Gold in New Hampshire
March 2002 by Edgar B. Heylmun, PhDNew Hampshire, one of five New England states, has an area of 9,351 square miles, a bit larger than Kern County, California. It is a playground for people who live in the large urban areas in the East.
Down, down, down I plummeted into the narrow granite chute. In a matter of a few seconds, I envisioned myself lying crumpled in a field of mammoth, sharp, jagged granite rocks. In those few seconds, my thoughts also imagined my life ebbing...
Under the previous administration, the EPA declared the ditch was a federally-protected waterway, and Robertson needed a federal permit under the Clean Water Act.
I can’t remember the exact day, but I do remember I was 11 years old when my father Charlie Sr. took me prospecting for the first time. That’s the day the fire and passion for gold was first ignited in me. I was born and raised in Grand Forks, British Columbia, and was lucky enough to have a gold bearing creek about 10 miles from our home.
The year 2004 feels much like the fabled month of March, entering like a lion, remaining stormy for much of the time, but exiting like a lamb. It is almost eerie how there has been a reduction of tension throughout the investment communities, both conventional and precious metals, in the past few weeks.
Metamorphic rocks such as gneiss and schist are known for their pocket gold deposits. Such pockets may not be large enough for major mining operations, but may be very rewarding for individuals or small companies. Gold-bearing quartz veins may cut gneiss or schist, but often the veins parallel the bedding, or foliation. The origin of mineralized veins, which parallel the foliation, has been kicked around for years.
On a personal note, very little has bothered me quite as much as the fact that some on the political left are crying “foul” about the fact that Secretary Clinton may have (the outcome is still slightly uncertain at press time) gained more popular votes than the President-elect and therefore the election result is “wrong.”
With successively lower temperatures as the water mixture cools, new sets of minerals are formed and many of those stable at a higher degree of heat became subject to alteration as the temperature progressively moved lower.
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