1.
Gwich'in
–
The Gwich’in are an Athabaskan-speaking First Nations of Canada and an Alaska Native people. They live in the part of North America, mostly above the Arctic Circle. Gwich’in men are known for their crafting of snowshoes, birchbark canoes. The women are renowned for their intricate and ornate beadwork and they also continue to make traditional caribou-skin clothing and porcupine quillwork embroidery, both of which are highly regarded among Gwichin. Today the economy is mostly a mix of hunting, fishing and their name is sometimes spelled Kutchin or Gwitchin and translates as one who dwells or resident of. Historically, the French called the Gwichin Loucheux, as well as the Tukudh, Gwich’in often refer to themselves by the term Dinjii Zhuu instead of Gwich’in. Dinjii Zhuu literally translates as Small People, but figuratively it refers to all Indians, the Gwich’in language, part of the Athabaskan language family, has two main dialects, eastern and western, which are delineated roughly at the United States-Canada border. Each village has unique dialect differences, idioms, and expressions, the Old Crow people in the northern Yukon have approximately the same dialect as those bands living in Venetie and Arctic Village, Alaska. Approximately 300 Alaskan Gwichin speak their language, according to the Alaska Native Language Center, innovative language revitalization projects are underway to document the language and to enhance the writing and translation skills of younger Gwichin speakers. Three major clans survive from antiquity across Gwich’in lands, two are primary clans and the third has a lower/secondary status. The first clan are the Nantsaii, which translates as First on the land. The last clan is called the Tenjeraatsaii, which translates as In the middle or independents and this last clan is reserved for people who marry within their own clan, which is considered incestual. To a lesser degree, it is for children of people who are outside of the clan system, in ancient times this would also refer to the children of Naain, people who were expelled from the tribe due to committing a crime. It also applied to the children of mothers who simply fell outside of the clan system, prior to 1900, being a Tenjeraatsaii automatically placed a Gwich’in at the third-lowest rung of the social ladder. They were to some degree ostracized, the second-lowest rung was reserved for war-captured slaves. The lowest social status was that of a banished Naain or bushman, the clan system is no longer well known or used among the Gwichin. Approximately 9,000 Gwich’in live in 15 small communities in the Northwest Territories and the Yukon Territory of Canada, Gwich’in comedies often contain bawdy humor. Other major characters from the Gwich’in oral tradition include, Googhwaii, Ool Ti, Tłoo Thal, Kaiheenjik, Kiizhazhal, numerous folk tales about prehistoric times all begin with the phrase Deenaadai, which translates roughly as In the ancient days
2.
Old Crow, Yukon
–
Old Crow is a dry community in the Canadian Territory of Yukon and is a periglacial environment. It had 245 inhabitants as of 2011, most of them belonging to the Gwichʼin-speaking Aboriginal Vuntut Gwitchin First Nation, the community is situated on the Porcupine River in the far north of the territory. Old Crow is the only Yukon community that cannot be reached by car, an indigenous chief named Deetru Kavihdik, literally Crow-May-I-Walk, helped settle a community here around the 1870s. The town was named after him, the village was founded around muskrat trapping, which continues to provide basic income. The people of Old Crow are dependent on the Porcupine caribou herd for food, the Porcupine caribou herd migrates to the coastal plain in the Arctic National Wildlife Refuge in Alaska to give birth to their young. Many citizens of Old Crow believe the herd is being threatened by oil-drilling in the ANWR and have been heavily involved in lobbying to prevent it. Old Crow Airport provides year-round transportation to other communities, during winter time, a temporary winter road is sometimes built to transport freight into Old Crow, it is not annual, but only when a significant need arises such as a major building project. Old Crow is served by Northwestel since 1971, in the late 1980s, a satellite ground station was installed in Old Crow, providing more reliable service. The long distance connection is noteworthy for two minor incidents, the community operated its own television transmitter to carry CBC television signals from satellite. The current status of this transmitter is unknown since the CBC in 2012 closed down analog transmitters it owned, the community has APTN television, as well as CHON-FM and CKRW transmitters and a community-owned transmitter picking up CBC station CHAK-AM in Inuvik. Old Crow has a subarctic climate. Average annual temperature is −8.3 °C, Old Crow experiences annual temperature average daily highs of 20.2 °C in July and average daily lows of −33.5 °C in January. Record high temperature was 32.8 °C on August 30,1976, Old Crow has little precipitation with an average annual snowfall of 141.4 centimetres and 154.8 millimetres of rainfall. As Old Crow is located north of the Arctic Circle, it experiences polar day or midnight sun in summer, the midnight sun is typically between May 5 and August 8 inclusive, while the polar night usually starts around December 14 and ends by December 29
3.
Yukon
–
Yukon is the smallest and westernmost of Canadas three federal territories. The territory has the smallest population of any province or territory in Canada, Whitehorse is the territorial capital and Yukons only city. The territory was split from the Northwest Territories in 1898 and was named the Yukon Territory, though officially bilingual, the Yukon Government also recognizes First Nations languages. At 5,959 m, Yukons Mount Logan, in Kluane National Park and Reserve, is the highest mountain in Canada, most of Yukon has a subarctic climate, characterized by long cold winters and brief warm summers. The Arctic Ocean coast has a tundra climate, notable rivers include the Yukon River, after which the territory was named, as well as the Pelly, Stewart, Peel, White and Tatshenshini rivers. Long before the arrival of Europeans, central and southern Yukon was populated by First Nations people, sites of archeological significance in Yukon hold some of the earliest evidence of the presence of human occupation in North America. The sites safeguard the history of the first people and the earliest First Nations of the Yukon, the volcanic eruption of Mount Churchill in approximately 800 AD in what is now the U. S. Coastal and inland First Nations had extensive trading networks, European incursions into the area only began early in the 19th century with the fur trade, followed by missionaries. By the 1870s and 1880s gold miners began to arrive and this drove a population increase that justified the establishment of a police force, just in time for the start of the Klondike Gold Rush in 1897. The increased population coming with the gold led to the separation of the Yukon district from the Northwest Territories. Its northern coast is on the Beaufort Sea and its ragged eastern boundary mostly follows the divide between the Yukon Basin and the Mackenzie River drainage basin to the east in the Mackenzie mountains. Most of the territory is in the watershed of its namesake, the southern Yukon is dotted with a large number of large, long and narrow glacier-fed alpine lakes, most of which flow into the Yukon River system. The larger lakes include Teslin Lake, Atlin Lake, Tagish Lake, Marsh Lake, Lake Laberge, Kusawa Lake, bennett Lake on the Klondike Gold Rush trail is a lake flowing into Nares Lake, with the greater part of its area within Yukon. Canadas highest point, Mount Logan, is in the territorys southwest, Mount Logan and a large part of the Yukons southwest are in Kluane National Park and Reserve, a UNESCO World Heritage Site. Other national parks include Ivvavik National Park and Vuntut National Park in the north, other watersheds include the Mackenzie River, the Peel Watershed and the Alsek–Tatshenshini, and a number of rivers flowing directly into the Beaufort Sea. The two main Yukon rivers flowing into the Mackenzie in the Northwest Territories are the Liard River in the southeast, notable widespread tree species within Yukon are the black spruce and white spruce. Many trees are stunted because of the growing season and severe climate. The capital, Whitehorse, is also the largest city, with about three-quarters of the population, the second largest is Dawson City, which was the capital until 1952
4.
Geographic coordinate system
–
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.
Mammoth
–
A mammoth is any species of the extinct genus Mammuthus, proboscideans commonly equipped with long, curved tusks and, in northern species, a covering of long hair. They lived from the Pliocene epoch into the Holocene at about 4,500 years ago in Africa, Europe, Asia and they were members of the family Elephantidae, which also contains the two genera of modern elephants and their ancestors. Mammoths stem from a species called M. africanavus, the African mammoth. These mammoths lived in northern Africa and disappeared about 3 or 4 million years ago, descendants of these mammoths moved north and eventually covered most of Eurasia. These were M. meridionalis, the southern mammoths, the earliest known proboscideans, the clade that contains the elephants, existed about 55 million years ago around the Tethys Sea area. The closest relatives of the Proboscidea are the sirenians and the hyraxes, the family Elephantidae is known to have existed six million years ago in Africa, and includes the living elephants and the mammoths. Among many now extinct clades, the mastodon is only a distant relative of the mammoths, and part of the separate Mammutidae family, which diverged 25 million years before the mammoths evolved. At the same time, the crowns of the teeth became longer, the first known members of the genus Mammuthus are the African species M. subplanifrons from the Pliocene and M. africanavus from the Pleistocene. The former is thought to be the ancestor of later forms, Mammoths entered Europe around 3 million years ago, the earliest known type has been named M. rumanus, which spread across Europe and China. Only its molars are known, which show it had 8–10 enamel ridges, a population evolved 12–14 ridges and split off from and replaced the earlier type, becoming M. meridionalis. In turn, this species was replaced by the mammoth, M. trogontherii, with 18–20 ridges. Mammoths derived from M. trogontherii evolved molars with 26 ridges 200,000 years ago in Siberia, the Columbian mammoth, M. columbi, evolved from a population of M. trogontherii that had entered North America. A2011 genetic study showed that two examined specimens of the Columbian mammoth were grouped within a subclade of woolly mammoths and this suggests that the two populations interbred and produced fertile offspring. It also suggested that a North American form known as M. jeffersonii may be a hybrid between the two species, variations in environment, climate change, and migration surely played roles in the evolutionary process of the mammoths. Take M. primigenius for example, Woolly mammoths lived in opened grassland biomes, the cool steppe-tundra of the Northern Hemisphere was the ideal place for mammoths to thrive because of the resources it supplied. With occasional warmings during the ice age, climate would change the landscape, the word mammoth was first used in Europe during the early 1600s, when referring to maimanto tusks discovered in Siberia. John Bell, who was on the Ob River in 1722 and they were called mammons horn and were often found in washed-out river banks. Some local people claimed to have seen a living mammoth, but they came out at night
6.
Carbon-14
–
Carbon-14, 14C, or radiocarbon, is a radioactive isotope of carbon with an atomic nucleus containing 6 protons and 8 neutrons. Its presence in organic materials is the basis of the radiocarbon dating method pioneered by Willard Libby, Carbon-14 was discovered on 27 February 1940, by Martin Kamen and Sam Ruben at the University of California Radiation Laboratory in Berkeley, California. Its existence had been suggested by Franz Kurie in 1934, carbon-12 and carbon-13 are both stable, while the half-life of carbon-14 is 5, 730±40 years. Carbon-14 decays into nitrogen-14 through beta decay, a gram of carbon containing 1 atom of carbon-14 per 1012 atoms will emit 0.40 beta particles per second. The primary natural source of carbon-14 on Earth is cosmic ray action on nitrogen in the atmosphere, however, open-air nuclear testing between 1955–1980 contributed to this pool. The different isotopes of carbon do not differ appreciably in their chemical properties, the emitted beta particles have a maximum energy of 156 keV, while their weighted mean energy is 49 keV. These are relatively low energies, the distance traveled is estimated to be 22 cm in air and 0.27 mm in body tissue. The fraction of the radiation transmitted through the dead layer is estimated to be 0.11. Liquid scintillation counting is the preferred method, the G-M counting efficiency is estimated to be 3%. The half-distance layer in water is 0.05 mm. Radiocarbon dating is a dating method that uses to determine the age of carbonaceous materials up to about 60,000 years old. The technique was developed by Willard Libby and his colleagues in 1949 during his tenure as a professor at the University of Chicago, in 1960, Libby was awarded the Nobel Prize in chemistry for this work. One of the frequent uses of the technique is to date organic remains from archaeological sites, plants fix atmospheric carbon during photosynthesis, so the level of 14C in plants and animals when they die approximately equals the level of 14C in the atmosphere at that time. However, it decreases thereafter from radioactive decay, allowing the date of death or fixation to be estimated. A calculation or a comparison of carbon-14 levels in a sample, with tree ring or cave-deposit carbon-14 levels of a known age. Carbon-14 is produced in the layers of the troposphere and the stratosphere by thermal neutrons absorbed by nitrogen atoms. When cosmic rays enter the atmosphere, they undergo various transformations, the resulting neutrons participate in the following reaction, n +14 7N →14 6C + p The highest rate of carbon-14 production takes place at altitudes of 9 to 15 km and at high geomagnetic latitudes. Production rates vary because of changes to the cosmic ray flux caused by the heliospheric modulation, the latter can create significant variations in 14C production rates, although the changes of the carbon cycle can make these effects difficult to tease out. Another extraordinarily large 14C increase has been associated with the 5480 BC event
7.
Last Glacial Maximum
–
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
8.
Beringia
–
It includes the Chukchi Sea, the Bering Sea, the Bering Strait, the Chukchi and Kamchatka Peninsulas in Russia as well as Alaska in the United States. The area includes land lying on the North American Plate and Siberian land east of the Chersky Range. Today, the land that is visible from the central part of the Bering land bridge are the Diomede Islands, the Pribilof Islands of St. Paul and St. George, St. Lawrence Island. The term Beringia was coined by the Swedish botanist Eric Hultén in 1937, during the ice ages, Beringia, like most of Siberia and all of North and Northeast China, was not glaciated because snowfall was very light. It was a grassland steppe, including the bridge, that stretched for hundreds of kilometres into the continents on either side. Before European colonization, Beringia was inhabited by the Yupik peoples on both sides of the straits and this culture remains in the region today along with others. In 2012, the governments of Russia and the United States announced a plan to establish a transboundary area of shared Beringian heritage. The underlying mechanism was first thought to be tectonics, but by 1930 changes in the icemass balance, the American arctic geologist David Hopkins redefined Beringia to include portions of Alaska and Northeast Asia. Beringia was later regarded as extending from the Verkhoyansk Mountains in the west to the Mackenzie River in the east. The distribution of plants in the genera Erythranthe and Pinus are good examples of this as genera members are found in Asia, during the Pleistocene epoch, global cooling led periodically to the expansion of glaciers and lowering of sea levels. This created land connections in various regions around the globe, today, the average water depth of the Bering Strait is 40–50 m, therefore the land bridge opened when the sea level dropped more than 50 m below the current level. Post-glacial rebound has continued to some sections of coast. During the last glacial period, enough of the water became frozen in the great ice sheets covering North America. For thousands of years the sea floors of many interglacial shallow seas were exposed, including those of the Bering Strait, the Chukchi Sea to the north, other land bridges around the world have emerged and disappeared in the same way. Beringias closeness to the sea created intermittent maritime cloud cover, which caused an interruption to the dry, in the Late Pleistocene, Beringia was a mosaic of biological communities. Commencing from c. 57,000 BP, steppe–tundra vegetation dominated large parts of Beringia with a diversity of grasses. There were patches of shrub tundra with isolated refugia of larch and spruce forests with birch and it has been proposed that the largest and most diverse megafaunal community residing in Beringia at this time could only have been sustained in a highly diverse and productive environment. These changes provided the most likely explanation for mammal migrations after c. 15,000 BP, as the warming provided increased forage for browsers, Beringia did not block the movement of most dry steppe-adapted large species such as saiga antelope, woolly mammoth, and caballid horses
9.
International Standard Serial Number
–
An International Standard Serial Number is an eight-digit serial number used to uniquely identify a serial publication. The ISSN is especially helpful in distinguishing between serials with the same title, ISSN are used in ordering, cataloging, interlibrary loans, and other practices in connection with serial literature. The ISSN system was first drafted as an International Organization for Standardization international standard in 1971, ISO subcommittee TC 46/SC9 is responsible for maintaining the standard. When a serial with the content is published in more than one media type. For example, many serials are published both in print and electronic media, the ISSN system refers to these types as print ISSN and electronic ISSN, respectively. The format of the ISSN is an eight digit code, divided by a hyphen into two four-digit numbers, as an integer number, it can be represented by the first seven digits. The last code digit, which may be 0-9 or an X, is a check digit. Formally, the form of the ISSN code can be expressed as follows, NNNN-NNNC where N is in the set, a digit character. The ISSN of the journal Hearing Research, for example, is 0378-5955, where the final 5 is the check digit, for calculations, an upper case X in the check digit position indicates a check digit of 10. To confirm the check digit, calculate the sum of all eight digits of the ISSN multiplied by its position in the number, the modulus 11 of the sum must be 0. There is an online ISSN checker that can validate an ISSN, ISSN codes are assigned by a network of ISSN National Centres, usually located at national libraries and coordinated by the ISSN International Centre based in Paris. The International Centre is an organization created in 1974 through an agreement between UNESCO and the French government. The International Centre maintains a database of all ISSNs assigned worldwide, at the end of 2016, the ISSN Register contained records for 1,943,572 items. ISSN and ISBN codes are similar in concept, where ISBNs are assigned to individual books, an ISBN might be assigned for particular issues of a serial, in addition to the ISSN code for the serial as a whole. An ISSN, unlike the ISBN code, is an identifier associated with a serial title. For this reason a new ISSN is assigned to a serial each time it undergoes a major title change, separate ISSNs are needed for serials in different media. Thus, the print and electronic versions of a serial need separate ISSNs. Also, a CD-ROM version and a web version of a serial require different ISSNs since two different media are involved, however, the same ISSN can be used for different file formats of the same online serial
10.
Cave painting
–
Cave paintings are painted drawings on cave walls or ceilings, mainly of prehistoric origin, to some 40,000 years ago in Eurasia. The exact purpose of the Paleolithic cave paintings is not known, evidence suggests that they were not merely decorations of living areas since the caves in which they have been found do not have signs of ongoing habitation. They are also located in areas of caves that are not easily accessible. Some theories hold that cave paintings may have been a way of communicating with others, the paintings are remarkably similar around the world, with animals being common subjects that give the most impressive images. Humans mainly appear as images of hands, mostly hand stencils made by blowing pigment on a hand held to the wall. The earliest known cave paintings/drawings of animals are at least 35,000 years old and are found in Pettakere cave on the island of Sulawesi in Indonesia, previously it was believed that the earliest paintings were in Europe. The earliest non-figurative rock art dates back to approximately 40,000 years ago, nearly 340 caves have now been discovered in France and Spain that contain art from prehistoric times. But subsequent technology has made it possible to date the paintings by sampling the pigment itself, the choice of subject matter can also indicate chronology. For instance, the reindeer depicted in the Spanish cave of Cueva de las Monedas places the drawings in the last Ice Age. The oldest date given to a cave painting is now a pig that has a minimum age of 35,400 years old at Pettakere cave in Sulawesi. Indonesian and Australian scientists have dated other non-figurative paintings on the walls to be approximately 40,000 years old, the method they used to confirm this was dating the age of the stalactites that formed over the top of the paintings. The art is similar in style and method to that of the Indonesian caves as there were also hand stencils and this date coincides with the earliest known evidence for Homo sapiens in Europe. Because of the cave arts age, some scientists have conjectured that the paintings may have made by Neanderthals. The earliest known European figurative cave paintings are those of Chauvet Cave in France and these paintings date to earlier than 30,000 BCE according to radiocarbon dating. Some researchers believe the drawings are too advanced for this era, the radiocarbon dates from these samples show that there were two periods of creation in Chauvet,35,000 years ago and 30,000 years ago. In 2009, cavers discovered drawings in Coliboaia Cave in Romania, an initial dating puts the age of an image in the same range as Chauvet, about 32,000 years old. Some caves probably continued to be painted over a period of thousands of years. This was created roughly between 10,000 and 5,500 years ago, and painted in rock shelters under cliffs or shallow caves, though individual figures are less naturalistic, they are grouped in coherent grouped compositions to a much greater degree
11.
Armenia
–
Armenia, officially the Republic of Armenia, is a sovereign state in the South Caucasus region of Eurasia. The Republic of Armenia constitutes only one-tenth of historical Armenia, Armenia is a unitary, multi-party, democratic nation-state with an ancient cultural heritage. Urartu was established in 860 BC and by the 6th century BC it was replaced by the Satrapy of Armenia, in the 1st century BC the Kingdom of Armenia reached its height under Tigranes the Great. Armenia became the first state in the world to adopt Christianity as its official religion, in between the late 3rd century to early years of the 4th century, the state became the first Christian nation. The official date of adoption of Christianity is 301 AD. The ancient Armenian kingdom was split between the Byzantine and Sasanian Empires around the early 5th century, under the Bagratuni dynasty, the Bagratid Kingdom of Armenia was restored in the 9th century. Declining due to the wars against the Byzantines, the fell in 1045. An Armenian principality and later a kingdom Cilician Armenia was located on the coast of the Mediterranean Sea between the 11th and 14th centuries. By the 19th century, Eastern Armenia had been conquered by the Russian Empire, during World War I, Armenians living in their ancestral lands in the Ottoman Empire were systematically exterminated in the Armenian Genocide. By 1920, the state was incorporated into the Transcaucasian Socialist Federative Soviet Republic, in 1936, the Transcaucasian state was dissolved, transforming its constituent states, including the Armenian Soviet Socialist Republic, into full Union republics. The modern Republic of Armenia became independent in 1991 during the dissolution of the Soviet Union, the Republic of Armenia recognises the Armenian Apostolic Church, the worlds oldest national church, as the countrys primary religious establishment. The unique Armenian alphabet was invented by Mesrop Mashtots in 405 AD, Armenia is a member of the Eurasian Economic Union, the Council of Europe and the Collective Security Treaty Organization. Armenia supports the de facto independent Nagorno-Karabakh Republic, which was proclaimed in 1991, the native Armenian name for the country is Հայք. The name in the Middle Ages was extended to Հայաստան, by addition of the Persian suffix -stan, the further origin of the name is uncertain. It is also postulated that the name Hay comes from one of the two confederated, Hittite vassal states—the Ḫayaša-Azzi. The exonym Armenia is attested in the Old Persian Behistun Inscription as Armina, the ancient Greek terms Ἀρμενία and Ἀρμένιοι are first mentioned by Hecataeus of Miletus. Xenophon, a Greek general serving in some of the Persian expeditions, describes many aspects of Armenian village life and he relates that the people spoke a language that to his ear sounded like the language of the Persians. According to the histories of both Moses of Chorene and Michael Chamchian, Armenia derives from the name of Aram, a descendant of Hayk
12.
Areni-1 cave
–
The Areni-1 cave complex is located near the Areni village in southern Armenia along the Arpa River. In 2010, it was announced that the earliest known shoe was found at the site, in January 2011, the earliest known winery in the world was announced to have been found. Also in 2011, the discovery of a straw skirt dating to 3900 BC was reported, in 2009, the oldest brain was discovered
13.
Austria
–
Austria, officially the Republic of Austria, is a federal republic and a landlocked country of over 8.7 million people in Central Europe. It is bordered by the Czech Republic and Germany to the north, Hungary and Slovakia to the east, Slovenia and Italy to the south, the territory of Austria covers 83,879 km2. The terrain is mountainous, lying within the Alps, only 32% of the country is below 500 m. The majority of the population speaks local Bavarian dialects of German as their native language, other local official languages are Hungarian, Burgenland Croatian, and Slovene. The origins of modern-day Austria date back to the time of the Habsburg dynasty, from the time of the Reformation, many northern German princes, resenting the authority of the Emperor, used Protestantism as a flag of rebellion. Following Napoleons defeat, Prussia emerged as Austrias chief competitor for rule of a greater Germany, Austrias defeat by Prussia at the Battle of Königgrätz, during the Austro-Prussian War of 1866, cleared the way for Prussia to assert control over the rest of Germany. In 1867, the empire was reformed into Austria-Hungary, Austria was thus the first to go to war in the July Crisis, which would ultimately escalate into World War I. The First Austrian Republic was established in 1919, in 1938 Nazi Germany annexed Austria in the Anschluss. This lasted until the end of World War II in 1945, after which Germany was occupied by the Allies, in 1955, the Austrian State Treaty re-established Austria as a sovereign state, ending the occupation. In the same year, the Austrian Parliament created the Declaration of Neutrality which declared that the Second Austrian Republic would become permanently neutral, today, Austria is a parliamentary representative democracy comprising nine federal states. The capital and largest city, with a population exceeding 1.7 million, is Vienna, other major urban areas of Austria include Graz, Linz, Salzburg and Innsbruck. Austria is one of the richest countries in the world, with a nominal per capita GDP of $43,724, the country has developed a high standard of living and in 2014 was ranked 21st in the world for its Human Development Index. Austria has been a member of the United Nations since 1955, joined the European Union in 1995, Austria also signed the Schengen Agreement in 1995, and adopted the euro currency in 1999. The German name for Austria, Österreich, meant eastern realm in Old High German, and is cognate with the word Ostarrîchi and this word is probably a translation of Medieval Latin Marchia orientalis into a local dialect. Austria was a prefecture of Bavaria created in 976, the word Austria is a Latinisation of the German name and was first recorded in the 12th century. Accordingly, Norig would essentially mean the same as Ostarrîchi and Österreich, the Celtic name was eventually Latinised to Noricum after the Romans conquered the area that encloses most of modern-day Austria, around 15 BC. Noricum later became a Roman province in the mid-first century AD, heers hypothesis is not accepted by linguists. Settled in ancient times, the Central European land that is now Austria was occupied in pre-Roman times by various Celtic tribes, the Celtic kingdom of Noricum was later claimed by the Roman Empire and made a province
14.
Tischofer Cave
–
The Tischofer Cave is a cave in the Kaisertal valley in the Kaisergebirge mountains in Austria. It was important locally as a place and weapons cache for local rebels during the Napoleonic Wars. The roughly 40 m long cave, which is about 8.5 m high at the entrance, was used during the Stone Age by bears and other predators as shelter and that makes the Tischofer Cave the oldest proven site of human occupation in Tyrol. Discoveries of human skeletons and tools also indicate that the cave acted as a copper smithy, the Tischofer Cave may be reached on foot via the Kaiser Path in the Kaisertal valley, a pathway secured with cable railings. It is recorded in the Tyrolean Cave Register as number 1312/001, article from Hofmann, Wege im Inntal with comprehensive description Die Tischofer Höhle im Kaisertal bei Kufstein at www. tirol-infos. at. Tischofer Höhle im Kaisertal at www. kaisergebirge-online. de
15.
Belgium
–
Belgium, officially the Kingdom of Belgium, is a sovereign state in Western Europe bordered by France, the Netherlands, Germany, Luxembourg, and the North Sea. It is a small, densely populated country which covers an area of 30,528 square kilometres and has a population of about 11 million people. Additionally, there is a group of German-speakers who live in the East Cantons located around the High Fens area. Historically, Belgium, the Netherlands and Luxembourg were known as the Low Countries, the region was called Belgica in Latin, after the Roman province of Gallia Belgica. From the end of the Middle Ages until the 17th century, today, Belgium is a federal constitutional monarchy with a parliamentary system of governance. It is divided into three regions and three communities, that exist next to each other and its two largest regions are the Dutch-speaking region of Flanders in the north and the French-speaking southern region of Wallonia. The Brussels-Capital Region is a bilingual enclave within the Flemish Region. A German-speaking Community exists in eastern Wallonia, Belgiums linguistic diversity and related political conflicts are reflected in its political history and complex system of governance, made up of six different governments. Upon its independence, declared in 1830, Belgium participated in the Industrial Revolution and, during the course of the 20th century, possessed a number of colonies in Africa. This continuing antagonism has led to several far-reaching reforms, resulting in a transition from a unitary to a federal arrangement during the period from 1970 to 1993. Belgium is also a member of the Eurozone, NATO, OECD and WTO. Its capital, Brussels, hosts several of the EUs official seats as well as the headquarters of major international organizations such as NATO. Belgium is also a part of the Schengen Area, Belgium is a developed country, with an advanced high-income economy and is categorized as very high in the Human Development Index. A gradual immigration by Germanic Frankish tribes during the 5th century brought the area under the rule of the Merovingian kings, a gradual shift of power during the 8th century led the kingdom of the Franks to evolve into the Carolingian Empire. Many of these fiefdoms were united in the Burgundian Netherlands of the 14th and 15th centuries, the Eighty Years War divided the Low Countries into the northern United Provinces and the Southern Netherlands. The latter were ruled successively by the Spanish and the Austrian Habsburgs and this was the theatre of most Franco-Spanish and Franco-Austrian wars during the 17th and 18th centuries. The reunification of the Low Countries as the United Kingdom of the Netherlands occurred at the dissolution of the First French Empire in 1815, although the franchise was initially restricted, universal suffrage for men was introduced after the general strike of 1893 and for women in 1949. The main political parties of the 19th century were the Catholic Party, French was originally the single official language adopted by the nobility and the bourgeoisie
16.
Neolithic flint mines of Spiennes
–
The mines were active during the mid and late Neolithic between 4,300 and 2,200 BC. Declared to be remarkable for the diversity of technological solutions used for extraction the site, discovered in 1843, the first excavations were undertaken during railway construction in 1867 and intermittent excavations have been carried out up to the present day. The Mines of Spiennes cover some 100 ha of downland four miles south-east of the city of Mons, the site is dotted with millions of scraps of worked flint and numerous mining pits, that Neolithic settlers have gradually turned into vertical mine shafts to depths of over 10 m. Research has illustrated Neolithic techniques for the cutting of the flint and the extraction of large slabs of flint, the nodules were extracted using flint picks. The stones were then knapped into rough-out shapes of axes, the SILEXS Interpretive Centre has opened in spring 2015. The rough-outs were exchanged over an area, about 150 km. Polishing strengthens the product, making the axe- or adze-head last longer. The smooth surface also aids the cutting action by lowering friction with the wood, the axes were used initially for forest clearance during the Neolithic period, and for shaping wood for structural applications, such as timber for huts and canoes. The site has been compared with Grimes Graves and Cissbury in the United Kingdom, and Krzemionki in Poland, however, different hard rocks were used for the polished stone axes. Examples include the Langdale axe industry, Penmaenmawr and Tievebulliagh, guillaume, Ph. Lipinski & A. Masson, Les mines de silex néolithiques de la Meuse dans le contexte européen. Musées de la Meuse, Sampigny 1987, F. Gosselin, Un site dexploitation du silex à Spiennes, au lieu-dit Petit-Spiennes. F. Hubert, Une minière néolithique à silex au Camp-à-Cayaux de Spiennes, F. Hubert, Lexploitation préhistorique du silex à Spiennes. Ministère de la Région wallonne, Direction générale de lAménagement du Territoire, du Logement et du Patrimoine, R. Shepherd, Prehistoric Mining and Allied Industries. Société de recherches préhistoriques en Hainaut, Minières néolithiques à Spiennes,1997 ICOMOS evaluation Collet, H. Les mines néolithiques de Spiennes, état des connaissances et perspectives de recherche. Section 10, The Neolithic in the Near East and Europe, actes du XIVème congrès UISPP, Université de Liège, Belgique,2 –8 septembre 2001 H. Collet, A. Hauzeur & J. Lech,2008. The prehistoric flint mining complex at Spiennes on the occasion of its discovery 140 years ago In P. Allard, F. Bostyn, flint mining in Prehistoric Europe, Interpreting the archaeological records. European Association of Archaeologists, 12th Annual Meeting, Cracow, Poland, 19–24 September 2006, H. Collet,2014. Les minières néolithiques de silex de Spiennes
17.
Scladina
–
The caves in the area have been undergone systematic exploration since 1949. Scladina Cave was discovered in 1971 by cavers of the CAS, in 1978 the Scientific Council of the Prehistory Department of the University of Liège began to direct the excavations. Since the site has yielded numerous artifacts of Mousterian Neanderthal origin, amidst assemblages of stone tools, bones, after the initially clearing of the entrance the excavations uncovered two strata of Neanderthal occupation, the oldest dating back 130,000 years. The sediments yielded artifacts and Mousterian stone tools, the earliest were attributed to the Middle Palaeolithic, two Neanderthal occupation sites were identified, one dated to be 130,000 years old and the other 40,000 years. Modern humans infrequently occupied the site between 32,000 and 9,000 years ago and used the site as a place during the late Neolithic. Continued excavations since 1978 have produced a stream of findings that culminated in the discovery of the remarkable Sclayn child fossils in 1993. Sclayn cave site has been classified as a heritage site of Wallonia on 27 May 2009 and is since open to the public. Dated to be around 127,000 years old, the first fragment of the now nearly complete mandible, was found on 16 July 1993, a maxillary fragment and several teeth of the child were excavated in subsequent campaigns. A genetic sample was successfully extracted from one of the molars at a laboratory for ancient DNA and analyzed at the Max Planck Institute for Evolutionary Anthropology. Initially it was suggested that the Scladina child was 2 to 4 years older than current estimates, some scholars, though debate universal periods of anterior tooth growth, as it is known that anterior tooth growth takes longer in great apes than in humans and varies among human populations. The study of the turned out to support the idea that extremely prolonged duration of human development is unique to Homo sapiens. This trend suggests to scientists the necessary prevalence of differing patterns of behavioral and social development as well. Neanderthal diet consisted to over 70% of meat, unlike that of contemporary Homo sapiens hunter-gatherer societies, although some cooked vegetables are evident. Provisioning techniques, made superior by extensive use, aided early Homo in pursuits of worldwide expansion. One large game evident in the diets of Scladina Neanderthals is bear, several bear bones were found amongst other stone tools and modifiers within the Scladina cave site. Wear marks on the bones,4 of the 6 bear bone tools which originated from a single femur, the idea is to correctly inform about prehistory, deemed to be still perceived as nebulous and mythical by the general public. The site and its center are open to the public all year round. Private groups, school classes are permanently granted access to the cave, the laboratory, list of human evolution fossils Scladina Cave Archaeological Center The Scladina cave Archéologie Andennaise SUPPLEMENTARY INFORMATION of tooth development
18.
Spy Cave
–
Spy Cave is located near Spy in the municipality of Jemeppe-sur-Sambre, province of Namur, Belgium above the left bank of the Orneau River. Classified as a premier Wallonian Heritage site of the Walloon Region, the cave consists of numerous small chambers and corridors. Since the first amateur investigations during the late 19th century numerous amateur and professional archaeologists have carried out excavations, the excavation was conducted by Liège, archaeologist Marcel de Puydt and geologist Max Lohest. Paleontologist and zoologist Julien Fraipont published the description in the American Anthropologist journal. The assemblages of the oldest excavations have been mixed, that makes the interpretation of the palaeoenvironment difficult, in addition publications of de Puydt, Lohest and Fraipoint disagree on the number of layers of knapped flints. The hominid skeletons discovered during the first excavations have been named Spy I, a female, and Spy 2 and these were dated to around 36,000 years BP, although a Bayesian analysis in 2014 concluded that they were probably more than 40,000 years old. The identification of the remains of a Neanderthal child, Spy VI, was published in 2010, almost 12,000 faunal remains of the Pleistocene were discovered, including mammoth, horse, cave hyena, woolly rhinoceros, reindeer, and cave bear bones. All levels contained mammoth remains, including a number of molars. It has been suggested that the Neanderthal occupants brought mammoth heads to the site and ate the brains, because many of the molars were unworn, these would have been very young or newborn calves, killed in early spring, when plant food would not yet have been available. Evidence of occupation by Upper Paleolithic anatomically modern humans has also found at Spy. Pendants and perforated beads made from ivory, presumably by modern humans, were found in the cave. Goyet Caves Media related to Spy Cave at Wikimedia Commons
19.
Bosnia and Herzegovina
–
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
20.
Badanj Cave
–
Badanj Cave is located in Borojevići village near the town of Stolac, Bosnia and Herzegovina. This rather small cave has come to attention after the 1976 discovery of its cave engravings. The site is rock shelter or overhang recessed beneath a cliff that descends to the bank of the river Bregava. Two chronologically distinct strata of Palaeolithic occupation were identified beneath the surface layer, of particular significance was the discovery of a particular carving of the Badanj site, as it ranks among the oldest works of art in Bosnia and Herzegovina. The carving is cut into the surface of a large polished block of stone. Only the rear half of the body survives, with flanks typical for a horse and part of the body, the Badanj carvings include depictions of animals and symbols, as is typical of Mediterranean prehistoric art. The site was dated to the late Upper Palaeolithic and it is also designated as a National Monument of Bosnia and Herzegovina since 2003
21.
Bulgaria
–
Bulgaria, officially the Republic of Bulgaria, is a country in southeastern Europe. It is bordered by Romania to the north, Serbia and Macedonia to the west, Greece and Turkey to the south, with a territory of 110,994 square kilometres, Bulgaria is Europes 16th-largest country. Organised prehistoric cultures began developing on current Bulgarian lands during the Neolithic period and its ancient history saw the presence of the Thracians, Greeks, Persians, Celts, Romans, Goths, Alans and Huns. With the downfall of the Second Bulgarian Empire in 1396, its territories came under Ottoman rule for five centuries. The Russo-Turkish War of 1877–78 led to the formation of the Third Bulgarian State, the following years saw several conflicts with its neighbours, which prompted Bulgaria to align with Germany in both world wars. In 1946 it became a one-party socialist state as part of the Soviet-led Eastern Bloc, in December 1989 the ruling Communist Party allowed multi-party elections, which subsequently led to Bulgarias transition into a democracy and a market-based economy. Bulgarias population of 7.2 million people is predominantly urbanised, most commercial and cultural activities are centred on the capital and largest city, Sofia. The strongest sectors of the economy are industry, power engineering. The countrys current political structure dates to the adoption of a constitution in 1991. Bulgaria is a parliamentary republic with a high degree of political, administrative. Human activity in the lands of modern Bulgaria can be traced back to the Paleolithic, animal bones incised with man-made markings from Kozarnika cave are assumed to be the earliest examples of symbolic behaviour in humans. Organised prehistoric societies in Bulgarian lands include the Neolithic Hamangia culture, Vinča culture, the latter is credited with inventing gold working and exploitation. Some of these first gold smelters produced the coins, weapons and jewellery of the Varna Necropolis treasure and this site also offers insights for understanding the social hierarchy of the earliest European societies. Thracians, one of the three primary groups of modern Bulgarians, began appearing in the region during the Iron Age. In the late 6th century BC, the Persians conquered most of present-day Bulgaria, and kept it until 479 BC. After the division of the Roman Empire in the 5th century the area fell under Byzantine control, by this time, Christianity had already spread in the region. A small Gothic community in Nicopolis ad Istrum produced the first Germanic language book in the 4th century, the first Christian monastery in Europe was established around the same time by Saint Athanasius in central Bulgaria. From the 6th century the easternmost South Slavs gradually settled in the region, in 680 Bulgar tribes under the leadership of Asparukh moved south across the Danube and settled in the area between the lower Danube and the Balkan, establishing their capital at Pliska
22.
Bacho Kiro cave
–
The Bacho Kiro cave is situated 5 km west of the town Dryanovo, Bulgaria, only 300 m away from the Dryanovo Monastery. It is embedded in the canyons of the Andaka and Dryanovo River, the cave is a four-storey labyrinth of galleries and corridors with a total length of 3,600 m,700 m of which are maintained for public access and equipped with electrical lights since 1964. An underground river has over time carved out the many galleries that contain countless stalactone, stalactite, galleries and caverns of a 1,200 m long section have been been musingly named as a popular description of this fairy-tale underground world. The formations succession, Bacho Kiro’s Throne, The Dwarfs, The Sleeping Princess, The Throne Hall, The Reception Hall, The Haidouti Meeting-Ground, The Fountain, the site has yielded the oldest human remains ever to be found in Bulgaria. Among one of the earliest known Aurignacian burials, two pierced animal teeth were found and ordered into the distinct Bachokiran artifact assemblage, radiocarbon dated to over 43,000 years ago, they currently represent the oldest known ornaments in Europe. With an approximate age of 46,000 years, human fossils consist of a pair of fragmented mandibles, whether these early humans were in fact Homo sapiens or Neanderthals is still disputed
23.
Devetashka cave
–
Devetàshka cave is a huge karst cave around 7 km east of Letnitsa and 15 km northeast of Lovech, near the village of Devetaki on the east bank of the river Osam, in Bulgaria. The site has continuously occupied by Paleo humans for tens of thousands of years. Devetashka cave is located approximately 2 km from the village of Devetaki, a narrow path by the river lead from the village to the cave. It can also be accessed directly via Road 301 along a 400 m long dirt road, the site is 35 m wide and 30 m high at the entrance. The cave widens after around 40 m, forming a hall with an area of 2,400 m2. Earliest traces of human presence back to the Middle Paleolithic around 70,000 years ago. The site also contained one of the richest sources of Neolithic cultural artifacts, besides significant archaeological findings, Devetashka cave is provides a habitat for a wide diversity of faunal residents. During the breeding season of mammalian species in the cave from early June to the end of July, thirty-four species of mammals, four of which are included in the Red List and fifteen species of bats are to be found at the Devetashka cave. Devetashka cave was shown in the action movie The Expendables 2, the Supreme Administrative Court of Bulgaria declared that several activities during filming violated Bulgarias environmental regulations. A contractor hired by The Expendables crew was subsequently fined for trimming the shrubbery in front of the site, after a fatal accident during the filming of a stunt, the production team again clashed with the authorities over damages to the cave. Loud noises, bright lights, crowds of people and fires in close proximity to the cave might have caused the displacement of large numbers of bats from the cave, however, by late 2012, the majority of the bats had returned to the cave. Media related to Devetashka cave at Wikimedia Commons Devetashka Cave
24.
Magura Cave
–
The Magura Cave is located in north-western Bulgaria close to the village of Rabisha,25 km from the town of Belogradchik in Vidin Province. Guided visits are conducted by the staff of Belogradchik municipality, to which the management of the cave was transferred in 2012 by the Bulgarian Council of Ministers, in 1984 the site was induced into UNESCOs tentative list of World Heritage. The total length of the 15 million year old cave is 2.5 km, the average annual temperature of the cave is 12 °C, except for one room where the temperature is always 15 °C. The air humidity reaches 80% and the displacement -56 m, the Magura cave was formed in the limestone Rabisha Hill. The morphology of the consists of one main gallery with six various-sized halls. The very spacious site also allows for music concerts to be held during Christmas, the inner temperature is constantly 11-12 °C. During the summers of 1974 and 1975 the cave was used for speleotherapy. Thirty patients slept in the cave for twelve nights, taking advantage of allergens absence, constant humidity. A part of the cave is now used for ageing sparkling and red wines, labelled Magura, bones from different prehistoric species like cave bear, cave hyena, fox, wolf, wild cat and otter have been discovered in the Magura Cave. Today, constant inhabitants of the cave is the collembola, as well as four types of bats, Cave paintings dating from the Epipaleolithic, late Neolithic, Eneolithic and early Bronze Age decorate some of the caves walls. The paintings have been estimated to be made between 10.000 and 8.000 years ago, the drawings represent important events of the society that had occupied the Magura cave, religious ceremonies, hunting scenes and depictions of deities which are unique on the Balkan peninsula. The Fertility Dance and the Hunting Ceremony rank among the most noteworthy paintings, one grouping from the Bronze Age has been interpreted as a solar calendar. The cave paintings allowed storing information about regional solar calendar, customs, religious festivals, contemporary imitations of possible fertility rites are reported — inscriptions in Latin and paintings made by treasure-hunters. The medium used to create the art was bat guano, more than 750 images have been identified. Painted signs can be organised into four groups, anthropomorphic, zoomorphic, geometric. For the first group, there are bitriangular silhouettes with raised rounded arms, archers, ithyphallic figures, copula, regarding zoomorpic items, there are caprids, bovids, dogs, ostrich-like animals and schematic linear quadrupeds. Few rayed circle figures, mainly the two unica of the so-called calendar scene, likely represent a sun depiction, taking count of some associated figures, it is possible to recognize dancing, hunting, and mating scenes. In the so-called Cult Hall a large dance and hunting scene is depicted, arranged in two main rows, these are the best known and most reproduced Magura Cave images
25.
Kozarnika
–
Kozarnika or Peshtera Kozarnika is a cave in northwestern Bulgaria that was used as a hunters’ shelter as early as the Lower Paleolithic. It marks an older route of human migration from Africa to Europe via the Balkans. The cave probably keeps the earliest evidence of symbolic behaviour. Kozarnika cave is located 6 km from the town of Belogradchik in northwestern Bulgaria, on the slopes of the Balkan Mountains. It is opened to the south, at 85 m above the valley, with its length of 210 m, the cave is among the small-sized in the Belogradchick karst region. The Kozarnika cave project started in 1984, since 1996, it has been headed by Dr. Prof. Nikolay Sirakov and Dr. Jean-Luc Guadelli. In the ground layers, dated to 1. 6–1, the findings from Middle Paleolithic layers, rather bifacial points, dating from 300, 000–50,000 BP prove presence of hunters’ groups possibly of Homo neanderthalensis. Upper Paleolithic layers consist flint assemblages from the earliest European Gravette complex dating from 43,000 up to 39,000 BP belonging to Homo sapiens sapiens, magura Cave Bacho Kiro cave Sićevo Gorge Peștera cu Oase Vértesszőlős Proto-Indo-Europeans Campanian Ignimbrite Eruption Rincon, Paul
26.
Croatia
–
Croatia, officially the Republic of Croatia, is a sovereign state between Central Europe, Southeast Europe, and the Mediterranean. Its capital city is Zagreb, which one of the countrys primary subdivisions. Croatia covers 56,594 square kilometres and has diverse, mostly continental, Croatias Adriatic Sea coast contains more than a thousand islands. The countrys population is 4.28 million, most of whom are Croats, the Croats arrived in the area of present-day Croatia during the early part of the 7th century AD. They organised the state into two duchies by the 9th century, tomislav became the first king by 925, elevating Croatia to the status of a kingdom. The Kingdom of Croatia retained its sovereignty for nearly two centuries, reaching its peak during the rule of Kings Petar Krešimir IV and Dmitar Zvonimir, Croatia entered a personal union with Hungary in 1102. In 1527, faced with Ottoman conquest, the Croatian Parliament elected Ferdinand I of the House of Habsburg to the Croatian throne. In 1918, after World War I, Croatia was included in the unrecognized State of Slovenes, Croats and Serbs which seceded from Austria-Hungary, a fascist Croatian puppet state backed by Fascist Italy and Nazi Germany existed during World War II. After the war, Croatia became a member and a federal constituent of the Socialist Federal Republic of Yugoslavia. On 25 June 1991 Croatia declared independence, which came wholly into effect on 8 October of the same year, the Croatian War of Independence was fought successfully during the four years following the declaration. A unitary state, Croatia is a republic governed under a parliamentary system, the International Monetary Fund classified Croatia as an emerging and developing economy, and the World Bank identified it as a high-income economy. Croatia is a member of the European Union, United Nations, the Council of Europe, NATO, the World Trade Organization, the service sector dominates Croatias economy, followed by the industrial sector and agriculture. Tourism is a significant source of revenue during the summer, with Croatia ranked the 18th most popular tourist destination in the world, the state controls a part of the economy, with substantial government expenditure. The European Union is Croatias most important trading partner, since 2000, the Croatian government constantly invests in infrastructure, especially transport routes and facilities along the Pan-European corridors. Internal sources produce a significant portion of energy in Croatia, the rest is imported, the origin of the name is uncertain, but is thought to be a Gothic or Indo-Aryan term assigned to a Slavic tribe. The oldest preserved record of the Croatian ethnonym *xъrvatъ is of variable stem, the first attestation of the Latin term is attributed to a charter of Duke Trpimir from the year 852. The original is lost, and just a 1568 copy is preserved—leading to doubts over the authenticity of the claim, the oldest preserved stone inscription is the 9th-century Branimir Inscription, where Duke Branimir is styled as Dux Cruatorvm. The inscription is not believed to be dated accurately, but is likely to be from during the period of 879–892, the area known as Croatia today was inhabited throughout the prehistoric period
27.
Krapina Neanderthal site
–
The following tables give a brief overview of several notable hominin fossil finds relating to human evolution beginning with the formation of the Hominini tribe in the late Miocene. Deprecated classifications may be found on the fossils page, most of the fossils shown are not considered direct ancestors to Homo sapiens but are closely related to direct ancestors and are therefore important to the study of the lineage. Westview Press, Boulder CO. ISBN 978-0-8133-3482-0, cS1 maint, Multiple names, authors list Larsen, Clark Spencer, Matter, Robert M, Gebo, Daniel L. CS1 maint, Multiple names, authors list Smithsonian Human Origins Program, schultz, J. Phenetic Affinities Among Early Homo Crania from East and South Africa
28.
Vela Spila
–
The Vela Spila cave, Cree, Vela Spila, Big Cave is situated above the town of Vela Luka on the island of Korčula, in Croatia on Pinski Rat hill at an elevation of approximately 130 m. The cave consists of an elliptically shaped cavern that measures 40 m in length,17 m in height, there are, similar to the Brillenhöhle in Germany, two openings in the roof of the cave which were caused by collapse at an yet undetermined time. Nikola Ostoic was the first person to describe the cave in modern literature, in 1856, he wrote Compendio Storico Dell Isola Di Curzola. A local historian, museum commissioner, and collector of antiquities, the cave has been mentioned in the Korčula Statute back in the 15th century. Scientific research of the started in the late 1940s. Marinko Gjivoje took up work at the site in 1949, in 1951, Marinko Gjivoje, Boris Ilakovac and Vinko Foretic started test excavations and the results were allowed the proposal to proceed. Based on these findings, Grga Novak decided to excavate in order to confirm the caves links with the island of Hvar. The explorations were carried out in September 1951 and he published his preliminary results in the Annals of the Yugoslav Academy. Since 1974, fieldwork were undertaken almost annually, initially led by Grga Novak, franko Oreb is a permanent member of the excavation crew and Dinko Radic joined the excavation in 1986. There is a sequence of sediments from the late Mesolithic to the Neolithic. Radiocarbon dated finds suggest seasonal human presence for hunting and the collection of resources from 20,000 years BC. Three child burials were discovered between 1986 and 1998 in the younger Mesolithic layers, further findings are dated between 13,500 and 12,600 BC. Eneolithic layers account for non-permanent human occupation of the cave, attributed to the Hvar Culture and this period is immediately being followed by a compact layer of the Bronze Age. The archeological finds are on display at the Centre for Culture in Vela Luka, in 2009 National Geographic featured an article about Vela Spila. In 1986, remains of two adults where found, scientific research dated their bodies back to late Neolithic times. The local towns people of Vela Luka called them Baba i Dida, further excavations between 2001 and 2006, produced 36 ceramic artifacts dated to the late Upper Palaeolithic period, about 17,500 to 15,000 years ago. These finds are the examples of ceramic figurative art in southeastern Europe during the Upper Palaeolithic. Croatia Vela Luka Korčula Drakonjina Spilja www. velaspila. hr Archaeologists uncover Palaeolithic ceramic art First Epigravettian Ceramic Figurines from Europe
29.
Vindija Cave
–
Vindija cave is an archaeological site of occupation associated with Neanderthals and modern humans, located in the municipality of Donja Voća, northern Croatia. One of these Neanderthals was selected as primary source of DNA for the Neanderthal genome project, the cave is located roughly 20 km west of the city of Varaždin and 10 km north of Ivanec. It is estimated that Neanderthals lived there about 45, 000-32,000 years ago, Vindija includes a total of 13 levels dated between 150,000 years ago and the present, spanning the upper part of the Lower Paleolithic, Middle Paleolithic and Upper Paleolithic periods. The earliest recognized hominid occupations date to ca and this record of animals in the region has been used to establish data about the climate and habitat of northwest Croatia during that period. The site was first excavated in the first half of the 20th century, there are numerous archaeological and faunal remains with over 100 hominin discoveries that have been found at Vindija Cave. Specimens in Level G3, the lowest hominin-bearing level, are Neanderthals and are associated with exclusively Mousterian artifacts, specimens in Level G1 represent the most recent Neanderthals at the site and are associated with both Mousterian and Upper Paleolithic stone tools. Hominins in Level F are associated with Aurignacian and according to researchers look a little like both AMH and Neanderthal. Hominins in Level D (less than 18,500 years bp, the uppermost hominid-bearing strata in the cave, are associated with Gravettian culture artifacts, and represent only anatomically modern humans. In 2008, researchers reported that a complete mtDNA sequence had been retrieved from a bone of one of the Neanderthals recovered from Vindija Cave. The bone comes from level G3, and it was direct-dated to 38,310 ±2,130 RCYBP and their research suggests that the two hominins who occupied Vindija Cave at different times—early modern Homo sapiens and Neanderthals—were clearly separate species. A recent study reported in Quaternary International describes the data recovered from Vindija Cave. The fauna indicate that during the period between 60,000 and 16,000 years ago, the region had a moderate, broadly temperate climate with a range of environments. In particular, there seems to have no significant evidence for what was thought to be a shift to cooler conditions at the onset of the Last Glacial Maximum. These include a thinner and less projecting brow ridge, reduced facial size, more likely, the Vindija Neanderthals were in transition from the classic robust form to a more gracile one. Neanderthal genome project Peștera cu Oase Marina Biluš, archived from the original on 11 July 2012. Špilja Vindija Video about Vindija on YouTube Dekodiran DNK neandertalca iz špilje Vindija
30.
Cyprus
–
Cyprus, officially the Republic of Cyprus, is an island country in the Eastern Mediterranean and the third largest and third most populous island in the Mediterranean. It is located south of Turkey, west of Syria and Lebanon, northwest of Israel and Palestine, north of Egypt, the earliest known human activity on the island dates to around the 10th millennium BC. Archaeological remains from this include the well-preserved Neolithic village of Khirokitia. Cyprus was settled by Mycenaean Greeks in two waves in the 2nd millennium BC, Cyprus was placed under British administration based on Cyprus Convention in 1878 and formally annexed by Britain in 1914. While Turkish Cypriots made up 18% of the population, the partition of Cyprus and creation of a Turkish state in the north became a policy of Turkish Cypriot leaders, following nationalist violence in the 1950s, Cyprus was granted independence in 1960. On 15 July 1974, a coup détat was staged by Greek Cypriot nationalists and elements of the Greek military junta in an attempt at enosis and these events and the resulting political situation are matters of a continuing dispute. The Cyprus Republic has de jure sovereignty over the island of Cyprus, as well as its territorial sea and exclusive economic area, another nearly 4% of the islands area is covered by the UN buffer zone. The international community considers the part of the island as territory of the Republic of Cyprus occupied by Turkish forces. The occupation is viewed as illegal under law, amounting to illegal occupation of EU territory since Cyprus became a member of the European Union. Cyprus is a major tourist destination in the Mediterranean, on 1 January 2008, the Republic of Cyprus joined the eurozone. The earliest attested reference to Cyprus is the 15th century BC Mycenaean Greek
31.
Czech Republic
–
The Czech Republic, also known as Czechia, is a nation state in Central Europe bordered by Germany to the west, Austria to the south, Slovakia to the east and Poland to the northeast. The Czech Republic covers an area of 78,866 square kilometres with mostly temperate continental climate and it is a unitary parliamentary republic, has 10.5 million inhabitants and the capital and largest city is Prague, with over 1.2 million residents. The Czech Republic includes the territories of Bohemia, Moravia. The Czech state was formed in the late 9th century as the Duchy of Bohemia under the Great Moravian Empire, after the fall of the Empire in 907, the centre of power transferred from Moravia to Bohemia under the Přemyslid dynasty. In 1002, the duchy was formally recognized as part of the Holy Roman Empire, becoming the Kingdom of Bohemia in 1198 and reaching its greatest territorial extent in the 14th century. Following the Battle of Mohács in 1526, the whole Crown of Bohemia was gradually integrated into the Habsburg Monarchy alongside the Archduchy of Austria, the Protestant Bohemian Revolt against the Catholic Habsburgs led to the Thirty Years War. After the Battle of the White Mountain, the Habsburgs consolidated their rule, reimposed Roman Catholicism, the Czech part of Czechoslovakia was occupied by Germany in World War II, and was liberated in 1945 by the armies of the Soviet Union and the United States. The Czech country lost the majority of its German-speaking inhabitants after they were expelled following the war, the Communist Party of Czechoslovakia won the 1946 elections. Following the 1948 coup détat, Czechoslovakia became a one-party communist state under Soviet influence, in 1968, increasing dissatisfaction with the regime culminated in a reform movement known as the Prague Spring, which ended in a Soviet-led invasion. Czechoslovakia remained occupied until the 1989 Velvet Revolution, when the communist regime collapsed, on 6 March 1990, the Czech Socialistic Republic was renamed to the Czech Republic. On 1 January 1993, Czechoslovakia peacefully dissolved, with its constituent states becoming the independent states of the Czech Republic and the Slovak Republic. The Czech Republic joined NATO in 1999 and the European Union in 2004, it is a member of the United Nations, the OECD, the OSCE, and it is a developed country with an advanced, high income economy and high living standards. The UNDP ranks the country 14th in inequality-adjusted human development, the Czech Republic also ranks as the 6th most peaceful country, while achieving strong performance in democratic governance. It has the lowest unemployment rate in the European Union, the traditional English name Bohemia derives from Latin Boiohaemum, which means home of the Boii. The current name comes from the endonym Čech, spelled Cžech until the reform in 1842. The name comes from the Slavic tribe and, according to legend, their leader Čech, the etymology of the word Čech can be traced back to the Proto-Slavic root *čel-, meaning member of the people, kinsman, thus making it cognate to the Czech word člověk. The country has traditionally divided into three lands, namely Bohemia in the west, Moravia in the southeast, and Czech Silesia in the northeast. Following the dissolution of Czechoslovakia at the end of 1992, the Czech part of the former nation found itself without a common single-word geographical name in English, the name Czechia /ˈtʃɛkiə/ was recommended by the Czech Ministry of Foreign Affairs
