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Classic rocks, also known as clastic rocks, are formed from the accumulation and lithification of fragments of pre-existing rocks or minerals. These fragments, or clasts, are transported by wind, water, or ice and deposited in various environments, such as riverbeds, lakes, or oceans. Over time, the sediments become compacted and cemented together, solidifying into rock. Common examples of clastic rocks include sandstone, shale, and conglomerate.

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