Plate techtonics, evidence & how it works Flashcards
What did Albert Wegener discover in 1910 and what did he call this?
In 1910 Alfred Wegener realised that the surface of the world had moved in the past.
He realised that the continents had moved and he called this “Continental Drift”.
What is the evidence for continental drift?
- Jigsaw of continents
- Geological
- Fossil Record
- Climatic
What is the Jigsaw Puzzle FitOff The Continents?
Wegner noticed that the coastlines of South America and Africa fit like the pieces of a puzzle. This was not a coincidence because it indicates that the two continents were once united and had since then drifted apart.
What is the fossil record evidence for continental drift?
Similar species of fossils were recognized between the east coast of South America and the west coast of Africa.
(For example, the fern Glossopteris which grew in a sub-polar climate was found in the rocks of Africa, Australia, India, and South America. This indicated that the landmasses were once a part of Gondwanaland).
What is the geological evidence for continental drift?
Wegener found rocks of the same type and age on both sides of the Atlantic Ocean. He thought that the rocks formed side by side. These rocks then drifted apart on separate continents.
Wegener also matched up mountain ranges across the Atlantic Ocean. The Appalachian Mountains were just like mountain ranges in eastern Greenland, Ireland, Great Britain, and Norway. Wegener concluded that they formed as a single mountain range. This mountain range broke apart as the continents split up. The mountain range separated as the continents drifted.
What is the climatic evidence for continental drift?
Coral reefs are found only in warm water. Coal swamps are also found in tropical and subtropical environments.
Wegener discovered ancient coal seams and coral reef fossils in areas that are much too cold today. Wegener thought that the continents have moved since the time of Pangaea.
What is Palaeomagnetism?
Palaeomagnetism is the study of the record of the Earth’s magnetic field in rocks, sediment, or archaeological materials.
What do certain minerals in rocks lock-in?
Certain minerals in rocks lock-in a record of the direction and intensity of the magnetic field when they form.
What information does this lock-in record provide?
This record provides information on the past behaviour of Earth’s magnetic field and the past location of tectonic plates.
Continents have moved over time but how or why could they move? How does it work?
The Earth is a giant ball of molten material floating in space.
The Earth hasn’t cooled down from when it was formed 4.6 billion years ago.
The inside of the Earth is very, very hot. It is estimated that the temperature at the centre is 4,500c (as hot as the surface of the Sun!)
Only the outer layer is cool enough to be a solid- this is the crust.
What is the outer layer of the Earth called?
the crust
When was the Earth formed?
4.5 billion years ago
What is the structure of the Earth (6 terms)?
- ALMMOI-
Asthenosphere:
Lithosphere:
Mesosphere:
Mantle:
Outer Core:
Inner Core:
What is the Asthenosphere?
The upper part of the Earth’s mantle, extending from a depth of about 75 km (46.5 mi) to about 200 km (124 mi).
The asthenosphere lies beneath the lithosphere and consists of partially molten rock.
What is the Lithosphere?
The lithosphere is the solid, outer part of the Earth.
The lithosphere includes the brittle upper portion of the mantle and the crust, the outermost layers of Earth’s structure. I
It is bounded by the atmosphere above and the asthenosphere (another part of the upper mantle) below