System Earth Ch 07 Flashcards

1
Q

seismology

A

the study of earthquakes and related phenomena

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2
Q

earthquakes

A

the rapid release of stored energy as a result of quick movement between rocks. Can be as deep as 700km below surface

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3
Q

fault

A

fracture caused by an earthquak

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4
Q

surface waves

A

travel along the earth’s surface and transmit earthquake energy

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5
Q

body waves

A

travel through the earth and are categorised as P or S waves

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6
Q

P waves

A

longitudinal
they can travel through the earth’s core but also through the crust. They provide the estimate for how big the core is

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7
Q

S waves

A

are transverse waves. They cannot travel through the earth’s core. Can only travel through solids. The furthest they travelis 103 degrees from where they were emitted.

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8
Q

mohorovcic discontinuity

A

difference in earth’s crust thickness

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9
Q

continental vs oceanic crust

A

continental is thicker but less dense. They differ in chemical and meteorological compositions as well.

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10
Q

igneous

A

cooling and solidification of magma. If this occurs below the earth’s surface, it is an intrusive rock

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11
Q

lithification

A

conversion of loose sediment into rocks (sedimentary rocks who would believe it)

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12
Q

sedimentary rocks

A

compacted sediment bigger than sand

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13
Q

metamorphic rock

A

rocks that form under high pressure. As long as no melting is involved, it’s metamorphic

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14
Q

major rock forming minerals

A

feldspars, quartz, olivine, pyroxene

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15
Q

what type of rock covers most of the earth’s surface

A

sedimentary

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16
Q

mantle

A

a seismic low velocity zone exists
mantle rotates in the same direction as the earth

17
Q

core

A

is made up of iron, nickel and ligth elements. It is much denser than the mantle, changing its seismic wave velocity. It is the source of earth’s magnetic field.

18
Q

earth’s magnetic field

A

in the core, like a dynamo, transforms energy into fluid motions. The liquid outer core convects and conducts electricity. The solidification of iron releases heat, allowing for a liquid iron core.

19
Q

mid ocean ridges

A

has a rift and is an indicator of seafloor spreading

20
Q

lithosphere and asthenosphere

A

upper crustal part of the lithosphere is brittle. Below this is the asthenosphere, a region of the upper mantle that acts more like a fluid than a solid. It is ductile.

21
Q

divergent margins

A

constructive plate boundary
rift vallyes, lava rises and cools, forming new land
triple junction is if there is a centre point of the margin

22
Q

convergent margin

A

destructive plate boundary. you get subduction of the denser plate and melting and slab pull and convection currents etc. the subducting plate creates deep sea trenches. you get a volcanic arc

23
Q

convergent margin oceanic vs. oceanic

A

same thing but it’s called a volcanic island arc. Marianas trench is an example.

24
Q

convergent continental vs. continental

A

neither can be subducted so you get a separation of crustal poition of the lithospheric plate from teh mantle bbelow. Subduction of teh mantle part might happen whil the continental crust compresses and crumples. This results in mountain formation like when india collided with asia.

25
Q

transform margins

A

conservative plate boundary
lithosphere is neither created (extruded) or destroyed (subducted)

26
Q

transform faults

A

form at conservative plate boundaries, like san andreas fault

27
Q

what drives plate tectonics

A

heat from the earth
convection in the mantle
forces acting on plates

28
Q

how does radioactive decay come into plate tectonics?

A

the heat of decay results in warmth = energy

29
Q

potential heat sources

A

the heat in the core is from earth’s creation and this is transferred to the mantle

30
Q

convection in the mantle

A

occurs, maybe split into two

31
Q

forces acting on plates

A

gravitation force generated by high topography of a mid-ocean ridge on te rest of the oceanic plate.
slab pull - pulls opposite end of the plate into a subduction zone.
bending resistance
trench suction
friction
negative buoyancy

32
Q

rock cycle

A

starts with igneous, they are weathered, turned in to sediment and transported around. Chemically altered sometimes, they are deposited and accumulated in sediment accumulation. This happens in the sea and ocean. If they remain above sea and surface level, stuff is eroded again and then the cycle can start again. If not, metamorphic rocks form under high pressure.

33
Q

where does metamorphism occur?

A

deep in sedimentary basins along passive margis, in the defomred regions of active margins, or in the crust where igneous activity ingects into something cold.

34
Q

wilson cycle

A

continents assemble into a super continent and then break up again. This takes about 500 M y

35
Q

hypothesis of the wilson cycle

A

the continents come together where the mantle is cold and then they accumulate and provide a thermal layer. So the heat circulation changes and then

36
Q
A