2000
DOI: 10.1016/s0037-0738(99)00120-7
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Seismic stratigraphy of Waterton Lake, a sediment-starved glaciated basin in the Rocky Mountains of Alberta, Canada and Montana, USA

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Cited by 29 publications
(36 citation statements)
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“…In general, the depositional history of Flathead Lake is typical for a lake basin recording the transition from glacial to post-glacial conditions. Thick late-glacial glaciolacustrine sediments are overlain by a thinner package of fine-grained Holocene deposits (Glenn and Kelts, 1991;Eyles et al, 2000). The infill is dominated by a thick succession of glacial till (unit A) and glaciolacustrine sediments (unit B) both immediately related to glacial activity in the lake basin.…”
Section: Resultsmentioning
confidence: 99%
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“…In general, the depositional history of Flathead Lake is typical for a lake basin recording the transition from glacial to post-glacial conditions. Thick late-glacial glaciolacustrine sediments are overlain by a thinner package of fine-grained Holocene deposits (Glenn and Kelts, 1991;Eyles et al, 2000). The infill is dominated by a thick succession of glacial till (unit A) and glaciolacustrine sediments (unit B) both immediately related to glacial activity in the lake basin.…”
Section: Resultsmentioning
confidence: 99%
“…5E). The drape-like geometry of units F and D suggests deposition of very fine-grained sediments by slow suspension settle out (Eyles et al, 2000). Although unit E does not display this drape-like geometry, its acoustic character and internal sedimentology also suggest deposition of fine-grained suspended sediments.…”
Section: Holocene Lake Historymentioning
confidence: 95%
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“…Glacial lakes often occupy these basins, and often contain a comprehensive record of late-glacial and post-glacial sediments (Pennington, 1978;Eyles et al, 2000). Lacustrine sediments further provide a high-resolution record of sediment provenance, biological history, catchment level anthropogenic activity and climatic and environmental change.…”
Section: Introductionmentioning
confidence: 99%
“…The remote sensing techniques employed to investigate the geophysical properties of the Lower Lough Erne Basin include highresolution Chirp sub-bottom profiler and a side-scan sonar system. The Chirp sub-bottom profiler is used to record continuous vertical sedimentary sequences of the lake basin, according to their acoustic reflectivity, to depths of approximately 30 m. Assessment of high-resolution sub-bottom data has greatly improved understanding of the evolutionary history of many lakes [8,16,25,31,38,51] and has also proved valuable in underwater archaeological investigations [44,45,46]. Sidescan sonar systems provide a graphic representation of how materials on the lake floor interact with acoustic energy.…”
Section: Introductionmentioning
confidence: 99%