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Geosciences LibreTexts

7: Sedimentary Minerals and Sedimentary Rocks

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Key Concepts
  • Weathering involves the decomposition and breaking apart of rocks at Earth’s surface.
  • Weathering produces solid clastic material and dissolved chemical material.
  • Products of weathering may be transported and deposited to produce clastic or chemical sediments.
  • Sediments of all sorts may be lithified to become rocks.
  • Clastic material typically comprises quartz and clays; less commonly other minerals.
  • Minerals produced by chemical precipitation include clays, carbonates, sulfates, halides, zeolites, and chert.
  • We name clastic sedimentary rocks based primarily on clast size.
  • We name chemical sedimentary rocks based primarily on composition.
7.1.png
Figure 7.1: Salt deposits on the shore of the Dead Sea, Jordan


This page titled 7: Sedimentary Minerals and Sedimentary Rocks is shared under a CC BY-NC-SA 4.0 license and was authored, remixed, and/or curated by Dexter Perkins via source content that was edited to the style and standards of the LibreTexts platform.

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