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Science Layers of Earth Chapter 9

AB
crustthe outer most and thinnest of earth's layers
mantlethe layer of earth between the crust and the core
lithospherethe top part of the mantle and the crust above it, covers all of Earth like a thin shell, but is not a solid sheet of material
outer corenear the center part of the earth which is made of a liquid iron that is not stationary, it flows in currents that make the Earth's magnetic field
seismographan instrument to record earthquake waves
platea large section of earth's crust and upper mantle
plate boundariesedges of plates
gravityone of the reasons plates move, pulls down on the plate towards the mantle
tsunamiearthquakes under the ocean can lead to these large destructive waves
magmahot liquid rock below the surface of the earth, sometimes this hot liquid rock can forced to the surface through a weak spot in the crust.
continental crustmakes up the land of the continents and generally meets the oceanic crust 100 kilometers from a coast
oceanic crustlies beneath most ocean floors and made mostly of basalt, which is dark green or black rock
volcanoesform near colliding plate boundaries, can ooze fountains of lava and create gases such as water vapor and carbon dioxide
converging boundarywhen two faults collide
spreading plate boundarywhen two plates move away from each other
sliding plate boundarywhen two plates move past each other in different directions
earthquakecaused when two plates move or shift at a fault (crack in the Earth's crust), the plates eventually jerk into place causing movement and vibrations that people feel .
convection currentsone of the reasons plates move, the force in the mantle that pushes and pulls on the plates.


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