plate tectonics Flashcards

1
Q

What is the earths structure

A

Core
Mantle
Crust
Lithosphere

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2
Q

What elements are in the crust

A

Silicon, oxygen, aluminium, pottasium

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3
Q

How thick is the crust below the ocean

A

6-10km

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4
Q

How thick is the crust below land

A

30-40km

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5
Q

How thick is the lithosphere

A

60-70km

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6
Q

What are the two types of crust

A

Continental and oceanic

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7
Q

Which type of crust is denser

A

Oceanic

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8
Q

What is the composition of continental crust

A

Mainly granite, silicon,aluminium and oxygen

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9
Q

What is the composition of oceanic crust

A

Basalt, silicon,magnesium and oxygen

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10
Q

How do the plates move

A

Convection currents which push and pull the plates

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11
Q

What was Alfred wegeners theory of tectonic

A

That tectonic plates have evolved from pangea, 300 million years ago

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12
Q

How is sea floor spreads evidenced

A

Examination of the oceanic crust either side of the mid Atlantic ridge (alternating polarity of magnetic rock)

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13
Q

What create thermal convection currents

A

Hot spots in the mantle

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14
Q

Biological evidence for continental drift

A

-Fossil remains of mesosaurus in Brazil and South Africa
-fossil brachiopods found in Indian limestone and Australia
-fossil remains of plant which existed when coal was being formed found in India and Antarctica (coal only forms in tropical conditions)

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15
Q

Evidence for continental drift- climatology

A

Evidence of glaciation found in South America and India

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16
Q

Evidence for continental drift- geology

A

Rocks of similar age,formation and structure found in Brazil and South Africa
Coal sandstone and limestone could not have been formed in Britain with its current climate

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17
Q

Palaeomagnetism

A

In underwater eruptions basaltic lava cools
Rock aligns with earths magnetic field
This is reversed every 400,000 years
Bands of rock facing different poles are formed

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18
Q

Constructive margins occurs where

A

Two plates move away from eachother

19
Q

What do constructive boundaries form

A

Rift valleys
Mid oceanic ridges

20
Q

Volcanic activity at constructive boundaries

A

Gentle slides
Basaltic lava
Gentle eruptions
Frequent
Effusive

21
Q

Transform faults

A

Occur at right angles to boundary as new crust is formed
Friction and earthquakes )shallow focused)

22
Q

Rift valleys

A

-form when plates move apart on continental areas
-areas of crust drop down parrallel faults
-forms an upstanding block known as a horst
-in east african rift valley it is said to be an emergent plate boundary and forming a new ocean

23
Q

Example of rift valley

A

East African rift valley
Extends for 5000km from Mozambique to the Red Sea and Jordan
Width varies from 10-50km

24
Q

Conservative plate margins occur when

A

Two plates move past eachother

25
What hazards occur at conservative margins
Earthquakes only
26
Example of conservative margin
San Andreas fault in california
27
Destructive margins occur when
Two plates move towards each other and the heavier plate sinks beneath the lighter plate
28
Example of destructive margin
Andes, west coast of South America Nazca plate subducts under South American plate Molten magma rises forming explosive volcanoes
29
What are island arcs and how are they formed
- subducting plate becomes hot -pressure and friction melts the plate -rises to the surface as a pluton of magma -composite volcano islands are formed
30
Where are fold mountains formed
-Destructive continental and continental boundaries -there is no subduction -edges and sediments are forced upwards -there is no volcanic activity -indo-australian plate travelling nirthwards into eurasian -formed the himalayas
31
How do fold mountains form
Lower density continental courts collide Plate edges forced upwards No subduction so no volcanic activity e.g. the Himalayas
32
Hotspots
Areas on the crust of volcanic activity that are not related to hazards
33
What do hot magma plumes do
Burn through weaker parts of the crust and states in the same plates as the plate moves
34
Hawaiian chain of volcanic islands facts and figures
60° bend in the shape of the islands 3,700 miles long Travelling NW Are getting eroded Up to 5 million years old
35
What does Tuzo Wilson say creates magma plumes
Static radioactive elements
36
What does Foulger 2003 suggest forms hotspots
Weakness in tectonic plates Faults in the crust allow plume of magma through
37
What is a mantle plume
A pocket of magma which has melted through the asthenosphere from the core due to static radioactivity
38
What is the most common rock type formed by the eruption of Hawaiian volcanoes
Basaltic rock (low silica and low gas content)
39
ocean ridges
longest continuois uplifted features when plates move apart in oceanic areas space is filled with basaltic lava, cools and forms magnetic rock volcanic acitivity - submarine volcanoes
40
deep sea trenches
where oceanic and continental plates move denser plate subducts nazca under south american formed peru-chile trench
41
island arcs
during subduction the descending plate enters hotter surroundings generated by frcition begins to melt the plate material is less dense and rise towards surface as plutons of magma eventually reach surface and form compositive explosive volcanoes
42
Sea floor spreading theory
After discovery of mid Atlantic ridge Altenratating polarity of the rocks - iron/magnetic particles in erupted lava Poles reverse every 400,000 years Results in magnetic stripes that are aligned to the poles Oceanic crust gets older with the distance from the ridge
43
Ridge push / gravitational sliding
Constructive boundaries Upwelling of hot material at ocean ridges - creates buoyancy effect Plates experience force that acts away from the ridge Gravity acting down the slope of the ridge
44
Slab pull
Destructive boundaries Downward gravitational force on the cold dense decending plate Pills the whole oceanic plate down as a result of negative buoyancy Frictional resistance - gives rise to shallow and deep earthquakes