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Nahal Paran
Nahal Paran ( he, נחל פארן, , Paran Stream) is a seasonal stream in Egypt's Sinai Peninsula and Israel's Negev Desert. With a length of 150 kilometers, it is the third largest watercourse in Israel after the Jordan River and Yarmouk River. It is also the widest watercourse in Israel. The association of the name "Paran Stream" with this specific wadi is a modern one. Israeli authorities have introduced the name "Paran Stream" by adopting it from the Paran Desert mentioned in the Hebrew Bible. However, the modern identification of the biblical Paran Desert with a specific part of the Sinai Peninsula might or might not be accurate. Hydrology The origin of the river is in the Paran Desert of the Sinai Peninsula, and it flows into the estuary of Nahal HaArava. Water flow exists only during flash floods. This is the drainage basin's largest river, with an area of thousands of square kilometers, creating broad planes that separate the Negev's high north and the Eilat moun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paran Desert
The Desert of Paran or Wilderness of Paran (also sometimes spelled Pharan or Faran; he, מִדְבַּר פָּארָן, ''Midbar Pa'ran''), is a location mentioned in the Hebrew Bible. It is one of the places where the Israelites spent part of their 40 years of wandering after the Exodus, and was also a home to Ishmael, and a place of refuge for David. In Islamic tradition, it has often been equated with an area of the Hejaz. Biblical Paran The Wilderness or Desert of Paran is said to be the place where Hagar (the Egyptian servant girl of Abraham's wife Sarah/Sarai and, by Sarah's suggestion, was made his wife and bore him a son Ishmael) was sent into exile from Abraham's dwelling in Beersheba (). Hagar "departed, and strayed in the wilderness of Beer-sheba" ():Then God opened her agar'seyes and she saw a well of water. So she went and filled the skin with water and gave the boy a drink. God was with the boy as he grew up. He lived in the desert and became an archer. While he ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arava Desert
The Arabah, Araba or Aravah ( he, הָעֲרָבָה, ''hāʿĂrāḇā''; ar, وادي عربة, ''Wādī ʿAraba''; lit. "desolate and dry area") is a loosely defined geographic area south of the Dead Sea basin, which forms part of the border between Israel to the west and Jordan to the east. The old meaning, which was in use up to the early 20th century, covered almost the entire length of what today is called the Jordan Rift Valley, running in a north–south orientation between the southern end of the Sea of Galilee and the northern tip of the Gulf of Aqaba of the Red Sea at Aqaba–Eilat. This included the Jordan River Valley between the Sea of Galilee and the Dead Sea, the Dead Sea itself, and what today is commonly called the Arava Valley. The contemporary use of the term is restricted to this southern section alone. Geography The Arabah is in length, from the Gulf of Aqaba to the southern shore of the Dead Sea. Topographically, the region is divided into three se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eilat
Eilat ( , ; he, אֵילַת ; ar, إِيلَات, Īlāt) is Israel's southernmost city, with a population of , a busy port and popular resort at the northern tip of the Red Sea, on what is known in Israel as the Gulf of Eilat and in Jordan as the Gulf of Aqaba. The city is considered a tourist destination for domestic and international tourists heading to Israel. Eilat is part of the Southern Negev Desert, at the southern end of the Arabah, adjacent to the Egyptian resort city of Taba to the south, the Jordanian port city of Aqaba to the east, and within sight of Haql, Saudi Arabia, across the gulf to the southeast. Eilat's arid desert climate and low humidity are moderated by proximity to a warm sea. Temperatures often exceed in summer, and in winter, while water temperatures range between . Eilat averages 360 sunny days a year. Name The name ''Eilat'' was given to ''Umm al-Rashrāsh'' () in 1949 by the Committee for the Designation of Place-Names in the Negev. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earth Surface Processes And Landforms
''Earth Surface Processes and Landforms'' is a peer-reviewed scientific journal published by John Wiley & Sons on behalf of the British Society for Geomorphology. It covers geomorphology and more in general all aspects of Earth sciences dealing with the Earth surface. The journal was established in 1976 as ''Earth Surface Processes'', obtaining its current name in 1981. The journal primarily publishes original research papers. It also publishes ''Earth Surface Exchanges'' which include commentaries on issues of particular geomorphological interest, discussions of published papers, shorter journal articles suitable for rapid publication, and commissioned reviews on key aspects of geomorphological science. Foci include the physical geography of rivers, valleys, glaciers, mountains, hills, slopes, coasts, deserts, and estuary environments, along with research into Holocene, Pleistocene, or Quaternary science. The editor-in-chief is Stuart Lane (University of Lausanne). Abstracting and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eilat Mountains
The Eilat Mountains ( he, הרי אילת ''Harei Eilat'') are a mountain range within the southern Negev in southern Israel. The ranges of the Timna Valley belong to the Eilat Mountains. Among the central block of mountains, Mount Hezekiah is the highest, followed by Mount Solomon. The mountains overlook the Gulf of Aqaba, which is part of the Red Sea. The rock formations in the Eilat mountains are a mix of granite, limestone, and sandstone, that can be described as "extremely colorful". Etymology The mountains are named after the nearby city of Eilat and the biblical name of the city Eilot (Eiloth), situated where today the city of Aqaba (Jordan) is located. Neighboring countries From the top of Mt. Tzfachot, in the southern tip of the mountain range, visitors may see Egyptian land (via the Sinai Peninsula) when looking southwestward. Visitors looking eastward, across the Gulf of Aqaba, may also see Jordanian land. On clear days, as well, Saudi Arabia can be seen, looking s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nahal HaArava
The Arava Stream ( he, נחל הערבה, Nahal HaArava) is an intermittent stream (occasionally flowing in the rainy, winter season) that flows from the approximate mid-point of the Arava desert in Israel's Southern District northward. It is 89 km long, and in many parts, serves as the actual border between Israel and Jordan. The stream originates on the crest of the Notza Ridge, which forms the watershed divide between the Dead Sea and the Red Sea, and from which all streams in the Arava desert flow either north to the Dead Sea or south to the Red Sea. The stream's prominent tributaries include: Nahal Paran, Nahal Barak, Nahal Tzin, Nahal Tzafit, and Nahal Nekorot. In addition to Israel and Jordan, parts of its drainage basin are in the Sinai Peninsula, Egypt. Northern flow The stream flows into the area of evaporation ponds in what used to be the southernmost end of the Dead Sea and divides these ponds into the Israel area (managed by the Dead Sea Works) and the Jordan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Estuary
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea level began to rise about 10,000–12,000 years ago. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns. They can have many different names, such as bays, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hebrew Bible
The Hebrew Bible or Tanakh (;"Tanach" ''Random House Webster's Unabridged Dictionary''. Hebrew: ''Tānāḵh''), also known in Hebrew as Miqra (; Hebrew: ''Mīqrā''), is the Biblical canon, canonical collection of Hebrew language, Hebrew scriptures, including the Torah, the Nevi'im, and the Ketuvim. Different branches of Judaism and Samaritanism have maintained different versions of the canon, including the 3rd-century Septuagint text used by Second-Temple Judaism, the Syriac language Peshitta, the Samaritan Torah, the Dead Sea Scrolls, and most recently the 10th century medieval Masoretic Text, Masoretic text created by the Masoretes currently used in modern Rabbinic Judaism. The terms "Hebrew Bible" or "Hebrew Canon" are frequently confused with the Masoretic text, however, this is a medieval version and one of several ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wadi
Wadi ( ar, وَادِي, wādī), alternatively ''wād'' ( ar, وَاد), North African Arabic Oued, is the Arabic term traditionally referring to a valley. In some instances, it may refer to a wet (ephemeral) riverbed that contains water only when heavy rain occurs. Etymology The term ' is very widely found in Arabic toponyms. Some Spanish toponyms are derived from Andalusian Arabic where ' was used to mean a permanent river, for example: Guadalcanal from ''wādī al-qanāl'' ( ar, وَادِي الْقَنَال, "river of refreshment stalls"), Guadalajara from ''wādī al-ḥijārah'' ( ar, وَادِي الْحِجَارَة, "river of stones"), or Guadalquivir, from ''al-wādī al-kabīr'' ( ar, اَلْوَادِي الْكَبِير, "the great river"). General morphology and processes Wadis are located on gently sloping, nearly flat parts of deserts; commonly they begin on the distal portions of alluvial fans and extend to inland sabkhas or dry lakes. In basin and r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nahal Paran Estuary
Nahal ( he, נח"ל) (acronym of ''Noar Halutzi Lohem'', lit. Fighting Pioneer Youth) is a program that combines military service with mostly social welfare and informal education projects such as youth movement activities, as well as training in entrepreneurship in urban development areas. Prior to the 1990s it was a paramilitary Israel Defense Forces program that combined military service and the establishment of agricultural settlements, often in peripheral areas. The Nahal groups of soldiers formed the core of the Nahal Infantry Brigade. History In 1948, a ''gar'in'' (core group) of Jewish pioneers wrote to Prime Minister David Ben-Gurion requesting that members be allowed to do their military service as a group rather than being split up into different units at random. In response to this letter, Ben-Gurion created the Nahal program, which combined military service and farming. Some 108 kibbutzim and agricultural settlements were established by the Nahal, many of them on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yarmouk River
The Yarmuk River ( ar, نهر اليرموك, translit=Nahr al-Yarmūk, ; Greek: Ἱερομύκης, ; la, Hieromyces or ''Heromicas''; sometimes spelled Yarmouk), is the largest tributary of the Jordan River. It runs in Jordan, Syria and Israel, and drains much of the Hauran plateau. Its main tributaries are the wadis of 'Allan and Ruqqad from the north, Ehreir and Zeizun from the east. Although it is narrow and shallow throughout its course, at its mouth it is nearly as wide as the Jordan, measuring thirty feet in breadth and five in depth. The once celebrated Matthew Bridge used to cross the Yarmuk at its confluence with the Jordan. History Yarmuk forms a natural border between the plains to the north - Hauran, Bashan and Golan - and the Gilead mountains to the south. Thus it has often served as boundary line between political entities. Neolithic The Yarmukian is a Pottery Neolithic culture that inhabited parts of Palestine and Jordan. Its type site is at Sha'ar HaGolan, on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
