1.
Argolis
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Argolis or the Argolid is one of the regional units of Greece. It is part of the region of Peloponnese, situated in the part of the Peloponnese peninsula and part of the tripoint area of Argolis. Much of the territory of region is situated in the Argolid Peninsula. Most arable land lies in the part of Argolis. Its primary agricultural resources are oranges and olives, Argolis has a coastline on the Saronic Gulf in the northeast and on the Argolic Gulf in the south and southeast. Notable mountains ranges are the Oligyrtos in the northwest, Lyrkeio and Ktenia in the west, Argolis has land borders with Arcadia to the west and southwest, Corinthia to the north, and the Islands regional unit to the east. Parts of the history of the area can be found in the articles on Argos, Mycenae, Epidaurus, Nafplio, Troezen, Ermioni, Kranidi, from 1833 to 1899, Argolis was part of Argolidocorinthia, which included present Corinthia, Hydra, Spetses and Kythira. It joined Corinthia to form Argolidocorinthia again in 1909, forty years later, in 1949, Argolis was finally separated from Corinthia. The regional unit Argolis is subdivided into 4 municipalities and these are, Argos-Mykines Epidaurus Ermionida Nafplio As a part of the 2011 Kallikratis government reform, the regional unit Argolis was created out of the former prefecture Argolis. The prefecture had the territory as the present regional unit
2.
Greece
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Greece, officially the Hellenic Republic, historically also known as Hellas, is a country in southeastern Europe, with a population of approximately 11 million as of 2015. Athens is the capital and largest city, followed by Thessaloniki. Greece is strategically located at the crossroads of Europe, Asia, situated on the southern tip of the Balkan peninsula, it shares land borders with Albania to the northwest, the Republic of Macedonia and Bulgaria to the north, and Turkey to the northeast. Greece consists of nine regions, Macedonia, Central Greece, the Peloponnese, Thessaly, Epirus, the Aegean Islands, Thrace, Crete. The Aegean Sea lies to the east of the mainland, the Ionian Sea to the west, the Cretan Sea and the Mediterranean Sea to the south. Greece has the longest coastline on the Mediterranean Basin and the 11th longest coastline in the world at 13,676 km in length, featuring a vast number of islands, eighty percent of Greece is mountainous, with Mount Olympus being the highest peak at 2,918 metres. From the eighth century BC, the Greeks were organised into various independent city-states, known as polis, which spanned the entire Mediterranean region and the Black Sea. Greece was annexed by Rome in the second century BC, becoming a part of the Roman Empire and its successor. The Greek Orthodox Church also shaped modern Greek identity and transmitted Greek traditions to the wider Orthodox World, falling under Ottoman dominion in the mid-15th century, the modern nation state of Greece emerged in 1830 following a war of independence. Greeces rich historical legacy is reflected by its 18 UNESCO World Heritage Sites, among the most in Europe, Greece is a democratic and developed country with an advanced high-income economy, a high quality of life, and a very high standard of living. A founding member of the United Nations, Greece was the member to join the European Communities and has been part of the Eurozone since 2001. Greeces unique cultural heritage, large industry, prominent shipping sector. It is the largest economy in the Balkans, where it is an important regional investor, the names for the nation of Greece and the Greek people differ from the names used in other languages, locations and cultures. The earliest evidence of the presence of human ancestors in the southern Balkans, dated to 270,000 BC, is to be found in the Petralona cave, all three stages of the stone age are represented in Greece, for example in the Franchthi Cave. Neolithic settlements in Greece, dating from the 7th millennium BC, are the oldest in Europe by several centuries and these civilizations possessed writing, the Minoans writing in an undeciphered script known as Linear A, and the Mycenaeans in Linear B, an early form of Greek. The Mycenaeans gradually absorbed the Minoans, but collapsed violently around 1200 BC and this ushered in a period known as the Greek Dark Ages, from which written records are absent. The end of the Dark Ages is traditionally dated to 776 BC, the Iliad and the Odyssey, the foundational texts of Western literature, are believed to have been composed by Homer in the 7th or 8th centuries BC. With the end of the Dark Ages, there emerged various kingdoms and city-states across the Greek peninsula, in 508 BC, Cleisthenes instituted the worlds first democratic system of government in Athens
3.
Regions of ancient Greece
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The regions of ancient Greece were areas identified by the ancient Greeks as geographical sub-divisions of the Hellenic world. These regions are described in the works of ancient historians and geographers, conceptually, there is no clear theme to the structure of these regions. Some, particularly in the Peloponnese, can be seen primarily as distinct units, defined by physical boundaries such as mountain ranges. These regions retained their identity, even when the identity of the living there changed during the Greek Dark Ages. Nevertheless, these regions also survived the upheaval of the Greek Dark Ages, outside the Peloponnese and central Greece, geographical divisions and identities did change over time suggesting a closer connection with tribal identity. Over time however, all the regions also acquired geo-political meanings and these traditional sub-divisions of Greece form the basis for the modern system of regional units of Greece. However, there are important differences, with many of the ancient regions not represented in the current system. To fully understand the ancient history of Greece therefore requires more detailed description of the ancient regions, continental Greece was a geographic region of Greece. In English the area is usually called Central Greece, but the equivalent Greek term is rarely used. Today it forms the part of the regional unit of Aetolia-Acarnania. The capital and principal city in ancient times was Stratos, the north side of Acarnania of the Corinthian Gulf was considered part of the region of Epirus. Acarnanias foundation in Greek mythology was traditionally ascribed to Acarnan, son of Alcmaeon, Aeniania or Ainis was a small district to the south of Thessaly. The lowland border in the Spercheios valley with Malis ran approximately north-south along from Oeta to the spur of Othrys. During the Archaic and Classical periods, the Aenianians were members of the Delphian Amphictyonic League, the country has a level and fruitful coastal region, but an unproductive and mountainous interior. The mountains contained many wild beasts, and acquired fame in Greek mythology as the scene of the hunt for the Calydonian Boar, Ancient Aperantia was a small region of Aetolia, south of Dolopia. The name of Attica was said to be derived from Atthis, daughter of Cranaus, Attica is bounded on the east by the Aegean sea, on the west by Megaris and the Saronic gulf and on the north by Boeotia. It is separated from Boeotia by a range of mountains, in the Archaic and Classical periods, the Atticans were members of the Delphian Amphictyonic League, and shared the two Ionian votes on the Amphictyonic council with the Euboeans. The region of Boeotia, along many of the cities that existed there in the Classical period, is described in the catalogue of ships
4.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
5.
Paleolithic
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The Paleolithic is a prehistoric period of human history distinguished by the development of the most primitive stone tools and covers roughly 95% of human technological prehistory. It extends from the earliest known use of tools, probably by Homo habilis initially,2.6 million years ago. The Paleolithic era is followed by the Mesolithic, the date of the Paleolithic–Mesolithic boundary may vary by locality as much as several thousand years. During the Paleolithic period, humans grouped together in small societies such as bands, the Paleolithic is characterized by the use of knapped stone tools, although at the time humans also used wood and bone tools. Other organic commodities were adapted for use as tools, including leather and vegetable fibers, however, due to their nature, surviving artifacts of the Paleolithic era are known as paleoliths. About 50,000 years ago, there was a increase in the diversity of artifacts. For the first time in Africa, bone artifacts and the first art appear in the archaeological record, the first evidence of human fishing is also noted, from artifacts in places such as Blombos cave in South Africa. The new technology generated an explosion of modern humans which is believed to have led to the extinction of the Neanderthals. Humankind gradually evolved from members of the genus Homo—such as Homo habilis. The climate during the Paleolithic consisted of a set of glacial and interglacial periods in which the climate periodically fluctuated between warm and cool temperatures, by c. 50,000 – c. 40,000 BP, the first humans set foot in Australia. By c. 45,000 BP, humans lived at 61°N latitude in Europe, by c. 30,000 BP, Japan was reached, and by c. 27,000 BP humans were present in Siberia, above the Arctic Circle. At the end of the Upper Paleolithic, a group of humans crossed Beringia, the term Paleolithic was coined by archaeologist John Lubbock in 1865. It derives from Greek, παλαιός, palaios, old, and λίθος, lithos, stone, human evolution is the part of biological evolution concerning the emergence of anatomically modern humans as a distinct species. The Paleolithic Period coincides almost exactly with the Pleistocene epoch of geologic time and this epoch experienced important geographic and climatic changes that affected human societies. During the preceding Pliocene, continents had continued to drift from possibly as far as 250 km from their present locations to positions only 70 km from their current location. South America became linked to North America through the Isthmus of Panama, most of Central America formed during the Pliocene to connect the continents of North and South America, allowing fauna from these continents to leave their native habitats and colonize new areas. Africas collision with Asia created the Mediterranean Sea, cutting off the remnants of the Tethys Ocean, climates during the Pliocene became cooler and drier, and seasonal, similar to modern climates. The formation of an Arctic ice cap around 3 million years ago is signaled by a shift in oxygen isotope ratios and ice-rafted cobbles in the North Atlantic
6.
Neolithic
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It ended when metal tools became widespread. The Neolithic is a progression of behavioral and cultural characteristics and changes, including the use of wild and domestic crops, the beginning of the Neolithic culture is considered to be in the Levant about 10, 200–8800 BC. It developed directly from the Epipaleolithic Natufian culture in the region, whose people pioneered the use of wild cereals, which then evolved into true farming. The Natufian period was between 12,000 and 10,200 BC, and the so-called proto-Neolithic is now included in the Pre-Pottery Neolithic between 10,200 and 8800 BC. By 10, 200–8800 BC, farming communities arose in the Levant and spread to Asia Minor, North Africa, Mesopotamia is the site of the earliest developments of the Neolithic Revolution from around 10,000 BC. Early Neolithic farming was limited to a range of plants, both wild and domesticated, which included einkorn wheat, millet and spelt, and the keeping of dogs, sheep. By about 6900–6400 BC, it included domesticated cattle and pigs, the establishment of permanently or seasonally inhabited settlements, not all of these cultural elements characteristic of the Neolithic appeared everywhere in the same order, the earliest farming societies in the Near East did not use pottery. Early Japanese societies and other East Asian cultures used pottery before developing agriculture, unlike the Paleolithic, when more than one human species existed, only one human species reached the Neolithic. The term Neolithic derives from the Greek νέος néos, new and λίθος líthos, stone, the term was invented by Sir John Lubbock in 1865 as a refinement of the three-age system. In the Middle East, cultures identified as Neolithic began appearing in the 10th millennium BC, early development occurred in the Levant and from there spread eastwards and westwards. Neolithic cultures are attested in southeastern Anatolia and northern Mesopotamia by around 8000 BC. The total excavated area is more than 1,200 square yards, the Neolithic 1 period began roughly 10,000 years ago in the Levant. A temple area in southeastern Turkey at Göbekli Tepe dated around 9500 BC may be regarded as the beginning of the period. This site was developed by nomadic tribes, evidenced by the lack of permanent housing in the vicinity. At least seven stone circles, covering 25 acres, contain limestone pillars carved with animals, insects, Stone tools were used by perhaps as many as hundreds of people to create the pillars, which might have supported roofs. Other early PPNA sites dating to around 9500–9000 BC have been found in Jericho, Israel, Gilgal in the Jordan Valley, the start of Neolithic 1 overlaps the Tahunian and Heavy Neolithic periods to some degree. The major advance of Neolithic 1 was true farming, in the proto-Neolithic Natufian cultures, wild cereals were harvested, and perhaps early seed selection and re-seeding occurred. The grain was ground into flour, emmer wheat was domesticated, and animals were herded and domesticated
7.
Greek language
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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
8.
Cave
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A cave is a hollow place in the ground, specifically a natural underground space large enough for a human to enter. Caves form naturally by the weathering of rock and often extend deep underground, the word cave can also refer to much smaller openings such as sea caves, rock shelters, and grottos. A cavern is a type of cave, naturally formed in soluble rock with the ability to grow speleothems. Speleology is the science of exploration and study of all aspects of caves, visiting or exploring caves for recreation may be called caving, potholing, or spelunking. The formation and development of caves is known as speleogenesis, which can occur over the course of millions of years, caves are formed by various geologic processes and can be variable sizes. These may involve a combination of processes, erosion from water, tectonic forces, microorganisms, pressure. Isotopic dating techniques can be applied to cave sediments, in order to determine the timescale when geologic events may have occurred to help form and it is estimated that the maximum depth of a cave cannot be more than 3,000 metres due to the pressure of overlying rocks. For karst caves the maximum depth is determined on the basis of the limit of karst forming processes. Most caves are formed in limestone by dissolution, solutional caves or karst caves are the most frequently occurring caves and such caves form in rock that is soluble. Most occur in limestone, but they can form in other rocks including chalk, dolomite, marble, salt. Rock is dissolved by acid in groundwater that seeps through bedding planes, faults, joints. Over geological epochs cracks expand to become caves and cave systems, the largest and most abundant solutional caves are located in limestone. Limestone dissolves under the action of rainwater and groundwater charged with H2CO3, the dissolution process produces a distinctive landform known as karst, characterized by sinkholes and underground drainage. Limestone caves are often adorned with calcium carbonate formations produced through slow precipitation and these include flowstones, stalactites, stalagmites, helictites, soda straws and columns. These secondary mineral deposits in caves are called speleothems, the portions of a solutional cave that are below the water table or the local level of the groundwater will be flooded. Lechuguilla Cave in New Mexico and nearby Carlsbad Cavern are now believed to be examples of type of solutional cave. They were formed by H2S gas rising from below, where reservoirs of oil give off sulfurous fumes and this gas mixes with ground water and forms H2SO4. The acid then dissolves the limestone from below, rather than from above, caves formed at the same time as the surrounding rock are called primary caves
9.
Argolic Gulf
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The Argolic Gulf is a gulf of the Aegean Sea off the east coast of the Peloponnese, Greece. It is about 50 km long and 30 km wide and its main port is Nafplio, at its northwestern end. At the entrance to the gulf is the island Spetses and this gulf and its islands are sometimes combined with the Saronic Gulf and Saronic Islands, with the result called the Argo-Saronic Gulf and the Argo-Saronic Islands. It is surrounded by two units, Arcadia to the southwest and Argolis to the north and east. The river Inachos drains into the Argolic Gulf near Nea Kios, the main islands in the gulf are Psili, Plateia and Bourtzi, a small island with a Venetian fortress that protects the port of Nafplio. The surrounding mountains protect it from the strong summer Meltemi wind
10.
Upper Paleolithic
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The Upper Paleolithic is the third and last subdivision of the Paleolithic or Old Stone Age. Very broadly, it dates to between 50,000 and 10,000 years ago, roughly coinciding with the appearance of behavioral modernity, modern humans are believed to have emerged about 195,000 years ago in Africa. Although these humans were modern in anatomy, their lifestyle changed very little from their contemporaries, such as Homo erectus, about 50,000 years ago, there was a marked increase in the diversity of artifacts. In Africa, bone artifacts and the first art appear in the archeological record, between 45,000 and 43,000 years ago, this new tool technology spread with human migration to Europe. The new technology generated an explosion of modern humans which is believed to have contributed to the extinction of the Neanderthals. The Upper Paleolithic has the earliest known evidence of organized settlements, in the form of campsites, artistic work blossomed, with cave painting, petroglyphs, carvings and engravings on bone or ivory. The first evidence of fishing is also noted, from artifacts in places such as Blombos cave in South Africa. More complex social groupings emerged, supported by more varied and reliable food sources and this probably contributed to increasing group identification or ethnicity. By 50, 000–40,000 BP, the first humans set foot in Australia, by 45,000 BP, humans lived at 61° north latitude in Europe. By 30,000 BP, Japan was reached, and by 27,000 BP humans were present in Siberia above the Arctic Circle, at the end of the Upper Paleolithic, a group of humans crossed the Bering land bridge and quickly expanded throughout North and South America. Both Homo erectus and Neanderthals used the same crude stone tools, archaeologist Richard G. Klein, who has worked extensively on ancient stone tools, describes the stone tool kit of archaic hominids as impossible to categorize. It was as if the Neanderthals made stone tools, and were not much concerned about their final forms and he argues that almost everywhere, whether Asia, Africa or Europe, before 50,000 years ago all the stone tools are much alike and unsophisticated. These new stone-tool types have been described as being distinctly differentiated from each other, the invaders, commonly referred to as the Cro-Magnons, left many sophisticated stone tools, carved and engraved pieces on bone, ivory and antler, cave paintings and Venus figurines. The Neanderthals continued to use Mousterian stone tool technology and possibly Chatelperronian technology and these tools disappeared from the archeological record at around the same time the Neanderthals themselves disappeared from the fossil record, about 40,000 years ago. Settlements were often located in valley bottoms, possibly associated with hunting of passing herds of animals. Hunting was important, and caribou/wild reindeer may well be the species of single greatest importance in the anthropological literature on hunting. Technological advances included significant developments in flint tool manufacturing, with industries based on fine blades rather than simpler and shorter flakes, burins and racloirs were used to work bone, antler and hides. Advanced darts and harpoons also appear in period, along with the fish hook, the oil lamp, rope
11.
Mesolithic
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In archaeology, the Mesolithic is the culture between Paleolithic and Neolithic. The term Epipaleolithic is often used for areas outside northern Europe, Mesolithic has different time spans in different parts of Eurasia. It was originally post-Pleistocene, pre-agricultural material in northwest Europe about 10,000 to 5000 BC, in the archaeology of Northern Europe, for example for archaeological sites in Great Britain, Germany, Scandinavia, Ukraine, and Russia, the term Mesolithic is almost always used. In the archaeology of other areas, the term Epipaleolithic may be preferred by most authors, in the New World, neither term is used. Other authors use the term Mesolithic for a variety of Late Paleolithic cultures subsequent to the end of the last glacial period whether they are transitional towards agriculture or not, conversely, those that are in course of transition toward artificial food production are assigned to the Mesolithic. Therefore, care must be taken in translating Mesolithic as Middle Stone Age, subdivisions of earlier and later were added to the Stone Age by Thomsen and especially his junior colleague and employee Jens Jacob Asmussen Worsaae. John Lubbock kept these divisions in his work Pre-historic Times in 1865 and he saw no need for an intermediate category. When Hodder Westropp introduced the Mesolithic in 1866, as an intermediate between Paleolithic and Neolithic, a storm of controversy immediately arose around it. A British school led by John Evans denied any need for an intermediate, the ages blended together like the colors of a rainbow, he said. A European school led by Louis Laurent Gabriel de Mortillet asserted that there was a gap between the earlier and later, edouard Piette claimed to have filled the gap with his discovery of the Azilian Culture. Knut Stjerna offered an alternative in the Epipaleolithic, a continuation of the use of Paleolithic technology, the start and end dates of the Mesolithic vary by geographical region. Childes view prevails that the term covers the period between the end of the Pleistocene and the start of the Neolithic. If the Mesolithic is more similar to the Paleolithic it is called the Epipaleolithic, the Paleolithic was an age of purely hunting and gathering while in the Neolithic domestication of plants and animals had occurred. Some Mesolithic peoples continued with intensive hunting, others were practising the initial stages of domestication. The type of remains the diagnostic factor, The Mesolithic featured composite devices manufactured with Mode V chipped stone tools. The Paleolithic had utilized Modes I–IV and the Neolithic mainly abandoned the chipped microliths in favor of polished, not chipped, the first period, known as Mesolithic 1, followed the Aurignacian or Levantine Upper Paleolithic periods throughout the Levant. By the end of the Aurignacian, gradual changes took place in stone industries, small stone tools called microliths and retouched bladelets can be found for the first time. The microliths of this period differ greatly from the Aurignacian artifacts
12.
Europe
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Europe is a continent that comprises the westernmost part of Eurasia. Europe is bordered by the Arctic Ocean to the north, the Atlantic Ocean to the west, yet the non-oceanic borders of Europe—a concept dating back to classical antiquity—are arbitrary. Europe covers about 10,180,000 square kilometres, or 2% of the Earths surface, politically, Europe is divided into about fifty sovereign states of which the Russian Federation is the largest and most populous, spanning 39% of the continent and comprising 15% of its population. Europe had a population of about 740 million as of 2015. Further from the sea, seasonal differences are more noticeable than close to the coast, Europe, in particular ancient Greece, was the birthplace of Western civilization. The fall of the Western Roman Empire, during the period, marked the end of ancient history. Renaissance humanism, exploration, art, and science led to the modern era, from the Age of Discovery onwards, Europe played a predominant role in global affairs. Between the 16th and 20th centuries, European powers controlled at times the Americas, most of Africa, Oceania. The Industrial Revolution, which began in Great Britain at the end of the 18th century, gave rise to economic, cultural, and social change in Western Europe. During the Cold War, Europe was divided along the Iron Curtain between NATO in the west and the Warsaw Pact in the east, until the revolutions of 1989 and fall of the Berlin Wall. In 1955, the Council of Europe was formed following a speech by Sir Winston Churchill and it includes all states except for Belarus, Kazakhstan and Vatican City. Further European integration by some states led to the formation of the European Union, the EU originated in Western Europe but has been expanding eastward since the fall of the Soviet Union in 1991. The European Anthem is Ode to Joy and states celebrate peace, in classical Greek mythology, Europa is the name of either a Phoenician princess or of a queen of Crete. The name contains the elements εὐρύς, wide, broad and ὤψ eye, broad has been an epithet of Earth herself in the reconstructed Proto-Indo-European religion and the poetry devoted to it. For the second part also the divine attributes of grey-eyed Athena or ox-eyed Hera. The same naming motive according to cartographic convention appears in Greek Ανατολή, Martin Litchfield West stated that phonologically, the match between Europas name and any form of the Semitic word is very poor. Next to these there is also a Proto-Indo-European root *h1regʷos, meaning darkness. Most major world languages use words derived from Eurṓpē or Europa to refer to the continent, in some Turkic languages the originally Persian name Frangistan is used casually in referring to much of Europe, besides official names such as Avrupa or Evropa
13.
European ass
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The European ass is an extinct equine from the middle and late Pleistocene of Eurasia. It appeared first in the fossil report 300,000 years before present, in the east the range apparently stretched at least to the Volga and to Iran. In the north it reached almost to the North Sea in Germany and it is possible that the Iberian cebro, extinct in the wild from the 16th century, could correspond to the Equus hydruntinus. Morphologically the European ass can be distinguished from asses and hemiones particularly by its molars, the exact systematic position is still not fully clear, but genetic and morphological analysis suggest that it is closely related to the Asiatic wild ass. The specific epithet, hydruntinus, means from Otranto, list of extinct animals of Europe
14.
Red deer
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The red deer is one of the largest deer species. The red deer inhabits most of Europe, the Caucasus Mountains region, Asia Minor, Iran, parts of western Asia and it also inhabits the Atlas Mountains region between Morocco and Tunisia in northwestern Africa, being the only species of deer to inhabit Africa. Red deer have been introduced to areas, including Australia, New Zealand, United States, Canada, Peru, Uruguay, Chile. In many parts of the world, the meat from red deer is used as a food source, Red deer are ruminants, characterized by a four-chambered stomach. Genetic evidence indicates the red deer as traditionally defined is a group, rather than a single species. It is probable that the ancestor of all red deer, including wapiti, originated in central Asia, although at one time red deer were rare in parts of Europe, they were never close to extinction. The red deer is the fourth-largest deer species behind moose, elk and it is a ruminant, eating its food in two stages and having an even number of toes on each hoof, like camels, goats and cattle. European red deer have a long tail compared to their Asian. The deer of Central and Western Europe vary greatly in size, large red deer stags, like the Caspian red deer or those of the Carpathian Mountains, may rival the wapiti in size. Female red deer are smaller than their male counterparts. The male red deer is typically 175 to 250 cm long and weighs 160 to 240 kg, the tail adds another 12 to 19 cm and shoulder height is about 95 to 130 cm. In Scotland, stags average 201 cm in length and 122 cm high at the shoulder. Size varies in different subspecies with the largest, the huge but small-antlered deer of the Carpathian Mountains, weighing up to 500 kg. At the other end of the scale, the Corsican red deer weighs about 80 to 100 kg, European red deer tend to be reddish-brown in their summer coats. The males of many subspecies also grow a short neck mane during the autumn, the male deer of the British Isles and Norway tend to have the thickest and most noticeable manes. Male Caspian red deer and Spanish red deer do not carry neck manes, male deer of all subspecies, however, tend to have stronger and thicker neck muscles than female deer, which may give them an appearance of having neck manes. Red deer hinds do not have neck manes, the European red deer is adapted to a woodland environment. Only the stags have antlers, which growing in the spring and are shed each year
15.
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
16.
Last Glacial Maximum
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The Last Glacial Maximum was the last period in the Earths climate history during the last glacial period when ice sheets were at their greatest extension. Growth of the ice sheets reached their positions in about 24,500 BCE. Vast ice sheets covered much of North America, northern Europe, the ice sheets profoundly affected Earths climate by causing drought, desertification, and a dramatic drop in sea levels. It was followed by the Late Glacial, the formation of an ice sheet or ice cap requires both prolonged cold and precipitation. Hence, despite having temperatures similar to those of glaciated areas in North America and Europe and this difference was because the ice sheets in Europe produced extensive anticyclones above them. These anticyclones generated air masses that were so dry on reaching Siberia and Manchuria that precipitation sufficient for the formation of glaciers could never occur, all over the world, climates at the Last Glacial Maximum were cooler and almost everywhere drier. Even in less affected regions, rainforest cover was greatly diminished, only in Central America and the Chocó region of Colombia did tropical rainforests remain substantially intact – probably due to the extraordinarily heavy rainfall of these regions. Most of the worlds deserts expanded and this also occurred in Afghanistan and Iran, where a major lake formed in the Dasht-e Kavir. In Australia, shifting sand dunes covered half the continent, whilst the Chaco, in northern China – unglaciated despite its cold climate – a mixture of grassland and tundra prevailed, and even here, the northern limit of tree growth was at least 20° farther south than today. During the Last Glacial Maximum, much of the world was cold, dry, and inhospitable, with frequent storms, the dustiness of the atmosphere is a prominent feature in ice cores, dust levels were as much as 20 to 25 times greater than now. This was probably due to a number of factors, reduced vegetation, stronger global winds, the massive sheets of ice locked away water, lowering the sea level, exposing continental shelves, joining land masses together, and creating extensive coastal plains. During the last glacial maximum,21,000 years ago, Northern Europe was largely covered by ice, the southern boundary of the ice sheets passing through Germany and Poland. This ice extended northward to cover Svalbard and Franz Josef Land and northeastward to occupy the Barents Sea, permafrost covered Europe south of the ice sheet down to present-day Szeged in Southern Hungary. Ice covered the whole of Iceland and almost all of the British Isles, britain was no more than a peninsula of Europe, its north capped in ice, and its south a polar desert. There were ice sheets in modern Tibet as well as in Baltistan, in Southeast Asia, many smaller mountain glaciers formed, and permafrost covered Asia as far south as Beijing. Palawan was also part of Sundaland, while the rest of the Philippine Islands formed one large island separated from the continent only by the Sibutu Passage and the Mindoro Strait. In Africa and the Middle East, many mountain glaciers formed. The Persian Gulf averages about 35 metres in depth and the seabed between Abu Dhabi and Qatar is even shallower, being less than 15 metres deep
17.
Obsidian
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Obsidian is a naturally occurring volcanic glass formed as an extrusive igneous rock. It is produced when felsic lava extruded from a volcano cools rapidly with minimal crystal growth, Obsidian is commonly found within the margins of rhyolitic lava flows known as obsidian flows, where the chemical composition induces a high viscosity and polymerization degree of the lava. The inhibition of atomic diffusion through this highly viscous and polymerized lava explains the lack of crystal growth. Obsidian is hard and brittle, it therefore fractures with very sharp edges, which were used in the past in cutting and piercing tools, among the various forms of glass we may reckon Obsidian glass, a substance very similar to the stone found by Obsidius in Ethiopia. Obsidian is the rock formed as a result of quickly cooled lava, tektites were once thought by many to be obsidian produced by lunar volcanic eruptions, though few scientists now adhere to this hypothesis. Obsidian is mineral-like, but not a true mineral because as a glass it is not crystalline, in addition and it is sometimes classified as a mineraloid. Though obsidian is usually dark in color similar to mafic rocks such as basalt, Obsidian consists mainly of SiO2, usually 70% or more. Crystalline rocks with obsidians composition include granite and rhyolite, because obsidian is metastable at the Earths surface, no obsidian has been found that is older than Cretaceous age. This breakdown of obsidian is accelerated by the presence of water, having a low water content when newly formed, typically less than 1% water by weight, obsidian becomes progressively hydrated when exposed to groundwater, forming perlite. Pure obsidian is usually dark in appearance, though the color varies depending on the presence of impurities, iron and other transition elements may give the obsidian a dark brown to black color. Very few samples are nearly colorless, in some stones, the inclusion of small, white, radially clustered crystals of cristobalite in the black glass produce a blotchy or snowflake pattern. Obsidian may contain patterns of gas bubbles remaining from the lava flow and these bubbles can produce interesting effects such as a golden sheen. An iridescent, rainbow-like sheen is caused by inclusions of magnetite nanoparticles, Obsidian can be found in locations which have experienced rhyolitic eruptions. Obsidian can also be found in the eastern U. S. states of Virginia, as well as Pennsylvania, there are only four major deposit areas in the central Mediterranean, Lipari, Pantelleria, Palmarola and Monte Arci. Ancient sources in the Aegean were Milos and Gyali, acıgöl town and the Göllü Dağ volcano were the most important sources in central Anatolia, one of the more important source areas in the prehistoric Near East. Use of obsidian in pottery of the Neolithic in the area around Lipari was found to be less at a distance representing two weeks journeying. Anatolian sources of obsidian are known to have been the used in the Levant. The first attested civilized use is from excavations at Tell Brak dated the late fifth millennia, Obsidian was valued in Stone Age cultures because, like flint, it could be fractured to produce sharp blades or arrowheads
18.
Melos
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Milos or Melos is a volcanic Greek island in the Aegean Sea, just north of the Sea of Crete. Milos is the southwesternmost island in the Cyclades group, the island is famous for the statue of Aphrodite, and also for statues of the Greek god Asclepius, the Poseidon and an archaic Apollo in Athens. Milos is a popular tourist destination during the summer, the Municipality of Milos also includes the uninhabited offshore islands of Antimilos and Akradies. The combined land area is 160.147 square kilometres and the 2011 census population was 4,977 inhabitants, obsidian from Milos was a commodity as early as 15,000 years ago. The mining of obsidian did not lead to the development of permanent habitation or manufacturing on the island, instead, those in search of obsidian arrived by boat, beaching it in a suitable cove and cutting pieces of the volcanic glass from the quarries. The position of Milos, between mainland Greece and Crete, and its possession of obsidian, made it an important centre of early Aegean civilisation, Milos lost its arms-making importance when bronze became the preferred material for the manufacture of weapons. The first settlement at Phylakopi arose in the Bronze Age, flourishing as the extraction of obsidian was in the decline, the first settlers were tuna fishermen. The famous fresco of the fish was found in the ruins of the Pillar room and was executed with delicate colouring. Stylistic similarities to Minoan frescoes are suggested, and it could perhaps have been the work of a Cretan artist, part of the site has been washed away by the sea. The antiquities found at the site covered three major periods, from the Early Cycladic period to the Mycenaean period, at the site much pottery was excavated, with several changing styles and influences over the sites long occupation. In the early occupation of the site, there are similarities and imports from other Cycladic islands. The quantities found at the Cycladic sites have taken to suggest a Minoan control over the region. At Phylakopi a Megaron structure, which is associated with the Mycenaean palaces, such as those at Tiryns, Pylos. This has been taken to suggest that the Mycenaeans conquered the settlement, the evidence is not clear, though again it could be a legacy of the islanders adopting foreign elements into their culture. Particularly unexpected was the discovery in the 1970s of a shrine at the site, the shrine is unprecedented in the Bronze Age Cyclades and has provided a valuable insight ito the beliefs and rituals of the inhabitants of Phylakopi. The site was abandoned and was never reoccupied. The first Dorian settlement on Melos was established no earlier than the 1st millennium BC, dorians are the ethnic group to which the Spartans belonged, but the Dorian settlers of Melos made themselves independent. They eventually established a city whose site lies on the shore of the bay
19.
Seafaring
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Seamanship is the art of operating a ship or boat. The degree of knowledge needed within these areas is dependent upon the nature of the work, navigation is the art and science of safely and efficiently directing the movements of a vessel from one point to another. Piloting uses water depth and visible references, while dead reckoning uses courses and distances from the last known position, more than just finding a vessels present location, safe navigation includes predicting future location, route planning and collision avoidance. Nautical navigation in western nations, like air navigation, is based on the nautical mile, navigation also includes electronics such as GPS and Loran. Celestial navigation involves taking sights by sextant on the planets, moon, stars, sun and using the data with a nautical almanac, accurate time information is also needed. After nautical dusk, navigation at sea referencing the horizon is no longer possible, a fundamental skill of professional seamanship is being able to maneuver a vessel with accuracy and precision. Unlike vehicles on land, a ship afloat is subject to the movements of the air around it, another complicating factor is the mass of a ship that has to be accounted for when stopping and starting. Ship-handling is about arriving and departing a berth or buoy, maneuvering in confined channels and harbours and in proximity to other ships, two other types of operations, berthing alongside another ship and replenishment at sea, are occasionally included. Fundamental to low-speed maneuvering is an understanding of the configuration and handedness of the propeller, thus to put the vessel into astern mode the rudder can be rotated through 180 degrees without altering the speed and direction of the engine. Since with the propeller or rudder configuration the propeller is designed to operate at maximum efficiency when going ahead. But with the Kortz Nozzle, the ahead and astern thrust is the same, most commercial vessels in excess of size limits determined by local authorities are handled in confined areas by a marine pilot. Marine pilots are seafarers with extensive seafaring experience and are usually qualified master mariners who have trained as expert ship-handlers. These pilots are conversant with all types of vessel and propulsion systems, as well as handling ships of all sizes in all weather and they are also experts in the geographical areas they work. In most countries, the pilot takes over the conduct of the navigation from the ship master and this means that the master and crew should adhere to the pilots orders in respect of the safe navigation of the vessel when in a compulsory pilotage area. The master may with good cause resume conduct of the vessels navigation, however this should never be done lightly. In situations where the pilot is an advisor even though he has the con, the master, upon realizing there is a dangerous situation developing, must take such action as to avoid an accident or at least to minimize the damage from one that cant be avoided. In some countries and areas, the role is as an advisor. However, in practice, they are likely to have the conduct of the vessel, especially on larger ships using tug boats to assist
20.
Anatomically modern humans
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Anatomically modern humans evolved from archaic humans in the Middle Paleolithic, about 200,000 years ago. The emergence of modern human marks the dawn of the species Homo sapiens. Other fossils include the proposed Homo sapiens idaltu from Herto in Ethiopia that are almost 160,000 years old and the Skhul hominids from Israel, which are 90,000 years old. The oldest human remains from which an entire genome has been extracted belongs to Ust-Ishim man, however, it can and has been argued that Homo sapiens have been fully capable of modern behavior from the time they first evolved. The binomial name for the species of the human population is Homo sapiens. The species is taken to have emerged from a predecessor within the Homo genus around 200,000 years ago. Generally, modern humans are more lightly built than archaic humans from which they have evolved, Humans are a highly variable species, modern humans can show remarkably robust traits, and early modern humans even more so. Despite this, modern humans differ from archaic people in a range of anatomical details, the cranium lacks a pronounced occipital bun in the neck, a bulge that anchored considerable neck muscles in Neanderthals. Modern humans, even the ones, generally have a larger fore-brain than the archaic people. This will usually give a higher forehead, and reduced brow ridge and this splits the ridge into a central part and two distal parts. In current humans, often only the section of the ridge is preserved. This contrasts with archaic humans, where the ridge is pronounced. Modern humans commonly have a steep, even vertical forehead whereas their predecessors had foreheads that sloped strongly backwards, according to Desmond Morris, the vertical forehead in humans not only houses larger brains, but plays an important role in human communication through eyebrow movements and forehead skin wrinkling. Compared to archaic people, anatomically modern humans have smaller, differently shaped teeth and this results in a smaller, more receded dentary, making the rest of the jaw-line stand out, giving an often quite prominent chin. The central part of the forming the chin carries a triangularly shaped area forming the apex of the chin called the mental trigon. Particularly in living population, the use of fire and tools require fewer jaw muscles, giving slender, compared to archaic people, modern humans have smaller, lower faces. The body skeletons of even the earliest and most robustly built modern humans were less robust than those of Neanderthals, particularly regarding the long bones of the limbs, the distal bones are nearly the same size or slightly shorter than the proximal bones. In ancient people, particularly Neanderthals, the bones were shorter
21.
Homo Erectus
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Homo erectus is an extinct species of hominid that lived throughout most of the Pleistocene geological epoch. Its earliest fossil evidence dates to 1.9 million years ago and extends to 70,000 years ago, or, possibly, as recently as 35,000 years ago. It is generally thought that H. erectus originated in Africa and spread from there, migrating throughout Eurasia as far as Georgia, India, Sri Lanka, China, a new debate appeared in 2013, with the documentation of the Dmanisi skulls.58 million years ago. From there it migrated, in part, by 2, the fossil record shows that its development from about 1.8 mya to one mya was widely distributed, in Africa, the Transcaucasus, Indonesia, and in Vietnam, China, and India. The second hypothesis is that H. erectus evolved in Eurasia and they occupied the Dmanisi site from 1.85 million to 1.77 million years ago, which was about the same time or slightly before their earliest evidence in Africa. There are several proposed explanations of the dispersal of H. erectus georgicus—including whether or not Africa is the source), the Dutch anatomist Eugène Dubois was fascinated by Darwins theory of evolution especially as it applied to humankind. In 1886, he set out for Asia—which then was the region accepted as the cradle of evolution despite Darwins theory of African origin. In 1891, his team discovered a human fossil on the island of Java, the Java fossil from Indonesia aroused much public interest. It was dubbed by the press as Java Man, but few scientists accepted Dubois argument that his fossil was the transitional form—the so-called missing link—between apes. Java Man is now classified as Homo erectus, most of the spectacular discoveries of H. erectus next took place at the Zhoukoudian Project, now known as the Peking Man Site, in Zhoukoudian, China. This site was first discovered by Johan Gunnar Andersson in 1921 and was first excavated in 1921, canadian anatomist Davidson Blacks initial description of a lower molar as belonging to a previously unknown species prompted widely publicized interest. Extensive excavations followed, which altogether uncovered 200 human fossils from more than 40 individuals including five nearly complete skullcaps, german anatomist Franz Weidenreich provided much of the detailed description of this material in several monographs published in the journal Palaeontologica Sinica. Throughout much of the 20th century, anthropologists debated the role of H. erectus in human evolution, early in the century, due in part to the discoveries at Java and Zhoukoudian, it was widely accepted that modern humans first evolved in Asia. From the 1950s forward, numerous finds in East Africa confirmed the hypothesis of an African genesis and it is now generally accepted that H. erectus descended from either, 1) the earliest hominin genera, or 2) the earliest Homo-species. East Africa provided sympatric coexistence for H. erectus and H, in the 1950s, archaeologists John T. Robinson and Robert Broom named Telanthropus capensis, Robinson had discovered a jaw fragment in 1949 in Swartkrans, South Africa. Later, Simonetta proposed to re-designate it to Homo erectus, in 1961, Yves Coppens discovered a skull of Tchadanthropus uxoris, then the earliest fossil human discovered in north Africa. It was reported that the fossil had been so eroded by sand that it mimicked the appearance of an australopith. Although at first considered to be a specimen of H. habilis, T. uxoris is no longer considered a valid taxon, and has been subsumed into H. erectus
22.
Homo Heidelbergensis
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Homo heidelbergensis – also Homo rhodesiensis – is an extinct species of the genus Homo that lived in Africa, Europe and western Asia between 600,000 and 200,000 years ago. The skulls of this species share features with both Homo erectus and anatomically modern Homo sapiens, its brain was nearly as large as that of Homo sapiens. The Sima de los Huesos cave at Atapuerca in northern Spain holds particularly rich layers of deposits that represent an exceptional reserve of data where excavations are still in progress. Neanderthals, Denisovans, and modern humans are all considered to have descended from Homo heidelbergensis that appeared around 700,000 years ago in Africa, fossils have been recovered in Ethiopia, Namibia and South Africa. Between 300,000 and 400,000 years ago a group of Homo heidelbergensis migrated into Europe and West Asia via yet unknown routes, archaeological sites exist in Spain, Italy, France, England, Germany, Hungary and Greece. Another Homo heidelbergensis group ventured eastwards into continental Asia, eventually developing into Denisovans, some researchers suggest that the finds associated to Homo heidelbergensis are mere variants of Homo erectus. Both Homo antecessor and Homo heidelbergensis are likely to have descended from the very similar Homo ergaster from Africa. The anatomy is more primitive than that of Neanderthal, but the harmoniously rounded dental arch. Heidelbergensis from other known human species, the species name heidelbergensis only experienced a renaissance with the many discoveries of the past 30 years and appears now to be recognized by an increasing number of researchers. Any form of segregation is considered arbitrary, which is why these researchers forgo the name H. heidelbergensis altogether. Paleoanthropologists often refer to the surrounding the specimens, their dating and morphology, as “the muddle in the middle. ”The fact that there seem to be no clear transitions makes it difficult to draw up a list of unique characteristics of H. heidelbergensis that distinguishes it from H. erectus. In general, the show a continuation of evolutionary trends that are emerging from around the Lower into Middle Pleistocene. Along with changes in the robustness of cranial and dental features, male H. heidelbergensis averaged about 1.75 m tall and 62 kg. Females averaged 1.57 m and 51 kg, the available space would allow for a far greater flexibility of development and It shows a combination of features, which has been previously found neither on a recent nor a fossil human mandible. The actual proof that we are dealing with human parts here only lies within the nature of the dentition, the completely preserved teeth bear the stamp human as evidence, The canines show no trace of a stronger expression in relation to the other groups of teeth. They suggest a moderate and harmonious co-evolution, as it is the case in recent humans, recent findings in a pit in Atapuerca of 28 human skeletons suggest that H. heidelbergensis might have been the first species of the Homo genus to bury its dead. Steven Mithen believes that H. heidelbergensis, like its descendant H. neanderthalensis, acquired a pre-linguistic system of communication. No forms of art have been uncovered, although red ochre, the morphology of the outer and middle ear suggests they had an auditory sensitivity similar to modern humans and very different from chimpanzees
23.
Crete
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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
24.
Younger Dryas
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The Younger Dryas is a geological period from c.12,900 to c.11,700 calendar years ago. It is named after a genus, the alpine-tundra wildflower Dryas octopetala. Leaves of Dryas octopetala are occasionally abundant in the Late Glacial, often minerogenic-rich, the Younger Dryas saw a sharp decline in temperature over most of the northern hemisphere, at the end of the Pleistocene epoch, immediately preceding the current warmer Holocene. It was the most recent and longest of several interruptions to the warming of the Earths climate since the severe Last Glacial Maximum. The Younger Dryas was a period of change, but the effects were complex. In the southern hemisphere, and some areas of the such as southeastern North America. The presence of a cold period at the end of the Late Glacial interval has been known for a long time. Paleobotanical and lithostratigraphic studies of Swedish and Danish bog and lake sites, e. g. the Allerød clay pit in Denmark, first recognized and described the Younger Dryas. The Younger Dryas is the youngest and longest of three stadials that resulted from typically abrupt climatic changes that took place over the last 16,000 calendar years. This is not securely dated, and estimates vary by 400 years, in northern Scotland the glaciers were thicker and more extensive than during the Younger Dryas. The Older Dryas, in turn, is preceded by another warmer stage and this stadial is often, but not always, known as the Oldest Dryas. The Oldest Dryas occurred approximately 1,770 calendar years before the Younger Dryas, according to the GISP2 ice core from Greenland, the Oldest Dryas occurred between about 15,070 and 14,670 calendar years BP. In Ireland, the Younger Dryas has also known as the Nahanagan Stadial. In the Greenland Summit ice core chronology, the Younger Dryas corresponds to Greenland Stadial 1, the preceding Allerød warm period is subdivided into three events, Greenland Interstadial-1c to 1a. This drastic change in vegetation is typically interpreted to be an effect of a decrease in temperature. In sharp contrast to the warming of the preceding Older Dryas interstadial and it has been inferred that its end occurred over a period of a decade or so, but the onset may have been faster. Thermally fractionated nitrogen and argon isotope data from Greenland ice core GISP2 indicate that the summit of Greenland was approximately 15 °C colder during the Younger Dryas than today. Nothing of the size, extent, or rapidity of this period of climate change has been experienced since its end
25.
Climate
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Climate is the statistics of weather, usually over a 30-year interval. Climate differs from weather, in that weather only describes the conditions of these variables in a given region. A regions climate is generated by the system, which has five components, atmosphere, hydrosphere, cryosphere, lithosphere. The climate of a location is affected by its latitude, terrain, climates can be classified according to the average and the typical ranges of different variables, most commonly temperature and precipitation. The most commonly used classification scheme was the Köppen climate classification, the Bergeron and Spatial Synoptic Classification systems focus on the origin of air masses that define the climate of a region. Paleoclimatology is the study of ancient climates, Climate models are mathematical models of past, present and future climates. Climate change may occur long and short timescales from a variety of factors. For example, a 3°C change in mean annual temperature corresponds to a shift in isotherms of approximately 300–400 km in latitude or 500 m in elevation, therefore, species are expected to move upwards in elevation or towards the poles in latitude in response to shifting climate zones. Climate is commonly defined as the weather averaged over a long period, the standard averaging period is 30 years, but other periods may be used depending on the purpose. Climate also includes statistics other than the average, such as the magnitudes of day-to-day or year-to-year variations, the classical period is 30 years, as defined by the World Meteorological Organization. These quantities are most often surface variables such as temperature, precipitation, Climate in a wider sense is the state, including a statistical description, of the climate system. The World Meteorological Organization describes climate normals as reference points used by climatologists to compare current climatological trends to that of the past or what is considered normal, a Normal is defined as the arithmetic average of a climate element over a 30-year period. A30 year period is used, as it is enough to filter out any interannual variation or anomalies. The WMO originated from the International Meteorological Organization which set up a commission for climatology in 1929. At its 1934 Wiesbaden meeting the commission designated the thirty-year period from 1901 to 1930 as the reference time frame for climatological standard normals. In 1982 the WMO agreed to update climate normals, and in these were completed on the basis of climate data from 1 January 1961 to 31 December 1990. The difference between climate and weather is usefully summarized by the popular phrase Climate is what you expect, weather is what you get. Over historical time spans there are a number of nearly constant variables that determine climate, including latitude, altitude, proportion of land to water and these change only over periods of millions of years due to processes such as plate tectonics
26.
Holocene
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The Holocene is the geological epoch that began after the Pleistocene at approximately 11,700 years before present. The term Recent has often used as an exact synonym of Holocene. The Holocene is part of the Quaternary period and its name comes from the Ancient Greek words ὅλος and καινός, meaning entirely recent. It has been identified with the current warm period, known as MIS1, given these, a new term, Anthropocene, is specifically proposed and used informally only for the very latest part of modern history involving significant human impact. It is accepted by the International Commission on Stratigraphy that the Holocene started approximately 11,700 years ago, the epoch follows the Pleistocene and the last glacial period. The Holocene can be subdivided into five time intervals, or chronozones, based on climatic fluctuations, Preboreal, Boreal, Atlantic, Subboreal and they find a general correspondence across Eurasia and North America, though the method was once thought to be of no interest. The scheme was defined for Northern Europe, but the changes were claimed to occur more widely. The periods of the include a few of the final pre-Holocene oscillations of the last glacial period. Paleontologists have not defined any faunal stages for the Holocene, if subdivision is necessary, periods of human technological development, such as the Mesolithic, Neolithic, and Bronze Age, are usually used. However, the time periods referenced by these terms vary with the emergence of those technologies in different parts of the world, climatically, the Holocene may be divided evenly into the Hypsithermal and Neoglacial periods, the boundary coincides with the start of the Bronze Age in Europe. According to some scholars, a division, the Anthropocene, has now begun. Continental motions due to plate tectonics are less than a kilometre over a span of only 10,000 years, however, ice melt caused world sea levels to rise about 35 m in the early part of the Holocene. The sea level rise and temporary land depression allowed temporary marine incursions into areas that are now far from the sea, Holocene marine fossils are known, for example, from Vermont and Michigan. Other than higher-latitude temporary marine incursions associated with depression, Holocene fossils are found primarily in lakebed, floodplain. Holocene marine deposits along low-latitude coastlines are rare because the rise in sea levels during the period exceeds any likely tectonic uplift of non-glacial origin, post-glacial rebound in the Scandinavia region resulted in the formation of the Baltic Sea. The region continues to rise, still causing weak earthquakes across Northern Europe, the equivalent event in North America was the rebound of Hudson Bay, as it shrank from its larger, immediate post-glacial Tyrrell Sea phase, to near its present boundaries. Climate has been stable over the Holocene. It appears that this was influenced by the glacial ice remaining in the Northern Hemisphere until the later date
27.
Natural environment
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The natural environment encompasses all living and non-living things occurring naturally. The term is most often applied to the Earth or some part of Earth and this environment encompasses the interaction of all living species, climate, weather, and natural resources that affect human survival and economic activity. Even acts which seem less extreme, such as building a mud hut or a system in the desert. Though many animals build things to provide an environment for themselves, they are not human, hence beaver dams. People seldom find absolutely natural environments on Earth, and naturalness usually varies in a continuum, more precisely, we can consider the different aspects or components of an environment, and see that their degree of naturalness is not uniform. If, for instance, in a field, the mineralogic composition and the structure of its soil are similar to those of an undisturbed forest soil. Natural environment is used as a synonym for habitat. For instance, when we say that the environment of giraffes is the savanna. Earth science generally recognizes 4 spheres, the lithosphere, the hydrosphere, the atmosphere, and the biosphere as correspondent to rocks, water, air, and life respectively. Some scientists include, as part of the spheres of the Earth, Earth science, is an all-embracing term for the sciences related to the planet Earth. There are four major disciplines in sciences, namely geography, geology, geophysics. These major disciplines use physics, chemistry, biology, chronology, the Earths crust, or lithosphere, is the outermost solid surface of the planet and is chemically and mechanically different from underlying mantle. It has been generated greatly by igneous processes in which magma cools, beneath the lithosphere lies the mantle which is heated by the decay of radioactive elements. The mantle though solid is in a state of rheic convection and this convection process causes the lithospheric plates to move, albeit slowly. The resulting process is known as plate tectonics, volcanoes result primarily from the melting of subducted crust material or of rising mantle at mid-ocean ridges and mantle plumes. An ocean is a body of saline water, and a component of the hydrosphere. Approximately 71% of the Earths surface is covered by ocean, a body of water that is customarily divided into several principal oceans. More than half of area is over 3,000 meters deep
28.
Small game
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Game or quarry is any animal hunted for sport or for food. The type and range of animals hunted for food varies in different parts of the world, in some countries, game is classified, including legal classification with respect to licences required, as either small game or large game. Game or quarry is any animal hunted for sport or for food, the term game arises in medieval hunting terminology by the late 13th century and is particular to English, from the generic meaning of Old English gamen joy, amusement, sport, merriment. Small game includes animals, such as rabbits, pheasants. Large game includes animals like deer and bear, big game is a term sometimes used interchangeably with large game although in other contexts it refers to large, typically African, mammals which are hunted mainly for trophies in safaris. The type and range of animals hunted for food varies in different parts of the world and this is influenced by climate, animal diversity, local taste and locally accepted views about what can or cannot be legitimately hunted. Sometimes a distinction is made between varieties and species of a particular animal, such as wild turkey and domestic turkey. Fish caught for sport are referred to as game fish, the flesh of the animal, when butchered for consumption is often described as having a gamey flavour. This difference in taste can be attributed to the diet of the animal. In some countries, game is classified, including legal classification with respect to licences required, a single small game licence may cover all small game species and be subject to yearly bag limits. Large game are often subject to individual licensing where a licence is required for each individual animal taken. In some parts of Africa, wild animals hunted for their meat are called bushmeat, see article for more detailed information on how this operates within the economy. In Africa, animals hunted for their pelts or ivory are sometimes referred to as the big game, also see the legal definition of game in Swaziland. South Africa has 62 species of gamebirds, including guineafowl, francolin, partridge, quail, sandgrouse, duck, geese, snipe, bustard, of the remaining 41 species,24 have shown an increase in numbers and distribution range in the last 25 years or so. The status of 14 species appears unchanged, with insufficient information being available for the three species. S. and Canada, deer are the most commonly hunted big game. Other game species include, In the PRC there is a special category called ye wei. In the UK game is defined in law by the Game Act 1831 and it is illegal to shoot game on Sundays or at night. Other that are hunted for food in the UK are specified under the Wildlife, the ban is generally considered voluntary on private lands, and few birds live away from RSPB or Forestry Commission land allegedly
29.
Fish
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A fish is any member of a group of animals that consist of all gill-bearing aquatic craniate animals that lack limbs with digits. They form a group to the tunicates, together forming the olfactores. Included in this definition are the living hagfish, lampreys, and cartilaginous, tetrapods emerged within lobe-finned fishes, so cladistically they are fish as well. However, traditionally fish are rendered obsolete or paraphyletic by excluding the tetrapods, because in this manner the term fish is defined negatively as a paraphyletic group, it is not considered a formal taxonomic grouping in systematic biology. The traditional term pisces is considered a typological, but not a phylogenetic classification, the earliest organisms that can be classified as fish were soft-bodied chordates that first appeared during the Cambrian period. Although they lacked a true spine, they possessed notochords which allowed them to be more agile than their invertebrate counterparts, fish would continue to evolve through the Paleozoic era, diversifying into a wide variety of forms. Many fish of the Paleozoic developed external armor that protected them from predators, the first fish with jaws appeared in the Silurian period, after which many became formidable marine predators rather than just the prey of arthropods. Fish are abundant in most bodies of water and they can be found in nearly all aquatic environments, from high mountain streams to the abyssal and even hadal depths of the deepest oceans. With 33,100 described species, fish exhibit greater species diversity than any group of vertebrates. Fish are an important resource for humans worldwide, especially as food, commercial and subsistence fishers hunt fish in wild fisheries or farm them in ponds or in cages in the ocean. They are also caught by fishers, kept as pets, raised by fishkeepers. Fish have had a role in culture through the ages, serving as deities, religious symbols, fish do not represent a monophyletic group, and therefore the evolution of fish is not studied as a single event. Early fish from the record are represented by a group of small, jawless. Jawless fish lineages are mostly extinct, an extant clade, the lampreys may approximate ancient pre-jawed fish. The first jaws are found in Placodermi fossils, the diversity of jawed vertebrates may indicate the evolutionary advantage of a jawed mouth. It is unclear if the advantage of a hinged jaw is greater biting force, improved respiration, fish may have evolved from a creature similar to a coral-like sea squirt, whose larvae resemble primitive fish in important ways. The first ancestors of fish may have kept the form into adulthood. Fish are a group, that is, any clade containing all fish also contains the tetrapods
30.
Mollusks
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The molluscs compose the large phylum Mollusca of invertebrate animals. Around 85,000 extant species of molluscs are recognized, molluscs are the largest marine phylum, comprising about 23% of all the named marine organisms. Numerous molluscs also live in freshwater and terrestrial habitats and they are highly diverse, not just in size and in anatomical structure, but also in behaviour and in habitat. The phylum is divided into 9 or 10 taxonomic classes. The gastropods are by far the most numerous molluscs in terms of classified species, the three most universal features defining modern molluscs are a mantle with a significant cavity used for breathing and excretion, the presence of a radula, and the structure of the nervous system. Other than these things, molluscs express great morphological diversity, so many textbooks base their descriptions on an ancestral mollusc. This has a single, limpet-like shell on top, which is made of proteins and chitin reinforced with calcium carbonate, the underside of the animal consists of a single muscular foot. Although molluscs are coelomates, the coelom tends to be small, the main body cavity is a hemocoel through which blood circulates, their circulatory systems are mainly open. The generalized mollusc has two paired nerve cords, or three in bivalves, the brain, in species that have one, encircles the esophagus. Most molluscs have eyes, and all have sensors to detect chemicals, vibrations, the simplest type of molluscan reproductive system relies on external fertilization, but more complex variations occur. All produce eggs, from which may emerge trochophore larvae, more complex veliger larvae, good evidence exists for the appearance of gastropods, cephalopods and bivalves in the Cambrian period 541 to 485.4 million years ago. Molluscs have, for centuries, also been the source of important luxury goods, notably pearls, mother of pearl, Tyrian purple dye and their shells have also been used as money in some preindustrial societies. Mollusc species can also represent hazards or pests for human activities, the bite of the blue-ringed octopus is often fatal, and that of Octopus apollyon causes inflammation that can last for over a month. Stings from a few species of large tropical cone shells can also kill, schistosomiasis is transmitted to humans via water snail hosts, and affects about 200 million people. Snails and slugs can also be serious pests, and accidental or deliberate introduction of some snail species into new environments has seriously damaged some ecosystems. The words mollusc and mollusk are both derived from the French mollusque, which originated from the Latin molluscus, from mollis, molluscus was itself an adaptation of Aristotles τα μαλακά, the soft things, which he applied to cuttlefish. The scientific study of molluscs is accordingly called malacology, as it is now known these groups have no relation to molluscs, and very little to one another, the name Molluscoida has been abandoned. The most universal features of the structure of molluscs are a mantle with a significant cavity used for breathing and excretion
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Tuna
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A tuna is a saltwater fish that belongs to the tribe Thunnini, a sub-grouping of the mackerel family – which together with the tunas, also includes the bonitos, mackerels, and Spanish mackerels. Thunnini comprises fifteen species across five genera, the sizes of which vary greatly, the bluefin averages 2 m, and is believed to live for up to 50 years. Tuna and mackerel sharks are the species of fish that can maintain a body temperature higher than that of the surrounding water. An active and agile predator, the tuna has a sleek, streamlined body, found in warm seas, it is extensively fished commercially, and is popular as a game fish. As a result of over-fishing, stocks of tuna species such as the southern bluefin tuna have been reduced dangerously close to the point of extinction. The term tuna ultimately derives from Thunnus, the Middle Latin form of the Ancient Greek, θύννος tunny-fish – which is in turn derived from θύνω, rush, the following cladogram illustrates the relationship between the tunas and other tribes of the family Scombridae. The true tunas are those that belong to the genus Thunnus, until recently, it was thought that there were seven Thunnus species, and that Atlantic bluefin tuna and Pacific bluefin tuna were subspecies of a single species. In 1999, Collette established that based on molecular and morphological considerations, they are in fact distinct species. The genus Thunnus is further classified into two subgenera, Thunnus, and Thunnus, the Thunnini tribe also includes seven additional species of tuna across four genera. They are, The tuna is a sleek and streamlined fish and it has two closely spaced dorsal fins on its back, The first is depressible – it can be laid down, flush, in a groove that runs along its back. Seven to ten yellow finlets run from the fins to the tail. The caudal peduncle, to which the tail is attached, is quite thin, the tunas dorsal side is generally a metallic dark blue, while the ventral side, or underside, is silvery or whitish, for camouflage. Thunnus are widely but sparsely distributed throughout the oceans of the world, generally in tropical, all tunas are able to maintain the temperature of certain parts of their body above the temperature of ambient seawater. For example, bluefin can maintain a body temperature of 25–33 °C. However, unlike typical endothermic creatures such as mammals and birds, tunas achieve endothermy by conserving the heat generated through normal metabolism. In all tunas, the heart operates at ambient temperature, as it receives cooled blood, also unlike most fish, which have white flesh, the muscle tissue of tuna ranges from pink to dark red. The red myotomal muscles derive their color from myoglobin, an oxygen-binding molecule, the oxygen-rich blood further enables energy delivery to their muscles. For powerful swimming animals like dolphins and tuna, cavitation may be detrimental, even if they have the power to swim faster, dolphins may have to restrict their speed, because collapsing cavitation bubbles on their tail are too painful
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Agriculture
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Agriculture is the cultivation and breeding of animals, plants and fungi for food, fiber, biofuel, medicinal plants and other products used to sustain and enhance human life. Agriculture was the key development in the rise of human civilization. The study of agriculture is known as agricultural science, the history of agriculture dates back thousands of years, and its development has been driven and defined by greatly different climates, cultures, and technologies. Industrial agriculture based on large-scale monoculture farming has become the dominant agricultural methodology, genetically modified organisms are an increasing component of agriculture, although they are banned in several countries. Agricultural food production and water management are increasingly becoming global issues that are fostering debate on a number of fronts, the major agricultural products can be broadly grouped into foods, fibers, fuels, and raw materials. Specific foods include cereals, vegetables, fruits, oils, meats, fibers include cotton, wool, hemp, silk and flax. Raw materials include lumber and bamboo, other useful materials are also produced by plants, such as resins, dyes, drugs, perfumes, biofuels and ornamental products such as cut flowers and nursery plants. The word agriculture is a late Middle English adaptation of Latin agricultūra, from ager, field, Agriculture usually refers to human activities, although it is also observed in certain species of ant, termite and ambrosia beetle. To practice agriculture means to use resources to produce commodities which maintain life, including food, fiber, forest products, horticultural crops. This definition includes arable farming or agronomy, and horticulture, all terms for the growing of plants, even then, it is acknowledged that there is a large amount of knowledge transfer and overlap between silviculture and agriculture. In traditional farming, the two are often combined even on small landholdings, leading to the term agroforestry, Agriculture began independently in different parts of the globe, and included a diverse range of taxa. At least 11 separate regions of the Old and New World were involved as independent centers of origin, wild grains were collected and eaten from at least 105,000 years ago. Pigs were domesticated in Mesopotamia around 15,000 years ago, rice was domesticated in China between 13,500 and 8,200 years ago, followed by mung, soy and azuki beans. Sheep were domesticated in Mesopotamia between 13,000 and 11,000 years ago. From around 11,500 years ago, the eight Neolithic founder crops, emmer and einkorn wheat, hulled barley, peas, lentils, bitter vetch, chick peas and flax were cultivated in the Levant. Cattle were domesticated from the aurochs in the areas of modern Turkey. In the Andes of South America, the potato was domesticated between 10,000 and 7,000 years ago, along with beans, coca, llamas, alpacas, sugarcane and some root vegetables were domesticated in New Guinea around 9,000 years ago. Sorghum was domesticated in the Sahel region of Africa by 7,000 years ago, cotton was domesticated in Peru by 5,600 years ago, and was independently domesticated in Eurasia at an unknown time
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Near East
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The Near East is a geographical term that roughly encompasses Western Asia. Despite having varying definitions within different academic circles, the term was applied to the maximum extent of the Ottoman Empire. The term has fallen into disuse in English and has replaced by the terms Middle East. The Food and Agriculture Organization of the United Nations defines the region similarly, but also includes Afghanistan while excluding the countries of North Africa and the Palestinian territories. Up until 1912 the Ottomans retained a band of territory including Albania, Macedonia and Southern Thrace, the Ottoman Empire, believed to be about to collapse, was portrayed in the press as the sick man of Europe. The Balkan states, with the exception of Bosnia and Albania, were primarily Christian. Starting in 1894 the Ottomans struck at the Armenians on the grounds that they were a non-Muslim people. The Hamidian Massacres aroused the indignation of the entire Christian world, in the United States the now aging Julia Ward Howe, author of the Battle Hymn of the Republic, leaped into the war of words and joined the Red Cross. Relations of minorities within the Ottoman Empire and the disposition of former Ottoman lands became known as the Eastern Question and it now became relevant to define the east of the eastern question. In about the middle of the 19th century Near East came into use to describe part of the east closest to Europe. The term Far East appeared contemporaneously meaning Japan, China, Korea, Indonesia, near East applied to what had been mainly known as the Levant, which was in the jurisdiction of the Ottoman Porte, or government. Those who used the term had little choice about its meaning and they could not set foot on most of the shores of the southern and central Mediterranean from the Gulf of Sidra to Albania without permits from the Ottoman Empire. Some regions beyond the Ottoman Porte were included, one was North Africa west of Egypt. It was occupied by piratical kingdoms of the Barbary Coast, de facto independent since the 18th century, formerly part of the empire at its apogee. Iran was included because it could not easily be reached except through the Ottoman Empire or neighboring Russia, in the 1890s the term tended to focus on the conflicts in the Balkan states and Armenia. The demise of the man of Europe left considerable confusion as to what was to be meant by Near East. It is now used only in historical contexts, to describe the countries of Western Asia from the Mediterranean to Iran. There is, in short, no universally understood fixed inventory of nations and they appear together in the journals of the mid-19th century
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Pre-Pottery Neolithic B
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Pre-Pottery Neolithic B is a division of the Neolithic developed by Kathleen Kenyon during her archaeological excavations at Jericho in the West Bank. In addition the flint tool kit of the period is new, one of its major elements is the naviform core. This is the first period in which architectural styles of the southern Levant became primarily rectilinear, earlier typical dwellings were circular, elliptical, pyrotechnology was highly developed in this period. During this period, one of the features of houses is evidenced by a thick layer of white clay plaster floors highly polished. It is believed that the use of plaster for floor. The earliest proto-pottery was White Ware vessels, made from lime and gray ash, built up around baskets before firing, sites from this period found in the Levant utilizing rectangular floor plans and plastered floor techniques were found at Ain Ghazal, Yiftahel, and Abu Hureyra. The period is dated to between ca.10,700 and ca.8,000 BP or 7000 -6000 BCE. Danielle Stordeurs recent work at Tell Aswad, an agricultural village between Mount Hermon and Damascus could not validate Henri de Contensons earlier suggestion of a PPNA Aswadian culture. Instead, they found evidence of a fully established PPNB culture at 8700 BC at Aswad, similar sites to Tell Aswad in the Damascus Basin of the same age were found at Tell Ramad and Tell Ghoraifé. How a PPNB culture could spring up in this location, practicing domesticated farming from 8700 BC has been the subject of speculation. Like the earlier PPNA people, the PPNB culture developed from the Earlier Natufian but shows evidence of a northerly origin, work at the site of Ain Ghazal in Jordan has indicated a later Pre-Pottery Neolithic C period which existed between 8,200 and 7,900 BP. Cultures practicing this lifestyle spread down the Red Sea shoreline and moved east from Syria into southern Iraq
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Anthropomorphic
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Anthropomorphism is the attribution of human traits, emotions, and intentions to non-human entities and is considered to be an innate tendency of human psychology. Personification is the attribution of human form and characteristics to abstract concepts such as nations, emotions and natural forces like seasons. Both have ancient roots as storytelling and artistic devices, and most cultures have traditional fables with anthropomorphized animals as characters, people have also routinely attributed human emotions and behavioural traits to wild as well as domestic animals. Anthropomorphism derives from its verb form anthropomorphize, itself derived from the Greek ánthrōpos and it is first attested in 1753, originally in reference to the heresy of applying a human form to the Christian God. One of the oldest known is a sculpture, the Löwenmensch figurine, Germany. It is not possible to say what these prehistoric artworks represent, in either case there is an element of anthropomorphism. This anthropomorphic art has been linked by archaeologist Steven Mithen with the emergence of more systematic hunting practices in the Upper Palaeolithic. In religion and mythology, anthropomorphism refers to the perception of a divine being or beings in human form, ancient mythologies frequently represented the divine as deities with human forms and qualities. They resemble human beings not only in appearance and personality, they exhibited many human behaviors that were used to explain phenomena, creation. The deities fell in love, married, had children, fought battles, wielded weapons and they feasted on special foods, and sometimes required sacrifices of food, beverage, and sacred objects to be made by human beings. Some anthropomorphic deities represented specific concepts, such as love, war, fertility, beauty. Anthropomorphic deities exhibited human qualities such as beauty, wisdom, and power, and sometimes human weaknesses such as greed, hatred, jealousy, Greek deities such as Zeus and Apollo often were depicted in human form exhibiting both commendable and despicable human traits. Anthropomorphism in this case is referred to as anthropotheism, from the perspective of adherents to religions in which humans were created in the form of the divine, the phenomenon may be considered theomorphism, or the giving of divine qualities to humans. Anthropomorphism has cropped up as a Christian heresy, particularly prominently with the Audians in third century Syria, but also in fourth century Egypt and tenth century Italy. This often was based on an interpretation of Genesis 1,27, So God created man in His own image, in the image of God created He him. Some religions, scholars, and philosophers objected to anthropomorphic deities. Ethiopians say that their gods are snub–nosed and blackThracians that they are pale and he said that the greatest god resembles man neither in form nor in mind. Both Judaism and Islam reject an anthropomorphic deity, believing that God is beyond human comprehension, judaisms rejection of an anthropomorphic deity grew during the Hasmonean period, when Jewish belief incorporated some Greek philosophy. Judaisms rejection grew further after the Islamic Golden Age in the tenth century, hindus do not reject the concept of a deity in the abstract unmanifested, but note practical problems
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Zoomorphic
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The word zoomorphism derives from the Greek ζωον, meaning animal, and μορφη, meaning shape or form. But this does not portray anything exactly like zoomorphism, Holy Spirit is seen like a dove and He is not a dove. The Holy Spirit was seen like a dove, bible does not teach zoomorphic appearance of God. Mark the Evangelist as a lion in later Christian iconography, the Egyptian gods were often depicted as zoomorphic or as hybrid A literary phrase such as The roar of the ocean. Sin lurking like a beast waiting to devour Cain in Genesis, fenrisulfr, a wolf in Norse mythology Airavata, the king god of elephants in Indian mythology. For instance, in Bedknobs and Broomsticks, the army that fights the Nazis is composed of anthropomorphized knightly body armor, in The Flintstones and Night at the Museum, the dinosaurs Dino and Rexy behave and vocalize like dogs. The city of Wau was to be transformed in the shape of a giraffe
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International Standard Book Number
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The International Standard Book Number is a unique numeric commercial book identifier. An ISBN is assigned to each edition and variation of a book, for example, an e-book, a paperback and a hardcover edition of the same book would each have a different ISBN. The ISBN is 13 digits long if assigned on or after 1 January 2007, the method of assigning an ISBN is nation-based and varies from country to country, often depending on how large the publishing industry is within a country. The initial ISBN configuration of recognition was generated in 1967 based upon the 9-digit Standard Book Numbering created in 1966, the 10-digit ISBN format was developed by the International Organization for Standardization and was published in 1970 as international standard ISO2108. Occasionally, a book may appear without a printed ISBN if it is printed privately or the author does not follow the usual ISBN procedure, however, this can be rectified later. Another identifier, the International Standard Serial Number, identifies periodical publications such as magazines, the ISBN configuration of recognition was generated in 1967 in the United Kingdom by David Whitaker and in 1968 in the US by Emery Koltay. The 10-digit ISBN format was developed by the International Organization for Standardization and was published in 1970 as international standard ISO2108, the United Kingdom continued to use the 9-digit SBN code until 1974. The ISO on-line facility only refers back to 1978, an SBN may be converted to an ISBN by prefixing the digit 0. For example, the edition of Mr. J. G. Reeder Returns, published by Hodder in 1965, has SBN340013818 -340 indicating the publisher,01381 their serial number. This can be converted to ISBN 0-340-01381-8, the check digit does not need to be re-calculated, since 1 January 2007, ISBNs have contained 13 digits, a format that is compatible with Bookland European Article Number EAN-13s. An ISBN is assigned to each edition and variation of a book, for example, an ebook, a paperback, and a hardcover edition of the same book would each have a different ISBN. The ISBN is 13 digits long if assigned on or after 1 January 2007, a 13-digit ISBN can be separated into its parts, and when this is done it is customary to separate the parts with hyphens or spaces. Separating the parts of a 10-digit ISBN is also done with either hyphens or spaces, figuring out how to correctly separate a given ISBN number is complicated, because most of the parts do not use a fixed number of digits. ISBN issuance is country-specific, in that ISBNs are issued by the ISBN registration agency that is responsible for country or territory regardless of the publication language. Some ISBN registration agencies are based in national libraries or within ministries of culture, in other cases, the ISBN registration service is provided by organisations such as bibliographic data providers that are not government funded. In Canada, ISBNs are issued at no cost with the purpose of encouraging Canadian culture. In the United Kingdom, United States, and some countries, where the service is provided by non-government-funded organisations. Australia, ISBNs are issued by the library services agency Thorpe-Bowker
38.
Cave of Zeus
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The Cave of Zeus is a system of caves located on the slopes of Mount Ida, on the island of Crete, Greece. The deep cave has an entrance and features stalagmites and stalactites. It is one of a number of believed to have been the birthplace or hiding place of Zeus. Excavations have revealed a number of votive cult offerings on the site. The Cave of Zeus may also refer to a cave by the name on the Aegean island of Naxos or the Psychro Cave on Crete. Cave of Zeus, Aydın in Turkey
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Petralona cave
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The site came to public attention when in 1960 a fossilized hominid skull was found. The cave had been discovered only a year earlier after erosion had left clefts in the rock. Bejeweled with impressive stalactite and stalagmite formations and holding an abundance of fossils the cave soon attracted geologists and paleontologists, after decades of excavations the cave is open to the public and scientific work is documented and presented in an adjacent Archaeological Museum. He considers it the oldest European hominid ever found and assessed it to be 800.000 years old, yet there was the constant problem that the skull was an isolated find as other scientists strongly disagree and the find has been a continuing cause of controversy since. The Anthropological Associations conclusions and results are in conflict with accepted speciation models of the genus Homo. The on-site Anthropological Museum of Petralona displays a selection of the caves findings, the cave was discovered accidentally in 1959 by Fillipos Chatzaridis, a local shepherd who was looking for a spring. In his effort to find a source he found a small cleft on the slopes of Mount Katsika. Two men were lowered down and later described a number of chambers and corridors, totaling 8 to 10 meters high with rich. The cave developed during the Mesozoic limestone, its sediments are divided into several stratigraphic levels, the rock formations resemble giant cactus, pink pearls, sturdy columns or delicate curtains, and in several places water ponds are fed by stalactite material. Covering an area of 10,400 m2, the length of the corridors is about 2,000 m, the first research of 1959 was undertaken by the Greek speleologist Ioannis Petrocheilos. He found numerous bones of animals, many of them covered with cave coral, the skull of the Archanthropus was according to Aris Poulianos found by another villager, Christos Sariannidis in 1960, hanging at the wall about 30 cm above ground, where it was held by sinter. Aris N. Poulianos states, that estimates at the time placed the age of the hominid remains to around 70,000 years. He announced that the date was based on analyses of the cave’s stratigraphy, in 1981, the age of the Petralona skull deduced by Poulianos was investigated and the protocol published in the Nature journal. The scientists involved used electron spin resonance measurements of the calcite encrustation and of bone fragments, however, Poulianos states that his excavations in the cave since 1968 provide evidence of human occupation from the Pleistocene era. The Petralona hominid, specifically, was located in a layer containing the highest amount of tools. Poulianos claims that the age of the layer is approximately 670,000 years old. Other researchers point out, that contextual animal fossils found with it are elsewhere from approximately 350,000 years ago. In 1987 researchers announced that the cranium cant be older than 620.000 years after palaeo-magnetic, the results confirm earlier findings that the whole of layer 10 represents a long time span, from about 160 ka to more than 350 ka
40.
Psychro Cave
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Psychro Cave is an ancient Minoan sacred cave in Lasithi plateau in the Lasithi district of eastern Crete. Psychro is associated with the Diktaean Cave, one of the sites of the birth of Zeus. Psychro is 1,025 metres above sea level, the cave is located in the prefecture of Lasithi. The Dictaean cave is famous in Greek mythology as the place where Amalthea, the archaeology attests to the sites long use as a place of cult worship. The nurse of Zeus, who was charged by Rhea to raise the infant Zeus in secret here and it is one of a number of caves believed to have been the birthplace or hiding place of Zeus. The mountains, of which the cave are part, are known in Crete as Dikte, the cave was first excavated in 1886 by Joseph Hatzidakis, President of the Syllogos at Candia, and F. Halbherr. In 1896, Sir Arthur Evans investigated the site, in 1899, J. Bones among the ash layer attest to sacrifice of bulls, sheep and goats, deer and a boar. More recent excavation has revealed the use of the cave reached back to Early Minoan times, the lower grotto falls steeply with traces of a rock-cut stair to a pool, out of which stalactites rise. Much earth had been thrown down by diggers of the Upper Grotto, Hogarth reported, in the vertical chinks of the lowest stalactites, Hogarths team found toy double-axes, knife-blades, needles, and other objects in bronze, placed there by dedicators, as in niches. The mud also at the edge of the pool was rich in similar things. In 1961, the art historian and archaeologist John Boardman published the finds uncovered by these, while clay human figurines are normally found in peak sanctuaries, Psychro and the sanctuary on Mount Ida stand out as the only sacred caves that have yielded human figurines. Psychro is also a sacred cave for a bronze leg, also known as a votive body part. More common sacred cave finds at Psychro include stone and ceramic lamps, Psychro yielded an uncommon number of semi-precious stones, including carnelian, steatite, amethyst, jasper and hematite. Psychros artefacts are now on display at the Heraklion Museum, the Ashmolean Museum in Oxford, the Louvre, jones, Donald W.1999 Peak Sanctuaries and Sacred Caves in Minoan Crete ISBN 91-7081-153-9 Rutkowski, B. and Krzysztof Nowicki,1996. The Psychro Cave and Other Sacred Grottoes in Crete, the Cave Sanctuary of Zeus at Psychro, A Study of Extra-Urban Sanctuaries in Minoan and Early Iron Age Crete Hellenic Ministry of Culture
