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Mass Movements, Wind, Glaciers, and Surface Water

AB
mass movementthe downslope movement of loose sediments and weathered rock resulting from the force of gravity
creepthe slow, steady, downhill flow of loose, weathered Earth materials, especially soils
mudflowswiftly moving mixtures of mud and water
landslidea rapid, downslope movement of Earth materials that occurs when a relatively think block of loose soil, rock, and debris separates from the underlying bedrock
slumpwhen the mass of material in a landslide rotates and slides along a curved surface
avalanchea landslide that occurs in mountainous areas with thick accumulations of snow
deflationthe lowering of the land surface that results from the wind's removal of surface particles
abrasionwhen particles such as sand rub against the surface of rocks or other materials
ventifactrocks that are shaped by wind-blown sediments
dunea pile of wind-blown sand
loessthick, wind-blown silt deposits
glaciera large moving mass of ice
valley glaciera glacier that forms in a valley located in high mountainous areas
continental glaciera glacier that covers broad, continent-sized areas
cirquea deep depression carved out by a glacier
morainea ridge that consists of till deposited by a glacier
outwash plainan area at the leading edge of a glacier, where the meltwater streams flow and deposit outwash
drumlinelongated landform created when glaciers move over older moraines
eskerlong, winding ridges of layered sediments that are deposited by streams flowing under a melting glacier
runoffwater flowing downslope along Earth's surface
watershedall of the land area whose water drains into a stream system
dividea high land area that separates one watershed from another
solutionmaterials that are carried in a stream's water after it becomes dissolved
suspensionthe way that all particles small enough to be held up by the turbulence of a stream's moving water are moved within a stream
bedloadconsists of sand, pebbles, and cobbles that the stream's water can roll or push along the bed of the stream
dischargethe measure of the volume of stream water that flows over a particular location within a given period of time
floodoccurs when water spills over the sides of a stream's banks onto the adjacent land
floodplainthe broad, flat area that extends out from stream's bank and is covered by excess water during times of flooding
stream channela narrow pathway that moving water carves into the sediment or rock
stream bankthe ground bordering a stream on each side
meandera bend or curve in a stream channel caused by moving water
deltaa triangular deposit that forms where a stream enters a large, quiet body of water
rejuvenationwhen a stream actively resumes the process of downcutting toward its base level


G. Gier

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