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Fracture
A break in a rock where there is no movement.
Cleavage
The tendency of a mineral to break along flat surfaces.
Streak
The color of a mineral in powdered form.
Fine grained
Rocks that have small crystals and are difficult to see.
Coarse grained
Rocks that have large crystals that are easily visible.
Sedimentary rocks
Rocks formed from the accumulation and cementation of mineral and organic particles.
Asthenosphere
The semi-fluid layer of the mantle beneath the lithosphere.
Divergent boundary
A tectonic plate boundary where two plates move away from each other.
Convergent boundary
A tectonic plate boundary where two plates move toward each other.
Seismic waves
Waves of energy that travel through the Earth as a result of an earthquake.
Rock
A solid material composed of one or more minerals.
Mineral
A naturally occurring inorganic solid with a definite chemical composition.
Body waves
Seismic waves that travel through the interior of the Earth.
Sial
The layer of the Earth's crust that is rich in silicon and aluminum.
Sima
The layer of the Earth's crust that is rich in silicon and magnesium.
Isostasy
The equilibrium between continental crust and the denser mantle below it.
Seismograph
An instrument that measures and records details of earthquakes.
Anticline
A type of fold that is arch-like and has its oldest rocks at the core.
Plastic strain
Deformation that results in permanent change in shape.
Focus
The actual place where seismic waves originate in an earthquake.
S-wave shadow zone
The area on the Earth's surface where S-waves do not arrive.
Richter scale
A scale used to measure the magnitude of earthquakes.
Silicon and oxygen
The elements that make up 92% of Earth's crust.
Oceanic plate and continental plate converge
An oceanic plate subducts beneath a continental plate.
Himalayan Mountains and Appalachian Mountain
Formed by the collision of tectonic plates.
Sea-floor spreading
The process by which new oceanic crust is created at mid-ocean ridges.
Continental crust
The layer of the Earth's crust that forms the continents.
Oldest rocks
Found in the continental crust.
Chains of mountains
The ocean contains chains of mountains called mid-ocean ridges.
Mid-Atlantic Ridge
A long valley that runs along the crest of the Mid-Atlantic Ridge.
Earth's crust is made of rigid plates
The theory of plate tectonics.
Columbia Plateau
Made of many layers of basalt from volcanic activity.
Rocky Mountains
Formed primarily by compressional stresses.
Sierra Nevada
A classic example of fault-block mountains.
Tensional stress
Likely to result in normal faults, rifting, and thinning of the crust.
Hanging wall slips downward
Describes a normal fault.