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Rhythmic Sedimentation in Glacial Lake Hitchcock, Massachusetts-Connecticut
Abstract
Most of the fine-grained bottom sediments of Glacial Lake Hitchcock are rhythmites composed of silt- clay couplets that occur in three structural groups :Group I—clay thickness greater than silt thickness.Group II—clay thickness approximately equal to silt thicknessGroup III—clay thickness less than silt thickness .Thin sections of impregnated sediments show flat bedding with as many as 40 graded laminae in one 5-cm layer. Erosional contacts and ripple cross-lamination are common in Group III, but rare in Groups I and II. The contact between silt and the overlying clay layer in any one rhythmite is gradational in less than 25 percent of the samples. Other sedimentary features include two distinct types of trace fossils. Mean grain size of the silt layers (5.50 to 8.50) depends up the environment of deposition of silt within the lake. Mean grain size of the clay layersis much the same everywhere (averaging 10.5ø).Data from 34 localities suggest thatthe rhythmites are annual (that is, they arevarves), andthefollowing depositional mechanism is proposed. Sediment was transported by streams from the glacier and from nearby deglaciated uplands. Gravel andsand were deposited on deltas. Silt and claywere carriedoutintothe lake, mainly by turbidity currents.Sediments coming into the lake contained asignificant amount ofclay that settled out continuously, but clay became the dominant deposit only during the winter when coarse material was less available.Varves belonging to Groups I and II generally were formed in still water away from river mouths, where little sediment was received directly from density currents. Group III varves were formed relatively near delta fronts, in environments characterized by high sedimentation rates.
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Metadata
- Authors
- Ashley, G. M.
- Affiliations
- University of Massachusetts Amherst (US)
- Corresponding author
- Ashley, Gail M.
- Venue
- Glaciofluvial and Glaciolacustrine Sedimentation
- Publisher
- SEPM Society for Sedimentary Geology
- Published
- 1975
- Pages
- 304-320
- OpenAlex
- W2245374685
- Cited by
- 220
- References
- 14
- Citations by year
- 2026: 1 · 2025: 2 · 2024: 5 · 2023: 3 · 2022: 3 · 2021: 5 · 2020: 8 · 2019: 6 · 2018: 5 · 2017: 6 · 2016: 6 · 2015: 7 · 2014: 4 · 2013: 8 · 2012: 3
- FWCI
- 5.13
- Type
- book chapter
- Language
- en
- Open access
- closed
- Locations
- SEPM (Society for Sedimentary Geology) eBooks (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and environmental studies
- Keywords
- rhythmic sedimentation, varves, lake sediments, turbidity currents, gravity currents, grain size, trace fossils, ripple cross-lamination, sedimentation rate, glacial lake sediments
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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