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Published byEileen Hoover Modified over 8 years ago
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Large, ancient landmass that was composed of all the continents joined together
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Theory that the Earth’s crust and upper mantle are broken into plates that float and move around on a plastic- like layer of the mantle
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Wegener’s hypothesis that all continents were once connected in a single, large land mass that broke apart about 200 million years ago and drifted slowly to their current positions
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Hess’s theory that new seafloor is formed when magma is forced upwards toward the surface at the mid-oceanic ridge
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Currents in Earth’s mantle that transfers heat in Earth’s interior and is the driving force for plate tectonics
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Motion of the Earth’s surface as it shifts downward relative to a datum such as sea=level
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Indicates a border
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PLATE BOUNDARIES
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Formed when two sections of Earth’s crust is colliding – coming together
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Forms where lithospheric plates are moving away from each other.
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Boundary between two lithospheric plates where the plates are sliding past each other.
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Long crack that forms between tectonic plates moving apart at plate boundaries
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Fracture that occurs when rocks change their shape by breaking can form as a result of compression, being pulled apart by shear
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Area in which one lithospheric plate slides under another, occurs at converging plate boundaries
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A chain of mountains or hills that form as continuous elevated crest for some distance
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Depression in the ground, generally defined by being deeper than they are wide.
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Plastic-like layer of the Earth on which the lithospheric plates float and move around
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Rigid layer of Earth about 100 km thick, plates moving apart at plate boundaries
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A physical map showing vertical features with a drawing such as shaded mountains
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Features of a land area caused by differences in elevation.
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A map that shows the shape and elevation of the land surface using contour lines, and shows other land features using symbols and colors
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On a map, lines that connect point of equal elevation above sea level.
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Height above average sea level
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Distance between contour lines on a topographic map
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A permanently affixed mark that establishes the exact elevation of a place; used by surveyors in measuring site elevations
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