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Intrabasinal rocks are deposited in the same basin as the source rock they are weathered from. Extrabasinal rocks are deposited outside the basin of their original source rock. Both are sedimentary rocks.
renal pelvis
When the ground subsides it can become lower than the surrounding terrain, forming a basin. Since water, which carries sediment, flows downhill, sediment will collects in these basins. If enough sediment collects, compaction and cementation will turn it into sedimentary rock.
It is where elevated material is transported to lower areas by wind, ice, water, and gravity, and deposited in a still environment, like a basin, lake, or ocean.
The transport of sediment depends on its grain size and the original location where it was produced. Terrigenous sediment can be transported to the deep sea via rivers or by wind. Material transported by rivers most commonly ends up deposited on thecontinental margin, the shallow portions of the ocean that are within several hundred kilometers of land. When continental margin deposits accumulate fast and get overly steep, or when an earthquake or storm causes the sediment to be resuspended, turbidity currents provide additional transport out to the deep sea. The resuspension of the sediment into the bottom water causes it to be more dense than the overlying water, and thus these turbidity currents flow downslope to the more distant ocean basin -humberto <3
The igneous rock gets weathered into sediment by wind, water, and ices. The sediment is deposited in a basin and buried. The pressure of burial and the heat inside Earth turns that sediment into stone.
Intrabasinal rocks are deposited in the same basin as the source rock they are weathered from. Extrabasinal rocks are deposited outside the basin of their original source rock. Both are sedimentary rocks.
William M. Brown has written: 'Sediment transport and turbidity in the Eel River basin, California' -- subject(s): Sediment transport 'Streamflow, sediment, and turbidity in the Mad River basin, Humboldt and Trinity Counties, California' -- subject(s): Stream measurements
J. M Knott has written: 'Sediment discharge data for selected sites in the Susitna River Basin, Alaska, 1981-82' -- subject(s): Sedimentation and deposition 'Sediment transport characteristics of selected streams in the Susitna River Basin, Alaska' -- subject(s): Stream measurements, Sedimentation and deposition, Bed load, Sediment transport, Measurement 'Sediment transport characteristics of selected streams in the Susitna River Basin, Alaska, October 1983 to September 1984' -- subject(s): Stream measurements, Sediment transport, Sedimentation and deposition
Basin
marine basin between India and Eurasia
it was formed when the earth's crust expanded subsided and filled with sediment between the carboniferous and triassic
the Pacific Ocean with a few in the Indian Ocean.
renal pelvis
When the ground subsides it can become lower than the surrounding terrain, forming a basin. Since water, which carries sediment, flows downhill, sediment will collects in these basins. If enough sediment collects, compaction and cementation will turn it into sedimentary rock.
Mississippian
abyssal plain