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54 Cards in this Set
- Front
- Back
surface water flowing to the sea in streams and rivers
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runoff
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some water seeps into the ground of a vast, subterranean resevoir
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ground water
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water also evaporates directly from plants as they breathe in
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transpiration
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all water flowing in a channel
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stream
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any large stream fed by smaller ones
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tributaries
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steepness of a stream
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gradient
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amount of water flowing down a stream
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discharge
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refer to the shape and roughness of a stream channel
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channel characteristics
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floor of the channel
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bed
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sides of the channel
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bank
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stream is a measure of the largest particle it can carry
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competence
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the total amount of sediment a stream can carry past a past a point in a given amount of time
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capacity
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ions dissolved in water
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dissolved loads
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smaller silt and clay particles remain in the water
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suspended load
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during a flood, when stream energy is highest, the rushing water can roll boulders and cobbles along the bottom as?
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bed load
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downward erosion
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downcutting
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deepest level to which it can erode its bed
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base level
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smooth, concave profile
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graded stream
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undercuts the valley sides and widens a stream valley
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lateral erosion
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most low gradient streams flow in a series of bends
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meanders
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sediment accumulates in the slower water on the inside of the meander to form a?
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point bar
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where the stream cuts across the neck of a meander and isolates an old meander loop
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oxbow lake
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flows in many shallow, interconnecting channels
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braided stream
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in a fan-shaped mound
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alluvial fan
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sediment settles out to form a nearly flat landform
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delta
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stream feeding a delta or fan splits into many channels
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distributaries
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when rainfall is heavy or snow melt is rapid, more water flows down a stream than the channel can hold
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flood
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the stream overflows onto low-lying adjacent land
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flood plain
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wall built along the banks of a stream to prevent rising water from spilling out of the stream channel onto the flood plain
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artificial levee
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engineers have tried to solve the problem of channel sedimentation by dredging
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artificial channels
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when these ice blocks melt, they leave depressions, which then fill with water, forming?
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kettle lake
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poorly nourished
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oligotrophic
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high nutrient supply
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eutrophic
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boundary between the warm and cool layers
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thermocline
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it sinks mixing the surface and deep waters and equalizing the water temperature
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turnover
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water that seeps into the hold is a part of the vast reservoir
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ground water
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proportional volume of these open spaces
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porosity
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porosity indicates the amount of water that rock or soil can hold
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permeability
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completely wet layer of soil and bedrock above the barrier
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zone of saturation
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top of the zone of saturation
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water table
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dig below the water table into the zone of saturation
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well
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body of rock or soil that can yield economically significant quantities of water
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aquifer
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where the water table intersects the land surface and water flows or seeps onto the surface
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spring
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top of a layer of impermeable rock or clay lies above the main water table, creating a locally saturated zone
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perched water table
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inclined aquifer, such as the sandstone layer, bounded top and bottom by impermeable rock
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artesian aquifer
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forms when acidic water seeps into cracks in limestone, dissolving the rock and enlarging the cracks
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cavern
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an icicle-like dripstone, deposited from drops of water, that hang from the ceiling of a cavern
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stalacite
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a deposit of mineral matter that forms on the floor of a cavern by the action of dripping water
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stalagmite
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if a roof a cavern collapses
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sinkhole
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forms in broad regions underlain by limestone and other readily soluble rocks
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karst topograpy
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hot water naturally flows to the surface
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hot springs
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violently erupt hot water and steam
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geysers
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energy extracted from the earth's heat
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geothermal energy
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swamps, bogs, marshes, sloughs, mud flats, and flood plains
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wetlands
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