C1.7 Changes in the earth and its atmosphere Flashcards
What are the only sources of minerals and resources that humans need?
- Earth’s crust
- Earth’s atmosphere
- Earth’s oceans
What does the earth consist of?
- A core made of nickel and iron (why we have magnetic poles)
- A very thin crust (5km - 50km)
- Mantle with all the properties of a solid but it can flow very slowly
What is earth’s crust and upper part of the mantle divided into?
Large pieces - tectonic plates
Why do tectonic plates move a few centimetres a year?
- Radioactive decay in the core releases heat
- This causes convection currents in the mantle
- This causes the tectonic plates of the crust to move
Explain the theory of continental drift.
- 300 million years ago, earth was one supercontinent called Pangea.
- Pangea broke into smaller chunks which moved apart to their current positions and are still drifting
How came up with the theory of continental drift?
Albert Wegner
What was Albert Wegner’s evidence for continental drift?
- Africa and South America fit together like a jigsaw
- Fossils and rock types matched on opposite sides of the world (people thought this was due to land bridges)
Explain the raisin/shrinking earth theory.
Mountain ranges were forced up by the wrinkling process of the earth as it was cooling down from the Big Bang
Give 3 reasons why Wegner’s theory was not accepted.
- He didn’t have a proper reason for the driving mechanism
- He wasn’t a “proper” geologist - he studied astrology
- He used inaccurate data in his predictions
What can happen at boundaries between tectonic plates?
- Earthquakes
- Volcanic eruptions
What has the atmosphere of earth been made up for the past 200 million years?
- 80 % nitrogen
- 20% oxygen
- Small proportions of carbon dioxide, water vapour and noble gases
Where did earth’s early atmosphere come from?
- During the first billion years there was intense volcanic activity
- This activity released gases forming earth’s early atmosphere
- Water vapour condensed to form the oceans
What was earth’s early atmosphere like?
Mostly carbon dioxide with some water vapour and traces of methane and ammonia
How did carbon dioxide from earth’s early atmosphere decrease?
- Plants evolved and absorbed carbon dioxide in photosynthesis
- Carbon dioxide was locked up in fossil fuels and sedimentary rocks as carbonates
- Carbon dioxide was dissolved in oceans
How did oxygen increase from earth’s early atmosphere?
Plants released it in photosynthesis