Total Pageviews

Showing posts with label chalcocite. Show all posts
Showing posts with label chalcocite. Show all posts

Monday, July 30, 2012

Tales of the Devil to Date


The new entrance to Mine #1 The shaft is 40 feet deep with an adit going off from the bottom northweat for 10 feet that is 6 feet wide and 7 feet high.  The adit is well timbered and the shaft was filled with debris dating back to the 19th Century.
Photo by John Carter


We have rediscovered an old mining complex in western Connecticut that to date comprises two mine shafts with accompanying adits.  The first mine consists of a shaft approximately forty feet deep with an adit going off to the northwest that is ten feet long, six feet wide and sever feet high.  Town records reveal the first mine was a prospect hole that may have been created in pre-Revolutionary days; the second mine was just discovered on July 30, 2012 and is yet to be explored.  Town records indicate this mine may have an adit up to 140 feet long.

At the end of May 2012 a blue ribbon committee was convened at the site consisting of Charles Merguerian of Hofstra University, Nicholas Bellantoni of Uconn, Stefan Nicholescue of Yale, John Carter of Geotek and two engineers, none of us could determine what they were mining.  The town P&Z Officer finally discovered some old records that divulged the fact the second mine was dated to 1858.  The mineral mined was chalcocite an ore of copper.

The mines were found within two miles of Cameron’s Line a major fault system that extends from Staten Island, NY the western mountains of Norway under a series of different names.  There are several important mines located in the proximity of this suture zone producing gold, silver and copper.  The largest copper mine in the U.S. before the discovery of copper in the Keweenah Peninsula of Michigan was the Argo Mine in Vermont that is also associated with this large fault system.

The property where these mines are located is highly mineralized containing in addition to chalcocite, malachite, pyrites, quartz, kyanite, ilmenite, magnetite, cerrussite, beryl and many other minerals yet to be identified.  Although there are no plans to resume mining operations at these old mines mineral specimens will be available for sale.  For further information contact John Carter at geotekllc@gmail.com or 860-469-4804.

Many of the specimens of kyanite, ilmenite and magnetite are of museum quality and are really spectacular.  Some of these specimens are on display at the Yale Peabody Museum in New Haven, CT.

Tuesday, July 10, 2012

Tales of the Devil: The Hammer of Thor


The new find on the site


Somebody asked me why we named this series, Tales of the Devil. Well back in 1819 one of the sources wrote in the American Journal of Science 1st Edition a paper about minerals found in Litchfield County.  Then he got religion and during the 1850’s wrote a tract called “Tales of the Devil.”  By then he must have been a full-fledged geologist from Yale.  At least he knew his subject matter.  However, “Tales of the Devil” fits this place as well as any other story, but finally some old records came to light that explained the whole place.

Since its rediscovery in March 2012 this site has had at least five PhDs tugging their forelocks trying to figure out what in blue blazes went on there.  Finally one of them found a collection of old records that explained the whole deal and even named some of the historical personages that were involved with the site including P.T. Barnum and Thomas Edison.

The first shaft and adit that was discovered was apparently a prospecting pit, or if you prefer a gopher hole. This consisted of the mineshaft that was 40 feet deep with an adit at its bottom going off that was 10 feet deep by 6 feet wide by 7 feet tall. It is apparent from the records that this may have existed since pre-Revolutionary War times. Most of the mining occurred in the mid-19th century and according to the records underground mining in the location included an adit that was more than 140 feet long.

Because of the geology on the site being similar to those where gold was found we assumed that was what they were looking for, and probably was. According to the old records covering the site what they were actually found was copper, and it was in the form of the copper sulfide mineral called chalcocite, a grey colored mineral.

Actually this tale doesn’t have anything to do with Thor except there’s a Norwegian involved in its telling. He was one of the PhD's.  Another one came from Transylvania.

Sunday, May 20, 2012

The Copper Mine in Bristol Connecticut

Bornite was the principal ore produced at Bristol, there are museum class specimens all over the world from this source.
Photo by Ra'ike

The copper mine at Bristol, Connecticut started in 1937 and continued in dribs and drabs until 1953.  It is a study in how not to operate a mine.  The owners always managed to spend more of their shareowners money then they could get out of the mine.  This mine was located along the contact between the Mesozoic sandstones of the Hartford Basin and the schists of the western uplands of Connecticut.  World class specimens of chalcocite and bornite much to the consternation of the operators were collected at the mine that are still found in many museums and in the hands of private collectors.

The early part of the 19th century was marked by many mines in Connecticut, the latest survey by the Connecticut Geological and Natural History pegs the number at over six-hundred, an online source has raised this to 1,246 mines.  The first mention of this mine was by Shepard in 1837, but later it was noted by Percival in 1842.  The mine itself lies about 4 miles northwest of the center of Bristol at an elevation of around 350 feet.

Although work on the mine began in 1837 it was worked in such a desultory way that only about 125 tons were shipped to England for refining.  From 1847 to 1853 the mine was at its most active and was more vigorously worked.  It was during this period that over half a million dollars were spent developing the mine.  The workings were extended to 240 feet and to 500 feet along the vein.  This and other tunnels gave the mine a maximum width of 120 feet.

During the same period the mine produced nearly $200,000 worth of ore weighing 2,200 tons with the picked ore having a copper content of 33%.  For years the mine was abandoned after the collapse of a heap of mine tailings destroyed a dam on Poland Creek precipitating a wall of water that almost wrecked the Forestville part of Bristol.

The mine was originally discovered by a farmer, one Theophilus Botsford became curious about why a spring on his property ran green, so he took a plow and team and uncovered a vein of copper ore.  Sure enough this was the source of the green water that stained the rocks in Poland Creek and killed the vegetation along the brook.  Finding the copper ore satisfied his curiosity and it wasn’t until 1800 when Asa Hooker, a brass founder in Bristol leased the land from the widow Sarah Yale.  She was a descendent of the founder of Yale University in New Haven.  She made a deal to be paid a percentage of any ore mined, but there was little mining done until 1836 long after she had died.

After 1836 the mine was worked on a large scale but never made a profit eventually falling into the hands of John M. Woolsey of Yale.  Under the hands of Prof. Silliman who was a good professor, but a lousy miner caused the most extravagant schemes and experiments were undertaken.  Hundreds of thousands of dollars were poured into the mine with far less coming out with the Bristol Mining Company that was incorporated in 1855 was bankrupt by 1857.

According to the Tunxis Valley Herald for December 17, 1886.

"The collapse which came was caused by the grossest mismanagement, and
not from any fault in the mine. The manager's crowning impulse seems to have
been to spend the most money in the shortest possible time. Large and expensive
buildings were for some trivial cause torn down and used for fuel, and new ones
erected which if reports are true, were liable to meet a similar fate.
"The agent resided in Farmington Street and kept eight or ten fast horses
at his stables in Farmington and others at the mine. The superintendent occupied the house near the mine. The office furniture and fittings were of an expensive style. Once a dance was given in the store room which had been provided with steam pipes for heating it on this occasion as it was winter. Sibley*s Band, of Hartford, the best in the State at that time, was hired for $100; the supper was a costly one, wine of several kinds being  furnished. That this wine was not an imitation may be  inferred  from the  f a ct that those at the  supper table amused themselves by throwing turkeys and chickens at each other.”

The mine also had gold that was associated with the copper ores.