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Extensive Boulder Erosion Resulting from a Range Fire on the Type-Pinedale Moraines, Fremont Lake, Wyoming

Published online by Cambridge University Press:  20 January 2017

Susan G. Zimmerman
Affiliation:
Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, Pennsylvania 18015
Edward B. Evenson
Affiliation:
Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, Pennsylvania 18015
John C. Gosse
Affiliation:
Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, Pennsylvania 18015
Charles P. Erskine
Affiliation:
Mobile Research Development Corporation, Princeton, New Jersey 08544

Abstract

In July 1988, the FlatFish Range Fire burned over the type-Pinedale moraines at Fremont Lake, Wyoming, and caused extensive exfoliation of exposed boulder surfaces. The mass of exfoliated material from 130 of 1030 boulders investigated was measured and recorded with information concerning factors that could influence the extent of fire-induced exfoliation. The range in thickness of material removed from 98 randomly selected boulders within the burn area (averaged over the entire exposed boulder surface area) is 6.1 to < 0.1 mm. The mean thickness loss for all 98 boulders is 0.9 mm/fire and the expected loss from individual boulders (median) is 0.4 mm/fire. At the 95% confidence level there is no significant relationship between the degree of exfoliation and boulder size, lithology, grain size, proximity to vegetation, or vegetation density. The expected fire-induced boulder surface erosion rates range from 5.9 to 0.3 x 10-3 mm/yr on boulders in sagebrush rangeland where fire recurrence intervals are typically every 20 to 400 yr. Fire-induced exfoliation may account for differences in boulder size and abundance on Pinedale and Bull Lake moraines. Surface dating methods using varnish or cosmogenic nuclides may yield exposure ages that are too young if the consequences of range fires are not considered when sampling boulder surfaces that are within about 2 m above ground level.

Type
Research Article
Copyright
University of Washington

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References

Bamosky, C. Anderson, P., and Bartlein, P. (1987). The northwestern U.S. during deglaciation; Vegetational history and paleoclimatic implications. In “North America and Adjacent Oceans During the Last Deglaciation” (Ruddiman, W. F. and Wright, H. E. Jr., Eds.), DNAG Vol. K-3, pp 289323. Geological Society of North America, Boulder, CO.Google Scholar
Beer, E, and Johnston, E. (1981). “Mechanics of Materials.” McGraw-Hill, New York.Google Scholar
Bierman, P., and Gillespie, A. (1991). Range fires: A significant factor in exposure-age determination and geomorphic surface evolution. Geology 19, 641644.Google Scholar
Birkeland, P. (1984). “Soils and Geomorphology.” Oxford Univ. Press, New York.Google Scholar
Blackwelder, E. (1915). Post-Cretaceous history of the mountains of central western Wyoming. Journal of Geology 23, 307340.Google Scholar
Blackwelder, E. (1927). Fire as an agent in rock weathering. Journal of Geology 35, 134140.Google Scholar
Dorn, R. I. (1992). Comment on “Range fires: A significant factor in exposure age determination and geomorphic surface evolution.” Geology 20, 283.Google Scholar
Dom, R. I. Jull, A. J. T. Donahue, D. J. Linick, T. W., and Toolin, L. J. (1989). Accelerator mass spectrometry radiocarbon dating of rock varnish. Geological Society of America Bulletin 101, 13631372.Google Scholar
Dom, R. I. Turrin, B. Jull, A. Linick, T., and Donahue, D. (1987). Radiocarbon and cation-ration ages for rock varnish on Tioga and Tahoe morainal boulders of Pine Creek, eastern Sierra Nevada, California, and their paleoclimatic implications. Quarternary Research 28, 3849.Google Scholar
Evenson, E. B. Gillespie, A., and Stephens, G. (1990). Extensive boulder spalling resulting from a range fire at Pinedale type locality, Fremont Lake, Wyoming. Geological Society of America Annual Meeting, Abstracts with Program 22(7), 110.Google Scholar
Evenson, E. B. Gosse, J. C., and Klein, J. (1993). Application of in situ produced cosmogenic radionulcide exposure ages to reconstruct glacial histories at the Pinedale type locality, Wyoming. Geological Society of America Annual Meeting. Abstracts with Program 25(6), 308.Google Scholar
Forster, R. Fox, A., and Isacks, B. (1992). Relative age determination of Walker Valley moraines in the eastern Sierra Nevada using Airborne Polarimetric Synthetic Aperture Radar (SAR). EOS, Transactions of the American Geophysical Union, Spring Meeting 73(14), 186.Google Scholar
Gillespie, A. Budinger, F. E. Jr., and Abbott, E. A. (1989). Verification of prehistoric campfires by Ar-Ar analysis of fire-baked stones. Journal of Archeological Science 16, 271291.Google Scholar
Griggs, D. T. (1936). The factor of fatigue in rock exfoliation. Journal of Geology 44, 781790.Google Scholar
Gosse, J. C. Klein, J. Evenson, E. B. Lawn, B. R., and Middleton, R. (1994). Precision dating of glacial events based on AMS measurements of cosmogenic ,0Be produced in boulders. In “Abstracts of the Eighth International Conference on Geochronology, Cosmochronology and Isotope Geology” (Lanphere, M. A. Dairymple, G. B., and Turrin, B. D., Eds.), U.S. Geological Survey Circular 1107, p. 114. U.S Geological Survey, Denver, CO.Google Scholar
Harrington, C., and Whitney, J. (1987). Scanning electron microscope method for rock-varnish dating. Geology 15, 967970.Google Scholar
Houston, P. (1973). Wildfires in Northern Yellowstone National Park. Ecology 54, 11111117.Google Scholar
Joumaux, A., and Coutard, J.-P. (1974). Experience de thermoclastie sur des roches siliceuses. Bulletin Trimestriel de la Centre de Geomorphologie de Caen 18, 427.Google Scholar
Ken, A. Smith, B. J. Whalley, W. B„ and McGreevy, J. P. (1984). Rock temperatures from southeast Morocco and their significance for experimental rock-weathering studies. Geology 12, 306309.Google Scholar
Lai, D. (1991). Cosmic ray labeling of erosion surfaces: In situ nuclide production rates and erosion rates. Earth and Planetary Science Letters 104, 424439.Google Scholar
Mahaney, W., and Halvorson, D. (1986). Rates of mineral weathering in the Wind River Mountains, western Wyoming. In “Rates of Chemical Weathering of Rocks and Minerals,” pp. 147167. Academic Press, New York.Google Scholar
McFadden, L. D. Ritter, J. B., and Wells, S. G. (1989). Use of multiparameter relative-age methods for age estimation and correlation of alluvial fan surfaces on a desert piedmont, eastern Mojave Desert, California. Quaternary Research 32, 276290.Google Scholar
Nishiizumi, K. Winterer, E. L. Kohl, C. P. Lai, D. Arnold, J, R. Klein, J., and Middleton, R. (1989). Cosmic ray production rates of 10Be and 26A1 in quartz from glacially polished rocks. Journal of Geophysical Research 94, 17,90717,915.Google Scholar
Peck, B. J. Kaufman, D. S., and Calkin, P. E. (1990). Relative dating of moraines using moraine morphometric and boulder weathering criteria, Kiguaik Mountains, Alaska. Boreas 19, 227239.Google Scholar
Pye, K. (1986). Mineralogical and textural controls on the weathering of granitoid rocks. Catena 13, 4757.Google Scholar
Richmond, G. (1987). Type-Pinedale till in the Fremont Lake area, Wind River Range, Wyoming. In “Geological Society of America Centennial Field Guide—Rocky Mountain Section,” Vol. 444, pp. 201204. Geological Society of America, Boulder, CO.CrossRefGoogle Scholar
Teensma, P. (1981). “Sagebrush (artemisia tridentata nutt.) and Fire in Owens Valley, CA.” Unpublished Ph.D. dissertation, University of Oregon.Google Scholar
United States Department of Agriculture. (1989). “Bridger Wilderness Fires >100 acres 1960-1989.” Forest Service Map for Bridger-Teton National Forest, Pinedale Ranger District, North Half; 1:126, 720.100+acres+1960-1989.”+Forest+Service+Map+for+Bridger-Teton+National+Forest,+Pinedale+Ranger+District,+North+Half;+1:126,+720.>Google Scholar
United States Department of Commerce. (1965). “Climatography of the United States, No. 86-42, Climatic Summary of the U.S. Supplement for 1951-1960”. U.S. Government Printing Office, Washington, DC.Google Scholar
Wright, H., and Bailey, A. (1982). “Fire Ecology.” Wiley, New York.Google Scholar
Zschaechner, G. (1985). Studying rangeland effects: A case study in Nevada. In “Rangeland Fire Effects.” (Sanders, K. and Durham, J., Eds.), Proceeding of a Bureau of Land Management Symposium, Nov. 27-29, 1984, pp. 6684. U.S. Department of Agriculture, Bureau of Land Management, Boise, Idaho State Office.Google Scholar
Zimmerman, S. (1993). “Investigations of Extensive Boulder Spalling Resulting from a Range Fire at the Pinedale Type Locality, Fremont Lake, Pinedale, Wyoming.” Unpublished MS thesis, Lehigh University, Bethlehem, PA.Google Scholar