Tectonics Flashcards

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1
Q

The crust

A

Added to by sedimentation and dead sea creatures. As no metals are involved it is able to ‘float’ on the mantle.

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2
Q

Why is the core metal?

A

As the Earth cooled, denser materials like iron and nickel sank. It’s kept solid by the pressure of all the layers.

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3
Q

Description of constructive margin

A

-Core heats magma, rises to asthenosphere
-Cannot break through so moves parallel
-Plates are dragged apart
-Ridge push as plates are pushed up in the middle and their weight pushes them apart
-Slab pull where the other end of the plate is on a destructive margin
-Mid Atlantic ridge

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4
Q

Paleomagnetism

A

Study of magnetic rock to record history of the magnetic field

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5
Q

Continental drift (pangea) and evidence for

A

Alfred Wegner 1915
-Jigsaw fit
-Geology that seems to be the same across continents
-Fossil evidence

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6
Q

Crust characteristics

A

400 C
Less dense
Granite & basalt
Solid

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7
Q

Mantle characteristics

A

870 C
Less to medium density
Upper=olivine Lower=magnesium silicate
Liquid & solid

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8
Q

Outer core characteristics

A

4400-6100 C
Dense
Iron & sulphur
Liquid

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9
Q

Inner core

A

7000 C
Very dense
Iron & Nickel
Solid

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10
Q

Effusive

A

Runny

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11
Q

Description of destructive margin

A

-Oceanic plate is subducted (slab pull)
-Fold mountains, as plate concertinas
-Melted rock & gas in subduction zone
-Great pressure so magma rises to make volcanoes, these are explosive
-Many shallow and deep EQs with benioff zone going deep
-Nazca and SA plates

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12
Q

Description of continental collision margin

A

-Neither subducts so no volcanoes
-Crumple upwards to make fold mountains
-EQs mainly on boundary and are very violent, also intra-plate as plates deform
-The Alps (African and Eurasian)

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13
Q

Description of transform margin

A

-Plates move parallel
-No subduction so no volcanoes
-Many shallow EQs
-Elastic rebound
-San Andreas Fault

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14
Q

Elastic rebound

A

Plates get stuck at the margin so start to bend. Snap back to original shape in new locations.

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15
Q

Formation of island chains

A

-Hotspot in oceanic plate
-Outpouring of basalt makes land
-Plate moves so creates island in new spot
-Hawaii

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16
Q

Causes of intra-plate EQs

A

-Old weaknesses from previous collisions
-Climate change causing isostatic rebound
(New Madrid fault line)
-Rising sea levels adding weight to crust

17
Q

Viscosity

A

Low=runny High=thick
More silica = Higher viscosity

18
Q

Basaltic lava

A

Low viscosity
Where lava is heated by core and low in gas
Low magnitude eruptions
Constructive margins

19
Q

Effusive

A

Lava runs down the volcano

20
Q

Rhyolitic lava

A

High viscosity
Where subduction adds silica, gas and water to the magma
Magma has difficulty making it to the surface but creates very explosive eruptions when it does
Ash clouds, pyroclastic flows, volcanic bombs and lahars
Destrucive margins

21
Q

Earthquakes

A

Focus- Origin point
Epicentre- Point on surface above focus
Seismic waves- Transmit energy from eq

22
Q

EQ wave types

A

P - Compression, less damaging, fastest
S - Vertical amplitude, slower
L - Side to side, most damaging, at surface

23
Q

Liquefaction

A

Water saturated material becomes loose and water surrounds all grains.
Christchurch, New Zealand

24
Q

Primary impacts of a volcano

A

Lava flow
Pyroclastic flow
Gas eruptions
Ash cloud

25
Q

Secondary impacts of a volcano

A

Lahars
Landslides
Jokulhlaup
Acid rain

26
Q

Pyroclastic flow

A

Formed from collapse of eruption column; lava dome or lava flow. Fluidized by water vapour and gases. Montserrat 1997

27
Q

Lahar

A

A slurry of mud, water and volcanic debris, formed when a pyroclastic flow melts snow/ice or there is heavy rainfall.