Geomorphology Flashcards
A wind-eroded depression in the side of a cliff of a homogenous rock type
Alcoves and yardang windows
A low, triangular-shaped deposits built from the accumulation of sediments at thr mouth of a valley
Alluvial fan
The size of an alluvial fan depends on which of the ff: (Area of Drainage Basin, Climate, Lithologies in the Source Area, Tectonic Activity, Space for Fan Growth)
All of the above
Roughly circular or oval in plan an have a surface exposure of over 100 km2; deep-seated and are usually composed of coarse-grained plutonic rocks
Batholiths, lopoliths, and stocks
Submarine, circular, steep-sided holes which occur in coral reefs
Blue hole
Shake hole, swallow hole, swallet, doline, or cenote
Sinkhole
A compound alluvial fan where neighboring alluvial fans converge into a single apron of deposits against a slope; may hole very shallow lakes called playa
Bajada
A small, steep-sided and flat-topped hill, built of flat lying soft rocks capped by a more resistant layer of sedimentary rock, lava flow, or duricrust, surrounded by a plain
Butte
A deeply-incised, steep-sided river valley
Canyon
An assymetrical upland feature usually associated with gently dipping rocks and comprisig a steep scarp slope (or escarpment) and a longer, gentler dip slope
Cuesta
Which of the following landforms are not associated with dipping and horizontal strata? (Cuesta, Homoclinal/Strike Ridge, Hogback, Butte, Mesa, Plateau, Canyon)
Canyon
Also pericline; formed by tectonic warping, igneous intrusion, or diapir
Dome
A depositional landform produced by sedimentation at and around the mouth of a river; river-, tide-, wave-dominated
Delta
A large area of sand dunes
Erg
A long winding ridge of stratified sand and gravel that are frequently several km long and are somewhat like railroad embankments; probably former sites of sub-glacial streams and rivers
Esker
A steep slope coinciding with the line of a fault
Fault scarp
Associated with hogback ridges; triangular-shaped remnants of the bed between v-shaped notches; steeply stoping wedge-shaped landscape features created by differential erosion
Flatirons
German “sea of rock”; areas covered by large angular blocks (formed in situ), traditionally believed to have been created by freeze-thaw action
Felsenmeer or blockfield
Major splits into limestone pavement, formed by widening, deepening, and eventual merging of solution features that develop along linear weakness in the rock
Grike (Bogaz)
Small closed depressions on horizontal and gently inclined rock surfaces; similar to solution pits in carbonate rocks;
Gnamma (weathering pit or panhole)