Canavesite
A variety of Minerals
What is Canavesite?
Canavesite, Mg2(HBO3)(CO3)∙5H2O, is a rare carboborate mineral from the abandoned Brosso mine in Italy. Canavesite is a secondary mineral that occurs due to the weathering of ludwigite-magnetite skarn on the surface of mine walls. The physical properties consist of milky-white rosette-like aggregates of elongated transparent fibers shown in figure one. It has the crystal symmetry of a monoclinic with a diffraction symbol of 2/mP-/-.
Market Value Factors
Pricing varies for every rock and mineral, so use these universal factors to gauge Canavesite before comparing listings or appraisals.
Size & Weight
Larger, intact specimens usually command higher prices.
Rarity & Demand
Scarce material or popular varieties sell at a premium.
Condition & Finish
Chips, repairs, and heavy wear lower value; clean prep helps.
Treatment & Provenance
Untreated specimens with documented locality are prized.
Canavesite Localities Map
See where Canavesite is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.
Key Characteristics
Characteristics of Canavesite
Canavesite occurs as a milky rosette-like aggregates of very thin [010] elongated fibers on surfaces and along fractures of ludwigite and magnetite skarns. Canavesite is an exceptionally rare secondary mineral that forms on the walls of the abandoned mine of Brosso, Italy and has formed since the mine was abandoned due to weathering of these ludwigite and magnetite skarns. Canvesite has a monoclinic P 2/m crystal structure and does not fluoresce under an ultraviolent light. It also has thin and slightly flexible vitreous fibers that are elongated parallel to [010]. Some crystal may show pseudohexagonal prismatic habit, but these cases are rare. The X-ray powder diffraction pattern strongest lines are 9.54(100)202, 8.12(40)(201), 7.80(18)(102,301), 4.56(21)(501,503), and 3.11(19)(407).
Formation of Canavesite
The Vola Gera tunnel in the Brosso mine is located in a village northwest of Ivrea, Piedmont, Italy in Canavese district. The mine was initially a pyrite mine but it was abandoned. It is a well known mine for fine minerals that build up between the zone where monzonite stock and marbles interbedded in the mica schists of the Sesia-Lanzo zone. Mineralization of boron within magnetite skarns were first reported by Giussani and Vighi in 1964. There has since been more canavesite discovered in New Jersey at the Sterling Mine. They are the only two places that have been known to produce the secondary mineral.
Composition of Canavesite
Canavesite has the chemical formula Mg2(HBO3)(CO3)∙5H2O, which makes it a carboborate mineral. Having two complete chemical analyses and one partial gives MgO (31.06),B2O3(12.70),CO2(18.57)H2O(37.44) and MgO (31.18),B2O3(13.47),CO2(17.02)H2O(38.33) in weight % oxides. Taking eleven oxygen ions, one can calculate from this data the empirical formula is as followed Mg2.03(HBO3)1.09(CO3)∙4.91H2O. A canavestie infrared spectrum is unlike that of well known families. It has bands near 3500, 1450, and 1000 cm-1 looks almost like OH. With a dilute HCl at or near room temperature canavestie will produce tiny bubbles of gas and foam with hissing sounds. The molecular formula has not been obtained for canavesite. The approximate density was obtained using the heavy liquid method, which shows a density of 1.8 g cm.
Quick Facts
Chemical Properties
- Chemical Formula
- Mg2(HBO3)(CO3) · 5H2O
- Elements
- B, C, H, Mg, O
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Canavesite FAQs
What is the characteristics of canavesite of Canavesite?
Canavesite occurs as a milky rosette-like aggregates of very thin [010] elongated fibers on surfaces and along fractures of ludwigite and magnetite skarns. Canavesite is an exceptionally rare secondary mineral that forms on the walls of the abandoned mine of Brosso, Italy and has formed since the mine was abandoned due to weathering of these ludwigite and magnetite skarns. Canvesite has a monoclinic P 2/m crystal structure and does not fluoresce under an ultraviolent light. It also has thin and slightly flexible vitreous fibers that are elongated parallel to [010]. Some crystal may show pseudohexagonal prismatic habit, but these cases are rare. The X-ray powder diffraction pattern strongest lines are 9.54(100)202, 8.12(40)(201), 7.80(18)(102,301), 4.56(21)(501,503), and 3.11(19)(407).
What is the formation of canavesite of Canavesite?
The Vola Gera tunnel in the Brosso mine is located in a village northwest of Ivrea, Piedmont, Italy in Canavese district. The mine was initially a pyrite mine but it was abandoned. It is a well known mine for fine minerals that build up between the zone where monzonite stock and marbles interbedded in the mica schists of the Sesia-Lanzo zone. Mineralization of boron within magnetite skarns were first reported by Giussani and Vighi in 1964. There has since been more canavesite discovered in New Jersey at the Sterling Mine. They are the only two places that have been known to produce the secondary mineral.
What is the composition of canavesite of Canavesite?
Canavesite has the chemical formula Mg2(HBO3)(CO3)∙5H2O, which makes it a carboborate mineral. Having two complete chemical analyses and one partial gives MgO (31.06),B2O3(12.70),CO2(18.57)H2O(37.44) and MgO (31.18),B2O3(13.47),CO2(17.02)H2O(38.33) in weight % oxides. Taking eleven oxygen ions, one can calculate from this data the empirical formula is as followed Mg2.03(HBO3)1.09(CO3)∙4.91H2O. A canavestie infrared spectrum is unlike that of well known families. It has bands near 3500, 1450, and 1000 cm-1 looks almost like OH. With a dilute HCl at or near room temperature canavestie will produce tiny bubbles of gas and foam with hissing sounds. The molecular formula has not been obtained for canavesite. The approximate density was obtained using the heavy liquid method, which shows a density of 1.8 g cm.
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