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Judean Desert
The Judaean Desert or Judean Desert ( he, מִדְבַּר יְהוּדָה, Midbar Yehuda}, both ''Desert of Judah'' or ''Judaean Desert''; ar, صحراء يهودا, Sahraa' Yahuda) is a desert in Palestine and Israel that lies east of Jerusalem and descends to the Dead Sea. Under the name El-Bariyah, it has been nominated to the Tentative List of World Heritage Sites in the State of Palestine, particularly for its monastic ruins. Etymology The term he, מִדְבַּר יְהוּדָה, , Desert of Judaea originates in the Hebrew Bible, and it is mentioned in Judges and Psalms. It is sometimes known as he2, יְשִׁימוֹן ''Yeshimon'', meaning ''desert'' or ''wildland'', or yet ''Wilderness of Judah'' or ''Wilderness of Judaea'', among others. Geography The Judaean Desert lies east of Jerusalem and descends to the Dead Sea. The Judaean Desert stretches from the northeastern Negev to the east of Beit El, and is marked by natural terraces with escarpments. I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Judea 2 By David Shankbone
Judea or Judaea ( or ; from he, יהודה, Standard ''Yəhūda'', Tiberian ''Yehūḏā''; el, Ἰουδαία, ; la, Iūdaea) is an ancient, historic, Biblical Hebrew, contemporaneous Latin, and the modern-day name of the mountainous southern part of the modern States of Palestine and Israel. The name originates from the Hebrew name Yehudah, a son of the biblical patriarch Jacob/Israel, with Yehudah's progeny forming the biblical Israelite tribe of Judah (Yehudah) and later the associated Kingdom of Judah. Related nomenclature continued to be used by the Babylonians, Persian, Hellenistic, and Roman periods as the Babylonian and Persian Yehud, Hasmonean Kingdom of Judea, and consequently Herodian and Roman Judea, respectively. Under Hasmonean, Herodian and Roman rule, the term was applied to an area larger than the historical region of Judea. In 132 AD, the province of Judaea was merged with Galilee into an enlarged province named Syria Palaestina. The term ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Escarpment
An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations. The terms ''scarp'' and ''scarp face'' are often used interchangeably with ''escarpment''. Some sources differentiate the two terms, with ''escarpment'' referring to the margin between two landforms, and ''scarp'' referring to a cliff or a steep slope. In this usage an escarpment is a ridge which has a gentle slope on one side and a steep scarp on the other side. More loosely, the term ''scarp'' also describes a zone between a coastal lowland and a continental plateau which shows a marked, abrupt change in elevation caused by coastal erosion at the base of the plateau. Formation and description Scarps are generally formed by one of two processes: either by differential erosion of sedimentary rocks, or by movement of the Earth's crust at a geologic fault. The first process is the more common type: the escarpment is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Hyrax
The rock hyrax (; ''Procavia capensis''), also called dassie, Cape hyrax, rock rabbit, and (in the King James Bible) coney, is a medium-sized terrestrial mammal native to Africa and the Middle East. Commonly referred to in South Africa as the dassie (; af, klipdassie), it is one of the five living species of the order Hyracoidea, and the only one in the genus ''Procavia''. Rock hyraxes weigh and have short ears and tails. Rock hyraxes are found at elevations up to above sea level in habitats with rock crevices, allowing them to escape from predators. They are the only extant terrestrial afrotherians in the Middle East. Hyraxes typically live in groups of 10–80 animals, and forage as a group. They have been reported to use sentries to warn of the approach of predators. Having incomplete thermoregulation, they are most active in the morning and evening, although their activity pattern varies substantially with season and climate. Over most of its range, the rock hyrax is n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Steppe Climate
A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes. Defining attributes of semi-arid climates A more precise definition is given by the Köppen climate classification, which treats steppe climates (''BSk'' and ''BSh'') as intermediates between desert climates (BW) and humid climates (A, C, D) in ecological characteristics and agricultural potential. Semi-arid climates tend to support short, thorny or scrubby vegetation and are usually dominated by either grasses or shrubs as it usually can't support forests. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. The method used to find the precipitation threshold (in millimeters): *mult ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Desert Climate
The desert climate or arid climate (in the Köppen climate classification ''BWh'' and ''BWk''), is a dry climate sub-type in which there is a severe excess of evaporation over precipitation. The typically bald, rocky, or sandy surfaces in desert climates are dry and hold little moisture, quickly evaporating the already little rainfall they receive. Covering 14.2% of earth's land area, hot deserts are the second most common type of climate on earth after the polar climate. There are two variations of a desert climate according to the Köppen climate classification: a hot desert climate (''BWh''), and a cold desert climate (''BWk''). To delineate "hot desert climates" from "cold desert climates", there are three widely used isotherms: most commonly a mean annual temperature of , or sometimes the coldest month's mean temperature of , so that a location with a ''BW'' type climate with the appropriate temperature above whichever isotherm is being used is classified as "hot arid sub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mediterranean Climate
A Mediterranean climate (also called a dry summer temperate climate ''Cs'') is a temperate climate sub-type, generally characterized by warm, dry summers and mild, fairly wet winters; these weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location. This climate type's name is in reference to the coastal regions of the Mediterranean Sea within the Mediterranean Basin, where this climate type is most prevalent. The "original" Mediterranean zone is a massive area, its western region beginning with the Iberian Peninsula in southwestern Europe and coastal regions of northern Morocco, extending eastwards across southern Europe, the Balkans, and coastal Northern Africa, before reaching a dead-end at the Levant region's coastline. Mediterranean climate zones are typically located along the western coasts of landmasses, between roughly 30 and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rainshadow Effect
A rain shadow is an area of significantly reduced rainfall behind a mountainous region, on the side facing away from prevailing winds, known as its leeward side. Evaporated moisture from water bodies (such as oceans and large lakes) is carried by the prevailing onshore breezes towards the drier and hotter inland areas. When encountering elevated landforms, the moist air is driven upslope towards the peak, where it expands, cools, and its moisture condenses and starts to precipitate. If the landforms are tall and wide enough, most of the humidity will be lost to precipitation over the windward side (also known as the ''rainward'' side) before ever making it past the top. As the air descends the leeward side of the landforms, it is compressed and heated, producing foehn winds that ''absorb'' moisture downslope and cast a broad "shadow" of dry climate region behind the mountain crests. This climate typically takes the form of shrub–steppe, xeric shrublands or even deser ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Judea
Judea or Judaea ( or ; from he, יהודה, Standard ''Yəhūda'', Tiberian ''Yehūḏā''; el, Ἰουδαία, ; la, Iūdaea) is an ancient, historic, Biblical Hebrew, contemporaneous Latin, and the modern-day name of the mountainous southern part of the modern States of Palestine and Israel. The name originates from the Hebrew name Yehudah, a son of the biblical patriarch Jacob/Israel, with Yehudah's progeny forming the biblical Israelite tribe of Judah (Yehudah) and later the associated Kingdom of Judah. Related nomenclature continued to be used by the Babylonians, Persian, Hellenistic, and Roman periods as the Babylonian and Persian Yehud, Hasmonean Kingdom of Judea, and consequently Herodian and Roman Judea, respectively. Under Hasmonean, Herodian and Roman rule, the term was applied to an area larger than the historical region of Judea. In 132 AD, the province of Judaea was merged with Galilee into an enlarged province named Syria Palaestina. The ter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ein-Gedi
Ein Gedi ( he, עֵין גֶּדִי, ), also spelled En Gedi, meaning "spring of the kid", is an oasis, an archeological site and a nature reserve in Israel, located west of the Dead Sea, near Masada and the Qumran Caves. Ein Gedi, a kibbutz, was established nearby in 1954. Ein Gedi is a popular tourist attraction, and was listed in 2016 as one of the most popular nature sites in Israel. The site attracts about one million visitors a year. Etymology The name ''Ein Gedi'' is composed of two words (In both Arabic and Hebrew): ''ein'' means spring or a fountain and ''gǝdi'' means goat-kid. Ein Gedi thus means "kid spring" or "fountain of the kid". History and archaeology Neolithic At Mikveh Cave archaeologists found Pre-Pottery Neolithic A (PPNA) flint tools and an arrowhead. Chalcolithic A Chalcolithic temple (ca. mid-fourth millennium BCE) belonging to the Ghassulian culture was excavated on the slope between two springs, Ein Shulamit and Ein Gedi. More Chalcolit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hebrew University Of Jerusalem
The Hebrew University of Jerusalem (HUJI; he, הַאוּנִיבֶרְסִיטָה הַעִבְרִית בִּירוּשָׁלַיִם) is a public research university based in Jerusalem, Israel. Co-founded by Albert Einstein and Dr. Chaim Weizmann in July 1918, the public university officially opened in April 1925. It is the second-oldest Israeli university, having been founded 30 years before the establishment of the State of Israel but six years after the older Technion university. The HUJI has three campuses in Jerusalem and one in Rehovot. The world's largest library for Jewish studies—the National Library of Israel—is located on its Edmond J. Safra campus in the Givat Ram neighbourhood of Jerusalem. The university has five affiliated teaching hospitals (including the Hadassah Medical Center), seven faculties, more than 100 research centers, and 315 academic departments. , one-third of all the doctoral candidates in Israel were studying at the HUJI. Among its fi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Judaean 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 country of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
