C1 7 Our Changing Planet Flashcards
Label the structure of the Earth.
From inside to out:
- Inner core
- Outer core
- Mantle
- Crust
- Atmosphere
What are the characteristics of the atmosphere?
- 80% of air lies within 10km of the surface
- Most of the rest is within 100km but not accurate
What are the characteristics of the crust?
- Average thickness is 6km under oceans
- 35km under continental areas
What are the characteristics of the mantle?
- Starts at crust
- Can go up to about 3000km below the surface
- Behaves like solid
- Can flow very slowly
What are the characteristics of the core?
- Radius of about 3500km
- Inner core is made of iron and nickel, solid
- Outer core is liquid
Where do all the minerals and other resources come from?
Crust
How have scientists identified the Earth’s crust?
Through earthquakes, the directions the seismic waves travel due to refraction. The different densities differ the direction the waves travel.
Why do continents move?
Due to the Earth’s crust and uppermost mantle being cracked into tectonic plates.
What causes tectonic plates to move?
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.
What happens at plate boundaries?
Plates meet eachother can either collide to form mountains, slip past each other causing earthwuskes .etc
Why aren’t earthquakes prevented?
They are hard to predict
What did Alfred Wegener’s theory of the Continental Drift suggest?
All the continents were fixed together like a jigsaw and started moving further apart.
Why didn’t scientists believe in his ideas?
He had no evidence to show how the continents moved further apart so people stayed to their theories such as the Land Bridge theory.
What do scientists believe about the coming of carbon dioxide, nitrogen and water vapour?
These were released by volcanoes. The water vapour condensed into rain and water was collected in the hollows of the crust turning into oceans.
What was the early atmosphere like?
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.