Chapter 9 and 10 Flashcards
Drainage Basin
Area of land where all surface water converges to a single point or flows into another body of water.
Drainage Density
Channel length per unit watershed area.
Terrace
Flat or gently sloping geomorphic surface that is typically bounded on one side by a scarp.
Gorge
“Small canyon” formed by geological uplift, eroison, and glaciers melting.
Tarn
Lakes formed in glacially carved cirques.
Legacy Sediment
Depositional bodies of sediment inherited from the increase of human activities since the early settlers.
Sediment Rating Curve
Average relation between discharge and suspended sediment concentrations for a certain location.
River/Stream Capture
Stream is diverted from its own bed and flows into the bed of neighboring stream.
Emergent/submergent coastlines
Land along the coast that has been exposed by the sea fall. Submergent has been covered by sea rise.
Plunging Breaker
Breaking wave whose crest curls over and collapses suddenly
Swash/Backwash
Turbulent layer of water that washes up on the beach after and incoming wave breaks.
Longshore Drift
The transportation of sediment dependent on the angles of the waves coming in. The movement of sediment down the beach in a zigzag pattern.
Lagoon
Shallow body of water that is seperated from a larger body of water by a narrow landform like a barrier island.
Submarine Canyon
Formed by erosion and mass wasting event. Narrow, steep-sided valley that cuts into a continential slope.
Beach nourishment
The replacement of sediments on a beach.
Dendritic Drainage Basin
TREE (homogenous and flat-lying)
Trellis
Bunch of little coming out of big (long linear valleys where drainage flows from eroded shales or limestones)
Rectangular
Enhanced groundwater etches from chemical weathering
Radial
Volcanoes (strato)
Shreve
Additive
Strahler
Game level
Fill terrace
stream incises into the material that is deposited into a valley
Strath terrace
Stream downcuts into bedrock.
Discharge Changes downstream
Decrease in arid/increase in temperate
3 Base leves/ Processes that lead them to change
Natural lake, dam, and ocean. Climate, tectonics, and isostacy.
Sediment Grain Size changes downstream
Sediment grain size decreases downstream where there is larger volume of water and higher energy which causes more erosion because the sediments are rubbing together.
History of sea level past 21000 years
Earth warmed 4 degrees, sea level rise by about 280 feet
Mechanisms that supply sediment to coastal zone
Longshore drive, constructive waves, and current.
Why are tides geomorphically important?
Groundwater fluctuations by the periodic saturated and unsaturated condition on the intertidal zone.
Four types of estuaries
Coastal plain: drowned river valley, when a risen sea fills an existing river valley
Fjord: formed by glacier retreat
Tectonic: formed by tectonic shift
Bar-built: formed from a lagoon or bay that is protected by a barrier island, like a sandbar
Geomorphic effects of jetty
Prevents erosion and traps sand from drifting along the beach