Geology 3 Flashcards
What is Igneous
Formed by the solidfication of magma
What is Sedimentary
Formed from the products of the breakdown of pre existing rocks
What is metamorphic
formed by the transformation of minerals in a preexisting rock under the influence of elevated temperature, pressure, hot fluids or all 3.
What is Magma
Molten rock that originates at the depths as great as 200km within the earth. It consist of Si, O, Fe, Ca, Na, K, Mg, and several gasses.
What is Lava
Magma without the gas that flows on the surface,
Volcanic (Extrusive)
on the surface, fine grained, glassy, vesicular, volcanic fragments.
Plutonic (Intrusive)
magma that crystalizes below the surface, larger crystal grains.
Crystalization of magma
- Ions are arranged in orderly patterns.
- Crystal size of rock is determied by the rate of cooling.
Cooling rate - Slow
Forms large crystals
Cooling rate - Fast
Forms microscopic crystals
Cooling rate- very fast
Forms glass
Igneous rock Classification
- Texture
2.Mineral Combustion
Texture meaning
Size and arrangement of crystals.
Texture types
Aphanitic
Phaneritic
Prphyritic
Glassy
Pegmatic
Vesicular
Pyroclastic
Aphanitic
fine grained, fast rate of cooling, less than 1cm across. Basalt and Andesite
Phaneritic
Coarse grained, slow rate of cooling, intrusive, large mineral grains (1mm to 1km). Granite and Diorite
Porphyritic
2 distinct crystal sizes, 2 rates of cooling, extrusive. Andesite Porphyry.
Glassy
Very fast rate of cooling, extrusive. Obsidian and Perlite.
Pegmatic
Intrusive, crystals larger than 1km across. Pegmatite.
Vesicular.
Extrusive, holes formed by escaping gas. Scoria (Vesicular basalt) and pumice.
Pyroclastic
Extrusive volcanic fragments of crystals, rocks, glass shards, pumice fragments. Ash flow tuff and volcanic Breccia
Mineral Combustion
Magma rich with silica along with Al, Mg, Fe, Ca, Na, and K.
Mineral Combustion Types
Felsic
Intermediate
Mafic
Ultramafic
Felsic
light colored like quartz, feldspars and minor dark materials like horneblende and biotite. Bhyolite and Granite
Intermediate
cotain equal amounds of dark horneblende biotite and lighter feldspars. Andesite and diorite.
Mafic
Cointain mostly dark Mg and Fe rich silicates along with olivine as well as very little light colored feldspars. Basalt and Gabbro.
Ultramafic
Consists of yellowing green olivine and pyrozene Peridotite.
Eruptive Materials
Lava Flows
Gases
Pyroclastics
Lava Flows
Basaltic Lavas are more fluid
Pahoehoe Lava type
loraided lava
Aa Lava Type
Rough, jagged blocks
Gases in magma
gasses are 1 - 5% of magma
H2O and Co2
HCL HF CO SO2 H2S H2 NH3 CH4 SiF4
Pyroclastics Meaning
Fire Fragments
Pyroclastic Types
Ash
Pumice
Lapilla
Cinders
Blocks
Bombs