Page 93 - Laboratory Manual in Physical Geology
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Tetrahedron
                                                               Needles
                                                               (acicular)                       (4 faces)

                                Twinned
            Pyramidal                                                                   EQUANT
                                              Cube
                                             (6 faces)
                                                               Bladed

                                                                                                 Dodecahedron
                                                                                                   (12 faces)
                                                                                Pyritohedron
             Octahedron                                                         (12 faces)
             ((dipyramid))                      Dendritic

                          Tabular (shaped                         Fibrous
                           like a book)
                                                                                                Radiating needles






                           Rhombohedron
                         (a leaning block with     Prismatic   Wires                            Botryoidal (bubbly
                       6 faces, each a rhombus)                                                 masses; radiating
         Dipyramid prism                                                       Scalenohedrons    needles inside)

          FIGURE 3.4   Crystal forms and combinations.           Crystal form  is the geometric shape of a crystal, and is formed by intersecting flat outer
        surfaces called  crystal faces . Combinations of two or more crystals can form patterns, shapes, or twins that also have names.  Massive  refers to a
        combination of mineral crystals so tightly inter-grown that their crystal forms cannot be seen in hand sample.


            Crystal Systems.   Each specific crystal form can be       Metallic Luster.   Minerals with a  metallic luster (M)
          classified into one of six  crystal systems  (  FIGURE   3.5   )   reflect light just like the metal objects in your home—they
        according to the number, lengths, and angular relation-  have opaque, reflective surfaces with a silvery, gold, brassy,
        ships of imaginary geometric axes along which its crystal   or coppery sheen (  FIGURES   3.2B   ,    3.6A   ,    3.7A   ).
        faces grew. The crystal systems comprise 32 classes of       Nonmetallic Luster.   All other minerals have a  nonmetallic

        crystal forms, but only the common crystal forms are
                                                             luster (NM) —a luster unlike that of the metal objects in
        illustrated in   FIGURE   3.5   .
                                                             your home (  FIGURES   3.1   ,    3.2A   ,    3.3   ). The luster of non-
            Mineral Habit.   A mineral’s  habit  is the  characteristic   metallic minerals can also be described with the more
        crystal form(s) or combinations (clusters, coatings,   specific terms below:
        twinned pairs) that it habitually makes under a given set       ■   Vitreous—very reflective luster resembling freshly

        of environmental conditions. Pyrite forms under a variety   broken glass or a glossy photograph
        of environmental conditions so it has more than one

        habit. Its habit is cubes, pyritohedrons, octahedrons, or      ■   Waxy—resembling the luster of a candle
        massive (  FIGURE   3.4   ).                             ■   Pearly—resembling the luster of a pearl


            Luster.   A mineral’s  luster  is a description of how light      ■   Earthy (dull)—lacking reflection, like dry soil
        reflects light from its surfaces. Luster is of two main types—     ■   Greasy—resembling the luster of grease, oily

        metallic and nonmetallic—that vary in intensity from bright
        (very reflective, shiny, polished) to dull (not very reflective,       Tarnish and Submetallic Luster.   Most metallic min-
        not very shiny, not polished). For example, if you make a list   erals will normally tarnish (chemically weather) to a
        of objects in your home that are made of metal (e.g., coins,   more dull nonmetallic luster, like copper coins. Notice
        knives, keys, jewelry, door hinges, aluminum foil), then   how the exposed metallic copper crystals in   FIGURE   3.6
        you are already familiar with metallic luster. Yet the metallic   and the galena crystals in   FIGURE   3.2A    have tarnished
        objects can vary from bright (very  reflective—like polished   to a nonmetallic luster. Always observe freshly broken
        jewelry, the polished side of aluminum foil, or new coins) to   surfaces of a mineral (e.g.,   FIGURE   3.2B   ) to determine
        dull (non-reflective—like unpolished jewelry or the unpol-  whether it has a metallic or nonmetallic luster. It is also
        ished side of aluminum foil).                        useful to note a mineral’s luster on fresh versus tarnished


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