Page 197 - Laboratory Manual in Physical Geology
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A CTIVIT Y          6.4  Biochemical and Chemical Sediment and Rock


        Name: ______________________________________   Course/Section: ______________________   Date: ___________



           A.   Seashells are grains of sediment made by the biochemical processes of organisms, so they are grains of biochemical sediment.
            When you find a rock with a fossil seashell, then you have found evidence that the rock contains sediment deposited where
            the sea animal lived (i.e., in the ocean, in a marine environment). Some limestone is entirely made of the seashells or broken
            pieces of seashells. Obtain a seashell (e.g., hard clam shell) and draw it to the right of this paragraph. It may be easiest to trace
            it, then fill in the outline with details of what the shell looks like inside or out. Next, place the shell into a plastic sandwich
            bag and take the bag to the hammering station in your lab. Lightly tap the bag with the hammer to break up the shell into
            pieces. Return to your table and view the broken pieces of shell with a hand lens.

            1.   The shell fragments that you just made are called  clasts  (from the Greek  klastós , meaning “broken in pieces”). Geologists
              commonly refer to several different kinds of clastic sediment. Circle the one that you just made.
              ■ pyroclastic sediment —volcanic bombs and/or volcanic rocks fragmented by volcanic eruption
              ■ bioclastic sediment —broken pieces of shells, plants, and/or other parts of organisms
              ■ siliciclastic sediment —broken pieces of silicate mineral crystals and/or rocks containing them



            2.    Compared to  FIGURE   6.3 , what is the roundness of your clasts? _________________________________




            3.   What is the roundness of the clasts in this picture (× 1 scale)? __________________________________
              Explain how and in what environment the shell clasts could have
              attained their roundness.

















            4.   Some limestone is made of shells that are calcareous (calcite or aragonite), like visible seashells, but they are microscopic
              and cannot even be seen with a hand lens. Chalk is such a limestone. Some chalk used with modern blackboards is clay or
              plaster-of-Paris, rather than real chalk. Obtain a piece of chalk from your lab room or instructor. Explain how dilute HCl
              (hydrochloric acid) can be used to help you test your chalk and find out if it is real chalk or not. Then conduct your test
              and report the results of your test.









            5.    Based on  FIGURE  6.10 (page 165), how and where does chalk form?













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