Now that minerals are a little clearer (hopefully) we can move on to rocks. Now
rocks have a lot more basic purposes than minerals including cement, building
materials, decorative materials and of course, paperweights. The way you
identify minerals is by certain characteristics like cleavage and hardness.
Identifying a rock is a lot different than that. It is not really harder or
easier, just different. Lets start of this page with the basic definition of a
rock, then go into some rock basics. Then from here we will move on to the three
main types of rocks; igneous, sedimentary, and metamorphic.
Definition of a Rock - A naturally formed
aggregate of mineral matter constituting a significant part of the
earth's crust. (www.dictionary.com)
- {essentially a rock is a mineral or a bunch of minerals mashed into
one lump and distorted from a pure mineral state.}
There are 3 main types of rocks. Click on the link to go
to their respective websites.
The Rock Cycle
Rock Breakdown
Igneous Rocks - Are formed from
the solidification of liquid rock, also known as magma or lava.
Sedimentary Rocks - Are
formed from the breakdown of others rocks and the cementation of those particles
from other rocks and animals
Metamorphic Rocks - Are formed
from the alteration of any other rock (including other metamorphic
rocks) due to increased heat and pressure
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The background image is an outline of a
Shuvosaurus skull, which was created by me for my Master's Thesis.