| Fossils
are... not old bones -- at least, not always. These ancient traces of life come in a variety of forms. Some are old bones, more or less altered by chemical processes. Others are old turds (coprolites, technically), or "trace fossils" like footprints or impressions of skin, feathers or scales.
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Dino-hunters look for
specimens in gullies, cliffs, and other heavily eroding lands. Craig Pfister
extracts a Hadrosaur (duckbill) bone in the Hell Creek Formation of Montana.
© Jeff Miller/UW-Madison Office of News and Public Affairs.
Fossilization -- the preservation process-- requires that the organism -- or the footprint or impression -- be covered with sediment before it is eaten or washed away. On land, this often happened when the corpse washes into a river and is covered with sediment. Generally, only hard tissue -- bones and teeth -- survives fossilization, but there were rare cases where some fool got lost in the mountains and ended up in a glacier for long-term storage cold ice. (The Why Files described a slew of several natural embalming techniques in a File on amber.)
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One place where there's plenty of erosion is in the Hell Creek Formation in South Dakota. The Why Files asked ace reporter Brian Mattmiller to describe a season under the sun. |
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