Limestone
Limestone is a sedimentary
                                                 rock, composed mainly of skeletal
                                                 fragments of marine organisms such
                                                 as coral, forams, and mollusks. Its
                                                 major minerals are the minerals
                                                 calcite and aragonite, which are
                                                 different crystal forms of calcium
                                                 carbonate (CaCo3).
COLOR: It is ordinarily white, but may be colored by impurities, iron oxide making it
brown, yellow, or red and carbon making it blue, black, or gray.
STREAK: White                                      LUSTER: Dull to Pearly
HARDNESS: 3-4                                      DENSITY: 2.3-2.7g/cm3
CLEAVAGE: Non-existent                             FRACTURE: Splintery
GRAIN SIZE: Fine Grained                           TRANSPERANCY: Opaque
Limestone can be considered as the following:
    Chemical sedimentary rock – formed by the
      precipitation of calcium carbonate from lake or
      ocean water.
             Ex. Tufa
                        Biological sedimentary rock – contains remains of
                    marine organisms/skeletal fragments of marine organisms
                    (corals, mollusks and etc.)
                           Ex. Chalk
       Limestone is composed primarily of 50% Calcium carbonate (CaCO3) in the
form of calcite. All limestones contain at least a few percentages of other materials,
such as quartz, feldspar, clay materials, pyrite, siderite
and etc.
       Limestones are mostly found in shallow, calm,
and warm marine waters. Others are found in caves,
which are formed through evaporation, like Stalactites
and Stalagmites.
        Stalactites (which is also a chemical sedimentary rock)
are formed when droplets of water seep down from above the
cave and evaporate before falling to the cave floor. When the
water evaporates, the calcium carbonate that was dissolved in
the water will be deposited on the cave ceiling. If the droplet falls
to the floor and evaporates there, a stalagmite could grow
upwards from the cave floor.
Varieties of Limestone
               Chalk – remains of marine organisms
               Tufa – produced by precipitation of calcium-laden waters at a hot
       spring, lake shores, or other locations.
Uses of Limestone
       For construction
              The Great Pyramid of Giza has an outside cover made entirely from
       limestone.
                                                     “The Giza Pyramids, built to
                                              endure an eternity, have done just
                                              that. The monumental tombs are
                                              relics of Egypt's Old Kingdom era and
                                              were constructed some 4,500 years
                                              ago.”
                                                      -National Geographic
              Used in making cement.