GLORIETA MOUNTAIN PALLASITE — A SUPERB COMPLETE SLICE FROM THE SCHONER MASS
Lot 54

GLORIETA MOUNTAIN PALLASITE — A SUPERB COMPLETE SLICE FROM THE SCHONER MASS

Stony-Iron – PAL-ANOMGlorieta Mountain, New Mexico

Closed19 October 2016

Price Realised

GBP 7,500

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GLORIETA MOUNTAIN PALLASITE — A SUPERB COMPLETE SLICE FROM THE SCHONER MASS
Stony-Iron – PAL-ANOM
Glorieta Mountain, New Mexico
This specimen features the signature sulfide inclusions of this meteorite along with crystals of olivine and peridot (the semi-precious birthstone of August) suspended in a highly polished metallic matrix. This is among the finest complete slices of the Glorieta Mountain pallasite known to exist.
203 x 169 x 3mm (8 x 6 2/3 x 1/8in.)
357g

Steve Schoner Meteorite Collection, Clyde Tombaugh House, Flagstaff, Arizona

Specialist note

The complete slice of Glorieta Mountain now offered was adjacent to the slice whose image served as the frontispiece of the Cambridge Encyclopedia of Meteorites. Less than 0.2% of all meteorites are pallasites — the most resplendent of all meteorites — and Glorieta Mountain is the most famous American pallasite. In 1965 the "Father of Meteoritics", Harvey Nininger, befriended a teenaged Steve Schoner and informed him of the small meteorites found on Glorieta Mountain in northern New Mexico. Years later, Schoner's recovery of tiny pallasitic fragments fueled his belief in the existence of a far larger mass — a Holy Grail to meteorite enthusiasts. After seventy searches of two to three weeks each over a period of 15 years, Schoner's efforts finally paid off. The stunning specimen now offered is from the 20 kg meteorite recovered by Schoner. As a result of the material lost from cutting, grinding and polishing, only 11 kg of fine specimens from this historic mass exist. While pallasites are extremely rare, Glorieta Mountain is rarer still because it is chemically and morphologically anomalous. It also has a relatively high abundance of iron sulfide (the mineral troilite), leading researchers to classify Glorieta as an anomalous member of the main pallasite group.