Lesson 1 Flashcards

(42 cards)

1
Q

produced by sudden movement of rock materials below the earths surface

A

earthquake

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2
Q

2 types of earthquake

A

tectonic earthquake
volcanic earthquake

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3
Q

movement along faults and plate boundaries

A

tectonic earthquake

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4
Q

induced by rising lava/magma beneath active volcanoes

A

volcanic earthquake

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5
Q

theory that explains the formation and deformation of the earths surface

A

Plate Tectonics Theory (1960)

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6
Q

earths outermost layer is divided into ___ major tectonic plates

A

15

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7
Q

Evidence for continental drift

A

matching coastlines
matching mountains
matching rock types and rock ages
matching glacier deposits
matching fossils

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8
Q

symptoms of active tectonic movements and as observed that the intense activity occurs predominantly on plate boundaries (seismic belts)

A

earthquake

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9
Q

large and stable rigid rock slabs with a thickness of about 100 km forming the crust and part of the upper mantle

A

plates

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10
Q

outer rock layer with non-uniform thickness of 25-60 km under the continents and 4-6 km under oceans

A

crust

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11
Q

portions of the earths interior below crust extending from 30 km - 2900 km

A

mantle

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12
Q

____ causes movement in the mantle with 1 to 10 cm/year

A

convection currents

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13
Q

Types of plate boundaries

A

divergent/rift zones
convergent/subduction zones
transform zones/transcurrent horizontal slip

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14
Q

plates separated by effusion of magma occurence; formation of mid-ocean ridge (Mid-Atlantic Ridge)

A

divergent/rift zones

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15
Q

adjacent plates collide; plates come together

A

convergent/subduction zones

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16
Q

two plates glide past one another but without subducting old lithosphere; plates slides past each other

A

transform zones/transcurrent horizontal slip

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17
Q

distorted blocks snaps back toward equilibrium and an earthquake ground motion is produced; AKA elastic rebound

18
Q

resulting fracture in the earths crust

19
Q

rocks bend under stress while storing elastic energy. when the strain in the rocks exceeds their strength, breaking will occur along the fault.

A

elastic rebound theory

20
Q

parameters used to describe fault motion and its dimension

A

azimuth
dip
slip/rake
relative displacement
area

21
Q

one block moves away vertically with respect to the other; footwall moves up the dip and away from the block overhanghing the fault plane

A

dip-slip faults

22
Q

adjacent blocks move horizontally past one another; can be right-lateral or left-lateral

A

strike-slip faults

23
Q

combination of strike-slip and dip slip movements; can either be normal or reverse and right or lefr lateral movements

24
Q

point under the surface where the rupture originates

A

focus/hypocenter

25
projection of the focus on the surface
epicenter
26
source parameters
epicentral distance hypocentral/focal distance focal depth
27
2 types of elastic seismic waves
body waves surface waves
28
aka 'preliminary tremors' because they are felt first and travels through the earths interior layers
body waves
29
cause alternate push (compression) and pull (tension) in the rock thus the waves propagates, the medium expands while keeping the same form
p-waves
30
material movement is the same direction as wave movement
p-waves
31
causes vertical and horizontal side-to-side motion and introduces shear stresses in rocks along their paths aka shear waves
s-waves
32
motion can be separated into horizontal and vertical components
s-waves
33
propagate across the outer layers of the crust generated by constructive interference of body waves travelling parallel to the ground surface and various underlying boundaries
surface waves
34
slower than body waves; rolling side to side movements
surface movements
35
generated by constructive interference of SH body waves and cannot travel across fluids
love waves
36
the motion is horizontally oscillating and perpendicular to the direction of propagation which is parallel to the earths surface
love waves
37
caused by constructive interference of body waves such as P and SV
rayleigh waves
38
particles of soil move in the form of a retrograde ellipse whose axis is perpendicular/vertically oscillating to the earths surface;
rayleigh waves
39
causes back and forth horizontal motion; motion is similar to that of being in a boat in the ocean; arrive last on seismogram
rayleigh waves
40
visual record of arrival time and magnitude of shaking associated with seismic wave
seismogram
41
adjustments that follow a major earthquake often generate smaller earthquake
aftershocks
42
small earthquakes often precede a major earthquake by days or by as much as several years
foreshocks