Rock Cycle
Geology
Geology P2
Geology P3
Atoms and Molecules
100

rock that forms from the weathering and erosion of other rocks (these sediments are deposited, compacted, and cemented)

Sedimentary Rock

100

the innermost layer of Earth, located beneath the mantle

Core

100

the thin, rocky outer layer of Earth, above the mantle

Crust

100

the hypothesis that the continents slowly move across Earth’s surface

Continental Drift

100

 smallest particle of an element.

Atom

200

rock that forms from other rocks as a result of intense heat, pressure, or chemical processes

Metamorphic Rock

200

the layer of rock between Earth’s crust and core

Mantle

200

 the process of moving farther apart

Divergence

200

a break in Earth’s crust where masses of rock slip past each other

Fault

200

two or more atoms that are chemically bonded.

Molecule

300

molten rock found under the Earth’s crust, containing dissolved gases and solid particles. At the Earth's surface, it is known as lava.

Magma

300

the process of moving closer together

Convergence

300

pieces of Earth’s crust and uppermost mantle (together called the lithosphere) that causes change in Earth’s surface by their movements

Tectonic Plates

300

a plate boundary where two plates move past each other in opposite directions

Transform Boundary

300

Force that holds atoms together.

Chemical Bonding

400

rock that forms when magma cools and solidifies

Igneous Rock

400

shapes, like mountains or hills that make up the Earth's surface.

Landforms

400

any remains, impressions, or traces of a living thing found in Earth of a former geologic age

Fossil

400

Type of heat transfer where fluids rise as they warm up, and sink as they cool down.

Convection Currents

400

a pure substance that cannot be broken down by chemical or physical means

Element

500

the processes that wear away, loosen, and dissolve materials of the Earth's crust, then move those small pieces somewhere else.

Weathering and Erosion
500

the name of the single landmass that broke apart 200 million years ago and gave rise to today’s continents

Pangea

500

the process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle at a convergent plate boundary

Subduction

500

the process by which ocean floors spread from crests of mid ocean ridges. As material moves away from the ridge, new material replaces it along the ridge.

Sea Floor Spreading

500

an arrangement tool of the known elements organized by properties

Periodic Table