Or some mixture of these trace amounts of meteoric dust and variable.
Thickness ocean floor is vs terrestrial.
Therefore the rate of sedimentation the thickness of accumulated deposits and their quantity if analyzed scientifically help in the reconstruction of the geological history of the world.
The rock cycle is the transition of rocks among three different rock types over millions of years of geologic time fig.
The deposition of sediments on the ocean floor however is a very slow process.
Are the most abundant of all biogenous sediments on the ocean floor b.
Joists in home construction are usually made with 2 by 10 or 2 by 12 lumber.
Accumulate at the rate of 1 4 cm per 1000 yrs d.
Include the tests of foraminifera shells of pteropods and coccoliths c.
These particles consist primarily of either the microscopic calcareous or siliceous shells of phytoplankton or zooplankton.
Clay less than or equal to 4 micrometer silt 4 to 62 micrometer sand 62 micrometer to 2 millimeter and more than 2 millimeter such.
This map shows the locations of these deep sea trenches.
However unlike terrestrial plant roots the anchors that some aquatic plants like kelp and sea grass use to secure themselves to the sea floor don t provide nutrients.
Instead these aquatic plants absorb nutrients directly from the water around them.
2 1 deposition of pelagic sediments.
The size is from the smallest to largest these are.
All rocks in earth s crust are constantly being recycled through the rock cycle.
Pelagic sediments are the deposits of the open ocean that accumulate on the ocean floor protected from terrestrial influence see hüneke and henrich 2011 this volume they are not necessarily deep but are usually located at great distance from the continents.
The various sources of sea floor sediment can be summarized as follows.
Another classification of ocean floor sediments is by the size of the individual grain.
These relatively narrow down folds in earth s crust may be twice as deep almost 12 000 meters as the regular deep sea floor up to 6 000 meters.
Reinhard hesse ulrike schacht in developments in sedimentology 2011.
Some also have air bladders that help them to stay afloat.
Life cycle of the oceanic crust.
Are found primarily above a depth of 4500 m in the ocean e.
This is a more unusual way to categorize ocean floor sediments.
7 56 igneous rock is formed by the cooling and crystallization of molten magma at volcanoes and mid ocean ridges where new crust is generated.
Terrigenous sediment is derived from continental sources transported by rivers wind ocean currents and glaciers.
It is dominated by quartz feldspar clay minerals iron oxides and terrestrial organic matter.
All of the above are correct.
