FLOOD Flashcards

1
Q

Described as the volume of water moving
through a channel over a given time interval,
commonly measured in units such as cubic
feet per second (ft 3 /s)

A

Stream Discharge

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2
Q

to drain water off the landscape and to transport sediment

A

role of streams

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3
Q

a process where water flows through
stream channels

A

Runoff

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4
Q

precipitation reaching the land
surface moves downslope in thin sheets

A

Overland Flow

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5
Q

discharge of
groundwater into the surface environment

A

Groundwater baseflow

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6
Q

provide information about a
river or stream by simply plotting the discharge versus
time

A

Stream hydrographs

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7
Q

are a result of less deep infiltration in
arid areas resulting in a water table that is below the
level of most stream channels

A

Losing streams

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8
Q

are generally small and relatively fast
moving and occupy narrow valleys, but then evolve

A

Headwater streams

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9
Q

Individual systems are separated from one another by a
topographic high or crest in the landscape called a

A

drainage divide

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10
Q

represents the land area that collects water for an
individual stream or river.

A

drainage basin

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11
Q

are any smaller streams that feed larger streams within a
drainage basin

A

Tributaries

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12
Q

A method of classifying or
ordering the hierarchy of
natural channels

A

Strahler Stream Order

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13
Q

reflects downstream trade off between discharge
and slope in setting transport capacity (and thus ability to move
sediment and incise rock)

A

Longitudinal Profile

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14
Q

The
level below which a river or stream cannot incise

A

Base Level

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15
Q

Most commonly formed on horizontally
bedded and uniform sediments or on
uniformly resistant crystalline rocks.

A

Dendritic

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16
Q

Usually develops on moderate to steep slopes,
but also where regional structure, such as
outcropping resistant rock bands, are
elongated and parallel. All forms of transition

A

Parallel

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17
Q

Patterns most commonly on dipping or folded
sedimentary or weakly metamorphosed
sedimentary rocks; also areas of joints and

A

Trellis

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18
Q

Usually have a more or less
perpendicular turns mainly
caused by criss crossing
fractures.

A

Rectangular

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19
Q

Occurs around domes or cones, and
particularly common on volcanic areas.

A

Radial

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20
Q

Patterns also develop around domes, where
there exists alternating resistant and weak
beds, so that the major channels cut through

A

Annular

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21
Q

Can occur in a variety of conditions where local
hummocks and depressions inhibit a continuous
channel network.

A

Multibasinal

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22
Q

Incised into rocks with complicated structural
patterns. Associated with crystalline metamorphic
rocks with a history of intense folding, jointing,
intrusions, alterations, and faulting.

A

Contorted

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23
Q

all year agas na river

A

perennial

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24
Q

mo agas lang during heavy rain

A

ephemeral

25
Q

naay month range para mo agas ni na river

A

intermittent

26
Q

are loose rock particles/sediments
deposited on a stream.

A

Alluvium

27
Q

One of the key factors in a stream’s ability
to erode the landscape is the

A

velocity of
the water

28
Q

are unstable overhang located
at the outer bank which is produced by the
velocity increase on the outer bank which
subsequently enhances the ability of the
water to cut (erode) into the bank.

A


Cutbanks

29
Q

On the inner bank where velocity decreases,
sediment tends to accumulate and form a
deposit known as a

A

point bar

30
Q

the sediment that physically scrapes
or wears away rock in a process called

A

abrasion

31
Q

Evidence for stream abrasion in solid rock can be seen in

A

potholes

32
Q

The velocity of a particular stream segment is controlled
by the steepness of the channel, called

A

stream
gradient

33
Q

is used to describe the lowest
level to which a stream can erode

A

base level

34
Q

often referred to as ultimate base level
because the oceans represent the end or low point of
most rivers (exceptions include isolated areas below sea
level, such as the Dead Sea and Death Valley)

A

Sea level

35
Q

describes the fraction of solid particles that is
in a suspended state and moving at the same velocity as the
water suspended material is what makes streams appear
muddy

A

Suspended load

36
Q

The process whereby water separates sediment grains based
on their size, shape, and density is called

A

called hydraulic sorting

37
Q

are mound shaped channel deposits consisting of sorted material ranging in size from boulders to
coarse gravel to fine sand.

A

Bars

38
Q

develop on the inside of meander bends where water velocity
decreases.

A

point bars

39
Q

are formed when a river enters a lake or ocean and splits into smaller channels and begins to
deposit sediment due to a decrease in velocity.

A

Deltas

40
Q

are large fan shaped deposits that form where steep mountain streams empty
out onto valley floors at the mouth of rivers.

A

Alluvial fans

41
Q

Streams also transport considerable amounts of dissolved ions (charged atoms) in what scientists refer to as the

A

dissolved load

42
Q

produces wider valleys over time, whereas deposition on the
inner
banks helps to build a flat plain on the valley floor called a

A

natural floodplain.

43
Q

are pair of ridges that run parallel to the bank
which are formed due to the deposition of sediment, commonly
sand, at the edge of the bank.

A

Natural levees

44
Q

are areas on the floodplain that are poorly
drained and can remain wet long after a flood.

A

Back swamps

45
Q

are old floodplain left high and dry as river
migrates.

A

Stream terraces

46
Q

The potential for flooding in a given area naturally increases as the_________ and _______ of rainfall
increases. Rainfall events range from light, steady rains that may last for days to heavy, and torrential rains

A

intensity and duration

47
Q

The ability of the ground to absorb water, referred to as

A

infiltration capacity,

48
Q

are floods that have short duration
with relatively high peak discharge; small
streams and rivers tend to rapidly overflow
their banks.

A

Flash Floods

49
Q

can be defined as one where a river
leaves its channel farther down in its drainage
basin, flowing out onto its floodplain and
inundating large areas of the valley floor.

A

Downstream Floods

50
Q

normally dry areas of
the land become inundated

A

flood

51
Q

the height at which a river
begins to overflow its banks.

A

Flood stage

52
Q

straightening and deepening a stream channel

A

Channelization

53
Q

temporarily stores some the excesses water in a
series of depressions

A

Retention Basins

54
Q

type of barrier in which
vegetated strips line the banks of stream channels,

A

Stream buffers

55
Q

made of a synthetic
fabric that is fi ne enough to trap sediment,

A

silt fences,

56
Q

Wetlands (swamps) are commonly found in
topographic depressions and adjacent to river channels, in
which case they are called

A

riparian wetlands

57
Q

Large pipes called _____ are typically used
for small streams that flow intermittently.

A

culverts

58
Q
A