Articles | Volume 2, issue 2
https://doi.org/10.5194/gchron-2-411-2020
https://doi.org/10.5194/gchron-2-411-2020
Research article
 | 
16 Dec 2020
Research article |  | 16 Dec 2020

Calibrating a long-term meteoric 10Be delivery rate into eroding western US glacial deposits by comparing meteoric and in situ produced 10Be depth profiles

Travis Clow, Jane K. Willenbring, Mirjam Schaller, Joel D. Blum, Marcus Christl, Peter W. Kubik, and Friedhelm von Blanckenburg

Viewed

Total article views: 2,892 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,938 803 151 2,892 391 150 192
  • HTML: 1,938
  • PDF: 803
  • XML: 151
  • Total: 2,892
  • Supplement: 391
  • BibTeX: 150
  • EndNote: 192
Views and downloads (calculated since 30 Apr 2020)
Cumulative views and downloads (calculated since 30 Apr 2020)

Viewed (geographical distribution)

Total article views: 2,892 (including HTML, PDF, and XML) Thereof 2,719 with geography defined and 173 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 29 Jul 2026
Download
Short summary
Meteoric beryllium-10 concentrations in soil profiles have great capacity to quantify Earth surface processes, such as erosion rates and landform ages. However, determining these requires an accurate estimate of the delivery rate of this isotope to local sites. Here, we present a new method to constrain the long-term delivery rate to an eroding western US site, compare it against existing delivery rate estimates (revealing considerable disagreement between methods), and suggest best practices.
Share