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97 Cards in this Set
- Front
- Back
rocky skin of the Earth, upper 100 km of Earth
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lithosphere
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where plates meet, either moving toward, sliding past, or moving away from each other
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plate boundaries
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composed of ultramafic rocky materials, denser than crust, causes plates to move
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mantle
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found in boundaries or interiors of plates, consist of a line of dormant volcanic features that ends abruptly in a single spot of active volcanism
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hot spots
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dramatic system of mountains resulting from ocean spreading between continental fragments
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mid-ocean ridges
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plates slide past each other. type of strike-slip fault, usually crossing the Mid-Ocean Ridge at a right angle, offsetting one segment of the Ridge from the next
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transform faults
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the descent of one plate beneath the other
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subduction
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molten rock underground
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magma
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chain of volcanic islands over a subduction zone. Arc is bowed toward the subducting plate
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island arcs
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where the ocean plate bends before sinking
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ocean trench
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doctrine that geologic processes have acted in the same regular manner throughout geologic time
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uniformitarianism
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first to give Earth a birthdate, 4004 BC. believed Earth was big ball of molten that cooled off
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Archbishop Ussher
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doctrine that sudden violent natural events are the chief agents for modifying Earth's crust
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catastrophism
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people who think Earth's crustal rocks were deposited by water
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Neptunists
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father of modern geology, discovered unconformity in rocks, gradualism (constant change)
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James Hutton
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discontinuity in rock layers, where one type of rock changes abruptly to another
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unconformity
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traced rock units across country, finding same fossils in diff areas.Noticed each layer had evolution of same fossil
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William Smith
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Earth is in continuous, gradual change, constantly decaying, renewing and repairing itself
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gradualism
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Rocks arranged into a vertical sequence, youngest being ontop
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stratigraphic column
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wrote Principles of geology, advocated uniformitarianism
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Charles Lyell
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early theory that the continents moved across the Earth's surface. replaced by plate tectonics (seafloor-spreading)
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Continental Drift
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Ancient supercontinent that included S America, Africa, Australia, Antarctica, and India
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Gondwana
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supercontinent of 300 million years ago that included most of Earth's landmasses
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Pangea
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any rock formed by evaporation, usually of salt water in a landlocked basin
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evaporite
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magnetic properties, lodestone
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magnetite
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study of measurement of the Earth's magnetic field from ancient rocks
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paleomagnetism
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a line connecting continents and magnetic poles. provided proof that continents move relative to poles and to each other
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polar wander curve
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In certain periods of time, Earth switched it's magnetic polarity
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magnetic reversal
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pattern that revealed long, zebra-like stripes of normal and reversed magnetic polarity in the basaltic ocean floor that alternated in a symmetrical fashion on either side of the ridge axis
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magnetic anomaly
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circulating convection currents under the ocean floor causes molted rock to ooze up beneath mid-ocean ridges as the seafloor spreads away to each side
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seafloor spreading
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increase in depth reflects the descent of oceanic crust. Descending slab creates inclined zone of earthquake foci
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Benioff Zone
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major distribution of earthquakes and volcanoes. adjacent to ocean trenches surrounding Pacific Ocean. Melting of Benioff Zone creates this
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Ring of Fire
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the descent of one plate below another
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subduction
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Theory that Earth's lithoshpere is made up of seperate pieces, plates, which migrate over the plastic mantle layer
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Plate Tectonics
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the plastic semisolid layer of Earth below the lithosphere
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asthenosphere
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results from continental blocks subsiding like the keystone of an arch, forming a steep wall. aka graben (non-marine sediments and basalt lava flows accumulate
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rift valley
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rift valleys that fail to open into oceans because spreading isn't successful. Become buried but are still active, causing earthquakes
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failed rifts
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Located in East Africa. Divergent plate boundary
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Great Rift Valley
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lithospheric plate forming from Great Rift Valley. Future plate
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Somali Plate
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Great Rift Valley, Somali Plate, and wide deep valley in Red Sea form this. (three arms of rift system) Example-Afar Triangle
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triple point
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Arid rift in Kenya and Tanzania. Causes evaporation as fast as the lakes fill
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Eastern Rift
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mineral often formed by evaporation and found in saline lake residue; major source of sodium compounds
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trona
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A volcanoe that is white. results from ash which contains sodium carbonate. then rain crystalizes it
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Ol Donyo Lengai
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chemistry ofa base. compounds produced from an antacid tablet are this. Magma form is rich in sodium, poor in silica
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alkaline
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common rock salt - sodium chloride. From evaporated hot dry air
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halite
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a calcium carbonate mineral deposited where groundwater is exposed to air. usually at hot springs, and in caves as stalactites and stalagmites
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travertine
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located on opposite side of Tanzania craton (ancient rocks) climate is wet unlike E Rift
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Western Rift
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deep, flat region of the ocean floor extending outward from the base of a continental slope
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abyssal plain
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first observation of mid-ocean ridges. SW of of the Azores.
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Project FAMOUS
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basalt drapes the valley slopes in bulbous flows called
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pillow lavas
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found in the East Pacific Rise, discovery of ribbed hollow pillars testified past presence of these
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submarine lava lakes
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region in Iceland that has had frequent eruptions since 1975
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Krafla
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formed when rising magma encounters waterlogged land and flash-heats the groundwater into steam which then explodes through overlying ground like a popping bubble
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pseudocrators
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Volcanoe that errupted with most lava in history. caused lava lakes and shortage of everything
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Lakakigar
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Lake that has lots of diatoms in it (free floating algae).
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Lake Myvatn
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death of diatoms create this on the lake floor. mined as polishing and filtering agent
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diatomite
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town with two volcanoes. known for fishing. Old volc- Helgafell. New- Eldfell
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Vestmannaeyar
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Precambrian
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Oldest Eon. 545-4600
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Proterozoic
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Youngest Eon in Precambrian. 545-2500
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Archean
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Middle Eon in Precambrian. 2500-4000
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Hadean
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Oldest Eon in Precambrian. 4000-4600
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Phanerozoic
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Youngest Eon. Longest Eon. .01-545
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Paleozoic
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Oldest Era in Phanerozoic. 245-545
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Cambrian
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Oldest Period in Paleozoic. 505-545
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Ordovician
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Above Cambrian in Paleozoic. 438-505
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Silurian
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Above Ordovician in Paleozoic. 408-438
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Devonian
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Last horizontal period in Paleozoic. 360-408
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Carboniferous
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First left block in Paleo. 286-360
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Mississippian
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Lowest right block in Paleo. 320-360
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Pennsylvanian
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Above right block in Paleo. 286-320
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Permian
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Above Side by side blocks. last in paleozoic. 245-286
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Mesozoic
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Middle Era. 66-245
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Triassic
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Oldest period in Mesozoic. 208-245
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Jurassic
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Middle period in Meso. 144-208
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Cretaceous
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youngest period in meso. 66-144
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Cenozoic
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Youngest era. 0-66
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Tertiary
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First left block period in ceno. 1.6-66
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Carboniferous
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First left block in Paleo. 286-360
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Mississippian
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Lowest right block in Paleo. 320-360
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Pennsylvanian
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Above right block in Paleo. 286-320
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Permian
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Above Side by side blocks. last in paleozoic. 245-286
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Mesozoic
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Middle Era. 66-245
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Triassic
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Oldest period in Mesozoic. 208-245
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Jurassic
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Middle period in Meso. 144-208
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Cretaceous
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youngest period in meso. 66-144
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Cenozoic
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Youngest era. 0-66
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Tertiary
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First left block period in ceno. 1.6-66
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paleogene
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First right block period in ceno. 23.7-66
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neogene
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Last right block period in ceno. 1.6-23.7
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Paleocene
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Oldest epoch in paleozoic. 57.8-66
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Eocene
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above paleocene in paleozoic. 36.6-57.8
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Oligocene
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youngest epoch in paleo. 23.7-36.6
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Miocene
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Oldest in Neogene. 5.3-23.7
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Pilocene
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Youngest in Neo. 1.6-5.3
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Pleistocene
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Oldest in quaternary period. .01-1.6
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Holocene
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Youngest epoch. 0-.01
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Quaternary
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Youngest period. 0-1.6
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