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Connecticut Water Trails Association |
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Connecticut Water Trails Program
Lakes
How Lakes Disappear
A lake may be in-filled with deposited sediment and
gradually become a wetland such as a swamp or marsh. Large water plants,
typically reeds, accelerate this closing process significantly because
they partially decompose to form peat soils that fill the shallows.
Conversely, peat soils in a marsh can naturally burn and reverse this
process to recreate a shallow lake. Turbid lakes and lakes with many
plant-eating fish tend to disappear more slowly. A "disappearing" lake
(barely noticeable on a human timescale) typically has extensive plant
mats at the water's edge. These become a new habitat for other plants,
like peat moss when conditions are right, and animals, many of which are
very rare. Gradually the lake closes, and young peat may form, forming a
fen. In lowland river valleys, where a river can meander, the presence
of peat is explained by the infilling of historical oxbow lakes. In the
very last stages of succession, trees can grow in, eventually turning
the wetland into a forest.
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