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Sultandağ
The Sultan Mountains ( tr, Sultandağ), also known as Sultan Dagh range or Sultan Dag, is a short mountain range on the western edge of the Anatolian Plateau, Turkey with highest elevation of . The town of Sultandağı is their namesake. They are made up of metamorphic rocks dating from the Lower Cambrian to the Carboniferous The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carbonifero ... period. West slopes of Sultan Mountains are part of the Lake Beyşehir drainage basin. References Mountain ranges of Turkey Aegean Region Central Anatolia Region Landforms of Afyonkarahisar Province {{Turkey-geo-stub ...
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Sultandağı
Sultandağı is a town of Afyonkarahisar Province in the Aegean region of Turkey. It is the seat of Sultandağı District.İlçe Belediyesi
Turkey Civil Administration Departments Inventory. Retrieved 12 January 2023.
Its population is 5,195 (2021). It is located at 68 km from the city of on the road to , near Lake Akşehir at the foothills of the

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Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. 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, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ...
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Anatolian Plateau
The Anatolian Plateau () is a plateau that occupies most of Turkey's surface area. The elevation of the plateau ranges from 600 to 1,200 meters (2,000 to 4,000 ft). Mount Erciyes near Kayseri is the peak at 3,917 m (12,851 ft). Ankara, the capital of Turkey, is located in the northwestern part of this plateau. Overview In Turkey, stretching inland from the Aegean coastal plain, the Central Anatolia Region occupies the area between the two zones of the folded mountains, extending east to the point where the two ranges converge. The plateau-like, semi-arid highlands of Anatolia are considered the heartland of the country. The region varies in elevation from 700 to 2000 meters from west to east. The two largest basins on the plateau are the ''Konya Konya () is a major city in central Turkey, on the southwestern edge of the Central Anatolian Plateau, and is the capital of Konya Province. During antiquity and into Seljuk times it was known as Iconium (), altho ...
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Turkey
Turkey ( tr, Türkiye ), officially the Republic of Türkiye ( tr, Türkiye Cumhuriyeti, links=no ), is a list of transcontinental countries, transcontinental country located mainly on the Anatolia, Anatolian Peninsula in Western Asia, with a East Thrace, small portion on the Balkans, Balkan Peninsula in Southeast Europe. It shares borders with the Black Sea to the north; Georgia (country), Georgia to the northeast; Armenia, Azerbaijan, and Iran to the east; Iraq to the southeast; Syria and the Mediterranean Sea to the south; the Aegean Sea to the west; and Greece and Bulgaria to the northwest. Cyprus is located off the south coast. Turkish people, Turks form the vast majority of the nation's population and Kurds are the largest minority. Ankara is Turkey's capital, while Istanbul is its list of largest cities and towns in Turkey, largest city and financial centre. One of the world's earliest permanently Settler, settled regions, present-day Turkey was home to important Neol ...
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Metamorphic Rocks
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and distort ...
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Lower Cambrian
The Cambrian Period ( ; sometimes symbolized Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ago (mya) to the beginning of the Ordovician Period mya. Its subdivisions, and its base, are somewhat in flux. The period was established as "Cambrian series" by Adam Sedgwick, who named it after Cambria, the Latin name for 'Cymru' (Wales), where Britain's Cambrian rocks are best exposed. Sedgwick identified the layer as part of his task, along with Roderick Murchison, to subdivide the large "Transition Series", although the two geologists disagreed for a while on the appropriate categorization. The Cambrian is unique in its unusually high proportion of sedimentary deposits, sites of exceptional preservation where "soft" parts of organisms are preserved as well as their more resistant shells. As a result, our understanding of the Cambrian biolo ...
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Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ...
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Lake Beyşehir
Lake Beyşehir ( tr, Beyşehir Gölü; anciently, Carallis or Karallis ( grc, Κάραλλις), or Caralis or Karalis (Κάραλις)) is a large freshwater lake in Isparta and Konya provinces in southwestern Turkey. It is located at around and is the largest freshwater lake in Turkey. It has an area of 650 km² and is 45 km long and 20 km wide. It carries the same name as the principal urban centre of its region, Beyşehir. Anciently, it was considered part of ancient Isauria. The lake is fed by streams flowing from the Sultan Mountains and the Anamas Mountains. The water level in the lake often fluctuates by year and by season. Lake Beyşehir is used for irrigation and aquaculture, although it is also a national park. There are thirty-two islets in varying sizes in the lake. Lake Beyşehir is also an important site for many bird species. The maximum depth is 10 metres. Water in the lake was at its lowest level during the period 1960-1990 in October 1975 at 112 ...
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Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ...
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Mountain Ranges Of Turkey
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Aegean Region
The Aegean Region () is one of the 7 Geographical regions of Turkey, geographical regions of Turkey. The largest city in the region is İzmir. Other big cities are Manisa, Aydın, Denizli, Muğla, Afyonkarahisar and Kütahya. Located in western Turkey, it is bordered by the Aegean Sea to the west, the Marmara Region to the north, the Central Anatolia Region to the east, and the Mediterranean Region, Turkey, Mediterranean Region to the south. Among the four coastal regions, the Aegean Region has the longest coastline. Subdivision *Aegean Section ( tr, Ege Bölümü) **Edremit Area ( tr, Edremit Yöresi) **Bakırçay Area ( tr, Bakırçay Yöresi) **Gediz Area ( tr, Gediz Yöresi) **İzmir Area ( tr, İzmir Yöresi) **Küçük Menderes Area ( tr, Küçük Menderes Yöresi) **Büyük Menderes Area ( tr, Büyük Menderes Yöresi) **Menteşe Area ( tr, Menteşe Yöresi) * Inner Western Anatolia Section ( tr, İç Batı Anadolu Bölümü) Ecoregions The ecoregions of this ...
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Central Anatolia Region
The Central Anatolia Region ( tr, İç Anadolu Bölgesi) is a geographical region of Turkey. The largest city in the region is Ankara. Other big cities are Konya, Kayseri, Eskişehir, Sivas, and Aksaray. Located in Central Turkey, it is bordered by the Aegean Region to the west, the Black Sea region to the north, the Eastern Anatolia Region to the east, and the Mediterranean Region to the south. It also shares a very slight border with the Marmara Region in Bilecik Province. Cities Cities located in Central Anatolia: Subdivisions * Konya Section ( tr, Konya Bölümü) ** Obruk Plateau ( tr, Obruk Platosu) ** Konya - Ereğli Vicinity ( tr, Konya - Ereğli Çevresi) * Upper Sakarya Section ( tr, Yukarı Sakarya Bölümü) ** Ankara Area ( tr, Ankara Yöresi) ** Porsuk Gully ( tr, Porsuk Oluğu) ** Sündiken Mountain Chain Area ( tr, Sündiken Dağları Yöresi) ** Upper Sakarya Gully ( tr, Yukarı Sakarya Yöresi) * Middle Kızılırmak Section ( tr, Orta Kızılı ...
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