Moraine chronosequence of the Donnelly Dome region, Alaska

A. Matmon*, J. P. Briner, G. Carver, P. Bierman, R. C. Finkel

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

24 Scopus citations


We present 10Be exposure ages from moraines in the Delta River Valley, a reference locality for Pleistocene glaciation in the northern Alaska Range. The ages are from material deposited during the Delta and Donnelly glaciations, which have been correlated with MIS 6 and 2, respectively. 10Be chronology indicates that at least part of the Delta moraine stabilized during MIS 4/3, and that the Donnelly moraine stabilized ~17ka. These ages correlate with other dates from the Alaska Range and other regions in Alaska, suggesting synchronicity across Beringia during pulses of late Pleistocene glaciation. Several sample types were collected: boulders, single clasts, and gravel samples (amalgamated small clasts) from around boulders as well as from surfaces devoid of boulders. Comparing 10Be ages of these sample types reveals the influence of pre/post-depositional processes, including boulder erosion, boulder exhumation, and moraine surface lowering. These processes occur continuously but seem to accelerate during and immediately after successive glacial episodes. The result is a multi-peak age distribution indicating that once a moraine persists through subsequent glaciations the chronological significance of cosmogenic ages derived from samples collected on that moraine diminishes significantly. The absence of Holocene ages implies relatively minor exhumation and/or weathering since 12ka.

Original languageAmerican English
Pages (from-to)63-72
Number of pages10
JournalQuaternary Research
Issue number1
StatePublished - Jul 2010


  • Alaska
  • Cosmogenic exposure ages
  • Delta
  • Donnelly
  • Moraines


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