2014-07-15T07:30:04Z
2014-07-15T07:30:04Z
2004
2014-07-15T07:30:05Z
Historical data about ancient avalanches are scarce in the Pyrenees. Dendrochronology can provide new data about past avalanches and their return period, but up to now little research has been carried out with this purpose. The Aludex project aims to obtain information about the frequency and extent of extreme avalanches, using a dendrochronological and a nivo-meteorological approach. In this paper, we present the results of a dendrochronological study of the Canal del Roc Roig avalanche path which was affected by two extreme avalanches in February 1996. This first dendrochronological study has permitted us to assess the tree-ring signals due to avalanche events in 53 out of 132 dated trees. The trees presented a variety of responses to the 1996 avalanche events. It is shown that the type of tree-ring signal depends on tree age. The methodology has proved successful in detecting the 1996 and 1972 documented avalanche events, and provided outstanding evidence of undocumented past events such as one in 1930.
Article
Published version
English
Allaus; Dendrocronologia; Pirineu axial; Pins; Avalanches; Dendrochronology; Central Pyrenees; Pine
International Glaciological Society
Reproducció del document publicat a: http://dx.doi.org/10.3189/172756404781815077
Annals of Glaciology, 2004, vol. 38, num. 1, p. 173-179
http://dx.doi.org/10.3189/172756404781815077
(c) International Glaciological Society., 2004