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Nahal Qana
Wadi Qana (, he, נחל קנה, translit=Nahal Qana), is a wadi, with an intermittent stream meandering westwards from Huwara south of Nablus in the West Bank down to Jaljulia in Israel 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 o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kanah
Kanah ( he, קָנָה, , reedy; brook of reeds) 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 with the sedgy streams that constitute the Wady Talaik, which enters the sea between Joppa and Caesarea Maritima. The stream rises in the Southwest of Shechem, flows through Wady Ishkar and joining Aujeh, reaches the sea not far to the north of Jaffa. Others identify it with the river Aujeh. The book of Joshua also refers to a town named Kanah in the north of the territory of the tribe of Asher (). It has been identified with 'Ain-Kana, a village on the brow of a valley some southeast of Tyre. About a mile north of this place are many colossal ruins strown about, and in the side of a neighbouring ravine are figures of men, women, and children cut in the face of the rock and supposed to be of Phoenician origin. See also * Wadi Qana Wadi Qana (, he, נחל ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kafr Thulth
Kafr Thulth ( ar, كفر ثلث) is a Palestinian town located on high, flat land south of Azzoun, south of Tulkarm in the Qalqilya Governorate. The average elevation is above sea level. According to the Palestinian Central Bureau of Statistics, the town's population was 3,921 in the 2007 census. Name ''Kafr'' in Syriac means "village" and ''Thulth'' means "three" or "a third". This Syriaic name preserves the place name of Baal-shalisha, an ancient village believed to have been located to the south at a site known in modern times as Khirbat Sirisya.Freedman et al., 2000p. 136 Geography Kafr Thulth is bordered by Azzun to the south, Sanniriya and Biddya villages to the east and Deir Istiya to the west. In 1948, parts of Kharab and Aizab, such as, Salman, al-Moudwer, al-Sheikh Ahmad, al-Ashqar, Ras Tirah, al-Dabha, Kirash Kherba and Ras Atiya — villages or land areas that originally belonged to Kafr Thulth were separated from the town by the Green Line, which forms the bo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, 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 hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...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] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Green Line (Israel)
The Green Line, (pre-)1967 border, 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. 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 question." [...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-Pales ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aquifer
An aquifer is an underground layer of water-bearing, permeable rock, rock fractures, or unconsolidated materials (gravel, sand, or silt). Groundwater from aquifers can be extracted using a water well. Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called hydrogeology. Related terms include aquitard, which is a bed of low permeability along an aquifer, and aquiclude (or ''aquifuge''), which is a solid, impermeable area underlying or overlying an aquifer, the pressure of which could create a confined aquifer. The classification of aquifers is as follows: Saturated versus unsaturated; aquifers versus aquitards; confined versus unconfined; isotropic versus anisotropic; porous, karst, or fractured; transboundary aquifer. Challenges for using groundwater include: overdrafting (extracting groundwater beyond the Dynamic equilibrium, equilibrium yield of the aquifer), groundwater-related subsidence of land, gro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anticline
In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is 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 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 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 geologic map. These formations occur because anticlinal ridges typically develop above thrust faults during crustal deformations. The uplifted core of the fold causes compression of strata that preferentially erodes to a deeper st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Highway 5 (Israel–Palestine)
Highway 5 or the Trans-Samaria Highway ( he, כביש חוצה שומרון, ''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 where it 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 ''Cross-Samaria highway'' though often this name is used when referring specifically to the section of the road in the West Bank, i.e., ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sharon Plain
The Sharon plain ( ''HaSharon Arabic: سهل شارون Sahel Sharon'') is the central section of the Israeli coastal plain. The plain lies between the Mediterranean Sea to the west and the Samarian Hills, to the east. It stretches from Nahal Taninim, a stream marking the southern end of Mount Carmel in the north, to the Yarkon River in the south, at the northern limit of Tel Aviv, over a total of about . The level of the Sharon plain is connected to the level of the Mediterranean Sea by the Sharon Escarpment. Parts of the Plain are included in the Central, Haifa and Tel Aviv Districts of Israel. History Early The Sharon valley is mentioned in an ancient Egyptian stele of Amenhotep II, and as the Sharon field containing both Jaffa and Dor on the Eshmunazar II sarcophagus. The Plain of Sharon is mentioned in the Bible ( 1 Chronicles 5:16, 27:29; Book of Isaiah 33:9, 35:2, 65:10), including the famous reference to the enigmatic "Rose of Sharon" ( Song of Songs 2:1). ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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