Hydrology and hillslope processes explain spatial variation in tree-ring responses to the 1983 earthquake at Borah Peak, Idaho, USA

Author:

Bekker Matthew F.1ORCID,Metcalf Douglas P.2,Harley Grant L.3ORCID

Affiliation:

1. Department of Geography, 690 KMBL; Brigham Young University; Provo UT 84602 USA

2. Department of Geological Sciences, S389 ESC; Brigham Young University; Provo UT 84602 USA

3. Department of Geography; University of Idaho; 875 Perimeter Drive, MS 3021 Moscow ID 83844 USA

Publisher

Wiley

Subject

Earth and Planetary Sciences (miscellaneous),Earth-Surface Processes,Geography, Planning and Development

Reference65 articles.

1. Dendrochronological interpretation of geomorphic process;Alestalo;Fennia,1971

2. Immediate damage by an earthquake to a temperate montane forest;Allen;Ecology,1999

3. Comparison of the 1959 Hebgen Lake, Montana and the 1983 Borah Peak, Idaho, earthquakes from geodetic observations;Barrientos;Bulletin of the Seismological Society of America,1987

4. Spatial variation in the response of tree rings to normal faulting during the Hebgen Lake Earthquake, southwestern Montana, USA;Bekker;Dendrochronologia,2004

5. Tree Rings and Earthquakes

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