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This naturally occurring anoxic basin allows for sediments to be deposited without bioturbation, forming varves of alternating light and dark color, which correspond to the dry or rainy season.
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This example is from Wikipedia and may be reused under a CC BY-SA license.The varves thus record the change in the lakes' environment around 1800, when the primeval forests in the region were replaced by open fields and farmland.
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This example is from Wikipedia and may be reused under a CC BY-SA license.At the deep permanent lake stage in a typical cycle there is normally a laminite, consisting of fine-scale alternations of clastic, carbonate and organic laminae, thought to represent annual varves.
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This example is from Wikipedia and may be reused under a CC BY-SA license.There is a distinct change in the color of the varves that occurred around 1800; the lower, older varves are dark brown, and the higher, younger varves are grey.
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This example is from Wikipedia and may be reused under a CC BY-SA license.The clays show a rhythmical,varve-like layering.
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This example is from Wikipedia and may be reused under a CC BY-SA license.Quaternary varves are used in stratigraphy and palaeoclimatology to reconstruct climate changes during the last few hundred thousand years.
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This example is from Wikipedia and may be reused under a CC BY-SA license.Of the many rhythmites found in the geological record, varves are among the most important and illuminating to studies of past climate change.
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This example is from Wikipedia and may be reused under a CC BY-SA license.Of the many rhythmites found in the geological record, varves are one of the most important and illuminating to studies of past climate change.
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This example is from Wikipedia and may be reused under a CC BY-SA license.Similar seasonal patterns also occur in ice cores and in varves (layers of sediment deposition in a lake, river, or sea bed).
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This example is from Wikipedia and may be reused under a CC BY-SA license.Each pair of layers is called avarveand represents one year.
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This example is from Wikipedia and may be reused under a CC BY-SA license.Varves have recently experienced a renaissance as methods and techniques of study have improved, and varves are now regularly used to calibrate radiocarbon timescales.
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This example is from Wikipedia and may be reused under a CC BY-SA license.In addition to seasonal variation of sedimentary processes and deposition,varveformation requires the absence of bioturbation.
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This example is from Wikipedia and may be reused under a CC BY-SA license.The mean thickness of avarvehere is 0.18 mm, with a minimum thickness of 0.014 mm and maximum of 9.8 mm.
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This example is from Wikipedia and may be reused under a CC BY-SA license.Each band is similar to avarve, to the extent that the banding is assumed to result from cyclic variations in available oxygen.
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Wikipedia
This example is from Wikipedia and may be reused under a CC BY-SA license.Such varves in meromictic lakes preserve an historical record something like tree rings do.
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Wikipedia
This example is from Wikipedia and may be reused under a CC BY-SA license.Laminae that represent seasonal changes (similar to tree rings) are called varves.
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This example is from Wikipedia and may be reused under a CC BY-SA license.Varve(or "varved clay") is clay with visible annual layers, which form from seasonal differences in erosion and organic content.
FromThis example is from Wikipedia and may be reused under a CC BY-SA license.
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This example is from Wikipedia and may be reused under a CC BY-SA license.As the varves get closer to the shoreline the clay layer will stay relatively the same thickness, but there will be an increase in thickness of the silt layer.
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This example is from Wikipedia and may be reused under a CC BY-SA license.However, international interest in varves diminished.
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Wikipedia
This example is from Wikipedia and may be reused under a CC BY-SA license.These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
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