Tectonic Processes And Hazards Flashcards

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1
Q

Convergent plate

A

. Denser oceanic crust is forced underneath the continental rust. This is know as slab pull
. Deep trench forms where oceanic plate is pushed under
. Composite volcanoes
. Tsunamis
. Earthquakes

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2
Q

Divergent

A

. Magma rises and seeps through the gap created as the plates move apart
. A ridge underwater
. Volcanic mountains
. Earthquakes

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3
Q

Collision

A

. Plates of similar weight collide and force upwards
. Built up of pressure suddenly releases
. Earthquakes
. Fold mountains

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4
Q

Conservative

A

. Plates rub against eachorher because they’re going at different speeds causing friction
. Release of friction causes fault lines in the ground
. Fault lines
. Earthquakes

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5
Q

Hotspots

A

. Occur in centre of plates where there is a hot mantle plume rising to surface that triggers the coast

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6
Q

Why do plates move?

A

Heat rises and falls, pulling the plated apart and making them move. This is done using convection currents

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7
Q

Tsunamis

A

. Triggered by an earthquake which occurs under an ocean
. When plate jolts, ocean above is forced upwards providing extra energy to the waves

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8
Q

Time of evidence supporting plate tectonics

A

. 1915: fossils collected by Wegener
. WW1: Found geologic features on ocean floor
. 1919: proposed concection currents exist
. 1946: ocean floor is mapped with solar technology
. 1954: first world mapf of volcanic eruptions is published
. 1960: hess and Dietz develop theory of sea floor spreading
. 1963: magnetic Rock reveals pattern of spreading away from centre of Atlantic ocean
. 1965: Wilson proposed idea that earth’s crust made of plates
. 1983: first gps made available

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9
Q

Shockwave body

A

. Two types- primary and secondary
. Travel through interior of earth’s layers
. Primary- faster but not felt
. Secondary- slower and do most damage

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10
Q

Shockwave surface

A

. Two types- love and Rayleigh
. On the surface and cause the most damage
. Love are transverse
. Rayleigh push ground forward and back
. Only found on shallow earthquakes

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11
Q

Secondary earthquake impacts

A

. Tsunamis
. Landslides
. Liquefaction
. General groun displacement

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12
Q

Volcanic explosivity

A

. Has a range from gentle fissures to explosive composite areas
. Links to energy of eruption
. Supervolcanoes are the largest
. Basaltic and andesitic
. Use of volcanic expolsivity index

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13
Q

Secondary volcano impacts

A

. Jokulhoup- flood causes by melted glacier
. Lahars- water mixed with volcanic deposits
. Most significant things involve water

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14
Q

Basaltic lava

A

. Hottest (1000-1200)
. Low gas content
. Thin and runny
. Gentle
. Location: ocean hot spots, mid ocean ridges and shield volcanoes

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15
Q

Andesitic lava

A

. Temp: 800-1000
. Gas content 3-4%
. Slow flow
. Violent eruption
. Location: composite cone volcanoes

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16
Q

Rhyolitic lava

A

. Temp: 650-800
. Gas content 4-6%
. Thick flow
. Violent eruption
. Location: super volcanoes

17
Q

Primary volcanic impacts

A

. Lava flows
. Pyroclastic flow
. Tephra and ashfall
. Gas eruption

18
Q

Secondary volcanic impact

A

. Lahars
. Jokulhoup

19
Q

How are tsunamis formed

A

. Caused by large underwater earthquakes along subduction zones
. Energy released during earthquake causes sea floor to uplift, displacing the water column above
. This displaced water forms the tsunami wave

20
Q

Difference between a disaster and hazard

A

Disaster- a hazard becomes a disaster when 10 or more people are killed and/or 100 or more people are affected

Hazard- a perceived natural/geophysical event that has the potential to threaten both life and property

21
Q

Why do people remain exposed to hazards?

A

. Unpredictability
. Lack of alternatives
. Changing levels of risk
. Russian roulette (optimistic it won’t happen to them)
. Cost vs benefit

22
Q

Define hazard vulnerability

A

The capacity of a person or group to anticipate, cope with, resist and recover from the impact of a natural hazard