Wakefieldite-(Y)

wakefieldite-(Y)

hellandite

montmorillonite

fergusonite

Images

Formula: Y(VO4)
Valence: Y(V5+O4)
Simple vanadate of yttrium, xenotime group
Crystal system: Tetragonal
Specific gravity: 4.25 calculated
Hardness: 5
Colour: Pale tan, yellow, canary-yellow, yellow-brown
Environments

Pegmatites

Localities

At the type locality, the Evans-Lou Mine, Lake Saint-Pierre, Saint-Pierre-de-Wakefield, Val-des-Monts, Les Collines-de-l'Outaouais RCM, Outaouais, Québec, Canada, the pegmatite has giant perthite-quartz at the centre and perthite-plagioclase quartz on the periphery. Fergusonite and hellandite were deposited before a period of brecciation and sometimes appear as fragments surrounded by quartz. Large crystals of pink microcline (up to 5 X 2 feet) and weathered allanite (up to 4 X 2 feet) appear on the quarry wall in the giant perthite-quartz zone. Also noted in this zone is an abundance of vugs up to several feet across that contain large quartz crystals (up to 7 lbs) commonly coated with montmorillonite, goethite or hematite. Of the accessory minerals on the dump, biotite, yttrium-bearing spessartine, allanite, hematite, goethite and fergusonite are the most common, probably in that order of abundance.
In the first-found specimen of wakefieldite taken from the dump, a pale tan mixture of wakefieldite, intimately associated with quartz and hellandite, and lesser amounts of kainosite-(Y) and montmorillonite, filled cavities in quartz in three sites on the specimen. Subsequently, canary-yellow wakefieldite was discovered at two locations within the quarry. At one, wakefieldite was associated with montmorillonite in vuggy quartz; yttrium-bearing fluorapatite and thorogummite were found nearby. At the other location, in the giant perthite-quartz zone, wakefieldite was mixed with montmorillonite in cavities in quartz near a cluster of fergusonite crystals. Fine-grained xenotime occurred a few inches away. Wakefieldite was found with montmorillonite in quartz in four additional specimens on the dump; in two of these specimens wakefieldite was intimately associated with hellandite (AM 56.395-410 as wakefieldite).
Wakefieldite-(Y) from the Evans-Lou Mine - Image

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