Global tectonics: Earth structure Flashcards

1
Q

Why is the earth an ellipsoid in shape?

A

The centripedal pressure exerted on the North and South poles, as the earth spins on its axis has squashed its shape.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

What is the Polar and equatorial radius of the Earth?

A

Polar-6357km

Equatorial-6378km

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

What depths is the Inner Core between?

A

6371km to approx. 5000km

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

What metals is the Inner Core believed to be made from?

A

Iron and Nickel

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Why is the Inner Core believed to be solid and what evidence is there to support this?

A

solid due to the extreme pressure

P and S waves move through the core ( S waves generated by P waves), S waves only move through solids.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

What evidence to do with meteorites is there to suggest the Inner Core is made from Nickel and iron?

A

Meteorite evidence= Believed whole solar system formed same time from a nebula cloud. Nearly all material coalesced to make planets, some remained to make meteorites and asteroids. Meteorites are either iron and nickel or silicate.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

How do we use density to infer the nature of the inner core?

A

There must be a dense material at the centre of the earth because the average density of the earth is 5.5 gm/cm^3 and the average density of the surface rocks is 2.7-2.8 gm/cm^3

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

What depth is the Lehmann Boundary at?

A

5000km

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

What type of Boundary is Lehmann’s Boundary?

A

It’s a phase boundary between materials of the same composition but in different states (Outer Core and Inner Core)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

How big is the Lehmann Boundary?

A

100km

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Describe the Lehmann Boundary?

A

A phase boundary. 100km Zone where the rocks change from all liquid through to liquid-solid mix to all solid.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

What depth is the Outer Core between?

A

5000km to 2900km.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

What is the state of the outer core and how do we know this?

A

Liquid
S waves cannot pass through liquid and they do not pass through he Outer Core. P waves slow down due to the reduction in rigidity.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

How do we know that the Outer Core is made form Iron and Nickel?

A

The density graphs show the same pattern as that of the inner core and the same meteorite evidence is true

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

What is the origin of the Earth’s magnetics field?

A

The temperature difference between the outer and inner core set up convection currents in the liquid outer core. The convecting mass of molten iron generates electricity which induces magnetism.- self exciting dynamo

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

What depth is the Gutenburg Boundary at?

A

2900km

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

Why is the Gutenburg boundary very clear and distinct?

A

It is at a change of material from metallic to a stony type of material and it also changes state as it goes form liquid to solid.

18
Q

What happens to the P-wave velocity and S waves at the Gutenburg boundary?

A

P wave velocity decreases

S waves stop

19
Q

What depth is the Lower Mantle between?

A

2900km to 700km

20
Q

How do we know the lower mantle is solid?

A

S waves travel through it.

21
Q

Why does the velocity of P waves increase as they pass through the lower mantle?

A

The increasing pressure causes the rocks to become more rigid- less compressible.

22
Q

What is the lower mantle made of?

A

The same type of silicates material as the stony meteorites.

23
Q

How does perovskite form in the lower mantle?

A

The pressure is high, therefore the elements push together to form tight bonds, creating dense silicate minerals- perovskite.

24
Q

What depth is the Upper Mantle between?

A

700km to an average of 30km

25
Q

What is the main rock type of the upper mantle?

A

peridotite

26
Q

What mineral is common in the upper mantle?

A

Olivine is common, but changes to spinel when the pressure increases with depth.

27
Q

What evidence is there to show what the upper mantle is made up of?

A

Rarely lumps of rock are brought up by volcanic action. The main source is kimberlite pipes which go down as far as 250km into the upper mantle.

28
Q

What is the asthenosphere?

A

A layer within the upper mantle where there is 5% partial melting as a result of the intersection of the geothermal gradient and the melting curve of peridotite

29
Q

What is the state of the asthenosphere and what is it composed of?

A

Rheid

peridotite

30
Q

What is the depth of the lithosphere?

A

100km

31
Q

Why is the MOHO different from other discontinuities?

A

It’s not straight and its shape mirrors the surface of the earth

32
Q

What is the depth of the MOHO?

A

Varies from 5-7km under the oceans to 15-90km under the continents

33
Q

How and why can we detect the MOHO?

A

We can detect it because both P and S waves can be reflected by it. This is because there is a difference in the density of the rock above and below

34
Q

What is the thickness of the continental and oceanic crust?

A

Continental- up to 90km thick

Oceanic crust- 5-10 km thick av 7km

35
Q

What is the chemical composition of the continental and oceanic crust?

A

Continental- rich in silica and aluminium SIAL

Oceanic- iron and magnesium

36
Q

What types of rock make up the continental and oceanic crust?

A

Continental- granitic on average but a great variety of sedimentary, metamorphic and igneous
Oceanic- Basalt on average and nearly all igneous

37
Q

What is the density of the continental and oceanic crust?

A

Continental- 2.7 gm/cm^3

Oceanic- 2.9 gm/cm^3

38
Q

What is the age of Continental and Oceanic crust?

A

Continental- between 400 million years- includes the worlds oldest rocks
Oceanic- fairly new maximum of 200 million years to 0

39
Q

What is the structure of the continental and oceanic crust?

A

Continental- deformed

Oceanic- In layers

40
Q

What do we mean by remnant magnetism?

A

Recorded in rocks due to the alignment of their magnetic minerals according to the earth’s magnetic field at the time of their formation.