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  • Juab County Commissioners support proposal to open Burgin mine, near Eureka


By Myrna Trauntvein
Times-News correspondent

The Burgin mine, located near Eureka, is a world-class mine and still has the possibility of being a valuable mining asset capable of producing lead, zinc and silver in marketable quantities.

Juab County Commissioners voted to write a letter in support of the mine development project and will attend a hearing to offer further support of the proposal to open the Burgin mine.

"It would be a good idea to have more jobs and to have a further water source for the people of Juab County," said Robert Steele, commissioner.

Paul C. Spor, LLC, Executive Director of Tintic Utah Metals with Chief Consolidated Mining Company, said that the Tintic area had a long history of mineral mining. The Tintic Mining District contained a high grade silver which contributed significantly to the world economy from 1896 with the discovery of the Humbug deposit.

Spor said the mine would employ 300 people and most of those workers would come from the Juab County area. Workers would make from $12 to $25 per hour and there would be some white collar jobs that would pay $100,000 per year.

In addition, since Nephi is 700-feet lower than Eureka, some of the water could be piped to Nephi for use.

The water is very old and has been below the surface for some time said Spor. "Since the Atomic tests in Nevada water has traces of tritium, a radiation trace mineral."

The water in the Burgin mine does not.

The mining company, he said, is interested in mining the 1.2 million tons of ore known to still be minable. Another 1 million tons within the Burgin resource area is likely available.

"The most recent mineral developments in the East Tintic District were the discoveries of the Burgin ore zone in 1958, the Trixie in 1969, and the Ball Park mineralized area in 1970," said Spor.

All of these later discoveries, he said, were made by Kennecott Copper Corporation and were based on intensive geologic and alteration studies made by the U.S. Geological Survey from 1943 to 1956.

Since 1963, essentially all of the primary ore production has come from the Burgin and Trixie mines.

During the Burgin mine's life, said Spor, approximately 1.8 million tons of ore were mined which assayed 8.6 percent lead, 8.5 ounces per ton silver, and 8.7 percent zinc.

"From an economic standpoint, Kennecott's operation of the Burgin mine proved largely unsuccessful," he said. "This was due to high mining costs as a result of significant inflows of hot, saline water and bad ground conditions. Kennecott suspended operations at the Burgin mine mid-1978."

Spor said the economics of the Burgin mine are based on the minable resources, grades, metal prices, and successfully dewatering.

"Waters pumped from the Burgin mine were geothermal with temperatures ranging from the 130 to over 150 degrees," said Spor. "When the Burgin mine was closed and the pumps were turned of, the dewatered portion of the mine flooded and returned to the 4,550-foot elevation within 24 hours."

He said no other water aquifers were affected by the 15 years of pumping because there would have been a change in water temperatures, mineral characteristics, and dissolved constituents in the Burgin inflows.

"A second conclusion is that the geothermal system is very large and deep-seated because of the very quick recharge experienced at closure," Spor said.

Sunshine Mining and several consulting firms have projected, based on the area and depth of the New Burgin mine, that approximately 12,000 to 18,000 gallons of geothermal water will need to be pumped per minute.

Treating the Burgin mine water and putting it to beneficial use seems to be the most environmentally sound and responsible method, he said.

"Geothermal mine water is hot and salty with some amounts of metals," said Spor. However, the water can be purified with common, reliable, treatment technique to a quality that will exceed Utah's drinking water standard. A byproduct of table salt is potentially recoverable in addition to the water.

There were nine entities and individuals who protested the Chief's application. They were all given 30 days to respond and only the Central Utah Water Conservancy District provided the further information in support of the objections they had made.

The geothermal water, said Spor, is likely volcanic and perhaps three to six miles below mean sea level and four to six miles below the surface of Goshen Valley.

"After 15 years of pumping up to 9,800 gallons per minute, the water level in the mine was only reduced 156 feet," said Spor.

During that 15 years, approximately 158,000 acre feet of water was pumped which is a volume only slightly less than the capacity of Deer Creek Reservoir on the Provo River. However, during that time, the quantity of inflow from geothermal springs into Utah Lake was not affected.

"We believe that the geothermal water is confined in to the area because of faults that lock it into place," said Spor.