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varve
(redirected from Rhythmite)

   Also found in: Encyclopedia, Wikipedia 0.01 sec.
varve  (värv)
n.
A layer or series of layers of sediment deposited in a body of still water in one year.

[Swedish varv, layer, from varva, to bend, from Old Norse hverfa.]

varve [vɑːv]
n Geology
1. (Earth Sciences / Geological Science) a typically thin band of sediment deposited annually in glacial lakes, consisting of a light layer and a dark layer deposited at different seasons
2. (Earth Sciences / Geological Science) either of the layers of sediment making up this band
[from Swedish varv layer, from varva, from Old Norse hverfa to turn]

varve  (värv)
A layer or series of layers of sediment deposited in a body of still water in one year. Varves are typically associated with glacial lake deposits and consist of two layersa lower, light-colored layer that consists primarily of sand and silt, and a darker upper layer that consists primarily of clay and organic matter. The lower layer is typically deposited in the summer by the rapid melt of glacial ice, and the upper layer is usually deposited in the winter by the slower settling of sediment through calm water. The thickness of the layers in a varve varies depending on the proximity to the margin of the glacier, with thicker layers forming closer to the glacial margin and thinner layers forming farther away from it. Varves have been used, like tree rings, to measure the ages of glacial deposits from the Pleistocene.


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In our opinion, unstable laminations in the central part could be interpreted as rhythmites deposited in a relatively shallow water basin with changing sediment supply from the catchment rather than glacial annual varves.
The rhythmites display layers of varying thickness, reflecting the high spring tides and low neap tides that mark the lunar month.
 
 
 
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