Wed. Jun 19th, 2024

Karst Geomorphology

  1. Who introduced the concept of cycle of erosion in karst?

    Options:
    1. H. Roques
    2. Jovan Cvijic
    3. W.M. Davis
    4. W.F. Beede

    Option: D

  2. According to W.M. Davis, what is the karst cycle of erosion characterized by?

    Options:
    1. Development of surface drainage
    2. Disappearance of surface drainage underground
    3. Reappearance of subterranean drainage as surface drainage
    4. All of the above

    Option: D

  3. What is karst cycle of erosion?

    Options:
    1. A cycle of erosion caused by water table of groundwater
    2. A cycle of erosion caused by sink holes and swallow holes
    3. A cycle of erosion caused by rainwater mixed with atmospheric carbon dioxide reacting with limestone
    4. A cycle of erosion caused by faulted beds of limestone

    Option: C

  4. What are the two types of conditions recommended for the initiation of karst cycle of erosion?

    Options:
    1. Exposure of thick limestone cover at the ground surface and shale cover overlain by non-soluble rocks
    2. Exposure of thin limestone cover at the ground surface and sandstone cover overlain by non-soluble rocks
    3. Exposure of thick limestone cover at the ground surface and limestone cover overlain by non-soluble rocks
    4. Exposure of thin limestone cover at the ground surface and shale cover overlain by non-soluble rocks

    Option: C

  5. What are the two types of structures where karst cycle of erosion becomes more operative?

    Options:
    1. Folded sandstones and non-soluble rocks
    2. Folded shales and non-soluble rocks
    3. Folded limestones and non-soluble rocks
    4. Faulted limestones and soluble rocks

    Option: C

  6. Who postulated the 3-stage karst cycle and what are the stages?

    Options:
    1. Beede – youth, maturity, old stage
    2. Cvijic – youth, mature, late maturity, old stage
    3. Beede – youth, mature, late maturity
    4. Cvijic – youth, maturity, old stage

    Option: A

  7. What is the characteristic feature of the youth stage of karst cycle of erosion?

    Options:
    1. Surface drainage disappears underground through sink holes and swallow holes
    2. Ground surface is characterized by rough terrain due to development of ‘lapies’
    3. Surface runoff first removes thin deposits of insoluble or non-calcareous formations
    4. Rainwater immediately comes in contact with the rocks and starts dissociating them

    Option: D

  8. What are the characteristic geomorphic features of the youth stage of karst topography?

    Options:
    1. Caves, sinkholes, lapies, blind valleys
    2. Uvalas, poljes, karst windows
    3. Dry, waterless conditions
    4. Thin cave roofs causing their collapse

    Option: A

  9. How is the initiation of early maturity in karst topography characterized?

    Options:
    1. By the destruction of most solutional landforms
    2. By the appearance of surface drainage
    3. By the disappearance of surface drainage underground
    4. By the formation of uvalas, poljes, and karst windows

    Option: C

  10. What happens to cave roofs during the early maturity stage of karst topography?

    Options:
    1. They become thicker
    2. They undergo thinning
    3. They collapse
    4. They become narrower

    Option: B

  11. What is the late maturity stage of karst topography characterized by?

    Options:
    1. Increased volume of water due to maximum development of subterranean drainage
    2. Destruction of most solutional landforms
    3. Total collapse of cave roofs
    4. Ridging between uvalas becoming reduced in height

    Option: B

  12. What are ‘hums’ in the old stage of karst topography?

    Options:
    1. The residuals of carbonate rocks that project slightly above the ground
    2. The subterranean drainage that appears on the ground surface
    3. The ridges between uvalas that become reduced in height
    4. The pitted surface that resembles the peneplain of normal fluvial cycle of erosion

    Option: A