|
Southern Anatolian Montane Conifer And Deciduous Forests
The Southern Anatolian montane conifer and deciduous forests ecoregion, in the Mediterranean forests, woodlands, and scrub biome, is in the eastern Mediterranean Basin. Lebanon cedar (''Cedrus libani'') is a characteristic tree. Geography The ecoregion covers an area of , in portions of Turkey, Syria, Lebanon, and Israel. The ecoregion lies mainly in the Taurus Mountains, which run through southern Anatolia roughly parallel to the coast. The Taurus is divided into three sub-ranges – the Western, or Isaurian, Taurus (highest peak Mt. Kizlarsivrisi ); the Central, or Lycian, Taurus (highest peak Medetsiz ); and the Eastern, or Cilician, Taurus (highest peak Demirkazık ). The ecoregion also includes the higher-elevation portions of the Nur Mountains (or Amanos) along the western Turkey-Syria border, and the Levantine Syrian Coastal Mountains, Lebanon Mountains, and Anti-Lebanon Mountains, which run parallel to the eastern Mediterranean shore in Syria, Lebanon, and norther ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taurus Mountains
The Taurus Mountains ( Turkish: ''Toros Dağları'' or ''Toroslar'') are a mountain complex in southern Turkey, separating the Mediterranean coastal region from the central Anatolian Plateau. The system extends along a curve from Lake Eğirdir in the west to the upper reaches of the Euphrates and Tigris rivers in the east. It is a part of the Alpide belt in Eurasia. Etymology The mountain range under the current name was mentioned in ''The Histories'' by Polybius as Ταῦρος (''Taûros''). Heinrich Kiepert writes in ''Lehrbuch der alten Geographie'' that the name was borrowed into Ancient Greek from the Semitic (Old Aramaic) root טורא ''ṭūrā'', meaning "mountain". Geography The Taurus mountains are divided into three chains from west to east as follows; * Western Taurus (Batı Toroslar) *Central Taurus (Orta Toroslar) *Southeastern Taurus (Güneydoğu Toroslar) Western Taurus The Western Taurus Mountains form an arc around the Gulf of Antalya. It includes th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mediterranean Climate
A Mediterranean climate (also called a dry summer temperate climate ''Cs'') is a temperate climate sub-type, generally characterized by warm, dry summers and mild, fairly wet winters; these weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location. This climate type's name is in reference to the coastal regions of the Mediterranean Sea within the Mediterranean Basin, where this climate type is most prevalent. The "original" Mediterranean zone is a massive area, its western region beginning with the Iberian Peninsula in southwestern Europe and coastal regions of northern Morocco, extending eastwards across southern Europe, the Balkans, and coastal Northern Africa, before reaching a dead-end at the Levant region's coastline. Mediterranean climate zones are typically located along the western coasts of landmasses, between roughly 30 and 45 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ophiolitic
An ophiolite is a section of Earth's oceanic crust and the underlying upper mantle that has been uplifted and exposed above sea level and often emplaced onto continental crustal rocks. The Greek word ὄφις, ''ophis'' (''snake'') is found in the name of ophiolites, because of the superficial texture of some of them. Serpentinite especially evokes a snakeskin. The suffix ''lite'' from the Greek ''lithos'' means "stone". Some ophiolites have a green color. The origin of these rocks, present in many mountainous massifs, remained uncertain until the advent of plate tectonic theory. Their great significance relates to their occurrence within mountain belts such as the Alps and the Himalayas, where they document the existence of former ocean basins that have now been consumed by subduction. This insight was one of the founding pillars of plate tectonics, and ophiolites have always played a central role in plate tectonic theory and the interpretation of ancient mountain belts. Ps ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Serpentinite
Serpentinite is a rock composed predominantly of one or more serpentine group minerals, the name originating from the similarity of the texture of the rock to that of the skin of a snake. Serpentinite has been called ''serpentine'' or ''serpentine rock'', particularly in older geological texts and in wider cultural settings.California Government Code § 425.2; ''see'' Formation and mineralogy Serpentinite is formed by near to complete serpentinization of mafic to ultramafic rocks. Serpentinite can be formed wherever ultramafic rock is infiltrated by water poor in carbon dioxide. This occurs at mid-ocean ridges and in the forearc mantle of subduction zones. The final mineral composition of serpentinite is usually dominated by lizardite, chrysotile, and magnetite. Brucite and antigorite are less commonly present. Lizardite, chrysotile, and antigorite all have approximately the formula or , but differ in minor components and in form. Accessory minerals, present in smal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qurnat As Sawda'
Qurnat as Sawdā ( ar , القرنة السوداء), is the highest point in Lebanon and the Levant, at 3,088 meters above sea level. It is found at the peak of Jabal al Makmel, a mountain range in the Bsharri District, North Lebanon. Name The mountain's name derives from the Classical Syriac (''Qornet Sohde''), for "Martyrs' Mountain". This, in turn, refers to late-13th century campaigns in the region by the Muslim Mamluk Sultanate during its conquest of the Christian Crusader states. Its name, like many other local toponyms, was retained even after the decline of Syriac as a vernacular tongue in the region. References in medieval religious literature In Jacobus de Voragine's ''Golden Legend'', the summit of Mount Lebanon (Qurnat as Sawda') is the site on which Noah, after having survived the flood, replanted a sacred tree. Voragine states that the tree's seeds were given to Seth by an angel in the Garden of Eden In Abrahamic religions, the Garden of Eden ( he, גַּ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anti-Lebanon Mountains
The Anti-Lebanon Mountains ( ar, جبال لبنان الشرقية, Jibāl Lubnān ash-Sharqiyyah, Eastern Mountains of Lebanon; Lebanese Arabic: , , "Eastern Mountains") are a southwest–northeast-trending mountain range that forms most of the border between Syria and Lebanon. The border is largely defined along the crest of the range. Most of the range lies in Syria. Etymology Its Western name ''Anti-Lebanon'' comes from the Greek and Latin , derived from its position opposite (') and parallel to the Mount Lebanon range (). Geology The Anti-Lebanon range is approximately in length. To the south, the range adjoins the lower-lying Golan Heights plateau, but includes the highest peaks, namely Mount Hermon (''Jabal el-Shaykh'', in Arabic), at 2,814 metres, and Ta'la't Musa, at 2,669 metres. These peaks, on the Lebanese-Syrian border, are snow-covered for much of the year. Anti-Lebanon mountains are an anticline. Their predominant rocks are limestone and chalk from the Juras ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lebanon Mountains
Mount Lebanon ( ar, جَبَل لُبْنَان, ''jabal lubnān'', ; syr, ܛܘܪ ܠܒ݂ܢܢ, ', , ''ṭūr lewnōn'' french: Mont Liban) is a mountain range in Lebanon. It averages above in elevation, with its peak at . Geography The Mount Lebanon range extends along the entire country for about , parallel to the Mediterranean coast. Their highest peak is Qurnat as Sawda', at . The range receives a substantial amount of precipitation, including snow, which averages around deep.Jin and Krothe. ''Hydrogeology: Proceedings of the 30th International Geological Congress'', p. 170 Lebanon has historically been defined by the mountains, which provided protection for the local population. In Lebanon, changes in scenery are related less to geographical distances than to altitudes. The mountains were known for their oak and pine forests. The last remaining old growth groves of the famous Cedar of Lebanon (''Cedrus libani'' var. libanii'') are on the high slopes of Mount Lebanon, in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Syrian Coastal Mountain Range
The Coastal Mountain Range ( ar, سلسلة الجبال الساحلية ''Silsilat al-Jibāl as-Sāḥilīyah'') also called Al-Anṣariyyah is a mountain range in northwestern Syria running north–south, parallel to the coastal plain.Federal Research Division, Library of Congress (2005"Country Profile: Syria"page 5 The mountains have an average width of , and their average peak elevation is just over with the highest peak, Nabi Yunis, reaching , east of Latakia. In the north the average height declines to , and to in the south. Name Classically, this range was known as the Bargylus; a name mentioned by Pliny the Elder. The el, Μπάργκυλος, Bargylus) had its roots in the name of an ancient city-kingdom called Barga most probably located in the vicinity of the mountains; it was a city of the Eblaite Empire in the third millennium BC, and then a vassal kingdom of the Hittites, who named the mountain range after Barga. In the medieval period were known as the Jabal Ba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Levant
The Levant () is an approximate historical geographical term referring to a large area in the Eastern Mediterranean region of Western Asia. In its narrowest sense, which is in use today in archaeology and other cultural contexts, it is equivalent to a stretch of land bordering the Mediterranean in South-western Asia,Gasiorowski, Mark (2016). ''The Government and Politics of the Middle East and North Africa''. }, ), meaning "the eastern place, where the Sun rises". In the 13th and 14th centuries, the term ''levante'' was used for Italian maritime commerce in the Eastern Mediterranean, including Greece, Anatolia, Syria-Palestine, and Egypt, that is, the lands east of Venice. Eventually the term was restricted to the Muslim countries of Syria-Palestine and Egypt. In 1581, England set up the Levant Company to monopolize commerce with the Ottoman Empire. The name ''Levant States'' was used to refer to the French mandate over Syria and Lebanon after World War I. This is probab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nur Mountains
The Nur Mountains ( tr, Nur Dağları, "Mountains of Holy Light"), formerly known as Alma-Dağ, the ancient Amanus ( grc, Ἁμανός), medieval Black Mountain, or Jabal al-Lukkam in Arabic, is a mountain range in the Hatay Province of south-central Turkey, which starts south of the Taurus Mountains (and is linked with it), south of the Ceyhan river (old name: Pyramus), runs roughly parallel to the Gulf of İskenderun (old name: Gulf of Issus) (İskenderun was called Alexandria of Cilicia) and ends in the Mediterranean coast between the Gulf of İskenderun and the Orontes ( Asi) river mouth. The range has about 100 miles (200 kilometers) in length and reaches a maximum elevation of and divides the coastal region of Cilicia from Antioch and inland Syria making a natural border between Asia Minor (Anatolia), in the southeast region, and the rest of Southwest Asia. The highest peak is Bozdağ Dağı. A major pass through the mountains known as the Belen Pass (Syrian Gates) is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.png "Click for more on -> Levant")