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The classification and description of the various chemically formed sedimentary rock types appears in the bottom section of the chart below Includes photos, examples, and detailed geological insights. Photos of each rock type appear beneath the chart.

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Sedimentary rocks are one of the three main types of rocks found on earth, along with igneous and metamorphic rocks How they form, main types, and why they matter They are formed through the accumulation, compaction, and cementation of various sediments over time.

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Sedimentary rocks are formed by the accumulation of sediments

There are three basic types of sedimentary rocks Clastic sedimentary rocks form from the accumulation and lithification of mechanical weathering debris Breccia, conglomerate, sandstone, siltstone, and shale. Gravel (>2 mm diameter), sand (0.06 to 2 mm diameter), and mud (60 μm diameter)

Mud is further divided into silt (60 to 4 μm diameter) and clay (4 μm diameter). For the purposes of the present discussion, three major categories of sedimentary rocks are recognized (1) terrigenous clastic sedimentary rocks, (2) carbonates (limestone and dolomite), and (3) noncarbonate chemical sedimentary rocks. Sedimentary rocks can be classified into three main types based on their origin

The three types of sedimentary rocks, based on their formation process, are clastic, chemical, and organic

Sedimentary rocks are one of the three major types of rocks found on earth, alongside igneous and metamorphic rocks. Sedimentary rocks are generally divided into three great categories, siliciclastic (or simply, clastic) rocks, chemical rocks and biochemical rocks Their relationships to the three divisions from the simple ideal model are shown in the figure below. Sedimentary rock classification is a complex system used to categorize rocks formed through various processes, including precipitation, crystallization, and compaction.