GPR stratigraphy used to infer transgressive deposition of spits and a barrier, Lake Bonneville, Stockton, Utah, USA

Geological Society Special Publication - Tập 211 Số 1 - Trang 79-86 - 2003
Derald G. Smith1, Chris Simpson2,1, Harry M. Jol3, Richard A. Meyers1, Donald R. Currey4
1Department of Geography, University of Calgary, Calgary, Alberta, T2N 1N4, Canada
2Department of Geography, Simon Fraser University, Burnaby, British Columbia V5A 1S6 Canada
3Department of Geography, University of Wisconsin-Eau Claire Eau Claire, WI 54702-4004, USA
4Department of Geography, University of Utah Salt Lake City, Utah, 84112-1183, USA

Tóm tắt

Abstract Ground penetrating radar (GPR) stratigraphic profiles of the classic cross-valley barrier and associated spits of Late Pleistocene Lake Bonneville, near Stockton, Utah, are used to infer transgressive depositional style and internal sedimentary structures. From onlapping patterns of radar reflections, which mimic subsurface stratigraphy, we reconstruct the following depositional sequence and style: (1) at the north end of the Rush Valley, the barrier formed by vertical accretion while keeping pace with hydro-isostatic-forced basin subsidence and/or slow lake-level rise; (2) a reorientation of the longshore transport pathway, induced by continued basin subsidence and/or a lake-level rise, produced a spit that prograded 2.5 km southwestward into Rush Valley. The NW-dipping radar reflections from the spit onlap SE-dipping reflections from the back-barrier, indicating that this spit was deposited after the barrier; (3) a final rise in lake level and/or basin subsidence again reoriented longshore transport and deposited the smaller upper spit. Radar reflections from the upper spit onlap the proximal eastern margin of the Stockton spit. This upper spit is the final landform deposited during the Bonneville highstand. The depositional sequence inferred from radar stratigraphy agrees with the transgressive hypothesis formulated in 1890 by G. K. Gilbert.

Từ khóa


Tài liệu tham khảo

Burr T. N., Currey D. R. , Machette M. N. The Stockton bar In the Footsteps of G.K. Gilbert — Lake Bonneville and Neotectonics of the Eastern Basin and Range Province 1988 66 73 Utah Geological and Mineral Survey

10.1016/S0380-1330(94)71129-1

10.1016/0031-0182(90)90113-L

Currey D. R., Oviatt C. G., Plyler G. B. , Gurgel K. D. Lake Bonneville stratigraphy, geomorphology, and isostatic deformation in west-central Utah Geologic Excursions in Neotectonics and Engineering Geology in Utah: Guidebook Part IV 1983 62 63 82 Utah Geological and Mineral Survey Special Studies

10.1111/j.1365-2478.1989.tb02221.x

Gilbert G. K. The topographic features of lake shores US Geological Survey Fifth Annual Report 1885 1883 1884 69 123

10.5962/bhl.title.45550

10.1130/0016-7606(1987)99<127:POTLPB>2.0.CO;2

10.1139/e91-175

Kesik A. B., Law J., McFall G. , McKenzie D. I. Geomorphology and geology of Lake Ontario; north shore Quaternary Environs of Lakes Erie and Ontario, Waterloo, ON 1990 Escart Press 163 265

10.1016/0031-0182(95)00117-4

Malde H. E. The Catastrophic Late Pleistocene Bonneville Flood in the Snake River Plain Idaho 1968 596 52 pp US Geological Survey Professional Papers

Nielsen E. Surficial Geology of the Swan River Area, Winnipeg, MB 1988 Mineral Resources Division Manitoba Department of Energy and Mines

10.1139/e84-089

10.1130/SPE274-p1

10.1130/0091-7613(1997)025<0155:LBFAGC>2.3.CO;2

10.1016/0031-0182(92)90017-Y

Smith D. G., Jol H. M. GPR results used to infer depositional processes of coastal spits in large lakes Geological Survey of Finland Special Paper 1992 16 169 177

10.1016/0926-9851(95)90032-2

10.1016/0025-3227(95)00110-7