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Wadi Qana
Wadi Qana (, ) is a wadi with an intermittent stream meandering westwards from Huwara, south of Nablus, in the West Bank, Palestine, down to Jaljulia in Israel, from where it flows into the Yarkon River, of which it is a tributary. Geography and demography Wadi Qana begins south of Mount Gerizim near the village of Burin in the West Bank. Lined by steep cliffs on either side, the wadi waters flow in a general ENE-WSW direction and reach the Sharon plain near Jaljulia, Israel, where it empties into the Yarkon just west of the Yarkon interchange. West of the central anticline, its surface and sub-aquifers form one of the recharging feeders of the Yarqon Tanninim basin, of which lie east of the Green Line. The Wadi Qana area of the West Bank portion of the drainage basin encompasses approximately . Harsh rocky limestone and karst terrain is characteristic of the terrain north of its border towards Kafr Thulth. As of 2018, the population of the area of the wadi in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kanah
Kanah is a toponym used in two distinct geographical contexts in the Hebrew Bible. Border river between tribes Kanah (), in the KJV the Brook Kanah, is a stream referred to in the Hebrew Bible forming the boundary between Ephraim and Manasseh, from the Mediterranean Sea eastward to Tappuah (). It has been identified variously with: * Wadi Qana, a wadi in the northern West Bank, crossing into Israel at Jaljulia, and flowing into the Yarkon River before this reaches the sea. It is generally seen as the biblical 'brook of Kanah'. * The sedgy streams that constitute the Wady Talaik, which enters the sea between Joppa and Caesarea Maritima. The stream rises southwest of Shechem near modern Nablus, flows through Wady Ishkar and joining Yarkon/Aujeh River, soon reaching the sea north of Jaffa. * The Yarkon (Hebrew) or Auja/Aujeh River (Arabic) Town of Kanah The Book of Joshua also refers to a town named Kanah in the north of the territory of the tribe of Asher According to the Heb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palestine
Palestine, officially the State of Palestine, is a country in West Asia. Recognized by International recognition of Palestine, 147 of the UN's 193 member states, it encompasses the Israeli-occupied West Bank, including East Jerusalem, and the Gaza Strip, collectively known as the occupied Palestinian territories, within the broader geographic and historical Palestine (region), Palestine region. Palestine shares most of its borders with Israel, and it borders Jordan to the east and Egypt to the southwest. It has a total land area of while Demographics of the State of Palestine, its population exceeds five million people. Its Status of Jerusalem, proclaimed capital is Jerusalem, while Ramallah serves as its administrative center. Gaza City was its largest city prior to Gaza Strip evacuations, evacuations in 2023. Situated at a Levantine corridor, continental crossroad, the region of Palestine was ruled by various empires and experienced Demographic history of Palestine (region ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. In regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's Oil and gas reserves and resource quantification, hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), 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 (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land in which 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 the drainage divide line. A drainage basin's boundaries are determined by watershed delineation, a common task in environmental engineering and science. In a closed drainage basin, or endorheic basin, rather than flowing to the ocean, water converges toward the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Green Line (Israel)
The Green Line, or 1949 Armistice border, is the demarcation line set out in the 1949 Armistice Agreements between the armies of Israel and those of its neighbors (Egypt, Jordan, Lebanon, and Syria) after the 1948 Arab–Israeli War. It served as the ''de facto'' borders of the State of Israel from 1949 until the Six-Day War in 1967, and continues to represent Israel's internationally recognized borders with the two Palestinian territories: the West Bank and the Gaza Strip. The Green Line was intended as a demarcation line rather than a permanent border. The 1949 Armistice Agreements were clear (at Arab insistence) that they were not creating permanent borders. The Egyptian–Israeli agreement, for example, stated that "the Armistice Demarcation Line is not to be construed in any sense as a political or territorial boundary, and is delineated without prejudice to rights, claims and positions of either Party to the Armistice as regards ultimate settlement of the Palestine questio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yarkon-Taninim Aquifer
The Yarkon-Taninim Aquifer, also known as the Western Mountain Aquifer of Israel/Palestine, is the western and larger part of the Mountain Aquifer, which also contains the Eastern and the smaller North-Eastern (Mountain) Aquifers.Water Authority, State of Israel The Water Issue Between Israel and the Palestinians: Main Facts February 2012. Accessed April 2019. The Mountain Aquifer and the Coastal Aquifer are the main aquifers shared by Israel in its pre-1967 borders, and Palestine (West Bank and Gaza Strip).It has been the main longterm reservoir of the Israeli water system. It is a limestone aquifer, located under the foothills in the centre of the country. It is used by Israel for roughly 340 million cubic meters of water every year and for Palestine at a rate of approximately 20 million cubic meters a year,a rate that remains unchanged from the days when the West Bank was under Jordanian rule. Eyal Benvenisti , Haim Gvirtzma'Harnessing International Law to Determine Israeli-Pale ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aquifer
An aquifer is an underground layer of water-bearing material, consisting of permeability (Earth sciences), permeable or fractured rock, or of unconsolidated materials (gravel, sand, or silt). Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called ''hydrogeology''. Related concepts include aquitard, a bed (geology), bed of low permeability along an aquifer, and aquiclude (or ''aquifuge''), a solid and impermeable region underlying or overlying an aquifer, the pressure of which could lead to the formation of a confined aquifer. Aquifers can be classified as saturated versus unsaturated; aquifers versus aquitards; confined versus unconfined; isotropic versus anisotropic; porous, karst, or fractured; and transboundary aquifer. Groundwater from aquifers can be sustainably harvested by humans through the use of qanats leading to a well. This groundwater is a major source of fresh water for many regions, althoug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anticline
In structural geology, an anticline is a type of Fold (geology), fold that is an arch-like shape and has its oldest Bed (geology), beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is convex curve, convex up in which the hinge or crest is the location where the curvature is greatest, and the limbs are the sides of the fold that Strike and dip, dip away from the hinge. Anticlines can be recognized and differentiated from antiforms by a sequence of rock layers that become progressively older toward the center of the fold. Therefore, if age relationships between various Stratum, rock strata are unknown, the term antiform should be used. The progressing age of the rock strata towards the core and uplifted center, are the trademark indications for evidence of anticlines on a geological map. These formations occur because anticlinal ridges typically develop above thrust faults during crustal deformations. The uplifted core of the fold cau ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Highway 5 (Israel–Palestine)
Highway 5 or the Trans-Samaria Highway (, ''Kvish Hotze Shomron''), is one of Israel's main highways, connecting the Mediterranean coast immediately north of Tel Aviv with the central Sharon plain and eastwards to Ariel and other Israeli settlements in the northern West Bank. The name ''Highway 5'' is commonly used to describe the section of the highway running from the road's western end at the Glilot Interchange until it reaches the main entrance of Ariel. In this capacity it intersects and creates a connection between four important arterial freeways in the northern Tel Aviv area: The Coastal Highway (Highway 2), the Ayalon Highway (Highway 20), Geha Highway (Highway 4) and the Cross-Israel Highway (Highway 6). An alternate name for the entire highway is ''Kvish Hotze Shomron'' meaning the ''Trans-Samaria Highway'' though often this name is used when referring specifically to the section of the road in the West Bank, i.e., past the Green Line, where it continues east tow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burin, Nablus
Burin () is a Palestinian village in the Nablus Governorate of the State of Palestine, in the northern West Bank, located southwest of Nablus. The town had a population of 2,844 in 2017. History The name itself may conserve the toponym of ''Beera'' mentioned in the Book of Judges 9:21. In the 12th and 13th centuries, during the Crusader era, Burin was inhabited by Muslims, according to the historian Diya al-Din al-Maqdisi.Ellenblum, 2003, pp244 In 1176, a part of the tithes from the village was pledged to the Church of Mount Zion, but there is no evidence that it was ever collected. The founder of the Banu Ghawanima family, Shaykh Ghanim, was born in the village in 1166 and entered Jerusalem with the army of Saladin in 1187.Auld, Hillenbrand and Natsheh 2000, pp. 66, 146. He was appointed as the sheikh of the city's al-Khanqah al-Salahiyya Mosque founded by Saladin in 1187 and he and his descendants served as the head judges of the Shafi'i ''fiqh'' (Islamic school of law) i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
