GLACIAL EROSION, SEDIMENT TRANSPORT, AND ENVIRONMENTAL CHANGE IN THE GRINNELL AND SWIFTCURRENT VALLEYS, GLACIER NATIONAL PARK, MONTANA, USA (Invited Presentation)
Glacier National Park, Montana is sensitive to climate change as observed through historical glacial retreat (e.g., Key et al., 2002) and ecosystem adjustments (e.g., Klasner and Fagre, 2002), and there is widespread interest in the effects of future climate change in this unique public space. Lake sediment cores from the Grinnell Glacier valley in the northeast region of the Park show the response of the glacier since the end of the Last Glacial Maximum (Schachtman and others, 2015). The mineralogy and elemental composition of the bedrock in the valley provides constraints for the sources of lake sediments over time, demonstrating shifts in the geomorphic sources of clastic sediment to the chain of lakes. Shifting organic carbon sources, climate change, fire response, and human impacts are also observed in the lake cores. This has implications for the use of lake sediment cores in our interpretations of the geomorphic response of alpine landscapes to environmental change.