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When a fault block is raised or tilted, a block mountain can result. [17] Higher blocks are called horsts, and troughs are called grabens. A spreading apart of the surface causes tensional forces. When the tensional forces are strong enough to cause a plate to split apart, it does so such that a center block drops down relative to its flanking ...
Download as PDF; Printable version; ... Hebrew Bible mountains (9 C, 41 P) N. New Testament mountains (3 C, 8 P) This page was ...
The southern end of the mountain range is at Beersheba [6] [7] [8] in the northern part of the Negev, where the mountains slope down into the Beersheba-Arad valley. [citation needed] The average height of the Judaean Mountains is of 900 metres (2,953 ft), and they encompass the cities of Ramallah, Jerusalem, Bethlehem and Hebron.
The Shephelah (Biblical Hebrew: הַשְּפֵלָה, romanized: hašŠəp̄ēlā, lit. 'the Lowlands') or Shfela (Modern Hebrew: הַשְּׁפֵלָה, romanized: haŠfelá), or the Judaean Foothills [1] (Modern Hebrew: שְׁפֵלַת יְהוּדָה, romanized: Šfelát Yəhūdá), is a transitional region of soft-sloping rolling hills in south-central Israel stretching over 10–15 km ...
Fault blocks are very large blocks of rock, sometimes hundreds of kilometres in extent, created by tectonic and localized stresses in Earth's crust. Large areas of bedrock are broken up into blocks by faults. Blocks are characterized by relatively uniform lithology. The largest of these fault blocks are called crustal blocks.
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Abarim (Hebrew: הָעֲבָרִים, romanized: Hā-Avārīm) [1] [2] is the Hebrew name used in the Bible for a mountain range "across the Jordan", understood as east of the Jordan Rift Valley, i.e. in Transjordan, to the east and south-east of the Dead Sea, extending from Mount Nebo — its highest point — in the north, perhaps to the Arabian desert in the south.
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