Types of Rocks
3 Basic Types Sedimentary Igneous Metamorphic
3 Types of Sedimentary Rocks Clastic Chemical Organic
Clastic Sedimentary Rock Sediments form when rocks are weathered and eroded Sediments are moved by wind, glaciers and water Most clastic sediments are deposited in the ocean
Clastic Sedimentary Rock Particle size is key to type of rock –Gravel is > 2 mm –Sand is 1/16 mm to 2 mm –Mud is < 1/16 mm Clay is < 4 um Silt is > 4 um
Sandstone
Conglomerate
Shale
Chemically Precipitated Sedimentary Rock Ions released during chemical weathering are carried away in solution Inorganic Precipitates –Halite –Gypsum Organic precipitates –Silica (diatoms) –Calcium carbonate – shells - CaCO 3 –Dolomite - CaMg(CO 3 ) 2
Halite
Gypsum
Diatomaceous Earth
Limestone
Dolomite
Organic Sedimentary Rock Sediments or rocks consisting mostly or entirely from plant material –Peat –Coal BituminousAnthracite
Sedimentary Environments Lakes Lower courses of rivers Shallow ocean Deep ocean
Extrusive & Intrusive Igneous Rocks Intrusive- Magma under the surface –Coarse-grained –Magma cools slowly and large crystals grow over a long period of time –Gabbro, diorite, granite
Granite
Gabbro
Extrusive & Intrusive Igneous Rocks Extrusive- Lava at the surface –Fine-grained –Lava cools very quickly, consequently crystals do not have time to grow and develop –Basalt, andesite, rhyolite, obsidian
Basalt
Rhyolite
Obsidian
Explosive Volcanism Fragmented magma ejected explosively –Ash plumes –Pyroclastic flows
Pumice
Metamorphic Rocks Rocks change at the chemical level Grade of metamorphism Shearing Foliation
Nature of Metamorphism Changes take place while a solid Due to heat and pressure Protolith – original rock
Metamorphic Rocks Foliated vs. Nonfoliated
Metamorphic Rocks Foliated- Metamorphic rock in which minerals have been rearranged into visible bands.
Schist
Gneiss
Slate
Metamorphic Rocks Nonfoliated- Metamorphic rock that does not show bands.
Marble
Quartzite
Regional vs. Contact Metamorphism Regional Contact (or thermal)
Contact Metamorphism