Chapter 16 Flashcards

(60 cards)

1
Q

hydrologic cycle

A

movement of water through Earth’s four spheres

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2
Q

inflitration

A

precipitation soaks into the ground

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3
Q

runoff

A

precipitation runs over the surface

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4
Q

transpiration

A

water absorbed by plants and later transferred to the atmosphere

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5
Q

evapotranspiration

A

as evaporation and transpiration both move water from the surface to the atmosphere

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6
Q

Runoff starts as

A

sheet flow which develops into tiny channels called rills which forms gullies which form streams

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7
Q

streams

A

any water that flows in a channel, regardless of size

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8
Q

river

A

carries a substantial amount of water and has many tributaries

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9
Q

Drainage Basin

A

stream drains an area of land

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10
Q

Divide

A

the imaginary line separating one basin from another; sometimes visible as high ridge mountain region

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11
Q

3 zones of river systems

A

Sediment production, sediment transportation, sediment deposition

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12
Q

Sediment production

A

zone of a river where more sediment is derived
Located in the headwater region of a river system
Generated by: broken bedrock, bank erosion

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13
Q

Sediment transport

A

transported in trunk streams; amount of sediment being eroded equals amount being deposited

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14
Q

Sediment deposition

A

when a river reaches a large body of water, the energy decreases and river deposits sediments; usually only fine sediments are deposited in oceans

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15
Q

laminar flow

A

water flowing in a nearly straight path

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16
Q

turbulent flow

A

water moving quickly in an erratic fashion

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17
Q

Factors affecting flow velocity

A

the slope, channel shape, roughness, discharge,

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18
Q

The slope, or gradient of a stream

A

steeper gradient has more gravitational energy to drive channel flow

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19
Q

Channel shape

A

most effective channel has a small wetted perimeter (area where the rive is in contact with the channel) compared to its cross-sectional area

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20
Q

Channel size and roughness

A

increase in channel size will increase the cross-sectional area to wetted perimeter ration thus increasing efficiency; rough channels create turbulence and decreased velocity

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21
Q

Discharge

A

volume of water flowing past a certain point in a given unit of time
when discharge increases; the width, depth, flow, and velocity increase

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22
Q

longitudinal profile

A

cross-sectional view of a stream

most have a concave shape

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23
Q

head or headwater

A

source of the stream

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24
Q

mouth

A

the downstream point where the stream empties into a larger body of water
discharge, channel size, and velocity increases towards the mouth

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25
Quarrying
involves removing large blocks from the channel bed
26
abrasion
scraping, bumping, and rubbing | erodes and polishes sediment s
27
Potholes
when fast moving, swirling sediment in eddies abrades a hole
28
Corrosion
rocks gradually dissolving in flowing water can occur in limestone bedrock channels
29
Transport of sediment by streams
``` Dissolved load (in solution) Suspended load (in suspension) Bed load (rolling along the bottom) ```
30
Dissolved load
most of the dissolved load is brought to a stream via groundwater NOT affect by stream velocity
31
Suspended load
largest part of a stream is carried in suspension amount carried is controlled by stream velocity and settling velocity (speed at which a particle falls through a liquid) of sediments
32
Bed load
Coarse sands, gravel, and boulders move along the stream bed by saltation (skipping or jumping) Less rapid and more localized than transport via suspended load
33
Capacity
maximum load of solid particles a stream can carry | The greater the discharge the greater the capacity
34
Competence
the maximum particle size a stream can transport | Streams with a faster velocity have a higher competence
35
deposition of sediments by a stream
occurs when a stream's velocity is less than the settling velocity
36
sorting
particles of the same size are deposited at the same time in this process Larger particles are settled out first
37
alluvium
sediments deposited by streams
38
Bedrock Channels
cut into the underlying strata
39
meanders
streams transport suspended sediment in broad sweeping bends
40
Cutbank
outside of a meander | zone of active erosion
41
point bar
inside of a meander | zone of deposition
42
cutoff oxbow lake
a meander that has been cut off from joined bends
43
braided channel
is a network of converging and diverging channels that thread among numerous islands or gravel bars
44
stream valley
channel and surrounding terrain that directs water to the stream alluvial channels have wide valley floors bedrock channels have V-shapped valleys
45
base level
lowest point to which a stream can erode
46
Ultimate base level
sea level
47
Local or temporary base level
includes lakes, resistant layers of rock, and large rivers
48
changing conditions causes readjustment of stream activities
raising base level= deposition | lowering base level= erosion
49
graded stream
only transports sediment
50
Deltas
when sediment-filled streams enter a large body of water
51
water gap
notch where a river cuts through a ridge that lies in its path
52
Antecedent stream
stream existed before the ridge was formed
53
Superposed stream
Stream eroded into a preexisting structure
54
headward erosion
stream that lengthen its coarse by extending the head of the valley upslope ; can result in stream piracy where the diversion of the drainage of one stream into another
55
flood
occurs when the stream exceeds the capacity of its channel; most common and most destructive geological hazard
56
Regional flood
seasonal flood that typically result from spring rains or rapid melting of snow
57
Flash floods
occur with little or no warning in mountainous areas
58
Ice-jam floods
ice forms in rivers creating dams that will break when temperatures rise
59
Dam-Failure floods
Dams fail and release large amounts of water
60
Flood Control
Artificial levees Channelization flood control dams non-structural approach