November 2003 by Lance HarkerAwhile back, I was doing some prospecting in a remote mountain region, located in the rugged, well-timbered valleys of north-central British Columbia, an area known for its coarse gold.
Geologists have long realized that the vast majority of gold in typical quartz veins is in the tiny, dust-size range, a lot smaller than the gold nuggets found by placer miners. This is common worldwide in many, many gold districts.
The Washington Department of Fish and Wildlife (WDFW) issued emergency rules without public comment just prior to our publication deadline.
• The "no shrimp left behind" act
• Someone has exceeded their credit limit
In Wyoming, garnets are often common where aluminum-rich (micaceous) rocks have been highly metamorphosed. Such rocks are recognized by abundant black (biotite), silver (muscovite), or green (chlorite) mica with periodic grains of red garnet.
New Interim Rules may be coming soon in the state of Washington.
Carbonatites are rocks that formed from molten calcite or dolomite. The thought of calcite being molten lava is difficult to accept, but it was confirmed when it poured out of a vent in Tanzania in 1960.
We needed something to cook on, so we brought most of our kitchen with us including our full-size oven, which was pretty funny to see in the middle of a rainforest. Food was always a concern, but fortunately for us...
The Ball Mill • British Columbia to Streamline Filing of Mining Claims • Millsite Opinion Overturned! • Continental Drift • Eight Mines Earn Prestigious Safety Awards • A Guide to Overlooked Gold Deposits—Part III • Company Notes • The Kennedy Gold Mine—An Impressive Piece of History • Buckhorn Mountain Project May Be Revived • Picks & Pans: An Arizona Miner • Gold Hill, Utah • Looking Back • Frozen Prospects • Platinum in Nevada • USFS Criticized for Renting Chopper in Nevada Dispute • Melman on Gold & Silver • New Guinea Denies Existence of Gold Stash • Mining Stock Quotes and Mineral & Metal Prices