1b.1 DM - Constructive Boundaries and Shield Volcanoes Flashcards

1
Q

How do we work out the type of volcano?

A

By its cross section

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2
Q

What’s the thickest layer of the Earth’s cross section?

A

Core

Outer core

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3
Q

What’s the densest layer of the Earth’s cross section?

A

Core

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4
Q

What is the core made out of?

A

Iron / Nickel

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5
Q

What’s the temperature at the Earth’s core?

A

4000-5000oc

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6
Q

What’s the ‘nature’ / ‘material’ of the mantle? (What’s it made up of?)

A

Peridotite

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7
Q

Where’s the athenosphere?

A

Top layer of the mantle

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8
Q

What’s the temperature of the mantle?

A

Ranges from 1000-4000oc

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9
Q

Where are convection currents generated?

A

Mantle

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10
Q

What’s the temperature of the Earth’s crust?

A

Ranges from air temperature to 900oc

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11
Q

What’s the least dense layer of Earth’s cross section?

A

Crust

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12
Q

What type of volcanoes occur on constructive plate boundaries?

A

Shield

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13
Q

How do volcanoes occur on constructive plate boundaries?

A

Convection currents cause the plates to move apart

Basaltic (low viscosity / runny) lava is erupted from the fissure

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14
Q

What type of lava do you get at a constructive plate boundary / shield volcano

A

Basaltic
Low viscosity / runny
It runs a long distance before it solidifies

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15
Q

What shape are shield volcanoes?

A

Wide
Short
(Like a shield)

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16
Q

What happens at constructive plate boundaries?

A

Plate move apart (diverge)

Magma/lava erupts from the resulting fissure

17
Q

Why do plates move?

A

Convection currents cause hot upflowing rock
These weakens the lithosphere
The crust spreads / splits

18
Q

How do convection currents form?

A

Scientists don’t know for sure.
They think: radioactive isotopes in the core breakdown
This creates heat
Heat initiates the movement of magma in the mantle
The mantle circulates in huge conection currents

19
Q

What are the three main layers of the Earth’s structure?

A

Core
Asthenosphere, at the top of the mantle
Lithosphere - with the crust at the top

20
Q

How do volcanoes happen at constructive plate boundaries

A

Convection currents drag plates in opposite direction
Plates pull apart
Hot magma rises from the mantle
The lava is basaltic - thin and runny
It runs a long way before cooling and solidifying