Geology test 1 BLINN MOSLEY – Flashcards

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The study of rock
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Geology
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minerals, stream flow, age dating
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Earth Geology
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deals with physical material and the processes that act on them.
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Physical Geology
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dating rocks, origin of the earth, and study of different types of plants and animals.
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Historical Geology
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other topics in geology
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-physics -chem -biology -math
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geologist working unit of time
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one million years
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what geologists consider to be "recent"
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last 10,000 years
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steps of scientific method
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1. make observations 2. make hypothesis 3. test hypothesis 4. theory
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2 big ideas of geology
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1. catastrophism 2. uniformitarianism
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sudden catastrophic events shape the surface of the earth. EXAMPLE: the grand canyon
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catastrophism
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the processes that we see on earth today happened the same way in the past. EXAMPLE: erosion
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uniformitarianism
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began in the early twentieth century as continental drift
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scientific revolution
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the theory that came from scientific revolution in 1968
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plate tectonics
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makes up continental crust
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Granite
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makes up oceanic crust
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Basalt
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four reasons why Pangea is proven to be real
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1. continents fit like puzzle 2.fossils match across continents 3. rock and geological features match 4. ancient climates (plants)
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seven continental crusts
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1.N. America 2.S. America 3. Pacific 4. Eurasia 5. Africa 6. Australia 7. Antartica
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what gave us a better picture of the ocean floor
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ocean ridge system
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the earth's crust has individual plates that interact in various ways.
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theory of plate tectonics
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the rigid outer layer of earth, includes crust and upper mantle
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lithosphere
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a subdivision of the mantle situated below the lithosphere
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asthenosphere
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a coherent unit of earth's rigid outer layer that includes the crust and upper unit
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lithosphere {plate}
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a boundary in which two plates move apart, resulting in upwelling of material from the mantle to create new seafloor.
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divergent plate boundaries (spreading center)
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process of splitting a continent into smaller pieces
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rifting
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a representation of where divergent takes place
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rift valley
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a hypothesis, first proposed in the 1960's by Harry Hess that suggested new oceanic crust is produced at the crests of mid- oceanic ridges, which are the sites of divergence.
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seafloor spreading
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A linear zone along which continental lithosphere stretches and pulls apart. makes a new oceanic basin
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continental rift
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seafloor spreading leads to the generation of new oceanic lithosphere at mid - ocean ridge systems
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divergent plate boundary
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a boundary in which two plates move together, resulting in oceanic lithosphere being thrust beneath an overriding plate, eventually to be absorbed into the mantle.
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convergent plate boundary
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A boundary in which two plates slide past one another without creating or destroying lithosphere.
transform plate boundary
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transform plate boundary
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three types of plate conversion
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1. oceanic - continental 2. oceanic - oceanic 3. continental - continental
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A narrow, elongated depression of the seafloor
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deep - ocean trench
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the process by which most igneous rocks melt
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partial melting
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mountains formed in part by igneous activity associated with the subduction of oceanic lithosphere beneath a continent.
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continental volcanic arc
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A chain of volcanic islands generally located a few hundred kilometers from a trench where there is active subduction of one ocean plate beneath another.
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volcanic island arc
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A linear zone of irregular topography on the deep - ocean floor that follows transforms faults and their inactive extensions.
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fracture zone
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A mass of hotter-than-typical mantle material that ascends toward the surface, where it may lead to igneous activity
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mantle plume
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a concentration of heat in the mantle, capable of producing magma that, in turn, extrudes onto Earth's surface. EXAMPLE: Hawaiian islands
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hot spot
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A chain of volcanic structures produced as a lithospheric plate moves over a mantle plume
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hot-spot track
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the temp above which a material loses its magnetization
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curie point
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the natural remnant magnetism in rock bodies
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paleomagnatism
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A change in Earth's magnetic field from normal to reverse.
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magnetic reversal
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A magnetic field the same as that which presently exists.
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normal polarity
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A magnetic field opposite as that which currently exhists
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reverse polarity
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A sensitive instrument used to measure the intensity of Earth's magnetic field at various points.
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magnetometer
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composed of minerals
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Rock
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minerals five components
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1. must be natural 2. inorganic 3. solid substance 4. definite chemical compound 5. definite crystal structure
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90 naturally occurring elements not man made
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Natural Elements
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atoms bound together
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compound
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Proton + neutron 0 electron -
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Atom
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number of protons, defines what element it is
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Atomic #
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number of protons and neutrons
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Atomic mass
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a charged atom (positive or negative)
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ionic bond
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six properties of minerals
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1. form 2. luster 3. color 5. hardness 6. cleavage 7. specific gravity
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name the eight mineral groups
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1. Oxygen 2. Silicon 3. Aluminum 4. Iron 5. Calcium 6. Sodium 7. Potassium 8. Magnetism
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partial melting in the lower crust and upper mantle produces...
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magma
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super heated, melted rock deep under ground
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magma (hot)
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liquid rock at the surface
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lava (hot)
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cool and harden deep under ground
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Intrusive igneous rocks (cold)
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cool and harden at surface
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Extrusive igneous rock (cold)
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-minerals that didn't melt -new mineral crystals
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solid magma
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-liquid rock
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liquid magma
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-kept in magma by pressure -happens when pressure decreases -water vapor and carbon dioxide make most of it
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gas magma
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As heat and energy decreases magma starts making a ___________ structure.
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crystal
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five different crystalline structures. ( tetrahedra)
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1. single tetrahedra 2.single chain tetrahedra 3. double chain tetrahedra 4. sheet silicate tetrahedra 5. 3D framework tetrahedra
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igneous rocks are classified by two stuctures
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-texture -composition
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size and orientation of grains
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texture
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what elements are in the rock and in what amounts
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composition
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three factors affecting crystal size
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1. rate of cooling 2. amount of silica present 3. amount of dissolved gas
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result: large crystal size
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slow cooling
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result: small crystal sizes
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fast cooling
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result: no crystals or minerales
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instant cooling
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6 textures
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1.Aphanetic 2. Phaneritic 3. Porphyritic 4. Obsidian 5. Pyroclastic 6. Pegmatetic
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-crystals too small to be seen (need magnification) -feels like sandpaper -can be vesicular
Aphanetic
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Aphanetic
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-crystals are large enough too see and can be used to identify the rock
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Phaneritic
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-has phenocrysts and ground mass -cools from slow to rapid
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Porphyritic
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-no crystals/ minerals -cools rapidly
Obsidian
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Obsidian
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-wide range of grain sizes -grain is not interlocked -comes from volcanic ash
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Pyroclastic
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-very large -forms in late stage of cooling -cools fast -lots of water and silica make the atoms move quickly
Pegmatic
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Pegmatic
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igneous rocks are made of _________ minerals
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silicate
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8 elements in the crust
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-oxygen -silicon -Aluminum -iron -calcium -sodium -potassium -magnesium
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2 composition groups
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-ferromagnesium silicate -nonferromagnesium silicate
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-has lots of iron and magnesium -less silicate -dark: black/green
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ferromagnesium silicate
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-has less iron and magnesium -more silicate -light: pink, white, clear
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nonferromagnesium silicate
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-felsic -low iron and magnesium -high silica
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granite
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-mafic -high iron and magnesium -low silica
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basaltic
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-ultramafic -very high iron and magnesium -very low silicate -makes most of mantle
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periodtite
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-intermediate -middle iron and magnesium -middle silica
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andersetic
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-felsic comp -quartz, feldspar, and mica -phaneritic texture -slow cooling EXAMPLE: continental crust
granite
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granite
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-felsic comp -quartz, feldspar, and mica -aphanitic texture -fast cooling EXAMPLE: Yellowstone park
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rhyolite
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-felsic - mafic comp -no minerals -glassy texture -rapid cooling EXAMPLE: lava cools instantly
obsidian
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obsidian
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-felsic- mafic comp -no minerals -glassy and vesicular texture -rapid cooling EXAMPLE: lava cools instantly
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pumice
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felsic composition (4 types)
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-granite -rhyolite -obsidian -pumice
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andesitic composition (2 types)
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-andesite -diorite
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-intermediate comp -plagioclase, amphibole -porphyritic to aphanitic textures PLATE TECTONICS: c-o conversions
andesite
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andesite
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-intermediate comp -plagioclase, amphibole -phaneritic texture PLATE TECTONICS: c-o conversions
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diorite
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mafic compositions (2 types)
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-basalt -gabbro
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-mafic comp -plagioclase feldspare, pyroxene, olivine -aphanitic texture PLATE TECTONICS: o-o spread to conversions
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basalt
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-mafic comp -plagioclase feldspare, pyroxene, olivine -phaneritic texture PLATE TECTONICS: oceanic crust
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gabbro
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