Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/65879
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Type: Journal article
Title: On the origin and significance of basal notches or footcaves in karst terrains
Author: McDonald, R.
Twidale, C.
Citation: Physical Geography, 2011; 32(3):195-216
Publisher: V H Winston & Son Inc
Issue Date: 2011
ISSN: 0272-3646
1930-0557
Statement of
Responsibility: 
Roy Charles McDonald, C. Rowland Twidale
Abstract: Albeit under various names (footcave, slot, cliff-foot cave, shelter, notch) basal indents form in various lithological and climatic environments. But footcaves in crystalline limestone are especially well and widely developed, not only in marine environments, but also inland. In the humid tropics, footcaves and swamp slots are associated with surface and shallow groundwaters charged with chemicals and biota. The indents developed around the bases of widely separated karst towers are responsible for their conversion from cupolas or domical residuals. Even in mature tower karst landscapes, some arcuate footcaves are shaped by laterally corrading streams in flood that have transported and deposited exotic debris. Such corrasion is, however, particularly widespread in youthful karst where valley floors are narrow. Here, footcaves not only may have been initiated, but also occasionally maintained, enhanced, and modified by migrating streams, as well as by scarp-foot weathering and sapping. Microorganisms that colonize moist walls of footcaves may also have contributed.
Keywords: karst tower
footcave
marine notch
swamp slot
subsurface weathering
lateral stream corrasion
DOI: 10.2747/0272-3646.32.3.195
Published version: http://dx.doi.org/10.2747/0272-3646.32.3.195
Appears in Collections:Aurora harvest 5
Earth and Environmental Sciences publications

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