1.2a drift theory Flashcards
What is Plate Tectonics
Refers to a set of concepts and theories explaining formation and distribution of Earth’s major structural features, seismic and volcanic events
What Helps to Explain Plate Tectonics
- Continental drift
- Sea-floor spreading
- Paleo-magnetism
- Convection currents and other
movement processes
Earth’s Structure
Crust
Lithosphere
Asthenosphere
Mantle
Outer Core
Inner Core
Crust Structure and Composition
approx.0-100km thick
200-400*C
Lithosphere Structure and Composition
Part of crust and uppermost solid mantle
Asthenosphere Structure and Composition
Part of lower crust and upper liquid plastic mantle
Mantle Structure and Composition
Made from silicon and oxygen
approx.3,000km
1000-5000*C
Outer Core Structure and Composition
Liquid iron and nickel
approx.5,000km
4000-6000*C
Inner Core Structure and Composition
Solid iron and nickel
approx.6000km
6000C-7000C
Continental Drift Theory Origins
Alfred Wegener: German geophysicist.
1912 published ‘The Origin of Continents andOceans’, which outlined his theory ofContinental Drift.
Approximately 300million years ago single continent existed which he named Pangaea.
Continental Drift Theory Evidence
- Geological evidence
Appalachian mountains in north-east USA geologically related to Caledonian mountains of north-west Scotland - Biological evidence
remains of the reptile Mesosaurus being found in southern Africa and South America – It would not have evolved identically in two different locations
Problem with Continental Drift Theory
Does explain how continents drift
Sea Floor Spreading Theory Evidence
Studied age of rocks on Atlantic seabed finding youngest in the middle of ocean in Iceland and oldest nearest USA and Europe.
Evidence Atlantic sea floor was spreading outwards from centre at approximately 5cm a year.
Sea Floor Spreading Theory Origins
1962,
Harry Hess, US geologist, outlined theory that could explain how continents could drift. This theory later became known as ‘Sea Floor Spreading’.
What is Palaeomagnetism
study of the history of changes in Earth’s magnetic field (polarity).
Every 400,000 years or so the Earth’s magnetic field switches polarity causing magnetic north and south poles to switch.