William R. Farrand
Affiliations: | 1965-2000 | Geological Sciences | University of Michigan, Ann Arbor, Ann Arbor, MI |
Area:
sedimentology, stratigraphy, and paleoclimatologyWebsite:
https://www.lib.umich.edu/faculty-history/faculty/william-r-farrandGoogle:
"William Farrand"Bio:
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Publications
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Evenson EB, Mickelson DM, Farrand WR. (2010) Stratigraphy and correlation of the Late Wisconsinan glacial events in the Lake Michigan basin Geographie Physique Et Quaternaire. 31: 53-59 |
Straus LG, González Morales M, Farrand WR, et al. (2001) Sedimentological and Stratigraphic Observations in El Mirón, a Late Quaternary Cave Site in the Cantabrian Cordillera, Northern Spain Geoarchaeology - An International Journal. 16: 603-630 |
Farrand WR. (2001) Sediments and stratigraphy in rockshelters and caves: A personal perspective on principles and pragmatics Geoarchaeology-An International Journal. 16: 537-557 |
Farrand WR. (1999) Comment on “Konispol Cave, southern Albania, and correlations with other Aegean caves occupied in the late quaternary by Joseph Schuldenrein” Geoarchaeology-An International Journal. 14: 471-472 |
Farrand WR, McMahon JP. (1997) History of the sedimentary infilling of Yarimburgaz Cave, Turkey Geoarchaeology-An International Journal. 12: 537-565 |
Evenson EB, Eschman DF, Farrand WR, et al. (1980) Comment on ``The Fossil Coleoptera of the Two Creeks Forest Bed, Wisconsin'', by Alan V. Morgan and Anne Morgan Quaternary Research. 14: 377-378 |
Farrand WR. (1979) Chronology and palaeoenvironment of levantine prehistoric sites as seen from sediment studies Journal of Archaeological Science. 6: 369-392 |
Evenson EB, Farrand WR, Eschman DF, et al. (1978) Reply to comments by P. F. Karrow and R. F. Black Quaternary Research. 9: 123-129 |
Evenson EB, Farrand WR, Eschman DF, et al. (1976) Greatlakean Substage: A replacement for Valderan Substage in the Lake Michigan basin Quaternary Research. 6: 411-424 |
Farrand WR. (1975) Sediment analysis of a prehistoric rockshelter: The Abri Pataud Quaternary Research. 5: 1-26 |