SEISMOLOGY Flashcards

1
Q

is the study of the generation, propagation and measurement of seismic waves through earth and the sources that generate them.

A

SEISMOLOGY

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2
Q

The earth’s shape is an

A

OBLATE SPHEROID

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3
Q

the average specific gravity
of earth is about

A

5.5

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4
Q

the outer part of the earth is where the life exist.

A

CRUST OR LITHOSPHERE

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5
Q

is a 2900 km thick layer

A

MANTLE

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6
Q

Upper Mantle reaching a
depth of about 400 km made of

A

OLIVINE AND PYROXENE

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7
Q

Lower Mantle made of more
homogeneous mass of

A

MAGNESIUM, IRON OXIDE AND QUARTZ

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8
Q

SPECIFIC GRAVITY OF MANTLE

A

5

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9
Q

Core has a radius of

A

3470 km

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10
Q

INNER CORE HAS A RADIUS OF

A

1370 Km

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11
Q

the core is composed of

A

molten iron, nickel, sulfur or silicon

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12
Q

proposed the hypothesis that the continents
had once formed a single landmass before breaking apart and drifting to their present locations.

A

German Scientist Alfred Wegener (1915)

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13
Q

explains that the lithosphere is broken into seven large (and several smaller) segments called

A

PLATES

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14
Q

He proposed that a large continent termed Pangae existed in earth around 200 million years ago and was surrounded by an ocean called.

A

PANTHALASA

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15
Q

WHAT IS THE CONTINENTAL SIZED PLATES

A

African, American, Antarctic, Indo-Australian, Eurasian
and pacific plate

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16
Q

are areas along the edges of plates move apart from each other

A

SPREADING RIDGES OR DIVERGENT BOUNDARIES

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17
Q

are formed where the two plates move toward each other. In this process, one plate could slip below the other one or both could collide with each other.

A

CONVERGENT BOUNDARIES

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18
Q

These boundaries are created when either oceanic lithosphere subducts beneath oceanic lithosphere (ocean-ocean convergence), or when oceanic lithosphere subducts beneath continental lithosphere (ocean-continent convergence).

A

SUBDUCTION BOUNDARIES

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19
Q

When two plates with continental lithosphere collide, subduction ceases and a mountain range is formed by squeezing together and uplifting the continental crust on both plates,

A

COLLISION BOUNDARIES

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20
Q

occur along the plate margins where two plate moves past each other without destroying or creating new crust

A

TRANSFORM BOUNDARIES

21
Q

is used to describe a discontinuity within rock mass, along which movement had happened in the past.

22
Q

are mappable linear surface features and may reflect subsurface phenomena.

A

LINEAMENTS

23
Q

The region on the fault, where rupture initiates is known as the

A

FOCUS OR HYPOCENTER

24
Q

is the location on the earth surface vertically above the focus.

25
Distance from epicenter to any place of interest is called the
EPICENTRAL DISTANCE
26
The depth of the focus from the epicenter is the
FOCAL DEPTH
27
The higher diameter along equator is caused by the higher ________________ generated along the equator due to rotation of earth.
CENTRIFUGAL FORCE
28
The oceanic crust is constituted by
BASALTIC ROCKS
29
continental part by
GRANITIC ROCKS
30
The mantle has an average temperature of about
2200 DEGREE CELCIUS
31
The specific gravity of outer core is about
9-12
32
The specific gravity of inner core is
15
33
create shear stresses at the bottom of the plates which drags them along the surface of earth.
CONVECTION CURRENTS
34
interior portion of a plate is usually tectonically quiet, earthquakes also occur far from plate boundaries
INTRA-PLATE EARTHQUAKES
35
The earthquake that occurs at a plate boundary is known as
INTER-PLATE EARTHQUAKES
36
It could be a fault, a joint or any other linear geological phenomena.
LINEAMENT
37
is the direction of a horizontal line on the surface of the fault
STRIKE
38
measured in a vertical plane at right angles to the strike of the fault
DIP
39
The vertical shift along a fault plane is called
THROW
40
the horizontal displacement is termed as
HEAVE
41
the slippage occurred along the dip of the fault
DIP-SLIP FAULT
42
the movement has taken place along the strike
STRIKE-SLIP FAULT
43
The movement occurs diagonally across the fault plane
OBLIQUE SLIP FAULT
44
the hanging wall has been displaced downward relative to the footwall
NORMAL FAULT
45
the hanging wall has been displaced upward relative to the footwall
REVERSE FAULT
46
the foot or the hanging wall do not move up or down in relation to one another
WRENCH FAULT
47
which are a subdivision of reverse faults, tend to cause severe earthquakes
THRUST FAULT
48
As the plate try to move relative to each other, strain energy gets built up along the boundaries
ELASTIC REBOUND THEORY