Rocks and Minerals
These
are the solid materials that make up the layers of the
Earth. Rocks are made up of one or more minerals. Minerals
grow in specific geologic environments ranging from deep
within the Earth (higher temperatures and pressures), to
near the surface (lower temperatures and pressures). Each
mineral has a distinctive set of chemical and physical
properties that makes it unique. All minerals are inorganic
(they were never alive) and have an internal order and
chemical composition. In Florida, some of the more common
minerals include quartz (beach sand), aragonite (shells),
calcite and clay minerals such as kaolinite and
montmorillonite.
In certain areas of Florida, some minerals are
of such economic importance that they are mined. In
northeast Florida, for example, a group of minerals known as
"heavy minerals" are mined from ancient beach ridges. These
minerals, which only comprise a few percent of the total
sand, are useful for their titanium (Ti) content. The
element Ti is useful for manufacturing paint. In southwest
Florida, phosphate minerals are mined for the manufacture of
fertilizer products. Florida produces about one-fourth of
the world's supply of phosphate.
There are three major rock types: igneous,
metamorphic and sedimentary. Igneous rocks, such as granite
or basalt, form as a result of a magma (molten rock) that
has cooled to form a variety of interlocking crystals.
Metamorphic rocks form due to changes in the temperature and
pressure resulting from a changing geologic environment. For
example, if limestone undergoes an intense amount of heat,
it becomes the metamorphic rock, marble. In Florida,
sedimentary rocks are the most common. These rocks are made
up of cemented mineral particles. One example is shell
fragments (the mineral aragonite) that are cemented together
by calcite to form the sedimentary rock coquina. Another
type of sedimentary rock is limestone, which is mined for
road building and other construction applications. This rock
is made up of small calcite particles formed by marine
organisms that build up large reefs in the oceans. During
much of Florida's geologic history, it was covered by the
ocean.
Much of the surface of Florida is covered by
sediment (loose mineral particles, such as quartz sand), or
sedimentary rocks such as limestone and dolostone. Igneous
and metamorphic rocks do not occur naturally at the surface,
but are found in deep wells reaching from 3,500 feet to
deeper than 18,670 feet below land surface.
Suggested reading:
- Lane, E., 1987, A guide to rocks and minerals of Florida;
Florida Geological Survey Special Publication 8 (revised),
61 p.