Detrital sedimentary rocks have clastic textures.

Name: Detrital sedimentary rocks have clastic textures.
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Detrital sedimentary rocks are formed from the accumulation of rock fragments, mineral grains, and other debris that have been transported and deposited by wind, water, or ice. These materials have a clastic texture because they are made up of discrete particles that are cemented together. Examples of detrital sedimentary rocks include sandstone, shale, and conglomerate.

Detrital Sedimentary Rocks Have Clastic Textures