Tectonics EQ1 Flashcards

(39 cards)

1
Q

Where do most earthquakes occur?

A

At plate boundaries

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2
Q

What type of plate boundaries usually lead to the most powerful earthquakes?

A

Convergent & Conservative

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3
Q

What percentage of earthquakes occur at plate boundaries?

A

95%

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4
Q

Where are active volcanoes most usually found?

A

At or near plate boundaries, in particular the Ring of Fire (75%)

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5
Q

What percentage of all earthquakes are found in the Ring of Fire?

A

70%

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6
Q

Why can intra-plate earthquakes occur?

A

Usually due to hotspots or old fault lines

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7
Q

What did Alfred Wegener propose?

A

The theory of continental drift where the continents were once joined together but have gradually moved over time

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8
Q

What are some evidence of continental movement?

A

Basalt lava flows where continents tear apart
Coal in Antarctica
Fossils of Mesosaurus
Fossils of Glossopteris
Outlines of continents piece together

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9
Q

What is the plate tectonic theory?

A

The Earth consists of plates which have a section of lithosphere, that move slowly over the lower mantle due to convection- this leads to crust being created, destroyed, torn or thrust up

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10
Q

Is the oceanic crust or the continental crust thicker?

A

Continental. (70km), whilst oceanic is 6km thick

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11
Q

Is the ocean crust or the continental crust more dense?

A

Oceanic. Continental crust has 60% silica content, making it less dense than oceanic which has basic composition (similar to basaltic lava)

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12
Q

What is the Mohorovicic Discontinuoty?

A

The division between the upper mantle and lower mantle, due to differences in seismic wave speed

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13
Q

What is the Benioff Zone?

A

An area of seismicity corresponding with the slab being thrust downwards in a subduction zone (area in which earthquakes occur)

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14
Q

What is the hypocentre?

A

The ‘focus’ point within the ground where the strain energy of the earthquake stored in the rock is first releases

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15
Q

Focal length

A

The distance between the hypocentre and epicentre

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16
Q

Epicentre

A

The point of the ground directly above the hypocentre

17
Q

Seismic waves

A

Waves that transmit the energy released by an earthquake (either primary, secondary or love waves)

18
Q

Liquefaction

A

The process by which water-saturated material can temporarily lose normal strength and behave like a liquid under the pressure of strong shaking

19
Q

Convection currents

A

Heat produced by the decay of radioactive elements in the Earth’s core heats the lower mantle causing upwards movement, creating convection currents (which are thought to move in circles)

20
Q

Paleomagnetism

A

The alternating polarisation of our magnetic field (evidence of sea floor spreading)

21
Q

What is sea floor spreading?

A

Hot magma is forced up the asthenosphere, before hardening and forming new oceanic crust, which pushes the plates apart (forming mid-ocean ridges/underwater mountain ranges_

22
Q

What is subduction?

A

As two oceanic plates (or continental+oceanic) move towards each other, one slides under the other (due to differences in density) into the mantle before melting in the subduction zone

23
Q

What is slab pull?

A

The density of the plate and gravity causes a plate to be pulled down into the mantle

24
Q

What is ridge push?

A

Newly formed oceanic crust at mid ocean ridges becomes denser and thicker as it cools, causing the lithosphere to slope away from the ridge and gravity to pull it down

25
What are the three ways volcanoes can be formed?
Convergent plate margins- composite cone volcanoes Divergent plate margins- rift volcanoes Hotspots
26
What are hotspots?
Areas in the mantle that form where radioactive decay is concentrated, from which heat rises as a hot thermal plume from deep in Earth
27
How are volcanic arc islands eg. Hawaii formed?
Hotspot volcanism, as magma plumes stay stationary, the lithosphere continues to move, creating a series of islands
28
Characteristics of effusive volcanoes
-High temperature -Low viscosity -High dissolved gas content -Low silica, basic magma -More likely at divergent margins
29
Characteristics of explosive volcanoes
-Low temperature -High viscosity -Low dissolved gas content -High silica, acidic magma -More likely at a subduction zone
30
How do volcanoes vary? (5 ways)
1) Viscosity (determined by temp+ dissolved gases) 2) Plate margins 3) Explosiveness of eruption 4) Materials ejected (lava/ash/lahars?) 5) Proximity of population centres
31
How do earthquakes occur?
1) Gradual build up of tectonic strain, storing elastic energy in the crust 2) When the pressure > strength of the fault, the rock fractures 3) Sudden release of energy (seismic waves) 4) Brittle brust rebounds on either side of the fracture (ground shaking)
32
P-Waves
Primary waves -fastest and first to reach surface -travel through solids and liquids -compressional waves (backwards + forwards motion)
33
S-Waves
Secondary waves -only travel through solids -move with sideways motion (right angles to travel direction) -more damaging than P waves but slower
34
L-Waves
Surface Love Waves -causes the most damage through crustal fracturing -shakes ground from side to side -slowest
35
What are impacts of liquefaction?
Causes the ground to sink and buildings to collapse
36
What is the difference between an ocean wave and tsunami wave?
Ocean waves are caused by the wind on the surface of the sea, tsunamis are caused by a large volume of water being displaced eg. volcanoes/earthquakes
37
How does a tsunami form?
1) An earthquake/volcano causes the displacement of the water column, causing waves to radiate in all directions 2) As the water becomes shallower, waves slow down and increase in height, which causes the wave energy to be concentrated in a smaller volume of water 3) The tsunami breaks onto the shore
38
What physical factors affect a tsunami?
-Magnitude of eruption/earthquake -Topography of ocean -Relief of the land -Speed of onset -Duration -Coastal ecosystem buffer -Distance travelled
39
What human factors affect a tsunami?
-Quality warning systems -Education of people (preparedness) -Population density -Degree of coastal development eg. coastal defences