Eden Valley Petrified Wood
| Wyoming is a state rich in fossil wood and has several petrified forests. The petrified wood from one forest is known to collectors as Eden Valley Petrified Wood and is named after the town of Eden, Wyoming. Eden is located in the west-central part of the state and is in the center of the 80 mile long area where the fossil wood is found. Three collecting areas are well known. | |||
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| The Big Sandy Reservoir is located just north of Farson. This area is known for Petrified Palm Wood. On the eastern end of the deposit, fossil wood is found around Oregon Buttes just east of South Pass, Wyoming. Oregon Buttes is a major landmark on the Oregon Trail. | |||
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| Eden Valley Petrified Wood was formed from plants living about 50 million years ago and the rock exhibits features not found in fossil wood anywhere else in the world. The petrification process for this area involved shallow "algae growing" lakes. In many cases, for undetermined reasons, the wood came to be in this water in its live condition (see image #1 below) before it had a chance to dry out and look like old dead wood. This wood became coated with algae (image #2) which adhered to the surface making a cast or mold around the wood. Later the wood dried and shrunk in the mold made of algae (image #3). Over time these algae casts became part of a layered rock formation. Silica-rich water solutions seeping through the rock then petrified the wood and filled in the spaces left between the dried wood and the hardened cast with agate, calcite, and quartz (image #4). | |||
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As the agate coated the inside surface of the algae cast, perfect impressions of the bark were left in the agate. Thus there are some rocks that show two 50 million year old "pictures" of the same plant -- one picture of how the plant looked alive and another after it died and dried out! |
The Blue Forest collecting area is located in the west end of the deposit
about 30 miles west of Farson. The fossil wood found in this area is known for the light
blue agate surrounding many of the pieces.
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| Exquisite representations of bark both live and dried out have been preserved. Worm holes, insect borings, woodpecker holes, and other events have been observed in the petrified wood. Even very rare lichen fossils and small clam shells have been duplicated in the agate. | ||
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Looking east from Oregon Buttes | |
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Petrified wood on the ground near Oregon Buttes | |
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Sorting pile at Blue Forest -- the pieces pictured here were discarded as being undesirable by the digger. | |
More information may be found in the following back
issues of
Lapidary Journal:
| 1950 | April | page 16 |
| 1953 | August | page 246 |
| 1968 | May | page 330 |
| 1972 | October | page 1078 |
| 1974 | May | page 366 |
