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97 Cards in this Set

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