|
Home Calendar About Bijou Mission & Goals Principal's Page Students Student Support/Resources Courses Counseling Library Staff D11 Home
"To the dull mind all nature is
leaden. To the illumined mind the whole world burns and sparkles with light." --
Ralph Waldo Emerson
| |
Minerals and Rocks |
|
| Metamorphic
Rocks
|
Table of
Contents:
|
-
See
some,
-
go to USGS
-
Go to
the Volcano World Metamorphic Rock Lesson...
-
- Rocks that have been changed by heat and pressure,
or in composition, over a very long time.
- Great heat and immense pressure can change any
rock, igneous, sedimentary, and metamorphic, without melting
- that change is a metamorphosis
Heat and Pressure
- Huge areas of rock under the surface can undergo
long periods and small areas of contact between opposing land masses can metamorphose
which can involve:
- Changing shape (flattening, spreading out)
- Changing composition (exchange of atoms, ions,
isotopes)
CLASSIFICATION OF METAMORPHIC ROCKS
Foliated
- Flattened mineral grains, lined up in parallel bands
Examples: slate, gneiss
CAUTION!!!
Be careful to not confuse these with
certain sedimentary rocks!
Nonfoliated
- Mineral grains are changed in many ways, but are not
arranged in layers or bands
Examples:
Quartzite (from sandstone)
Marble (from limestone, high in calcite)
|