Fluvial Systems - meandering streams and lacustrine Flashcards

(35 cards)

1
Q

What sediment size dominates meandering streams?

A

Mud

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2
Q

What are some characteristics of a meandering stream?

A
  • single channel
  • less sediment load and less variable discharge
  • max velocity & erosion at outer meander, and deposition at inner meander
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3
Q

What is a flood plain?

A

Flat plain near a fluvial system, gets periodically flooded.

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4
Q

A meandering stream is occasionally/constantly flowing.

A

constantly

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5
Q

What is an oxbow lake?

A

As the meandering stream gets more and more curve-y, the water constantly wants to go straight, so eventually, the very curved part gets cut off.

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6
Q

Meandering streams have less/more energy than a braided stream.

A

less

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7
Q

What are some common sediments you would see in an oxbow lake?

A

They have a lot of clay and are organic-rich.

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8
Q

What is a crevasse splay?

A

It is like an alluvial fan in shape, but happens when a natural levee breaks when the meandering stream floods. Consist of fine-very fine grained sandstones with ripples, trough crossbedding, parallel lamination and scour and fill structures. Upper part full of roots and burrows.

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9
Q

One of the most characteristic products of a meandering river is the _______________ sequence, which forms at the inner bank of a meander.

A

point-bar

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10
Q

At the edge of the meandering stream bank, where the bed is just high enough to begin to slow the current, gravel and coarse sand are deposited, forming a thin, discontinuous ___________ lag.

A

channel

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11
Q

What are natural levees?

A

Wall of sand and mud that forms a high bank on each side of a river, formed when a flood recedes.

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12
Q

What are the layers in a Bouma sequence?

A

The classic sequence has a scoured base overlain by a massive graded bed (unit A) which represents the coarsest material to settle of suspension as the turbidity current slowed. Over is plane lamination (B) which is believed to represent high-flow-regime plane beds. C displays ripples and wave lamination, indicative of lower flow regime. D is laminated silt and E is laminated mud that settled out of suspension during the waning of the turbidity current. In some cases E is topped by laminated hemipelagic mud that settled from suspension in the episodes between turbidity currents.

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13
Q

Study this slide summarizing meandering stream deposits

A
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14
Q

What sediment size are lake deposits dominated by?

A

mud

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15
Q

What is a very strong defining feature of lake deposits?

A

Laminated mud, thin bedding

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16
Q

How does the water in a lake mix?

A

wind, especially at the upper part

if it’s shallow, there will be a mixing zone. however, the bottom is commonly anoxic (oxygen deprived)

17
Q

Does the vertical deposit of a former lake area have coarsening or fining up?

A

Coarsen-up as the lake dries.

In the attached image, the rootlets and desiccation cracks signify edges of the lake; climbing ripples, parallel-laminated sand/mud-stone and wave ripples are at shore line; hummocky, burrows and graded beds are close to shore. The bottom: homogeneous (ie. laminated) mudstones are at the basin

18
Q

How can you tell the difference between lake and ocean deposit?

A

Scale.
Lakes are significantly smaller. Also, lake deposits tend to be thin whereas oceans are thick.

19
Q

What is black shale?

A

Organic rich shale

20
Q

If you see a lake deposit with slightly green sediment, what would that tell you?

A

It is a little anoxic.

21
Q

A deltatic deposit looks like an alluvial fan, but it is ______ from the source and it is ______ dominated.

22
Q

______ form where rivers carry more sediment into the sea than marine erosion can carry away.

23
Q

T/F: Deltas are more common on active, subducting continental margins

A

False, they seldom do bc there is no stable shallow shelf on which sediments can accumulate

24
Q

What are topset beds in a Gilbert-type delta?

A

Topset beds are the nearly flat, upper layers of a Gilbert delta, formed in shallow water by river deposits. They consist of coarse to medium sediment (like sand and gravel) and often show horizontal bedding.

25
What are foreset beds in a Gilbert-type delta?
Foreset beds are steeply sloping layers that form the front of the delta. Sediment cascades down the slope into deeper water, creating thick, inclined beds of coarse material like gravel and sand.
26
What are bottomset beds in a Gilbert-type delta?
Bottomset beds are the thin, gently sloping layers that extend into the deeper basin beyond the foreset. They are made of fine sediments like silt and clay, settling from suspension in calm water.
27
What are the four different types of deltas?
lobate, elongate, cuspate and estuarine
28
study this tertiary diagram about the different classifications of deltas.
29
A river-dominated delta has a large volume of sediment and tends to be ________ in shape when there is a moderate sediment supply and ___________ in shape when the sediment supply is large.
lobate, enlongate
30
A ____-dominated delta has many linear channels parallel to the tidal flow and perpendicular to the shore.
tide
31
A _____-dominated delta is smoothly acrute, the sediment is reworked and makes the deltas sandier than other types.
wave
32
A _________ mouth bar is a sandbar that forms across the mouth of a delta __________ channel, usually where the freshwater flow of the river slows down as it meets the sea and dumps its load of sediment.
distributary, distributary
33
A ___________ channel is a smaller river branch that splits from the main channel and spreads water and sediment across a delta.
distributary
34
What is an interdistributary bay?
Branching off stream they start branching and the bays are what’s in between. The flood plain of deltas.
35
Study this chart on delta sequences