Oceans part 2 Flashcards
Wave motion is caused by
the effects of wind acting on the surface of the ocean (friction).
The motion of water follows _____
looping orbitals
Wave orbitals begin to ____ in shallow water due to ____
flatten, drag forces at the base of the seafloor
Zone of strong erosion
Region where wave crests overtake deeper water causing waves to break in the surf zone
Longshore drift
When waves approach the shore and undergo refraction, the oscillating motions are converted to longshore current which carries sediments
Sediments are carried in the direction of ___
longshore current
Tides originate from
gravitational interactions with the sun and moon
Locations of high/low tide
High tides are both nearest and furthest from the center of mass, and low tides at 90 degrees
Most areas experience high tide during:
lunar days (every 24 hours and 50 minutes)
In the open ocean, the tide typically rises and falls by ___
1 m
The tidal range is amplified by _____
shallow water
Bay of fundy tide
16 m
Spring tides
When the sun and moon are in line with the earth, the highest seasonal tides are created
Neap tides
The sun and moon are at 90 degrees to each other with respect to the earth. The resulting tides are the mildest tidal ranges of the year and generate the lowest high tides.
Submergence
result of changes in sea levels where land submerges under the sea
Emergence
result of changes in sea levels where new land emerges
Eustatic changes
changes that result from a combination of worldwide sea-level change
How ice affects eustatic change in sea levels
Glaciers, ice sheets, and ice caps change volume over geologic time due to changes in climate. In cool periods, they sequester significant water from oceans, causing lower global sea levels.
Causes of local changes to sea level
tectonic movements, isostatic responses to ice caps and ice sheets, and the compaction of sediments.
Where ocean sediments can be deposited
oceans near the coast, on the continental shelf, or the deep ocean
Examples of ocean deposits on the coast
deltas, estuaries, and beaches
Pelagic sediments
deep ocean sediment deposited
Benthic zone versus pelagic zone
benthic zone refers to the bottom of the ocean where organisms live and pelagic refers to the water column
Pelagic sections
photic zone and aphotic zone
Photic zone
zone of the pelagic zone where sunlight reaches (200 meters)
Aphotic zone
zone of the pelagic zone where sunlight does not reach
Littoral zone
When dividing the ocean as a function of distance from the shore, the littoral zone is the thin region near the shore that experiences tides.
Neritic zone
When dividing the ocean as a function of distance from the shore, the neritic zone goes from the position of the low tide to the continental shelf slope.
Oceanic zone
When dividing the ocean as a function of distance from the shore, it is the zone beyond the shelf.
Deltas
forms in areas where a river enters the sea, and the erosional action of waves and currents are not great enough to remove all sediment being transported into the river causing a sediment pile to build out into the sea.
Estuaries
Semi-encolsed embayments that are fed by freshwater from one or more rivers and are areas of rapid changing salinity and an environment where significant sediment may occur.
Salinity of freshwater
<500 ppm
Open ocean salinity
35000 ppm (35%)
Beaches
accumulations of well-sorted sediment that lie at the edge of the water
Areas of a beach shoreline that experience weaker wave action accumulate ___ sediment and ___ beaches.
more, wider
Carbonate Shorelines
In clear tropic areas, organisms build reefs (structures of calcium carbonate built from the seafloor)
Atolls
When reefs are built on areas with tectonic rings around volcanic islands.
Continental shelves
large areas that are part of the continent where the depth below sea level is greater than 200 m.
Continental shelves are covered by
clastic sediment (sand and mud) or carbonate sediment in tropical areas of high productivity
Pelagic sediments
cover the deep ocean and are comprised of pelagic clay particles that settle through the water column and ultimately deposit
Pelagic clay
clay from pelagic ooze (shells of microscopic organisms) and continents/islands.
Turbidite
A geologic deposit that may reach the deep seafloor is caused by gravity-driven avalanches of sediment at the connection of the continental shelf to the deep seafloor connection.
Carbonate oozes are more common than carbonate shells because:
carbonate shells are more susceptible to dissolution before deposition
Pelagic ooze
comprised of micron-scale carbonate and silica shells of planktonic organisms