
At one time or another, you have probably
held a rock in your hand. Recall the texture.
Was it smooth, polished by the force of sand and salt water
pounding it onto the beach? Was it rough and cragged, left
exposed for centuries to the wind and sun of a canyon wall?
Recall the color. Was it coral and pink, like the
colors of Bermuda's sand? Was it fiery red, like the colors
of Arizona's canyons? Recall the size. Was it a
handful, heavy with the weight of being worn? Was it a tiny
pebble, a small fragment broken off from what it once
was?
Rock is our world. The planet Earth is,
essentially, just one big interesting rock, sometimes called
"the third rock from the sun." The multi-faceted rock we
live on supports life in many ways. The deep oceans, the
vast deserts, and the high mountains, are just a few of the
ways rock emerges and supports life.
Rock remembers. Geology is the science and
study of the earth and its life, especially as recorded in
rock. Rock, then, keeps record of the passage of time
and the evolution of living things.
The word rock refers to solid mineral
deposits. Rock is mineral, but not all minerals are
rock. Minerals are all substances that can't be classified
as "animal" or "vegetable." Metal ores found in the earth,
like gold and silver, are minerals. Crystalline substances,
like salt and quartz, are minerals. Homogeneous natural
substances, like water and gas, are also minerals. These non-solid
minerals, however, are not considered "rock."
- Begin with Minerals
Minerals are classified in several "classes" based upon
common properties or characteristics. Explore the diversity
of minerals as preparation for thinking about rock. The
alphabetical listing of minerals by name quickly shows how
diverse minerals really are. Specimens, on display at The
Geology Museum, range from the most common to the extremely
rare. The Mineral Gallery offers both descriptions and a
growing collection of images.
- The Mineral Gallery
- Minerals
By Name
- Minerals from the Geology Museum
- The
Clausthal Online Mineral Collection
- The Mineral and Gemstone Kingdom
- Alphabetical Mineral Reference
- Chemical Formulae for Minerals and Gems
- Commercial Mineral Names
- A Virtual Tour of the Janet Annenberg Hooker Hall of Geology, Gems, and Minerals at the Smithsonian
- Form Solid Mineral Deposits
Some minerals, given time and circumstance, form solid
deposits. These solid mineral deposits are known as rock.
Pressure, temperature, erosion, and friction are forces that
effect the formation of rock. The rock formation process
allows geologists to classify rock into three groups:
sedimentary, igneous, and metamorphic.
Sedimentary rock forms when layers of "sediment" (small
particles of solid minerals like sand and pebbles) fuse
together over time under the force of water or wind.
Sedimentary rock is commonly found in and near riverbeds and
streambeds. Igneous ("fire-formed") rock forms after
minerals are heated to extremely high temperatures and then
allowed to cool. Hawaii is a well-known source of igneous
rock. Most igneous rock forms when hot molten lava cools to
a solid state. Metamorphic rock forms when rock undergoes a
transformation from one structure to another, usually caused
by pressure, heat, and water. For example, a rock that is
compacted to a more crystalline condition has undergone a
metamorphosis.
- These resources offer more information about the
formation of rock.
- Rocks and Minerals of Kentucky
- Add Unusual Characteristics
Some rock formations develop the unusual property of
fluorescence. The minerals in the rock give off radiation as
visible light in certain circumstances. These fluorescent
rock specimens show their behavior in three different
lighting situations: normal cool light, longwave ultraviolet
light, and shortwave ultraviolet light.
- Fluorescent
Rocks
- Ken's Fluorescent Minerals
- Cut and Polish Some Rock
Gemstones are rock or other fossilized organic
materials (like amber below) that are cut and polished to a
brilliant state. Gemstones possess certain characteristics
that make them attractive and valuable. Optical properties
and durability are two examples. If a gemstone can be cut
such that it reflects light brilliantly it becomes valuable
for its luster. Extremely strong gemstones are desired for
their durability. A diamond, for example, has a high luster
and a high durability. Therefore, the diamond has become
valuable and has come to symbolize long enduring
relationships.
- The Rainbow of Gems
- How are Gemstones Classified?
- Fossilize Some Treesap
And then there's amber. Amber is the fossilized resin of
ancient trees. Approximately thirty and ninety million years
ago, sticky sap oozed from trees, catching insects, leaves,
seeds, and other forest debris in a sticky trap. Over a
long, long time, the sticky resin hardened into a solid
fossilized deposit known as amber.
- The
World of Amber
- Assume A Fixed and Definite Shape
Many minerals are capable of forming solid crystalline
deposits. Crystals are formed when a mineral solidifies
under force in such a way that the solid forms a regular
repeating arrangement on both the external surface and the
molecular level. Quartz, a transparent crystal of silica
(sand), is an abundant crystal used for many purposes.
- Introduction to Crystallography and Mineral Crystal Systems
- Crystal Structure Movies
- Frequently Asked Questions About Crystals
- Sand
- Consider Some Other Ideas
So we have all of this rock, now what do we do? Throughout
human history, civilizations have invented ways to use rock
to improve the quality of their lives. Coal mining is a
recent case worth study. Powder River Coal Company in
Gillette, Wyoming, is the second largest coal producing
company in the United States. Consider the process, the
reward, and the consequence.
- Powder River Coal Company
- Alone in the wilderness without matches or a lighter,
you can rub two sticks together to create heat from friction
that can cause a spark and light a campfire. Or, you can
strike certain pieces of rock together to create a spark. If
striking
two small pieces of rock together can cause a spark, imagine
what
happens when two huge rock plates underneath continents bump
into each other. The sparks really fly! Earthquakes,
landslides, floods, and volcanic eruptions are a few
possible results.
- A Model of Three Faults
- Every rock has a story to tell. A good geologist knows
when to shut up and listen. Each rock has a long and winding
history. The rock of the Ocoee River Gorge along US Highway
64 in the scenic Cherokee National Forest of southeastern
Tennessee has been waiting millions of years to tell its
story. So shut up and listen.
- The Geologic Story
of the Ocoee River
- Teach Others About Rock
These educational resources offer suggestions for teaching
others about the fascinating world of rock. The activities
and lesson plans may enhance your traditional geology
curriculum.
- Atlas of Rocks and Minerals
- Rock Classification
- A Gem of a Story Activities
The best way to wrap your mind around rock,
however, is to wrap your hands around rock. No matter which
of these resources you decide to use in your study of rock
and minerals, make sure you get outside and get your hands
on some rock. Compare textures. Compare colors. Compare
sizes. The rock will remember.

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