The city of Venice, Italy, has been subjected to periodic flooding, or acqua alta, for centuries. "Venice Shall Rise Again" presents a unique proposition to halt this flooding. Based on years of work and experiment, experts Gambolati and Teatini describe an innovative yet technologically simple, economically inexpensive, and environmentally friendly project to raise Venice by 25-30 cm over ten years by injecting seawater into 650-1000 m deep geological formations. This project would be conducted under conditions of absolute safety, stability and integrity conserving the unique artistic and architectural patrimony of this deeply beloved city. Beginning with a brief history of the Venetian Republic, "Venice Shall Rise Again" addresses the actions undertaken by Venice to protect the city and the lagoon from the sea and land attack for more than a millennium, including the MoSE project, a system of mobile barriers presently under construction. Detailed in its engineering details and ideas, but with enough background information and context to help the interested reader understand the concepts, this book will be of interest to all readers concerned about the fate of Venice.
Provides a history of the technical measures taken by the Venetian Republic to preserve the lagoon and the city or VeniceDetails technical specifications of a new method to secure Venice against periodic flooding

The Upper Adriatic Sea basin comprises a very precarious coastal environment subject to continuous changes which prove appreciable not only over the geological scale but also in historical and modern times. According to some Authors the Venice Lagoon was formed 2000-3000 years ago, and other lagoons (e. g. the Grado Lagoon in the northernmost part of the Adriatic) are even more recent. In addition to lagoons, the Upper Adriatic coastal area includes salt and fresh-water marshes and reclaimed land separated by several watercourses originating from the Alpine and Apennine ranges with a ground elevation not exceeding in many places 2 m above the mean sea l. evel (msl). A significant fraction of this lowland is already now below msl because of natural and anthropogenic land subsidence, land reclamation and sea level rise occurred over the last century. Natural land subsidence is still under way as a result of deep downward tec tonic movement and consolidation of soils deposited in the most recent time. An thropogenic subsidence is primarily due to groundwater pumping for agricultural, industrial, civil, and tourist use, and to gas withdrawal from a large number of gas fields scattered through the Upper Adriatic basin, and may still continue, al though at a reduced rate, in the years to come. At the same time msl is expected to rise in the next century due to global climate change, mainly because of the greenhouse effect.

The Upper Adriatic Sea basin comprises a very precarious coastal environment subject to continuous changes which prove appreciable not only over the geological scale but also in historical and modern times. According to some Authors the Venice Lagoon was formed 2000-3000 years ago, and other lagoons (e. g. the Grado Lagoon in the northernmost part of the Adriatic) are even more recent. In addition to lagoons, the Upper Adriatic coastal area includes salt and fresh-water marshes and reclaimed land separated by several watercourses originating from the Alpine and Apennine ranges with a ground elevation not exceeding in many places 2 m above the mean sea l. evel (msl). A significant fraction of this lowland is already now below msl because of natural and anthropogenic land subsidence, land reclamation and sea level rise occurred over the last century. Natural land subsidence is still under way as a result of deep downward tec tonic movement and consolidation of soils deposited in the most recent time. An thropogenic subsidence is primarily due to groundwater pumping for agricultural, industrial, civil, and tourist use, and to gas withdrawal from a large number of gas fields scattered through the Upper Adriatic basin, and may still continue, al though at a reduced rate, in the years to come. At the same time msl is expected to rise in the next century due to global climate change, mainly because of the greenhouse effect.