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flowing surface water contained within a channel
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rivers
larger streams
headwaters
upper portion of a river or stream where it originates.
mouth
lower part of stream where it flows into another body of water.
tribituaries
smaller streams or rivers that flow into a larger river
gradient
change in elevation/distance
velocity
speed and direction of moving water (m/s)
cross sectional area
area of stream channel occupied if the channel was sliced in half (width x avg depth)
discharge
volume of water passing a particular location within a designated time
does discharge increase or decrease downstream
increase due to tribituaries combining into the stream
physical weathering
breaks rocks without altering composition
chemical weathering
alters composition, water is important due to polarity
erosion
removes and transports sediment
deposition
when sediment settles in a new location
sediment load
material transported by a river/stream
competence
largest particle size a stream can transport
capacity
total amount of sediment a stream can transport
Do larger particles deposit first or smaller ones?
larger particles first due to energy
meander
bend or curve in river channel
cut bank
occurs on the outside of the meander (erosion)
point bar
occurs on inside of meander (deposition)

oxbow lake
sediment cuts off bend from main channel
floodplain
flat land adjacent to river that periodically floods
floods can…
redistribute minerals
widening/ narrowing stream channels
impact velocity
streams are narrow, steep, with coarse sediment
headwaters/ top of stream
downstream the channel becomes
wider, smaller sediment, near mouth
near mouth of stream there is
high discharge, low gradient, deposition
delta
when sediment accumulates faster than waves/ tides/ currents remove it, the sediment builds outwards into a fan shaped deposition called a delta