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Jerusalem Mountains
The Judaean Mountains, or Judaean Hills ( he, הרי יהודה, translit=Harei Yehuda) or the Hebron Mountains ( ar, تلال الخليل, translit=Tilal al-Khalīl, links=, lit=Hebron Mountains), is a mountain range in Palestine and Israel where Jerusalem, Hebron and several other biblical cities are located. The mountains reach a height of . The Judean Mountains can be separated to 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 generally 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 count ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Nabi Yunis
Nabi Yunis ( ar, جبل النبي يونس) is the highest point of the Palestinian territories, with an altitude of 1,030 metres (3,380 ft). Peakbagger, retrieved 2012-10-14. It is located in the town of , . See also * Geography of the Palestinian territories * |
Israeli Coastal Plain
Israeli coastal plain ( he, מישור החוף, ''Mishor HaḤof'') is the coastal plain along Israel's Mediterranean Sea coast, extending north to south. It is a geographical region defined morphologically by the sea, in terms of topography and soil, and also in its climate, flora and fauna. It is narrow in the north and broadens considerably towards the south, and is continuous with the exception of the short section where Mount Carmel reaches almost all the way to the sea. The Coastal Plain is bordered to the east by – north to south – the topographically higher regions of the Galilee, the low and flat Jezreel Valley, the Carmel range, the mountains of Samaria, the hill country of Judea known as the Shephelah, and the Negev Mountains in the south. To the north it is separated from the coastal plain of Lebanon by the cliffs of Rosh HaNikra, which jut out into the sea from the Galilee mountains, but to the south it continues into the Egyptian Sinai Peninsula. The plain ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sinai Peninsula
The Sinai Peninsula, or simply Sinai (now usually ) (, , cop, Ⲥⲓⲛⲁ), is a peninsula in Egypt, and the only part of the country located in Asia. It is between the Mediterranean Sea to the north and the Red Sea to the south, and is a land bridge between Asia and Africa. Sinai has a land area of about (6 percent of Egypt's total area) and a population of approximately 600,000 people. Administratively, the vast majority of the area of the Sinai Peninsula is divided into two Governorates of Egypt, governorates: the South Sinai Governorate and the North Sinai Governorate. Three other governorates span the Suez Canal, crossing into African Egypt: Suez Governorate on the southern end of the Suez Canal, Ismailia Governorate in the center, and Port Said Governorate in the north. In the classical era the region was known as Arabia Petraea. The peninsula acquired the name Sinai in modern times due to the assumption that a mountain near Saint Catherine's Monastery is the Biblical ... [...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] |
Syrian Arc
The Syrian Arc is a series of fold structures that extend from Syria, through Lebanon and 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 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, with structures trending WSW–ENE ... [...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 strata, that are bent or curved during permanent 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''). Synsedimentary folds are those formed during sedimentary deposition. Folds form under varied conditions of stress, pore pressure, and temperature gradient, as evidenced by their presence in soft 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 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 fault (''fault bend fold''), at the tip of a propagating fault (''fault propagation fold''), by differential compaction or due to ... [...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 Grand Can ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestones
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 limestone co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hebron Hills
The Hebron Hills, also known as Mount Hebron ( ar, جبل الخليل, translit=Jabal al-Khalīl, he, הר חברון, translit=Har Hevron), are a mountain ridge, geographic region, and geologic formation, comprising the southern part of the Judean Mountains. The Hebron Hills are located in the southern West Bank. Geography The highest peak of the mountain ridge is in the Palestinian city of Halhul, where a tableland exists with an altitude of . History Iron Age The Book of Joshua mentions Maon, Carmel, Adora and Juttah among others as part of the tribal territory of the Tribe of Judah. The modern Arabic names of Ma'in, al-Karmil, Dura, and Yatta respectively preserve the ancient names. As the Nabataeans pushed northwards, the Edomites were driven out of old Edom to the south of the Dead Sea and into the southern Hebron Hills between the southern part of the Dead Sea and the Mediterranean, establishing new Edom or Idumaea. Hellenistic period During the Hellenistic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bethlehem
Bethlehem (; ar, بيت لحم ; he, בֵּית לֶחֶם '' '') is a city in the central West Bank, Palestine, about south of Jerusalem. Its population is approximately 25,000,Amara, 1999p. 18.Brynen, 2000p. 202. and it is the capital of the Bethlehem Governorate of the State of Palestine. The economy is primarily tourist-driven, peaking during the Christmas season, when Christians make pilgrimage to the Church of the Nativity. The important holy site of Rachel's Tomb is at the northern entrance of Bethlehem, though not freely accessible to the city's own inhabitants and in general Palestinians living in the Israeli-occupied West Bank due to the Israeli West Bank barrier. The earliest known mention of Bethlehem was in the Amarna correspondence of 1350–1330 BCE when the town was inhabited by the Canaanites. The Hebrew Bible, which says that the city of Bethlehem was built up as a fortified city by Rehoboam, identifies it as the city David was from and where he was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arad (Israel)
Arad ( he, עֲרָד ) is a city in the Southern District (Israel), Southern District of Israel. It is located on the border of the Negev and the Judaean Desert, Judean Deserts, west of the Dead Sea and east of Beersheba. The city is home to a diverse population of , including Ashkenazi Jews, Ashkenazi and Sephardi Jews, both secular and religious, Negev Bedouin, Bedouins and Black Hebrew Israelites, 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. 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 town located at Tel Arad (a Biblical archae ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Negev
The Negev or Negeb (; he, הַנֶּגֶב, hanNegév; ar, ٱلنَّقَب, an-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 city and port of Eilat. It contains several development towns, including Dimona, Arad and Mitzpe Ramon, as well as a number of small Bedouin towns, including Rahat and 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, David Ben-Gurion, after his retirement from politics. Although historically part of a separate region (known during the 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 Trans-Jordan's name". Despite this, the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
