Scienceas Flashcards

(57 cards)

1
Q

intensity and magnitude may be described in terms of

A

Earthquakes

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2
Q

Earthquakes are caused by

A

stress

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3
Q

tension, shearing, and compression may result in

A

faults and folds

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3
Q

stress may be due to

A

tension, shearing, and compression

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4
Q

faults are classified as

A

reverse, normal, and strike slip

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5
Q

is the boundary between the earths crust and mantle

A

Moborovicic disconuinity

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6
Q

the mohorovicic disconuinity was first identified by

A

Andrijia Mohorovicic in 1909

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7
Q

makes up by 85 percent of earths volume

A

mantle

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8
Q

is composed of iron and nickel alloy.

A

core

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9
Q

proposed the existence of a supercontinent he called Pangaea in his account of the origins and continents.

A

German meteorologist Alfred Wegener

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10
Q

that at one time these two continents had been joined together and slowly drifted apart

A

Continental drift theory

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11
Q

called the nothern half

A

Laurasia

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12
Q

southern half

A

Gondwanaland

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13
Q

seperated by a big body of water called

A

Tethys Sea

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14
Q

deals with the study of the record of earth’s magnetic field in rocks is called

A

paleomagnetisim

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15
Q

Suggests that the Earth is divided into seven large plates and small rigid plates

A

plate tectonics

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16
Q

is the region where plates meet

A

plate boundary

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17
Q

types of boundaries (3)

A

Transform , Convergent , and Divergent

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18
Q

two plates slide each other horizontally

A

Transform boundary

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19
Q

is the most active type of boundary

A

Convergent boundary

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20
Q

when the sinking occurs is called the

A

subduction zone

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21
Q

is the deepest part of an ocean floor

A

trench

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22
Q

triggeresd by the melting of subducting the atmosphere

A

Volcanic activity

23
Q

when plates move apart

A

DIvergent boundary

24
are sites where earths crust are growing
boundaries
25
continous chain of volcanic mountains and rifts is called
mid-ocean ridges
26
is a rift zone in the middle of the ocean
Mid-Atlantic ocean
27
refers to all the movements in the lithosphere
Diastrophism
28
stress that rocks undergo may be due to
Tension , Compression , and shearing forces.
29
stretch or pull rock layers
Tension
30
push rock layers
Compression
31
makes rock layers slide
Shearing forces
32
causes rock layers to break
compressional or tensional
33
deformed or disturbed rocks
Mountains
34
the bending of the rock layer upward
anticline
35
breaks and causes tremors
faulting
35
strengths or elastic limits, they snap and an earthquake occurs
elastic rebound theory
36
occurs when one block of rock moves down and another moves up
normal fault
37
produces a horizontal displacement
strike-slip fault
38
form ridges along the fault line
fault scarps
39
combination of a strike-slip fault and a normal fault
oblique slip fault
40
one block moves upward in relation to another
thrst or reverse fault
41
produced when rock layers break and release energy
Seismic waves
42
Earth in the form of strain in rock layers is released
Earthquakes
43
The point on the surface of earth above the focus is called the
epicenter
44
Movement in the tectonic plats produces two types of seismic waves
body waves and surface waves
45
Waves that propagate through the earth's interior
Body waves
46
propogate through medium faster than the other seismic wave
Surface waves
47
propagate through the medium slower than P waves
Secondary waves
48
named after british geophyscist, are the fastest surface waves
Augustus Love , Love waves
49
roll around just like a wave rolls across a lake or ocean , named by briish physical scientist
John William Strut , Rayleigh Waves
50
describes the amount of energy at the focus of origin
magnitude
50
two ways scientists quanify the size of an earthquake
intensity and magnitude
51
is measured by its perceivable damage
intensity
52
Types of fault
normal, strike-slip, oblique slip, and reverse fault
53
3 main layers of the earth
Crust , mantle , and core.
54
instruments predicting an earthquake
Seismometer , seismograph, laser range funer, tide gauge, geiger counter , global posting system