Weathering in the Tropics, and Related Extratropical Processes

Research output: Chapter in Book/Report/Conference proceedingChapter

6 Scopus citations

Abstract

Weathering processes are partially responsible for a characteristic geomorphology that occurs in the tropics and subtropics. Resistant landforms such as inselbergs, extreme solution processes such as silica karst, and deep weathering profiles with end stage weathering products such as laterite and kaolin are common features of tropical weathering. Many of these features also occur outside the tropics. In part, climate change and paleotectonics were responsible for tropical conditions in areas not now tropical. But, some processes assumed to require tropic conditions that are not so limited, sufficient moisture, and time sufficing for their development. This chapter reviews the weathering processes and distinctive landforms of the broadly defined tropics, and explores the debates over weathering factors as they pertain to tropic and extratropical environment.

Original languageEnglish
Title of host publicationTreatise on Geomorphology
PublisherElsevier Inc.
Pages179-196
Number of pages18
Volume4
ISBN (Print)9780080885223
DOIs
StatePublished - 1 Mar 2013

Keywords

  • Climate change
  • Climatic geomorphology
  • Geomorphology
  • Karst
  • Subtropics
  • Tropics
  • Weathering
  • Weathering landforms
  • Weathering profiles

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