Plate Movement Flashcards
Continental shelf
The part of the continental plate that stretches beyond the continent into the ocean
Tectonics
Relating to the plates and their involvement in the earths land masses
Crust
The thinnest layer of the earths structure. There are two types: continental and oceanic.
Big Bang
The theory States that about 13.7 billion years ago all the matter in the universe was concentrated into a single incredibly tiny point. This began to enlarge rapidly in an extremely hot explosion, and is still expanding to this day.
Mantle
Molten silicates and minerals from 2900km up, at temperatures up to 3800*c.
Core
From 2900km into the earth and down, is the size of Mars, densest part of the planet, made of rocks rich in iron and nickel
Mantle
Depth: 2900 km upwards
Mainly silicate rocks
Temperature: 3800C
Core
Depth: 2900km to centre Size: size of Mars Rich in iron and nickel Made up of semi-molten outer core and solid inner core Temperature: can reach 5000C
Lithosphere
The crust and upper mantle
Asthenospere
Rest of mantle
Primary Waves
The first waves of an earthquake
Secondary Waves
The second waves of an earthquake
Suface Waves
Seismic wave
Tectonic Plates
Irregularly shaped ‘raft’ of lithosphere ‘floating’ on the asthenosphere
Oceanic crust
Mainly Sima
Less than 200 million years old
Continental crust
Mainly Sial
Over 1500 million years old
Plate margins
Where two plates either: move apart, move towards each other or move past each other
Convection currents
Heat from core generates currents in mantle, which drive the movement of tectonic plates
Continental drift
Theory states that all continents were once together, and have all slowly drited apart from each other (and still are)