CH 25 Flashcards

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1
Q

Mountain ranges on the seafloor separated by valleys.

A

mid-Ocean ridge

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2
Q

A long, narrow depression forms in between peaks along the mid-ocean ridge.

A

Rift Valley

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3
Q

The boundary where two plates collide

A

convergent plate boundary

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4
Q

the denser plate dives beneath the continent

A

subduction

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5
Q

boundary between two plates that are moving apart

A

divergent plate boundary

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6
Q

boundary where plates slide horizontally past each other in opposite directions

A

transform plate boundary

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7
Q

the sudden movement or vibration of the ground that occurs when rocks slip

A

earthquake

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8
Q

a crack in earths crust along which rock has moved

A

fault

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9
Q

sudden release of strain energy as rock moves along a fault

A

elastic rebound

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10
Q

point of origin for an earthquake

A

focus

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11
Q

point on earths surface directly above the focus

A

epicenter

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12
Q

who came up with the continental drift hypothesis

A

Alfred Wegener

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13
Q

what is some evidence of the continental drift

A
  1. The coast lines matched up like a puzzle piece.
  2. Mountain ranges with the same rock types
  3. large land animals
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14
Q

What was the name of the super continent

A

Pangaea

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15
Q

who came up with the sea floor spreading hypothesis

A

Harry Hess

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16
Q

how did he discover the sea floor spreading

A

sonar

17
Q

on the ocean floor where is the newer rock formed

A

closer to the MOR

18
Q

what are the three types of plate boundaries

A
  1. divergent plate boundary
  2. convergent plate boundary
  3. transform plate boundary
19
Q

how do convergent plat boundaries move

A

move together

20
Q

Subduction only happens with which type of plate boundary

A

Convergent plate boundary

21
Q

what are the 2 types of crust do we have

A
  1. continental crust

2. oceanic crust

22
Q

what do hot spots create

A

volcanic islands

23
Q

how do divergent plate boundaries move

A
24
Q

how do transform plate boundaries move

A

slide past each other

25
Q

what is a convection current

A
  1. magma heats up, becomes less dense, and rises

2. magma cools, becomes more dense,and sinks