Lakes, Peat Swamps and Coal Deposits Flashcards

1
Q

Middle of lakes:

A
  • Deep water, not a lot of energy
  • Sediment raining out of the water column -> fine grained
  • Sediment comes from organisms living in the water + a lot of dust blown in the air + fine grain muddy sediment that was suspended by the river flow
  • Finest grain sizes (mud/clay)
  • Suspended sediment, windblown dust, organisms living there
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2
Q

Edges of Lake:

A
  • More activity.

- Some lakes have braided rivers bring in heaps of sediment

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3
Q

Shorelines (variety of environments):

A
  • River deltas bring in most of sediment
  • Waves can create beaches on shoreline
    (both methods providing sediment into the lake)
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4
Q

Sediment settling

A
  • Settling velocity = constant (based on grain density, gravity, fluid viscosity) * diameter squared
    Middle of the lake = sediment settling with all the fine grained sediment just going to blanket the bed.
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5
Q

Lakes in the Eastern African Rift:

A

Can often record seasonal change due to different plankton living in each lake for each season

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6
Q

Lakes Facies Model:

A
  • Turbidity currents from shoreline
  • Water temperature affects sediment suspension
  • Sediment comes in with any flow that flows into the lake
  • Lakes are thermally stratified (sediment can be trapped/suspended due to different layers of density)
  • denser, coarser sediments hug at the bottom as turbidity currents
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7
Q

Waves in lakes

A
  • Away from deltas but on the shoreline you will see the effect of waves
  • Wave size is determined by fetch (how long the wind has travelled for)
  • Shorelines are reworked by waves (size controlled by fetch - winds that blows lengthwise of the wave will make larger waves compared to winds that blow across the lake)
  • Wetting/drying -> mud cracks
  • Shoreline marshes with roots
  • Ice crystals.
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8
Q

Lakes in Arid Environments:

A

Arid: more evaporation than precipitation
Arid climate lakes:
- could be very seasonal rain/dry
- evaporation > precipitation
- Dries out (ephemeral) and gets saltier
Arid regions are pretty much 30 degrees North and South or in Rain Shadow Regions
- When evaporation is greater than precipitation, get salt deposits (evaporites)
- Salt crusts
- Water is super-saturated with respect to dissolved minerals -> form crystals (crystals nucleate with something on the surface e.g. another crystal or dust)

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9
Q

Bathtub ring:

A
  • Precipitated minerals in flood plain
  • Salt dissolves really easily and is in the middle (constantly in and out of solution)
  • Things that are less easy to dissolve are on the outer edges as are left over when it floods heaps
  • Corresponds to different amounts of flood levels.
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10
Q

Lakes in cold environments:

A
  • Cold environments you get ice -> ice blocks sediment at the surface
  • most seasonal lacustrine deposits (Varves)
  • Varves = seasonal layers from freezing and thawing
  • End up with extremely seasonal deposits
  • When the ice melts, all the sediment in/on the ice is released
  • good to use for climate change and good dating technique
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11
Q

Mires:

A
  • Lakes infill with sediment and vegetation and over time become a low lying mire (swampy ground, but water level does not change)
  • Low lying mire - water level is the same as the original lake (controlled by the ground water table elevation)
  • Raised Mires -> vegetation growth is fast tom make a dome (sediment s are the vegetation, and produce coal)
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12
Q

Ingredients of Organic coal

A

Woody plant materials tend to form coal as there is enough solid material to stay as a coherent carbon rich sediment)
- Algae and bacteria tend to form oil

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13
Q

Peat Accumulation

A
  • Woody plant growth is more rapid than decomposition - so stop the decomposition
    Physical:
  • Protected from sediment and groundwater
  • Rain - lots of it
  • Subsidence - not too fast or slow
    Chemical:
  • Low oxygen
  • Low pH
    Low lying marginal marine swamps are not goods for accumulating peat - too much oxygen?
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14
Q

Raised Mires produce purest coal due to:

A
  • Raised enough so all the water flows away from the centre of the mire
  • Are isolated from sediment and river input
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15
Q

Lakes and Mires:

A
  • Dominated by sediment settling (very fine grained)
  • Temperature Stratified water -> different densities, different chemistry, different sediment load
  • Sediment sources (wind-born dust, muddy surface water, aquatic organisms, down-slope turbidity currents - Bioturbation stirs together different layers
  • organic matter accumulates if decomposition is limited
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