Final Exam Flashcards
Erosion
The removal, transport, and deposition of weathered material over a very large distances, often (though not always) by water.
Fluvial erosion
Erosion resulting from streams- any channel flowing water
How do fluvial erosions begin
When water moves in thin sheets downslope (overland flow). Eventually the moving water forms channels. The hydraulic power of the channel flow scours out deeper gullies and eventually connects to the drainage system of a valley
Sinuous Stream Channels
Have gentle irregular curvature.
Very common.
As stream gradient lessens (the slope down which the stream flows flatten), the sinuosity increases
Straight Stream Channels
Are relatively rare and typically only occur over short distances.
Straight channels are typically controlled by the underlying geological structure
Braided Stream Channels
Occur in streams that carry large amounts of sediment
Braided channels consist of numerous interwoven channels
Meandering Stream Channels
Occur over flatter land with lower gradients and are characterized by tightly curving serpentine stream channels
Competence
Refers to the size of the largest object that a stream can transport
Higher competence means a stream can transport larger objects
Competence primarily depends on stream velocity, such that moving faster moving streams have higher stream competence.
Capacity
A stream is the amount of material a stream a stream can transport
Capacity depends both on stream velocity and stream volume
Stream load
The material transported by a stream
Dissolved load
Is the minerals dissolved in the moving stream water
Suspended load
The fine clay and silt particles that move along the stream via suspension and never touch the stream bed
Bedload
Is the larger sand grains and gravel that bounce along the bottom of the stream (saltation) or for larger objects, get dragged along the stream bed (traction)
Bedload moves slower than the dissolved and suspended loads above it (closer to the surface) because of friction
Valley depending
Happens in areas with steeper stream gradients when the fast moving water erodes away rock and forms v-shaped valleys- a process called Dow cutting.
The hydraulic power of the fast-moving water and abrasion from eroded material along the stream bed erode the valley and create deep canyons
Valley Widening
Happens in areas with low stream gradients (flat land), the water slows down and the stream takes on a more meandering flow.
Faster moving water along the _______ of a meander erodes _______ the bank (a cut bank) and widens the valley. Slower moving water in the _______ of a meander redúceles the streams competence and capacity and results in decomposition along a point bar.
Outside, away, inside
Delta Formation
Occurs when the stream enters a larger body of water
The flow velocity drops rapidly, which causes the stream competence and capacity to decrease and results in depositions of the stream load in a delta
How much water is stored in the oceans
97%
Water is always moving
True
Groundwater
Refers to underground water in the subsurface zone
Zone of saturation
Refers to underground water in the subsurface zone where spaces are completely filled with water
Aquifers
Where groundwater is stored
Porosity
Measure of the “empty spaces” of a material
Permeability
Is a measure of ability of material to transmit water though interconnected pores/voids
Aquicludes
Are impermeable layers in an aquifer system that prevent water from infiltrating
Confided aquifer
Surrounded by aquicludes
Take a longer time to recharge since water cannot readily percolate through the soil to the aquifer given the presence of impermeable layer.
Do not require pumps
Artesian wells
When a well opening is drilled into a confined aquifer
Cone of Depression
When humans rapidly extract water from an aquifer, the water table near the well will lower and the well may run dry. This local lowering of the water table near and overused well is called this
Land Subsidence
When humans extract water from an aquifer faster than water is recharged to the aquifer, the pores formerly filled with water will compact
Karst Landscapes
In areas where the underlying bedrock is limestone or some other water-soluble rock (Florida)
Weakly acidic rainfall dissolves carbonate (limestone) rock and results in the formation of solution cavities in the bedrock. These cavities grow in time and form an ____________ system of __________ and __________. Discharge of groundwater through ____________ occurs at the openings of the ________ to the surface.
Underground, caverns, water transport, natural springs, aquifer
As solution cavities grow in the bedrock, they can cause __________ to sink or collapse. This is how ________ form.
Overburden, sinkholes
Dissolution Sinkholes
Form when limestone under a thin layer of sandy soil dissolves near the surface and gradually leads to the development of depression in the land
Cover subsidence sinkholes
Form when the overburden is composed of a thicker layer of sand. As the solution cavities in the bedrock grow, sand from the overburden spills into into the cavity, causing a depression.