Abstract
A desert can be defined as a continental area on which there is a little or no plant cover because of insufficient rainfall, i.e., areas where the potential rate of evaporation exceeds the rate of precipitation, and where wind action is an important geological agent. Several factors may lead to such conditions, like position of the area within wind systems of natural low humidity, the presence of a mountain chain in the path of rain-bringing winds, the absence of sufficient relief to induce rainfall, etc.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 1973 Springer-Verlag Berlin · Heidelberg
About this chapter
Cite this chapter
Reineck, HE., Singh, I.B. (1973). Desert Environment. In: Depositional Sedimentary Environments. Springer Study Edition. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-96291-2_17
Download citation
DOI: https://doi.org/10.1007/978-3-642-96291-2_17
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-07377-2
Online ISBN: 978-3-642-96291-2
eBook Packages: Springer Book Archive