Patterns of cover-type use in winter by snowshoe hares (Lepus americanus) were determined from presence of pellets on plots searched during 1969-84 when hare numbers increased substantially and subsequently declined. During population lows pellets were present more often in vegetation providing low, dense cover; i.e., Balsam Fir (Abies balsamea)-White Spruce (Picea glauca) (BS) and Cedar (eastern arborvitae, Thuja occidentalis) (CD) types. As hare numbers increased the proportion of plots with pellets increased for all cover types, but fewer were found in types with less cover; i.e., Red Pine (Pinus resinosa)White Pine (P. strobus) (PP) and nonforested (NF). J. WILDL. MANAGE. 50(2):261-264 Snowshoe hare populations in nonfragmented boreal forest cycle markedly with a periodicity of about 10 years (Keith 1963, Keith and Windberg 1978, Wolff 1980). Changes in hare distribution within different cover types occur during these fluctuations (Keith 1966, Wolff 1980), but no long-term record of them has been presented. This note describes such changes as indicated by the relative abundance of hare fecal pellets (Adams 1959, Wolff 1980, Orr and Dodds 1982, Pietz and Tester 1983, Litvaitis et al. 1985) during 1969-84 when the hare population in northern Minnesota increased substantially and subsequently declined. We gratefully acknowledge the assistance of numerous field personnel of the Sect. Wildl., Minn. Dep. Nat. Resour. (MDNR), particularly J. J. Mooty, J. A. Markl, and B. A. Toms. This study was funded and supported by the For. Wildl. Populations and Res. Group (MDNR) and the Off. Endangered Species, U.S. Fish and Wildl. Serv. D. W. Kuehn, L. B. Keith, and R. E. Lake reviewed the manuscript and provided helpful suggestions for improvement. STUDY AREA AND METHODS Hare population levels and cover-type use were studied in the 9-township (839-km2) Bearville Study Area in northeastern Itasca County, Minnesota. Topography in the area is gently to strongly rolling. The mean January temperature at Grand Rapids, about 50 km southwest of the study area, is -15 C, and the July mean is 20 C (Natl. Oceanic and Atmos. Adm. 1983). During winters 1968-69 through 1983-84, January-March snow depth averaged 37 cm (range = 13-71 cm). Snow cover usually is present from early December through early-late
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