Sedimentary rocks of weathered rock fragments are called clastic rocks.
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Sedimentary rocks made of weathered rock fragments are called clastic sedimentary rocks. These rocks are formed from the accumulation and cementation of fragments that have been weathered, eroded, and transported from their original source. Examples include sandstone, shale, and conglomerate.
Weathered rocks that are composed of smaller fragments and grains are referred to as sedimentary rocks. These rocks are formed through the process of erosion, transportation, deposition, and lithification of the weathered materials.
They are called clastic sedimentary rocks.
Sedimentary rocks made from fragments of rocks, minerals, and shells are known as clastic sedimentary rocks. Examples include sandstone, shale, and conglomerate. These rocks form when pre-existing rocks are weathered, eroded, transported, and deposited in layers.
Sedimentary rocks typically begin as weathered fragments of pre-existing rocks or as organic material that accumulate and undergo compaction and cementation to form solid rock.
No, sedimentary rocks formed from fragments of other rocks are called clastic sedimentary rocks. Chemical sedimentary rocks form from minerals that are dissolved in water and precipitate out to form rocks like limestone or halite.