Revise morning of Flashcards

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1
Q

What is the core

A

consists of iron and nickel
Temperature =6,200 degreed Celsius
Inner core is soldi 1,250 km thick
Outer core is semi molten , 2,200 km thick

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2
Q

What is the mantle

A

consists of silicate rocks, rich in magnesium, making up 84%
of earths volume
2,900km thick
temperatures of 1000 degrees c near crust, 4000 degrees c
near core
Semi Molten

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3
Q

What is the crust

A

Thin outer layer of the Earth consist of
- Oceanic crust, 6-10km thick, made of basaltic rock such as
silica and magnesium created into sima
- Continental crust, 70 km thick made of granite rock made up
of silica and alumni created into sail

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4
Q

What is the lithosphere

A

The lithosphere is the rigid outer layer of the Earth consisting of the crust and soil outer most layer of the upper mantle

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5
Q

What is the asthenosphere

A

A layer between the upper and mantle and the lithosphere

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6
Q

What are the different plate margins

A

Converging/diverging plate margins
diverging/constructive plate margins
conservative plate margins

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7
Q

What is the converging plate margin

A

Where plates move towards each other, for example off the west of South America

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8
Q

What is the diverging plate margin

A

Where plates move apart from each other, for example in Iceland

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9
Q

What are conservative plate margins

A

Where plates move alongside each other in opposite directions , or the same direction at different speeds, for example the San Andreas Fault in California

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10
Q

What is slab pull

A

At many convergent plate boundaries one plate is denser than the other this plate subducts beneath the other (less dense plate) The subducting plate is colder and heavier and therefore continuous to sink pulling the rest of the plate with it

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11
Q

What is ridge push

A

Where magma rising from the core can escape through weaknesses in the earths crust creating ridges or oceanic mounds to form

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12
Q

What are the negatives of measuring volcanic activity

A

it is still not possible to accurately predict when an eruption will occur or how long it will be

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13
Q

How can scientists measure to predict for volcanic eruptions

A

Its easier and more reliable to predict volcanoes compared to earthquakes because scientists can measure changes in gas emissions, ground deformation, hydrology, temperature changes and seismic activity

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14
Q

What is the seismic gap theory

A

Overtime all parts of a fault must average the same level of movement, a large seismic gap can indicate a earthquake is imminent, however there is still no definite proven way to predict earthquakes

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15
Q

Predicting tectonic hazards

A

If predicted wrong, people may ignore warnings
if predicted correctly loss can be minimised

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16
Q

How can volcanoes be measured

A

The VEI (volcanic eruption indicator)
ranges from 1-8 with no upper limit

17
Q

Why not use VEI

A

no account of sulphur so no account for climate change
Doesnt measure mass of erupted material, may be incacurate

18
Q

Revise volcanic hazards

A
19
Q

Revise tectonic hazard mitigation

A