Chapter 32: Vocab Flashcards

1
Q

A machine that measure seismic waves.

A

Seismograph

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2
Q

Waves that travel through the Earths interior.

A

Body waves

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3
Q

Fastest waves that compress and expand rock. Can travel through anything.

A

Primary waves (p waves)

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4
Q

Transverse. Particles travel perpendicular to the direction of wave motion. Can travel only through solids.

A

Secondary waves (s waves)

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5
Q

Travel on the earths surface.

A

Surface waves

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6
Q

Waves that move up and down.

A

Rayleigh waves

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7
Q

Waves that move side to side and are the slowest.

A

Love waves

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8
Q

Separates the crust from the mantle.

A

Mohorovoicic discontinuity

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9
Q

Composed of iron and nickel.

A

Core

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10
Q

Solid layer of the earth.

A

Inner core

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11
Q

Movement of the outer core helps create the earths magnetic field.

A

Outer core

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12
Q

Surrounds the core, 3000 km thick.

A

Mantle

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13
Q

Lower part of the upper mantle. Flows like plastic.

A

Asthenosphere

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14
Q

100 km thick, includes the upper portion upper mantle and the crust.

A

Lithosphere

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15
Q

The top part of the lithosphere varies in depth. Oceanic

Crust- 10 km thick. Continental crust- 20-60 km thick.

A

Crust

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16
Q

Compression of rocks cause the Earth’s crust to bend.

17
Q

Rocks that are folded or pushed downward.

18
Q

Rocks that are pushed upward.

19
Q

Rocks that are under pressure and actually break.

20
Q

The rock that is above the fault plane.

A

Hanging wall

21
Q

The rock that is below the fault plane.

22
Q

Hanging wall that drops below the footwall.

A

Normal fault

23
Q

The hanging wall moves above the footwall. (Rockies)

A

Reverse fault

24
Q

Footwall and hanging wall move horizontally past each other. (San Andreas fault)

A

Strike slip fault

25
Measures amplitude of seismic waves. Logarithmic. Energy/ magnitude.
Richter scale
26
Measures damage caused by earthquake.
Mercalli scale
27
All the continents were once connected into a single supercontinent.
Pangaea
28
Proposed by Alfred wegener. The idea that all the continents were connected and over time have moved to their current locations.
Continental drift
29
Proposed by H. H. Hess. Convection cells in the mantle push new material up to the surface at mid ocean ridges. Older lithospheric material will be found farther from the mid ocean ridge.
Seafloor spreading
30
The earths lithosphere is divided into several large plates that ride on the asthenosphere. Earthquakes, volcanoes, and mountains typically occur at plate boundaries.
Theory of plate tectonics
31
Plate boundary with plates moving apart. (Mid Atlantic ridge)
Divergent boundary
32
Plate boundary with plates that run into each other.
Convergent boundary
33
One plate is forced under the other plate, creates an oceanic trench.
Subduction
34
The more dense plate is pushed downward, creates island arcs.
Oceanic-oceanic
35
Oceanic plate is subducted. Creates active volcanoes and mountains.
Oceanic- continental
36
The plates break and fold on each other; form mountains (Himalayas). Earthquakes are common but no subduction.
Continental-continental
37
Plates are sliding past each other. No subduction, earthquakes are common. (Strike-slip fault) (San Andreas fault)
Transform fault
38
Earthquake generated waves.
Seismic waves