plate tectonics Flashcards

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1
Q

earth’s internal crust

A

crust
Mantle
Outer core
Inner core

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2
Q

Lithosphere

A

Earth’s crust and rigid upper mantle

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3
Q

Asthenosphere

A

it is in a molten state and the lower mantel and lithosphere float on top of it

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4
Q

describe the continental crust

A

Thick, averaging between 30 km and 70 km in thickness
Made up of light rocks, e.g. granite
Made from silica and alumina (SIAL)

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5
Q

MOHO line

A

the boundary between earth’s crust and the mantle

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6
Q

describe the oceanic crust

A

Thinner than the continental crust, averaging between
3 km and 10 km
Made up of heavy rocks,
e.g. basalt
Made from silica and magnesium (SIMA)

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7
Q

who came up with the idea of continental drift and when

A

Alfred Wegener 1912

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8
Q

what was the supercontinent called

A

Supercontinent Pangaea

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9
Q

what did the supercontinent split in

A

Laurasia and Gondwanaland

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10
Q

Proof of continental drift

A

Continental fit
Fossil distribution
Common rock types
Matching glacial deposits

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11
Q

when did pangaea split apart

A

200 million years ago

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12
Q

why is continental drift happening

A

The continents were fuelled by the convection currents and so they began to drift apart

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13
Q

who came up with the idea of seafloor spreading and when

A

Harry Hess 1960s

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14
Q

what is seafloor spreading

A

New rock is formed where plates were split apart

Ocean floor widens; magma rises from within the mantle and fills the opening

Magma cools; new ocean floor formed

New ocean floor is youngest at the mid-ocean ridge

Older crust moves away towards continents

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15
Q

There are three types of plate boundaries:

A

Divergent
Convergent
Transform

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16
Q

what are divergent plate boundaries also known as

A

constructive boundaries

17
Q

what are convergent plate boundaries also known as

A

destructive boundaries

18
Q

what are transform plate boundaries also known as

A

conservative/passive boundaries

19
Q

what happens at divergent plate boundaries

A

Fissure: new rock is formed
Rift valleys, volcanic islands, mid-ocean ridges created
Plates separate and move away from each other (sea-floor spreading)