Flooding - Drainage Patterns Flashcards

1
Q

what are the different types of drainage patterns?

A
  1. Dendritic
  2. Parallel
  3. Trellis
  4. Rectangular
  5. Radial
  6. Annular
  7. Multibasinal
  8. Contorted
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2
Q

is it the most commonly formed on horizontally or slightly dipping beds and uniform sediments or on uniformly resistant crystalline rocks

A

dendritic

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3
Q

t or f: in dendritic drainage pattern, the subsurface geology has a similar resistance to weathering so there is no apparent control over the direction the tributaries take

A

t

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4
Q

dendritic pattern have tributaries joining larger streams at what angle?

A

acute (<90 degrees)

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5
Q

this drainage pattern is the most common form and looks like the branching pattern of tree roots.

A

dendritic drainage

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6
Q

this drainage pattern is the most common form and looks like the branching pattern of tree roots.

A

dendritic drainage

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7
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
can occur this type and dendritic and trellis
pattern.

A

Parallel

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8
Q

parallel drainage pattern develop on what slopes?

A

moderate to steep slopes

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9
Q

this type of drainage pattern could be a manifestation of rigid structures or faults

A

parallel

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10
Q

Because of the steep slopes, the streams are swift and straight, this drainage pattern have very few tributaries, and all flow in the same direction.

A

Parallel

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11
Q

sometimes indicates the presence of a major fault that cuts across an area of steeply folded bedrock

A

Parallel

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12
Q

Patterns most commonly on dipping or folded
sedimentary or weakly metamorphosed
sedimentary rocks; also areas of joints and
faults which intersect with right angles and old
sand dunes with parallel alignment

A

Trellis

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13
Q

what is the drainage pattern of the Appalachian Mountains of North America?

A

Trellis

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14
Q

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

A

Rectangular

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15
Q

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

A

Radial

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16
Q

develops around a central elevated point

A

radial

17
Q

Patterns also develop around domes, where
there exists alternating resistant and weak
beds, so that the major channels cut through
the strike and the low order streams follow the
dip of the rocks.

A

Annular

18
Q

streams flow toward a central depression

A

annular

19
Q

Can occur in a variety of conditions where local
hummocks and depressions inhibit a continuous
channel network. Irregular glacial deposits or
erosional hollows due to solution of underlying
lithology, irregular thawing permafrost. Coastal
dunes, delta plains, and wind eroded hollows

A

multibasinal

20
Q

multibasinal patterns are usually in lithologies underlain by _______

A

limestone

21
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