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Judaean Desert Location of Judaean Desert in Israel and the West Bank in red. The Judaean Desert or Judean Desert (Hebrew: מִדְבַּר יְהוּדָה, romanized: Midbar Yehuda, Arabic: برية الخليل, romanized: Bariyat al-Khalil [clarification needed]) is a desert in the West Bank and Israel that stretches east of the ridge of the Judaean Mountains and in their rain shadow, so ...
Technically, however, the Arava is a separate desert with its own unique climate and ecology. A 250 MW solar park in Ashalim , an area in the northern Negev, the Ashalim Power Station , produces 121 Megawatts of power, using solar mirrors and thermal water heating.
This page is subject to the extended confirmed restriction related to the Arab-Israeli conflict. Geography of Israel Continent Asia Region Levant Coordinates 31°N 35°E / 31°N 35°E / 31; 35 Area Ranked 150th • Total 20,770 km 2 (8,020 sq mi) • Land 97.88% • Water 2.12% Coastline 273 km (170 mi) Borders Egypt: 208 km Jordan: 307 km Lebanon: 81 km Syria: 83 km West Bank: 330 ...
Get the Desert Area, Amman local weather forecast by the hour and the next 10 days.
Judea is a mountainous region, part of which is considered a desert. It varies greatly in height, rising to an altitude of 1,020 metres (3,350 ft) in the south at the Hebron Hills , 30 km (19 mi) southwest of Jerusalem , and descending to as much as 400 metres (1,300 ft) below sea level in the east of the region.
The Judaean Desert, the Dead Sea and the western slopes of the Moab Mountains on the opposite side are rain-shadowed by the Judaean Mountains. [citation needed] The Dasht-i-Lut in Iran is in the rain shadow of the Elburz and Zagros Mountains and is one of the most lifeless areas on Earth.
The "Lot's Wife" pillar on Mount Sodom, Israel, made of halite Salt cave in Mount Sodom Bedded halite at Mount Sodom. Mount Sodom (Hebrew: הר סדום, Har Sedom) is a hill along the southwestern part of the Dead Sea in Israel; it is part of the Judaean Desert Nature Reserve. [1]
To delineate "hot desert climates" from "cold desert climates", a mean annual temperature of 18 °C (64.4 °F) is used as an isotherm so that a location with a BW type climate with the appropriate temperature above this isotherm is classified as "hot arid subtype" (BWh), and a location with the appropriate temperature below the isotherm is ...