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Mount Hermon
Mount Hermon ( / ALA-LC: ('Mountain of the Sheikh', ), , ) is a mountain, mountain cluster constituting the southern end of the Anti-Lebanon mountain range. Its summit straddles the Lebanon–Syria border, border between Syria and Lebanon and, at above sea level, is the highest point in Syria, and the Israeli occupation of the Golan Heights, Israeli-occupied Golan Heights. On the top, in the United Nations Disengagement Observer Force, United Nations buffer zone between Syrian and Israeli-occupied territories, is the highest permanently manned UN position in the world, known as "Hermon Hotel", located at . The southern slopes of Mount Hermon extend to the Israeli-occupied portion of the Golan Heights, where the Mount Hermon ski resort is located with a top elevation of . Geography Wider mountain range The Anti-Lebanon range, of which the Hermon range constitutes the southernmost part, extends for approximately in a northeast–southwest direction, running parallel to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Bental
Mount Bental (, / ALA-LC: ''Jabal al-Gharam'' / "Mountain of Lust" "Jabal Bental"; , ''Har Bental'', "Mount Bental" (lit. "Son of Dew") is a dormant volcano in the North-Eastern part of the Golan Heights, It extends to an elevation of 1,171 Meters above sea level. Geology The mountain is a part of a chain of dormant volcanic mountains spanning along the eastern part of the Golan Heights starting from Mount Ram in the north and ending on Tal Saki in the south. It is the northern neighbor of Mount Avital which shares the same volcanic magma source with it. Mount Bental was formed in a volcanic eruption that formed a scoria volcanic cone when the magma that tried to erupt from Mount Avital's top could not do so, and the pressure led to an eruption of the western side of Mount Avital and of Mount Bental. The Mountain Mount Bental is covered with Quercus calliprinos trees and on its top is an IDF stronghold which was built on an older Syrian stronghold, which is an attraction ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United Nations Disengagement Observer Force
The United Nations Disengagement Observer Force (UNDOF) is a United Nations peacekeeping mission tasked with maintaining the ceasefire between Israel and Syria in the aftermath of the 1973 Yom Kippur War. The mission was established by United Nations Security Council Resolution 350 on 31 May 1974, to implement Resolution 338 (1973) which called for an immediate ceasefire and implementation of United Nations Security Council Resolution 242. The resolution was passed on the same day as the Agreement on Disengagement. It was signed by Israeli and Syrian forces on the Golan Heights, finally establishing a ceasefire to end the war. From 1974 to 2012, UNDOF performed its functions with the full cooperation of both sides. Since 1974 its mandate has been renewed every six months. The United Nations Truce Supervision Organization (UNTSO) and UNDOF operate in a buffer zone between the two sides and continue to supervise the ceasefire. Before the Syrian Civil War, the situation in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jordan River
The Jordan River or River Jordan (, ''Nahr al-ʾUrdunn''; , ''Nəhar hayYardēn''), also known as ''Nahr Al-Sharieat'' (), is a endorheic river in the Levant that flows roughly north to south through the Sea of Galilee and drains to the Dead Sea. The river passes by or through Jordan, Syria, Israel, and the Palestinian territories. Jordan and the Israeli-occupied Golan Heights border the river to the east, while Israel and the Israeli-occupied West Bank lie to its west. Both Jordan and the West Bank derive their names in relation to the river. The river holds major significance in Judaism and Christianity. According to the Bible, the Israelites crossed it into the Promised Land and Jesus of Nazareth was baptized by John the Baptist in it. Etymology Several hypotheses for the origin of most of the river's names in modern languages (e.g., Jordan, Yarden, Urdunn), one is that it comes from Semitic 'Yard, on' 'flow down' <√ירד reflecting the river's declivity, possibly a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River
A river is a natural stream of fresh water that flows on land or inside Subterranean river, caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the Runoff (hydrology), runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their Bank (geography), banks and flood the surrounding area, spreading nutrients to the surrounding area. Sedime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long, large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known, amongst others, as brook, creek, rivulet, rill, run, tributary, feeder, freshet, narrow river, and streamlet. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snow
Snow consists of individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide, or Sublimation (phase transition), sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes Nucleation, nucleate around particles in the atmosphere by attracting supercooling, supercooled water droplets, which Freezing, freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns, and Hard rime, rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst Topography
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] |
Geologic Fault
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 geological 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 b ... [...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] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precipitation (meteorology)
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls from clouds due to gravitational pull. The main forms of precipitation include drizzle, rain, rain and snow mixed ("sleet" in Commonwealth usage), snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation; their water vapor does not condense sufficiently to precipitate, so fog and mist do not fall. (Such a non-precipitating combination is a colloid.) Two processes, possibly acting together, can lead to air becoming saturated with water vapor: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called shower (p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hermon Nature Reserve
Hermon nature reserve () is a nature reserve in the north of the Golan Heights. It includes an area in southern Mount Hermon Mount Hermon ( / ALA-LC: ('Mountain of the Sheikh', ), , ) is a mountain, mountain cluster constituting the southern end of the Anti-Lebanon mountain range. Its summit straddles the Lebanon–Syria border, border between Syria and Lebanon a ... which is located in the Israeli occupied portion of the Golan Heights. The reserve excludes the Mount Hermon ski resort, Neve Ativ and the Nimrod Fortress National Park. The total area of the reserve is approximately 78,270 dunam (19,340 acres). Flora and fauna The common birds in the reserve include white-throated robin, western rock nuthatch, sombre tit and northern wheatear. There are many species of butterflies, of which 23 are unique to the Hermon nature reserve and do not exist in pre-1967 Israel. The common reptiles in the reserve include the '' Vipera bornmuelleri'' and the four-lined sna ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
