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Specimen
Ridge Virtual Hike
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The upper part of this tree is burried in a conglomerate and
exhibits much abrasion. The extensive root system penetrates
into a tuffaceous sandstone. This tree was growing in place when
it was pushed over by an advancing volcanic mudflow (Yuretich,
1984, p. 160). |
Yuretich, R.F. (1984). Yellowstone fossil forests: New evidence
for burial in place: Geology, v. 12, p. 159-162. |
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