Location | Name | CHX | CHY | Lat. | Lon. |
Visp (VS) | 631,735 | 119,923 | 46.32 | 7.85 | |
Date/time (UTC) | July 25, 1855 | 11:50 a.m. | |||
Intensity | Epicentral intensity (Io): VIII | Maximum intensity (Ix): VIII | |||
Magnitude (Mw) | 6.2 | ||||
Effects | Primary: known | Secondary: known | |||
Level of documentation | This is an outstandingly well-documented event, particularly with respect to primary effects, since a contemporary damage assessment is preserved completely. In combination with available statistical data (population, building stock and prizes) a quantification of the losses was feasible | ||||
Remarks | Strong aftershock on July 26, 1855 (Io: VIII, Ix: VIII) caused further primary effects and triggered mass movements. Epicenter at 634,050/119,935 (46.23/7.88) For historic sources and quotations see Online Resource 1 and Fritsche (2008) | ||||
References | Fritsche et al. 2006 Fritsche 2008 Gisler et al. 2008b Gisler and Fäh 2011 |