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54 Cards in this Set

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