plate tectonics + rocks

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56 Terms

1
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wegener’s five arguments

fit of the continents, locations of past glaciations, distribution of climate belts, distribution of fossils, matching geologic units

2
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how does new ocean floor form?

continents rift apart, upwelling of magma reaches the surface and pushes continental plates apart

3
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young ocean floor is located [closer to/farther away from] the MOR

closer to

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the farther away you are from the MOR, the [younger / older] the ocean floor

older

5
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common bathymetric features to identify an MOR

high point in elevation at the MOR, symmetrical decrease in elevation on either side

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where is the MOR?

C

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positive anomalies

magnetic north aligned with geographic north

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negative anomalies

magnetic north aligned with geographic south

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Where is the MOR 

point C

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common paleomagnetic features to identify MOR

normal polarity, symmetrical banding on either side

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newest seafloor corresponds to [upper/lower] rock in the geometric polarity timescale

upper

12
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divergent boundary

two or more plates are spreading apart from each other

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what force acts at divergent boundaries?

ridge-push

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convergent boundary

when plates collide with each other

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what happens at an ocean-continental boundary?

oceanic lithosphere subducts under continent

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force during convergent boundaries

slab pull forces

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what features emerge at a convergent boundary

trenches and volcanic arcs

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hot spot

fixed spot in the mantle that forms volcanoes as lithospheric plates move across it

19
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ridge push

gravity forces push new crust downwards, away from divergent boudary

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slab pull force

dense ocean slab is pulled down by gravity, bringing ocean plate into the mantle and facilitating pulling oceanic lithosphere from MOR

21
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true/false: slab pull forces also work on divergent boundaries

true

22
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how do slab pull forces affect divergent boundaries

they facilitate movement of plates

23
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true/false: youngest seafloor is at convergent boundaries

false

24
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where are earthquakes found at divergent boundaries

concentrated at the boundary

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where are earthquakes found at convergent boundaries

along the boundary and inland on continental plate

26
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fit of the continents

continents look like they can fit like puzzle pieces

27
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evidence for fit of the continents

maps, geography, edges, of the continents

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locations of past glaciations

glaciations appear to have been originally connected in Pangaea

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evidence for locations of past glaciations

striations, glacial till

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striations

scratch marks left by glacier

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distribution of climate belts

continents once occupied different climate zones

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evidence for distribution of climate belts

specific flora/fauna

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distribution of fossils

same fossils found in South Africa and South America

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evidence for distribution of fossils

fossils

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matching geologic units

same precambrian rocks found in multiple continents

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evidence for matching geologic units

rocks, mountain ranges

37
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minerals

naturally occuring (formed by a geological process), solid, orderly arangement of atoms and a definable chemical composition (inorganic)

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crystalline

regular internal geometric shape

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ways to form minerals

solidification, precipitation from water, diffusion, biomineralization, precipitation from gas

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solidification

when minerals crystalize out of a fish

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precipitation from water

when minerals crystalize from water

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diffusion

atoms migrate and build mineral structures

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biomineralization

when minerals crystalize from organisms

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precipitation from gas

when minerals crystalize from a gas

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how many classes are minerals grouped into

seven

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where is the anion in the chemical formula

the end of the formula

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where is the cation in the chemical formula

the beginning of the formula

48
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silicates

SiO4/4 anionic group

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sulfides

metal cation bonded to sulfide anion (S2)

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oxides

metal cation bonded to oxygen aniona

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halide

halogen or salt producing ion

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carbonate

CO2 is anionic group

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native metals

pure masses of a single metal

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sulfates

metal cation bonded to SO4/2 anionic group

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ways to identify minerals

color, streak, luster, hardness, fracture & cleavage

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