Skip to content
Karst Geomorphology
-
Who introduced the concept of cycle of erosion in karst?
Options:
- H. Roques
- Jovan Cvijic
- W.M. Davis
- W.F. Beede
-
According to W.M. Davis, what is the karst cycle of erosion characterized by?
Options:
- Development of surface drainage
- Disappearance of surface drainage underground
- Reappearance of subterranean drainage as surface drainage
- All of the above
-
What is karst cycle of erosion?
Options:
- A cycle of erosion caused by water table of groundwater
- A cycle of erosion caused by sink holes and swallow holes
- A cycle of erosion caused by rainwater mixed with atmospheric carbon dioxide reacting with limestone
- A cycle of erosion caused by faulted beds of limestone
-
What are the two types of conditions recommended for the initiation of karst cycle of erosion?
Options:
- Exposure of thick limestone cover at the ground surface and shale cover overlain by non-soluble rocks
- Exposure of thin limestone cover at the ground surface and sandstone cover overlain by non-soluble rocks
- Exposure of thick limestone cover at the ground surface and limestone cover overlain by non-soluble rocks
- Exposure of thin limestone cover at the ground surface and shale cover overlain by non-soluble rocks
-
What are the two types of structures where karst cycle of erosion becomes more operative?
Options:
- Folded sandstones and non-soluble rocks
- Folded shales and non-soluble rocks
- Folded limestones and non-soluble rocks
- Faulted limestones and soluble rocks
-
Who postulated the 3-stage karst cycle and what are the stages?
Options:
- Beede – youth, maturity, old stage
- Cvijic – youth, mature, late maturity, old stage
- Beede – youth, mature, late maturity
- Cvijic – youth, maturity, old stage
-
What is the characteristic feature of the youth stage of karst cycle of erosion?
Options:
- Surface drainage disappears underground through sink holes and swallow holes
- Ground surface is characterized by rough terrain due to development of ‘lapies’
- Surface runoff first removes thin deposits of insoluble or non-calcareous formations
- Rainwater immediately comes in contact with the rocks and starts dissociating them
-
What are the characteristic geomorphic features of the youth stage of karst topography?
Options:
- Caves, sinkholes, lapies, blind valleys
- Uvalas, poljes, karst windows
- Dry, waterless conditions
- Thin cave roofs causing their collapse
-
How is the initiation of early maturity in karst topography characterized?
Options:
- By the destruction of most solutional landforms
- By the appearance of surface drainage
- By the disappearance of surface drainage underground
- By the formation of uvalas, poljes, and karst windows
-
What happens to cave roofs during the early maturity stage of karst topography?
Options:
- They become thicker
- They undergo thinning
- They collapse
- They become narrower
-
What is the late maturity stage of karst topography characterized by?
Options:
- Increased volume of water due to maximum development of subterranean drainage
- Destruction of most solutional landforms
- Total collapse of cave roofs
- Ridging between uvalas becoming reduced in height
-
What are ‘hums’ in the old stage of karst topography?
Options:
- The residuals of carbonate rocks that project slightly above the ground
- The subterranean drainage that appears on the ground surface
- The ridges between uvalas that become reduced in height
- The pitted surface that resembles the peneplain of normal fluvial cycle of erosion