Lakes, Peat Swamps and Coal Deposits Flashcards
Middle of lakes:
- 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
Edges of Lake:
- More activity.
- Some lakes have braided rivers bring in heaps of sediment
Shorelines (variety of environments):
- River deltas bring in most of sediment
- Waves can create beaches on shoreline
(both methods providing sediment into the lake)
Sediment settling
- 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.
Lakes in the Eastern African Rift:
Can often record seasonal change due to different plankton living in each lake for each season
Lakes Facies Model:
- 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
Waves in lakes
- 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.
Lakes in Arid Environments:
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)
Bathtub ring:
- 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.
Lakes in cold environments:
- 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
Mires:
- 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)
Ingredients of Organic coal
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
Peat Accumulation
- 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?
Raised Mires produce purest coal due to:
- Raised enough so all the water flows away from the centre of the mire
- Are isolated from sediment and river input
Lakes and Mires:
- 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