The geological map of the Bagnoli-Agnano reclamation area was produced by Bonaventura Montani in 1856 with the purpose to assist in the reclamation project of the Agnano Lake area, which was plagued by unhealthy conditions and endemic malaria. The Phlegraean Fields are a volcanic region renowned for its susceptibility to cataclysmic events and high population density, which major eruptions took place approximately 39,000 and 14,500 years ago. Montani provided information about the nature of the volcanic rocks and the previous existence of marine deposits in the Bagnoli plain, excluding the presence of peat deposits in the underground, also through the drilling of seven geognostic boreholes. Based on geological observation, Montani proposed an optimal route for the drainage channel of Agnano Lake, thereby avoiding the challenging task of perforating the trachitic lava bodies of Accademia and Monte Olibano. He demonstrated that the diffuse gas emissions in the region had a volcanic origin and were not the primary cause of illnesses among the local peasants, which he related to the fermentation of plants processed on the shores of Agnano Lake. The reclamation of the Agnano Lake area was subsequently completed in 1870 after the Unification of Italy.
The geognostic map of Phlegraean Fields by Bonaventura Montani (1856). The Bagnoli-Agnano reclamation area / Fabbi, Simone; Console, Fabiana; Pantaloni, Marco; Principe, Claudia. - In: RENDICONTI ONLINE DELLA SOCIETÀ GEOLOGICA ITALIANA. - ISSN 2035-8008. - 62:(2024), pp. 89-102. [10.3301/rol.2024.10]
The geognostic map of Phlegraean Fields by Bonaventura Montani (1856). The Bagnoli-Agnano reclamation area
Fabbi, Simone
Primo
;
2024
Abstract
The geological map of the Bagnoli-Agnano reclamation area was produced by Bonaventura Montani in 1856 with the purpose to assist in the reclamation project of the Agnano Lake area, which was plagued by unhealthy conditions and endemic malaria. The Phlegraean Fields are a volcanic region renowned for its susceptibility to cataclysmic events and high population density, which major eruptions took place approximately 39,000 and 14,500 years ago. Montani provided information about the nature of the volcanic rocks and the previous existence of marine deposits in the Bagnoli plain, excluding the presence of peat deposits in the underground, also through the drilling of seven geognostic boreholes. Based on geological observation, Montani proposed an optimal route for the drainage channel of Agnano Lake, thereby avoiding the challenging task of perforating the trachitic lava bodies of Accademia and Monte Olibano. He demonstrated that the diffuse gas emissions in the region had a volcanic origin and were not the primary cause of illnesses among the local peasants, which he related to the fermentation of plants processed on the shores of Agnano Lake. The reclamation of the Agnano Lake area was subsequently completed in 1870 after the Unification of Italy.File | Dimensione | Formato | |
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