86 research outputs found
Landslides Triggered by the MW 7.8 14 November 2016 Kaikoura Earthquake, New Zealand
The MW 7.8 14 November 2016 Kaikoura earthquake generated more than 10000 landslides over a total area of about 10000 km2, with the majority concentrated in a smaller area of about 3600 km2. The largest landslide triggered by the earthquake had an approximate volume of 20 (±2) M m3, with a runout distance of about 2.7 km, forming a dam on the Hapuku River. In this paper, we present version 1.0 of the landslide inventory we have created for this event. We use the inventory presented in this paper to identify and discuss some of the controls on the spatial distribution of landslides triggered by the Kaikoura earthquake. Our main findings are (1) the number of medium to large landslides (source area ≥10000 m2) triggered by the Kaikoura earthquake is smaller than for similar sized landslides triggered by similar magnitude earthquakes in New Zealand; (2) seven of the largest eight landslides (from 5 to 20 x 106 m3) occurred on faults that ruptured to the surface during the earthquake; (3) the average landslide density within 200 m of a mapped surface fault rupture is three times that at a distance of 2500 m or more from a mapped surface fault rupture ; (4) the “distance to fault” predictor variable, when used as a proxy for ground-motion intensity, and when combined with slope angle, geology and elevation variables, has more power in predicting landslide probability than the modelled peak ground acceleration or peak ground velocity; and (5) for the same slope angles, the coastal slopes have landslide point densities that are an order of magnitude greater than those in similar materials on the inland slopes, but their source areas are significantly smaller
Asymptotic Pairs in Positive-Entropy Systems
We show that in a topological dynamical system (X;T ) of positive entropy there exist proper (positively) asymptotic pairs, that is, pairs (x; y) such that x 6= y and limn!+1 d(T y) = 0. More precisely we consider a T -ergodic measure of positive entropy and prove that the set of points that belong to a proper asymptotic pair is of measure 1. When T is invertible, the stable classes (i.e., the equivalence classes for the asymptotic equivalence) are not stable under T : for -almost every x there are uncountably many y that are asymptotic with x and such that (x; y) is a Li-Yorke pair with respect to . We also show that asymptotic pairs are dense in the set of topological entropy pairs
Compte rendu d'une réunion informelle (3 février 1994) concernant la recherche de personnes (RP) et le téléphone cellulaire (GSM)
P251: Validation de pratiques diagnostiques nutritionnelles en oncologie adulte et en ambulatoire
Resolving vibration in H+ + H2 charge transfer collisions
We measure the vibrational distribution of H2+ ions issued from charge transfer in H+ + H2 collisions to probe the details of the electron transfer mechanism from low to high impact energies. The experiments are accompanied by theoretical calculations. This joint experimental-theoretical study allows us to elicit the adequacy and accuracy of widely used assumptions in the description of molecular collisions
Les prélèvements de renards limitent-ils leur densité? La compensation par immigration, un concept clé pour comprendre l'impact des prélèvements sur les populations de renards
International audienc
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