Introduction to Landforms - Rocks
Classification of Rocks
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- all rocks fit into
three (3) major categories:
- Igneous - "fire
rocks" from inside Earth
- Sedimentary
- sediments cemented together
- Metamorphic
- recycled and changed
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Igneous
rocks - magma & lava
- mafic to felsic (or acidic)
- intrusive - "plutonic"
rocks formed deep beneath Earths surface
- lighter granite (Sierra
Nevada)
- dark gabbro (Penryn, CA)
- coarse crystals
- cools much
slower beneath surface
- volcanic / extrusive - volcanic
events
- "jointed"
igneous rocks
Sedimentary
rocks
stratification
- "strata" or layers stacked upon one another
- sediments compacted by
pressure
- removing air spaces
and pores
- cementation from
silicon dioxide, calcium carbonate, iron oxide
- visible
in southwestern landscapes
Sedimentary categories
- clastics / detrital - broken
rock fragments glued together
- organic rocks
- remains of plants and animals
- chemical (precipitates)
- chemical solutions
Metamorphic
- "change shape"
- characterized by foliation
and hardness
- enormous heat and
pressure change structure of rock
- harder and more compact,
resistant to erosion
- sedimentary and igneous
changed
- metamorphism found in
Gold country
Rock
Cycle - recycled rocks
- how do hard rock become
sediment?
- how do sediments become
molten igneous rock?
- how do igneous become
metamorphic rock?
Isostasy and crustal rebound
- major uplift and deformation
of large landmasses
- well after plate tectonics
- mountains continue to rise; float on denser asthenosphere
- lifted primarily
by removal of weight & mass (ice caps, oceans,
or rock)
- N. America, Florida,
Yucatan Peninsula