Water changing from liquid to gas (water vapor) driven by heat from
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Surface Runoff
Water flowing on land surface downhill to oceans
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precipitation
Any liquid or frozen water that forms in the atmosphere and falls back to the earth.
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longitudinal profile
plot of evaluation of river from head (source) to mouth (end)
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longitudinal profile near the headwaters
\-Gradient is steep and velocity is high
\-channel roughness is high
\-discharge is low
\-channel size is low
\-erosion
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Longitudinal profile near the mouth
\-gradient flattens (is lower)
\-channel is smoother but meanders
\-discharge is high
\-channel size is wide
\-transportation
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Gradient
Change in elevation as function of distance from head to mouth
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Near the headwaters
Where is gradient the highest?
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Near the mouth
Where is gradient the lowest?
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Excess in evaporation vs precipitation
The amount of water evaporated is the same as the excess amount of precipitation
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What balances the excesses?
The excess precipitation “runs off” into the oceans making everything level
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Watershed (drainage basin)
The area of land over which precipitation falls, it would be drained by rivers in that basin
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Continental divide
splits a continent into different drainage basins
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Discharge
volume of water passing a point per unit of time
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Discharge increases
How does the discharge of a stream change downstream?
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They compete in terms of velocity from head to mouth. Gradient decreases while discharge increases
How velocity is dependent on both discharge and gradient
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high
At the start, near the head velocity is _____ because of steep gradient
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Slows
In the middle it hits a switch off where the velocity _____.
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high
At the end, near the mouth the velocity is _____ due to high discharge
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competence
The maximum size of sediment transported
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Capacity
The maximum load of sediment transported
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floodplain
an area of low-laying ground adjacent to a river, formed mainly of river sediments and subject to flooding. Formed over time by the meandering stream
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Meander
bends or curve in river/stream, water velocities are lower on the inside and higher on the outside.
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point bar
On the inside of a meander, the low velocity and low competence cause deposition.
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Ox bow lake
On the outside of a meander, so much erosion causes the meander to break off because of high velocity and competence.
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Delta
Consists of sediment deposited at the mouth of a stream. When a stream enters standing war, the current slows, loses competence, and sediments drop out.
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Alluvial fan
Conical, fan shaped structures that build at the base of a mountain font. Sediments drop out rapidly with a change in stream gradient.
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flood
When a river/stream overflows its bank
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Natural levees
Deposits that occur along banks of rivers/streams during floods. Raised areas adjacent to the channel formed during a flood event
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X-year flood
possibility that only once in X years that amount of flood size will occur again
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2-3 year flood cycle
During what flood cycle does the river do most work of erosion and transport
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porosity
\-groundwater resides in subsurface pore spaces
\-the measurement of voids
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permeability
\-The ease of water flow due to pore interconnectedness
\-high=flow easily
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aquifer
sediment or rock that transmits water easily
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aquiclude
material that water cannot easily flow through (low permeability)
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Water table
A subsurface boundary between zone of aeration and saturation
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Zone of aeration
where voids are filled with water or air or partially filled
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Zone of saturation
Where voids are filled with water
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.00002km per hour
How fast does groundwater move?
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Confined aquifer
An aquifer beneath an aquitard, isolated from the surface and less susceptible to pollution
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unconfined aquifer
An aquifer that intersects the surface, is in contact with the atmosphere and easily contaminated
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Well
Holes excavated or drilled to obtain groundwater
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Cone of depression
a dip that happens in water line when too much groundwater is withdrawn
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Caves
\-Develop when groundwater dissolves limestone
\-grow as joints and widened by dissolution of the limestone