Foundations
Earth Structure
Plate Tectonics
Rock Formation
It's Not Just a Boulder
100

Theory Earth's land masses have been moving over time.

Continental drift


100

Earth's outermost and thinnest layer

Crust

100

Plate boundary where plates slide past each other

transform

100

When bits of land get scraped off from plate movement

shearing

100

Term for broken down pieces of rock

sediment

200

Reason Wegener's theory was at first rejected by the early scientific community.

Lack of evidence

200

Layer made of molten rock and drives plate tectonics

Mantle

200

plate boundary where plates move away from each other

divergent

200

breaking down rock with physical force

mechanical weathering

200

rock formed from pieces of rock cementing together

sedimentary

300

What eventually proved (to an extent) and improved on Wegener's ideas?

Plate Tectonics Theory

300

Innermost layer of the Earth made of solid Iron and Nickel; acts like a giant magnet

Inner Core

300

plate boundary where plates crash into each other

convergent

300

breaking down rock on a molecular level

chemical weathering

300

Rock formed from getting warped/recrystallized as a result of extreme heat and pressure

Metamorphic

400

Assumption Earth's surface developed because of random disasters.

Catastrophism

400

Second centermost layer made of molten iron and nickel

Outer core

400

When an overridden plates gets recycled into the mantle

subduction

400

Process of change in a rock

metamorphosis

400

Type of rock formed from the cooling of lava (be super specific)

extrusive igneous

500

Assumption that Earth's surface slowly developed because of routine, natural processes.

Uniformitarianism

500

Area between the crust and mantle where tectonic plate movements are observed

Lithosphere


500

Driving force of plate tectonics

convection

500

Process of broken down rock hardening into a sedimentary rock

cementation; compaction; lithification

500

Type of rock formed from the cooling of magma

Intrusive igneous

M
e
n
u