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Nahal Betzet
Nahal Betzet ( he, נחל בצת, lit. "Betzet stream"), Arabic: Wadi Karkara, is a once-perennial and now intermittent stream in the Upper Galilee, Israel. Most of it is part of the nature reserve named for the stream. Geography The stream crosses the border from Lebanon into Israel between Shtula and Zar'it, and flows westward, emptying into the Mediterranean Sea south of Rosh HaNikra. The stream runs along a geological fault line through dolomite and limestone, and is fed along its course by springs. Currently, Mekorot (the national water company) pumps the water of the stream's springs, and has been accused of causing the stream to dry up. Many caves are formed on the banks of the stream, most notably the arch known as Keshet Cave (Rainbow Cave). Nature reserve Most of the stream is part of a nature reserve that bears its name. The reserve, declared in 1972 covers 7650-dunam and part of it reaches the Israel-Lebanese border. In 2009, 1225 dunams were added to the reserve. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Betzet Map
Betzet ( he, בֶּצֶת) is a moshav in the Western Galilee in northern Israel. Located near Shlomi and Nahariya, it falls under the jurisdiction of Mateh Asher Regional Council. As of its population was . History Antiquity Betzet is known in historical records as one of several places along the route to Tyre where produce transported from the Land of Israel was often sold in the local marketplaces, mentioned as such in the Tosefta (''Shevi'it'' 4:8-ff.) and in the 3rd century Mosaic of Rehob. Betzet is listed in the Tosefta and the Jerusalem Talmud as subject to the laws of Shmita. State of Israel Moshav Betzet was founded in 1951 on land belonging to the Palestinian village al-Bassa, which was depopulated during the 1948 Arab–Israeli War. The founders were immigrants to Israel from the Balkan states, especially Yugoslavia and Romania. The community retains the name of the ancient village of Betzet, which is estimated to have existed nearby. On 12 August 1968, two Syr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of Israel
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, spring ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adiantum Capillus-veneris
''Adiantum capillus-veneris'', the Southern maidenhair fern, black maidenhair fern, maidenhair fern, and venus hair fern, is a species of ferns in the genus ''Adiantum'' and the family Pteridaceae with a subcosmopolitan worldwide distribution. It is cultivated as a popular garden fern and houseplant.Wildflower.org-NPIN: Adiantum capillus-veneris (Southern maidenhair fern) . accessed 4.04.2011 Distribution ''Adiantum capillus-veneris'' is native to the southern half of the United States from to the Atlantic coast, through Mexico and Central America, to South America. It is also native to |
Platanus Orientalis
''Platanus orientalis'', the Old World sycamore or Oriental plane, is a large, deciduous tree of the Platanaceae family, growing to or more, and known for its longevity and spreading crown. In autumn its deep green leaves may change to blood red, amber, and yellow. Etymology The species' name means 'eastern'. (In comparison, the 'western' plane (or American sycamore) is named ''Platanus occidentalis''). The eastern plane's original distribution was eastward from the Balkans. The tree was called ''platane'' in ancient Greek history and literature and by related names in continental Europe. Equally well known in Asia from Anatolia to India and usually called ''chinar'' or ''chenar''. Range The native range is Eurasia from the Balkans to at least as far east as Iran. Some accounts extend its native range to Iberia in the west, and to the Himalayas in the east. As it has been known in cultivation from early times in much of this region it can be difficult to determine if it is truly ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nerium Oleander
''Nerium oleander'' ( ), most commonly known as oleander or nerium, is a shrub or small tree cultivated worldwide in temperate and subtropical areas as an ornamental and landscaping plant. It is the only species currently classified in the genus ''Nerium'', belonging to subfamily Apocynoideae of the dogbane family Apocynaceae. It is so widely cultivated that no precise region of origin has been identified, though it is usually associated with the Mediterranean Basin. Nerium grows to tall. It is most commonly grown in its natural shrub form, but can be trained into a small tree with a single trunk. It is tolerant to both drought and inundation, but not to prolonged frost. White, pink or red five-lobed flowers grow in clusters year-round, peaking during the summer. The fruit is a long narrow pair of follicles, which splits open at maturity to release numerous downy seeds. Nerium contains several toxic compounds, and it has historically been considered a poisonous plant. Howeve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dunam
A dunam ( Ottoman Turkish, Arabic: ; tr, dönüm; he, דונם), also known as a donum or dunum and as the old, Turkish, or Ottoman stremma, was the Ottoman unit of area equivalent to the Greek stremma or English acre, representing the amount of land that could be ploughed by a team of oxen in a day. The legal definition was "forty standard paces in length and breadth", but its actual area varied considerably from place to place, from a little more than in Ottoman Palestine to around in Iraq.Λεξικό της κοινής Νεοελληνικής (Dictionary of Modern Greek), Ινστιτούτο Νεοελληνικών Σπουδών, Θεσσαλονίκη, 1998. The unit is still in use in many areas previously ruled by the Ottomans, although the new or metric dunam has been redefined as exactly one decare (), which is 1/10 hectare (1/10 × ), like the modern Greek royal stremma. History The name dönüm, from the Ottoman Turkish ''dönmek'' (, "to turn"), appears ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keshet Cave
The Keshet Cave ( he, מערת קשת, Rainbow Cave, also Qeshet Cave) is a natural arch on a ridge by the northern bank of Betzet Stream, Upper Galilee, Israel, in the area of the , in the Betzet Stream Nature Reserve, close to the border with Lebanon. It is a remnant of a large collapsed karst cave and is a narrow strip of rock overhanging a deep abyss."פארק אדמית" (Adamit Park) Assessed from Route 8993, the cave is a tourists attraction. It also attracted the attention of rock climbers, and at the end of 2012 it was opened for sports climbing, however the climbing website 26crags.com had the info about the cave replaced with the notice that rock climbing was prohibited in the area. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mekorot
Mekorot ( he, מקורות, lit. "Sources") is the national water company of Israel and the country's top agency for water management. Founded in 1937, it supplies Israel with 90% of its drinking water and operates a cross-country water supply network known as the National Water Carrier. Mekorot and its subsidiaries have partnered with numerous countries around the world in areas including desalination and water management. History Mekorot was established as the "''Ḥevrat ha-Mayim''" ('Water Company') on 15 February 1937 by Levi Shkolnik (later Eshkol, Prime Minister of Israel between 1963-1969), water engineer Simcha Blass, and Pinchas Koslovsky (later Sapir, Minister of Finance between 1963-1968). Water supply system Mekorot supplies 80% of Israel's drinking water and 70% of its water supplies. The company runs 3,000 installations throughout the country for water supply, water quality, infrastructure, sewage purification, desalination, rain enhancement, etc. Mekorot overse ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring (hydrosphere)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels throu ... [...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] |
Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite which ind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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