Geography Of The Palestinian Territories
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Geography Of The Palestinian Territories
Geography of the State of Palestine refers to the geographic, climatic and other properties of the areas claimed by State of Palestine. Physiographic regions The terrain of the Gaza Strip is flat or rolling, with dunes near the coast. The highest point is Abu 'Awdah (Joz Abu 'Auda), at above sea level. The terrain of the West Bank is mostly rugged dissected upland, with some vegetation in the west, but somewhat barren in the east. The elevation span reaches from a low on the northern shore of the Dead Sea at below sea level, to the highest point at Mount Nabi Yunis at above sea level. The area of the West Bank is landlocked; the highlands are the main recharge area for Israel's coastal aquifers. Geology The coastal plain of Gaza is composed of sand dunes and fertile sandy sediments. Except for a porous calcareous sandstone called ''kurkar''_in_Arabic,_there_are_no_other_rocks_in_this_region._In_contrast,_the_West_Bank_is_dominated_by_low_mountains:_Mount_Gerizim.html" ...
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State Of Palestine
Palestine ( ar, فلسطين, Filasṭīn), Legal status of the State of Palestine, officially the State of Palestine ( ar, دولة فلسطين, Dawlat Filasṭīn, label=none), is a state (polity), state located in Western Asia. Officially governed by the Palestine Liberation Organization (PLO), it claims the West Bank, including East Jerusalem, and the Gaza Strip as its territory, though the entirety of that territory has been Israeli-occupied territories, occupied by Israel since the 1967 Six-Day War. As a result of the Oslo Accords of 1993–1995, the West Bank is currently divided into 165 Palestinian enclaves that are under partial Palestinian National Authority (PNA) rule; the remainder, including 200 Israeli settlement, Israeli settlements, is under Area C (West Bank), full Israeli control. The Gaza Strip has been ruled by the militant Islamic group Hamas and has been subject to Blockade of the Gaza Strip, a long-term blockade by Egypt and Israel since 2007. After W ...
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Jordan Valley (Middle East)
The Jordan Valley ( ar, غور الأردن, ''Ghor al-Urdun''; he, עֵמֶק הַיַרְדֵּן, ''Emek HaYarden'') forms part of the larger Jordan Rift Valley. Unlike most other river valleys, the term "Jordan Valley" often applies just to the lower course of the Jordan River, from the spot where it exits the Sea of Galilee in the north, to the end of its course where it flows into the Dead Sea in the south. In a wider sense, the term may also cover the Dead Sea basin and the Arabah valley, which is the rift valley segment beyond the Dead Sea and ending at Aqaba/Eilat, farther south. The valley, in the common, narrow sense, is a long and narrow trough, long if measured " as the crow flies", with a width averaging with some points narrowing to over most of the course, before widening out to a delta when reaching the Dead Sea. Due to meandering, the length of the river itself is . This is the valley with the lowest elevation in the world, beginning at below sea level ...
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List Of Lakes In Palestine
The following notable lakes are completely or partially within the borders of the State of Palestine: * Dead Sea * Marj Sanur ( seasonal lake) See also * {{Asia topic, List of lakes of * State of Palestine Lakes ...
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Syria
Syria ( ar, سُورِيَا or سُورِيَة, translit=Sūriyā), officially the Syrian Arab Republic ( ar, الجمهورية العربية السورية, al-Jumhūrīyah al-ʻArabīyah as-Sūrīyah), is a Western Asian country located in the Eastern Mediterranean and the Levant. It is a unitary republic that consists of 14 governorates (subdivisions), and is bordered by the Mediterranean Sea to the west, Turkey to the north, Iraq to the east and southeast, Jordan to the south, and Israel and Lebanon to the southwest. Cyprus lies to the west across the Mediterranean Sea. A country of fertile plains, high mountains, and deserts, Syria is home to diverse ethnic and religious groups, including the majority Syrian Arabs, Kurds, Turkmens, Assyrians, Armenians, Circassians, Albanians, and Greeks. Religious groups include Muslims, Christians, Alawites, Druze, and Yazidis. The capital and largest city of Syria is Damascus. Arabs are the largest ethnic group, and Mu ...
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Jordan
Jordan ( ar, الأردن; tr. ' ), officially the Hashemite Kingdom of Jordan,; tr. ' is a country in Western Asia. It is situated at the crossroads of Asia, Africa, and Europe, within the Levant region, on the East Bank of the Jordan River. Jordan is bordered by Saudi Arabia to the south and east, Iraq to the northeast, Syria to the north, and the Palestinian West Bank, Israel, and the Dead Sea to the west. It has a coastline in its southwest on the Gulf of Aqaba's Red Sea, which separates Jordan from Egypt. Amman is Jordan's capital and largest city, as well as its economic, political, and cultural centre. Modern-day Jordan has been inhabited by humans since the Paleolithic period. Three stable kingdoms emerged there at the end of the Bronze Age: Ammon, Moab and Edom. In the third century BC, the Arab Nabataeans established their Kingdom with Petra as the capital. Later rulers of the Transjordan region include the Assyrian, Babylonian, Roman, Byzantine, Rashidun ...
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Friends Of The Earth Middle East
EcoPeace Middle East, formerly Friends of the Earth Middle East (?–2014), is a regional environmental peacebuilding organization in the Middle East, bringing together Jordanians, Palestinians, and Israelis to create shared solutions for the most water-scarce region on the planet. Name EcoPeace was formed in 1994, bringing together Israelis, Palestinians, Egyptians and Jordanians in the wake of the Arab-Israeli peace processes of the 1990s. After joining the international Friends of the Earth network, EcoPeace became Friends of the Earth Middle East, but in 2014 it left the network, reverting to the initial name as EcoPeace Middle East. Description The people and wildlife of the region are dependent on many of the same natural resources. Shared surface and sub-surface freshwater basins, shared seas, common flora and fauna species and a shared air-shed are some of the characteristics that necessitate regional cooperation. As a tri-lateral organization that brings together Jord ...
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River Jordan
The Jordan River or River Jordan ( ar, نَهْر الْأُرْدُنّ, ''Nahr al-ʾUrdunn'', he, נְהַר הַיַּרְדֵּן, ''Nəhar hayYardēn''; syc, ܢܗܪܐ ܕܝܘܪܕܢܢ ''Nahrāʾ Yurdnan''), also known as ''Nahr Al-Sharieat'' ( ar, نهر الشريعة), is a river in the Middle East that flows roughly north to south through the Sea of Galilee (Hebrew: כנרת Kinneret, Arabic: Bohayrat Tabaraya, meaning Lake of Tiberias) and on to the Dead Sea. Jordan and the Golan Heights border the river to the east, while the West Bank and Israel lie to its west. Both Jordan and the West Bank take their names from 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. Geography The Jordan River has an upper course from its sources to the Sea of Galilee (via the Bethsaida Valley), and a lower course south of the ...
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Moment Magnitude Scale
The moment magnitude scale (MMS; denoted explicitly with or Mw, and generally implied with use of a single M for magnitude) is a measure of an earthquake's magnitude ("size" or strength) based on its seismic moment. It was defined in a 1979 paper by Thomas C. Hanks and Hiroo Kanamori. Similar to the local magnitude scale, local magnitude/Richter scale () defined by Charles Francis Richter in 1935, it uses a logarithmic scale; small earthquakes have approximately the same magnitudes on both scales. Despite the difference, news media often says "Richter scale" when referring to the moment magnitude scale. Moment magnitude () is considered the authoritative magnitude scale for ranking earthquakes by size. It is more directly related to the energy of an earthquake than other scales, and does not saturate—that is, it does not underestimate magnitudes as other scales do in certain conditions. It has become the standard scale used by seismological authorities like the U.S. Geological ...
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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 ...
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1033 Jordan Rift Valley Earthquake
An earthquake struck the Jordan Rift Valley on December 5, 1033 and caused extreme devastation in the Levant region. It was part of a sequence of four strong earthquakes in the region between 1033 AD and 1035 AD. Scholars have estimated the moment magnitude to be greater than 7.0 and evaluated the Modified Mercalli intensity to X (''Extreme''). It triggered a tsunami along the coast of modern-day Israel and Palestine, causing damage and fatalities. At least 70,000 people were killed in the disaster. Tectonic setting In the past 2,000 years of human history, documented earthquakes have been associated with the long Dead Sea Transform Fault System, a left-lateral transform boundary. Since the early Miocene, the fault system has accounted for between and of left-lateral displacement between the African and Arabian Plates. While left-lateral strike-slip is dominant, the fault also display features of normal and thrust faulting. The fault displays varying slip rates across its ...
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The Seventh Earthquake
A devastating earthquake known in scientific literature as the Earthquake of 749 struck on January 18, 749, in areas of the Umayyad Caliphate, with the epicenter in Galilee. The most severely affected areas were parts of Palestine and western Transjordan. The cities of Tiberias, Beit She'an, Pella, Gadara, and Hippos were largely destroyed while many other cities across the Levant were heavily damaged. The casualties numbered in the tens of thousands. There are firm reasons to believe that there were either two, or a series of earthquakes between 747 and 749, later conflated for different reasons into one, not least due to the use of different calendars in different sources.Karcz, 2004, p. 778-787 It seems probable that the second quake, centered more to the north, which created massive damage mainly in northern Israel and Jordan, did so not so much due to its catastrophic magnitude, but rather as a result of buildings being weakened by the previous, more southerly earthquake. I ...
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Arabian Plate
The Arabian Plate is a minor tectonic plate in the Northern and Eastern Hemispheres. It is one of the three continental plates (along with the African and the Indian Plates) that have been moving northward in geological history and colliding with the Eurasian Plate. That is resulting in a mingling of plate pieces and mountain ranges extending in the west from the Pyrenees, crossing Southern Europe to Iran, forming the Alborz and the Zagros Mountains, to the Himalayas and ranges of Southeast Asia. Lexicology The ''Arabian Plate'' is a designation of the region, and it is also sometimes referred to as the ''Arab Plate''. Borders The Arabian Plate consists mostly of the Arabian Peninsula; it extends westward to the Sinai Peninsula and the Red Sea and northward to the Levant. The plate borders are: *East, with the Indian Plate, at the Owen Fracture Zone *South, with the African Plate to the west and the Somali Plate and the Indian Plate to the east *West, a left lateral fa ...
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