Erosion by cooling

David Lundbek Egholm ()
Additional contact information
David Lundbek Egholm: Aarhus University, 8000 Aarhus, Denmark.

Nature, 2013, vol. 504, issue 7480, 380-381

Abstract: The thermal history of thousands of rock samples convincingly confirms the idea that climate cooling accelerates the rate of erosion at Earth's surface — and implicates glaciers in particular. See Letter p.423

Date: 2013
References: Add references at CitEc
Citations:

Downloads: (external link)
https://www.nature.com/articles/504380a Abstract (text/html)
Access to the full text of the articles in this series is restricted.

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:504:y:2013:i:7480:d:10.1038_504380a

Ordering information: This journal article can be ordered from
https://www.nature.com/

DOI: 10.1038/504380a

Access Statistics for this article

Nature is currently edited by Magdalena Skipper

More articles in Nature from Nature
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().