1.
Summit
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A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. Mathematically, a summit is a maximum in elevation. The topographic terms acme, apex, peak, and zenith are synonymous, the UIAA definition is that a summit is independent if it has a prominence of 30 metres or more, it is a mountain if it has a prominence of at least 300 metres. This can be summarised as follows, A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top, Summit may also refer to the highest point along a line, trail, or route. In many parts of the western United States, the term refers to the highest point along a road, highway. For example, the highest point along Interstate 80 in California is referred to as Donner Summit while the highest point on Interstate 5 is Siskiyou Mountain Summit, geoid Hill List of highest mountains Maxima and minima Nadir Summit accordance Peak finder
2.
Crimea
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The peninsula is located south of the Ukrainian region of Kherson and west of the Russian region of Kuban. It is connected to Kherson Oblast by the Isthmus of Perekop and is separated from Kuban by the Strait of Kerch, the Arabat Spit is located to the northeast, a narrow strip of land that separates a system of lagoons named Sivash from the Sea of Azov. Crimea has historically been at the boundary between the world and the Pontic–Caspian steppe. Crimea and adjacent territories were united in the Crimean Khanate during the 15th to 18th century, in 1783, Crimea was annexed by the Russian Empire. It became the Autonomous Republic of Crimea within newly independent Ukraine in 1991, with Sevastopol having its own administration, within Ukraine, the ex-Soviet Black Sea Fleet and its facilities were divided between Russias Black Sea Fleet and the Ukrainian Naval Forces. The two navies shared some of the harbours and piers, while others were demilitarised or used by either country. Sevastopol remained the location of the Russian Black Sea Fleet headquarters with the Ukrainian Naval Forces Headquarters also based in the city, most of the international community does not recognize the annexation and considers Crimea to be Ukrainian territory. Russia currently administers the peninsula as two federal subjects, the Republic of Crimea and the city of Sevastopol. Ukraine continues to assert its right over the peninsula, the classical name Tauris or Taurica is from the Greek Ταυρική, after the peninsulas Scytho-Cimmerian inhabitants, the Tauri. In English usage since the modern period the Crimean Khanate is referred to as Crim Tartary. The Italian form Crimea also becomes current during the 18th century, the omission of the definite article in English became common during the later 20th century. The name Crimea follows the Italian form from the Crimean Tatar name for the city Qırım which served as a capital of the Crimean province of the Golden Horde, the name of the capital was extended to the entire peninsula at some point during Ottoman suzerainty. The origin of the word Qırım is uncertain, suggestions argued in various sources include, a corruption of Cimmerium. A derivation from the Turkic term qirum, from qori-, other suggestions that have not been supported by sources but are apparently based on similarity in sound include, a derivation from the Greek Cremnoi. However, he identifies the port, not in Crimea, no evidence has been identified that this name was ever in use for the peninsula. The classical name was revived in 1802 in the name of the Russian Taurida Governorate, in the 8th century BCE the Cimmerians migrated to the region and subsequently the Scythians as well it being the site of Greek colonies. The most important city was Chersonesos at the edge of todays Sevastopol, the Persian Achaemenid Empire expanded to Crimea. Later occupiers included the Romans, Goths, Huns, Bulgars, the Byzantine Empire, Khazars, the Kipchaks, the Golden Horde, consideration of the succeeding residents of the peninsula by their linguistic grouping is also of relevance
3.
Cretaceous
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The Cretaceous is a geologic period and system that spans 79 million years from the end of the Jurassic Period 145 million years ago to the beginning of the Paleogene Period 66 Mya. It is the last period of the Mesozoic Era, the Cretaceous Period is usually abbreviated K, for its German translation Kreide. The Cretaceous was a period with a warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites and rudists, during this time, new groups of mammals and birds, as well as flowering plants, appeared. The Cretaceous ended with a mass extinction, the Cretaceous–Paleogene extinction event, in which many groups, including non-avian dinosaurs, pterosaurs. The end of the Cretaceous is defined by the abrupt Cretaceous–Paleogene boundary, the name Cretaceous was derived from Latin creta, meaning chalk. The Cretaceous is divided into Early and Late Cretaceous epochs, or Lower and Upper Cretaceous series, in older literature the Cretaceous is sometimes divided into three series, Neocomian, Gallic and Senonian. A subdivision in eleven stages, all originating from European stratigraphy, is now used worldwide, in many parts of the world, alternative local subdivisions are still in use. As with other geologic periods, the rock beds of the Cretaceous are well identified. No great extinction or burst of diversity separates the Cretaceous from the Jurassic and this layer has been dated at 66.043 Ma. A140 Ma age for the Jurassic-Cretaceous boundary instead of the usually accepted 145 Ma was proposed in 2014 based on a study of Vaca Muerta Formation in Neuquén Basin. Víctor Ramos, one of the authors of the study proposing the 140 Ma boundary age sees the study as a first step toward formally changing the age in the International Union of Geological Sciences, due to the high sea level there was extensive space for such sedimentation. Because of the young age and great thickness of the system. Chalk is a type characteristic for the Cretaceous. It consists of coccoliths, microscopically small calcite skeletons of coccolithophores, the group is found in England, northern France, the low countries, northern Germany, Denmark and in the subsurface of the southern part of the North Sea. Chalk is not easily consolidated and the Chalk Group still consists of sediments in many places. The group also has other limestones and arenites, among the fossils it contains are sea urchins, belemnites, ammonites and sea reptiles such as Mosasaurus. In southern Europe, the Cretaceous is usually a marine system consisting of competent limestone beds or incompetent marls
4.
Mountain range
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A mountain range is a geographic area containing numerous geologically related mountains. A mountain system or system of ranges, sometimes is used to combine several geological features that are geographically related. Mountain ranges are usually segmented by highlands or mountain passes and valleys, individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, most geologically young mountain ranges on the Earths land surface are associated with either the Pacific Ring of Fire or the Alpide Belt. The Andes is 7,000 kilometres long and is considered the worlds longest mountain system. The Alpide belt includes Indonesia and southeast Asia, through the Himalaya, the belt also includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, mountain ranges outside of these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Altai Mountains and the Hijaz Mountains. If the definition of a range is stretched to include underwater mountains. The mountain systems of the earth are characterized by a tree structure, the sub-range relationship is often expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains, equivalently, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, and the White Mountains and the Blue Ridge Mountains are children of the Appalachians. The position of mountains influences climate, such as rain or snow, when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the side, it warms again and is drier. Often, a shadow will affect the leeward side of a range. Mountain ranges are constantly subjected to forces which work to tear them down. Erosion is at work while the mountains are being uplifted and long after until the mountains are reduced to low hills, rivers are traditionally believed to be the principle erosive factor on mountain ranges, with their ability of bedrock incision and sediment transport. The rugged topography of a range is the product of erosion. The basins adjacent to a mountain range are filled with sediments which are buried and turned into sedimentary rock. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example and this mass of rock was removed as the range was actively undergoing uplift
5.
Steppe
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In South Africa they are referred to as Veld. The prairie is an example of a steppe, though it is not usually called such and it may be semi-desert, or covered with grass or shrubs or both, depending on the season and latitude. The term is used to denote the climate encountered in regions too dry to support a forest. The soil is typically of chernozem type, steppes are usually characterized by a semi-arid and continental climate. Extremes can be recorded in the summer of up to 45 °C and in winter, besides this huge difference between summer and winter, the differences between day and night are also very great. In the highlands of Mongolia,30 °C can be reached during the day with sub-zero °C readings at night, the mid-latitude steppes can be summarized by hot summers and cold winters, averaging 250–510 mm of precipitation per year. Precipitation level alone is not what defines a steppe climate, potential evapotranspiration must also be taken into account, the Eurasian Grass-Steppe of the temperate grasslands, savannas, and shrublands had a role in the spread of the horse, the wheel, and the Indo-European languages. The Indo-European expansion and diverse invasions of horse archer civilizations of the steppe eventually led to, the Pannonian Plain is another steppe region in eastern Europe, primarily Hungary. Another large steppe area is located in the central United States, western Canada, the shortgrass prairie steppe is the westernmost part of the Great Plains region. The Channeled Scablands in Southern British Columbia and Washington State is an example of a region in North America outside of the Great Plains. In South America, cold steppe can be found in Patagonia, relatively small steppe areas can be found in the interior of the South Island of New Zealand. In Asia, a subtropical steppe can be found in semi-arid lands that fringe the Thar Desert of the Indian subcontinent, in Australia, subtropical steppe can be found in a belt surrounding the most severe deserts of the continent and around the Musgrave Ranges. Ecology and Conservation of Steppe-land Birds by Manuel B. Morales, Santi Mañosa, Jordi Camprodón, international Symposium on Ecology and Conservation of steppe-land birds
6.
Yalta
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Yalta is a resort city on the south coast of the Crimean Peninsula surrounded by the Black Sea. It serves as the center of Yalta Municipality, one of the regions within Crimea. The city is located on the site of an ancient Greek colony and it is situated on a deep bay facing south towards the Black Sea, surrounded by the mountain range Ai-Petri. It has a humid subtropical climate and surrounded by numerous vineyards and orchards. The existence of Yalta was first recorded in the 12th century by an Arab geographer and it became part of a network of Genoese trading colonies on the Crimean coast in the 14th century, when it was known as Etalita or Galita. Yalta was annexed by the Russian Empire in 1783, along with the rest of Crimea, sparking the Russo-Turkish War, prior to the annexation of the Crimea, the Crimean Greeks were moved to Mariupol in 1778, one of the villages they established nearby is also called Yalta. In the 19th century, the became a fashionable resort for the Russian aristocracy. The town was closely associated with royalty. In 1889 Tsar Alexander III finished construction of Massandra Palace a short distance to the north of Yalta, during the 20th century Yalta was the principal holiday resort of the Soviet Union. Numerous workers sanatoria were constructed in and around Yalta and the surrounding district, there were, in fact, few other places that Soviet citizens could come for a seaside holiday, as foreign travel was forbidden to all but a handful. The Soviet elite also came to Yalta, the Soviet premier Joseph Stalin used the Massandra Palace as his summer residence, Yalta was occupied by the German Army from 9 November 1941 to 16 April 1944. The town came to attention in 1945 when the Yalta Conference between the Big Three powers – the Soviet Union, the United States and the United Kingdom – was held at the Livadia Palace. Following the dissolution of the Soviet Union in 1991, Yalta has struggled economically, the towns transport links have been significantly reduced with the end of almost all passenger traffic by sea. The longest trolleybus line in Europe goes from the station in Simferopol to Yalta. Yalta is crowded in the season and prices for accommodation are very high. Most of the tourists are from countries of the former Soviet Union, in 2013, Yalta has a beautiful embankment along the Black Sea. People can be seen strolling there all seasons of the year, there are several beaches to the east and west of the embankment. The town has several theaters, a drama theater, plenty of restaurants
7.
Chatyr-Dag
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Chatyr-Dah is a mountainous massif in Crimea, near Simferopol-Alushta highway. In the Crimean Tatar language çatır means tent and dağ means mountain, the mountain consists of two plateaus, the lower and the upper. The lower plateau slopes gently down to its side, which is covered in steppe grass. On its southern end, the plateau is covered with beech forests. It has many hiking trails and several beautiful caves, on the east side of the lower plateau there is a grove of yews. The upper plateau has the shape of a giant bowl and on its rim, the upper plateau is covered with alpine meadows. Its slopes are steep and offer some routes for multipitch climbing. Marble Caves Emine Bair Hosar cave Fur-tree cave Obvalnaya cave Vyalova cave Artuch-Koba Vyalova cave system Mangup The Valley Of Ghosts Kara Dag Mountain
8.
Ai-Petri
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Ai-Petri, is a peak in the Crimean Mountains. For administrative purposes it is in the Yalta municipality of Crimea, the name has Greek origin, and is translated as St. Peter. Ai-Petri is one of the windiest places in Crimea, the wind blows for 125 days a year, reaching a speed of 50 m/s. The peak is located above the city of Alupka and the town of Koreiz, there is a cable car that takes passengers from a station near Alupka to the main area in Ai-Petri
9.
Alushta
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Alushta is a city of regional significance on the southern coast of the Autonomous Republic of Crimea in Ukraine claimed by Russia as the Republic of Crimea. It serves as the center of Alushta Municipality, one of the regions Crimea is divided into. Founded in the 6th century AD by Emperor Justinian, today it is a resort town and it is situated at the Black Sea beach line on the road from Hurzuf to Sudak, as well as on the Crimean Trolleybus line. The area is notable for its arid, rocky terrain due to its proximity to Crimean mountains, during Byzantine times the town was called Alouston meaning Unwashed. Vestiges survive of a Byzantine defensive tower from a fortress of which the city name has derived, during the Genoese rule the name modified to Lusta. Adam Mickiewicz dedicated two of his Crimean Sonnets to Alushta and it is also the home of Seyit the Wolf in the Turkish drama Kurt Seyit ve Sura. In 1910,544 Jews lived in Alushta, consisting about 13% of the town population, in 1939, they consisted only 2. 3% of the town overall population, numbering 251 individuals. On 4 November 1941, the Germans occupied the town and on 24 November 1941, in early December 1941, about 250 Jews from Alushta were shot to death by sonderkommando 11b in the park of trade union sanatorium no. 7, which is today in the center for children. Alushta is twinned with, Santa Cruz, United States Dzierżoniów, Poland Äänekoski, Central Finland Jūrmala, Latvia
10.
Anatomically modern human
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Anatomically modern humans evolved from archaic humans in the Middle Paleolithic, about 200,000 years ago. The emergence of modern human marks the dawn of the species Homo sapiens. Other fossils include the proposed Homo sapiens idaltu from Herto in Ethiopia that are almost 160,000 years old and the Skhul hominids from Israel, which are 90,000 years old. The oldest human remains from which an entire genome has been extracted belongs to Ust-Ishim man, however, it can and has been argued that Homo sapiens have been fully capable of modern behavior from the time they first evolved. The binomial name for the species of the human population is Homo sapiens. The species is taken to have emerged from a predecessor within the Homo genus around 200,000 years ago. Generally, modern humans are more lightly built than archaic humans from which they have evolved, Humans are a highly variable species, modern humans can show remarkably robust traits, and early modern humans even more so. Despite this, modern humans differ from archaic people in a range of anatomical details, the cranium lacks a pronounced occipital bun in the neck, a bulge that anchored considerable neck muscles in Neanderthals. Modern humans, even the ones, generally have a larger fore-brain than the archaic people. This will usually give a higher forehead, and reduced brow ridge and this splits the ridge into a central part and two distal parts. In current humans, often only the section of the ridge is preserved. This contrasts with archaic humans, where the ridge is pronounced. Modern humans commonly have a steep, even vertical forehead whereas their predecessors had foreheads that sloped strongly backwards, according to Desmond Morris, the vertical forehead in humans not only houses larger brains, but plays an important role in human communication through eyebrow movements and forehead skin wrinkling. Compared to archaic people, anatomically modern humans have smaller, differently shaped teeth and this results in a smaller, more receded dentary, making the rest of the jaw-line stand out, giving an often quite prominent chin. The central part of the forming the chin carries a triangularly shaped area forming the apex of the chin called the mental trigon. Particularly in living population, the use of fire and tools require fewer jaw muscles, giving slender, compared to archaic people, modern humans have smaller, lower faces. The body skeletons of even the earliest and most robustly built modern humans were less robust than those of Neanderthals, particularly regarding the long bones of the limbs, the distal bones are nearly the same size or slightly shorter than the proximal bones. In ancient people, particularly Neanderthals, the bones were shorter
