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Rock Types Concept Maps

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Rock Types Concept Maps Teacher instructions: Run the concept map pieces off on colored paper. It is best to run the 3 different sets of pieces on 3 different colors ... – PowerPoint PPT presentation

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Title: Rock Types Concept Maps


1
Rock Types Concept Maps
Teacher instructions Run the concept map pieces
off on colored paper. It is best to run the 3
different sets of pieces on 3 different colors of
paper. Run the concept map outlines on white
paper. Run a regular white paper copy of each
concept map outline for each student. Let
students work in small groups using their books
or other sources to place the pieces in the
correct spot on the concept map outline. When
they have everything in place, they call the
teacher to check their work. Teacher oks or
gives guidance into which area(s) need to be
re-worked. When all is correct, teacher gives
each student in group a blank copy of the outline
to write in the answers (shown on pieces).
Students keep their copy of the concept map for
reference, and begin the next concept map with a
new set of pieces and outline.
2
Sedimentary rocks
Compaction pressure from weight of water pushes
sediments together
Cementation sediments stuck together with
mineral glue
All form from sediments into layers under water
Clastic
Organic
Chemical
Evaporation
Evaporites
Conglomerate
Breccia
Sandstone
Shale
Chalk
Coal
Limestone
Gypsum
Rock Salt
Sediments of various sizes
Once living materials
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Metamorphic Rocks
Any kind of rock
Mineral crystal bands or layers
Mineral crystal bands or layers
Foliated
Quartzite
Unfoliated
Gneiss
Marble
Shale
Schist
Sandstone
Limestone
Granite
Slate
Heat, pressure, chemical reactions
Granite, basalt, or slate
Regional metamorphism occurs over large areas
when deep rocks are changed by heat and pressure
Contact metamorphism occurs when rocks are
heated by contact with hot magma
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8
Igneous rocks
Hot, molten lava
Two cooling rates
Light colored
Light colored
Dark colored
Dark colored
Coarse grained
Fine grained
Half and half
Earths surface
Earths interior
Slow cooling
Fast cooling
Intrusive
Extrusive
Porphyry
Granite
Diorite
Gabbro
Peridotite
Rhyolite
Andesite
Pumice
Basalt
Scoria
Obsidian
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