Contemporary evolution of the natural environment of the region between Antiatlas and Sahara (Morocco)
Skiba S., Krzemień K. (red.), 2008, Contemporary evolution of the natural environment of the region between Antiatlas and Sahara (Morocco), Prace Geograficzne, z. 118.
Język publikacji: angielski
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Morphostructural and geomorphological outline of Morocco
Recent erosion measurements in Morocco
Physical geography of the Coude du Dra region
Soils of the southern part of Morocco
Summary: Soils of the discussed area have been formed in the arid climatic conditions where evaporation prevails over precipitation. Those are the soils of the aridic and dry desert areas. Gypsisols prevail, also Calcisols can be found. Vast areas of the regions are covered by dune formations where initial Arenosols occur. Within the oasis where agricultural soils are subject to irrigation Solonchaks can be found. The existing described agricultural value of the discussed soils (Categories I-IV) is at present of very little use because of the strong desertification processes that take place in the investigation area.
Słowa kluczowe (w języku angielskim): Desert soils, Gypsisols, Arenosols
Prace Geograficzne, 2008, z. 118, s. 37-42.
Instytut Geografii i Gospodarki Przestrzennej UJ
Properties of the desert soils of the Mhamid area
Reasons for development of the dune fields in the Coude du Dra region
Extorted forms of aeolian accumulation in the Coude du Dra region
The source of the Aeolian sediments in the Coude du Dra region
Surface features of sand grains from the Coude du Dra region (Morocco)
The geomorphological role of episodic rivers based on the example of the Oueds el Mut and el Feija (AntiAtlas Mountains, Morocco)
Natural and anthropogenic factors of the development of Erg Chebbi
© IGiGP UJ "2019"