PALEOMAGNETISM OF TILLS AND ASSOCIATED PALEOSOLS IN SOUTHWESTERN ALBERTA AND NORTHERN MONTANA - EVIDENCE FOR LATE PLIOCENE - EARLY PLEISTOCENE GLACIATIONS

Sequences of pre-Wisconsinan till and intercalated paleosols were samp led for paleomagnetic study. The tills were deposited during successiv e glaciations and the paleosols formed during interglacial intervals. Paleoargillic horizons of the paleosols and the carbonate cement (calc rete) found in some till-paleosol units generally yielded excellent da ta. Magnetizations of paleosols probably were acquired during the form ation of the paleosols rather than during initial deposition of the ti lls in which they were developed. At Mokowan Butte (Alberta), the lowe st paleosol has normal polarity, two of the middle tills have reversed polarity, and the uppermost till - paleosol unit has normal polarity. At Saint Mary Ridge (Montana), three of the lower tills have reversed polarity, and the upper two till-paleosol units have normal polarity. At Two Medicine Ridge (Montana), the lowest three tills are reversed, but the paleoargillic horizon on the uppermost (fourth) till is norma l. Magnetostratigraphic correlation indicates that at least six glacia l and six interglacial episodes are represented in the Kennedy Drift. The upper normal polarity units are interpreted as having been develop ed during the Brunhes Normal Chron, the underlying reversed polarity s ediments during the Matuyama Reversed Chron, and the lowest normal pol arity unit at Mokowan Butte during the Gauss Normal Chron. The oldest glaciations here extend into the Pliocene (2600 ka), making these sedi ments among the oldest glacial deposits in North America. Alternativel y, the lowest normally magnetized paleosol at Mokowan Butte may have f ormed during either the Jaramillo or the Olduvai subchrons, although t his is considered less likely.