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APRON If into water, a varve.
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The part of a varve deposited in summer is likely to be composed of lighter colored, coarser sediment with higher organic content, reflecting increased biological productivity during the warmer months. Summer varves often show distinct layers that can be identified and dated accurately due to their unique characteristics.
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A pair of sedimentary layers (one coarse, one fine) that is deposited in an annual cycle, commonly in glacial lakes, and that can be used to determine absolyte age.
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Varves are sedimentary deposits that are deposited in a still body of water (e.g. lake). Varves are created by melting and freezing of glacial ice. In the summer when the glacier melts (retreats) silt- and sand-sized particles are carried by the melt water to the lake and deposited. In the winter when the still body of water is frozen, fine clays settle out on top of the coarser silt and sand. This cycle is repeated seasonally. Therefore, a varve sequence represents one year.
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An annually deposited sedimentary layer is called a varve. Originally the word referred only to those annual layers of sediment deposited in a lake by glaciers, but now the more general use is accepted. Another term used in the literature is "annually laminated."
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