for revenge, the journey of the Burgundians to the court of Etzel, the first chapter introduces the court of Burgundy. Kriemhild has a dream of a falcon that is killed by two eagles and her mother interprets this to mean that Kriemhilds future husband will die a violent death, and Kriemhild consequently resolves to remain unmarried. The second chapter tells of the background of Siegfried, crown prince of Xanten and his youth is narrated with little room for the adventures later attributed to him. In the third chapter, Siegfried arrives in Worms with the hopes of wooing Kriemhild, Siegfried leaves his treasure in the charge of a dwarf named Alberich. After killing the dragon, Siegfried then bathed in its blood, in spite of Hagens threatening stories about his youth, the Burgundians welcome him, but do not allow him to meet the princess. Disappointed, he remains in Worms and helps Gunther defeat the invading Saxons
Nibelungenlied
–
First page from Manuscript C (ca. 1230)
Nibelungenlied
–
Sigurd and Brunhild – Illustration by Harry George Theaker for Children's Stories from the Northern Legends by M. Dorothy Belgrave and Hilda Hart, 1920
Nibelungenlied
–
Siegfried and Kriemhild
Nibelungenlied
–
Gunther's wedding night (
Johann Heinrich Füssli 1807)
38.
Chrysoprase
–
Chrysoprase, chrysophrase or chrysoprasus is a gemstone variety of chalcedony that contains small quantities of nickel. Its color is normally apple-green, but varies to deep green, the darker varieties of chrysoprase are also referred to as prase. Chrysoprase is cryptocrystalline, which means that it is composed of crystals so fine that they cannot be seen as distinct particles under normal magnification and this sets it apart from rock crystal, amethyst, citrine, and the other varieties of crystalline quartz. Other members of the cryptocrystalline silica family include agate, carnelian, unlike many non-transparent silica minerals, it is the color of chrysoprase, rather than any pattern of markings, that makes it desirable. The word chrysoprase comes from the Greek χρυσός chrysos meaning gold and πράσινον prasinon, unlike emerald which owes its green color to the presence of chromium, the color of chrysoprase is due to trace amounts of nickel compounds in the form of very small inclusions. The nickel reportedly occurs as different silicates, like kerolite or pimelite, chrysoprase results from the deep weathering or lateritization of nickeliferous serpentinites or other ultramafic ophiolite rocks. In the Australian deposits, chrysoprase occurs as veins and nodules with brown goethite and other iron oxides in the magnesite-rich saprolite below an iron, as with all forms of chalcedony, chrysoprase has a hardness of 6–7 on the Mohs hardness scale and a conchoidal fracture like flint. The best known sources of chrysoprase are Queensland, Western Australia, Germany, Poland, Russia, Arizona, California, and Brazil. The chrysoprase and Ni silicate ore deposit in Szklary, Lower Silesia, Poland, was probably the biggest European chrysoprase occurrence, a very similar mineral to chrysoprase is chrome chalcedony, in which the color is provided by chromium rather than nickel
Chrysoprase
–
Chrysoprase (Poland)
Chrysoprase
–
A polished chrysoprase stone
39.
Flinders Petrie
–
Sir William Matthew Flinders Petrie, FRS, FBA, commonly known as Flinders Petrie, was an English Egyptologist and a pioneer of systematic methodology in archaeology and preservation of artefacts. He held the first chair of Egyptology in the United Kingdom, some consider his most famous discovery to be that of the Merneptah Stele, an opinion with which Petrie himself concurred. Petrie developed the system of dating based on pottery and ceramic findings. William Matthew Flinders Petrie was born in Maryon Road, Charlton, Kent, England, Anne was the daughter of Captain Matthew Flinders, surveyor of the Australian coastline, spoke six languages and was an Egyptologist. His father taught his son how to survey accurately, laying the foundation for his archaeological career, at the age of eight, he was tutored in French, Latin, and Greek, until he had a collapse and was taught at home. He also ventured his first archaeological opinion aged eight, when visiting the Petrie family were describing the unearthing of the Brading Roman Villa in the Isle of Wight. The boy was horrified to hear the rough shovelling out of the contents, and protested that the earth should be pared away, inch by inch, to see all that was in it and how it lay. All that I have done since, he wrote when he was in his seventies, was there to begin with. I was already in archaeology by nature, on 26 November 1896, Petrie married Hilda Urlin in London. They had two children, John and Ann and they originally lived in Hampstead, where an English Heritage blue plaque now stands on the building they lived in,5 Cannon Place. Their son was John Flinders Petrie, the mathematician, who gave his name to the Petrie polygon, when he died in 1942, Petrie donated his head to the Royal College of Surgeons of London while his body was interred in the Protestant Cemetery on Mt. Zion. World War II was then at its height, and the head was delayed in transit, after being stored in a jar in the college basement, its label fell off and no one knew who the head belonged to. It was identified however, and is now stored, but not displayed, the chair of Edwards Professor of Egyptian Archaeology and Philology at University College London was set up and funded in 1892 by a bequest of Amelia Edwards following her sudden death in that year. Petries supporter since 1880, Edwards had instructed that he should be its first incumbent and he continued to excavate in Egypt after taking up the professorship, training many of the best archaeologists of the day. In 1913 Petrie sold his collection of Egyptian antiquities to University College, London. One of his students was Howard Carter who went on to discover the tomb of Tutankhamun, in his teenage years, Petrie surveyed British prehistoric monuments in attempts to understand their geometry. On that visit, he was appalled by the rate of destruction of monuments, impressed by his scientific approach, they offered him work as the successor to Édouard Naville. Petrie accepted the position and was given the sum of £250 per month to cover the excavations expenses, in November 1884, Petrie arrived in Egypt to begin his excavations
Flinders Petrie
–
Flinders Petrie, 1903
Flinders Petrie
–
Flinders Petrie by Philip Alexius de Laszlo, 1934 (detail)
Flinders Petrie
–
The distinctive black-topped Egyptian pottery of the PreDynastic period associated with Flinders Petrie's Sequence Dating System,
Petrie Museum
Flinders Petrie
–
A photograph Petrie took of his view from the tomb he lived in in Giza 1881
40.
Sediment
–
For sediment in beverages, see dregs. For example, sand and silt can be carried in suspension in water and on reaching the sea be deposited by sedimentation. Sediments are most often transported by water, but also wind, beach sands and river channel deposits are examples of fluvial transport and deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of transport and deposition. Glacial moraine deposits and till are ice-transported sediments, sediment can be classified based on its grain size and/or its composition. Sediment size is measured on a log base 2 scale, called the Phi scale, composition of sediment can be measured in terms of, parent rock lithology mineral composition chemical make-up. This leads to an ambiguity in which clay can be used as both a size-range and a composition, sediment is transported based on the strength of the flow that carries it and its own size, volume, density, and shape. Stronger flows will increase the lift and drag on the particle, causing it to rise, rivers and streams carry sediment in their flows. This sediment can be in a variety of locations within the flow and these relationships are shown in the following table for the Rouse number, which is a ratio of sediment fall velocity to upwards velocity. If the upwards velocity is less than the settling velocity, but still high enough for the sediment to move, it will move along the bed as bed load by rolling, sliding. If the upwards velocity is higher than the velocity, the sediment will be transported high in the flow as wash load. As there are generally a range of different particle sizes in the flow, sediment motion can create self-organized structures such as ripples, dunes, antidunes on the river or stream bed. These bedforms are often preserved in rocks and can be used to estimate the direction. Overland flow can erode soil particles and transport them downslope, the erosion associated with overland flow may occur through different methods depending on meteorological and flow conditions. If the initial impact of rain droplets dislodges soil, the phenomenon is called rainsplash erosion, if overland flow is directly responsible for sediment entrainment but does not form gullies, it is called sheet erosion. If the flow and the substrate permit channelization, gullies may form, glaciers carry a wide range of sediment sizes, and deposit it in moraines. The overall balance between sediment in transport and sediment being deposited on the bed is given by the Exner equation and this expression states that the rate of increase in bed elevation due to deposition is proportional to the amount of sediment that falls out of the flow. This can be localized, and simply due to obstacles, examples are scour holes behind boulders, where flow accelerates
Sediment
–
Cobbles on a beach
Sediment
–
River Rhône flowing into
Lake Geneva
Sediment
–
Sediment billowing out from Italy's shore into the
Adriatic Sea
Sediment
–
Sediment in the
Gulf of Mexico
41.
Volcanic ash
–
Volcanic ash consists of fragments of pulverized rock, minerals and volcanic glass, created during volcanic eruptions and measuring less than 2 mm in diameter. The term volcanic ash is often loosely used to refer to all explosive eruption products. Volcanic ash is formed during volcanic eruptions when dissolved gases in magma expand. The force of the escaping gas shatters the magma and propels it into the atmosphere where it solidifies into fragments of volcanic rock and glass. Ash is also produced when magma comes into contact with water during phreatomagmatic eruptions, once in the air, ash is transported by wind up to thousands of kilometers away. Volcanic ash is formed during volcanic eruptions, phreatomagmatic eruptions. Explosive eruptions occur when magma decompresses as it rises, allowing dissolved volatiles to exsolve into gas bubbles, as more bubbles nucleate a foam is produced, which decreases the density of the magma, accelerating it up the conduit. Fragmentation occurs when bubbles occupy ~70-80 vol% of the erupting mixture, when fragmentation occurs, violently expanding bubbles tear the magma apart into fragments which are ejected into the atmosphere where they solidify into ash particles. Fragmentation is an efficient process of ash formation and is capable of generating very fine ash even without the addition of water. Volcanic ash is produced during phreatomagmatic eruptions. During these eruptions fragmentation occurs when magma comes into contact with bodies of water groundwater, as the magma, which is significantly hotter than the boiling point of water, comes into contact with water an insulating vapor film forms. Eventually this vapor film will collapse leading to direct coupling of the cold water and this increases the heat transfer which leads to the rapid expansion of water and fragmentation of the magma into small particles which are subsequently ejected from the volcanic vent. Fragmentation causes an increase in area between magma and water creating a feedback mechanism, leading to further fragmentation and production of fine ash particles. Pyroclastic density currents can also produce ash particles and these are typically produced by lava dome collapse or collapse of the eruption column. Within pyroclastic density currents particle abrasion occurs as particles interact with each resulting in a reduction in grain size. In addition, ash can be produced during secondary fragmentation of pumice fragments and these processes produce large quantities of very fine grained ash which is removed from pyroclastic density currents in co-ignimbrite ash plumes. Physical and chemical characteristics of volcanic ash are primarily controlled by the style of volcanic eruption, another parameter controlling the amount of ash produced is the duration of the eruption, the longer the eruption is sustained, the more ash will be produced. The types of minerals present in volcanic ash are dependent on the chemistry of the magma from which it erupted, low energy eruptions of basalt produce a characteristically dark coloured ash containing ~45 - 55% silica that is generally rich in iron and magnesium
Volcanic ash
–
Ash cloud from the 2008 eruption of
Chaitén volcano,
Chile, stretching across
Patagonia from the
Pacific to the
Atlantic Ocean.
Volcanic ash
–
Ash plume from
Mt Cleveland, a
stratovolcano.
Volcanic ash
–
454 million year old volcanic ash between layers of
limestone in the catacombs of
Peter the Great's Naval Fortress in
Estonia near
Laagri. The diameter of objective cover is 58 mm (2.3 in). This is remnant of one of the oldest
large eruptions preserved.
Volcanic ash
–
Particle of volcanic ash from
Mount St. Helens.
42.
Hydrothermal circulation
–
Hydrothermal circulation in its most general sense is the circulation of hot water. Hydrothermal circulation occurs most often in the vicinity of sources of heat within the Earths crust, in general, this occurs near volcanic activity, but can occur in the deep crust related to the intrusion of granite, or as the result of orogeny or metamorphism. Hydrothermal circulation in the oceans is the passage of the water through mid-oceanic ridge systems, the former circulation type is sometimes termed active, and the latter passive. The heat source for the active vents is the newly formed basalt, and, for the highest temperature vents, the heat source for the passive vents is the still-cooling older basalts. Heat flow studies of the seafloor suggest that basalts within the oceanic crust take millions of years to cool as they continue to support passive hydrothermal circulation systems. Hydrothermal vents are locations on the seafloor where hydrothermal fluids mix into the overlying ocean, perhaps the best-known vent forms are the naturally occurring chimneys referred to as black smokers. Hydrothermal circulation is not limited to ocean ridge environments, the source water for hydrothermal explosions, geysers, and hot springs is heated groundwater convecting below and lateral to the hot water vent. Hydrothermal circulating convection cells exist any place an anomalous source of heat, such as an intruding magma or volcanic vent, hydrothermal also refers to the transport and circulation of water within the deep crust, in general from areas of hot rocks to areas of cooler rocks. During the early 1900s, various geologists worked to classify hydrothermal ore deposits that they assumed formed from upward-flowing aqueous solutions, waldemar Lindgren developed a classification based on interpreted decreasing temperature and pressure conditions of the depositing fluid. His terms, hypothermal, mesothermal, epithermal and teleothermal, expressed decreasing temperature, recent studies retain only the epithermal label
Hydrothermal circulation
–
Waves
43.
Dendrite (crystal)
–
A crystal dendrite is a crystal that develops with a typical multi-branching tree-like form. Dendritic crystal growth is common and illustrated by snowflake formation. Dendritic crystallization forms a natural fractal pattern, Dendritic crystals can grow into a supercooled pure liquid or form from growth instabilities that occur when the growth rate is limited by the rate of diffusion of solute atoms to the interface. In the latter case, there must be a concentration gradient from the value in the solution to the concentration in equilibrium with the crystal at the surface. Any protuberance that develops is accompanied by a concentration gradients at its tip. This increases the rate to the tip. In opposition to this is the action of the surface tension tending to flatten the protuberance, however, overall, the protuberance becomes amplified. This process occurs again and again until a dendrite is produced, the term dendrite comes from the Greek word dendron, which means tree. In paleontology, dendritic mineral crystal forms are often mistaken for fossils and these pseudofossils form as naturally occurring fissures in the rock are filled by percolating mineral solutions. They form when water rich in manganese and iron flows along fractures, a variety of manganese oxides and hydroxides are involved, including, birnessite coronadite cryptomelane hollandite romanechite todorokite and others. A three-dimensional form of dendrite develops in fissures in quartz, forming moss agate, in chemistry, a dendrite is a crystal that branches into two parts during growth. Dendritic solidification is one of the most common forms of solidifying metals, when materials crystallize or solidify under certain conditions, they freeze unstably, resulting in dendritic forms. Scientists are particularly interested in dendrite size, shape, and how the branches of the dendrites interact with each other and these characteristics largely determine the properties of the material. Monocrystalline whisker Whisker Brownian tree Patterns in nature STS-87 - Space Shuttle mission Mindat Manganese Dendrites What is a dendrite, the Isothermal Dendritic Growth Experiment Snow crystals Dendritic Solidification Dendritic growth in Local-Nonequilibrium Solidification Model
Dendrite (crystal)
–
Manganese dendrites on a limestone bedding plane from
Solnhofen, Germany. Scale in mm.
Dendrite (crystal)
–
Example of a dendrite on pyrolusite.
Dendrite (crystal)
–
A silver crystal
electrolytically refined with visible dendritic structures.
44.
Orbicular jasper
–
Orbicular jasper is a variety of jasper which contains variably-colored orbs or spherical inclusions or zones. The material is attractive when polished and is used as an ornamental stone or gemstone. Various local or commercial names have been used for the material, such as kinradite, oregonite, owyhee jasper, ocean jasper and poppy-patterned jasper, poppy-patterned jasper or poppy jasper is the varietal name for material from Morgan Hill, Santa Clara County, California. The trade name ocean jasper is used for a variety found along the shores of northeast Madagascar. In Nebraska orbicular jasper is found in altered rhyolite beds noted for a variety of jaspers, R. V. Dietrich - Gemrocks Mindat with location data Agate variety names - University of Nebraska-Lincoln USGS - jasper and other volcanic materials from Nebraska
Orbicular jasper
–
Orbicular jasper from Madagascar
Orbicular jasper
–
Unpolished poppy jasper, Morgan Hill
Orbicular jasper
–
Madagascar orbicular jasper (detail)
45.
Breccia
–
Breccia is a rock composed of broken fragments of minerals or rock cemented together by a fine-grained matrix that can be similar to or different from the composition of the fragments. The word has its origins in the Italian language, in which it means either loose gravel or stone made by cemented gravel. A breccia may have a variety of different origins, as indicated by the named types including sedimentary breccia, tectonic breccia, igneous breccia, impact breccia, and hydrothermal breccia. Sedimentary breccia is a type of sedimentary rock which is made of angular to subangular. A conglomerate, by contrast, is a rock composed of rounded fragments or clasts of pre-existing rocks. Both breccia and conglomerate are composed of fragments averaging greater than 2 millimetres in size, the angular shape of the fragments indicates that the material has not been transported far from its source. Sedimentary breccia consists of angular, poorly sorted, immature fragments of rocks in a finer grained groundmass which are produced by mass wasting and it is lithified colluvium or scree. Thick sequences of sedimentary breccia are generally formed next to fault scarps in grabens, Breccia may occur along a buried stream channel where it indicates accumulation along a juvenile or rapidly flowing stream. Sedimentary breccia may be formed by debris flows. Turbidites occur as fine-grained peripheral deposits to sedimentary breccia flows, in a karst terrain, a collapse breccia may form due to collapse of rock into a sinkhole or in cave development. Fault breccia results from the action of two fault blocks as they slide past each other. Subsequent cementation of these fragments may occur by means of the introduction of mineral matter in groundwater. Volcanic pyroclastic rocks are formed by explosive eruption of lava and any rocks which are entrained within the eruptive column and this may include rocks plucked off the wall of the magma conduit, or physically picked up by the ensuing pyroclastic surge. Lavas, especially rhyolite and dacite flows, tend to form volcanic rocks by a process known as autobrecciation. This occurs when the thick, nearly solid lava breaks up into blocks, the resulting breccia is uniform in rock type and chemical composition. Lavas may also pick up rock fragments, especially if flowing over unconsolidated rubble on the flanks of a volcano, within the volcanic conduits of explosive volcanoes the volcanic breccia environment merges into the intrusive breccia environment. There the upwelling lava tends to solidify during quiescent intervals only to be shattered by ensuing eruptions, clastic rocks are also commonly found in shallow subvolcanic intrusions such as porphyry stocks, granites and kimberlite pipes, where they are transitional with volcanic breccias. Intrusive rocks can become brecciated in appearance by multiple stages of intrusion and this may be seen in many granite intrusions where later aplite veins form a late-stage stockwork through earlier phases of the granite mass
Breccia
–
Basalt breccia; green
groundmass is composed of
epidote
Breccia
–
Megabreccia (left) at
Titus Canyon Narrows, Death Valley National Park, California
Breccia
–
Tertiary breccia at Resting Springs Pass, Mojave Desert, California
Breccia
–
Unusual breccia cemented by
azurite and
malachite,
Morenci Mine, Arizona
46.
Bruneau River
–
The Bruneau River is a 153-mile-long tributary of the Snake River, in the U. S. states of Idaho and Nevada. It runs through a canyon cut into ancient lava flows in southwestern Idaho. The Bruneau Canyon, which is up to 1,200 feet deep and 40 miles long, features rapids and hot springs, making it a popular whitewater trip. The Bruneau Rivers drainage basin is bounded by the Jarbidge Mountains to the southeast, the Owyhee Mountains and Chalk Hills to the west, the Bruneau River system originates within and near the Jarbidge and Mountain City Ranger Districts of the Humboldt-Toiyabe National Forest in northern Elko County. The three main streams are the East Fork Bruneau River, the West Fork Bruneau River, the Jarbidge River joins the West Fork, then the East and West Forks join to form the mainstem Bruneau River. Sheep Creek and Jacks Creek join from the west, and Clover Creek joins from the east, the Bruneau River emerges from the plateau and canyon region 16 miles upstream from its mouth at the Snake Rivers C. J. Strike Reservoir. At this point the river enters the broad and fertile Snake River Plain and this lower section of the watershed is occupied by farms and ranches, and the town of Bruneau. The Bruneau River is used for irrigation purposes near the Snake River, irrigation withdrawals result in a number of its tributary streams being largely dewatered annually. Much of the mainstem Bruneau River above Hot Spring is designated as a Wild and Scenic River, as are parts of the West Fork and East Fork, the Jarbidge Wilderness covers a portion of the southern end of the Bruneau watershed. The Bruneau River is protected in the new Bruneau - Jarbidge Rivers Wilderness, whitewater rafting and kayaking opportunities exist on the Bruneau and Jarbidge Rivers. The canyons contain stretches of whitewater with class 5 and class 6 rapids, Bruneau Dunes State Park Salmon Falls Creek List of longest streams of Idaho List of National Wild and Scenic Rivers NASA Earth Observatory page
Bruneau River
–
Bruneau River in Idaho
Bruneau River
–
The Bruneau River at Charleston-Deeth Road in
Elko County, Nevada, near its source.
Bruneau River
–
Charleston Reservoir near
Charleston, Nevada
47.
Idaho
–
Idaho is a state in the northwestern region of the United States. It borders the state of Montana to the east and northeast, Wyoming to the east, Nevada and Utah to the south, to the north, it shares a small portion of the Canadian border with the province of British Columbia. With a population of around 1.7 million people and an area of 83,569 square miles, Idaho is the 14th largest, the states capital and largest city is Boise. Idaho prior to European settlement was inhabited solely by Native American peoples, in the early 19th century, Idaho was considered part of the Oregon Country, an area disputed between the U. S. and the United Kingdom. Idaho was eventually admitted to the Union on July 3,1890, forming part of the Pacific Northwest, Idaho is divided into several distinct geographic and climatic regions. In the states north, the relatively isolated Idaho Panhandle is closely linked with Eastern Washington, the states south includes the Snake River Plain, while the south-east incorporates part of the Great Basin. Idaho is quite mountainous, and contains several stretches of the Rocky Mountains, additionally, around 38 percent of Idahos land is held by the United States Forest Service, the most of any state. Industries significant for the economy include manufacturing, agriculture, mining, forestry. Idahos agricultural sector supplies a number of different products, but the state is best known for its potato crop, the official state nickname is the Gem State, which references Idahos reputation for gemstones and, more broadly, its many wilderness areas. The exact origin of the remains a mystery. Willing later claimed that he had invented the name. Congress ultimately decided to name the area Colorado Territory when it was created in February 1861, thinking they would get a jump on the name, locals named a community in Colorado Idaho Springs. However, the name Idaho did not fall into obscurity, the same year Congress created Colorado Territory, a county called Idaho County was created in eastern Washington Territory. The county was named after a steamship named Idaho, which was launched on the Columbia River in 1860 and it is unclear whether the steamship was named before or after Willings claim was revealed. Regardless, a portion of Washington Territory, including Idaho County, was used to create Idaho Territory in 1863. Despite this lack of evidence for the origin of the name, the name Idaho may be derived from the Plains Apache word ídaahę́, which means enemy. The Comanches used this word to refer to the Idaho Territory, a 1956 Idaho history textbook says, Idaho is a Shoshoni Indian exclamation. The word consists of three parts, the first is Ee, which in English conveys the idea of coming down
Idaho
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Digitally colored elevation map of Idaho.
Idaho
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Flag
Idaho
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Shoshone Falls in south central Idaho.
Idaho
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Reynolds Creek Experimental Watershed in the Owyhee Mountains, about 50 miles (80 km) southwest of
Boise, Idaho
48.
Ynys Llanddwyn
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Ynys Llanddwyn or Llanddwyn Island is a small tidal island off the west coast of Anglesey northwest Wales. The island is of geological interest with pillow lava, jasper formations, the island forms part of the National Nature Reserve of Newborough Warren which includes the extensive and floristically rich sand dune system. Ynys Llanddwyn is an island, it remains attached to the mainland at all. It provides views of Snowdonia and the Llŷn Peninsula, the island is very rich in legends, and in particular the association with Dwynwen. The name Llanddwyn means The church of St. Dwynwen, Dwynwen is the Welsh patron saint of lovers, making her the Welsh equivalent of St. Valentine. Her Saints day is 25 January and is celebrated by the Welsh with cards. The island bears the remains of St Dwynwens Church. There are more than 10 miles of footpaths crossing Ynys Llanddwyn and Newborough Warren, including the Anglesey Coastal Path, the island provides a worth-while goal after the mile-long walk along the beach from the nearest car park. Ynys Llanddwyn, with the beach, has been awarded Blue Flag beach status in recognition of the cleanliness of the sea. Tŵr Mawr lighthouse marks the entrance to the Menai Strait. 1873 Construction of lighthouse on Ynys Llanddwyn,1903 Closure of the lifeboat station on Ynys Llanddwyn. 1911 RSPB Cymru opens in Llanddwyn. Bird charity born 100 years ago at Llanddwyn Island 3 December 1920 - Five crew members from the Rhoscolyn lifeboat are lost off Llanddwyn, in 2004, Ynys Llanddwyn was used as a filming location in Demi Moores romantic thriller Half Light. Tŵr Mawr was used as a lighthouse which plays a key role in the film, CGI was used to create the effect of a real light on top of the lighthouse. Bryn Terfel filmed his video for Cavatina on Ynys Llanddwyn a very romantic place In 2009. Lighthouses of Wales Their Architecture and Archaeology ISBN 1-871184-08-8 Half Light Filming Locations Anglesey History History of Llanddwyn Island, Llanddwyn by Janet Wood A walk on Llanddwyn and a few photos Bird charity born 100 years ago at Llanddwyn Island Aerial Video of Llanddwyn Island
Ynys Llanddwyn
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Ynys Llanddwyn Island old lighthouse with
Snowdonia in background
Ynys Llanddwyn
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The large lighthouse and cross at Llanddwyn.
Ynys Llanddwyn
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St Dwynwen's Church, Llanddwyn
Ynys Llanddwyn
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Pilots' cottages on Llanddwyn
49.
Flint
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Flint is a hard, sedimentary cryptocrystalline form of the mineral quartz, categorized as a variety of chert. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks, inside the nodule, flint is usually dark grey, black, green, white or brown in colour, and often has a glassy or waxy appearance. A thin layer on the outside of the nodules is usually different in colour, typically white, from a petrological point of view, flint refers specifically to the form of chert which occurs in chalk or marly limestone. Similarly, common chert occurs in limestone, the exact mode of formation of flint is not yet clear but it is thought that it occurs as a result of chemical changes in compressed sedimentary rock formations, during the process of diagenesis. One hypothesis is that a gelatinous material fills cavities in the sediment, such as bored by crustaceans or molluscs. This hypothesis certainly explains the shapes of flint nodules that are found. The source of dissolved silica in the media could be the spicules of silicious sponges. Certain types of flint, such as that from the south coast of England, pieces of coral and vegetation have been found preserved like amber inside the flint. Thin slices of the stone often reveal this effect, puzzling giant flint formations known as paramoudra and flint circles are found around Europe but especially in Norfolk, England on the beaches at Beeston Bump and West Runton. Flint sometimes occurs in large flint fields in Jurassic or Cretaceous beds, flint was used in the manufacture of tools during the Stone Age as it splits into thin, sharp splinters called flakes or blades when struck by another hard object. This process is referred to as knapping, flint mining is attested since the Palaeolithic, but became more common since the Neolithic. When struck against steel, a flint edge will produce sparks, the hard flint edge shaves off a particle of the steel that exposes iron which reacts with oxygen from the atmosphere and can ignite the proper tinder. Prior to the availability of steel, rocks of pyrite would be used along with the flint. These methods are popular in woodcraft, bushcraft, and among those who wish to use traditional skills, a later, major use of flint and steel was in the flintlock mechanism, used primarily in flintlock firearms, but also used on dedicated fire-starting tools. The sparks ignite the powder and that flame, in turn, ignites the main charge, propelling the ball, bullet. While the military use of the flintlock declined after the adoption of the cap from the 1840s onward, flintlock rifles. Flint and steel used to strike sparks were superseded by ferrocerium and this man-made material, when scraped with any hard, sharp edge, produces sparks that are much hotter than obtained with natural flint and steel, allowing use of a wider range of tinders. Because it can produce sparks when wet and can start fires when used correctly, ferrocerium is used in many cigarette lighters, where it is referred to as flint
Flint
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A sample of Miorcani flint from the
Cenomanian chalky marl layer of the
Moldavian Plateau. (ca. 7.5 cm wide)
Flint
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Pebble beach made up of flint nodules eroded out of the nearby
chalk cliffs,
Cape Arkona,
Rügen
Flint
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Neolithic flint axe, about 31 cm long
Flint
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Detail of flint used in a building in Wiltshire, England.
50.
Chert
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Chert is a fine-grained sedimentary rock composed of microcrystalline or cryptocrystalline silica. Depending on its origin, it can contain either microfossils, small macrofossils, Chert occurs as oval to irregular nodules in greensand, limestone, chalk, and dolostone formations as a replacement mineral, where it is formed as a result of some type of diagenesis. Where it occurs in chalk or marl, it is usually called flint and it also occurs in thin beds, when it is a primary deposit. Thick beds of chert occur in marine deposits. These thickly bedded cherts include the novaculite of the Ouachita Mountains of Arkansas, Oklahoma, the banded iron formations of Precambrian age are composed of alternating layers of chert and iron oxides. Chert also occurs in deposits and is known as diatomaceous chert. Diatomaceous chert consists of beds and lenses of diatomite which were converted during diagenesis into dense, in petrology the term chert is used to refer generally to all rocks composed primarily of microcrystalline, cryptocrystalline and microfibrous quartz. The term does not include quartzite, chalcedony is a microfibrous variety of quartz. Strictly speaking, the flint is reserved for varieties of chert which occur in chalk. Among non-geologists, the distinction between flint and chert is often one of quality - chert being lower quality than flint, among petrologists, chalcedony is sometimes considered separately from chert due to its fibrous structure. Since many cherts contain both microcrystalline and microfibrous quartz, it is difficult to classify a rock as completely chalcedony. The cryptocrystalline nature of chert, combined with its above average ability to resist weathering, recrystallization, for example, The 3.2 Ga chert of the Fig Tree Formation in the Barbeton Mountains between Swaziland and South Africa preserved non-colonial unicellular bacteria-like fossils. The Gunflint Chert of western Ontario preserves not only bacteria and cyanobacteria but also believed to be ammonia-consuming and some that resemble green algae. The Apex Chert of the Pilbara craton, Australia preserved eleven taxa of prokaryotes, the Bitter Springs Formation of the Amadeus Basin, Central Australia, preserves 850 Ma cyanobacteria and algae. The Rhynie chert of Scotland has remains of a Devonian land flora, in prehistoric times, chert was often used as a raw material for the construction of stone tools. Like obsidian, as well as some rhyolites, felsites, quartzites and this results in conchoidal fractures, a characteristic of all minerals with no cleavage planes. When a chert stone is struck against an iron-bearing surface sparks result and this makes chert an excellent tool for starting fires, and both flint and common chert were used in various types of fire-starting tools, such as tinderboxes, throughout history. Cherts are subject to problems when used as concrete aggregates, deeply weathered chert develops surface pop-outs when used in concrete that undergoes freezing and thawing because of the high porosity of weathered chert
Chert
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Chert
Chert
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A chert nodule from the
Onondaga limestone layer,
Buffalo, New York. (3.8 cm wide)
Chert
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Chert (dark bands) in the
Devonian Corriganville-New Creek limestone,
Everett, Pennsylvania
Chert
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One or more of the preceding sentences incorporates text from a publication now in the public domain: Frederick William Rudler (1911). "Jasper". In Chisholm, Hugh. Encyclopædia Britannica (11th ed.). Cambridge University Press.
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