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Fezzan Basin
The Fazzan Basin, or Fezzan Basin, is a large endorheic basin in Libya. It has no outlet to the sea and contains large areas of desert or semi-arid land. It is one of two basins in southern Libya on the northern flanks of the Tibesti Mountains in the central Sahara, Sahara desert, the other being the Kufra, Kufra Basin, further to the east. Formation The Fazzan Basin is situated on the junction between two Plate tectonics, tectonic plates. Collision between these occurred in the Paleozoic period and caused thickening of the Earth's crust, which then Isostasy, downwarped under its own weight to form a depression in the ground, the Fazzan Basin. Since then, there has been a deposition of "continental intercalaire" and other continental rocks, and large quantities of water have been trapped in underground aquifers. An outcrop of basalt occurs between the Fazzan and the Kufra Basins, and both are overlaid by sand. The climate of this region has varied greatly in the past, with pluvial ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Endorheic Basin
An endorheic basin ( ; also endoreic basin and endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water (e.g. rivers and oceans); instead, the water drainage flows into permanent and seasonal lakes and swamps that equilibrate through evaporation. Endorheic basins are also called closed basins, terminal basins, and internal drainage systems. Endorheic regions contrast with open lakes (exorheic regions), where surface waters eventually drain into the ocean. In general, water basins with subsurface outflows that lead to the ocean are not considered endorheic; but cryptorheic. Endorheic basins constitute local base levels, defining a limit of the erosion and deposition processes of nearby areas. Endorheic water bodies include the Caspian Sea, which is the world's largest inland body of water. Etymology The term ''endorheic'' derives from the French word , which combines ( 'within') and 'flow'. Endorheic lake ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Endorheic Basins Of Africa
An endorheic basin ( ; also endoreic basin and endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water (e.g. rivers and oceans); instead, the water drainage flows into permanent and seasonal lakes and swamps that wiktionary:equilibrate, equilibrate through evaporation. Endorheic basins are also called closed basins, terminal basins, and internal drainage systems. Endorheic regions contrast with open and closed lakes, open lakes (exorheic regions), where surface waters eventually drain into the ocean. In general, water basins with subsurface outflows that lead to the ocean are not considered endorheic; but cryptorheic. Endorheic basins constitute local base levels, defining a limit of the erosion and Deposition (geology), deposition processes of nearby areas. Endorheic water bodies include the Caspian Sea, which is the world's largest inland body of water. Etymology The term ''endorheic'' derives from the French ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Messinian
The Messinian is in the geologic timescale the last age or uppermost stage of the Miocene. It spans the time between 7.246 ± 0.005 Ma and 5.333 ± 0.005 Ma (million years ago). It follows the Tortonian and is followed by the Zanclean, the first age of the Pliocene. The Messinian overlaps the Turolian European Land Mammal Mega Zone (more precisely MN 12 and 13) and the Pontian Central European Paratethys Stage. It also overlaps the late Huayquerian and early Montehermosan South American Land Mammal Ages, and falls inside the more extensive Hemphillian North American Land Mammal Age. During the Messinian, around 6 million years ago, the Messinian salinity crisis took place, which brought about repeated desiccations of the Mediterranean Sea. Definition The Messinian was introduced by Swiss stratigrapher Karl Mayer-Eymar in 1867. Its name comes from the Italian city of Messina on Sicily, where the Messinian evaporite deposit is of the same age. The base of the Messinian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sahabi River
The Companions of the Prophet () were the Muslim disciples and followers of the Islamic prophet Muhammad who saw or met him during his lifetime. The companions played a major role in Muslim battles, society, hadith narration, and governance during and after the life of Muhammad. The era of the companions began following the death of Muhammad in 632 CE, and ended in 110 AH (728 CE) when the last companion Abu al-Tufayl died. Later Islamic scholars accepted their testimony of the words and deeds of Muhammad, the occasions on which the Quran was revealed and other important matters in Islamic history and practice. The testimony of the companions, as it was passed down through trusted chains of narrators ('' asānīd''), was the basis of the developing Islamic tradition. From the traditions (''hadith'') of the life of Muhammad and his companions are drawn the Muslim way of life (''sunnah''), the code of conduct (''sharia'') it requires, and Islamic jurisprudence (''fiqh''). The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
