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
Properties of the desert soils of the Mhamid area
Summary: Research has been carried out in the area situated on the border of the Antiatlas Mountains on vast and geologically and geomorphologically differentiated region of the Sahara Desert. Typical soil profiles of the investigated desert soils (Gypsisols, Arenosols, Solonchaks) have been shown and described. For the chosen soils and dunes a mineral composition analysis has been made. In the mineral composition quartz together with calcium minerals (gypsum, calcite) prevail. In the soils and dunes of the Iriqui Lake area also feldspars and micas can be found as well as ferruginous lithoclasts.
Słowa kluczowe (w języku angielskim): Antiatlas, Desert soils.
Prace Geograficzne, 2008, z. 118, s. 43-50.
Instytut Geografii i Gospodarki Przestrzennej UJ
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
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