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According to (Week 4 Ch. 8 Reading. (n.d.). Sedimentary rocks originate from
the erosion of pre-existing rocks that have been broken down through weathering. When
the sediment is placed and underground, it lithifies and develops into new rock.
Furthermore, According to (Amethyst Galleries. (1995-2010). Sedimentary Rocks are
shaped through assembly and successive alliances of residue into several kinds of
rock. Its source is the residue. Sediments are unmerged substances that possess
distinct backgrounds. Eventually, the background of the residue is due to weathering,
erosion and the substance analysis of additional rocks. These additional rocks may be
metamorphic, igneous or also could be additional sedimentary rocks. The category plus
the magnitude of the residues and the way they are developed will indicate the
categorization of various sedimentary rocks. The three categories of sedimentary rocks
are biochemical, clastic and evaporative. The distinguishing characteristics between the
the erosion of pre-existing rocks that have been broken down through weathering. When
the sediment is placed and underground, it lithifies and develops into new rock.
Furthermore, According to (Amethyst Galleries. (1995-2010). Sedimentary Rocks are
shaped through assembly and successive alliances of residue into several kinds of
rock. Its source is the residue. Sediments are unmerged substances that possess
distinct backgrounds. Eventually, the background of the residue is due to weathering,
erosion and the substance analysis of additional rocks. These additional rocks may be
metamorphic, igneous or also could be additional sedimentary rocks. The category plus
the magnitude of the residues and the way they are developed will indicate the
categorization of various sedimentary rocks. The three categories of sedimentary rocks
are biochemical, clastic and evaporative. The distinguishing characteristics between the