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19 Cards in this Set

  • Front
  • Back
origination of ocean crust
1. rock sweats, 2. channels form 3/ melt oozes slowly, 4. barriers block flow, 5. cracks open 6.melt flows quickly
descriptive classification of coastal classification
army corps of engineers 1977
looks like: mangrove coast, coral coast, rocky coast with limited beach, short barrier island shoreline, straight barrier island shoreline
genetic classification
geologic history, sea level changes, tectonic environments, glaciation, sediment supply, wave and tidal regime
degree of modification
modification by coastal process and geologic history
primary- form of coast is from land process (non marine)
secondary- form of coast is from marine processes
land erosion coasts
shaped by subaerial erosion and partly drowned by postglacial rise of sea level
emergent coast
flat sea floor, straight coastlines with barrier beaches, erosive features
submergent coast
ria coast- strike controlled river valleys
fjord-long- glacially eroded arm of sea
mainland beach
attached to the upland and is forming as the upland erodes
mid atlantic ridge
the rift boundary between two great crustal slabs and comprises a chain of volcanic mountains on the seafloor that continue to evolve wherever lava upwells and pushes the two plates away from each other
trailing edge
the eastern side of north american continent because it is tucked behind a continental mass that is drifting away from a rift zone
till
a complex mixture of unsorted mud, sand, and gravel that was deposited directly by a glacier
moraine
a glacial deposit composed of till that occasionally has layered sands and gravels
drumlin
an elongate hill, usually hundreds of yards in length and teardrop shaped in map view, that was deposited by a glacier and then overridden by it to produce a streamlined outline
outwash
sediment deposited by glacial meltwater and rivers draining melting ice- most common type are outwash plains
glacial marine sediment
a general term for glacially derived sediment that was deposited below sea level, including muds that were deposited by meltwater that issued from tunnels in glaciers that were below sea level
overwash fans
the bodies of storm sand deposited across an island
ebb tidal deltas
deltas built into the open ocean
flood tidal deltas
those built on the back side of a barrier island
transgression
the landward movement of coastal enviornments in response to sea level rise