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Rocks, Minerals, and FossilsWritten by Rachel Tayse Baillieul, Ohio State University Geology StudentUse this two page publication as the starting place for your 4-H Self Determined Project. You may choose to do a little or a lot depending on your level of interest in this topic. Use in conjunction with our 4-H 365, Self Determined Project Guide; available through your county OSU Extension office or by visiting our web page at www.ag.ohio-state.edu/~idea. Be sure to register your Self Determined Project with your county OSU Extension office.
Do you know that table salt is a mineral? Have you ever thought about animals other than dinosaurs that are extinct and fossilized? Do you know that dull gray limestone and shiny green marble share the same chemistry? These an other questions can be undersood with a basic knowledge of rocks, minerals, and fossils. By definition, a mineral is an inorganic substance with a chemical formula
and crystal structure that can be found in nature. But what does this
mean? The word inorganic describes all things that are not living, or
have no carbon in their makeup. The chemical formula of each mineral is
like its list of ingredients. Table salt has a chemical formula of NaCl,
or sodium chloride. This tells us that all pieces of salt contain sodium
(Na) and chlorine (Cl.) Crystal structure is the shape of a well-formed
mineral. If you look closely at a piece of salt from your salt shaker,
you might notice that it is shaped like a cube. This is characteristic
of every salt crystal. Rocks are made of one or more minerals. If you look closely at concrete
or blacktop, you will notice there are many tiny pieces of minerals that
are glued together. Because humans create concrete and blacktop, most
geologists do not think of them as true rocks. However, many common rocks
such as granite and sandstone have visible pieces of minerals in a glue-like
background. Rocks are grouped into three categories: sedimentary, igneous, and metamorphic.
These groups reflect the manner in which the rock was formed. Sedimentary
rocks are formed by processes we can observe on the surface of the earth,
such as erosion, precipitation, and cementation. Limestone is a sedimentary
rock that is formed when calcium carbonate (CaCO3) precipitates, or dries,
from water. Igneous rocks are formed when the magma underneath the earth
solidifies. When a sedimentary or igneous rock is exposed to high temperature
or pressure underneath the surface of the earth, the rock becomes metamorphic.
If limestone is exposed to heat and pressure, it becomes marble, a metamorphic
rock that looks very different from limestone but actually has the same
chemical elements. Fossils are the remains of animals and plants that have been preserved
in rocks or minerals. Fossils can be grouped into body fossils and trace
fossils. Body fossils are preserved parts of the original body of the
organism. Trace fossils are evidence of the mode of life of ancient plants
and animals. They include tracks, burrows, borings, and feces that tell
us directly about the way an animal or plant lived and moved. Although
dinosaur bones are the most well now fossils, they are not the only fossils
that have taught us about the ancient past. The remains of snails, clams,
ferns, and many other organisms are common and also provide clues to life
on Earth before humans.
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