Clastic sedimentary rocks form by weathering processes which break down rocks into pebble, sand, or clay particles by exposure to wind, ice, and water.
Pieces of rock are loosened by weathering, then transported to some basin or depression where sediment is trapped. Chemical sedimentary rocks, such as rock salt, iron ore, chert, flint, some dolomites, and some limestones, form … Clastic sedimentary rocks such as breccia, conglomerate, sandstone, siltstone, and shale are formed from mechanical weathering debris. Clastic and nonclastic sedimentary rocks are the only members of the rock family that contain fossils as well as indicators of the climate (ripple marks, mudcracks and raindrops) that was present when the rock was formed.
In general, the greater the distance traveled, the smaller and more rounded the … Clastic sedimentary rocks are made up of pieces (clasts) of pre-existing rocks. Clastic sedimentary rocks are classified according to the grain size of the sediment and the kinds of rock fragments that make up the sediment (Table ).Grain size is largely a function of the distance the particle was transported. For example, sand on a beach or in a dune can get buried. Clastic sedimentary rocks are the group of rocks most people think of when they think of sedimentary rocks.
Clastic sedimentary rocks are made up of pieces of other rocks. Under the pressure of burial, the sand is pressed together and compacted.
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