C1 7 Our Changing Planet Flashcards

1
Q

Label the structure of the Earth.

A

From inside to out:

  • Inner core
  • Outer core
  • Mantle
  • Crust
  • Atmosphere
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2
Q

What are the characteristics of the atmosphere?

A
  • 80% of air lies within 10km of the surface
  • Most of the rest is within 100km but not accurate
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3
Q

What are the characteristics of the crust?

A
  • Average thickness is 6km under oceans
  • 35km under continental areas
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4
Q

What are the characteristics of the mantle?

A
  • Starts at crust
  • Can go up to about 3000km below the surface
  • Behaves like solid
  • Can flow very slowly
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5
Q

What are the characteristics of the core?

A
  • Radius of about 3500km
  • Inner core is made of iron and nickel, solid
  • Outer core is liquid
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6
Q

Where do all the minerals and other resources come from?

A

Crust

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7
Q

How have scientists identified the Earth’s crust?

A

Through earthquakes, the directions the seismic waves travel due to refraction. The different densities differ the direction the waves travel.

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8
Q

Why do continents move?

A

Due to the Earth’s crust and uppermost mantle being cracked into tectonic plates.

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9
Q

What causes tectonic plates to move?

A

Radioactive decay in the core produce vast amounts of energy which heats up the molten rock in the mantle to become less dense and rise towards the surface. Cooler material snk to replace their place and create convection currents.

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10
Q

What happens at plate boundaries?

A

Plates meet eachother can either collide to form mountains, slip past each other causing earthwuskes .etc

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11
Q

Why aren’t earthquakes prevented?

A

They are hard to predict

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12
Q

What did Alfred Wegener’s theory of the Continental Drift suggest?

A

All the continents were fixed together like a jigsaw and started moving further apart.

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13
Q

Why didn’t scientists believe in his ideas?

A

He had no evidence to show how the continents moved further apart so people stayed to their theories such as the Land Bridge theory.

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14
Q

What do scientists believe about the coming of carbon dioxide, nitrogen and water vapour?

A

These were released by volcanoes. The water vapour condensed into rain and water was collected in the hollows of the crust turning into oceans.

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15
Q

What was the early atmosphere like?

A

It was mainly carbon dioxide and there could have been some water vapour with traces of methane and ammonia. There would have been very little or no oxygen. Some believe that nitrogen was also present.

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16
Q

How did oxygen arrive to the Earth?

A

Simple organisms such as bacteria broke down other chemicals to provide themselves with energy. These evolved into other organisms such as algae which used the sun’s energy to make food through photosynthesis producing oxygen as a waste product. As more and more plants evolved the levels of oxygen rised and carbon dioxide dropped.

17
Q

What was done in the Milley-Urey experiment and what did it suggest about the molecules which made up the simple organisms?

A

Theory: Life started when chemicals in a “primordial soup” combined to created molecules such as DNA and other molecules in living things.

They put water, ammonia, methane and hydrogen to replicate the earth’s atmosphere and these were given a high voltage shock replicating lightning.

This provided evidence to support the theory that molecules (amino acids) can be made from a reaction of the gases in the early atmosphere.

18
Q

What was the Murchison Meterorite and what did it suggest about the molecules which made up the simple organisms?

A

Theory: Life started because meteorites picked up organic molecules from space and landed on earth.

Chemicals which make up the body (amino acids) were found in this meteorite showing that compounds may have come from outer space.

19
Q

What was the volcanic vents in the seabed experiment and what did it suggest about the molecules which made up the simple organisms?

A

Theory: Life started near volcanic vents where the chemicals produced helped sustain bacteria.

The water coming out from the hydrothermal vent is mineral-rich and therefore new animals are being discovered.

20
Q

What are the advantages and disadvantages of each theory?

A
21
Q

What are amino acids made of?

A

Oxygen, hydrogen, carbon, nitrogen and sometimes sulphur

22
Q

What happened to the carbon dioxide from the Earth’s early atmosphere? How did it get locked up in the Earth’s crust?

A
  • It was taken up by plants during photosynthesis
  • The carbon then ended up in plant material and got eaten by animals which transferred it to their tissues
  • After they die, the fossils build up on the ocean’s sea bed creating sedimentary rock.
  • Some were crushed and heated by the crust forming fossil fuels
  • It also dissolved in ocean, it reacted and formed insoluble compounds turning into carbonate rocks.
23
Q

What happened to the ammonia and methane?

A

They reacted with oxygen and got rid of.

24
Q

What happened to the nitrogen?

A

It built up as it is unreactive

25
Q

How can gases in the atmosphere get separated by?

A

Fractional distillation

26
Q

How do the seas and oceans act as a buffer?

A

By absorbing CO2but releasing it if necessary. The insoluble carbon dioxide such as calcium carbonate gets deposited as sediments on the seabed. Whereas soluble carbon dioxide such as calcium gets dissolved. Plants and sea creatures in the oceans release the carbon dioxide.

27
Q

What problem are the oceans currently coping with?

A

Additional carbon dioxide causing coral reefs to die due to acidic conditions.

28
Q

What is a solution for excess CO2?

A

Carbon Capture and Storage

29
Q

Give a diagram of the carbon cycle.

A