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Newberyite

Cave Name:

Skipton (lavatube) Cave, Victoria, Australia

Speleothems:

  • loose tabular crystals with remnants of struvite in them

  • white, opac, compact powder after struvite

Frequency: Rare

Other geologic settings:

  • -

Other occurrence:

  • white crystalline coatings or crusts (Ficus, Boon and Crystal Caves, Transvaal, South Africa)

  • rose colored crust and thick flowstone (Gumburdek Cave, Bulgaria)

  • white wall popcorn (Gâuab Aas Cave, Namibia) or crust (Gcwihaba Cave, Namibia)

  • small hard nodules consisting of platy transparent crystals (Niah caves, Sarawak, Malaysia)

First description of cave occurrence:

  • vom Rath, G. 1879. Note sur deux nouveaux phosphates du guano. Bulletin de la Société Minéralogique de France 2: 79-82

First description of non-cave occurrence:

  • - 

Other cave locations & References:

  • Petrogale Cave, Western Australia

  • Ficus, Boon and Crystal Caves, Transvaal, South Africa

  • Gumburdek Cave, Bulgaria - Kolev, B & Shopov, Y.Y. 1992. The volcanic caves in Bulgaria. Geo2 (Geol. Geog. Sect., Natl. Speleol. Soc.) 19 (1): 22

  • Sul-Unkur cave, Khaidarkan, Kirghistan - Stepanov, V.I. 1971. Studies on the Khaidarkan caves, both hydrothermal and cold: in Velikii, A.S. et al. (eds.) Structural features and genetic sequences for some central Asian Hg-Sb depositions, Unpub. report, IMGRE All-Russian Geol. Found.: 184-220 (in Russian)

  • Gâuab Aas and Gcwihaba caves, Namibia - Martini, J.E. 1996. Contribution to the mineralogy of the caves of Gcwihaba Hills, northwestern Botswana. South African Speleol. Assoc. Bull. 36

  • Niah caves, Sarawak, Malaysia - Wilford, G.E. 1965. The geology of Sarawak and Sabah caves. Bull. Geol. Surv. Borneo, Malaysia 6: 1-181

Latitude: 37°44'13'' S

Longitude: 143°20'52''E

Water: No

Type of rock:

  • basalt 

IMA status: Approved

Group: Phosphates

Chemical formula:
[According to the official IMA-CNMNC List of Mineral Names (http://nrmima.nrm.se/imalist.htm)]

Mg(PO3OH) · 3H2O

Deposition and stability:

  • it derived from guano and basalt (which provided magnesium) (in Skipton Cave)

  • ussually it forms directly from guano solutions (in Niah caves, Malaysia)

  • less often, it is a decomposition product of struvite, due to the loss of ammonia

Color: white to light grey

Luster: dull

Hardness: 3

Chemical analysis:
  • P205 40.73; Fe203 0.85; Mn203 0.21; MgO 22.37; H20 35.84 (H20 - by diference)

Mineral assemblage:

  • + hannayite, struvite (Skipton Cave, Australia)

  • + biphosphammite (Petrogale Cave, Western Australia)

  • + taranakite (Sul-Unkur Cave, Kirghiztan)

  • + gypsum (Gcwihaba Cave, Namibia)

  • + variscite, vivianite, brushite (Niah caves, Malaysia)

Crystal system:
  • Orthorhombic
Cell parameter a (Å): 10.2096

Cell parameter b (Å): 10.6781

Cell parameter c (Å): 10.0096

Cell parameter α (Å): 90

Cell parameter β (Å): 90

Cell parameter γ (Å): 90



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Cave_mineral_ | by Dr. Radut