Quantitative identification of erosional Lake Bonneville shorelines, Utah

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منابع مشابه

Controls of Tufa Development in Pleistocene Lake Bonneville, Utah

Prominent tufa localities along the Provo level (∼14,000 C yr B.P.) shoreline in Pleistocene Lake Bonneville have been characterized in detail. Three types of tufa are recognized: capping tufa, beachrock, and capping tufa over beachrock. Capping tufa and beachrock are end members of a continuum based on variable clastic content. All three types typically occur on headland environments that had ...

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Late Pleistocene to early Holocene lake level and paleoclimate insights from Stansbury Island, Bonneville basin, Utah

a r t i c l e i n f o Keywords: Great Basin Lake Bonneville Great Salt Lake Stansbury Island Stansbury shoreline Stansbury oscillation Stansbury Gulch Paleolake chronology Paleoclimate Multiple proxy This paper reports on recent multiproxy research conducted to determine the chronology of lake-level fluctuations recorded in sediments from a natural exposure at a classic Bonneville basin site. G...

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Morphology and paleoclimatic significance of Pleistocene Lake Bonneville spits

Pleistocene Lake Bonneville of western Utah contains a variety of spits associated with shorelines and other features that formed between 21,000 and 12,000 C yr BP. Field studies in the low-lying mountain ranges of the central portion of Lake Bonneville identified 17 spits of various types. The spits are connected to small mountain ranges and islands, vary in size from 0.02 to 0.5 km, and are c...

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Dendroarchaeology of the Salt Lake Tabernacle, Utah

We examined tree rings from Douglas-fir (Pseudotsuga menziesii var. glauca (Beissn.) Franco) timbers in the Salt Lake Tabernacle, constructed from 1863–1867 in Salt Lake City, Utah. A seismic upgrade to the Tabernacle initiated in 2005 required the replacement of wooden timbers with steel beams. Our objectives were to 1) determine cutting dates for the timbers to identify logs that may have bee...

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Lake-size variations in the Lahontan and Bonneville basins

Benson, L., Currey, D., Yong Lao and Hostetler, S., 1992. Lake-size variations in the Lahontan and Bonneville basins between 13,000 and 9000 14C yr B.P.. Palaeogeogr., Palaeoclimatol., Palaeoecol., 95: 19-32. Recessions of Lakes Lahontan and Bonneville that commenced ~ 13,500 ~4C yr B.P. were interrupted at i> 11,500 14C yr B.P. in the Lahontan basin and ~ 12,200 14C yr B.P. in the Bonneville b...

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ژورنال

عنوان ژورنال: Geomorphology

سال: 2016

ISSN: 0169-555X

DOI: 10.1016/j.geomorph.2015.09.022