Lesson 5 Flashcards

1
Q

Advantages of volcanoes

A

Serve as a foreign and local tourist attraction

Help improve the quality of the surrounding soil by
providing nutrients for crops.

Their geothermal component is also an excellent source
of energy and recreational facilities.

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2
Q

Disadvantages of volcanoes

A

Pose a threat on the communities surrounding the volcano

Bury adjacent communities in lahar and affect global climate

People living in areas distant from the site can also be affected by
the ash fall, poisonous gases, and lahar.

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3
Q

a vent on the earth’s surface that opens
downward to a pool of molten rock, debris, and gases. Its
formation involves the process of subduction.

A

volcano

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4
Q

takes place when two plates converge.

A

subduction

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5
Q

the place where the two plates
converge and the volcano is formed (DOST-PHILVOCS,
n.d.).

A

subduction zone

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6
Q

The thickness of the magma caused by____makes it difficult for gases to be released easily.

A

silica content

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7
Q

forms inside the steep cone and this

collects the gases.

A

magma chamber

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8
Q

When the_____accumulate, the volcano erupts because
the pressure rises within the chamber as it cannot contain
the magma.

A

gases

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9
Q

can harm people and surroundings.

A

erupts explosively, expels lava, rocks, ash, and gas

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10
Q

The occurrence of ____(4)is also possible.

A

earthquake, lahar flow, debris,

avalanche, or tsunami

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11
Q

large underground pool of magma

A

magma chamber

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12
Q

it is magma, yet this is the term once it reaches the surface

A

lava

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13
Q

bowl-shaped basin in the top of the volcano

A

crater

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14
Q

central tube which magma travels through

A

vent

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15
Q

eruptions from other vents may build up_____on the flanks

A

secondary cones

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16
Q

materials thrown out by the volcano

A

ash, steam and gas

17
Q

larger materials thrown out by the force of eruption

A

volcanic bombs

18
Q

are steep-sided and cone-shaped,
made up of layers of ash and lava
and containing sticky lava which
doesn’t flow very far.

A

composite volcanoes

19
Q

have gently sloping sides and
runny lava that covers a wide
area. Gases escape very
easily from shield volcanoes.

A

shield volcanoes

20
Q

currently erupting or is showing signs of

eruption. Have erupted within the last 600 years.

A

active

21
Q

has erupted and then entered a

long period of inactivity.

A

potentially active

22
Q

has not shown any sign of activity for a long
period of time. Has no record of volcanic eruption in the
past thousand years.

A

inactive

23
Q

volcanic eruption hazards

A
lava flow
pyroclastic flow
tephra falls
ballistic projectiles 
volcanic gas
lahar
24
Q

mass of magma that flows down the slope
of the volcano at a rate of 3 km/d (slightly high viscosity)
or 45 km/h (low viscosity).

A

lava flow

25
Q

hot dry masses of fragmented
volcanic materials that move along a slope and in contact
with ground surface at a speed greater than 60 km/h.

A

pyroclastic flow

26
Q

showers of fine to coarse-grained
volcanic materials and other airborne products of volcanic
eruption.

A

terphra falls

27
Q

rocks that are released into

the air by an erupting volcano.

A

ballistic projectiles

28
Q

one of the basic components of

magma or lava.

A

volcanic gas

29
Q

flowing mixture of volcanic debris and water.

A

lahar

30
Q

is the downward movement of soil, rocks, and

earth materials along a slope.

A

landslide

31
Q

is a slow or gradual

movement of soil

A

creep

32
Q

is the downslope flowage of

soft and unconsolidated materials.

A

slump

33
Q

is the slow
to rapid downslope movement of
unconsolidated soil and rock
details.

A

Rock and debris slide

34
Q

is the free falling
movement of massive rocks from a
cliff or steep slopes.

A

rock fall

35
Q

is the rapid flowage of

debris and other rock materials.

A

debris flow

36
Q

is the mass movement
characterized by a flowing mass of
mud along the flank of a volcano.

A

mud flow

37
Q

Geologic formations caused by exposure to water, erosion,

and ground movement.

A

sinkholes

38
Q

usually formed by erosion of bedrocks
composed of soft minerals and rocks such as salt, gypsum,
limestone, dolomite, and other materials that belong to the
evaporate or carbonate classes of rocks.

A

sinkholes

39
Q

Acid water underground and rainwater dissolve the rocks

and form underground passage for water called

A

conduits