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In Ancient Egypt, Hammamat was a major quarrying area for the Nile Valley.Quarrying expeditions to the Eastern Desert are recorded from the second millennia BCE, where the wadi has exposed Precambrian rocks of the Arabian-Nubian Shield.
Deserts of Egypt, barren areas of landscape where little precipitation occurs and, consequently, living conditions are hostile for plant and animal life. Wikimedia Commons has media related to Deserts of Egypt .
The Moghra Oasis is an uninhabited oasis in the northeastern part of the Qattara Depression in the Western Desert of Egypt. It has a 4 km 2 (1.5 sq mi) lake containing brackish water, salt marshes and a swamp with reeds .
[2]: 90 Egypt leads Africa in the extraction of both talc and gypsum. It is second in salt production, third for phosphate and vermiculite, and fourth for iron ore. [3] Egypt also extracts oil, and is the largest non-OPEC producer of oil in Africa. Additionally, Egypt also produces the second most natural gas in Africa.
In Ancient Egypt, the oasis had two names.The name 'ḏsḏs' is first mentioned on a scarab dating back to the Middle Kingdom.In the New Kingdom, this name is rarely found, although it does appear for example in the Temple of Luxor and in the account of King Kamose, who occupied the oasis during the war against the Hyksos.
Siwa is an oasis located in Egypt, about 50 km (30 mi) east of the Libyan border, in the eastern part of the Great Sand Sea or Egyptian Sand Sea. Although well-known to the Tuareg and traders who traveled with caravans across the Sahara , Friedrich Gerhard Rohlfs was the first European to document the Great Sand Sea.
When the flow of dry air continuously blows over vast desert regions, it picks up fine sand and dust particles and finally results in a dusty wind which is generally felt in the periphery of the desert. When this wind blows over Egypt, it causes high temperatures to soar temporarily at dangerous levels, usually over 49–50 °C (120–122 °F ...
The Black Desert (الصحراء السوداء) is a region of volcano-shaped and widely spaced mounds, distributed along about 30 km (19 mi) in the Western Desert between the White Desert in the south and the Bahariya Oasis in the north. Most of its mounds are capped by basalt sills, giving them the characteristic black color.