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A CTIVIT Y  6.3  Clastic and Detrital Sediment


        Name: ______________________________________   Course/Section: ______________________   Date: ___________



           A.   Obtain two pieces of granite or diorite. Hold one in each hand and tap them together over a piece of paper. As you do this
            you should notice that you are breaking tiny sedimentary grains from the larger rock samples. These broken pieces of rocks
            and minerals are called clasts (from the Greek  klastós , meaning “broken in pieces”).

            1.   Using a hand lens or microscope, observe the tiny clasts that you just broke from the larger rock samples. Describe what
              minerals make up the clasts and whether or not the clasts are fragments of mineral crystals, rock fragments, or a mixture
              of both.





            2.   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



            3. Roundness  is a measure of how
              much the profile of a grain of                          GRAIN ROUNDNESS
              sediment resembles a circle. It is most
              often visually estimated using a chart
              like this one. Re-examine your clasts
              from Part A1 and sketch the outline
              of several of them. Compared to the
              chart, what is the roundness of the   Very angular  Subangular        Subround      Well-rounded
              clasts that you sketched?









            4.   Using a grain size scale (from GeoTools 1 or 2 at the back of your manual), circle the Wentworth size class(es) of the clastic
              sediment that you made above.

                gravel        sand             silt                           clay
                 (grains > 2 mm)     (grains 1/16 to 2 mm)   (grains too small to see but you can     (grains too small to see or feel; like
                                              feel them)                     chalk dust)

            5.   Obtain a piece of quartz sandpaper and lay it flat on the table. Find a sharp corner on one of the granite/diorite samples that
              you used above and sketch its outline in the “before abrasion” box below. Next, rub that corner against the quartz sandpaper
              for about 10 seconds. Sketch its profile in the “after abrasion” box. What did this abrasion process do to the sharp corner?














        Before abrasion                                             After abrasion


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