Shoshone Silver - riesiges Silberportfolio - 500 Beiträge pro Seite
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SHSH.PK ist ein interessantes Minenunternehmen aus den USA.
Sie verfuegen ueber Minen in Mexiko und den Staaten. Mit Einem Marketcap unter 3 mio U$ erhaelt man 9 verschiedene Minen, wobei einige ueber Infrastruktur und Equipment verfuegen. Die Tatsache, dass SHoshone zwischen 1970 und 1990 produzierte ist auch sehr positiv zu bewerten. Management ist Klasse, Leute von Sterling Mining, dem Besitzer der legendaeren Sunshine Mine.
Kurs kommt von 2,25 als SHoshone produzierte, jetzt hat er den Boden bei 16 cent gefunden.
Sie verfuegen ueber Minen in Mexiko und den Staaten. Mit Einem Marketcap unter 3 mio U$ erhaelt man 9 verschiedene Minen, wobei einige ueber Infrastruktur und Equipment verfuegen. Die Tatsache, dass SHoshone zwischen 1970 und 1990 produzierte ist auch sehr positiv zu bewerten. Management ist Klasse, Leute von Sterling Mining, dem Besitzer der legendaeren Sunshine Mine.
Kurs kommt von 2,25 als SHoshone produzierte, jetzt hat er den Boden bei 16 cent gefunden.
Hier die Webseite.
http://www.shoshone-mining.com/
Shoshone ist einer der wenigen einen Silberwerte mit einem Klasse Portfolio von "9" verschiedenen Minen.
Shoshone ist eine Klasseaktie, die man in sein spekulatives Minenportfolio befuegen kann.
Sobald Silber die 8 Dollar erreicht hat, wird man eine Menge Spass damit haben.
http://www.shoshone-mining.com/
Shoshone ist einer der wenigen einen Silberwerte mit einem Klasse Portfolio von "9" verschiedenen Minen.
Shoshone ist eine Klasseaktie, die man in sein spekulatives Minenportfolio befuegen kann.
Sobald Silber die 8 Dollar erreicht hat, wird man eine Menge Spass damit haben.
Schon auf meiner Liste!
Great stock to ride the silver wave ! The Silver Revolution will come !!!
Great stock to ride the silver wave ! The Silver Revolution will come !!!
Lakeview und das Bilbao Projekt in Mexico sind klasse.
Shoshone hat ja schon ueber 20 mio resourcen und es fehlen noch die Zahlen fuer die uebrigen 8 Properties.
Shoshone hat ja schon ueber 20 mio resourcen und es fehlen noch die Zahlen fuer die uebrigen 8 Properties.
Lakeview gefällt mir recht gut. Die Tatsache, dass dort schon produziert wurde und für recht wenig Geld die Produktion wieder angefahren werden kann macht das Projekt attraktiv.
Wer kennt sich mit den Leaseverträgen mit Sterling Mining aus ?
Wer kennt sich mit den Leaseverträgen mit Sterling Mining aus ?
Trading Spotlight
Die sitzen auf einer Menge Silber. Bin dabei.
Hat das Potential eine zweite Sterling zu werden.
Sterlingleute sind da involviert !!!!
Hat das Potential eine zweite Sterling zu werden.
Sterlingleute sind da involviert !!!!
Das Teil ist saubillig!!!
Man bekommt eine Menge Silber für ein Marketc. von 1,8 mio
Man bekommt eine Menge Silber für ein Marketc. von 1,8 mio
Shoshone hat eine Menge Gebiete auch im Silver Valley, dem Ort mit dem hoechstten Anteil an Silber auf unserem Planeten. Im Valley sollen noch ueber 2 Mrd. Unzen Silber im Boden sein.
Silber 16 cent im Plus, bis zu den 20 Dollar die uns rech machen werden ist es noch ein steiniger Weg.
Die Silber Revolution ist im Anmarsch !!!!
Die Silber Revolution ist im Anmarsch !!!!
Shoshone hat das Zeug zu einem Mittelgrossen Produzenten aufzusteigen. Genug Minen haben sie ja.
Eines der Hauptprojekte
Lakeview and the Silver Valley
The Lakeview District mines are located within the same Belt metamorphic rocks (the Wallace, St. Regis, and Revett Formations) and have similar mineralization as the world- lass Coeur d`Alene District, just 25 miles south. However, exploration at the Lakeview District has been minimal compared to the Coeur District, and many geologists believe that mineralization at Lakeview, like Coeur, may grow much richer at depth.
Shoshone Silver has assembled an impressive portfolio of silver properties in northern Idaho surrounding our centerpiece, the Lakeview Mine and Mill operation. We expect this collection of past-producing mines will enable Shoshone Silver to re-enter the ranks of producing companies and provide a signifi cant return to our shareholders at higher silver prices.
The Lakeview Mine & Mill
The Lakeview Mine & Mill are the flagship assets of Shoshone`s rich silver producing history and today serve as the focal point of its north Idaho operations and a key element of its overall revitalization strategy.
The Lakeview Mine is the most extensively developed of Shoshone`s Lakeview District properties, with six main levels reaching a depth of 1400 feet. Vein material is encountered at each mine level and with ore grades generally improving with depth. The Lakeview Mill is an on-site, expandable, 200-ton per day facility that produced concentrates for Shoshone mining operations from the 1970s into the early 1990s.
Sunshine Mining & Refi ning became active in the district in the early 1960s, identifying several veins at the Lakeview Mine reportedly grading up to 25 oz/t silver over a 5-foot vein width, with one drill hole intersecting a narrow section that assayed 185 oz/t silver. Historic production data indicates that Lakeview ore graded in excess of 10 oz/t silver with signifi cant gold values.
There are presently 24,190 tons of mineralized material delineated at Lakeview, grading an average of 11.8 oz/t silver. Exploration plans include mine and mill rehabilitation, surface and airborne geophysics and underground drilling.
Conjecture Mine
The Conjecture Mine is located in the Lakeview Mining District of Idaho, some 30 miles to the northwest of the Coeur d`Alene mining district. The rock groups of the Lakeview District are the same Precambrian belt series associated with the world-class silver deposits of the Coeur d`Alene mining district to the south.
In the late 1950s and early 1960s, Federal Resources of Salt Lake City, Utah, invested approximately $3 million in shaft sinking and underground development at the Conjecture Mine. In all, Federal Resources completed a 2,000 foot deep, concrete lined, three compartment vertical shaft and nearly 12,000 feet of drifts, cross-cuts and raises to establish a block of mineralized material of 336,000 tons at a grade of 11 ounces per ton of silver, and .03 ounces of gold, with some lead and zinc.
An additional block of 370,000 tons of similar grade was listed as a possible block of mineralization between the levels.
The Weber Mine
Initial discoveries of mineralization in the Lakeview District were made in 1888 near the site of the Weber Mine, which is among the most historically productive of the Lakeview District. The mineralized vein at Weber is hosted in a shear zone up to 80 feet wide and 3,600 feet long and was mined as an open pit operation. Historic mining at Weber focused on a supergene enriched oxide ore zone that averaged over 40 oz/t silver. A second enriched zone was discovered by Shoshone in 1978, exposing a vein 10 to 12 feet wide and 135 feet long that was mined in the early 1980s. Production records from the Bunker Hill Smelter indicate that concentrates from Weber assayed roughly 120-185 oz/t silver, 0.54-0.70 oz/t gold, 12-20% lead, and 15-36% zinc.
The Keep Cool Mine
The Keep Cool Mine has been explored by fi ve adits and 3,000 feet of tunneling and historic production records indicate average grades of 11.5 oz/ t silver, 0.10 oz/t gold and 5.2% lead. Drilling at Keep Cool by Sunshine Mining & Refi ning in the 1970s reportedly included select intercepts that assayed over 70 oz/t silver. Keep Cool was most recently operated as an open pit by Shoshone in the early 1980s.
Silver Valley Properties
The “Silver Valley”, along with the surrounding mining districts of northern Idaho, make up the richest primary silver-producing region on Earth, with over a billion silver ounces produced in the last century. “The Valley” has hosted some of the world`s most legendary silver mines, including the Sunshine, the Bunker Hill, the Morning-Star (the deepest mine in North America at over a mile and a half deep), and Hecla`s Lucky Friday.
The Shoshone and Bullion claim groups are located in the St. Joe Mining District of eastern Shoshone County, along the Montana border. The properties are comprised of twelve patented claims and cover several prospect pits and other historic mine workings. Both properties have been leased to Sterling Mining Company.
The Shoshone claim group was the subject of considerable interest and speculation in the early 1980s as Anaconda Minerals drilled the property. Surface outcroppings, including a vein structure 7,000 feet long and up to 80 feet wide, along with “enormous geological anomalies” shown in soil and vegetation sampling by the USGS, led geologists to believe that substantial silver mineralization might be found at depth. In fact, USGS geologists then theorized that the largest silver deposits in Idaho`s “Silver Valley” might be found in its southeast corner.
Anaconda drilled four exploratory holes near the property boundary shared with Stevens Peak Mining, in an effort to locate a site for deeper drilling. One of the holes was suffi ciently encouraging to justify its continuation and was planned to extend to depths reaching 6,000 feet, targeting the Champion Vein, deep in the Revett Formation. However, the planned hole was collared at just over 3,000 feet and although core samples confirmed earlier projections about geology and structure at depth, the program was never completed.
Lakeview and the Silver Valley
The Lakeview District mines are located within the same Belt metamorphic rocks (the Wallace, St. Regis, and Revett Formations) and have similar mineralization as the world- lass Coeur d`Alene District, just 25 miles south. However, exploration at the Lakeview District has been minimal compared to the Coeur District, and many geologists believe that mineralization at Lakeview, like Coeur, may grow much richer at depth.
Shoshone Silver has assembled an impressive portfolio of silver properties in northern Idaho surrounding our centerpiece, the Lakeview Mine and Mill operation. We expect this collection of past-producing mines will enable Shoshone Silver to re-enter the ranks of producing companies and provide a signifi cant return to our shareholders at higher silver prices.
The Lakeview Mine & Mill
The Lakeview Mine & Mill are the flagship assets of Shoshone`s rich silver producing history and today serve as the focal point of its north Idaho operations and a key element of its overall revitalization strategy.
The Lakeview Mine is the most extensively developed of Shoshone`s Lakeview District properties, with six main levels reaching a depth of 1400 feet. Vein material is encountered at each mine level and with ore grades generally improving with depth. The Lakeview Mill is an on-site, expandable, 200-ton per day facility that produced concentrates for Shoshone mining operations from the 1970s into the early 1990s.
Sunshine Mining & Refi ning became active in the district in the early 1960s, identifying several veins at the Lakeview Mine reportedly grading up to 25 oz/t silver over a 5-foot vein width, with one drill hole intersecting a narrow section that assayed 185 oz/t silver. Historic production data indicates that Lakeview ore graded in excess of 10 oz/t silver with signifi cant gold values.
There are presently 24,190 tons of mineralized material delineated at Lakeview, grading an average of 11.8 oz/t silver. Exploration plans include mine and mill rehabilitation, surface and airborne geophysics and underground drilling.
Conjecture Mine
The Conjecture Mine is located in the Lakeview Mining District of Idaho, some 30 miles to the northwest of the Coeur d`Alene mining district. The rock groups of the Lakeview District are the same Precambrian belt series associated with the world-class silver deposits of the Coeur d`Alene mining district to the south.
In the late 1950s and early 1960s, Federal Resources of Salt Lake City, Utah, invested approximately $3 million in shaft sinking and underground development at the Conjecture Mine. In all, Federal Resources completed a 2,000 foot deep, concrete lined, three compartment vertical shaft and nearly 12,000 feet of drifts, cross-cuts and raises to establish a block of mineralized material of 336,000 tons at a grade of 11 ounces per ton of silver, and .03 ounces of gold, with some lead and zinc.
An additional block of 370,000 tons of similar grade was listed as a possible block of mineralization between the levels.
The Weber Mine
Initial discoveries of mineralization in the Lakeview District were made in 1888 near the site of the Weber Mine, which is among the most historically productive of the Lakeview District. The mineralized vein at Weber is hosted in a shear zone up to 80 feet wide and 3,600 feet long and was mined as an open pit operation. Historic mining at Weber focused on a supergene enriched oxide ore zone that averaged over 40 oz/t silver. A second enriched zone was discovered by Shoshone in 1978, exposing a vein 10 to 12 feet wide and 135 feet long that was mined in the early 1980s. Production records from the Bunker Hill Smelter indicate that concentrates from Weber assayed roughly 120-185 oz/t silver, 0.54-0.70 oz/t gold, 12-20% lead, and 15-36% zinc.
The Keep Cool Mine
The Keep Cool Mine has been explored by fi ve adits and 3,000 feet of tunneling and historic production records indicate average grades of 11.5 oz/ t silver, 0.10 oz/t gold and 5.2% lead. Drilling at Keep Cool by Sunshine Mining & Refi ning in the 1970s reportedly included select intercepts that assayed over 70 oz/t silver. Keep Cool was most recently operated as an open pit by Shoshone in the early 1980s.
Silver Valley Properties
The “Silver Valley”, along with the surrounding mining districts of northern Idaho, make up the richest primary silver-producing region on Earth, with over a billion silver ounces produced in the last century. “The Valley” has hosted some of the world`s most legendary silver mines, including the Sunshine, the Bunker Hill, the Morning-Star (the deepest mine in North America at over a mile and a half deep), and Hecla`s Lucky Friday.
The Shoshone and Bullion claim groups are located in the St. Joe Mining District of eastern Shoshone County, along the Montana border. The properties are comprised of twelve patented claims and cover several prospect pits and other historic mine workings. Both properties have been leased to Sterling Mining Company.
The Shoshone claim group was the subject of considerable interest and speculation in the early 1980s as Anaconda Minerals drilled the property. Surface outcroppings, including a vein structure 7,000 feet long and up to 80 feet wide, along with “enormous geological anomalies” shown in soil and vegetation sampling by the USGS, led geologists to believe that substantial silver mineralization might be found at depth. In fact, USGS geologists then theorized that the largest silver deposits in Idaho`s “Silver Valley” might be found in its southeast corner.
Anaconda drilled four exploratory holes near the property boundary shared with Stevens Peak Mining, in an effort to locate a site for deeper drilling. One of the holes was suffi ciently encouraging to justify its continuation and was planned to extend to depths reaching 6,000 feet, targeting the Champion Vein, deep in the Revett Formation. However, the planned hole was collared at just over 3,000 feet and although core samples confirmed earlier projections about geology and structure at depth, the program was never completed.
Mexican Assets - Bilbao Project
Das Mexiko Projekt
The Bilbao Property is located in southeastern Zacatecas State, Mexico. It lies within the Panfi lo Natera Mining District about 350 miles northwest of Mexico City and 35 miles southeast of the city of Zacatecas.
This mining district is ancient. High-grade, silver-bearing ores were discovered and initially exploited in 1600. A signifi cant amount of mining was completed on the Bilbao Property between 1900 and 1927 by the International Mining Company (Consejo De Recursos Minerales, 1992). Additional work may have been done on the property from 1939-1945. No signifi cant mechanized work is known to have been completed after 1945. The Bilbao Property was controlled by Frisco from 1945-1967 and Penoles from 1967 to 1991 (Kilborn, 1995).
An estimated one million tons have been mined from underground workings and two glory holes (Kilborn, 1995). Highgrade mineralization was followed to exploit direct shipping ore. There is no evidence of drilling on the property. Documented mining has been conducted only to a depth of 250 feet (76 meters) where sulfi de ore was encountered.
Two primary types of mineralization are found on the property. Distal Copper- lead-zincsilver pyroxene skarn mineralization has been documented within altered Cretaceous Age carbonates near granitic intrusives. Hydrothermal veins, of secondary importance at this time, are hosted by both the granitic intrusive and the Cretaceous Age marine sediments. The zinc-lead skarn could grade laterally into both Au-bearing garnet skarn or massive zinc-lead replacement ores in carbonate rocks.
Oxidation has reached a depth of about 250 feet on the property, creating an upper oxide resource that may overlie a signifi cant sulfi de resource. Zinc, lead, and copper oxides/ carbonates and silver chloride minerals are found in potentially economic quantities within the oxide zone.
Within this oxide zone, the 1997 Kilbourne pre-feasability study defi ned an inferred resource ranging from 3.211 million tons averaging 3.94% zinc equivalent to 0.234 million tons averaging 14.31% zinc equivalent. This inferred resource is based upon a systematic underground sampling program on three levels (approximately 1200 samples). The study also indicates positive cash fl ow and payback on capital within 2 years of mining the oxide resource.
Sulfi de potential is virtually untested, but could be exceedingly important with respect to overall potential. Skarn bodies in the region are documented to extend to depths of 3,000 feet (900 meters) below the surface (Consejo De Recursos Minerales, 1992).
For a relatively small expenditure, untested areas in a known, productive mineral district can be evaluated. This could only add to the value of the resource identifi ed thus far. Areas to the west, particularly those covered by alluvium and Tertiary Age volcanics, may hold the most promise for hidden skarn deposits.
Based on the similar geology and morphology of the area, it seems likely that the oxide mineralization defi ned thus far could exist on other parts of the property beneath thin layers of colluvium or post-mineral volcanics. If so, this might reduce overall mining and leach costs of the total oxide mineralization. Alternatively, it is possible that an economic sulfi de resource might be discovered.
Das Mexiko Projekt
The Bilbao Property is located in southeastern Zacatecas State, Mexico. It lies within the Panfi lo Natera Mining District about 350 miles northwest of Mexico City and 35 miles southeast of the city of Zacatecas.
This mining district is ancient. High-grade, silver-bearing ores were discovered and initially exploited in 1600. A signifi cant amount of mining was completed on the Bilbao Property between 1900 and 1927 by the International Mining Company (Consejo De Recursos Minerales, 1992). Additional work may have been done on the property from 1939-1945. No signifi cant mechanized work is known to have been completed after 1945. The Bilbao Property was controlled by Frisco from 1945-1967 and Penoles from 1967 to 1991 (Kilborn, 1995).
An estimated one million tons have been mined from underground workings and two glory holes (Kilborn, 1995). Highgrade mineralization was followed to exploit direct shipping ore. There is no evidence of drilling on the property. Documented mining has been conducted only to a depth of 250 feet (76 meters) where sulfi de ore was encountered.
Two primary types of mineralization are found on the property. Distal Copper- lead-zincsilver pyroxene skarn mineralization has been documented within altered Cretaceous Age carbonates near granitic intrusives. Hydrothermal veins, of secondary importance at this time, are hosted by both the granitic intrusive and the Cretaceous Age marine sediments. The zinc-lead skarn could grade laterally into both Au-bearing garnet skarn or massive zinc-lead replacement ores in carbonate rocks.
Oxidation has reached a depth of about 250 feet on the property, creating an upper oxide resource that may overlie a signifi cant sulfi de resource. Zinc, lead, and copper oxides/ carbonates and silver chloride minerals are found in potentially economic quantities within the oxide zone.
Within this oxide zone, the 1997 Kilbourne pre-feasability study defi ned an inferred resource ranging from 3.211 million tons averaging 3.94% zinc equivalent to 0.234 million tons averaging 14.31% zinc equivalent. This inferred resource is based upon a systematic underground sampling program on three levels (approximately 1200 samples). The study also indicates positive cash fl ow and payback on capital within 2 years of mining the oxide resource.
Sulfi de potential is virtually untested, but could be exceedingly important with respect to overall potential. Skarn bodies in the region are documented to extend to depths of 3,000 feet (900 meters) below the surface (Consejo De Recursos Minerales, 1992).
For a relatively small expenditure, untested areas in a known, productive mineral district can be evaluated. This could only add to the value of the resource identifi ed thus far. Areas to the west, particularly those covered by alluvium and Tertiary Age volcanics, may hold the most promise for hidden skarn deposits.
Based on the similar geology and morphology of the area, it seems likely that the oxide mineralization defi ned thus far could exist on other parts of the property beneath thin layers of colluvium or post-mineral volcanics. If so, this might reduce overall mining and leach costs of the total oxide mineralization. Alternatively, it is possible that an economic sulfi de resource might be discovered.
Western Gold Prospect
Shoshone acquired the Western Gold Prospect in late 2003. The property is located in the Oatman Mining District, the most productive primary gold district in Arizona with over two million ounces of recorded production at average grades exceeding one-half ounce per ton. The district holds excellent potential for the discovery of additional volcanic-hosted epithermal vein deposits.
The claims are one mile west of the Gold Road Mine and one mile northof the United Western Mine, both owned and formerly operated by Addwest Minerals. Other past producing mines in the immediate area include the United Eastern Mine, 1.5 miles to the southeast and theTom Reed Mine, 2.5 miles to the southeast. The Western claims have geology similar to the nearby United Western and United Eastern mines and cover the lateral extension of their same primary vein structure.
Shoshone acquired the Western Gold Prospect in late 2003. The property is located in the Oatman Mining District, the most productive primary gold district in Arizona with over two million ounces of recorded production at average grades exceeding one-half ounce per ton. The district holds excellent potential for the discovery of additional volcanic-hosted epithermal vein deposits.
The claims are one mile west of the Gold Road Mine and one mile northof the United Western Mine, both owned and formerly operated by Addwest Minerals. Other past producing mines in the immediate area include the United Eastern Mine, 1.5 miles to the southeast and theTom Reed Mine, 2.5 miles to the southeast. The Western claims have geology similar to the nearby United Western and United Eastern mines and cover the lateral extension of their same primary vein structure.
Interessanter Artikel
http://www.goldseiten.de/content/diverses/artikel.php?storyi…
Silber zweistellig, dann ist Shoshone einstellig, in Dollar natürlich!
http://www.goldseiten.de/content/diverses/artikel.php?storyi…
Silber zweistellig, dann ist Shoshone einstellig, in Dollar natürlich!
gestern 20 % plus. Wird nett sobald Volumen in die Aktie kommt.
Klasse Silberplay aus dem Silver Valley!
Reagiert wie ein Future auf den Silberpreis!
Reagiert wie ein Future auf den Silberpreis!
Bodenbildung abgeschlssen, der Zug geht nach Norden!!!
Sehr gute Silberwette! Strong buy!
hat sich ja schön entwickelt!
Silber ueber 10 Dollar
Strong buy!!!
Strong buy!!!
Jetzt gehts loouuus !!
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