Unit 14 Flashcards

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1
Q

Plate tectonics & earthquakes

A

•Continents seem fixed from human perspective. Until the mid-twentieth century, scientists believed Earth’s continents were rigid

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2
Q

Continental Drift

A

continents move on Earth’s surface; Alfred Wegener proposed this idea in 1912; Pangaea

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3
Q

Plate Tectonics

A

Theory behind motion of lithospheric plates; plates float on the ATHENOSPHERE
(get tectonic plates image form slides)

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4
Q

Convection

A

transfer of heat through a fluid; the asthenosphere bubbles up and encounters the crust which leads it to fracture the crust.

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5
Q

mid-oceanic ridges

A

formed by magma rising up from mantle

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6
Q

sea floor separates

A

new basaltic crust created

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7
Q

ocean trenches

A

sea floor comes together; older lithosphere descends into the asthenosphere where it is recycled

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8
Q

Plate Boundaries

A

the border between two plates

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9
Q

Divergent

A

moving away from each other; constructive; mid-oceanic ridge; youngest crust

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10
Q

Convergent

A

moving towards each other; destructive; collisions

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11
Q

oceanic-continental (destructive)

A

A) oceanic plates sink since it is more dense
B) forms oceanic trench and continental mountains (cascades &Andes)
C) earthquakes occur along margin
D) volcano formation along the plates (continental volcanic arc)
E) forms metamorphic rocks-blueschist

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12
Q

oceanic-oceanic (destructive)

A

A) subduction results in undersea trench formation
B) deep and shallow earthquakes
C) island volcanic arc

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13
Q

continental-continental

A

A) no subduction since two plates are highly buoyant
B) builds huge mountain ranges
C) volcanoes are rare
D) shallow earthquakes are relatively common
E) examples: Himalayan mountains

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14
Q

Transform (Stripe-slip)

A

slide against one another; neither creates nor destroys crust; commonly produce shallow earthquakes; San Andreas fault line (right lateral transform boundary)

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15
Q

Fault

A

a crack in the Earth’s surface

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16
Q

Earthquakes

A

The shaking and trembling of the Earth’s surface caused by sudden releases of stress within the crust; can happen near the surface, deep in the crust, or even in the upper mantle
•generate pulses of energy known as seismic waves

17
Q

Body waves

A

A)p waves: travel faster and can move though any material; can travel through entirety of Earth
B)S Waves: travel slower and can only pass through solid material

18
Q

Surface Waves

A

waves you feel and shake the surface

•Seismograph

19
Q

Focus

A

the actual center of the earthquake; source of shaping

20
Q

Epicenter

A

the point on the Earth’s surface directly above the focus

21
Q

Magnitude

A

is energy that is actually released, and it is measured by Richter scale (logarithmic), there is only 1 rating per earthquake;1-10

22
Q

Intensity

A

is the severity of shaping and it is measured by the Mercalli scale; multiple Mercalli ratings (highest at the epicenter) 1-12

23
Q

Tsunamis

A
  • seismic sea wave

* Produced when ocean water is suddenly displaced by movement of the crust in an earthquake or by a large land slide

24
Q

San Francisco Earthquake of 1906

A

occurred April 18, 7.8 earthquake occurred at 5 am with an 11 on the Mercalli scale; 3000 people died and 80% of san Francisco was destroyed due to the fires