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

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

to drain water off the landscape and to transport sediment

A

role of streams

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

a process where water flows through
stream channels

A

Runoff

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

precipitation reaching the land
surface moves downslope in thin sheets

A

Overland Flow

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

discharge of
groundwater into the surface environment

A

Groundwater baseflow

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

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

A

Stream hydrographs

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
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

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

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

A

Headwater streams

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

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

A

drainage divide

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

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

A

drainage basin

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

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

A

Tributaries

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

A method of classifying or
ordering the hierarchy of
natural channels

A

Strahler Stream Order

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
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

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

The
level below which a river or stream cannot incise

A

Base Level

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

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

A

Dendritic

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
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

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

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

A

Trellis

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
18
Q

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

A

Rectangular

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
19
Q

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

A

Radial

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
20
Q

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

A

Annular

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
21
Q

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

A

Multibasinal

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
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

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
23
Q

all year agas na river

A

perennial

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
24
Q

mo agas lang during heavy rain

25
naay month range para mo agas ni na river
intermittent
26
are loose rock particles/sediments deposited on a stream.
Alluvium
27
One of the key factors in a stream’s ability to erode the landscape is the
velocity of the water
28
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.
 Cutbanks
29
On the inner bank where velocity decreases, sediment tends to accumulate and form a deposit known as a
point bar
30
the sediment that physically scrapes or wears away rock in a process called
abrasion
31
Evidence for stream abrasion in solid rock can be seen in
potholes
32
The velocity of a particular stream segment is controlled by the steepness of the channel, called
stream gradient
33
is used to describe the lowest level to which a stream can erode
base level
34
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)
Sea level
35
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
Suspended load
36
The process whereby water separates sediment grains based on their size, shape, and density is called
called hydraulic sorting
37
are mound shaped channel deposits consisting of sorted material ranging in size from boulders to coarse gravel to fine sand.
Bars
38
develop on the inside of meander bends where water velocity decreases.
point bars
39
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.
Deltas
40
are large fan shaped deposits that form where steep mountain streams empty out onto valley floors at the mouth of rivers.
Alluvial fans
41
Streams also transport considerable amounts of dissolved ions (charged atoms) in what scientists refer to as the
dissolved load
42
produces wider valleys over time, whereas deposition on the inner banks helps to build a flat plain on the valley floor called a
natural floodplain.
43
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.
Natural levees
44
are areas on the floodplain that are poorly drained and can remain wet long after a flood.
Back swamps
45
are old floodplain left high and dry as river migrates.
Stream terraces
46
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
intensity and duration
47
The ability of the ground to absorb water, referred to as
infiltration capacity,
48
are floods that have short duration with relatively high peak discharge; small streams and rivers tend to rapidly overflow their banks.
Flash Floods
49
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.
Downstream Floods
50
normally dry areas of the land become inundated
flood
51
the height at which a river begins to overflow its banks.
Flood stage
52
straightening and deepening a stream channel
Channelization
53
temporarily stores some the excesses water in a series of depressions
Retention Basins
54
type of barrier in which vegetated strips line the banks of stream channels,
Stream buffers
55
made of a synthetic fabric that is fi ne enough to trap sediment,
silt fences,
56
Wetlands (swamps) are commonly found in topographic depressions and adjacent to river channels, in which case they are called
riparian wetlands
57
Large pipes called _____ are typically used for small streams that flow intermittently.
culverts
58