Category Archives: Uncategorized

Bixbyite, Rutile, & Amethyst Crystals

Near Marysvale, Piute County Geologic information: The Marysvale area is dominated by Tertiary igneous rocks ranging from intermediate to silicic compositions with both volcanic and plutonic representatives. The especially thick volcanic section is thought to be the result of a large stratovolcano complex and associated calderas that existed during mid-Tertiary time. One of the common units

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Dugway Geode Beds

Geologic information: Approximately 6 to 8 million years ago (Miocene epoch), volcanic activity occurred in western Utah and deposited an extrusive igneous rock called rhyolite. Trapped gasses formed cavities within the rhyolite, and millions of years of ground-water circulation allowed minerals to precipitate into the cavities. The result is geodes with spherical shapes and crystal-lined cavities.

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Gold Trivia

Gold is one of the most recycled substances of all.  It’s quite possible that the gold contained in the first nuggets found over 6,000 years ago still exist today, melted and recast into a contemporary piece of jewelry or as the filling in your teeth.  Worldwide, wedding rings are probably the single biggest gold jewelry item.  One

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Lapidary Notes

The hardness of rocks is a fascinating and puzzling study for the beginning rockhound.  The durability of gemstones is of great importance to anyone setting up a tumbler or starting to make cabochons.  The rock’s resistance to wear (abrasion or “scratching”) is indicated by its hardness, or as sometimes defined by mineralogists, its “scratchability”.  The hardness of any material depends

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