Ch16 Flashcards

0
Q

Channeled movement of water along a valley bottom.

A

Stream flow

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1
Q

the unchanneled movement of surface water down a slope

A

Overland flow

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2
Q

That portion of the total terrain in which a drainage system is clearly established.

A

Valley

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3
Q

The higher land above the valley sides that separates adjacent valleys

A

Interfluve

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4
Q

An area that contributes overland flow & groundwater to a specific stream (also called a watershed or catchment) terminates at drainage divide

A

Drainage basin

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5
Q

The line of separation between runoff that descends into two different drainage basins

A

Drainage divide

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6
Q

When something is transferred to another location and set down

A

Deposition

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7
Q
  • involve running water
  • running water is earths most important external agent
  • it is ubiquitous (everywhere except Antarctica) frozen glaciers not water.
A

Impact of

FLUVIAL PROCESSES

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8
Q
  • also involves running water & FLUVIAL processes

- CHANNELED movement of watt along valley bottom. Wether tiny creek or enormous river.

A

Stream flow

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9
Q

UNCHANNELED downslope movement of water along surface water.

A

Overland flow

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10
Q

This is a drainage system of channeled (stream) flow. The portion of terrain where the drainage system is clearly established. partially or totally occupied by a channel of stream. ““Bottom and ““walls that rise above “” bottom in both sides.

A

Valley

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11
Q

No clearly established channeled flow. Higher land area between valleys. Overland flow. Higher land above valley walls that separated adjacent valleys. anything in the terrain not part of the valley is an?

A

Interfluve

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12
Q

Valley bottoms, valley sides, interfluves that drain toward the valley are the divide sub basins of

A

The drainage basin

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13
Q

Line of separation between runoff that discards in the direction of one drainage basin,

A

Drainage divides

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14
Q

the hierarchy of smaller tributary sub basins are part of the “”

A

Main stream basin.

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15
Q

1st order stream is the smallest stream, has no tributaries.
2nd order behind at the confluence of 1st order streams.
3rd order begins at the confluence of the 2nd order streams.

A

Stream orders.

Divide of main drainage basin.

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16
Q

Load
Types of load
Competence/capacity.

A

Transportation

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17
Q

Amount of loads water can carry depends on 2 things
Speed/velocity
And volume.
(And slope)

A

Load

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18
Q

When volume and speed /velocity decreases, this happens

A

Transportation deposition

19
Q

This begins when rain falls over the lithosphere

A

Erosion

20
Q
  1. Particles move downhill on slope

2. Across surface as a thin sheet

A

Splash erosion

Sheet erosion

21
Q
  1. Turbulence breaks up into tiny channels.

2. fewer larger gullies. Goes from land flow to stream flow.

A

Rills erosion

Gully erosion

22
Q

Bed load
Saltation
Traction
Dissolved (pushing)& suspended (bouncing/jumping)load.

A

Types of load

23
Q
  1. Minerals mostly salts, dissolved -load
  2. Fine particles of clay & silt carried in suspension very slow settling speed-suspended load
  3. sand/gravel & large rocks- bed load.
A

Types of loads defined

24
Q

Stream deposited sediment””. When smooth, sorted rounded particles become stratified deposits. That cause a decrease in flow speed. Usually reduced to 1.2.3.4.5.6 what are they in order?

A

ALLUVIUM.

  1. boulders.
  2. cobblers.
  3. pebbles.
  4. sand.
  5. silt.
  6. clay.
25
Q

Periods of peak stream flow, -erode upper portions of valleys -form vast flood plains in lower parts of valleys.

A

Floods

26
Q

Stream that flows w/water 12months of the year.

Streams that flow during rain, “intermittent stream” seasonal. water only in wet season.

A

Perennial

Ephemeral

27
Q

Tightly curved loops.
Abandoned channels.
“Mississippi river”
Where land is flat, like in large flood plains.

A

Meandering channels

28
Q

Erosion occurs ““of the curves.

Deposition occurs “” of the curves.

A

Outside

Inside

29
Q

Erosion takes place here because water moves faster. Outer curve also called “”

A

Outer-bank

30
Q

Inside bank, inside curve, also called “” where deposition takes place and water moves slow

A

Point bar

31
Q

When a river cuts across a “” of a meander, the river bend becomes an “” lake. And then an”” swamp and then a “ scar.

A

Neck
Oxbow
Oxbow
Meander

32
Q

A measure of the particle size a steam can transport, expressed by the diameter of the largest particle that can e moved. Depends on flow and speed.

A

Competence

33
Q

Measure of amount of solid material a stream has the potential to transport, normally expressed as volume of material passing a given time interval.

A

Capacity

34
Q

A type of stream drainage pattern that reflects the underlying geologic structure or topography. It is the most common drainage “tree like” pattern and numerous. Random merging of streams, tributaries joining larger streams irregularly but always at an angle of 90 or less. whose underlying structure does not control the pattern evolution.

A

Dendritic drainage pattern

35
Q

This team pattern develops in response to underlying structure containing alternating bands of tilted hard and soft rocks, long parallel streams cut into soft rocks and parallel stream jointed by short right angle 90 degree segments

A

Trellis drainage pattern

36
Q

Water follows digging deeper in entrenched “”

A

Meanders

37
Q

Down Cutting and V shaped heads to the upper ends of a valley, rapid speed and volume. Area.

A

Valley deepening .

38
Q

Lateral erosion by a meandering stream. Area.

A

Valley widening

39
Q

Headward erosion. (Lower end lengthens valley.) delta formation (deposition happens seaward in quiet waters) (linear)

A

Valley lengthening.

40
Q

William Davis theory of landform formation. (geomorphology cycle) “cycle of erosion” stages.

A

Youth
Maturity
Old age
Rejuvenation

41
Q

Surface is uplifted rapidly, erosion has little time till uplift is completely flat land far above sea level. What stage is this?

A
  1. Youth.
42
Q

Equilibrium condition, smooth profiles, stream meanders. Extensive drainage. System. Absence of initial surface. what stage?

A

2nd maturity

43
Q

Slopes absent. Extensive floodplains. Flat features. Landscape “peneplain” almost plain. Why stage? Entrenched Meanders.

A

3rd old age

44
Q

Raise land, interrupt cycle at any stage. Reenergize system initiates period of down cutting and cycle restarts. What stage?

A

Rejuvenation

45
Q

Flat surface is uplifted, incised by fluvial erosion into slopes and valleys then denuded till its flat surface if low elevation again.

A

Geomorphic cycle -William Davis