Three Occurrences of Oregon Sunstone

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Three Occurrences of Oregon Sunstone

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Oregon Sunstones are so special, and I'm very pleased that Pala did a spread on them this month that included this article from GIA, among other things. The sunstones I have came from the Dust Devil mine since I was at an ISG chat when Don Buford offered a deal on faceted champagne sunstones that a group of us got together and went in on, plus I have a piece of rough with red in the center from there that Robert James sent me.

I think you'll agree with me that the first faceted sunstone in the article is simply breathtaking, and it's stones like that that make me hope that someday I'll get out to these mines to try my own hand at finding such a beauty to have cut for me; if I can drag John along with me since he knows some of these people. 8-)

One caveat though. This is the gemstone that was the target of the shake 'n baked fraudulent stones trying to be passed off as Tibetan sunstones during what I call the scamdesine fiasco some years ago, which any of you aren't unaware of can read about here viewtopic.php?f=9&t=4198&p=17130&hilit=Gobsmacked#p17130

The fake stones are still out there. I know because I bought one or two when the 'Olympic sunstones' hit the market, which I kept for comparison with genuine Oregon sunstones, so if you're looking to buy any I suggest you buy from the mines directly, or from reputable sellers such as our own r2d, who often has some lovely specimens up for sale at great prices. ... and before you ask, no, I don't get a kickback for recommending him, but I have bought gemstones from him so I know I can safely direct you his way. Now on to the article. Enjoy! :)

Three Occurrences of Oregon Sunstone
Duncan Pay, Robert Weldon, Shane McClure, and Kevin Schumacher

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Figure 1. The sparsely populated high desert of eastern Oregon is home to three localities producing natural copper-bearing labradorite feldspar. In this view of Lake County’s Dust Devil mine, the local source of the sunstone-bearing lavas is the group of rounded hills (Dudeck Ridge) in the background. Photo by Robert Weldon.

ABSTRACT

"Over five days in late July 2013, we visited three important sources of gem-quality sunstone in eastern Oregon: the Ponderosa mine in Harney County, and the Dust Devil (figure 1) and Sunstone Butte mines, both of which are about 120 miles further south, in Lake County.


INTRODUCTION

Oregon sunstone, the official state gemstone since 1987, is natural copper-bearing labradorite feldspar. Some examples exhibit red to green dichroism, and fine specimens (figure 2) larger than 5 ct can sell for more than $1,000 per carat.

Feldspars are silicate minerals that contain variable amounts of sodium (Na), potassium (K), and calcium (Ca). Labradorite belongs to the plagioclase feldspar series, which forms a solid solution between anorthite (CaAl2Si2O8) and albite (NaAlSi3O8). Oregon sunstone, which contains substantially more calcium than sodium, has a composition of about 70% anorthite and 30% albite, or An70/Ab30. For more on feldspar classification and nomenclature, see box B in Rossman (2011).

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Figure 2. This superb 2.85 ct sunstone from Sunstone Butte displays the gem’s most valued attributes: a blend of green and red bodycolor, with reflective spangles of native copper glittering in the interior. Photo by Robert Weldon.

No discussion of this topic would be complete without mention of the controversy surrounding treated copper-bearing feldspar; Rossman (2011) provides a chronology. In the early 2000s, Asian treaters perfected a method of diffusing copper into pale feldspar, flooding the market with low-priced, attractive red and green gems—which destabilized the market for Oregon sunstone. Promoted as “andesine” and purportedly from mines in Congo or Tibet, this material was subsequently found to be treated, but the resulting furor hindered the public’s trust in natural copper-bearing feldspar. Despite this setback, Oregon sunstone miners have strived to rebuild the market, and there are signs of renewed consumer interest in their one-of-kind gem.

TRIP OBJECTIVES

This paper incorporates trip findings and previous GIA research to provide a comparative analysis of the gem materials and their geological context and history. We also hope to initiate research that will answer some open questions:

Are all the eastern Oregon sunstone occurrences the same age?
How do sunstone occurrences correlate with the local geology?
How did the very uneven color distribution develop in fractured crystals?
Are sunstones from each of the three mines distinguishable?

In 2006, GIA collected gems from the Ponderosa and Dust Devil mines to characterize natural Oregon sunstone and help distinguish it from treated material (McClure, 2009). For the present study, we collected representative suites of gem materials and rock samples from each mine, documenting the GPS coordinates of each find. By performing argon-argon (40Ar/39Ar) dating on basalt samples and labradorite feldspar crystals from the Ponderosa mine, we hope to confirm the age of its sunstone-bearing basalt and compare that to the Lake County mining locations. We also intend to perform petrographic analyses to characterize the gem-bearing rocks from each deposit and determine their context within the surrounding geology.

We intend to publish the results of these studies in a future G&G feature article and on the GIA website.

LOCATION AND ACCESS

Past stratovolcanoes of the High Cascades and across Oregon’s remote High Lava Plains lie three sunstone mines (figure 3). All three produce labradorite feldspar ranging from near-colorless to pale yellow to red and green, including bicolor specimens. The sunstone often contains tiny reflective platelets of native copper, referred to as “schiller.”

Image
Figure 3. This map shows the location of the three mines visited in eastern Oregon. Illustration by Larry Lavitt.

From Portland, we drove five hours southeast to Ponderosa, near the town of Burns. We spent three days there before driving three hours southwest to spend the next two days at the Dust Devil and Sunstone Butte mines. These deposits are referred to in the literature as the Lakeview, Lake County, Plush, or Rabbit Basin occurrences.

GEOLOGIC CONTEXT

In eastern Oregon, sunstone occurs as phenocrysts in highly porphyritic basalt flows (see figure 4). They are a minor but fascinating part of the region’s recent geologic history, likely originating during an episode of widespread basaltic volcanism that occurred 15–17 million years ago (Ma), during the Miocene epoch. Geologists debate whether the volcanic events were caused by melting of subducted oceanic crust or by a hot plume in the earth’s mantle. The Steens Basalt of the Oregon Plateau (figure 5), where volcanic flow deposits can contain up to 50% large feldspar crystals (Walker, 1979), erupted around the same time as the more extensive Columbia River basalts further north. 40Ar/39Ar dating indicates the eruptions took place between 15.51 +/- 0.28 Ma and 16.59 +/- 0.10 Ma (Brueseke et al., 2007).

Image
Figure 4. This specimen of basalt porphyry from Ponderosa shows a gem-quality sunstone phenocryst surrounded by smaller non-gem feldspar crystals. A porphyry is an igneous rock consisting of large crystals (phenocrysts) in a finer-grained matrix or groundmass. Photo by Robert Weldon.

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Figure 5. The High Cascade stratovolcanoes (A) are fueled by subduction under the Pacific Northwest. Flood basalts (B) inundated Oregon 15–17 million years ago. Sunstone occurrences (×) are linked to the local eruptive center of these basalts, Steens Mountain (SM) and Abert Rim (AR). As the basalts ebbed, new volcanic forces kindled a hot spot in the earth’s mantle, spawning volcanic calderas (C) across Idaho’s Snake River Plain (SRP) to the Yellowstone supervolcano (Y). Meanwhile, renewed activity (D) moved west across Oregon’s High Lava Plains (HLP) to Newberry Caldera (N). Illustration by Larry Lavitt, adapted from Long (2009) and Grunder and Meigs (2009).

Considerable work has recently been done on the geology of eastern Oregon, principally under the aegis of the High Lava Plains Project, supported by the Carnegie Institute of Washington’s Department of Terrestrial Magnetism (http://www.dtm.ciw.edu/research/HLP). This project sought to explain Oregon’s recent (20 Ma) volcanic history through the work of specialists in petrology, geochemistry, geochronology, and geophysics. Their studies provided a much better understanding of the dynamics of plate subduction and magmatism under the Pacific Northwest.

According to Stewart (1966), the sunstone lavas within the Rabbit Basin are petrographically similar to plagioclase-rich flows within the Steens Basalt. They are also strikingly similar to lava flows exposed at the Abert Rim, a spectacular fault scarp some 760 meters (2,490 feet) high, located 10–15 miles southwest of the Rabbit Basin sunstone localities. Gunn and Watkins (1970) proposed that these lavas are part of the same volcanic episode, and that their feldspar phenocrysts might even have originated in the same magma chamber. In a future visit, we aim to collect representative samples from plagioclase-rich flows at Abert Rim and Steens Mountain and compare them with material from each of the three mines to see if we can confirm their relationships.

Feldspar phenocrysts that formed before eruption are surrounded by a finer-grained or glassy groundmass of the lava flow. Also contained in such groundmasses are smaller labradorite phenocrysts (An60), usually just a few millimeters in size, that crystallized in the flow as it cooled. Stewart’s analysis (1966) gave a composition of An67.2/Ab31.5/Or1.3 for the larger feldspar phenocrysts and An60 for the smaller labradorite phenocrysts in the groundmass. We intend to perform Ar-Ar dating on samples of basalt and feldspar phenocrysts from all three mine locations to determine their relative ages.

The feldspar must have formed over time within a magma chamber of calcium-rich magma that cooled slowly, allowing it to reach considerable size. Stewart (1966) proposed that primary crystallization occurred at depth under relatively uniform conditions of about 1100°C. He cited a large lath-shaped crystal measuring 8.3 × 2.6 × 0.8 cm. This is a substantial crystal by most standards, but we found larger, blockier ones at the Sunstone Butte mine. This might be because the crystals at Sunstone Butte cooled more slowly in a larger body of rock—within a cinder cone—and were not extruded in thinner lava flows, as elsewhere in the Rabbit Basin. As a result, there appears to be less fracturing due to thermal and mechanical shock, and intact crystals are recovered more frequently.

PONDEROSA MINE

The road to the Ponderosa mine gains in elevation as the scenery gradually changes from meadows to thick stands of tall ponderosa pines. It is classic volcanic highland, littered with cinder cones, extensive basalt flows, ashfall tuffs, and red cinder beds.

A map drawn by John Woodmark, Ponderosa’s owner and the president of Desert Sun Mining & Gem Co., led us to the mine, where we stayed in a bunkhouse. Woodmark purchased the property in 2003. For earlier history of the Ponderosa mine, see Johnston (1991) and Sinkankas (1997).

The mine is located at an elevation of 1,753 meters (5,700 feet) on the southwest side of Donnelly Butte. The mining season runs from June to October, when the mine is free of snow. Because Woodmark owns the property, it is not subject to regulation from the Bureau of Land Management or other government agencies.

The mine site covers some 60 acres (just over 24 hectares). Although only one-fourth of an acre has been mined to a depth of 6 meters (20 feet), Woodmark said that sunstone occurs throughout the property.

Johnston (1991) reported on the Ponderosa mine and its gem materials, characterizing the labradorite as 70% anorthite and 30% albite, placing it at the labradorite/bytownite boundary.

The sunstone occurs in a localized, weathered basalt flow (figure 6). So far, this is the only one of four basalt flows examined at the site that contains sunstone. The basalt being mined is moderately to heavily weathered, reduced to reddish brown soil containing nuggets of harder basalt in sections of the pit. Currently, Woodmark is recovering higher than normal quantities of red to pink rough from a section of the pit—approximately 20% of the sunstone mined. In 2010, his estimated recovery rate of red to pink rough was around 2–4%.

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Figure 6. At a section of freshly dug pit wall in the red zone, red cores of fragmented sunstone crystals glint in the sun. Photo by Robert Weldon.

The working area of the mine has more than doubled since being documented by Johnston (1991), but it still represents a relatively small area. This is because of the high concentration of feldspar in the decomposed basalt. Woodmark estimates a recovery rate of 1.5 kg of rough per cubic yard of earth moved and a possible reserve of more than a trillion carats of cuttable rough. In his opinion, this would make the Ponderosa one of the richest colored gemstone mines in the world.

Ponderosa produces 1 million carats of rough per year (figures 7–9) over the course of approximately 20 days (in three or four increments). Woodmark estimates he could mine 4­–6 million carats per year, given sufficient demand. Currently there are only a handful of people to drive the loaders and operate and maintain the other equipment. The mine also employs Native American teenagers from the nearby reservation. Woodmark pays the pickers $10 per kilogram of concentrate recovered. Each picker averages 1 kg per hour.

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Figure 7. This loader transfers crushed basalt ore to a dry trommel, separating rock and feldspar crystals from the decomposed basalt, which is essentially dirt. Photo by Robert Weldon.

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Figure 8. Pickers, including John Woodmark (foreground), load concentrate onto mesh screening tables at Ponderosa. They methodically sweep the table with a trowel, leaving “no stone unturned.” Photo by Duncan Pay.

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Figure 9. During screening, sparks of red to pink rough sunstone glitter in the sun among pea-sized chunks of vesicular basalt. Photo by Robert Weldon.

He personally grades the rough, first by color (red, orange, pink, yellow, colorless, green, bicolor, or schiller) and then by size. The strategy is geared toward providing a consistent supply of calibrated gems less than 7.0 mm in well-defined grades. These smaller stones are cut overseas. Woodmark does not trim or cob the rough, leading to lower yields (approximately 12% recovery, or 500–600 carats per kilogram). Larger fine-color or clear rough is supplied to designer cutters for high-priced, one-of-a-kind gems.

Woodmark stockpiles the colorless and yellow material because it is so easily treatable (Emmett and Douthit, 2009), and he is concerned it could harm the market for untreated Oregon sunstone. Woodmark is considering bead production as a source of revenue from this clear to champagne-colored rough.

DUST DEVIL MINE

The Rabbit Basin lies three hours south of Burns, through a desolately beautiful landscape of alkaline lakes, sand dunes, and volcanic ridges. Alt and Hynd­man (1978) provide a brief summary of the roadside geology. At Hogback Road, the paved surface ends and 35 miles of gravel road begins, leading eventually to the Dust Devil mine.

Travel trailers punctuate the desert, marking the sites where miners are working claims. At 1,402 meters (4,600 feet), this is high desert country dotted with sagebrush. No permanent structures are permitted by the Bureau of Land Management, and mining activities are subject to strict environmental regulations. As with the Ponderosa mine, the weather dictates the mining season, which runs from mid-May to mid-October, when the first snows typically fall.

The sunstone-bearing basalts cover about seven square miles (18 km2) at the northern end of the basin. They are a sequence of gray to strong reddish brown vesicular flows that form low rounded hills, reaching their highest point at Dudeck Ridge. The flows are typically only 3–6 meters (10–20 feet) thick, narrowing considerably toward the edges. The bedrock beneath the sunstone basalts is a gray-brown ashflow tuff of variable thickness. Underneath the tuff lies a vesicular black basalt (Peterson, 1972).

According to Don Buford, co-owner of the Dust Devil mine, thin flows cool rapidly, exerting pressure on crystals as they contract and causing extensive fracturing. Thicker flows cool more slowly, exerting less stress on the crystals and allowing them to retain their size. Phenocryst fracturing may also be due to movement and mechanical contact between crystals within the lava flow during emplacement (Peterson, 1972).

Buford and co-owner Terry Clarke (figure 10) have been very active in marketing untreated Oregon sunstone. Gems from Dust Devil have been used by notable artists such as Dalan Hargrave, Will Cox, Larry Winn, Larry Woods, Krista McMillan, and John Dyer to garner more than 15 American Gem Trade Association (AGTA) Cutting Edge awards. A pit operation with a modern separation plant (figures 11–14), the mine is known for its variety of stone colors and sizes up to 1,093 ct—nearly as large as a tennis ball.

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Figure 10. Left to right: Dust Devil employee Mark Shore, owners Terry Clarke and Don Buford, and gemologist Mariana Photiou, who works with the miners and helps market the gem. Photo by Robert Weldon.

At the mine, we both witnessed and captured on video the careful recovery of crystal fragments by employee Mark Shore (figure 11, left). The fine sunstone crystal in figure 11 (right), mined from a decomposed basalt nodule, would have constituted an 841.74 ct stone if found in one piece.

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Figure 11. Left: Mark Shore recovers a large sunstone crystal from its matrix as Don Buford observes. Right: Three principal stones with bodycolor or schiller totaling almost 300 carats, along with 500 carats of pale yellow stones, were recovered from this fragmented crystal; courtesy of Mark Shore, Dust Devil Mining Co. Photos by Robert Weldon.

This crystal is a telling example of the challenges facing the sunstone miner and the gem cutter: It is highly fractured and has the most desirable colors confined to zones in its interior, restricting the size and orientation of the gems that can be cut from it. These limit the cutter’s choices and make it challenging to produce fine gems. The recovery yielded the following: ... "

https://www.gia.edu/gems-gemology/FA13- ... -137313009
PinkDiamond
ISG Registered Gemologist


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