ENGINEERING GEOLOGY

The collapse of the Sella Zerbino gravity dam
Petaccia G, Lai CG, Milazzo C and Natale L
When a severe flood wave completely filled the Ortiglieto reservoir on August 13, 1935, the 14 m high "Sella Zerbino" secondary dam failed catastrophically causing > 100 casualties. Both of the dams, Sella Zerbino-Zerbino Saddle and Bric Zerbino-Zerbino Peak (Fig. 1) were overtopped but only the Sella Zerbino failed whereas the main barrage did not suffer any damage. The lawsuit that followed this tragic event ended with a full acquittal of the dam's designers since the plaintiff experts succeeded in demonstrating that the collapse was due to an extreme rainfall storm of unpredictable intensity. The case was then officially closed and still today the failure of the Sella Zerbino dam is attributed to the unpredictable hydrological event. Recently, Natale and Petaccia (2013) re-examined the case assessing the capacity of the flood spillways which equipped the Bric Zerbino dam. This paper thoroughly reviews the mechanics of the collapse of the Sella Zerbino dam focusing on the stability of the structure. The water pressure underneath the dam and the poor quality of the foundation rock is believed to have played a major role in the sequence of events that ended in the collapse of the barrage.
Mountain torrents: Quantifying vulnerability and assessing uncertainties
Totschnig R and Fuchs S
Vulnerability assessment for elements at risk is an important component in the framework of risk assessment. The vulnerability of buildings affected by torrent processes can be quantified by vulnerability functions that express a mathematical relationship between the degree of loss of individual elements at risk and the intensity of the impacting process. Based on data from the Austrian Alps, we extended a vulnerability curve for residential buildings affected by fluvial sediment transport processes to other torrent processes and other building types. With respect to this goal to merge different data based on different processes and building types, several statistical tests were conducted. The calculation of vulnerability functions was based on a nonlinear regression approach applying cumulative distribution functions. The results suggest that there is no need to distinguish between different sediment-laden torrent processes when assessing vulnerability of residential buildings towards torrent processes. The final vulnerability functions were further validated with data from the Italian Alps and different vulnerability functions presented in the literature. This comparison showed the wider applicability of the derived vulnerability functions. The uncertainty inherent to regression functions was quantified by the calculation of confidence bands. The derived vulnerability functions may be applied within the framework of risk management for mountain hazards within the European Alps. The method is transferable to other mountain regions if the input data needed are available.
9th Annual Report on the International Status of Engineering Geology-Year 2003-2004. Encompassing hydrogeology, environmental geology and the applied geosciences
Hatheway AW, Kanaori Y, Cheema T, Griffiths J and Promma K
The year began with additional evidence that global warming effects were bringing about unusual increases in free precipitation, as rain in greater amounts, but not as snow, in the mid latitudes of Europe and North America, setting new records for flooding. These effects surely will continue to magnify as practical concerns for Engineering Geologists, not the least of which will be slope instability. Worldwide, the profession appeared to be in a truly advanced state, as marked by a new high in indigenous practice, a broad base of authors in this journal, and of cooperation between practitioners of the various nations.