Skip to main content

Part of the book series: Springer Study Edition ((SSE))

  • 724 Accesses

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.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 74.99
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints 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

Publish with us

Policies and ethics