MODULE 4: HYDROLOGIC CYCLE: STREAMS, FLOODS, GROUNDWATER, GLACIERS & ICE SHEETS Flashcards
streams
bodies of water that flow downslope along clearly defined channels
continental divide
a topographic high point that separates adjacent drainage basins
st. lawrence seaway
continental divide that runs thru ohio
water goes to either lake erie or ohio river
watershed/drainage basin
the total are from which water flows into a stream
colorado river drainage basin
drains into gulf of california
ohio river basin
maumee river drainage basin
fort wayne to defiance to perrysburg to lake erie
stream gradient
steepness of a channel
(high gradient=steep, mountains)
(low=flat)
stream discharge
volume of water passing by a single point in the stream at any given time
area = depth x width
discharge = area x velocity
sediment load
the suspended and dissolved sediment carried by a stream
the faster the stream, the more sediment load it can carry
combined
if gradient increases along a channel - velocity of a stream increases - greater sediment load can be carried
alluvial fan
typically formed at the base of mountains where stream gradients abruptly decrease and sediment load can settle out
delta
similar to alluvial fans
occur when a stream empties into a standing body of water (lake, ocean)
straight streams
usually occur over short differences, particularly in upstream, high gradient areas and have the classic V-shaped valley
yellowstone river
meandering streams
meanders back and forth
usually develop where stream gradient is low in downstream areas where stream is emptying into another surface water body
missouri river
cut bank
outer edges of the bend - fastest along the cut banks
erosion concentrate along the outer sides of the meandering stream channel
point bar
flows slower, depositional side
where sediment is deposited
oxbow lake
abandoned meadner of a stream, was a curve on the meander, was cutoff after a flooding event
braided streams
common in glacial environments due to variable sediment load
arise when a stream’s ability to move it’s sediment load varies over time, usually occur in low gradient areas with a large and variable sediment load
floods
event in which a body of water overflows its banks - all water bodies undergo changes in water volume
stream stage
measures the water level or height of water
stream speed
velocity - from which stream discharge can be calc’d
recurrence interval (t)
n=number of years of stream discharge data
(n+1)/m
m=rank of discharge events
97.5% salt water
salt water ocean basins
2.5% freshwater
2% in glaciers
infiltration (percolation)
how water seeps through the ground
Zone of aeration (vadose/unsaturated zone)
pore spaces mostly filled with air
zone of saturation (phreatic zone)
pore spaces filled with water
water table
where the zones meet
mimics surface landscape
porosity
open/void space btwn mineral grains in sediment/rocks (measure as a percentage of void space)
permeability
ability of water to flow through pore spaces (measured as a speed or rate cm/s)
high porosity and high permeability
good spot for a well
igneous rock
low pore low perm
clay-rich
high pore low perm
quartz sandstone
high pore high perm
glacial till
low pore low perm
limestone
highly dissolvable rock - tend to be noth porous and permeable
aquifer
layer of rock or sediment that is
1. water saturated
2. porous
3. permeable
aquiclude/aquitard
unconfined does not have this, but are easily contaminated
a confining layer of impermeable rock or sediment
confined has this
spring
where water table meets land surface
recharge
replenishment of groundwater
hotspring
produced by emergence of geothermally heated groundwater
geyser
a spring characterized by intermittent discharge of water ejected turbulently and accompanied by a vapor phase (steam)