Our Changing Planet Flashcards
Describe the crust
- Between 5km and 70km thick
- Very thin layer
- Top layer of the Earth
Describe the mantle
- 3000km thick
- Almost entirely solid but parts can flow very slowly
- Goes almost halfway to the centre of the Earth
Describe the core
- About half the diameter of the Earth
- Has a high proportion of the magnetic metals iron and nickel
- Has a liquid outer part and solid inner part
Describe the atmosphere
- Surrounds the Earth
- Most of the air is within 10km of the surface
- Most of the atmosphere is within 100km of the surface
Name the layers of the Earth
- Inner core
- Outer core
- Mantle
- Crust
- Atmosphere
What are techtonic plates?
The huge slabs of rock that make up the Earth’s crust and the top part of its mantle
How and why do techtonic plates move?
- Move a few centimetres each year due to convection currents in the mantle
- These are caused by the energy released by the decay of radioactive elements heating up the mantle
- Where the plates meet, huge forces build up. Eventually, the rocks give way, changing shape or moving suddenly. This causes earthquakes, volcanoes, or montains to form
Why can scientists not predict when and where earthquakes will occur?
Because they still do not know enough about what is happening inside the earth
We do not have good enough data/models to make accurate predicitions
Describe the theory of continental drift and why there was opposition to it
- Put forward by Alfred Wegener in 1915
- Other scientists at the time did not accept his ideas, mainly because he couldn’t prove why
- They believed the Earth was shrinking as it cooled
- In the 1960s, scientists found new evidience and plate techtonics was developed
How do scientists think the Earth’s atmosphere has changed over time?
- Scientists think the Earth was formed 4.5 billion years ago
- In the 1st billion years it was covered with volcanoes which released CO2, water vapour, and nitrogen
- As the Earth cooled, most of the water vapour condensed to form oceans. This meant that the early atmosphere was mostly CO2 with some water vapour. Some scientists believe there was also some nitrogen and possible amonia + methane
- In the next 2 billion years, bacteria, algae, and plants evolved. Algae and plants used CO2 for photosynthesis and released oxygen
- As the number of plants increased, the amount of CO2 decreased and the amount of oxygen increased
Why are we not sure how life began?
There is insufficient evidence / lots of theories but no proof
What was the Miller-Urey experiment and what did it show?
- Conducted in 1952 by Miller + Urey. Based on what scientists at the time was in the early atmosphere
- Used a mixture of water, ammonia, methane, and hydrogen and a high voltage spark to simulte lighting
- After a week they found that amino acids, the building blocks for proteins, had been produced
- Showed that lighting could have triggered reaction to create amino acids which would then create proteins, and from there complex life (plants)
What are the other theories about how life on Earth developed?
- Since the 1950s, theories about what was in the early atmosphere have changed, but amino acids have never been able to be produced using a different combination of gasses to Miller and Urey
- One theory suggests that these organic molecules formed a ‘primordial soup’ and that the amino acids in this mixture of gasses combined to make proteins
- Many other theories have been proposed, but there is not enough evidence
How do scientists think life on Earth began?
- The plants that produced the oxygen in the atmosphere probably evolved from simple organisms like plakton and algae in the ancient oceans
- But we don’t know how the molecules of the simplest living things were formed
- No one knows for sure because there’s not enough evidence
Where did most of the CO2 from Earth’s early atmosphere go?
- Plants took up much of the CO2 in the Earth’s early atmosphere
- Animals ate the plants and much of the carbon ended up in plant + animal remains as sedimentary rock and fossil fuels
- Limestone was formed from the shells and skeletons of marine organisms
- Fossil fuels contain carbon and hydrogen from plants and animals
- CO2 dissolved in oceans and some probably formed insoluble carbonate compounds that were deposited on the seabed to become sedimentary rocks