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Jerusalem Hills
The Judaean Mountains, or Judaean Hills (, or ,) are a mountain range in the West Bank and Israel where Jerusalem, Bethlehem, Hebron and several other biblical sites are located. The mountains reach a height of . The Judean Mountains can be divided into a number of sub-regions, including the Mount Hebron ridge, the Jerusalem ridge and the Judean slopes. The Judaean Mountains formed the heartland of the Kingdom of Judah (930–586 BCE), where the earliest Jewish settlements emerged, and from which Jews are originally descended. Geography The Judaean Mountains are part of a more extended range that runs in a north-south direction. The ridge consists of the Samarian Hills in its northern part, and of the Judaean Mountains in its southern part, the two segments meeting at the latitude of Ramallah. The westward descent from the hard limestone country of the Judaean mountains towards the coastal plain is by way of a longitudinal trough of fosse cut through chalk, followed by the low ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Nabi Yunis, Palestine
Nabi Yunis () is the highest point of the Judean Mountains and the southern portion of the West Bank, with an altitude of 1,030 metres (3,380 ft). Peakbagger, retrieved 2012-10-14. It is located in the town of Halhul, Hebron Governorate. See also * Geography of the Palestinian territories * Geography of the West Bank * Tall Asur, one of the highest points in the West Bank (1,016 m / 3,333 ft) * List of countries by highest point#Countries with disputed sovereignty, List of countries by highest point (Countries with disputed sovereignty)References Mountains of the West Bank Highest points of countries {{palestine-geo-stub ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Samarian Hills
Samaria (), the Hellenized form of the Hebrew name Shomron (), is used as a historical and biblical name for the central region of the Land of Israel. It is bordered by Judea to the south and Galilee to the north. The region is known to the Palestinians in Arabic under two names, Samirah (, ''as-Sāmira''), and Mount Nablus (جَبَل نَابُلُس, ''Jabal Nābulus''). The first-century historian Josephus set the Mediterranean Sea as its limit to the west, and the Jordan River as its limit to the east. Its territory largely corresponds to the biblical allotments of the tribe of Ephraim and the western half of Manasseh. It includes most of the region of the ancient Kingdom of Israel, which was north of the Kingdom of Judah. The border between Samaria and Judea is set at the latitude of Ramallah. The name "Samaria" is derived from the ancient city of Samaria, capital of the northern Kingdom of Israel. The name Samaria likely began being used for the entire kingdom not ... [...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] |
Syrian Arc
The Syrian Arc is a series of fold structures that extend from Syria, through Lebanon and Israel/Palestine into northern Sinai and on into Egypt's Eastern and Western deserts. The folds started forming during the Late Cretaceous epoch as a result of the closure of the Neotethys Ocean that caused shortening of the continental margin with reactivation of the extensional faults formed during the Jurassic period. Extent The furthest west that folds have been attributed to the Syrian Arc deformation phase is in the northern Western Desert near Matruh. The area of folding continues to the east forming a broad zone about 200 km wide passing into the Eastern Desert, including major structures such as Kattaniya and the breached anticline at Wadi Araba, near the Dead Sea on the western side of the Gulf of Suez. In Sinai, a series of other breached anticlinal structures are developed, such as those at Halal, Maghara and Yelleg. Geometry The Syrian Arc has an overall S-shape, wit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fold (geology)
In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary rock, sedimentary stratum, strata, that are bent or curved (''"folded"'') during permanent deformation (engineering), deformation. Folds in rocks vary in size from microscopic crinkles to mountain-sized folds. They occur as single isolated folds or in periodic sets (known as ''fold trains''). wikt:synsedimentary, Synsedimentary folds are those formed during sedimentary deposition. Folds form under varied conditions of stress (physics), stress, pore pressure, and temperature gradient, as evidenced by their presence in soft sedimentary rock, sediments, the full spectrum of metamorphic rocks, and even as primary flow structures in some igneous rocks. A set of folds distributed on a regional scale constitutes a fold belt, a common feature of orogeny, orogenic zones. Folds are commonly formed by shortening of existing layers, but may also be formed as a result of displacement on a non-planar f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monocline
A monocline (or, rarely, a monoform) is a step-like fold in rock strata consisting of a zone of steeper dip within an otherwise horizontal or gently dipping sequence. Formation Monoclines may be formed in several different ways (see diagram) * By differential compaction over an underlying structure, particularly a large fault at the edge of a basin due to the greater compactibility of the basin fill, the amplitude of the fold will die out gradually upwards. * By mild reactivation of an earlier extensional fault during a phase of inversion causing folding in the overlying sequence. * As a form of fault propagation fold during upward propagation of an extensional fault in basement into an overlying cover sequence. * As a form of fault propagation fold during upward propagation of a reverse fault in basement into an overlying cover sequence. Examples * Waterpocket Fold in Capitol Reef National Park, Utah * Comb Ridge in southern Utah * Grandview-Phantom Monocline in Gra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestones
Limestone 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 calcium carbonate . 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 limestone co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hebron Hills
The Hebron Hills, also known as Mount Hebron (, ), are a mountain ridge, geographic region, and geologic formation, constituting the southern part of the Judaean Mountains, Judean Mountains. The Hebron Hills are located in the southern West Bank. During the History of ancient Israel and Judah, Iron Age, the Hebron Hills were part of the Kingdom of Judah, which underwent a forced exile after being conquered by the Neo-Babylonian Empire, Babylonians. Subsequently, in the Hellenistic period, an Edom, Edomite population migrating to the area became dominant, leading to its being referred to as ''Idumaea''. The Edomites later converted to Judaism and assimilated into the Jewish population. Despite many settlements being destroyed or abandoned due to the brutal suppression of the Bar Kokhba revolt, Bar Kokhva revolt, a Jewish presence persisted in the area. In the Late Roman and Byzantine Empire, Byzantine periods, the Hebron Hills were divided demographically into a Christian northe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arad (Israel)
Arad ( ) is a city in the Southern District of Israel. It is located on the border of the Negev and the Judaean deserts, west of the Dead Sea and east of Beersheba. The city is home to a diverse population of in , including Ashkenazi and Sephardi Jews (both secular and religious), Bedouins and Black Hebrews, as well as new immigrants. After attempts to settle the area in the 1920s, Arad was founded in November 1962 as an Israeli development town, the first planned city in Israel. Arad's population grew significantly with the Aliyah from the former Soviet Union. It became a city in 1995. Landmarks in Arad include the ruins of Tel Arad, Arad Park, a domestic airfield and Israel's first legal race circuit. The city is known for its annual summer music festival, the Arad Festival. History Antiquity Arad is named after the Biblical Bronze Age Canaanite and later Israelite town located at Tel Arad (a Biblical archaeology site famous for the discovery of ostraca), which is loc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Negev
The Negev ( ; ) or Naqab (), is a desert and semidesert region of southern Israel. The region's largest city and administrative capital is Beersheba (pop. ), in the north. At its southern end is the Gulf of Aqaba and the resort town, resort city and port of Eilat. It contains several development towns, including Dimona, Arad, Israel, Arad, and Mitzpe Ramon, as well as a number of small Negev Bedouin, Bedouin towns, including Rahat, Tel Sheva, and Lakiya. There are also several kibbutzim, including Revivim and Sde Boker; the latter became the home of Israel's first Prime Minister of Israel, prime minister, David Ben-Gurion, after his retirement from politics. Although historically part of a separate region (known during the Roman Empire, Roman period as Arabia Petraea), the Negev was added to the proposed area of Mandatory Palestine, of which large parts later became Israel, on 10 July 1922, having been conceded by British representative St John Philby "in Emirate of Transjordan, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beersheba
Beersheba ( / ; ), officially Be'er-Sheva, is the largest city in the Negev desert of southern Israel. Often referred to as the "Capital of the Negev", it is the centre of the fourth-most populous metropolitan area in Israel, the eighth-most populous Israeli city with a population of , and the second-largest city in area (after Jerusalem), with a total area of 117,500 dunams (45 mi2 / 117.5 km2). Human habitation near present-day Beersheba dates back to the fourth millennium BC. In the Bible, Beersheba marks the southern boundary of ancient Israel, as mentioned in the phrase " From Dan to Beersheba." Initially assigned to the Tribe of Judah, Beersheba was later reassigned to Simeon. During the monarchic era, it functioned as a royal city but eventually faced destruction at the hands of the Assyrians. The Biblical site of Beersheba is Tel Be'er Sheva, lying some 2.5 miles (4km) distant from the modern city, which was established at the start of the 20th century by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jordan Rift Valley
The Jordan Rift Valley, also Jordan Valley ( ''Bīqʿāt haYardēn'', Al-Ghor or Al-Ghawr), is an elongated endorheic basin located in modern-day Israel, Jordan and the West Bank, Palestine. This geographic region includes the entire length of the Jordan River – from its sources, through the Hula Valley, the Korazim block, the Sea of Galilee, the Jordan Valley (Middle East), (Lower) Jordan Valley, all the way to the Dead Sea, the lowest land elevation on Earth – and then continues through the Arabah depression, the Gulf of Aqaba whose shorelines it incorporates, until finally reaching the Red Sea proper at the Straits of Tiran. History and physical features The Jordan Rift Valley was formed many millions of years ago in the Miocene epoch (23.8 – 5.3 Myr ago) when the Arabian plate moved northward and then eastward away from Africa. One million years later, the land between the Mediterranean Sea, Mediterranean and the Jordan Rift Valley rose so that the sea water stoppe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
