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Inside Earth

AB
FaultA break in Earth's crust where rocks have slipped past each other
GraniteContinental crust mainly consist of granite
Alfred WegnerFirst propose the theory of continental drift
Wegner's theory was rejected becauseit couldn't explain what force pushes or pulls continents
SubductionThe process by which oceanic crust sinks beneath trenches
PlatesSection of Earth's lithosphere is broken into separate pieces that slowly moves over the asthenosphere
Geologistsscientists who study the forces that make and shape planet Earth
RadiationTransfer of energy through space
ConductionTransfer of heat within a material or between materials that are touching
ConvectionTransfer of heat by movement of a fluid
ConvectionCooler, denser fluids sink to the bottom
Mid-ocean ridgeUndersea mountain chain where new floor is produced
What erupts from a mid-ocean ridgemolten material comes up
Asthenospheresoft layer of mantel that the lithosphere floats on, can bend like plastic
LithosphereRigid layer made up of the uppermost part of the mantle and crust
Sea-flooring spreadingprocess that continually adds new material to the ocean floor
Continental driftHypothesis that continents slowly moved across Earth's surface
Transform plate/boundaryTwo plates slip or slide past one anothe
Convergent plate/boundaryTwo plates come together, collide-one goes on top of the other
Divergent plate/boundaryTo plates divide, move apart from one another
StressForce that acts on rock to change its shape or volume *tension
P wavesSeismic waves that arrive first, primary waves, compress and expand the ground like an accordian
AnticlinesFold in rock that bends upward to form an inch
SynclinesFold in rock that bends downward to form a valley
FocusPoint beneath Earth's surface where the crust breaks and triggers an earthquake
TensionType of stress that pulls on the crust and stretches rock
SeismographAn instrument used to measure and record ground movements during an earthquake
LiquefactionProcess that occurs when an earthquake's shaking turns loose soil into mud
Normal FaultFault is at an angle - the hanging wall slips downward
Strike-slip faultrocks slip past each other side-ways with little up or down motion
Reverse faultSame structure as a normal fault, but hanging wall moves upward past the footwall
ShearingStress that pushes rock in two opposite directions, causes strike-slip faults
CompressionStress force that squeezes rock until it folds/breaks
PlateauLarge flat area of land that is elevated high above sea level
Moment magnitude scalerating system that estimates the total energy released by an earthquake
EpicenterPoint on Earth's surface directly above an earthquake's focus
TsunamisWater displaced by an undersea earthquake
Hot spotArea where magma melts through the crust in the middle of a plate
Magma chambermagma collects in a pocket inside a volcano
Physical properties of magma from explosive eruptionsthick, sticky, high viscosity, high in silica
Volcanic soils containpotassium and phosphorus
Lava plateauLayers of thin, runny lava that flows over a wide area before they cool and harden
Stages of volcano activityDormant - sleeping Extinct - dead, unlikely to erupt again Active - one that is erupting or showing signs it will erupt again
MagmaMolten mixture of rock - forming substances, gases and water deep in Earth's mantle
Ring of fireBelt of volcanoes around the rim of the Pacific Ocean
SilicaCompound that is made up of the particles oxygen and silicon, is one of the most abundant materials in Earth's crust, more silica = thicker magma
Volcanic neckForms when magma harden in a volcano's pipe and is later exposed


6th Grade

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