Ch. 5 Notes (Volcanoes) Flashcards

1
Q

Crater

A

steep-walled depression at the summit, generally less than 1 kilometer in diameter

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2
Q

Caldera

A

a summit depression typically greater than 1 kilometer in diameter, produced by collapse following a massive eruption

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3
Q

Vent:

A

opening connected to the magma chamber via a pipe

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4
Q

Factors determining the “violence” or explosiveness of a volcanic eruption and also These three factors control the viscosity of a given magma

A

Composition of the magma
Temperature of the magma
Dissolved gases in the magma

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5
Q

Viscosity

A

is a measure of a material’s resistance to flow (e.g., higher viscosity materials flow with greater difficulty)

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6
Q

Factors affecting viscosity

A

Temperature: hotter magmas are less viscous
Composition: silica (SiO2) content
Higher silica content = higher viscosity

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7
Q

aa Flow

A

blocky, crumbly, colder, slow doesn’t flow well, rolls overself

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8
Q

Pahoehoe flow

A

flows like a liquid, smooth, hotter, ropy

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9
Q

Lava Tubes

A

once served as conducts carrying lava from an active vent to the flow’s leading edge

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10
Q

Pillow lava

A

form on ocean floor, resemble toothpaste coming out of the tube

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11
Q

Ash and dust:

A

fine, glassy fragments

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12
Q

Pumice:

A

porous rock from “frothy” lava

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13
Q

Lapilli:

A

walnut-sized material

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14
Q

Cinders:

A

pea-sized material

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15
Q

Blocks:

A

hardened or cooled lava

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16
Q

Bombs:

A

ejected as hot lava

17
Q

3 types of volcanoes

A

Shield- slightly domed, largest, mild eruptions (ex: Mauna Loa on Hawaii)
cinder cone- built from ejected lava, small in size (ex: Paricutin in Mexico)
composite/stratovolcano- most violent, produces pyroclastic (mt. st. Helens)

18
Q

Lahar

A

volcanic mudflow

19
Q

Pyroclastic Flows

A

Associated with felsic and intermediate magma

Consist of ash, pumice, and other fragmental debris

20
Q

Volcanic Hazards

A

Climate: ash and gases can cool the climate after an eruption
Fume hazards also present.

21
Q

Convergent volcanism

A

subduction zones
dehydration melting of mantle
water from subducting plate