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    BACKGROUND:
    Quartz  is a very common mineral. It is composed of
    silicon and oxygen atoms, and has the chemical formula SiO2
    (silicon dioxide). Quartz is very hard (7 on the Moh’s Hardness Scale). It
    grows in an easily recognizable hexagonal crystal habit. It fractures when
    broken, i.e., it does not have cleavage. Quartz occurs in many varieties. Most common is the
    clear variety, which the ancient Greeks called "crystallos" or
    "clear ice." The word "crystallos" eventually evolved
    into the word "crystal." Depending on its color, which is caused
    by trace chemical impurities, quartz forms a great variety of gemstones
    including agate, amethyst, adventurine, bloodstone,
     smoky quartz, carnelian,
    citrine, onyx, rose quartz, and  tiger's eye. Quartz is a very important mineral commodity. It has
    many uses including applications in the computer, communications, food, and
    jewelry industries. Quartz is also the main component of the sand used to
    produce concrete and glass, as well as in sandpaper, sandblasting, and
    smelting. Your students may be familiar with two other
    substances that are composed of silicon dioxide, obsidian and glass. While
    these materials have the same composition as quartz, they lack a crystalline
    structure, so they are not minerals. They are classified as amorphous
    solids.PROCEDURE: 
      Get a beaker with water. Explain to the students that the water
        represents "pure" quartz because it contains no impurities. As
        they add food coloring to the water, explain how the resulting color
        change is analogous to colored quartz. Make sure they understand that a
        tiny, or trace, amount of color gives the whole substance a different
        look.
In exercise 2, have the students examine the following examples of
        silicon dioxide and describe their characteristics. They should also
        determine whether the substances are minerals, rocks, or amorphous
        solids. 
        ROSE QUARTZ  - a mineral, a common gemstone; pink color caused by
        trace amounts of titanium ADVENTURINE  - a mineral, a common gemstone that has inclusions of
        mica and hematite imparting a green color to the stone CLEAR CRYSTAL OF QUARTZ  - a mineral, 6-sided crystal is the shape
        in which a quartz crystal grows CHERT  - a sedimentary rock, made of very fine quartz crystals;
        composed of fossil radiolarians (one celled organisms that make a
        skeleton of quartz) CITRINE  - a mineral, yellowish-brown color caused by high
        temperatures AMETHYST  - a mineral, purple color, caused by ferric iron in
        trace amounts MILKY QUARTZ  - a mineral, color caused by trace amounts of water
        inside the mineral QUARTZ GEODE  - a rock composed of many visible quartz crystals:
        formed in a rock cavity that slowly filled with quartz along its margins OBSIDIAN  - an igneous rock, non-crystalline silicon dioxide GLASS  - man-made, non-crystalline silicon dioxide QUARTZ SANDSTONE  - a sedimentary rock, composed of rounded quartz
        grains cemented together QUARTZITE  - a metamorphic rock, probably originally quartz
        sandstone, that has been subjected to extreme pressures and temperatures QUARTZ SAND  - rounded quartz grains not cemented together
The students should conclude that quartz is a very common mineral that
        can occur in a wide variety of forms. It sometimes makes up gems, or
        entire rocks like quartzite or quartz sandstone. The reason quartz is
        found in many materials is that quartz is hard and thus lasts longer
        than most minerals. |