To: Bill/WA who wrote (2792 ) 8/21/2002 7:14:41 AM From: E. Charters Respond to of 8273 The geode may be chippable. Most often they are recognized by their spherical shape, which is rare, really, in stones. They can be many colours common to where they come from, and quite rough on the exterior, which is most often a mono-texture, which again is not that common. Most pebbles can be recognized for the rock they emanate from, such as granite, gabbro, etc,, and they will have crystals in their texture. If they are volcanic they will probably wear flattened and have striations. Often too the geode is cracked and crystals will form at the edges of the crack. Near all the placer areas of the world there are usually point source veins that feed the placer. These veins could be economic. That someone blasted this one does not mean it is not, and they just left it. On the other hand, it could be someone's claim. A map would tell. When you see gold, the rule is to stake. Perhaps it was missed by assay. You never know, and cannot assume. I don't know what mineral you saw that was gold colour but it could me muscovite mica, which is also known as sericite. This could be an indicator of gold in veins. It could be pyrite which is also an indicator.(I would think you wold know pyrite) The key to gold is the rock it came from and the habit of the quartz emplacement. Deep blue-green rock with rust and pyrite and deep colour, grey to white quartz and rock that fizzes with the application of HCL (you can get 10% hydrochloric in a drugstore) -- these are indicators. The Whiteshell (name?) gravels of the Dawson area were a white and green rock with mica that is identical in type to Kerr Addison mine ore back in Ontario. Other things to look for are parallel shears with quartz and calcite, ladderwork white quartz veining, fractured or ground rock, and micas on the vein edge. Rusty quartz is the neon sign of productive veins. But it does not have to be rusty. Veinlets of any colour could be interesting for different reasons. Shearing and signs of tension fractures are important. Gold will be in a vein that looks like it was injected in a ragged way into the rock. Veins are often discontinuous, and sinuous, and often may be just drips and draps of quartz in zones, seeming not more than a foot or so a time, but reporting as it were to a structure of shear lines, with mineral differentiation that is colourful compared to the surrounding rock. Veins will be in wider shear zones that my be zones of 100 feet or more wide. In major gold areas, parallelism could be for 1000's of feet, but veins are followed in the direction of the shears and may be continuous to continual for miles. If you find gold its like cockroaches. It signifies more and more will be found. Dawson has not revealed its hardrock sources as few prospectors know the art of hard rock gold hunting who do placer mining. The assumption for many years, wrongly was that the placer mines did not have economic sources but the gold came from granite. In some cases the sources were known as in California. There must however be vast undiscovered veins I would guess of economic grade in the California area not far from the placer mines. Some people did some drilling in Atlin for sources and found some veins. They did not develop any mines of note, but drilling in the mountains is tough. In Stewart, however that is how they found the Snip and Johnny Mountain, by tracing placer gold back to source. I first suggested this back in 1980 to a bunch of no good bastards who worked at Esso Minerals amongst whom was a man who was president of the BC and Yukon Miners Association. This lit up a bulb and later the rush was on. They sent me back to Toronto and I never got to participate. Ignorance and theft are legion. Never trust a mining man. They aren't just no good they are no goddamned good at all. Whitehorse has little or no gold that I know of. There is copper north of there. EC<:-}