Thickness Ocean Floor Is Vs Terrestrial

Joists in home construction are usually made with 2 by 10 or 2 by 12 lumber.

Thickness ocean floor is vs terrestrial.

It is dominated by quartz feldspar clay minerals iron oxides and terrestrial organic matter. The deposition of sediments on the ocean floor however is a very slow process. When two plates come together under the ocean a deep sea trench is formed. 2 1 deposition of pelagic sediments.

Some also have air bladders that help them to stay afloat. 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. Are the most abundant of all biogenous sediments on the ocean floor b. Another classification of ocean floor sediments is by the size of the individual grain.

This map shows the locations of these deep sea trenches. 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. 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. Reinhard hesse ulrike schacht in developments in sedimentology 2011.

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. 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. The rock cycle is the transition of rocks among three different rock types over millions of years of geologic time fig. Or some mixture of these trace amounts of meteoric dust and variable.

Terrigenous sediment is derived from continental sources transported by rivers wind ocean currents and glaciers. The bulk of the floor s thickness comes from the joists which are the horizontal beams that carry the floor s weight. The various sources of sea floor sediment can be summarized as follows. 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.

All of the above are correct. The size is from the smallest to largest these are. Include the tests of foraminifera shells of pteropods and coccoliths c. Accumulate at the rate of 1 4 cm per 1000 yrs d.

Life cycle of the oceanic crust. Pelagic sediment or pelagite is a fine grained sediment that accumulates as the result of the settling of particles to the floor of the open ocean far from land. Are found primarily above a depth of 4500 m in the ocean e. This is a more unusual way to categorize ocean floor sediments.