The White Desert, known locally as Sahara el Beyda, lies about 45 kilometers north of the town of Farafra in Egypt's Western Desert, protected today as a national park covering roughly 300 square kilometers within a wider expanse of chalk and limestone terrain. Its landscape is built from layers of chalk and limestone laid down by an ancient sea during the Cretaceous period, between roughly 145 and 66 million years ago, later uplifted and exposed to the elements. Because chalk and limestone are relatively soft and porous, they erode readily under wind-driven sand and occasional rain, and centuries of that erosion have carved the rock into ventifacts, the wind-sculpted forms that give the desert its recognizable mushroom- and chicken-shaped outcrops of chalky white and cream stone standing out against the surrounding sand. This entity documents the White Desert specifically as a geological formation shaped by wind erosion of an ancient marine chalk and limestone deposit.
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Protected StatusNational Park or Reserve 1 Connections
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Source Wikipedia: White Desert National Park
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Source Wikipedia: White Desert National Park
Source Wikipedia: White Desert National Park
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Source Wikipedia: White Desert National ParkLeadQuote, Lead
Sahara el Beyda, the White Desert Protected Area, is a national park in Egypt, first established as a protected area in 2002.
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1. Wikipedia: White Desert National Park
Lead paragraph
Sahara el Beyda, the White Desert Protected Area, is a national park in Egypt, first established as a protected area in 2002.
Associated With: Chalk, Article text, rock Chalk
The park is the site of large white chalk rock formations, created through erosion by wind and sand, "one of the most important karst massifs in the Western Desert.
Caused By: Erosion, Article text, process Erosion
The park is the site of large white chalk rock formations, created through erosion by wind and sand, "one of the most important karst massifs in the Western Desert.
Caused By: Karstification, Article text, process Karstification
The park is the site of large white chalk rock formations, created through erosion by wind and sand, "one of the most important karst massifs in the Western Desert.
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