microscopic view of ash (photo)
Volcanic ash magnified 525 times.
All Ashfall skeletons are buried in a bed of pure volcanic ash. Volcanic ash consists of tiny shards of glass from broken glass bubbles. These glass bubbles form and then break apart during powerful volcanic eruptions.

The ash particles are small enough to have been breathed deeply into the lungs of animals when volcanic ash blanketed northern Nebraska 12 million (12,000,000) years ago.

At the Ashfall fossil site in northeast Nebraska, the ground beneath the soil looks something like this in cross-sectional view.

Sedimentary rock layers (strata) contain fossils that reveal clues to environmental conditions and the animal life of specific times in the past. The particles of sediment that make up the rock reveal clues about the environmental setting and how the rock was deposited.
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An aerial view of a portion of the Ashfall site. MORE


GEOLOGIC SETTING OF ASHFALL FOSSIL BEDS AND VICINITY


Ashfall Fossil Beds State Historical Park
86930 517th Avenue
Royal, NE 68773
Phone: (402) 893-2000

Email: ashfall2@unl.edu

Rick Otto, Superintendent
A Cooperative Project of the
University of Nebraska State Museum &
Nebraska Game and Parks Commission


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