1.
Via Appia
–
The Appian Way was one of the earliest and strategically most important Roman roads of the ancient republic. It connected Rome to Brindisi, in southeast Italy and its importance is indicated by its common name, recorded by Statius, Appia longarum. The Appian Way was used as a route for military supplies since its construction for that purpose in 312 B. C. The Appian Way was the first long road built specifically to transport troops outside the region of greater Rome. The few roads outside the city were Etruscan and went mainly to Etruria. By the late Republic, the Romans had expanded over most of Italy and were masters of road construction, Rome had an affinity for the people of Campania, who, like themselves, traced their backgrounds to the Etruscans. The Samnite Wars were instigated by the Samnites when Rome attempted to ally itself with the city of Capua in Campania, the Italic speakers in Latium had long ago been subdued and incorporated into the Roman state. They were responsible for changing Rome from a primarily Etruscan to a primarily Italic state, dense populations of sovereign Samnites remained in the mountains north of Capua, which is just north of the Greek city of Neapolis. Around 343 BC, Rome and Capua attempted to form an alliance, the Samnites reacted with military force. Between Capua and Rome lay the Pontine Marshes, a swamp infested with malaria, a tortuous coastal road wound between Ostia at the mouth of the Tiber and Neapolis. The via Latina followed its ancient and scarcely more accessible path along the foothills of Monti Laziali and Monti Lepini, in the First Samnite War the Romans found they could not support or resupply troops in the field against the Samnites across the marsh. A revolt of the Latin League drained their resources further and they gave up the attempted alliance and settled with Samnium. The Romans were only biding their time while they looked for a solution, the first answer was the colonia, a cultivation of settlers from Rome, who would maintain a permanent base of operations. The Second Samnite War erupted when Rome attempted to place a colony at Cales in 334, the Samnites, now a major power after defeating the Greeks of Tarentum, occupied Neapolis to try to ensure its loyalty. The Neapolitans appealed to Rome, which sent an army and expelled the Samnites from Neapolis, in 312 BC, Appius Claudius Caecus became censor at Rome. He was of the gens Claudia, who were descended from the Sabines taken into the early Roman state. He had been given the name of the ancestor of the gens. He was a populist, i. e. an advocate of the common people, a man of inner perspicacity, in the years of success he was said to have lost his outer vision and thus acquired the name caecus, blind
Via Appia
–
The path of the Via Appia and of the Via Appia Traiana.
Via Appia
–
Remains of the Appian Way in
Rome, near Casalrotondo
Via Appia
–
Near Rome.
Via Appia
–
Porta San Sebastiano is the gate of the Appia in the
Aurelian Walls.
2.
Italy
–
Italy, officially the Italian Republic, is a unitary parliamentary republic in Europe. Located in the heart of the Mediterranean Sea, Italy shares open land borders with France, Switzerland, Austria, Slovenia, San Marino, Italy covers an area of 301,338 km2 and has a largely temperate seasonal and Mediterranean climate. Due to its shape, it is referred to in Italy as lo Stivale. With 61 million inhabitants, it is the fourth most populous EU member state, the Italic tribe known as the Latins formed the Roman Kingdom, which eventually became a republic that conquered and assimilated other nearby civilisations. The legacy of the Roman Empire is widespread and can be observed in the distribution of civilian law, republican governments, Christianity. The Renaissance began in Italy and spread to the rest of Europe, bringing a renewed interest in humanism, science, exploration, Italian culture flourished at this time, producing famous scholars, artists and polymaths such as Leonardo da Vinci, Galileo, Michelangelo and Machiavelli. The weakened sovereigns soon fell victim to conquest by European powers such as France, Spain and Austria. Despite being one of the victors in World War I, Italy entered a period of economic crisis and social turmoil. The subsequent participation in World War II on the Axis side ended in defeat, economic destruction. Today, Italy has the third largest economy in the Eurozone and it has a very high level of human development and is ranked sixth in the world for life expectancy. The country plays a prominent role in regional and global economic, military, cultural and diplomatic affairs, as a reflection of its cultural wealth, Italy is home to 51 World Heritage Sites, the most in the world, and is the fifth most visited country. The assumptions on the etymology of the name Italia are very numerous, according to one of the more common explanations, the term Italia, from Latin, Italia, was borrowed through Greek from the Oscan Víteliú, meaning land of young cattle. The bull was a symbol of the southern Italic tribes and was often depicted goring the Roman wolf as a defiant symbol of free Italy during the Social War. Greek historian Dionysius of Halicarnassus states this account together with the legend that Italy was named after Italus, mentioned also by Aristotle and Thucydides. The name Italia originally applied only to a part of what is now Southern Italy – according to Antiochus of Syracuse, but by his time Oenotria and Italy had become synonymous, and the name also applied to most of Lucania as well. The Greeks gradually came to apply the name Italia to a larger region, excavations throughout Italy revealed a Neanderthal presence dating back to the Palaeolithic period, some 200,000 years ago, modern Humans arrived about 40,000 years ago. Other ancient Italian peoples of undetermined language families but of possible origins include the Rhaetian people and Cammuni. Also the Phoenicians established colonies on the coasts of Sardinia and Sicily, the Roman legacy has deeply influenced the Western civilisation, shaping most of the modern world
Italy
–
The
Colosseum in Rome, built c. 70 – 80 AD, is considered one of the greatest works of
architecture and
engineering of ancient history.
Italy
–
Flag
Italy
–
The
Iron Crown of Lombardy, for centuries symbol of the
Kings of Italy.
Italy
–
Castel del Monte, built by German Emperor
Frederick II,
UNESCO World Heritage site
3.
Apulia
–
Apulia is a region of Italy in Southern Italy bordering the Adriatic Sea in the east, the Ionian Sea to the southeast, and the Strait of Òtranto and Gulf of Taranto in the south. Its southernmost portion, known as the Salento peninsula, forms a stiletto on the boot of Italy, the region comprises 19,345 square kilometers, and its population is about 4 million. It is bordered by the other Italian regions of Molise to the north, Campania to the west, across the Adriatic and Ionian Seas, it faces Albania, Bosnia-Herzegovina, Croatia, Greece, and Montenegro, The Apulia region extends as far north as Monte Gargano. Puglias coastline is longer than any other mainland Italian region, in the north, the Gargano promontory extends out into the Adriatic, while in the south, the flat and dry Salento peninsula forms the heel of Italys boot. It is home to the Alta Murgia and Gargano National Parks, see also, History of Apulia Apulia is one of the richest archaeological regions in Italy. It was first colonized by Mycenaean Greeks, a number of castles were built in the area by Holy Roman Emperor Frederick II, including Castel del Monte, sometimes called the Crown of Apulia. After 1282, when the island of Sicily was lost, Apulia was part of the Kingdom of Naples, as a result of the French–Spanish war of 1501–1504, Naples again came under the rule of Aragon and the Spanish Empire from 1504 to 1714. When Barbary pirates of North Africa sacked Vieste in 1554, they took an estimated 7,000 slaves, in 1861 the region became part of the Kingdom of Italy, with the new capital city at Turin. In the words of one historian, Turin was so far away that Otranto is today closer to seventeen foreign capitals than it is to Turin, the regions contribution to Italys gross value added was around 4. 6% in 2000, while its population was 7% of the total. The per capita GDP is low compared to the national average, in comparison with the country as a whole, the economy of Apulia is characterised by a greater emphasis on agriculture and services and a smaller part played by industry. In the last 20 years the base of the regions economy has changed radically. The majority of firms are financed by local capital. In certain of these sectors – especially textiles, clothing, footwear, vehicles, the region has a good network of roads but the railway network is somewhat inadequate, particularly in the south. Apulias 800 kilometers of coastline is studded with ports, which make this region an important terminal for transport and tourism to Greece, between 2007 and 2013 the economy of Apulia expanded more than that of the rest of southern Italy. Such growth, over decades, is a severe challenge to the hydrogeological system. Emigration from the depressed areas to northern Italy and the rest of Europe was very intense in the years between 1956 and 1971. Subsequently, the trend declined as economic conditions improved, to the point where there was net immigration in the years between 1982 and 1985, since 1986 the stagnation in employment has led to a new inversion of the trend, caused by a decrease in immigration. Since 1 June 2015, former judge and mayor of Bari Michele Emiliano of the Democratic Party has served as President, Apulia is divided into five administrative provinces and one metropolitan city, Cuisine plays an important role throughout Apulia
Apulia
–
Marina di Marittima,
Salento
Apulia
–
Apulia Puglia
Apulia
–
Castel del Monte, built by the
Holy Roman Emperor Frederick II between 1240 and 1250 in
Andria
Apulia
–
The medieval town
Ostuni
4.
Provinces of Italy
–
In Italy, a province is an administrative division of intermediate level between a municipality and a region. There are currently 107 provinces in Italy, a further 4 such cities were added later. The reorganization of the Italian provinces became operative by January 2015, a province of the Italian Republic is composed of many municipalities. Usually several provinces together form a region, the region of Aosta Valley is the sole exception – it is not subdivided into provinces, the three main functions devolved to provinces are, local planning and zoning, provision of local police and fire services, transportation regulation. The number of provinces in Italy has been growing in recent years. Usually, the name is the same as that of its capital city. According to the 2014 reform, each province is headed by a President assisted by a body, the Provincial Council, and an executive body. President and members of Council are elected together by mayors and city councilors of each municipality of the province, the Executive is chaired by the President who appoint others members, called assessori. Since 2015 the President and others members of the Council will not receive a salary, in each province there is also a Prefect, a representative of the central government who heads an agency called prefettura-ufficio territoriale del governo. The Questor is the head of States Police in the province, there is also a provinces police force depending from local government, called provincial police. Sardinia - following the outcome of the referendums of 2012 it was decreed that such institutions should be reformed or abolished by March 2013. In January 2014 the Sardinian Regional Administrative Court declared unconstitutional the abolition of the Sardinian provinces, sicily - provinces were replaced by Free Communal Consortia in 2013. In 1861, at the birth of the Kingdom of Italy, however, at that time the national territory was smaller than the current one, regions of Veneto, Friuli-Venezia Giulia, Trentino Alto Adige and Lazio were not included in the kingdom. In 1866, following the Third Independence War, territories of Veneto, Friuli, there were therefore nine more provinces, Belluno, Mantua, Padua, Rovigo, Treviso, Venice, Verona, Vicenza and Udine, all previously part of the Austrian Empire. Eventually, in 1870, following the annexion of Rome and its province from the Papal States, after the First World War, new territories were annexed to Italy. The Province of Trento was created in 1920, Provinces of La Spezia, Trieste and Ionio in 1923. In 1924 the new provinces of Fiume, Pola, and Zara were created, in 1927, following a Royal charter, a general province rearrangement took place. 17 new provinces were created and the province of Caserta was suppressed, in the same year the institution of circondari, sub-provincial wards created before the unification, was abolished
Provinces of Italy
–
Italian Republic
5.
Metropolitan cities of Italy
–
The metropolitan city is an administrative division of Italy, operative since 2015. In 2009, amendments added Reggio Calabria to the list, the metropolitan areas individuated by the autonomous regions were, Trieste in Friuli-Venezia Giulia, Cagliari in Sardinia, Catania, Messina and Palermo in Sicily. On 3 April 2014 the Italian Parliament approved a law that establishes 10 metropolitan cities in Italy, the new metropolitan cities have been operative since 1 January 2015. The metropolitan city is composed by the municipalities that before had been members of the same province, each metropolitan city is headed by a metropolitan mayor assisted by a legislative body, the Metropolitan council, and by a non-legislative assembly, the metropolitan conference. Members of the Metropolitan council are elected and chosen by mayors and city councilors of each municipality in the metropolitan city, the metropolitan conference is composed by the mayors of the municipalities closest to the capital. The main functions devolved to the new cities are, local planning and zoning, provision of local police services, transport. Regions of Italy Provinces of Italy Municipalities of Italy Media related to Metropolitan cities of Italy at Wikimedia Commons
Metropolitan cities of Italy
–
Metropolitan cities of Italy.
6.
Province of Brindisi
–
The Province of Brindisi is a province in the Apulia region of Italy. Its capital is the city of Brindisi and it has an area of 1,839 square kilometres and a total population of 401,652. The Province of Brindisi is situated in southeastern Italy, extending for 1,839 square kilometres and it was established in 1927 from the ancient Terra dOtranto. With the Adriatic Sea to the east, it is bordered to the north by the Province of Bari, the maximum height reached within the province is 414 metres above sea level, near Selva di Fasano. The other peaks are lower and are all located in the north-central area. The coastline in the province is 80.606 kilometres long, partly rocky, with many alternating stretches of beaches, small harbours. To the south it is flat and widely used for crops. In the north-central part, particularly Bari and Mola, the stems from the Late Cretaceous. There are no significant rivers, because of the karst terrain, as for waterways, the longest is the Canale Reale, which flows into the territory of Villa Castelli, bordering Francavilla Fontana, and flows into the Natural Reserve of Torre Guaceto. Along the coast, in addition, there are ponds and small freshwater lakes. In 1861, the province had a population of 114,790 which grew steadily until 2001 when there were 402,422 inhabitants. It has been more or less static since 2002 when there were 401,534 inhabitants, rising to 403,163 in 2010, in 2010, only 7,437 foreigners resided in the province. There are 20 comunes in the province, Surrounded by vineyards, artichoke and olive groves, in modern times, the province has experienced a process of change in its economic structure, with a progressive decrease in the weight of industry and growth of the tertiary sector. A significant increase in tourism, due to a good infrastructure has been witnessed, as well as the growth of its artistic, in 2011, the principal sectors of activity in the province were commerce, agriculture and construction, together representing 70% of the economy. The number of rose to a peak of 38,435 in 2005. Of these,8,453 were active in agriculture, mainly in production with small percentages in the areas of livestock, agricultural support. In addition to Brindisi, Oria, with its 13th century castle built by Frederick II, is one of the main attractions. Ostuni, still protected by its walls, is noted for its citadel, its cathedral
Province of Brindisi
–
Itria Valley
Province of Brindisi
–
Map highlighting the location of the province of Brindisi in Italy
7.
Demonym
–
A demonym is a word that identifies residents or natives of a particular place, which is derived from the name of that particular place. It is a neologism, previously gentilic was recorded in English dictionaries, e. g. the Oxford English Dictionary, thus a Thai may be any resident or citizen of Thailand, of any ethnic group, or more narrowly a member of the Thai people. Conversely, some groups of people may be associated with multiple demonyms, for example, a native of the United Kingdom may be called a British person, a Brit, or a Briton. In some languages, when a parallel demonym does not exist, in English, demonyms are capitalized and are often the same as the adjectival form of the place, e. g. Egyptian, Japanese, or Greek. Significant exceptions exist, for instance the adjectival form of Spain is Spanish, English widely includes country-level demonyms such as Ethiopian or Guatemalan and more local demonyms such as Seoulite, Wisconsinite, Chicagoan, Michigander, Fluminense, and Paulista. Some places lack a commonly used and accepted demonym and this poses a particular challenge to those toponymists who research demonyms. The word gentilic comes from the Latin gentilis and the English suffix -ic, the word demonym was derived from the Greek word meaning populace with the suffix for name. National Geographic attributes the term demonym to Merriam-Webster editor Paul Dickson in a recent work from 1990 and it was subsequently popularized in this sense in 1997 by Dickson in his book Labels for Locals. However, in What Do You Call a Person From, a Dictionary of Resident Names attributed the term to George H. Scheetz, in his Names Names, A Descriptive and Prescriptive Onymicon, which is apparently where the term first appears. Several linguistic elements are used to create demonyms in the English language, the most common is to add a suffix to the end of the location name, slightly modified in some instances. Cairo → Cairene Cyrenaica → Cyrene Damascus → Damascene Greece → Greek Nazareth → Nazarene Slovenia → Slovene Often used for Middle Eastern locations and European locations. Kingston-upon-Hull → Hullensian Leeds → Leodensian Spain → Spaniard Savoy → Savoyard -ese is usually considered proper only as an adjective, thus, a Chinese person is used rather than a Chinese. Monaco → Monégasque Menton → Mentonasque Basque Country → Basque Often used for French locations, mostly they are from Africa and the Pacific, and are not generally known or used outside the country concerned. In much of East Africa, a person of an ethnic group will be denoted by a prefix. For example, a person of the Luba people would be a Muluba, the plural form Baluba, similar patterns with minor variations in the prefixes exist throughout on a tribal level. And Fijians who are indigenous Fijians are known as Kaiviti and these demonyms are usually more informal and colloquial. In the United States such informal demonyms frequently become associated with mascots of the sports teams of the state university system. In other countries the origins are often disputed and these will typically be formed using the standard models above
Demonym
–
Merriam-Webster's Collegiate Dictionary has not adopted the term "demonyn" for these adjectives and nouns
8.
Daylight saving time
–
Daylight saving time is the practice of advancing clocks during summer months by one hour so that evening daylight lasts an hour longer, while sacrificing normal sunrise times. Typically, regions that use Daylight Savings Time adjust clocks forward one hour close to the start of spring, American inventor and politician Benjamin Franklin proposed a form of daylight time in 1784. New Zealander George Hudson proposed the idea of saving in 1895. The German Empire and Austria-Hungary organized the first nationwide implementation, starting on April 30,1916, many countries have used it at various times since then, particularly since the energy crisis of the 1970s. The practice has both advocates and critics, DST clock shifts sometimes complicate timekeeping and can disrupt travel, billing, record keeping, medical devices, heavy equipment, and sleep patterns. Computer software often adjusts clocks automatically, but policy changes by various jurisdictions of DST dates, industrialized societies generally follow a clock-based schedule for daily activities that do not change throughout the course of the year. The time of day that individuals begin and end work or school, North and south of the tropics daylight lasts longer in summer and shorter in winter, with the effect becoming greater as one moves away from the tropics. However, they will have one hour of daylight at the start of each day. Supporters have also argued that DST decreases energy consumption by reducing the need for lighting and heating, DST is also of little use for locations near the equator, because these regions see only a small variation in daylight in the course of the year. After ancient times, equal-length civil hours eventually supplanted unequal, so civil time no longer varies by season, unequal hours are still used in a few traditional settings, such as some monasteries of Mount Athos and all Jewish ceremonies. This 1784 satire proposed taxing window shutters, rationing candles, and waking the public by ringing church bells, despite common misconception, Franklin did not actually propose DST, 18th-century Europe did not even keep precise schedules. However, this changed as rail transport and communication networks came to require a standardization of time unknown in Franklins day. Modern DST was first proposed by the New Zealand entomologist George Hudson, whose shift work job gave him time to collect insects. An avid golfer, he also disliked cutting short his round at dusk and his solution was to advance the clock during the summer months, a proposal he published two years later. The proposal was taken up by the Liberal Member of Parliament Robert Pearce, a select committee was set up to examine the issue, but Pearces bill did not become law, and several other bills failed in the following years. Willett lobbied for the proposal in the UK until his death in 1915, william Sword Frost, mayor of Orillia, Ontario, introduced daylight saving time in the municipality during his tenure from 1911 to 1912. Starting on April 30,1916, the German Empire and its World War I ally Austria-Hungary were the first to use DST as a way to conserve coal during wartime, Britain, most of its allies, and many European neutrals soon followed suit. Russia and a few other countries waited until the year
Daylight saving time
–
Ancient
water clock that lets hour lengths vary with season.
Daylight saving time
–
G. V. Hudson invented modern DST, proposing it first in 1895.
Daylight saving time
–
Retailers generally favor DST.
United Cigar Stores hailed a 1918 DST bill.
Daylight saving time
–
William Willett independently proposed DST in 1907 and advocated it tirelessly.
9.
Central European Summer Time
–
It corresponds to UTC + two hours. Other names which have been applied to Central European Summer Time are Middle European Summer Time, Central European Daylight Saving Time, and Bravo Time. Since 1996 European Summer Time has been observed between 1,00 UTC on the last Sunday of March and 1,00 on the last Sunday of October, the following countries and territories use Central European Summer Time. In addition, Libya used CEST during the years 1951–1959, 1982–1989, 1996–1997, European Summer Time Other countries and territories in UTC+2 time zone Other names of UTC+2 time zone
Central European Summer Time
–
light blue
10.
Theodore of Amasea
–
For another Saint Theodore, see, Theodore Stratelates or Saint Theodore. Saint Theodore of Amasea is one of the two saints called Theodore, who are venerated as Warrior Saints and Great Martyrs in the Eastern Orthodox Church and he is also known as Theodore Tyron. The other saint of the name is Theodore Stratelates, also known as Theodore of Heraclea. When the epithet is omitted, the reference is usually to St Theodore of Amasea, Tiro is a word from classical Latin meaning a recently enlisted soldier or recruit. The Latin word was transliterated into Greek with various spellings, nothing reliable is known about St Theodore except that he was martyred in the early 4th century. The stories told about his life and martyrdom are all matters of myth, however, he again protested paganism by setting fire to the temple of Cybele at Amasea. He was then condemned to death and, after tortures, was executed by being thrown into a furnace and his remains were said to have been obtained by a woman from Eusebia and interred at Euchaita, where he had been born. This was a Byzantine city which no longer exists but is thought to correspond to the modern Avkhat, a shrine was erected there, which became an important place of pilgrimage. Gregory of Nyssa preached in honour of St Theodore in his sanctuary in the late 4th century, and this became a particularly important attribute of St Theodore. He was adopted by crusaders as their patron, the sanctuary of the saint was established at Euchaita, possibly his birthplace, and legends of his life and martyrdom have been developed by hagiographers over the years. Later additions to the story, between the 8th and 10th centuries, told of a dragon who was terrorising the district round Amasea, Amasea was by then in a district liable to attacks by marauding barbarians, against whom the saint was said to have interceded. His sanctuary continued to be visited until around 1100, although the district was by then occupied by the Arabs, in Western Christianity, he is usually called Theodore of Amasea from the ancient city in Pontus where he suffered martyrdom. Sometimes he is called Theodore Euchaita, from the place where he was born and to which his body had been carried. In Eastern Christianity, he is often known as Theodore Teron. There is much confusion between him and St Theodore Stratelates of Heraclea, who is sometimes said to have had a shrine at Euchaita. His lives are listed in Bibliotecha Hagiographica Graeca 1760-1773, St Theodore became especially important in the Eastern Orthodox Church, where his cult spread widely. The first church dedicated to him in Constantinople was built in 452 and he was famous in Syria, Palestine and Asia Minor. Many churches of the Eastern Orthodox Church are dedicated to him, the oldest Georgian Bir el Qutt inscriptions mention him twice
Theodore of Amasea
–
Saint Theodore of Amasea
Theodore of Amasea
–
Tomb in
San Salvador, Venice
Theodore of Amasea
–
Russian icon of the Miracle of St. Theodore (17th century),
egg tempera by Nikifor Saviny,
Stroganov School (
State Russian Museum,
Saint Petersburg)
Theodore of Amasea
–
Theodore of Amasea (on the left) and
Theodore Stratelates (on the right) - a
fresco from
Rila Monastery, Bulgaria (19th century?)
11.
St. Lawrence of Brindisi
–
Born Giulio Cesare Russo, was a Roman Catholic priest and a theologian as well as a member of the Order of Friars Minor Capuchin. He was beatified on 1 June 1783 and was canonized as a saint on 8 December 1881 and he was named a Doctor of the Church in 1959. Giulio Cesare Russo was born in Brindisi, Kingdom of Naples and he was educated at Saint Marks College in Venice, and joined the Capuchins in Verona as Brother Lawrence. He received further instruction from the University of Padua, an accomplished linguist, Lawrence spoke most European and Semitic languages fluently. He was appointed definitor general to Rome for the Capuchins in 1596, beginning in 1599, Lawrence established Capuchin monasteries in modern Germany and Austria, furthering the Counter-Reformation and bringing many Protestants back to the Catholic faith. In 1601, he served as the chaplain for the army of Rudolph II, Holy Roman Emperor. He then led the army during the liberation of Székesfehérvár in Hungary from the Ottoman Empire. In 1602, he was elected general of the Capuchin friars. He was elected again in 1605, but refused the office and he entered the service of the Holy See, becoming papal nuncio to Bavaria. After serving as nuncio to Spain, he retired to a monastery in 1618 and he was recalled as a special envoy to the King of Spain regarding the actions of the Viceroy of Naples in 1619, and after finishing his mission, died on his birthday in Lisbon. He was entombed at the Poor Clares Convento de la Anunciada in Villafranca del Bierzo and he was beatified in 1783 by Pope Pius VI, canonized in 1881 by Pope Leo XIII, and declared a Doctor of the Church by Pope John XXIII in 1959. His feast day is July 21, St. Lawrence of Brindisi Complete Works were published in 15 volumes, in a critical edition, between 1926 and 1956. Francis of Assisi Poor Clares St. Lawrence Seminary High School St. Lorenzo Da Brindisi Saint Lorenzo of Brindisi Saint Lawrence of Brindisi A Homily by Lawrence of Brindisi
St. Lawrence of Brindisi
–
Saint Lawrence of Brindisi, O.F.M. Cap.
St. Lawrence of Brindisi
–
Virgin Mary
12.
Latin language
–
Latin is a classical language belonging to the Italic branch of the Indo-European languages. The Latin alphabet is derived from the Etruscan and Greek alphabets, Latin was originally spoken in Latium, in the Italian Peninsula. Through the power of the Roman Republic, it became the dominant language, Vulgar Latin developed into the Romance languages, such as Italian, Portuguese, Spanish, French, and Romanian. Latin, Italian and French have contributed many words to the English language, Latin and Ancient Greek roots are used in theology, biology, and medicine. By the late Roman Republic, Old Latin had been standardised into Classical Latin, Vulgar Latin was the colloquial form spoken during the same time and attested in inscriptions and the works of comic playwrights like Plautus and Terence. Late Latin is the language from the 3rd century. Later, Early Modern Latin and Modern Latin evolved, Latin was used as the language of international communication, scholarship, and science until well into the 18th century, when it began to be supplanted by vernaculars. Ecclesiastical Latin remains the language of the Holy See and the Roman Rite of the Catholic Church. Today, many students, scholars and members of the Catholic clergy speak Latin fluently and it is taught in primary, secondary and postsecondary educational institutions around the world. The language has been passed down through various forms, some inscriptions have been published in an internationally agreed, monumental, multivolume series, the Corpus Inscriptionum Latinarum. Authors and publishers vary, but the format is about the same, volumes detailing inscriptions with a critical apparatus stating the provenance, the reading and interpretation of these inscriptions is the subject matter of the field of epigraphy. The works of several hundred ancient authors who wrote in Latin have survived in whole or in part and they are in part the subject matter of the field of classics. The Cat in the Hat, and a book of fairy tales, additional resources include phrasebooks and resources for rendering everyday phrases and concepts into Latin, such as Meissners Latin Phrasebook. The Latin influence in English has been significant at all stages of its insular development. From the 16th to the 18th centuries, English writers cobbled together huge numbers of new words from Latin and Greek words, dubbed inkhorn terms, as if they had spilled from a pot of ink. Many of these words were used once by the author and then forgotten, many of the most common polysyllabic English words are of Latin origin through the medium of Old French. Romance words make respectively 59%, 20% and 14% of English, German and those figures can rise dramatically when only non-compound and non-derived words are included. Accordingly, Romance words make roughly 35% of the vocabulary of Dutch, Roman engineering had the same effect on scientific terminology as a whole
Latin language
–
Latin inscription, in the
Colosseum
Latin language
–
Julius Caesar 's
Commentarii de Bello Gallico is one of the most famous classical Latin texts of the Golden Age of Latin. The unvarnished, journalistic style of this
patrician general has long been taught as a model of the urbane Latin officially spoken and written in the floruit of the
Roman republic.
Latin language
–
A multi-volume Latin dictionary in the
University Library of Graz
Latin language
–
Latin and Ancient Greek Language - Culture - Linguistics at
Duke University in 2014.
13.
Adriatic Sea
–
The Adriatic Sea /ˌeɪdriˈætᵻk/ is a body of water separating the Italian Peninsula from the Balkan peninsula and the Apennine Mountains from the Dinaric Alps and adjacent ranges. The Adriatic is the northernmost arm of the Mediterranean Sea, extending from the Strait of Otranto to the northwest, the countries with coasts on the Adriatic are Albania, Bosnia and Herzegovina, Croatia, Greece, Italy, Montenegro and Slovenia. The Adriatic contains over 1,300 islands, mostly located along its eastern, Croatian and it is divided into three basins, the northern being the shallowest and the southern being the deepest, with a maximum depth of 1,233 metres. The Otranto Sill, a ridge, is located at the border between the Adriatic and Ionian Seas. The prevailing currents flow counterclockwise from the Strait of Otranto, along the eastern coast, tidal movements in the Adriatic are slight, although larger amplitudes are known to occur occasionally. The Adriatics salinity is lower than the Mediterraneans because the Adriatic collects a third of the water flowing into the Mediterranean. The surface water temperatures range from 30 °C in summer to 12 °C in winter. The Adriatic Sea sits on the Apulian or Adriatic Microplate, which separated from the African Plate in the Mesozoic era, the plates movement contributed to the formation of the surrounding mountain chains and Apennine tectonic uplift after its collision with the Eurasian plate. In the Late Oligocene, the Apennine Peninsula first formed, separating the Adriatic Basin from the rest of the Mediterranean, all types of sediment are found in the Adriatic, with the bulk of the material transported by the Po and other rivers on the western coast. The western coast is alluvial or terraced, while the eastern coast is indented with pronounced karstification. There are dozens of protected areas in the Adriatic, designed to protect the seas karst habitats. The sea is abundant in flora and fauna—more than 7,000 species are identified as native to the Adriatic, many of them endemic, rare and threatened ones. The Adriatics shores are populated by more than 3.5 million people, the earliest settlements on the Adriatic shores were Etruscan, Illyrian, and Greek. By the 2nd century BC, the shores were under Romes control, following Italian unification, the Kingdom of Italy started an eastward expansion that lasted until the 20th century. Following World War I and the collapse of Austria-Hungary and the Ottoman Empire, the former disintegrated during the 1990s, resulting in four new states on the Adriatic coast. Italy and Albania agreed on their maritime boundary in 1992, Fisheries and tourism are significant sources of income all along the Adriatic coast. Adriatic Croatias tourism industry has grown faster economically than the rest of the Adriatic Basins, maritime transport is also a significant branch of the areas economy—there are 19 seaports in the Adriatic that each handle more than a million tonnes of cargo per year. The largest Adriatic seaport by annual cargo turnover is the Port of Trieste, in the southeast, the Adriatic Sea connects to the Ionian Sea at the 72-kilometre wide Strait of Otranto
Adriatic Sea
–
Bay of Kotor, a
ria in the Southern Adriatic
Adriatic Sea
–
Map of the Adriatic Sea
Adriatic Sea
–
Adriatic islands off
Croatia 's coast
Adriatic Sea
–
A
submarine spring near
Omiš, observed through sea surface rippling
14.
Italian Peninsula
–
The Italian Peninsula or Apennine Peninsula is the central and the smallest of the three large peninsulas of Southern Europe. It extends 1,000 km from the Po Valley in the north to the central Mediterranean Sea in the south, the peninsulas shape gives it the nickname lo Stivale. Three smaller peninsulas contribute to this shape, namely Calabria, Salento. Geographically, the Italian peninsula consists of the south of a line extending from the Magra to the Rubicon rivers. It excludes the Po Valley and the slopes of the Alps. All of the lies within the territory of the Italian Republic except for the microstates of San Marino. Additionally, Sicily, Elba and other islands, such as Palagruža, are usually considered as islands off the peninsula. The peninsula lies between the Tyrrhenian Sea on the west, the Ionian Sea on the south, and the Adriatic Sea on the east, the backbone of the Italian peninsula consists of the Apennine Mountains, from which it takes one of its names. Most of its coast is lined with cliffs, the Italian Peninsulas location between the centre of Europe and the Mediterranean Sea made it the target of many conquests. The peninsula has mainly a Mediterranean climate, though in the parts the climate is much cooler. Its natural vegetation includes macchia along the coasts and deciduous and mixed coniferous forests in the interior. Political divisions of the peninsula sorted by area, Apennine Mountains Roman Republic Roman Italy Insular Italy Media related to Italian Peninsula at Wikimedia Commons
Italian Peninsula
–
Satellite view of the peninsula in March 2003.
15.
Greece
–
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
Greece
–
Fresco displaying the Minoan ritual of "bull leaping", found in
Knossos,
Crete.
Greece
–
Flag
Greece
–
The
Lion Gate,
Mycenae
Greece
–
The
Parthenon on the
Acropolis of Athens is one of the best known symbols of
classical Greece.
16.
Middle East
–
The Middle East is a transcontinental region centered on Western Asia and Egypt. The corresponding adjective is Middle-Eastern and the noun is Middle-Easterner. The term has come into usage as a replacement of the term Near East beginning in the early 20th century. Arabs, Turks, Persians, Kurds, and Azeris constitute the largest ethnic groups in the region by population. Indigenous minorities of the Middle East include Jews, Assyrians and other Arameans, Baloch, Berbers, Copts, Druze, Lurs, Mandaeans, Samaritans, Shabaks, Tats, in the Middle East, there is also a Romani community. European ethnic groups form a diaspora in the region include Albanians, Bosniaks, Circassians, Crimean Tatars, Franco-Levantines. Among other migrant populations are Bengalis as well as other Indians, Chinese, Filipinos, Indonesians, Pakistanis, the history of the Middle East dates back to ancient times, with the importance of the region being recognized for millennia. Most of the countries border the Persian Gulf have vast reserves of crude oil. The term Middle East may have originated in the 1850s in the British India Office, however, it became more widely known when American naval strategist Alfred Thayer Mahan used the term in 1902 to designate the area between Arabia and India. During this time the British and Russian Empires were vying for influence in Central Asia, Mahan realized not only the strategic importance of the region, but also of its center, the Persian Gulf. Mahan first used the term in his article The Persian Gulf and International Relations, published in September 1902 in the National Review, a British journal. The Middle East, if I may adopt a term which I have not seen, will some day need its Malta, as well as its Gibraltar, it does not follow that either will be in the Persian Gulf. The British Navy should have the facility to concentrate in force if occasion arise, about Aden, India, mahans article was reprinted in The Times and followed in October by a 20-article series entitled The Middle Eastern Question, written by Sir Ignatius Valentine Chirol. During this series, Sir Ignatius expanded the definition of Middle East to include regions of Asia which extend to the borders of India or command the approaches to India. After the series ended in 1903, The Times removed quotation marks from subsequent uses of the term, in the late 1930s, the British established the Middle East Command, which was based in Cairo, for its military forces in the region. After that time, the term Middle East gained broader usage in Europe, the description Middle has also led to some confusion over changing definitions. Before the First World War, Near East was used in English to refer to the Balkans and the Ottoman Empire, while Middle East referred to Iran, the Caucasus, Afghanistan, Central Asia, and Turkestan. The first official use of the term Middle East by the United States government was in the 1957 Eisenhower Doctrine, the Associated Press Stylebook says that Near East formerly referred to the farther west countries while Middle East referred to the eastern ones, but that now they are synonymous
Middle East
–
The
Temple Mount in
Jerusalem
Middle East
–
Map of the Middle East (green).
Middle East
–
The
Kaaba, located in
Mecca,
Saudi Arabia
Middle East
–
Islam is the largest religion in the Middle East. Here, Muslim men are
prostrating during prayer in a mosque.
17.
United Nations
–
The United Nations is an intergovernmental organization to promote international co-operation. A replacement for the ineffective League of Nations, the organization was established on 24 October 1945 after World War II in order to prevent another such conflict, at its founding, the UN had 51 member states, there are now 193. The headquarters of the UN is in Manhattan, New York City, further main offices are situated in Geneva, Nairobi, and Vienna. The organization is financed by assessed and voluntary contributions from its member states, the UNs mission to preserve world peace was complicated in its early decades by the Cold War between the US and Soviet Union and their respective allies. The organization participated in actions in Korea and the Congo. After the end of the Cold War, the UN took on major military, the UN has six principal organs, the General Assembly, the Security Council, the Economic and Social Council, the Secretariat, the International Court of Justice, and the UN Trusteeship Council. UN System agencies include the World Bank Group, the World Health Organization, the World Food Programme, UNESCO, the UNs most prominent officer is the Secretary-General, an office held by Portuguese António Guterres since 2017. Non-governmental organizations may be granted consultative status with ECOSOC and other agencies to participate in the UNs work, the organization won the Nobel Peace Prize in 2001, and a number of its officers and agencies have also been awarded the prize. Other evaluations of the UNs effectiveness have been mixed, some commentators believe the organization to be an important force for peace and human development, while others have called the organization ineffective, corrupt, or biased. Following the catastrophic loss of life in the First World War, the earliest concrete plan for a new world organization began under the aegis of the US State Department in 1939. It incorporated Soviet suggestions, but left no role for France, four Policemen was coined to refer to four major Allied countries, United States, United Kingdom, Soviet Union, and China, which emerged in the Declaration by United Nations. Roosevelt first coined the term United Nations to describe the Allied countries, the term United Nations was first officially used when 26 governments signed this Declaration. One major change from the Atlantic Charter was the addition of a provision for religious freedom, by 1 March 1945,21 additional states had signed. Each Government pledges itself to cooperate with the Governments signatory hereto, the foregoing declaration may be adhered to by other nations which are, or which may be, rendering material assistance and contributions in the struggle for victory over Hitlerism. During the war, the United Nations became the term for the Allies. To join, countries had to sign the Declaration and declare war on the Axis, at the later meetings, Lord Halifax deputized for Mr. Eden, Wellington Koo for T. V. Soong, and Mr Gromyko for Mr. Molotov. The first meetings of the General Assembly, with 51 nations represented, the General Assembly selected New York City as the site for the headquarters of the UN, and the facility was completed in 1952. Its site—like UN headquarters buildings in Geneva, Vienna, and Nairobi—is designated as international territory, the Norwegian Foreign Minister, Trygve Lie, was elected as the first UN Secretary-General
United Nations
–
1943 sketch by Franklin Roosevelt of the United Nations' original three branches: The
Four Policemen, an executive branch, and an international assembly of forty UN member states.
United Nations
–
Flag
United Nations
–
The
Chilean delegation signing the
UN Charter in San Francisco, 1945
United Nations
–
Dag Hammarskjöld was a particularly active Secretary-General from 1953 until his death in 1961.
18.
Bosnia
–
Bosnia and Herzegovina, sometimes called Bosnia-Herzegovina, and, in short, often known informally as Bosnia, is a country in Southeastern Europe located on the Balkan Peninsula. Sarajevo is the capital and largest city, in the central and eastern interior of the country the geography is mountainous, in the northwest it is moderately hilly, and the northeast is predominantly flatland. The inland is a larger region and has a moderate continental climate, with hot summers and cold. The southern tip of the country has a Mediterranean climate and plain topography, Bosnia and Herzegovina is a region that traces permanent human settlement back to the Neolithic age, during and after which it was populated by several Illyrian and Celtic civilizations. Culturally, politically, and socially, the country has a rich history, the Ottomans brought Islam to the region, and altered much of the cultural and social outlook of the country. This was followed by annexation into the Austro-Hungarian Monarchy, which lasted up until World War I. In the interwar period, Bosnia was part of the Kingdom of Yugoslavia and after World War II, following the dissolution of Yugoslavia, the country proclaimed independence in 1992, which was followed by the Bosnian War, lasting until late 1995. The country is home to three ethnic groups or, officially, constituent peoples, as specified in the constitution. Bosniaks are the largest group of the three, with Serbs second and Croats third, a native of Bosnia and Herzegovina, regardless of ethnicity, is identified in English as a Bosnian. The terms Herzegovinian and Bosnian are maintained as a rather than ethnic distinction. Moreover, the country was simply called Bosnia until the Austro-Hungarian occupation at the end of the 19th century, Bosnia and Herzegovina has a bicameral legislature and a three-member Presidency composed of a member of each major ethnic group. The Federation of Bosnia and Herzegovina is itself complex and consists of 10 cantons, additionally, the country has been a member of the Council of Europe since April 2002 and a founding member of the Mediterranean Union upon its establishment in July 2008. The name is believed to have derived from the hydronym of the river Bosna coursing through the Bosnian heartland. According to philologist Anton Mayer the name Bosna could be derived from Illyrian Bass-an-as which would be a diversion of the Proto-Indo-European root bos or bogh, meaning the running water. According to English medievalist William Miller the Slavic settlers in Bosnia adapted the Latin designation Basante, to their own idiom by calling the stream Bosna, the name Herzegovina originates from Bosnian magnate Stephen Vukčić Kosačas title, Herceg of Hum and the Coast. Hum, formerly Zahumlje, was a medieval principality that was conquered by the Bosnian Banate in the first half of the 14th century. Bosnia is located in the western Balkans, bordering Croatia to the north and west, Serbia to the east and it has a coastline about 20 kilometres long surrounding the city of Neum. It lies between latitudes 42° and 46° N, and longitudes 15° and 20° E, the countrys name comes from the two regions Bosnia and Herzegovina, which have a very vaguely defined border between them
Bosnia
–
Mogorjelo, ancient Roman suburban Villa Rustica from the 4th century, near
Čapljina
Bosnia
–
Flag
Bosnia
–
Gazi Husrev-beg Mosque in
Sarajevo dating from 1531
Bosnia
–
Bosniak resistance against the
Austro-Hungarian military intervention in 1878
19.
World Wide Fund for Nature
–
It was formerly named the World Wildlife Fund, which remains its official name in Canada and the United States. It is the worlds largest conservation organization with five million supporters worldwide, working in more than 100 countries, supporting around 1,300 conservation. WWF is a foundation, with 55% of funding from individuals and bequests, 19% from government sources, the groups mission is to stop the degradation of the planet’s natural environment and to build a future in which humans live in harmony with nature. Currently, much of its work concentrates on the conservation of three biomes that contain most of the biodiversity, oceans and coasts, forests. Among other issues, it is concerned with endangered species, sustainable production of commodities. The Conservation Foundation, a precursor to WWF, was founded in 1947 by Fairfield Osborn in New York City in support of capitalism-friendly ecological practices. The advisory council included leading scientists such as Charles Sutherland Elton, G Evelyn Hutchinson, Aldo Leopold, Carl Sauer, and Paul Sears. It supported much of the work cited by Rachel Carsons Silent Spring, including that of John L. George, Roger Hale, Robert Rudd. In 1990, the Conservation Foundation was merged into WWF, after becoming an affiliate of WWF in 1985, the organization now known as the Conservation Foundation in the United States is the former Forest Foundation of DuPage County. The idea for a fund on behalf of endangered animals was initially proposed by Victor Stolan to Sir Julian Huxley in response to articles he published in the British newspaper The Observer, nicholson thought up the name of the organization. WWF was conceived on 29 April 1961, under the name of World Wildlife Fund, godfrey A. Rockefeller also played an important role in its creation, assembling the first staff. For sending experts to danger spots and training, making it all possible that their needs are met before it is too late. WWF has set up offices and operations around the world, the organization also began to run its own conservation projects and campaigns, and by the 1980s started to take a more strategic approach to its conservation activities. In 1986, the changed its name to World Wide Fund for Nature. However, it continued at that time to operate under the name in the United States. We shant save all we should like to, but we shall save a great deal more than if we had never tried, – Sir Peter Scott In 1996, the organization obtained general consultative status from UNESCO. WWFs giant panda logo originated from a panda named Chi Chi that had transferred from Beijing Zoo to London Zoo in 1958. The logo was founded by Young in 1966, the organization also needed an animal that would have an impact in black and white printing
World Wide Fund for Nature
–
Earth Hour 2013 at the
Verona Arena amphitheatre,
Piazza Bra,
Verona, Italy before (top) and while the street lighting was switched off.
World Wide Fund for Nature
–
World Wide Fund for Nature
World Wide Fund for Nature
–
The WWF hot air balloon in Brazil
World Wide Fund for Nature
–
The giant panda has become the symbol of WWF.
20.
Ionian Sea
–
The Ionian Sea is an elongated embayment of the Mediterranean Sea, south of the Adriatic Sea. It is bounded by southern Italy including Calabria, Sicily, and the Salento peninsula to the west, southern Albania to the north, all major islands in the sea belong to Greece. They are collectively referred to as the Ionian Islands, the ones being Corfu, Zakynthos, Kephalonia, Ithaca. There are ferry routes between Patras and Igoumenitsa, Greece, and Brindisi and Ancona, Italy, that cross the east and north of the Ionian Sea, and from Piraeus westward. Calypso Deep, the deepest point in the Mediterranean at −5,267 m, is located in the Ionian Sea, the sea is one of the most seismically active areas in the world. The name Ionian comes from the Greek language Ἰόνιον, Ancient Greek writers, especially Aeschylus, linked it to the myth of Io. In Ancient Greek the adjective Ionios was used as an epithet for the sea because Io swam across it, according to the Oxford Classical Dictionary, the name may derive from Ionians who sailed to the West. There were also narratives about other eponymic legendary figures, according to one version, Ionius was a son of Adrias, according to another, Ionius was a son of Dyrrhachus. When Dyrrhachus was attacked by his own brothers, Heracles, who was passing through the area, came to his aid, the corpse was cast into the sea, which thereafter was called the Ionian Sea. The International Hydrographic Organization defines the limits of the Ionian Sea as follows, On the North. A line running from the mouth of the Butrinto River in Albania, to Cape Karagol in Corfu, along the North Coast of Corfu to Cape Kephali, from the mouth of the Butrinto River in Albania down the coast of the mainland to Cape Matapan. A line from Cape Matapan to Cape Passero, the Southern point of Sicily, the East coast of Sicily and the Southeast coast of Italy to Cape Santa Maria di Leuca
Ionian Sea
–
The Ionian Sea, view from the island
Kefalonia,
Greece
Ionian Sea
–
Map of the Ionian Sea
Ionian Sea
–
The Ionian Sea, as seen from
Corfu Island,
Greece, and with
Saranda, Albania in the background
Ionian Sea
–
Gjipe Canyon terminating at the Ionian sea,
Albania
21.
Limestone
–
Limestone is a sedimentary rock, composed mainly of skeletal fragments of marine organisms such as coral, forams and molluscs. Its major materials are the minerals calcite and aragonite, which are different crystal forms of calcium carbonate, about 10% of sedimentary rocks are limestones. The solubility of limestone in water and weak acid solutions leads to karst landscapes, most cave systems are through limestone bedrock. The first geologist to distinguish limestone from dolomite was Belsazar Hacquet in 1778, like most other sedimentary rocks, most limestone is composed of grains. Most grains in limestone are skeletal fragments of organisms such as coral or foraminifera. Other carbonate grains comprising limestones are ooids, peloids, intraclasts and these organisms secrete shells made of aragonite or calcite, and leave these shells behind when they die. Limestone often contains variable amounts of silica in the form of chert or siliceous skeletal fragment, some limestones do not consist of grains at all, and are formed completely by the chemical precipitation of calcite or aragonite, i. e. travertine. Secondary calcite may be deposited by supersaturated meteoric waters and this produces speleothems, such as stalagmites and stalactites. Another form taken by calcite is oolitic limestone, which can be recognized by its granular appearance, the primary source of the calcite in limestone is most commonly marine organisms. Some of these organisms can construct mounds of rock known as reefs, below about 3,000 meters, water pressure and temperature conditions cause the dissolution of calcite to increase nonlinearly, so limestone typically does not form in deeper waters. Limestones may also form in lacustrine and evaporite depositional environments, calcite can be dissolved or precipitated by groundwater, depending on several factors, including the water temperature, pH, and dissolved ion concentrations. Calcite exhibits a characteristic called retrograde solubility, in which it becomes less soluble in water as the temperature increases. Impurities will cause limestones to exhibit different colors, especially with weathered surfaces, Limestone may be crystalline, clastic, granular, or massive, depending on the method of formation. Crystals of calcite, quartz, dolomite or barite may line small cavities in the rock, when conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together, or it can fill fractures. Travertine is a banded, compact variety of limestone formed along streams, particularly there are waterfalls. Calcium carbonate is deposited where evaporation of the leaves a solution supersaturated with the chemical constituents of calcite. Tufa, a porous or cellular variety of travertine, is found near waterfalls, coquina is a poorly consolidated limestone composed of pieces of coral or shells. During regional metamorphism that occurs during the building process, limestone recrystallizes into marble
Limestone
–
Limestone outcrop in the
Torcal de Antequera nature reserve of
Málaga, Spain
Limestone
–
Limestone quarry at
Cedar Creek, Virginia, USA
Limestone
–
Cutting the limestone blocks at a quarry in
Gozo,
Malta
Limestone
–
Limestone as building material
22.
Clay
–
Clay is a fine-grained natural rock or soil material that combines one or more clay minerals with traces of metal oxides and organic matter. Geologic clay deposits are composed of phyllosilicate minerals containing variable amounts of water trapped in the mineral structure. Clays are plastic due to water content and become hard, brittle. Depending on the content in which it is found, clay can appear in various colours from white to dull grey or brown to deep orange-red. Although many naturally occurring deposits include both silts and clay, clays are distinguished from other fine-grained soils by differences in size, silts, which are fine-grained soils that do not include clay minerals, tend to have larger particle sizes than clays. There is, however, some overlap in size and other physical properties. The distinction between silt and clay varies by discipline, geologists and soil scientists usually consider the separation to occur at a particle size of 2 µm, sedimentologists often use 4–5 μm, and colloid chemists use 1 μm. Geotechnical engineers distinguish between silts and clays based on the plasticity properties of the soil, as measured by the soils Atterberg limits, ISO14688 grades clay particles as being smaller than 2 μm and silt particles as being larger. These solvents, usually acidic, migrate through the rock after leaching through upper weathered layers. In addition to the process, some clay minerals are formed through hydrothermal activity. There are two types of deposits, primary and secondary. Primary clays form as residual deposits in soil and remain at the site of formation, secondary clays are clays that have been transported from their original location by water erosion and deposited in a new sedimentary deposit. Clay deposits are associated with very low energy depositional environments such as large lakes. Depending on the source, there are three or four main groups of clays, kaolinite, montmorillonite-smectite, illite, and chlorite. Chlorites are not always considered to be a clay, sometimes being classified as a group within the phyllosilicates. There are approximately 30 different types of clays in these categories. Varve is clay with visible annual layers, which are formed by deposition of those layers and are marked by differences in erosion. This type of deposit is common in glacial lakes
Clay
–
Gay Head cliffs in
Martha's Vineyard consist almost entirely of clay.
Clay
–
Electron microscope photograph of smectite clay – magnification 23,500
Clay
–
Quaternary clay in
Estonia
Clay
–
Deforestation for clay extraction in
Rio de Janeiro,
Brazil. The picture is of Morro da Covanca, Jacarepaguá.
23.
Pleistocene
–
The Pleistocene is the geological epoch which lasted from about 2,588,000 to 11,700 years ago, spanning the worlds most recent period of repeated glaciations. The end of the Pleistocene corresponds with the end of the last glacial period, the Pleistocene is the first epoch of the Quaternary Period or sixth epoch of the Cenozoic Era. In the ICS timescale, the Pleistocene is divided into four stages or ages, all of these stages were defined in southern Europe. In addition to this subdivision, various regional subdivisions are often used. Charles Lyell introduced the term pleistocene in 1839 to describe strata in Sicily that had at least 70% of their molluscan fauna still living today and this distinguished it from the older Pliocene Epoch, which Lyell had originally thought to be the youngest fossil rock layer. The Pleistocene has been dated from 2.588 million to 11,700 years before present and it covers most of the latest period of repeated glaciation, up to and including the Younger Dryas cold spell. The end of the Younger Dryas has been dated to about 9640 BC, the IUGS has yet to approve a type section, Global Boundary Stratotype Section and Point, for the upper Pleistocene/Holocene boundary. The proposed section is the North Greenland Ice Core Project ice core 75°06 N 42°18 W, the lower boundary of the Pleistocene Series is formally defined magnetostratigraphically as the base of the Matuyama chronozone, isotopic stage 103. Above this point there are notable extinctions of the calcareous nanofossils, Discoaster pentaradiatus, the Pleistocene covers the recent period of repeated glaciations. The name Plio-Pleistocene has, in the past, been used to mean the last ice age. The revised definition of the Quaternary, by pushing back the date of the Pleistocene to 2.58 Ma. Pleistocene climate was marked by repeated glacial cycles in which continental glaciers pushed to the 40th parallel in some places and it is estimated that, at maximum glacial extent, 30% of the Earths surface was covered by ice. In addition, a zone of permafrost stretched southward from the edge of the sheet, a few hundred kilometres in North America. The mean annual temperature at the edge of the ice was −6 °C, during interglacial times, such as at present, drowned coastlines were common, mitigated by isostatic or other emergent motion of some regions. The effects of glaciation were global, antarctica was ice-bound throughout the Pleistocene as well as the preceding Pliocene. The Andes were covered in the south by the Patagonian ice cap, there were glaciers in New Zealand and Tasmania. The current decaying glaciers of Mount Kenya, Mount Kilimanjaro, glaciers existed in the mountains of Ethiopia and to the west in the Atlas mountains. In the northern hemisphere, many glaciers fused into one, the Cordilleran ice sheet covered the North American northwest, the east was covered by the Laurentide
Pleistocene
–
The maximum extent of
glacial ice in the north polar area during the Pleistocene period.
Pleistocene
–
Ice ages as reflected in atmospheric CO 2, stored in bubbles from glacial ice of
Antarctica.
Pleistocene
–
Pleistocene of
Northern Spain showing
woolly mammoth,
cave lions eating a
reindeer,
tarpans, and
woolly rhinoceros.
Pleistocene
–
Pleistocene of
South America showing
Megatherium and two
Glyptodon.
24.
Mesozoic
–
The Mesozoic Era is an interval of geological time from about 252 to 66 million years ago. This Era is also called from a paleobotanist view the Age of Conifers, Mesozoic means middle life, deriving from the Greek prefix meso-/μεσο- for between and zōon/ζῷον meaning animal or living being. It is one of three eras of the Phanerozoic Eon, preceded by the Paleozoic and succeeded by the Cenozoic. The era is subdivided into three periods, the Triassic, Jurassic, and Cretaceous, which are further subdivided into a number of epochs. The Mesozoic was a time of significant tectonic, climate and evolutionary activity, the era witnessed the gradual rifting of the supercontinent Pangaea into separate landmasses that would eventually move into their current positions. The climate of the Mesozoic was varied, alternating between warming and cooling periods, overall, however, the Earth was hotter than it is today. Birds first appeared in the Jurassic, having evolved from a branch of theropod dinosaurs, the first mammals also appeared during the Mesozoic, but would remain small—less than 15 kg —until the Cenozoic. Following the Paleozoic, the Mesozoic extended roughly 186 million years and this time frame is separated into three geologic periods. It is also known as the Great Dying because it is considered the largest mass extinction in the Earths history, the upper boundary of the Mesozoic is set at the Cretaceous–Paleogene extinction event, which may have been caused by the impactor that created Chicxulub Crater on the Yucatán Peninsula. Towards the Late Cretaceous large volcanic eruptions are believed to have contributed to the Cretaceous–Paleogene extinction event. Approximately 50% of all genera became extinct, including all of the non-avian dinosaurs, the Triassic ranges roughly from 252 million to 201 million years ago. The Triassic is a time in Earths history bracketed between the Permian Extinction and the Triassic–Jurassic extinction event, two of the big five, and precedes the Jurassic Period and it has three major epochs, the Early Triassic, the Middle Triassic and the Late Triassic. The Early Triassic was between about 252 million to 247 million years ago and was dominated by deserts as Pangaea had not yet broken up, thus the interior was nothing, the Earth had just witnessed a massive die-off in which 95% of all life became extinct. The most common life on earth were Lystrosaurus, labyrinthodonts. Temnospondyls evolved during this time and would be the dominant predator for much of the Triassic, the Middle Triassic spans roughly from 247 million to 237 million years ago. The Middle Triassic featured the beginnings of the breakup of Pangaea, the ecosystem had recovered from the devastation that was the Great Dying. Algae, sponge, corals, and crustaceans all had recovered, new aquatic reptiles evolved, such as ichthyosaurs and nothosaurs. Meanwhile, on land, pine forests flourished, as did groups of insects like mosquitoes, the first ancient crocodilians evolved, which sparked competition with the large amphibians that had since ruled the freshwater world
Mesozoic
–
Plateosaurus (a
prosauropod)
Mesozoic
–
Rhamphorhynchus
Mesozoic
–
(Inaccurately portrayed)
Stegosaurus
Mesozoic
–
Tylosaurus (a
mosasaur) hunting
Xiphactinus
25.
Carbonate
–
In chemistry, a carbonate is a salt of carbonic acid, characterized by the presence of the carbonate ion, a polyatomic ion with the formula of CO2−3. The name may mean an ester of carbonic acid, an organic compound containing the carbonate group C2. In geology and mineralogy, the term carbonate can refer both to carbonate minerals and carbonate rock, and both are dominated by the ion, CO2−3. Carbonate minerals are extremely varied and ubiquitous in chemically precipitated sedimentary rock, sodium carbonate and potassium carbonate have been used since antiquity for cleaning and preservation, as well as for the manufacture of glass. Carbonates are widely used in industry, e. g. in iron smelting, as a raw material for Portland cement and lime manufacture, in the composition of ceramic glazes, the carbonate ion is the simplest oxocarbon anion. It consists of one carbon atom surrounded by three oxygen atoms, in a planar arrangement, with D3h molecular symmetry. It has a mass of 60.01 g/mol and carries a total formal charge of −2. It is the base of the hydrogen carbonate ion, HCO−3. The Lewis structure of the ion has two single bonds to negative oxygen atoms, and one short double bond to a neutral oxygen. This structure is incompatible with the symmetry of the ion. This process is called calcination, after calx, the Latin name of quicklime or calcium oxide, CaO, exceptions include lithium, sodium, potassium and ammonium carbonates, as well as many uranium carbonates. In aqueous solution, carbonate, bicarbonate, carbon dioxide, in strongly basic conditions, the carbonate ion predominates, while in weakly basic conditions, the bicarbonate ion is prevalent. In more acid conditions, aqueous carbon dioxide, CO2, is the main form, thus sodium carbonate is basic, sodium bicarbonate is weakly basic, while carbon dioxide itself is a weak acid. Carbonated water is formed by dissolving CO2 in water under pressure, in living systems an enzyme, carbonic anhydrase, speeds the interconversion of CO2 and carbonic acid. Although the carbonate salts of most metals are insoluble in water, in solution this equilibrium between carbonate, bicarbonate, carbon dioxide and carbonic acid changes consonant to changing temperature and pressure conditions. In the case of ions with insoluble carbonates, e. g. CaCO3. This is an explanation for the buildup of scale inside pipes caused by hard water, in organic chemistry a carbonate can also refer to a functional group within a larger molecule that contains a carbon atom bound to three oxygen atoms, one of which is double bonded. These compounds are known as organocarbonates or carbonate esters, and have the general formula ROCOOR′
Carbonate
–
Carbonate
26.
Mediterranean climate
–
A Mediterranean climate /ˌmɛdɪtəˈreɪniən/ or dry summer climate, is the climate typical of the lands in the Mediterranean Basin. The Mediterranean climate is characterised by dry summers and mild, moist winters, the Azores High is associated with the Mediterranean climate found in southern Europe and north Africa and the Sahara Desert with France and England both bordering this climate, France especially. The South Atlantic High is similarly associated with the Namib Desert, under the Köppen climate classification, hot dry-summer climates and cool dry-summer climates are often referred to as mediterranean. Under the Köppen climate system, the first letter indicates the climate group, temperate climates or C zones have an average temperature above 0 °C, but below 18 °C, in their coolest months. The second letter indicates the precipitation pattern, Köppen has defined a dry summer month as a month with less than 30 mm of precipitation and with less than one-third that of the wettest winter month. Some, however, use a 40 mm level, the third letter indicates the degree of summer heat, a represents an average temperature in the warmest month above 22 °C, while b indicates the average temperature in the warmest month below 22 °C. Under the Köppen classification, dry-summer climates usually occur on the sides of continents. Under Trewarthas system, at least eight months must have average temperatures of 10 °C or higher, during summer, regions of mediterranean climate are dominated by subtropical high pressure cells, with dry sinking air capping a surface marine layer of varying humidity and making rainfall unlikely. In many Mediterranean climates there is a strong character to daily temperatures in the warm months. The majority of the regions with mediterranean climates have relatively mild winters, however winter and summer temperatures can vary greatly between different regions with a mediterranean climate. Or to consider summer, Athens experiences rather high temperatures in that season, in contrast, San Francisco has cool summers with daily highs around. In North America, areas with Csc climate can be found in the Olympic, Cascade, Klamath and these locations are found at high altitude nearby lower altitude regions characterized by a warm-summer mediterranean climate or hot-summer mediterranean climate. A rare instance of this occurs in the tropics, on Haleakalā Summit in Hawaii. In South America, Csc regions can be found along the Andes in Chile, the town of Balmaceda is one of the few towns confirmed to have this climate. Small areas with a Csc climate can also be found at elevations in Corsica. Mediterranean climate Explanation of Mediterranean Climate
Mediterranean climate
–
Mediterranean climate distribution in the Americas
Mediterranean climate
–
Hot-summer Mediterranean climate (Csa)
27.
Precipitation
–
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravity. The main forms of precipitation include drizzle, rain, sleet, snow, graupel, Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor, so that the water condenses and precipitates. Thus, fog and mist are not precipitation but suspensions, because the vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated, Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers, moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condensed into clouds and rain. This process is active when freezing rain is occurring. A stationary front is often present near the area of freezing rain, provided necessary and sufficient atmospheric moisture content, the moisture within the rising air will condense into clouds, namely stratus and cumulonimbus. Eventually, the droplets will grow large enough to form raindrops. Lake-effect snowfall can be locally heavy, thundersnow is possible within a cyclones comma head and within lake effect precipitation bands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation, on the leeward side of mountains, desert climates can exist due to the dry air caused by compressional heating. The movement of the trough, or intertropical convergence zone. Precipitation is a component of the water cycle, and is responsible for depositing the fresh water on the planet. Approximately 505,000 cubic kilometres of water falls as precipitation each year,398,000 cubic kilometres of it over the oceans and 107,000 cubic kilometres over land. Given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres, Climate classification systems such as the Köppen climate classification system use average annual rainfall to help differentiate between differing climate regimes. Precipitation may occur on celestial bodies, e. g. when it gets cold, Mars has precipitation which most likely takes the form of frost. Precipitation is a component of the water cycle, and is responsible for depositing most of the fresh water on the planet. Approximately 505,000 km3 of water falls as precipitation each year,398,000 km3 of it over the oceans, given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres. Mechanisms of producing precipitation include convective, stratiform, and orographic rainfall, Precipitation can be divided into three categories, based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or ice
Precipitation
–
A thunderstorm with heavy precipitation
Precipitation
–
Long-term mean precipitation by month
Precipitation
–
Late-summer
rainstorm in
Denmark
Precipitation
–
Lenticular cloud forming due to mountains over Wyoming
28.
Relative humidity
–
Relative humidity is the ratio of the partial pressure of water vapor to the equilibrium vapor pressure of water at a given temperature. Relative humidity depends on temperature and the pressure of the system of interest and it requires less water vapor to attain high relative humidity at low temperatures, more water vapour is required to attain high relative humidity in warm or hot air. Humans are sensitive to high humidity because the body uses evaporative cooling, enabled by perspiration. Perspiration evaporates from the more slowly under humid conditions than under arid. For example, if the air temperature is 24 °C and the humidity is zero percent. If the relative humidity is 100 percent at the air temperature. In other words, if the air is 24 °C and contains saturated water vapor, then the human body cools itself at the rate as it would if it were 27 °C. The heat index and the humidex are indices that reflect the effect of temperature. In cold climates, the temperature causes lower capacity for water vapour to flow about. Dry cracked skin can result from dry air, low humidity causes tissue lining nasal passages to dry, crack and become more susceptible to penetration of Rhinovirus cold viruses. Low humidity is a cause of nosebleeds. The use of a humidifier in homes, especially bedrooms, can help with these symptoms, indoor relative humidities should be kept above 30% to reduce the likelihood of the occupants nasal passages drying out. Humans can be comfortable within a range of humidities depending on the temperature—from thirty to seventy percent—but ideally between 50% and 60%. Very low humidity can create discomfort, respiratory problems, and aggravate allergies in some individuals, in the winter, it is advisable to maintain relative humidity at 30 percent or above. Extremely low relative humidities may also cause eye irritation, wooden furniture can shrink, causing the paint that covers these surfaces to fracture. When the temperature is low and the humidity is high. When relative humidity approaches 100 percent, condensation can occur on surfaces, leading to problems with mold, corrosion, decay, condensation can pose a safety risk as it can promote the growth of mold and wood rot as well as possibly freezing emergency exits shut. The basic principles for buildings, above, also apply to vehicles, in addition, there may be safety considerations
Relative humidity
–
Humidity and hygrometry
29.
Sunshine duration
–
It is a general indicator of cloudiness of a location, and thus differs from insolation, which measures the total energy delivered by sunlight over a given period. Sunshine duration is usually expressed in hours per year, or in hours per day, the first measure indicates the general sunniness of a location compared with other places, while the latter allows for comparison of sunshine in various seasons in the same location. Another often-used measure is percentage ratio of recorded bright sunshine duration, an important use of sunshine duration data is to characterize the climate of sites, especially of health resorts. This also takes account the psychological effect of strong solar light on human well-being. It is often used to promote tourist destinations, if the Sun were to be above the horizon 50% of the time for a standard year consisting of 8,760 hours, apparent maximal daytime duration would be 4,380 hours for any point on Earth. However, there are physical and astronomical effects that change that picture, namely, atmospheric refraction allows the Sun to be still visible even when it physically sets below the horizon. For that reason, average daytime is longest in polar areas, places on the Arctic Circle have the longest total annual daytime,4,647 hours, while the North Pole receives 4,575. Because of elliptic nature of the Earths orbit, the Southern Hemisphere is not symmetrical, the Equator has a total daytime of 4,422 hours per year. Given the theoretical maximum of daytime duration for a given location, bright sunshine hours represent the total hours when the sunlight is stronger than a specified threshold, as opposed to just visible hours. Visible sunshine, for example, occurs around sunrise and sunset, measurement is performed by instruments called sunshine recorders. For the specific purpose of sunshine duration recording, Campbell–Stokes recorders are used, when the intensity exceeds a pre-determined threshold, the tape burns. The total length of the trace is proportional to the number of bright hours. Another type of recorder is the Jordan sunshine recorder, newer, electronic recorders have more stable sensitivity than that of the paper tape. In 2003, the duration was finally defined as the period during which direct solar irradiance exceeds a threshold value of 120 W/m². The sky is clear in these regions, and fair weather is virtually perpetual, the descending branch of the Hadley cell and the long-term lack of atmospheric disturbances helps to explain the seemingly endless supply of sunny, cloud-free days in the deserts. Low clouding conditions are associated with rainfall shortage, as seen in these dry regions. In the belt encompassing northern Chad and the Tibesti Mountains, northern Sudan, southern Libya, some places in the interior of the Arabian Peninsula receive 3, 600–3,800 hours of bright sunshine annually. The largest sun-baked region in the world is North Africa, the sunniest month in the world is December in Eastern Antarctica, with almost 23 hours of bright sun daily
Sunshine duration
–
Campbell–Stokes recorder measures sunshine
listen); in the local dialect: Brìnnisi; Latin: Brundisium[1]) is a city in the region of Apulia in southern Italy, the capital of the province of Brindisi, on the coast of the Adriatic Sea. Historically, the city has played an important role in trade and culture, due to its strategic position on the Italian Peninsula and its natural port on the Adriatic Sea, the city remains a major port for trade with Greece and the Middle East. Brindisi's most flourishing industries include agriculture, chemical works, and the generation of electricity.
Denmark
France
Honorary Consulate of Greece
Netherlands
