Soru

Zorluk: ZorLandform Evolution by Running Water and Underground Water

Match each geomorphic landform developed through fluvial or groundwater action with its precise evolutionary process.

  • Blind ValleyTermination of a surface stream channel abruptly at a swallow hole, leaving a dry valley downstream bounded by a wall.
  • PoljeFormation of an expansive, flat-floored depression in limestone through combined tectonic faulting and extensive solution collapse.
  • PotholesCylindrical bed depressions carved in upper river courses by swirling eddy currents executing mechanical abrasion with trapped pebbles.
  • Oxbow LakeSealing of an abandoned meander loop by river silt deposition following high-discharge neck chute cut-offs.

Cevap

Blind Valley matches with abrupt river termination at a swallow hole; Polje matches with expansive solutional-tectonic depression; Potholes match with cylindrical bed grinding by eddy currents; Oxbow Lake matches with meander cut-off and depositional sealing.
Each feature is correctly matched with its specific geomorphic evolution mechanism: Blind Valley with river capture into sinkholes, Polje with large-scale structural limestone dissolution, Potholes with fluvial eddy-current corrasion, and Oxbow Lake with flood stage meander cut-off and deposition.

Adım Adım Çözüm

1
Analyze karst surface drainage features
Identify that a Blind Valley ends abruptly where surface streams plunge underground into sinkholes or ponors.
Karst hydrology frequently redirects surface drainage subterraneanly through swallow holes.
2
Evaluate major subterranean and surface karst depressions
Identify Polje as the expansive, flat-bottomed depression resulting from structural faulting combined with chemical solution.
Poljes are distinctive large-scale karst features requiring long-term tectonic and carbonation processes.
3
Analyze upper course fluvial erosional mechanisms
Connect Potholes with vertical mechanical abrasion (corrasion) by swirling pebbles trapped in channel floor depressions.
Eddy currents spin bedload pebbles to hollow out smooth cylindrical pits.
4
Evaluate lower course depositional and erosional processes
Connect Oxbow Lake with neck chute cut-offs during flood stages followed by silting up of the abandoned meander ends.
Meander necks narrow through lateral erosion until high discharge forces a straight cut-off.

Anahtar Kavram

Classification of Fluvial and Karst Geomorphic Processes and Landforms
Bu soruyu puanla