4 Flashcards

(44 cards)

1
Q

caused by the sudden and rapid movement of large volumes of rock along fractures on the surface of the earth called

A

Faults

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2
Q

The outermost shell of the earth, which includes the crust and the uppermost mantle, consists of

A

Tectonic plates

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3
Q

There are two types of seismic waves:

A

Body waves
Surface waves

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4
Q

are seismic waves that travel through the interior of the earth.

A

Body waves

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5
Q

are the first waves that reach the surface of the earth and make the ground shake. They move the ground back and forth along the direction they are traveling.

A

Primary waves

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6
Q

are body waves that vibrate perpendicular to their propagation direction, producing an up and down motion. They move slower but shake the ground more strongly than P waves.

A

Secondary waves

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7
Q

are waves that are trapped near the surface

A

Surface waves

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8
Q

are surface waves that have a horizontal motion perpendicular to the direction they are traveling.

A

Love waves

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9
Q

the ground in a rotational manner with no transverse motion.

A

Rayleigh waves

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10
Q

is the number of times a movement such as ground shaking is repeated within a certain amount of time. High frequency earthquakes affect small buildings more than the high rise ones.

A

Frequency

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11
Q

is the primary cause of earthquake damage to man-made structures.

A

Groundshaking

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12
Q

is a secondary hazard if the shaking sufficiently damages electric and gas lines.

A

Fire

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13
Q

Ground shaking also triggers other earthquake hazards such as

A

Landslides liquefaction

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14
Q

a set of rules that set standards on the construction of buildings. If properly implemented, it can ensure that buildings are constructed properly, can survive an earthquake with minimal damage, and therefore, not endanger the occupants. Earthquake-resistant buildings are by no means immune to earthquakes, but will sustain less damage than their conventional counterparts.

A

Building code

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15
Q

is the visible breaking and displacement of the Earth’s surface along the trace of a fault.

A

Ground rupture

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16
Q

faults are vertical or near-vertical faults that displace rock horizontally.

A

Strike slip

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17
Q

If the block opposite you when looking across a fault moves to the left, it is a

A

Sinistral

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18
Q

If the block moves to the right

19
Q

cause vertical (normal or reverse) movement.

A

Dip slip faults

20
Q

cause lateral (dextral or sinistral) movement.

A

Strike slip faults

21
Q

There are cases wherein water rising from the ground as the ground shakes.

22
Q

Mass wasting, more commonly known as a

23
Q

These waves initially have a small height but grow as they move through shallower depths, a process called

A

Wave shoaling

24
Q

affect a wide geographical area, typically within 1,000 km or 1-3 hours of the wave travel time.

A

Regional tsunami

25
is a molten rock or magma that has reached the surface of the earth
Lava
26
occurs when magma contacts the surface of a volcano and erupts or overflows downhill from different volcanic openings.
Lava flow
27
Lava flows can be
Fluid or vicous
28
Lava with low silica content
Fluid
29
High silica content
Viscous
30
Lava flows comes in two types
Pahoehoe and Aa
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lava flow that has high fluidity creating a smooth and ropy texture when they harden. As this type of lava cools, transitions into an Aa.
Pahoehoe
32
Has a blocky and hagged texture
Aa
33
Recognizable volcano in the wolrd that produces lava flow
Kilauea volcano
34
Volcanic gases are composed of different materials depending on its location.
Water vapor (H2O) and carbon dioxide (CO2) typically make up the bulk composition of volcanic gases, followed by sulfur dioxide (SO2). Other common volcanic gases include hydrogen chloride (HCl), and hydrogen fluoride (HF).
35
are hot, dry, turbulent mass mixtures of different pyroclastic materials and gases that move downwards along the slope of a volcano at speed that can go up to several hundred meters per second
Pyroclastic flow
36
is a collective term for volcanic fragments that have been ejected out of a volcano which vary in sizes from ash to boulders.
Tephra
37
Pyroclastic flows are composed of two parts:
A basal and a turbulent
38
flow of coarse pyroclastic materials
Basal
39
ash cloud riding over the basal flow
Turbulent
40
When the turbulent ash cloud separates from the main pyroclastic flow, they are separately called the
Pyroclastic surge
41
Pyroclastic flows occur in different ways. The most notable type is called the
Soufriere type
42
This forms from the collapse of a high vertical column coming from a highly explosive eruption. When the force of gravity overcomes the momentum of the upward thrust of the eruption, the pyroclastic materials begin to fall creating a pyroclastic flow along the sides of the volcano.
Soufriere type
43
occurs when a highly viscous lava dome blocks the opening of a volcano, building pressure until it can no longer be contained and explodes to one side of the volcano without forming a high eruption column.
Pelee type
44
on the other hand, occurs when a lava dome grows too steep over a volcanic crater which then falls due to gravitational force
Merapi type