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Dorothy Sack

Affiliations: 
Geography Ohio University, Athens, OH, United States 
Area:
Physical geography
Website:
https://www.ohio.edu/cas/sack
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"Dorothy Sack"
Bio:

https://books.google.com/books?id=ao8vAQAAIAAJ

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Parents

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Donald Rusk Currey grad student 1988 University of Utah
 (Studies of G.K. Gilbert, Lake Bonneville chronology reconstructions, and the quaternary geology of Tule Valley, West-Central Utah)

Children

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Mark Alan Fonstad grad student 1997 Ohio University

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Publications

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Li N, Li M, Sack D, et al. (2020) Diatom evidence for mid-Holocene peatland water-table variations and their possible link to solar forcing. The Science of the Total Environment. 725: 138272
Li N, Sack D, Sun J, et al. (2020) Quantifying the carbon content of aeolian sediments: Which method should we use? Catena. 185: 104276
Li N, Sack D, Gao G, et al. (2018) Holocene Artemisia-Chenopodiaceae-dominated grassland in North China: Real or imaginary?: The Holocene. 28: 834-841
Nishizawa S, Currey DR, Brunelle A, et al. (2013) Bonneville basin shoreline records of large lake intervals during Marine Isotope Stage 3 and the Last Glacial Maximum Palaeogeography, Palaeoclimatology, Palaeoecology. 386: 374-396
Nishizawa S, Currey DR, Brunelle A, et al. (2012) Bonneville basin shoreline records of a large lake during Marine Isotope Stage 16 Quaternary Science Reviews. 58: 1-6
Patrickson SJ, Sack D, Brunelle AR, et al. (2010) Late Pleistocene to early Holocene lake level and paleoclimate insights from Stansbury Island, Bonneville basin, Utah Quaternary Research. 73: 237-246
Sack D, Luz Sd. (2003) Sediment Flux And Compaction Trends On Off-Road Vehicle (Orv) And Other Trails In An Appalachian Forest Setting Physical Geography. 24: 536-554
Sack D. (1999) The composite nature of the Provo level of Lake Bonneville, Great Basin, Western North America Quaternary Research. 52: 316-327
Sack D. (1995) The shoreline preservation index as a relative-age dating tool for late pleistocene shorelines: An example from the bonneville basin, U.S.A. Earth Surface Processes and Landforms. 20: 363-377
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