ESCL 2 Flashcards

1
Q

assessing risk involves

A

(1) understanding the type(s) and extent of hazard, (2) assessing exposure and vulnerability of the potentially affected area and population, including infrastructure
and things like evacuation routes, etc., and (3) determining total potential loss/ risk based on all of these factors

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2
Q

mid continental earthquakes

A

would be more devastating becuase people are not prepared and do not expect an earthquake

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3
Q

earthquake risk in illinois

A

is actually very high

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4
Q

explosive volcanoes

A

Explosive eruptions occur where cooler, more viscous magmas (such as andesite) reach the surface. Dissolved gases cannot escape as easily, so pressure may build up until gas explosions blast rock and lava fragments into the air!

Lava flows are much more thick and sticky so do not flow downhill as easily. These eruptions build up more steeply-sloping Composite volcanoes like this one in Chile.

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5
Q

effusive volcanoes

A

Effusive eruptions occur when hot, (1200oC) runny basalt magmas reach the surface. Dissolved gases escape easily as the magma erupts, forming lava that flows downhill quite easily.

Effusive eruptions build up gently-sloping Shield Volcanoes like Hawaii.

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6
Q

List of Volcanic Hazards

A

Pyroclastic Density Currents (pyroclastic flows andsurges)Lahars.Structural Collapse: Debris flow-Avalanches.Dome Collapse and the formation of pyroclastic flows and surges.Lava flows.Tephra fall and ballistic projectiles.
Volcanic gas.Tsunamis.

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7
Q

subductionzone/ convergent boundary

A

higher viscosity with more silica slow to no movement cinder cone explosive

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8
Q

viscosity

A

ease of magma flow

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9
Q

divergent

A

lower viscosity with less silica fluid movement creates composite

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10
Q

geotectonic setting

A

formation of rock in earths crust

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11
Q

cinder cones

A

pyroclastic flow bits of violently erupted material higher viscosity mono inyo craters in california

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12
Q

shield volcanos

A

lower viscosity flows like in hawaii

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13
Q

`stratovolcano/ composite volcanos

A

are a mix with a cake like layer with both magma and gas mt fuji japan are the most dangerous

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14
Q

hot spot

A

area not at boundary will have high viscosity at land and low viscosity at sea

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15
Q

high silica content

A

high viscosity more explosive style

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16
Q

volatiles

A

trapped gases and water vaport leading to explosive eruptions

17
Q

more explosive volcanoes

A

cause fissure eruption and lava fountain

18
Q

hazard

A

damage

19
Q

risk

A

people getting hurt

20
Q

ocean volcanos

A

sea floor hot spots sea floor spreading mid ocean ridges non explosive volcanos low silica content convection of earths mantle that pushes plates and exudes magma

21
Q

phreatic effects

A

steam explosion

22
Q

lahar

A

wet mudflow mass of volcanic fragments stratovolcano trait

23
Q

lateral blast

A

do not erupt at summit but on the side of volcano

24
Q

glacial volcanos

A

flood and also phreatic effects

25
Q

caldera

A

when large pool of magma melts mountain to a crater

26
Q

active dormant extinct

A

currrently erupting 10,000 years ago and due will never again

27
Q

Volcanic risk rating by scientists includes consideration of:

A

historical (oral, written, geologic) record of eruptions - size, type, etc.
evidence of prehistoric eruptions and types of eruption products
classification of volcano (current “restlessness”? i.e., earthquakes, gas emissions, ground swell/deformation, etc.)
demographics: population density, economics, potential losses (property, crops, etc.), infrastructure and vulnerability

28
Q

why do people live near volcanos

A

fertile soil - why is this associated with volcanoes?
geothermal (hot springs and energy source)
many important mineral and rock resources – pumice, sulfur, metal ores, etc.
please note that tourism is not a geologic benefit!
also consider: “creation of new land” time scale

29
Q

questions for geologic resources

A

what used where found how get how needed how useful what impacts

30
Q

volcanic explosive index

A

measures amount of eject volume