Zobrazeno 1 - 10
of 21
pro vyhledávání: '"N. Abou Karaki"'
Autor:
R. A. Watson, E. P. Holohan, D. Al-Halbouni, L. Saberi, A. Sawarieh, D. Closson, H. Alrshdan, N. Abou Karaki, C. Siebert, T. R. Walter, T. Dahm
Publikováno v:
Solid Earth, Vol 10, Pp 1451-1468 (2019)
Enclosed topographic depressions are characteristic of karst landscapes on Earth. The developmental relationship between depression types, such as sinkholes (dolines) and uvalas, has been the subject of debate, mainly because the long developmental t
Externí odkaz:
https://doaj.org/article/b91f0ba555ca44309ed633ea2ffe77fa
Publikováno v:
Hydrology and Earth System Sciences, Vol 23, Pp 2111-2127 (2019)
The Dead Sea shore is a unique, young and dynamic salt karst system. Development of the area began in the 1960s, when the main water resources that used to feed the Dead Sea were diverted towards deserts, cities and industries. During the last decade
Externí odkaz:
https://doaj.org/article/280b3e4146844190bf934d6a90ccf1d0
Publikováno v:
Environmental Earth Sciences. 59:1417-1430
The level of the Dead Sea lowers 1 m/year and this rate is in acceleration. The decline is causing one of the major environmental disasters of the twenty-first century. The freshwater resources management policy of Israel, Jordan, and Palestine contr
Autor:
Damien Closson, N. Abou Karaki
Publikováno v:
Environmental Geology. 58:371-380
The Dead Sea is a terminal lake whose level is currently dropping at a rate of about 1 m per year due to the over exploitation of all its tributaries. The lowering started about four decades ago but geological hazards appeared more and more frequentl
Publikováno v:
Scopus-Elsevier
This work deals with the creation of a sinkholes database for the Jordanian coast of the Dead Sea, Ghor Al Haditha area. Ground collapses inventories were carried out between 1991 and 2012. The lineament is replaced and analyzed in its structural set
Publikováno v:
Bulletin of the Seismological Society of America. 101:926-927
Publikováno v:
Geophysical Journal International
Geophysical Journal International, 2000, ⟨10.1046/j.1365-246x.2000.00165.x⟩
Geophysical Journal International, Oxford University Press (OUP), 2000, ⟨10.1046/j.1365-246x.2000.00165.x⟩
Geophysical Journal International, 2000, ⟨10.1046/j.1365-246x.2000.00165.x⟩
Geophysical Journal International, Oxford University Press (OUP), 2000, ⟨10.1046/j.1365-246x.2000.00165.x⟩
The Araba valley lies between the southern tip of the Dead Sea and the Gulf of Aqaba. This depression, blanketed with alluvial and lacustrine deposits, is cut along its entire length by the Dead Sea fault. In many places the fault is well defined by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e6809f05379e0201a94bc7d3e2ac22a8
https://insu.hal.science/insu-01301465/document
https://insu.hal.science/insu-01301465/document
Publikováno v:
Geophysical Journal International
Geophysical Journal International, Oxford University Press (OUP), 2000, 142 (3), pp.769-782. ⟨10.1046/j.1365-246x.2000.00166.x⟩
Geophysical Journal International, 2000, 142 (3), pp.769-782. ⟨10.1046/j.1365-246x.2000.00166.x⟩
Geophysical Journal International, Oxford University Press (OUP), 2000, 142 (3), pp.769-782. ⟨10.1046/j.1365-246x.2000.00166.x⟩
Geophysical Journal International, 2000, 142 (3), pp.769-782. ⟨10.1046/j.1365-246x.2000.00166.x⟩
International audience; SUMMAR Y The Dead Sea fault zone is a major left-lateral strike-slip fault. South of the Dead Sea basin, the Wadi Araba fault extends over 160 km to the Gulf of Aqaba. The Dead Sea fault zone is known to have produced several
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3616633312036919475f3613f1ef156b
https://hal-insu.archives-ouvertes.fr/insu-01302207/document
https://hal-insu.archives-ouvertes.fr/insu-01302207/document
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