CONSTRAINING GLACIAL HISTORY AND PROCESS ON MOUNT MANSFIELD, VERMONT'S HIGHEST PEAK, WITH IN SITU COSMOGENIC 10BE AND 14C
Below 1200 m, seven bedrock surfaces and three boulders have 10Be exposure ages that form a single population (average, 14.2 ± 0.4 ka, 1SD), suggesting rapid lowering of the ice surface during deglaciation, possibly coincident with Bølling/Allerød warming. A boulder and a bedrock sample collected near one another have indistinguishable ages suggesting similar erosion and exposure histories (15.0 ± 0.3 and 14.4 ± 0.3 ka, 1σ internal uncertainties). Another boulder has similar 10Be and 14C ages (10Be 13.8 ± 1.1 ka; 14C 12.9 ± 1.7 ka; 1σ external uncertainties), suggesting that most nuclides formed prior to the LGM were removed by erosion and that the boulder has a simple exposure history. Mount Mansfield’s mid-elevations were likely glaciated by warm-based, erosive ice, and hence isotopic concentrations record the timing of Latest Pleistocene deglaciation.
The higher elevations of Mount Mansfield (>1200) m are characterized by older 10Be ages but younger 14C ages. Five samples (all bedrock) have 10Be exposure ages ranging from 15.5 to 24.4 ka, forming a population statistically separable from the low-elevation samples. For the two samples in which we measured 14C and 10Be, there is a several-fold age difference (14C 10.2 ± 1.1 ka, 10Be 18.1 ± 1.5 ka; and 14C 8.5 ± 0.8 ka, 10Be 24.4 ± 2.0 ka, 1σ external uncertainties). The two summit 14C ages likely underestimate the true age of deglaciation of the mountaintop, perhaps due to post-glacial burial by snow/ice. The high 10Be ages likely represent inheritance of nuclides produced prior to the LGM due to shallow erosion depths, perhaps because Laurentide ice was frozen to the bed. Isotopic data suggest that the summit of Mount Mansfield likely experienced a complex interplay of glacial and periglacial processes.