Qattara Depression

Qattara Depression is located in Egypt

The Qattara Depression (Arabic: منخفض القطارةMunḫafaḍ al-Qaṭṭārah) is a depression in northwestern Egypt, specifically in the Matruh Governorate. The depression is part of the Western Desert of Egypt. The Qattara Depression lies below sea level, and its bottom is covered with salt pans, sand dunes, and salt marshes. The depression extends between the latitudes of 28°35' and 30°25' north and the longitudes of 26°20' and 29°02' east.[3]

The Qattara Depression was created by the interplay of salt weathering and wind erosion. Some 20 kilometres west of the depression lie the oases of Siwa in Egypt and Jaghbub in Libya in smaller but similar depressions.

The Qattara Depression contains the second lowest point in Africa at an altitude of 133 metres (436 ft) below sea level, the lowest point being Lake Assal in Djibouti. The depression covers about 19,605 square kilometres (7,570 sq mi), a size comparable with Lake Ontario or twice as large as Lebanon. Due to its size and proximity to the shores of the Mediterranean Sea, studies have been made for the potential to generate hydroelectricity here.

The Qattara Depression has the shape of a teardrop, with its point facing east and the broad deep area facing southwest. The northern side of the depression is characterised by steep escarpments up to 280 meters high, marking the edge of the adjacent El Diffa plateau. To the south the depression slopes gently up to the Great Sand Sea.

Within the Depression are salt marshes, under the northwestern and northern escarpment edges, and extensive dry lake beds that flood occasionally. The marshes occupy approximately 300 square kilometres (120 sq mi), although wind-blown sands are encroaching in some areas. About a quarter of the region is occupied by dry lakes composed of hard crust and sticky mud, and occasionally filled with water.

The depression was initiated by either wind or fluvial erosion in the late Neogene, but during the Quaternary Period the dominant mechanism was a combination of salt weathering and wind erosion working together. First, the salts break up the depression floor, then the wind blows away the resulting sands. This process is less effective in the eastern part of the depression, due to lower salinity groundwater.[4]

Groves of Acacia raddiana, growing in shallow sandy depressions, and Phragmites swamps represent the only permanent vegetation. The acacia groves vary widely in biodiversity and rely on runoff from rainfall and groundwater to survive. The Moghra Oasis in the northeastern part of the Depression has a four km2 brackish lake and a Phragmites swamp.[5][6]

This page was last edited on 14 July 2018, at 19:31 (UTC).
Reference: under CC BY-SA license.

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