1.
Provinces of Turkey
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Turkey is divided into 81 provinces. Each province is divided into a number of different districts, the provincial government is seated in the central district. The central area usually bears the name of the province, there are only two exceptions to this naming scheme, Antakya of Hatay province İzmit of Kocaeli province A province is administered by an appointed governor from the ministry of interior. Below is a list of the 81 provinces of Turkey, sorted according to their license plate code, after Zonguldak the ordering is not alphabetical but in the order of the creation of provinces, as these provinces were created more recently and thus their plate numbers were assigned thereafter. The numbers of the ISO code, the first two digits of the registration plates of Turkey and the first digits of the postal codes in Turkey are the same
2.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
3.
Turkey
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Turkey, officially the Republic of Turkey, is a transcontinental country in Eurasia, mainly in Anatolia in Western Asia, with a smaller portion on the Balkan peninsula in Southeast Europe. Turkey is a democratic, secular, unitary, parliamentary republic with a cultural heritage. The country is encircled by seas on three sides, the Aegean Sea is to the west, the Black Sea to the north, and the Mediterranean Sea to the south. The Bosphorus, the Sea of Marmara, and the Dardanelles, Ankara is the capital while Istanbul is the countrys largest city and main cultural and commercial centre. Approximately 70-80% of the countrys citizens identify themselves as ethnic Turks, other ethnic groups include legally recognised and unrecognised minorities. Kurds are the largest ethnic minority group, making up approximately 20% of the population, the area of Turkey has been inhabited since the Paleolithic by various ancient Anatolian civilisations, as well as Assyrians, Greeks, Thracians, Phrygians, Urartians and Armenians. After Alexander the Greats conquest, the area was Hellenized, a process continued under the Roman Empire. The Seljuk Sultanate of Rûm ruled Anatolia until the Mongol invasion in 1243, the empire reached the peak of its power in the 16th century, especially during the reign of Suleiman the Magnificent. During the war, the Ottoman government committed genocides against its Armenian, Assyrian, following the war, the conglomeration of territories and peoples that formerly comprised the Ottoman Empire was partitioned into several new states. Turkey is a member of the UN, an early member of NATO. Turkeys growing economy and diplomatic initiatives have led to its recognition as a regional power while her location has given it geopolitical, the name of Turkey is based on the ethnonym Türk. The first recorded use of the term Türk or Türük as an autonym is contained in the Old Turkic inscriptions of the Göktürks of Central Asia, the English name Turkey first appeared in the late 14th century and is derived from Medieval Latin Turchia. Similarly, the medieval Khazar Empire, a Turkic state on the shores of the Black. The medieval Arabs referred to the Mamluk Sultanate as al-Dawla al-Turkiyya, the Ottoman Empire was sometimes referred to as Turkey or the Turkish Empire among its European contemporaries. The Anatolian peninsula, comprising most of modern Turkey, is one of the oldest permanently settled regions in the world, various ancient Anatolian populations have lived in Anatolia, from at least the Neolithic period until the Hellenistic period. Many of these peoples spoke the Anatolian languages, a branch of the larger Indo-European language family, in fact, given the antiquity of the Indo-European Hittite and Luwian languages, some scholars have proposed Anatolia as the hypothetical centre from which the Indo-European languages radiated. The European part of Turkey, called Eastern Thrace, has also been inhabited since at least forty years ago. It is the largest and best-preserved Neolithic site found to date, the settlement of Troy started in the Neolithic Age and continued into the Iron Age
4.
NUTS statistical regions of Turkey
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As a candidate country of the European Union, Turkey is included in the Nomenclature of Territorial Units for Statistics. Interactive map of statistics indicators by NUTS levels
5.
Electoral system of Turkey
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The Electoral system of Turkey varies for general, presidential and local elections that take place in Turkey every four years, five years and five years respectively. Turkey has been a multi-party democracy since 1950, with the first democratic election held on 14 May 1950 leading to the end of the single-party rule established in 1923. The current electoral system for electing Members of Parliament to the Grand National Assembly has a 10% election threshold, the highest of any country. Presidential elections, A Two-round system, with the top two contesting a run-off election two weeks after the initial election should no candidate win at least 50%+1 of the popular vote. Turkey elects 550 Members of Parliament to the Grand National Assembly using the DHondt method, E. g. in the 2002 general election the AKP won 34. 28% of the vote but won nearly two-thirds of the seats. This was the case in the 2007 and 2011 general election, where the Kurdish Democratic Society Party, the main criticism of the current system is the high 10% threshold necessary to gain seats. Under these proposals, the threshold would fall from 10% to either 7 or 8% while Turkey would be split into 129 electoral districts rather than the existing 85, İstanbul itself would have been split into 17 or 20 districts. The two main opposition parties CHP and MHP do not have a number of electoral strongholds. The AKPs proposals for reform have raised concerns about gerrymandering, Turkey is split into 85 electoral districts, which elect a certain number of Members to the Grand National Assembly of Turkey. The Grand National Assembly has a total of 550 seats, which each district allocated a certain number of MPs in proportion to their population. The Supreme Electoral Council of Turkey conducts population reviews of each district before the election, in all but three cases, electoral districts share the same name and borders of the 81 Provinces of Turkey. The exceptions are İzmir, İstanbul and Ankara, Provinces electing between 19 and 36 MPs are split into two electoral districts, while any province electing above 36 MPs are divided into three. As the countrys three largest provinces, İzmir and Ankara are divided into two subdistricts while İstanbul is divided into three, the distribution of elected MPs per electoral district is shown below. A total of eight districts had their number of MPs adjusted since the 2011 general election by the electoral council. The two electoral districts of Ankara also had their boundaries changed, the number of voters in each province was announced on 17 May 2015. In total, there are 53,741,838 voters in the provinces, however, because of the electoral system, this was not distributed equally to the provinces. In İzmir, where voters per MP was the highest,118,669 votes corresponded to an MP, two factors caused this more than fourfold disparity. Namely, the electoral law favours provinces smaller in size, which caused İzmir, İstanbul and Ankara, Turkeys largest cities and provinces, to have the least representation per voter
6.
Vehicle registration plate
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A vehicle registration plate, also known as a number plate or a license plate, is metal or plastic plate attached to a motor vehicle or trailer for official identification purposes. The registration identifier is a numeric or alphanumeric ID that uniquely identifies the owner within the issuing regions database. The first two letters indicate the state to which the vehicle is registered, the next two digit numbers are the sequential number of a district. Due to heavy volume of vehicle registration, the numbers were given to the RTO offices of registration as well, the third part indicates the year of registration of the vehicle and is a 4 digit number unique to each plate. In some countries, the identifier is unique within the entire country, whether the identifier is associated with a vehicle or a person also varies by issuing agency. In the vast majority of jurisdictions, the government holds a monopoly on the manufacturing of vehicle registration plates for that jurisdiction. Thus, it is illegal for private citizens to make and affix their own plates. Alternately, the government will merely assign plate numbers, and it is the owners responsibility to find an approved private supplier to make a plate with that number. In some jurisdictions, plates will be assigned to that particular vehicle for its lifetime. If the vehicle is destroyed or exported to a different country. Other jurisdictions follow a policy, meaning that when a vehicle is sold the seller removes the current plate from the vehicle. Buyers must either obtain new plates or attach plates they already hold, as well as register their vehicles under the buyers name, a person who sells a car and then purchases a new one can apply to have the old plates put onto the new car. One who sells a car and does not buy a new one may, depending on the laws involved, have to turn the old plates in or destroy them. Some jurisdictions permit the registration of the vehicle with personal plates, in some jurisdictions, plates require periodic replacement, often associated with a design change of the plate itself. Vehicle owners may or may not have the option to keep their original plate number, alternately, or additionally, vehicle owners have to replace a small decal on the plate or use a decal on the windshield to indicate the expiration date of the vehicle registration. Plates are usually fixed directly to a vehicle or to a frame that is fixed to the vehicle. Sometimes, the plate frames contain advertisements inserted by the service centre or the dealership from which the vehicle was purchased. Vehicle owners can also purchase customized frames to replace the original frames, in some jurisdictions licence plate frames are illegal
7.
Turkish language
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Outside of Turkey, significant smaller groups of speakers exist in Germany, Bulgaria, Macedonia, Northern Cyprus, Greece, the Caucasus, and other parts of Europe and Central Asia. Cyprus has requested that the European Union add Turkish as an official EU language, in 1928, as one of Atatürks Reforms in the early years of the Republic of Turkey, the Ottoman Turkish alphabet was replaced with a Latin alphabet. The distinctive characteristics of Turkish are vowel harmony and extensive agglutination, the basic word order of Turkish is subject–object–verb. Turkish has no classes or grammatical gender. Turkish has a strong T–V distinction and usage of honorifics, Turkish uses second-person pronouns that distinguish varying levels of politeness, social distance, age, courtesy or familiarity toward the addressee. The plural second-person pronoun and verb forms are used referring to a person out of respect. Turkic languages belong to the Altaic language group, the Turkic family comprises some 30 living languages spoken across Eastern Europe, Central Asia, and Siberia. Turkish is a member of the Oghuz group of languages, a subgroup of the Turkic language family, there is a high degree of mutual intelligibility between Turkish and the other Oghuz Turkic languages, including Azerbaijani, Turkmen, Qashqai, Gagauz, and Balkan Gagauz Turkish. The earliest known Old Turkic inscriptions are the three monumental Orkhon inscriptions found in modern Mongolia, erected in honour of the prince Kul Tigin and his brother Emperor Bilge Khagan, these date back to the second Turk Kaghanate. The Seljuqs of the Oghuz Turks, in particular, brought their language, following the adoption of Islam c. Turkish literature during the Ottoman period, particularly Divan poetry, was influenced by Persian, including the adoption of poetic meters. One of the tasks of the newly established association was to initiate a reform to replace loanwords of Arabic. By banning the usage of imported words in the press, the association succeeded in removing several hundred words from the language. While most of the words introduced to the language by the TDK were newly derived from Turkic roots, owing to this sudden change in the language, older and younger people in Turkey started to differ in their vocabularies. While the generations born before the 1940s tend to use the terms of Arabic or Persian origin. The past few decades have seen the work of the TDK to coin new Turkish words to express new concepts and technologies as they enter the language. Many of these new words, particularly information technology terms, have received widespread acceptance, however, the TDK is occasionally criticized for coining words which sound contrived and artificial. Some earlier changes—such as bölem to replace fırka, political party—also failed to meet with popular approval, some words restored from Old Turkic have taken on specialized meanings, for example betik is now used to mean script in computer science
8.
Eastern Anatolia Region
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The Eastern Anatolia Region is a geographical region of Turkey. The region and the name Doğu Anadolu Bölgesi were first defined at the First Geography Congress in 1941 and it has the highest average altitude, largest geographical area, and lowest population density of all regions of Turkey. Prior to getting its current name by the Turkish state, most of the region was part of the Six Armenian provinces in the known as the Armenian Highlands. After the Armenian Genocide, the geopolitical term Eastern Anatolia was created to replace what had historically been known as Western Armenia, starting from 1880 the name Armenia was forbidden to be used in official Ottoman documents. The government of Sultan Abdul Hamid II replaced the name Armenia with such terms as Kurdistan or Anatolia, the Sublime Porte was trying to cover up the Armenian Question, if there was no Armenia, then there was no Armenian Question. The process of “nationalization” of toponyms was continued by the Kemalists, who were the successors of the Young Turks. Starting from 1923 the entire territory of Western Armenia was officially renamed “Eastern Anatolia”, in the 17th century when the Armenian Question was not as yet included into the international diplomacy agenda, the terms Anatolia or Eastern Anatolia were never used to indicate Armenia. Furthermore, the Islamic World Map of the 16th century and other Ottoman maps of the 18th and 19th centuries have clearly indicated Armenia on a territory as well as its cities. Armenia, together with its boundaries, was mentioned in the works of earlier Ottoman historians. Kâtip Çelebi, a famous Ottoman chronicler of the 17th century, had a chapter titled “About the Country Called Armenia” in his book Jihan Numa. When, however, this book was republished in 1957, its modern Turkish editor H. Selen changed this title into “Eastern Anatolia”. Osman Nuri, a historian of the half of the 19th century, mentions Armenia repeatedly in his three-volume Abdul Hamid. The word Anatolia means “sunrise” or “east” in Greek and this name was given to the Asia Minor peninsula approximately in the 5th or 4th centuries B. C. During the Ottoman era, the term Anadolou included the vilayets of Asia Minor with Kyotahia as its center. The numerous European, Ottoman, Armenian, Russian, Persian, Arabic and this testifies, inter alia, to the fact that even after the loss of its statehood the Armenian nation still constituted a majority in its homeland, which was recognized by Ottoman occupiers as well. The area of the region is 146,330 km², which comprises 18. 7% of the area of Turkey. The total population of the region is 6,100,000 and 5,906,565, the region has the second most rural population of Turkey after the Black Sea region. The migration level is high and population density is lower than the average for Turkey, the migration toward other Turkeys regions and toward foreign countries is higher than the natural population increase, a fact which is leading to a slight decline of the Regions population
9.
Kars Province
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Kars Province is a province of Turkey, located in the northeastern part of the country. It shares part of its border with the Republic of Armenia. The provincial capital is the city of Kars, the provinces of Ardahan and Iğdır were until the 1990s part of Kars Province. In ancient times, Kars was part of the province of Ararat in the Kingdom of Armenia, the first known people were the followers of Vanand, for whom Kars was their main settlement and fortress. In 928, Kars became the capital of Armenia, in 968, the capital of Armenia was moved to Ani, but Kars remained the capital of the feudal principality of Vanand. Later on, in 1209, Georgian army commanded by David Soslan and brothers Ivane, as a result of the Russo-Turkish War of 1877 to 1878, the province of Kars was incorporated into the Russian Empire as part of the militarily administered Kars Oblast and remained so until 1918. It was seen as a province of a Russian Empire which was seeking to expand yet further by the conquest of more territory belonging to the Ottoman Empire. Many from the non-Russian Christian Orthodox communities had fought in or collaborated with the Russian Imperial army to capture Kars province from the Muslim Ottomans. They saw this as a means of fulfilling their own ambitions to recapture Christian territory on the back of the Russian imperial enterprise, turkish and Caucasian peoples make up the majority of the provinces population. It is suggested that about 20% of the population is Kurdish, Kars province is divided into 8 districts, each named after the administrative center of the district, There are 383 villages in Kars. Kars has a wealth of wildlife that is being documented by the Kars-Igdir Biodiversity Project run by the KuzeyDoga Society, the project has recorded 323 of Turkeys 468 bird species in the region. At least 223 of these occur at Lake Kuyucuk, that is the most important wetland in the region. Sarikamis Forests in the south harbor Indian wolves, Syrian brown bear, Caucasian lynx and other animals, Aras River Bird Research and Education Center at Yukari Ciyrikli village has recorded 228 bird species at this single location alone. The economy of Kars Province is dominated by agriculture, livestock breeding, 85% of the active population in Kars Province are farmers or herders. 60% of the domestic income is received from those sectors. Industry, tourism and commerce is developing, the climate limits the cultivation of plants in the region. In Kağızman and Tuzluca, cotton, sugar beet, beans, vegetable gardening and orchards are not very developed. Wheat, barley, cotton and in small quantity tobacco are grown in the province, livestock breeding in the region is more important than agriculture
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Bayburt Province
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Bayburt Province is a province in the north-east of Turkey. Population of the province is 74,412 and total area is 3,652 km², bayburt is traversed by the northeasterly line of equal latitude and longitude
11.
Rize Province
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Rize Province is a province of north-east Turkey, on the eastern Black Sea coast between Trabzon and Artvin. The province of Erzurum is to the south and it was formerly known as Lazistan, the designation of the term of Lazistan was officially banned in 1926, by Kemalists. Its capital is the city of Rize, the province is home to Laz, Hemshin, Turkish people and Georgian communities. The name comes from Greek ρίζα, meaning mountain slopes, the Georgian name is Rize, Laz name is Rizini and the Armenian name is Rize. Rize is located between the Pontic Mountains and the Black Sea and it is considered to be the wettest corner of Turkey and is the countrys main tea producing region. In addition to tea, the region is known for growing kiwi fruit. The province is rural and very scenic, containing many mountain valleys. The district of Çamlıhemşin is one of Turkeys most popular venues for trekking, the new Black Sea coast road has made Rize more accessible, but has drawn criticism for its negative effect on the regions wildlife. Since the early 2000s, Rize has seen an increase in visitors from outside the province and this increase in tourism has raised concerns among locals that the traditional way of life and the unblemished character of the natural surroundings is being endangered. Native plants include the Cherry Laurel, the fruit of which is a small dark plum that leaves a dark stain on the mouth and teeth. In addition, the Bilberry, which are now being actively cultivated, Rize is traversed by the northeasterly line of equal latitude and longitude. Valleys first appeared during the Cretaceous period and have expanded due to erosion. The regions climate is characterized by high temperatures and evenly distributed precipitation throughout the year. The Köppen Climate Classification subtype for this climate is Cfa and we have little information as to the prehistory of this region, which being covered in thick forest is difficult to excavate and reveals little. Qulha or Kolkhis which existed from the c, then in 714 BC a tribe of Cimmerians came to settle by the Çoruh River, fleeing as their homeland in the Caucasus was overrun by the Saka branch of the Scythians. The Cimmerians spread throughout Anatolia and still there are many places named Kemer as a record of their presence. Later the Persian armies were defeated by Alexander the Great, following the death of Alexander a number of separate kingdoms were established in Anatolia including Bithynia and Cappadoccia and in this corner of the eastern Black Sea, Pontus. Rize was brought into the Kingdom of Pontus by Pharnaces in 180 BC, the kingdom was absorbed into the Roman Empire between 10 AD and 395 AD, when it passed to the Byzantines
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Artvin Province
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Artvin Province is a province in Turkey, on the Black Sea coast in the north-eastern corner of the country, on the border with Georgia. The provincial capital is the city of Artvin, the weather in Artvin is very wet and mild at the coast, and as a result is heavily forested. This greenery runs from the top all the way down to the Black Sea coast, the rain turns to snow at higher altitudes, and the peaks are very cold in winter. The forests are home to bears and wolves. The Çoruh is now being dammed in 11 places for hydro-electric power, including the 249 m Deriner Dam and others at Borçka, in addition to the vast majority ethnic Turks, the province is home to communities of Laz people and Hemshin peoples. Autochthonous Muslim Georgians form the majority in parts of Artvin Province east of the Çoruh River, immigrant groups of Georgian origins, found scattered in Turkey are known as Chveneburi. With such diverse peoples, Artvin has a variety of folk song. Local industries include bee-keeping especially in Macahel region, Artvin is traversed by the northeasterly line of equal latitude and longitude. The city of Artvin has an ancient castle and a number of Ottoman period houses, mosques, every June, there is a bull-wrestling festival in the high plateau of Kafkasör The Parekhi monastery, a Georgian monastery Popular places for walking and outdoor expeditions. The Kaçkar Mountains are among the venues for trekking holidays in Turkey. Macahel Valley on the Georgian border, is popular location for walking holidays. Papart forest in Şavşat Genciyan Hill in Şavşat, overlooks the border, the lakes of Şavşat and Borçka and the crater lake of Kuyruklu. The Çoruh River is excellent for rafting and championships have been held here There are a number of Georgian churches in the valleys of Yusufeli, bilbilan Yaylası - a typical Turkish high meadow. Savangin pre-historical cave with a written in an unknown or unsolved alphabet The singer. Folk rock singer, guitarist and composer Kazım Koyuncu was born in Artvins Black Sea town of Hopa, the bard of Artvin, poet Turgut Çelik Folk singer Şükriye Tutkun The father of TV personality Beyaz was from a village in Ardanuç. The singer, composer and engineer Mircan Kaia was born into a family from Borcka, in 1924, the Liva Sanjak was abolished and the Artvin Vilayet was created. Artvin Vilayet was combined with Rize to form Çoruh Vilayet with the capital at Rize, later it was separated into Artvin Province with the districts of Ardanuç, Arhavi, Artvin, Borçka, Hopa, Murgul, Şavşat and Yusufeli. Photos of Artvin HQ pictures of Artvin more photos World Wildlife Fund report on the area photos and villages of Artvin
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Ardahan Province
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Ardahan Province, is a province in the north-east of Turkey, at the very end of the country, where Turkey borders with Georgia. The provincial capital is the city of Ardahan, Ardahan province is located in the far north east of Turkey, where the eastern extremity of the high plateau of Eastern Anatolia converges with the Lesser Caucasus mountain range. It is consequently an area of high altitude and severe winters. This is attractive open countryside which however spends many months of the year under snow, at this altitude temperatures on average reach −20 °C and can drop below freezing all year round, including summer months. The local economy depends on farming and raising livestock, the Turkish military have a strong presence in this border district, another boost to the local economy. Smaller locales, districts, villages and a significant portion of the landscape, exhibits a true subarctic climate, Ardahan is an impoverished area that since the 1950s has seen a large number of its people migrate to other parts of Turkey or abroad. The population declined from 170,000 people in 1990 to 119,000 in 2000, the population is 105,454 as of 2010. Ethnic groups in the include, Turks, Georgians, Turkmens, Kurds. They were removed in the Treaty of Kars due to their Christian religion, in 680 BC Scythians came across the Caucasus from the north and captured this area from the Urartu Kings that ruled from their capital on the shores of Lake Van to the south. The Scythians were replaced by Persians and then in 330 BC Alexander the Great came through with his armies, in 1878, after the Russo-Turkish War, the region was incorporated into the Russian Empire, and until 1918 was known as Kars Oblast. Part of the Democratic Republic of Georgia from 1918 to 1921, the construction of the Baku–Tbilisi–Ceyhan pipeline gave the local economy a brief boost from 2000 onwards. Ardahan province is divided into 6 districts, Ardahan Çıldır Damal Göle Hanak Posof Ardahan City 17,171 inh, There are a number of medieval castles in the district including Ardahan Castle itself. Lake Çıldır Phantom of Atatürk in city of Damal There is a unique natural incident, between mid of June and mid July during sunset, depending on angles of sun xrays and it was first seen by a shepherd who was with his herd over the hill. List of populated places in Ardahan Province
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Tortum
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Tortum is a town and district of Erzurum Province in the Black Sea region of Turkey. The population is 4,507 as of 2010. There are 4 different ethnic group in the district. Ethnicity distribution Turkish Hemshin Kurdish Circassians Tortum was part of the known as Upper Tao and was ruled by Romans, Persians, Georgians, Armenians. Between the 13th and 17th century it was part of the Georgian principality of Samtskhe-Saatabago and it was first an Ottoman vassal in the early 16th century and was annexed in 1550. The area of Tortum was contested by the Safavids and the Ottoman Empire in the 16th-17th century, Tortum was a sanjak in Erzurum Eyalet. The region was in the early Ottoman period largely Christian but acquired a Muslim majority in the mid 18th century, during World War I, Ottoman troops crossed Tortum in the disastrous Battle of Sarikamish. Then the Russians occupied the town and held it between 1915 and 1917, after the February revolution of 1917 they left it to the Armenians. The Ottoman army advanced some time later and captured Tortum on 16 March 1918, the town has a ruined citadel. As of 1920, Tortum was producing coal, cağ kebabı Khakhuli Monastery Tortum Waterfall Official website
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Elevation
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GIS or geographic information system is a computer system that allows for visualizing, manipulating, capturing, and storage of data with associated attributes. GIS offers better understanding of patterns and relationships of the landscape at different scales, tools inside the GIS allow for manipulation of data for spatial analysis or cartography. A topographical map is the type of map used to depict elevation. In a Geographic Information System, digital models are commonly used to represent the surface of a place. Digital terrain models are another way to represent terrain in GIS, USGS is developing a 3D Elevation Program to keep up with growing needs for high quality topographic data. 3DEP is a collection of enhanced elevation data in the form of high quality LiDAR data over the conterminous United States, Hawaii, there are three bare earth DEM layers in 3DEP which are nationally seamless at the resolution of 1/3,1, and 2 arcseconds. This map is derived from GTOPO30 data that describes the elevation of Earths terrain at intervals of 30 arcseconds and it uses color and shading instead of contour lines to indicate elevation. Hypsography is the study of the distribution of elevations on the surface of the Earth, the term originates from the Greek word ὕψος hypsos meaning height. Most often it is used only in reference to elevation of land, related to the term hypsometry, the measurement of these elevations of a planets solid surface are taken relative to mean datum, except for Earth which is taken relative to the sea level. In the troposphere, temperatures decrease with altitude and this lapse rate is approximately 6.5 °C/km. S
16.
Depression (geology)
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A depression in geology is a landform sunken or depressed below the surrounding area. Erosion-related, Blowout, a depression created by wind erosion typically in either a partially vegetated sand dune ecosystem or dry soils, glacial valley, a depression carved by erosion by a glacier. River valley, a depression carved by erosion by a river. Area of subsidence caused by the collapse of a structure such as sinkholes in karst terrain. Sink, an endorheic depression generally containing a persistent or intermittent lake, collapse-related, Sinkhole, a depression formed as a result of the collapse of rocks lying above a hollow. This is common in karst regions, kettle, a shallow, sediment-filled body of water formed by melting glacial remnants in terminal moraines. Thermokarst hollow, caused by loss of the ground as the result of permafrost thawing. Impact-related, Impact crater, a depression created by an impact such as a meteorite crater, sedimentary-related, Sedimentary basin, in sedimentology, an area thickly filled with sediment in which the weight of the sediment further depresses the floor of the basin. Structural or tectonic-related, Structural basin, a depression, a region of tectonic downwarping as a result of isostasy or subduction. Graben or rift valley, fallen and typically linear depressions or basins created by rifting in a region under tensional tectonic forces, pull-apart basin caused by offset in a strike slip or transform fault. Oceanic trench, a linear depression on the ocean floor. Oceanic trenches are caused by subduction of oceanic crust beneath either oceanic crust or continental crust, pit crater, a volcanic depression smaller than a caldera formed by a sinking, or caving in, of the ground surface lying over a void. Maar, a resulting from phreatomagmatic eruption or diatreme explosion. Cryptodepression List of places on land with elevations below sea level
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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
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Continental climate
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In the Köppen climate system, Continental climates were bordered to the south by Temperate climates or C climates and to the north by Boreal climate or E climates. Köppen also defined continental climates as having more than 30 days with continuous snowcover on the ground, Continental climates often have a significant annual variation in temperature. They tend to occur in the latitudes, where prevailing winds come from over land. Continental climates occur mostly in the Northern Hemisphere which has the large landmasses required for this type of climate to develop, most of northern and northeastern China, eastern and southeastern Europe, and the central and upper eastern United States have this type of climate. In Continental climates, Precipitation tends to be moderate in amount, a portion of the annual precipitation falls as snowfall, and snow often remains on the ground for more than a month. Summers in continental climates can feature thunderstorms and frequent cool temperatures, the timing of intermediate spring-like or autumn-like temperatures in this zone vary depending on latitude and/or elevation. For example, spring may arrive as soon as early March in the parts of this zone. Annual precipitation in this zone is usually between 600 millimetres and 1,200 millimetres, most of it in the form of snow during winter and it also has cold winters and warm summers. Most such areas fit Köppen classifications of Dfa, Dwa or Dfb or Dwb, dry summer continental climates exist in high altitude areas near Mediterranean climates. In some cases, the climate classification of BSk can also be considered to be continental as long it has cold winter. Some climatologists use the 0 °C isotherm instead for the coldest month, Continental climates exist where cold air masses infiltrate during the winter and warm air masses form in summer under conditions of high sun and long days. Places with continental climates are as a rule either far from any moderating effects of oceans or are so situated that prevailing winds tend to head offshore. Such regions get quite warm in the summer, achieving temperatures characteristic of tropical climates but are colder than any other climates of similar latitude in the winter. These climates grade off toward subtropical climates equator-ward where winters are less severe, in Europe these climates may grade off into oceanic climates in which the influence of moderating air masses is more marked toward the west. The subarctic climate, with cold, long and dry winters. Canada, Throughout much of southern Canada from the Rocky Mountains to Atlantic Canada, major cities, Whistler, Prince George, Kamloops, Calgary, Edmonton, Fort McMurray, Saskatoon, Regina, Winnipeg, Kenora, Thunder Bay, Sault Ste
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Precipitation
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In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravity. The main forms of precipitation include drizzle, rain, sleet, snow, graupel, Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor, so that the water condenses and precipitates. Thus, fog and mist are not precipitation but suspensions, because the vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated, Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers, moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condensed into clouds and rain. This process is active when freezing rain is occurring. A stationary front is often present near the area of freezing rain, provided necessary and sufficient atmospheric moisture content, the moisture within the rising air will condense into clouds, namely stratus and cumulonimbus. Eventually, the droplets will grow large enough to form raindrops. Lake-effect snowfall can be locally heavy, thundersnow is possible within a cyclones comma head and within lake effect precipitation bands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation, on the leeward side of mountains, desert climates can exist due to the dry air caused by compressional heating. The movement of the trough, or intertropical convergence zone. Precipitation is a component of the water cycle, and is responsible for depositing the fresh water on the planet. Approximately 505,000 cubic kilometres of water falls as precipitation each year,398,000 cubic kilometres of it over the oceans and 107,000 cubic kilometres over land. Given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres, Climate classification systems such as the Köppen climate classification system use average annual rainfall to help differentiate between differing climate regimes. Precipitation may occur on celestial bodies, e. g. when it gets cold, Mars has precipitation which most likely takes the form of frost. Precipitation is a component of the water cycle, and is responsible for depositing most of the fresh water on the planet. Approximately 505,000 km3 of water falls as precipitation each year,398,000 km3 of it over the oceans, given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres. Mechanisms of producing precipitation include convective, stratiform, and orographic rainfall, Precipitation can be divided into three categories, based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or ice
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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
