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interlocking spur
An interlocking spur, also known as an overlapping spur, is one of any of a number of projecting ridges that extend alternately from the opposite sides of the wall of a young, V-shaped valley down which a river with a winding course flows. Each of these spurs extends laterally into a concave bend of the river such that when viewed either upstream or from overhead, the projecting ridges, which are called ''spurs'', appear to "interlock" or "overlap" in a staggered formation like the teeth of a zipper.〔Jackson, JA, J Mehl and K Neuendorf (2005) ''Glossary of Geology.'' American Geological Institute, Alexandria, Virginia. 800 pp. ISBN 0-922152-76-4〕
While similar in general appearance, the mechanism behind the formation of interlocking spurs is different from that behind meanders, which arise out of a combination of horizontal erosion and deposition. Interlocking spurs are formed as either a river or stream cuts its valley into local bedrock. As it entrenches its valley, it preferentially follows and erodes zones of weaknesses within the bedrock that typically consist of intersecting sets of joints. This process creates a zig-zagging fluvial valley that "interlock" or "overlap" in a staggered manner.
If the river valley is subsequently subject to glaciation, glacial erosion widens the V-shaped valley and removes the ends of the interlock spurs projecting into the valley. As a result, the ridges are truncated to form ''truncated spurs''. 〔〔Thornbury, W. D. (1954) ''Principles of Geomorphology.'' John Wiley and Sons, Inc. New York. 618 pp. ISBN 978-8123908113〕
==References==
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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