Cavediggers.com Magazine Issue #9(PDF format)
Cavediggers.com Magazine Issue #9(PDF format)
Cavediggers.com Magazine Issue #9(PDF format)
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Fig. 2. Different types of blockages responsible for plugging open-mouth shafts in the high-mountain<br />
karst.<br />
Fig. 3. A sketch illustrating the development of a pitch-ramp morphology. Vertical pits can readily<br />
enlarge in diameter even by small water flows, while flow concentration within the upper part of<br />
vadose zone is not sufficient to develop wide meanders when flow migrates laterally along bedding<br />
planes. In result of rapid uplift of the Aladaglar massif during Pleistocene-Holocene, cave streams<br />
downcut quickly forming high but narrow meanders between vertical pits.