Toirano cave system, Toirano, Savona Province, Liguria, Italyi
| Regional Level Types | |
|---|---|
| Toirano cave system | Group of Caves |
| Toirano | Commune |
| Savona Province | Province |
| Liguria | Region |
| Italy | Country |
This page is currently not sponsored. Click here to sponsor this page.
Latitude & Longitude (WGS84):
44° 8' 16'' North , 8° 12' 7'' East
Latitude & Longitude (decimal):
Type:
Group of Caves
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Toirano | 2,430 (2014) | 1.2km |
| Boissano | 2,184 (2014) | 1.6km |
| Morteo | 249 (2014) | 2.7km |
| Pineland | 160 (2014) | 2.8km |
| Balestrino | 387 (2014) | 2.9km |
The Toirano cave system is located in the Varatella Valley, to the north of Toirano, and develops in dolostones and dolomitic limestones of the San Pietro ai Monti Formation (Triassic). From the lower (186 m a.s.l.) to the upper level (247 m a.s.l.), the caves are organised as follows: Básura (see coordinates), Santa Lucia Inferiore, Santuario, and Colombo.
Phosphates have been found and sampled only in the highest level of Colombo, which is a horizontal 310 m-long cave. Here, important bat guano deposits and associated intense condensation-corrosion features show that bats have used this cave for a long time. The cave is of archeological interest, as are most of the caves in the area, and guanodeposits have been trenched by scientific excavations.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
6 valid minerals.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 5 - Nitrates and Carbonates | |||
|---|---|---|---|
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Aragonite | 5.AB.15 | CaCO3 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Gypsum | 7.CD.40 | CaSO4 · 2H2O |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Newberyite | 8.CE.10 | Mg(PO3OH) · 3H2O |
| ⓘ | Ardealite | 8.CJ.50 | Ca2(PO3OH)(SO4) · 4H2O |
| ⓘ | Brushite | 8.CJ.50 | Ca(PO3OH) · 2H2O |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Ardealite | Ca2(PO3OH)(SO4) · 4H2O |
| H | ⓘ Brushite | Ca(PO3OH) · 2H2O |
| H | ⓘ Gypsum | CaSO4 · 2H2O |
| H | ⓘ Newberyite | Mg(PO3OH) · 3H2O |
| C | Carbon | |
| C | ⓘ Aragonite | CaCO3 |
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Aragonite | CaCO3 |
| O | ⓘ Ardealite | Ca2(PO3OH)(SO4) · 4H2O |
| O | ⓘ Brushite | Ca(PO3OH) · 2H2O |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Gypsum | CaSO4 · 2H2O |
| O | ⓘ Newberyite | Mg(PO3OH) · 3H2O |
| Mg | Magnesium | |
| Mg | ⓘ Newberyite | Mg(PO3OH) · 3H2O |
| P | Phosphorus | |
| P | ⓘ Ardealite | Ca2(PO3OH)(SO4) · 4H2O |
| P | ⓘ Brushite | Ca(PO3OH) · 2H2O |
| P | ⓘ Newberyite | Mg(PO3OH) · 3H2O |
| S | Sulfur | |
| S | ⓘ Ardealite | Ca2(PO3OH)(SO4) · 4H2O |
| S | ⓘ Gypsum | CaSO4 · 2H2O |
| Ca | Calcium | |
| Ca | ⓘ Aragonite | CaCO3 |
| Ca | ⓘ Ardealite | Ca2(PO3OH)(SO4) · 4H2O |
| Ca | ⓘ Brushite | Ca(PO3OH) · 2H2O |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Gypsum | CaSO4 · 2H2O |
Other Regions, Features and Areas containing this locality
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.
References
Audra, Philippe, De Waele, Jo, Bentaleb, Ilham, Chroňáková, Alica, Krištůfek, Václav, D’Angeli, Ilenia, Carbone, Cristina, Madonia, Giuliana, Vattano, Marco, Scopelliti, Giovanna, et al. (2019) Guano-related phosphate-rich minerals in European caves. International Journal of Speleology, 48 (1). 75-105 doi:10.5038/1827-806x.48.1.2252