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.

A

FAULT

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.

A

EPICENTER

25
Q

Distance from epicenter to any place of interest is called the

A

EPICENTRAL DISTANCE

26
Q

The depth of the focus from the epicenter is the

A

FOCAL DEPTH

27
Q

The higher diameter along equator is caused by the higher ________________ generated along the equator due to rotation of earth.

A

CENTRIFUGAL FORCE

28
Q

The oceanic crust is constituted by

A

BASALTIC ROCKS

29
Q

continental part by

A

GRANITIC ROCKS

30
Q

The mantle has an average
temperature of about

A

2200 DEGREE CELCIUS

31
Q

The specific gravity of
outer core is about

A

9-12

32
Q

The specific gravity of
inner core is

A

15

33
Q

create shear stresses at the bottom of the plates which drags them along the surface of earth.

A

CONVECTION CURRENTS

34
Q

interior portion of a plate is usually tectonically quiet, earthquakes also occur far from plate boundaries

A

INTRA-PLATE EARTHQUAKES

35
Q

The earthquake that occurs at a plate boundary is known as

A

INTER-PLATE EARTHQUAKES

36
Q

It could be a fault, a joint or any other linear geological phenomena.

A

LINEAMENT

37
Q

is the direction of a horizontal line on the surface of the fault

A

STRIKE

38
Q

measured in a vertical plane at right angles to the strike of the fault

A

DIP

39
Q

The vertical shift along a fault plane is called

A

THROW

40
Q

the horizontal displacement is termed as

A

HEAVE

41
Q

the slippage occurred along the dip of the fault

A

DIP-SLIP FAULT

42
Q

the movement has taken place along the strike

A

STRIKE-SLIP FAULT

43
Q

The movement occurs diagonally across the fault plane

A

OBLIQUE SLIP FAULT

44
Q

the hanging wall has been displaced downward relative to the footwall

A

NORMAL FAULT

45
Q

the hanging wall has been displaced upward relative to the footwall

A

REVERSE FAULT

46
Q

the foot or the hanging wall do not move up or down in relation to one another

A

WRENCH FAULT

47
Q

which are a subdivision of
reverse faults, tend to cause severe earthquakes

A

THRUST FAULT

48
Q

As the plate try to move relative to each other, strain energy gets built up along the
boundaries

A

ELASTIC REBOUND THEORY