Detrital sediment is rock in small particles or other material worn or broken away from a mass, as by the action of water or glacial ice. They include (in decreasing size) boulders, cobbles, pebbles, sand, silt, and clay.
In ascending order of grain size one can find
mudstones (dominantly clay)
siltstones (dominantly silt)
sandstones (dominantly sand)
conglomerates / breccias (dominantly gravel)
Each of these rock types can be further specified as they are only endmembers and a virtually infinite number of possible varities of sedimentary rocks results from their grain size distribution.
For example a silty fine sandstone would be a sandstone made up mostly by fine sand containing some silt as well.
Rough sediment grading from largest to smallest in diameter would include the following:
Boulder--larger than 256 mm
Cobble--256 to 64mm
Pebble--64 to 2 mm
Sand--2 to 1/16 mm
Silt--1/16 to 1/256 mm
Clay--less than 1/256 mm
clay-sized grains, silt-sized grains, sandstone and pebbles
because some are big and small like a grain
Clay-sized, silt-sized, sand-sized, pebbles in my science textbook New York science pg.76
Shale, Sandstone, Conglomerate
Clay particles. Less than 2 micrometres in diameter.
Grain size
1)Clay-sized 2)Silt-sized 3)Sand-sized 4)Pebbles
That is correct. A detrital (or "clastic") sedimentary rock is formed by sediment grains that have been weathered and eroded by existing rocks and then deposited as layers.
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Clay particles. Less than 2 micrometres in diameter.
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Grain size
Asteroids can be as small as a grain of sand as big as 600 miles! Olivia
1)Clay-sized 2)Silt-sized 3)Sand-sized 4)Pebbles
its largest grain crop is milling wheat
Rock.
no
That is correct. A detrital (or "clastic") sedimentary rock is formed by sediment grains that have been weathered and eroded by existing rocks and then deposited as layers.
Sandstone is the classification of rock composed of small rounded rock particles, usually quartz in nature.
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The smallest thing you could imagine - a dust grain, a molecule, an atom, a quark.