Term 3 MTR Key Terms + More Flashcards
Continental crust
25-100km thick, mostly made of granite, less dense than oceanic crust
Oceanic crust
5-10km thick, made from basalt, denser than continental crust
The crust
-50 °C to 50 °C, made from rocks and soil, 5-100km thick
The mantle
500-900 °C, consists mainly of magma, 2900km thick
The outer core
4700 °C, rich in iron and nickel and lava, 2220km thick
The inner core
5430 °C, hot solid ball of iron, 1260km thick
Pangea
A super continent where all of the land was connected 250 million years ago
Continent
One of 7 large land masses on earth
County
A small part of a country
Continental drift
Study of the movement, collision and division of continents
Boundaries / Margins
The edges of the plate
Constructive plate boundary
This is when two plates are moving apart. Next, a gap appears and molten magma fills the gap. A new crust will be formed.
Destructive-Oceanic/Continental plate boundary
When two plates are pushed together and the heavier crust gets subducted. The plate then sticks and the magma in the mantle starts to melt the crust.
Destructive-Collision plate boundary
When two plates crash into each other, and rocks get pushed up and folded.
Conservative plate boundary
This is when two plates move past each other, but one is moving faster. Pressure and tension builds up.