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Tushka Depression

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Journal Article
Journal: Geosphere
Published: 01 April 2008
Geosphere (2008) 4 (2): 375-386.
... water spilled northwestward toward the Tushka depression due to an unusual water rise in Lake Nasser induced by high precipitation in the Ethiopian Highlands. Five lakes were formed in local depressions underlain by an impermeable Paleocene shale and chalk formation. The lakes developed through three...
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Journal Article
Journal: Geology
Published: 01 December 2010
Geology (2010) 38 (12): 1135-1138.
... Topography Mission (SRTM) data at the available 3 arc-second (90 m) spatial resolution (see the GSA Data Repository 1 ) to delineate the topography and surficial deposits of the Kiseiba-Tushka depression, bounded by Kiseiba Oasis on the west, Wadi Tushka on the east, the Egyptian western limestone plateau...
FIGURES
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Figure 8. ( continued ). (D) North-south geological cross sections showing ...
in > Geosphere
Published: 01 April 2008
Figure 8. ( continued ). (D) North-south geological cross sections showing morphological, geological, and structural features in the Tushka depression and their relation to the distribution of the New Lakes of Sahara. The locations of the cross-section baselines are shown in A.
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Figure 2. A 7–4-2 Landsat Enhanced Thematic Mapper Plus (ETM+) mosaic produ...
in > Geosphere
Published: 01 April 2008
Figure 2. A 7–4-2 Landsat Enhanced Thematic Mapper Plus (ETM+) mosaic produced from images acquired between 2001 and 2002 showing physiographic features of Egypt and the location of the New Lakes of Sahara within the Tushka depression west of Lake Nasser. Box shows location of Figure 3 .
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Figure 3. A 7–4-2 Landsat Enhanced Thematic Mapper Plus (ETM+) image acquir...
in > Geosphere
Published: 01 April 2008
narrow conduits. The lakes were formed within the Tushka depression, which is bound in the north by the Kalabsha fault zone, which represents the southern escarpment of the Sin El Kaddab Plateau. See Figure 2 for location.
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Figure 7. (A) Hill-shade digital elevation model (DEM) covering the New Lak...
in > Geosphere
Published: 01 April 2008
Figure 7. (A) Hill-shade digital elevation model (DEM) covering the New Lakes of Sahara within the Tushka depression extracted from the Shuttle Radar Topography Mission (SRTM) data, which were acquired in April 2000. The hill-shade DEM was developed through 135° sun azimuth and 20° sun angle
Journal Article
Published: 01 June 2014
South African Journal of Geology (2014) 117 (1): 97-108.
... 3 ). This tectonic setting regulates a potential recharge from the occasional rains that fall on the high rising Red Sea hills in the Eastern desert into the local tectonic depressions. This also portrays the extent of the groundwater basin, which is regulated by synclinal folding and an associated...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 2018
AAPG Bulletin (2018) 102 (2): 175-193.
... of 320,000 km 2 (123,000 mi 2 ), is a large sedimentary basin located in the western part of the North China block ( Yang et al., 2005 ), and it can be divided into six geological structural units: the Yimeng uplift, Jinxi fold belt, Yishan slope, Tianhuan depression, Western thrust belt, and Wei River...
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