Sharp crystals of Veszelyite to 3mm on Hemimorphite lined vugs in matrix. Lots and lots of Veszelyite crystals all over the ridges and vugs. Veszelyite is a rare phosphate mineral only found in a few places worldwide as collectable mineral specimens. These specimens have only been found in the past few years and are one of the more interesting mineral surprises from China.

Sharp crystals of Veszelyite to 9mm lining vugs in matrix. Veszelyite is a rare phosphate mineral only found in a few places worldwide as collectable mineral specimens. These specimens have only been found in the past few years and are one of the more interesting mineral surprises from China.

Bright blue, velvety spheres to 5mm of Azurite against a pale blue/grey matrix. Visually stunning contrast between the spheres and the lighter matrix background. Ex. Mark Hay collection. Saw cut on back.

Powder blue spheres of Rosasite on the sides and within a protected vug in the specimen. Gorgeous and undamaged, this competition quality specimen is similar to the example shown on the cover of the 2nd addition of Minerals of Arizona. High quality and undamaged Rosasite from here are rare. To Bruce Murphy via the Arkenstone who acquired it in 2005 from the Ernie Schlichter collection.

Vug filled with chocolate brown, curving Vanadinite crystals. Crystals of this size are very rare from this obscure locality near Tombstone, Arizona. Ex. Ann Williams collection, acquired by Bruce Murphy in 2007. Fine and undamaged specimen thought to be collected in the early 1930’s. Specimens from the Gallagher Mine are rarely seen on the market and this one may be the best extent.

White Calcite crystals on matrix. Main crystal is 2.5cm and double-terminated. From a very unusual and relatively unknown locality.

Large cluster of Azurite from the famous Chessy mines of France. These mines are long closed and I understand these specimens were found in the 1800s. This specimen is out of an old collection built in the 1960s and 70s and has minor amounts of attached Malachite.