Gypsum is an important raw material for constructions and other industrial sectors. In Piedmont (NW Italy), main gypsum bodies are located in the Monferrato area, where large open pits and underground quarries are present. The gypsum-bearing formation outcropping in this area shows typical geological, structural and hydrogeological features, which affect the quarrying and the related interaction with natural phenomena, human activities and land use. In particular, gypsum karst has considerable influence on mining operations, as well as mining operations can produce strong impact on gypsum karst. In Monferrato, a specific case of interaction between the quarrying activity and geological, hydrogeological and territorial setting is represented by the event of water inrush that happened in the Moncalvo underground quarry in association to the development of a surface sinkhole phenomenon.

Subsidence hazard connected to quarrying activities in a karst area:a case of the Moncalvo sinkhole event (Piedmont, NW Italy)

BONETTO, SABRINA MARIA RITA;
2008-01-01

Abstract

Gypsum is an important raw material for constructions and other industrial sectors. In Piedmont (NW Italy), main gypsum bodies are located in the Monferrato area, where large open pits and underground quarries are present. The gypsum-bearing formation outcropping in this area shows typical geological, structural and hydrogeological features, which affect the quarrying and the related interaction with natural phenomena, human activities and land use. In particular, gypsum karst has considerable influence on mining operations, as well as mining operations can produce strong impact on gypsum karst. In Monferrato, a specific case of interaction between the quarrying activity and geological, hydrogeological and territorial setting is represented by the event of water inrush that happened in the Moncalvo underground quarry in association to the development of a surface sinkhole phenomenon.
2008
57
125
134
BONETTO S.; FIORUCCI A.; FORNARO M.; VIGNA B.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2318/101774
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