PYRITE SUNS AND COAL MINING
With their thin, at, disk-like shapes, brassy color and bright metallic luster, “suns” are the most eye-catching and popular of all pyrite concretions. Concretions, a word derived from the Latin con, meaning “together,” and crescere, “to grow,” are growths of crystallizing minerals that have displaced sediments or lled pores in sedimentary rock. Concretions can be spherical, ovoidal, elongated,
attened, or irregular in shape and range in size from microscopic to several feet in diameter.
THE ILLINOIS COAL FIELDS
Suns are the rarest form of concretionary pyrite. Most pyrite-sun specimens, including the largest and nest, come from the vicinity of Sparta, Illinois, near the center of the vast Illinois Coal Basin. is basin of coal-rich, 300-million-year-old Pennsylvanian sediments covers central and southern Illinois and adjacent parts of Indiana and Kentucky. Since commercial mining began here in the mid-1800s, the Illinois Coal Basin has yielded more than nine billion tonnes of coal.
Near Sparta, the six-to-eight-foot-thick Herrin Coal Seam rests roughly 250 feet beneath the surface. On top of this coal seam is the Anna Shale, a massive layer of black, organic-rich, marine shale. e bituminous Herrin coal is rich in sulfur, while the Anna shale is rich in iron and sulfur. Under the heat and pressure of deep burial, the iron and sulfur combined into pyrite (iron disul
de) concretions that developed within shale laminations just above the shale-coal contact.
HOW SUNS ARE FORMED
Under most conditions, this pyrite would have formed roughly spherical nodules. But trapped under great pressure in the hard shale, the pyrite grew in the directions of least resistance, laterally within the horizontal laminations to form at, disk-like suns.
Tiny pyrite suns, most only a fraction of an inch in diameter, are found in coal-shale environments worldwide. But pyrite suns from the Sparta-area mines are by far the most numerous, largest
and best developed. Many are three to four inches in diameter; the largest are nearly eight inches in diameter.
e chemical stability of pyrite suns has long been debated. While some last inde nitely, others quickly display the unmistakable signs of pyrite oxidation, a sulfuric-acid odor and a slow crumbling into particles of iron hydroxides. According to the Illinois State Geological Survey, pyrite suns from the Sparta mines contain low amounts of marcasite, an orthorhombic polymorph of iron disul de that oxidizes readily and likely accelerates the oxidation of the pyrite.
SUN POPULARITY
Sparta-area miners began collecting pyrite suns as novelty items in the 1800s. But not until the 1950s, when national interest in mineral collecting began growing rapidly, did strong commercial demand develop. Miners then began “high-grading” the suns.
ey carried them from the mines in their lunch buckets and sold them to mineralspecimen dealers.
Iridescent pyrite suns became quite popular again during the 1990s. While suns occasionally exhibit natural iridescence, most that reached the market were treated with acid to arti cially induce or to enhance iridescence. Unfortunately, treated iridescent suns show a much higher rate of oxidation than untreated specimens.
THE FUTURE OF SUNS
e market supply of pyrite suns has always depended on coal mining. In the 1950s, Illinois had 27,000 coal miners and some 150 mines. Most were small, hands-on, underground operations that were ideal venues for collecting suns.
Coal mining has declined sharply as power plants moved away from coal, especially the Illinois Coal Basin’s high-sulfur coal. Today, only 2,700 Illinois miners work in 17 coal mines. Sparta’s Randolph County, where most pyrite suns are found, has only one underground and two surface mines. Because these mines are now highly mechanized, miners have few opportunities to collect pyrite suns.
Today, dealer supplies are still substantial and limited numbers of new specimens continue to come from the mines and shale-waste heaps. In the not-distant future, time may run out on both coal mining and the supply of pyrite suns.
Steve Voynick is a science writer, mineral collector, and former hardrock miner, and the author of guidebooks like “Colorado Rockhounding” and “New Mexico Rockhounding.”
Tiny pyrite suns, most only a fraction of an inch in diameter, are found in coal-shale environments worldwide. But pyrite suns from the Sparta-area mines are by far the most numerous, largest and best developed. Many are three to four inches in diameter; the largest are nearly eight inches in diameter.”