Tectonics Pack B Flashcards

(25 cards)

1
Q

What is the global distribution of tectonic hazards?

A
  • Earthquakes are located in long, narrow belts along all types of plate boundaries
  • Volcanoes and earthquake activity occur in similar places in narrow zones of activity (e.g. Mid-Atlantic Ridge and Pacific Ring of Fire)
  • Hotspots are small areas away from plate margins with an unusually high heat flow linked to volcanic activity
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2
Q

What are the characteristics of earthquakes along different plate boundaries?

A
  • Divergent margins = shallow and related to volcanic activity
  • Oceanic crust subduction zones = frequent powerful earthquakes that might create tsunamis
  • Collision margins = shallow but powerful/hazardous if humans inhabit area
  • Some occur away from margins due to stress creating movement along old fault lines
  • Human activity like fracking can cause minor earthquakes
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3
Q

What are the statistics for earthquake and volcano distribution?

A
  • 450 of world’s volcanoes (active and dormant) and 90% of earthquakes are located in Pacific Ring of Fire
  • 80% of active volcanoes are at subduction zones
  • 75% of magma reaching the surface happens at divergent boundaries
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4
Q

What are the characteristics of volcanoes at different boundaries?

A
  • Divergent = non-violent, in the deep ocean, little hazard except where inhabited land is crossed
  • Convergent = violent, hazardous (e.g. Mt St Helens)
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5
Q

What is the hotspot theory?

A
  • There are fixed spots in the mantle where magma rises to the surface
  • Eruptions are usually not very violent but produce large quantities of lava
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6
Q

How do hotspots form?

A
  • A plume of magma rises from the asthenosphere
  • Magma pushes through the crust to form volcanoes at the surface
  • Form a chain of volcanoes as plate moves over hotspot
  • The line of volcanoes move with the plate
  • Oceanic volcanoes cool and subside as islands or sea mounts
  • Continental volcanoes become extinct
    E.g. Hawaiian Islands extending 2400km
    E.g. Yellowstone (continental)
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7
Q

What is an alternative theory to the hotspot theory?

A
  • Plates have weaknesses from former collisions or are stretched by slab oull
  • When the weak sections pass over previously subducted material, the molten rock can move to the surface
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8
Q

What physical factors does the impact of a tectonic hazard depend on?

A
  • Magnitude
  • Spatial predictability
  • Duration
  • Areal extent
  • Speed of onset
  • Frequency
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9
Q

What are the human factors that influence the impact of a tectonic hazard?

A
  • Population density
  • Level of development
  • Vulnerability of the population
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10
Q

What is a hazard profile?

A

Only looks at physical factors of a hazardous event

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11
Q

What are the uses of hazard profiles?

A
  • Understand and compare the physical characteristics and processes of the different types of tectonic hazard
  • Compare the same type of hazard in different locations and at different times
  • Valuable to decision makers who are involved in the day to day management of hazards
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12
Q

How does spatial predictability influence impact?

A
  • An area that has never had an event will experience greater impacts
  • More people and places will be unprepared
  • Accurate prediction allows for evacuation of danger zones
  • Too many inaccurate predictions mean people start to ignore warnings
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13
Q

How can earthquakes be predicted?

A
  • No characteristic pattern of change or seismic activity that indicates EQs
  • Possibilites are radon gas, water table changes, magnetic field variations and animal behaviour changes
  • Seismic gap theory suggests all parts of a fault line must move the same over a given time period so this may be useful to predict for places that have had a gap in seismic acitivity
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14
Q

How can volcanoes be predicted?

A
  • Changes in gas emissions
  • Ground deformation
  • Hydrology
  • Temperature changes
  • Seismic activity
  • Not accurate in terms on magnitude
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15
Q

How does areal extent influence impact?

A
  • The larger the area affected, the greater the potential impact
  • More people and places will be affected
  • Local -> regional = shield volcano, composite volcano, subduction zone earthquake, tsunami
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16
Q

How does frequency influence impact?

A
  • Events that occur more often are likely to create cumulative impacts
  • Reduces time to recover
  • Although, rare events have more energy
17
Q

How does magnitude influence impact?

A
  • The greater the amount of energy released, the greater the impacts
  • The most important factor
  • It is the size of the physical force of a hazard event
18
Q

What is the magnitude scale for volcanic eruptions?

A
  • VEI
  • 0 to 8 but no actual upper limit
  • 10 fold increase each time
  • Looks at volume of material in eruption, height of ash cloud, direction of eruption and observations
  • No account of material density or SO2 emissions
19
Q

What are the scales to measure earthquake magnitude?

A
  • Richter scale
  • Moment magnitude scale
  • Mercalli scale
20
Q

What is the Richter scale?

A
  • 1 to 10
  • Uses the amplitude of the largest wave recorded
  • Old
21
Q

What is the Moment Magnitude scale?

A
  • 1 to 10
  • Looks at area of fault rupture and amount of fault movement = amount go energy released
22
Q

What is the Mercalli scale?

A
  • I to XII
  • Amount of dmage caused by surface shaking
  • Descriptive scale
23
Q

How does speed of onset influence impact?

A
  • The faster the event, the greater the impact
  • Shorter warning time so places will be unprepared and will not have evacuatd
  • Looks at how quickly the peak of the hazard event arrives
  • EQs are instant so there is no warning time
24
Q

How does duration influence impact?

A
  • Longer an event lasts, the greater the impacts
  • Aftershocks and tsunamis may follow an EQ
  • Secondary hazards may follow an eruption (e.g. lahars)
25
How do hazard profiles help for recovery?
- Created after an event - Record characteristics to help planners in future - Retrofitting