Ocean Environments Test Flashcards
Coast
the zone where the land meets the sea
Drowned coast
“Submergent coast”
2 types: ria, fjords
Ria coast
sea-level rise has drowned a region of coastal river valleys forming a series of wide estuaries often separated by a long peninsula
*Prevalent in Northwestern Europe, eastern US, and Australia
Fjord coast
sea-level rise has drowned one or more deep glacier-carved valleys
*Prevalent in coastal Norway, Chile, Canada, and New Zealand
Estuary
salt water meets fresh water
Emergent coast
occur where land has uplifted faster than the sea has risen since the last ice age.
Areas that were formerly sea floor may become exposed above the shoreline while former beaches often end up well behind the shoreline or even on clifftops.
Staircase structures called marine terraces are created by a combination of uplift and waves gradually cutting flat platforms at the base of cliffs.
Global sea-level change
Most important cause: the increase or decrease in the extent of the world’s ice sheets and glaciers
Related to Earth’s climate
If it cools, more water is frozen into glaciers=less oceans
If it warms up, more water melts from glaciers=more ocean volume
Affects ocean water temperature
Local sea-level change
Occurs when a particular area of land rises or falls relative to the general sea level
One cause occurs in regions where oceanic crust is being forced beneath continental crust.
Another cause is the glacial rebound-gradual rise of a specific area of land after an ice sheet that once weighed it down rises.
Coastal landscapes
can be classified into primary or secondary.
Primary coasts
have formed as a result of land-based processes like land erosion and volcanic activity.
Secondary coasts
have been shaped by marine erosional processes or by activities of organisms like corals and mangroves and people.
Wave-erosion coasts
secondary coast
waves hurl beach material against the cliffs which abrade the rock
each wave compresses air within cracks in the rock and on reexpansion, the air shatters the rock.
Marine-deposition coasts
Formed by sediment brought to the coast by rivers, eroded from headlands, or moved from offshore by waves.
Spit formation
sand and water are carried past the headland by longshore drift but the sand settles at the mouth of an estuary where the waves are opposed by the sluggish outflow from a river.
Beaches
deposits of sedimentary material
Commonly occur on coasts above the low-tide line
Sources of beach material-sediment brought to the coast by rivers or eroded from cliffs or the sea floor or the biological material such as shells.
Wind can also influence beach development and is instrumental in forming coastal dunes