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The Bawl Mill
July 2004 by Staff
• Government discovers new method to subsidize airlines• California uses environmentalists' favorite tool against them
• Delayed gratification
• Hold my seat; I'll be right back...
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Better Worse:
December 2022Desert Gold Hunting Boo-Boo's And No-No's
The Bawl Mill
April 2017
• Protesters trash the place
• IRS can't keep a secret
• Make way for minimum wage
• Protesters trash the place
• IRS can't keep a secret
• Make way for minimum wage
Endurance Is Golden
September 2011
Feeling through the mud, I felt the weight and shape of what could only be gold. Throwing my hand in the water revealed a sixteen-gram nugget oozing with character.
Feeling through the mud, I felt the weight and shape of what could only be gold. Throwing my hand in the water revealed a sixteen-gram nugget oozing with character.
The Guyana Highlands
October 2004
The Guyana Highlands referred to here are a tropical upland area that extends from French Guiana on the east to Colombia on the west, with elevations reaching 9,219 feet. It occupies a vast and remote region between the Orinoco River on the north and the Amazon River on the south. There are mountains, tablelands, mesas, and swamps, largely impassable to those on foot.
The Guyana Highlands referred to here are a tropical upland area that extends from French Guiana on the east to Colombia on the west, with elevations reaching 9,219 feet. It occupies a vast and remote region between the Orinoco River on the north and the Amazon River on the south. There are mountains, tablelands, mesas, and swamps, largely impassable to those on foot.
Gold Deposits in Skarn
July 2003
Skarn consists of coarse-grained calcium, magnesium, iron, and aluminum silicates formed by hydrothermal solutions, which replace limestone or dolomite near the contact with an igneous intrusion. The contact metamorphism is usually caused by an intrusion such as quartz monzonite, granodiorite, or similar rock type, which may or may not be mineralized.
Skarn consists of coarse-grained calcium, magnesium, iron, and aluminum silicates formed by hydrothermal solutions, which replace limestone or dolomite near the contact with an igneous intrusion. The contact metamorphism is usually caused by an intrusion such as quartz monzonite, granodiorite, or similar rock type, which may or may not be mineralized.
Melman on Gold & Silver
November 2005
Your correspondent has been around quite a while on this globe of ours, but seldom have we ever seen a collection of calamities such as has occurred during this past ten months.
Your correspondent has been around quite a while on this globe of ours, but seldom have we ever seen a collection of calamities such as has occurred during this past ten months.
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