Characteristics of volcanoes formed by varying types of volcanic eruption, and associated secondary hazards

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how are shield volcanoes formed

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1

how are shield volcanoes formed

runny basaltic lava flows quickly and cools slowly so spreads out over a large area

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2

give an example of a shield volcano

mauna loa

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3

how are composite volcanoes formed

alternating eruptions of fragmented material and lava build up to form a tall volcano.

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4

how are special characteristics of composite volcanoes formed (2)

explosive eruptions can blow the top off the cone leaving a crater with a secondary cone inside, parasitic cones form due to secondary eruptions along the volcano

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5

give an example of a composite volcano

mount etna

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6

how are cinder volcanoes formed

solid material builds up in a steep conical hill around a vent. they are usually not tall

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7

give an example of a cinder volcano

inferno cone in the us

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8

silica causes lava to be more viscous. what is the main source of silica

ocean sediments

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9

what is the result of viscous vs runny lava

viscous lava produces more violent eruptions than runny lava

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10

what are the impacts of pyroclastic flows (3)

health hazard due to toxic components, damage to infrastructure as ash is heavy, damage to ecosystems

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11

what is a lahar

a mixture of ash and rain that flows in a dense, sticky mass

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12

what are the impacts of lahars (3)

can coat land making it unusable, trap people, damage infrastructure

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13

what is the difference between lahars and debris avalanches

debris avalanches contain debris and large material whilst lahars are made of finer ash

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14

What is a pyroclastic flow

a hot mixture of gas, ash, and debris blown at high speeds

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15

why does silica thicken lava

it reacts with oxygen to form a lattice structure which creates stringy chains

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16

where does basaltic lava form

constructive plate boundaries

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17

where does feltic (silica-rich) lava form

destructive plate boundaries

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