Mount Karadağ
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Mount Karadağ
Karadağ (literally: ''Black mountain'') is an extinct volcano in Karaman Province, Turkey. Geography The crater of the volcano, which is now a lava plain, is approximately north of Karaman at at AMSL. The peak of the mountain is east of this plain at an elevation of . Since the average elevation of the Karaman plains is about , the height of the peak with respect to surrounding area is more than . Up to a century ago there was a volcanic crater lake in the mountain which has since dried up. The shape of the mountain is roughly conical with a base diameter of . History The slopes of the volcano have always been inhabited. In fact, Çatalhöyük (ca 7500 BC), one of the earliest neolithic settlements in Anatolia, is located at the north-west of the volcano, and there are Hittite inscriptions on the hills at the south-east of the mountain. The mountain was called Boratinon in late antiquity. Ancient Derbe, which is one of the towns Paul the Apostle had visited, is sit ...
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Karaman Karadağ Transmitting Station, Turkey
Karaman, historically known as Laranda (Greek: Λάρανδα), is a city in south central Turkey, located in Central Anatolia, north of the Taurus Mountains, about south of Konya. It is the capital district of the Karaman Province. According to the 2000 census, the population of the province is 231,872 of which 132,064 live in the town of Karaman. The district covers an area of , and the town lies at an average elevation of . The Karaman Museum is one of the major sights. Etymology The town owes its name to Karaman Bey, who was one of the rulers of the Karamanid dynasty. The former name ''Laranda'' which in turn comes from the Luwian language ''Larawanda'', literally means "sandy, a sandy place". History In ancient times, Karaman was known as Laranda ( el, Λάρανδα). In the 6th century BC it came under Achaemenid rule until 322 BC, when it was destroyed by Perdiccas, a former general of Alexander the Great, after he had defeated Ariarathes I, king of Cappadocia. It lat ...
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Paul The Apostle
Paul; grc, Παῦλος, translit=Paulos; cop, ⲡⲁⲩⲗⲟⲥ; hbo, פאולוס השליח (previously called Saul of Tarsus;; ar, بولس الطرسوسي; grc, Σαῦλος Ταρσεύς, Saũlos Tarseús; tr, Tarsuslu Pavlus; la, Paulus Tarsensis AD), commonly known as Paul the Apostle and Saint Paul, was a Christian apostle who spread the teachings of Jesus in the first-century world. Generally regarded as one of the most important figures of the Apostolic Age, he founded several Christian communities in Asia Minor and Europe from the mid-40s to the mid-50s AD. According to the New Testament book Acts of the Apostles, Paul was a Pharisee. He participated in the persecution of early disciples of Jesus, possibly Hellenised diaspora Jews converted to Christianity, in the area of Jerusalem, prior to his conversion. Some time after having approved of the execution of Stephen, Paul was traveling on the road to Damascus so that he might find any Christians ...
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Extinct Volcanoes
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ...
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Landforms Of Karaman Province
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ...
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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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Volcanoes Of Turkey
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ...
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Kılbasan
Kılbasan is a village in Karaman District, Karaman Province, Turkey. Its population is 1,571 (2022). Before the 2013 reorganisation, it was a town ('' belde''). Geography Kılbasan is at the north of Karaman and the highway distance to Karaman is . The town is in the even plain with an altitude of . The extinct volcano Karadağ (2271 m.) is at the north west of the town. History During Byzantine Empire era, the main settlement was in ''Karışmaa Birindi'', an ancient town on a tumulus A tumulus (plural tumuli) is a mound of earth and stones raised over a grave or graves. Tumuli are also known as barrows, burial mounds or ''kurgans'', and may be found throughout much of the world. A cairn, which is a mound of stones buil ... few kilometers south west of Kılbasan. Kılbasan and vicinity had been a part of Seljuk Empire in the second half of the 11th century. After Mongol Empire, Mongol domination, the area became a part of Karamanids, Karamanid Anatolian beyli ...
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