Geomorphology and Quaternary Geology Flashcards
7 cards from real ASBOG practice questions. Tap to flip, then mark Knew It or Still Learning โ missed cards come back until you master them.
Read the first 7 Geomorphology and Quaternary Geology flashcards as text
Stream terraces form primarily as a result of:
Answer: Stream incision following a change in base level or sediment supply
Stream terraces are abandoned floodplains left elevated when a river incises downward due to falling base level or decreased sediment supply.
Which process describes the downslope movement of water-saturated soil and debris as a coherent mass over a curved failure surface?
Answer: Rotational slump
A rotational slump involves movement along a concave-upward failure surface, with the mass rotating backward as it slides.
Pleistocene pluvial lakes, such as Lake Bonneville, formed primarily because of:
Answer: Increased precipitation and reduced evaporation under cooler climates
Pluvial lakes expanded during glacial intervals due to cooler, wetter conditions that reduced evaporation and increased precipitation.
What is the term for a crescent-shaped sand dune with horns pointing downwind?
Answer: Barchan
Barchan dunes are crescent-shaped with the concave side downwind, forming where sand supply is limited and wind direction is consistent.
Drumlins are elongated glacial landforms that indicate:
Answer: The direction of former glacial flow
Drumlins are streamlined subglacial landforms whose long axes parallel the direction of ice flow, with the blunt end facing up-ice.
Which luminescence dating technique uses heat to release trapped electrons from mineral grains to determine burial age?
Answer: Thermoluminescence (TL)
Thermoluminescence (TL) dating releases trapped electrons by heating mineral grains, measuring light emitted to calculate the time since last exposure to heat or light.
A wave-cut platform is best described as:
Answer: A subhorizontal bedrock surface eroded by wave action at the base of a sea cliff
Wave-cut platforms are flat or gently sloping bedrock surfaces formed by wave erosion at the base of retreating sea cliffs.