Geomorphology Flashcards
Endogenic Processes
driven by plate tectonics
mountains, volcanoes, faults
create new landmass
Relief
differences in height in a specific location
enodogenic processes increase relief, exogenic processes (weathering) reduce it
exogenic processes
processes driven by energy sources external to the mantle, mainly solar energy
weathering and movement of weathered material
geologic cycle
natural cycle of recycling of Earth’s minerals over time, involves the rock cycle and the endo and exogenic processes
Mass wasting
mass movement of eroded material due to gravity (ex: landslides)
Fluvial transport
sediment transported by water, eroded and deposited
Rain Shadow effect
winds accumulate humidity over ocean, cools as it rise up mountain face, condenses and rains down, wind passes over mountain to other side, no rain
Drainage Basin
topographical region which concentrates water received as precipitation into a series of geographically isolated rivers, eventually lead to one type of water body
Zones in drainage basins
erosion zone - where water collects sediment for transport, forms v-shape valleys
transport zone - some sediment begins to be deposited, meandering river systems are formed
deposition zone - where remainder of the sediment is deposited, forms estuaries and deltas
Meandering river systems formation:
determined by flow rate of water, size of particles being eroded, local geography
faster edge of river erodes existing landmass –> gradual movement of the river over time
Estuaries
river flow not strong enough to hold back the ocean, ocean waters moving inland brings salt and sediment
Deltas
when flow of river is greater than the pressure of the ocean water, freshwater and sediment extends past the coastline
Alluvial Fans
when deposition zones occur inland away from oceans, sediment depostited in a fan shaped landform
as water drains into a groundwater source
V-shaped valleys
have steep slopes but gradually form rounder slopes as erosion removes increasing amounts of rock
formed by rivers
Glacial Movement
glaciers form where air temperature is cold enough for long term snow build-up –> pressure converts snow into ice –> snow at the head of the glacier forces mass down
leaves behind a U-shaped valley and characteristic sediment deposits (glacial till, isolated drop stones)