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Chapter Four - Plate Tectonics

AB
anticlinea bowl-shaped fold in sedimentary rock layers
asthenospherethe soft layer of the mantle on which pieces of the lithosphere move
compressionthe type of stress that occurs when an object is squeezed
continental driftthe theory that continents can drift apart from one another and have done so in the past
convergent boundarythe boundary between two colliding tectonic plates
divergent boundarythe boundary between two tectonic plates taht are moving away from each other
faulta break in the Earth's crust which blocks of the crust slide releative to one another due to tectonic forces
fault-block mountaina mountain that forms when faulting causes large blocks of the Earth's crust to drop down relative to other blocks
folded mountaina mountain that forms when rock layers are squeezed together and pushed updward
foldingthe bending of rock layers due to stress in the Earth's crust
footwallthe fault block that is below a fault
hanging wallthe fault block that is above a fault
inner corethe solid, dense center of the Earth
lithospherethe outermost, rigid layer of the Earth that consists of the crust and the rigid upper part of the mantle
magnetic reversalthe process by which the Earth's north and south magnetic poles periodically change places
mantlethe layer of the Earth between the crust and the core
mesopherethe middle shpere, the strong lower part of the mantle between the asthenosphere and the outer core
mid-ocean ridgea long mountain chain that forms on the ocean floor where tectonic plates pull aprt, usually extends along the center of the ocean basins
monoclinea fold in sedimentary rock layers in which the layers are horizontal
normal faulta fault in which the hanging wall moves down relative to the footwall
outer corethe liquid layer of the Earth's core that lies beneath the mantle and surrounds the inner core
plate tectonicsthe theory that the Earth's lithosphere is divided into tectonic plates that move around on top of the asthenosphere


Granby, CT

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