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bn:27870710n
Noun Concept
Categories: Geomorphology, Geological hazards
EN
cambering  Gull  valley bulging
EN
Cambering is a phenomenon typically seen at a valley crest or plateau margin whereby blocks of competent strata such as sandstone stretch, tilt or rotate with respect to underlying incompetent rock layers such as clay or mudstone. Wikipedia
English:
geology
Definitions
Sources
EN
Cambering is a phenomenon typically seen at a valley crest or plateau margin whereby blocks of competent strata such as sandstone stretch, tilt or rotate with respect to underlying incompetent rock layers such as clay or mudstone. Wikipedia
The downslope movement of competent strata into a valley Wikipedia Disambiguation
Wikipedia
EN
cambering
Wikipedia Redirections
EN
Cambering (geology), Gull (geology), valley bulging

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