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Bagni Marii thermal spring concession, Rapolano Terme, Siena Province, Tuscany, Italyi
| Regional Level Types | |
|---|---|
| Bagni Marii thermal spring concession | Mining Concession (Active) |
| Rapolano Terme | Commune |
| Siena Province | Province |
| Tuscany | Region |
| Italy | Country |
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Area:
1.0 km2
Type:
Mining Concession (Active) - last checked 2026
Mining concession for thermal waters called “Bagni Marii”
The concession pertains to the Bagni Marii spring, which supplies the San Giovanni spa. Prior to the construction of Well 1 (named "Sorgente"), thermal water was collected through an infrastructure located atop the "travertine ridge". This system consisted of a subsurface pipeline and a surface collection well, referred to as "Acqua della Rupe."
Well 1 was established in 1954 within the plant premises, originally reaching a depth of approximately 17 meters. Subsequent cleaning and deepening operations performed in 2004 extended its depth to around 25 meters (see Fig. 5.2). The well is artesian, with a water temperature of about 40°C. It is lined to a depth of roughly 8 meters with an 8-cm diameter pipe. This narrow lining facilitates the natural ascent of thermal fluids, driven by a high concentration of dissolved gases. The well likely taps into a fracture that serves as a conduit for both thermal water and gas, with the gas assisting in elevating the water to the surface. The source is protected by glass.
Routine maintenance, typically conducted every decade, involves inserting equipment into the casing to clean the well walls. This temporarily reduces the flow section, subsequently restoring the original extraction efficiency.
The well demonstrates stable flow rates over time, unaffected by seasonal changes. The discharge at the wellhead exhibits a consistent cyclical pattern, alternating between minimum and maximum values. The thermal water is characterized by elevated CO₂ content; therefore, the protective glass structure is specifically designed to mitigate risks to living organisms. To ensure safety, the enclosure must remain open with a designated outlet at the top.
Routine maintenance, typically conducted every decade, involves inserting equipment into the casing to clean the well walls. This temporarily reduces the flow section, subsequently restoring the original extraction efficiency.
The well demonstrates stable flow rates over time, unaffected by seasonal changes. The discharge at the wellhead exhibits a consistent cyclical pattern, alternating between minimum and maximum values. The thermal water is characterized by elevated CO₂ content; therefore, the protective glass structure is specifically designed to mitigate risks to living organisms. To ensure safety, the enclosure must remain open with a designated outlet at the top.
The designated perimeter delineates the concession area, while the point coordinates (lat="43.279843106878" long="11.591002602909") identify the location of Well 1, "Sorgente."
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Standard Detailed Gallery Strunz Chemical ElementsMineral List
Mineral list contains entries from the region specified including sub-localities1 valid mineral.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Rock list contains entries from the region specified including sub-localities
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Alphabetical List Tree DiagramGallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 5 - Nitrates and Carbonates | |||
|---|---|---|---|
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
List of minerals for each chemical element
| C | Carbon | |
|---|---|---|
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Calcite | CaCO3 |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
Geochronology
Mineralization age: Quaternary : 0.00324 ± 0.00055 Ma to 0 MaImportant note: This table is based only on rock and mineral ages recorded on mindat.org for this locality and is not necessarily a complete representation of the geochronology, but does give an indication of possible mineralization events relevant to this locality. As more age information is added this table may expand in the future. A break in the table simply indicates a lack of data entered here, not necessarily a break in the geologic sequence. Grey background entries are from different, related, localities.
| Geologic Time | Rocks, Minerals and Events | ||||||
|---|---|---|---|---|---|---|---|
| Phanerozoic | |||||||
| Cenozoic | |||||||
| Quaternary | |||||||
| Anthropocene |
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| Holocene |
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Fossils
This region is too big or complex to display the fossil list, try looking at smaller subregions.Localities in this Region
- Tuscany
- Siena Province
- Rapolano Terme
- Bagni Marii thermal spring concession
- Rapolano Terme
- Siena Province
Other Regions, Features and Areas that Intersect
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References
Bambini, Anna Maria; Brogi, Andrea; Cornamusini, Gianluca; Costantini, Armando; Foresi, Luca Maria; Lazzarotto, Antonio (2010) Geologia dell’area di Rapolano Terme in Provincia di Siena (Appennino Settentrionale) [Geological setting of the Rapolano Terme area (Siena, Northern Apennines)]. Italian Journal of Geosciences (Boll.Soc.Geol.It.), 129 (3). 457-495 doi:10.3301/ijg.2010.12