Plate Tectonics (GLY 326) Practice Flashcards

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A comprehensive set of vocabulary flashcards covering the basic definitions of plate tectonics, Earth's internal layers, plate boundary types, faults, and seismic terminology.

Last updated 6:27 PM on 7/5/26
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28 Terms

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Plate tectonics (theory)

The theory that Earth's outer shell is divided into several plates that glide over the mantle, acting like a hard and rigid shell compared to the rocky inner layer above the core.

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Core

The center of the Earth, divided into a solid inner core of 1,216km1,216\,km thickness and a molten outer core of 2,270km2,270\,km thickness.

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Mantle

The layer surrounding the core with a thickness of 2,900km2,900\,km, made mostly of silicates of magnesium and iron; its uppermost section behaves like melted plastic.

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Lithosphere

The rigid outermost layer of the Earth that combines the crust and the uppermost solid mantle.

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Asthenosphere

The partially molten part of the upper mantle where the tectonic plates are able to move.

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Inner Core properties

Solid Iron and Nickel with a density of 17g/cm317\,g/cm^3 and temperatures between 4,0004,700C4,000-4,700^\circ\text{C} generated by radioactive decay.

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Outer Core properties

Molten Iron and Nickel with a density of 12g/cm312\,g/cm^3 and temperatures between 3,5004,000C3,500-4,000^\circ\text{C}.

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Oceanic crust

A thin layer (78km7-8\,km) composed of dense (mafic) iron magnesium silicate igneous rocks, such as basalt, with a density of 3.3g/cm33.3\,g/cm^3.

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Continental crust

A layer (3590km35-90\,km) composed of less dense (felsic) sodium potassium aluminium silicate rocks, such as granite, with a density of 2.67g/cm32.67\,g/cm^3.

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Faults

Planar rock fractures along which movement has occurred.

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Normal Faults

Rock fractures where the hanging wall block moves down relative to the footwall block.

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Reverse Fault

A dip-slip fault, particularly along convergent boundaries, associated with powerful earthquakes of magnitude 88 or more.

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Convergent boundary

A plate margin formed when two plates collide with each other, such as the Indo-Australian Plate colliding with the Eurasian Plate to form the Himalayas.

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Divergent boundary

A plate margin formed when plates separate from each other, leading to features like sea-floor spreading at the Mid-Atlantic Ridge.

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Transform boundary

A plate margin where plates slide alongside each other, exemplified by the San Andreas Fault in California.

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Triple junction

A point where three plates are pulling away from one another, such as the Afar Triangle where the Arabian Plate meets two others in East Africa.

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Seismicity

The worldwide or local distribution and measure of the frequency of earthquakes in space, time, and magnitude.

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Earthquake

The result of a sudden release of energy in the Earth's core that creates seismic waves, often due to movements within the crust or volcanic action.

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Richter Magnitude Scale

A scale that gives a single numerical value to quantify the amount of energy released during an earthquake.

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Modified Mercalli Intensity Scale

A scale ranging from I to XII used to measure the severity of an earthquake based on its effects on the earth's surface and humans.

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Seismograph

A sensitive pendulum instrument used to detect and record the shaking of the Earth.

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Seismogram

The output of a seismograph, which can be produced on paper or recorded digitally by computers.

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Epicenter

The point on the Earth's surface directly above the focus or hypocenter.

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Focus (Hypocenter)

The point within the earth where an earthquake rupture starts.

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Aftershock

An earthquake that occurs after a mainshock in the same region, representing the crust adjusting to the effects of the initial displacement.

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Earthquake swarms

Sequences of earthquakes striking a specific area in a short period where no single earthquake is clearly the mainshock.

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Soil liquefaction

A secondary effect of shaking where water-saturated granular material temporarily loses strength and transforms from a solid to a liquid.

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Tsunami

Long-wavelength sea waves produced by abrupt water movement, typically traveling at 600800km/h600-800\,km/h and caused by subduction earthquakes of magnitude 7.57.5 or higher.