|
Although no glaciers got into the Willamette Valley during
the ice ages between 2 million years ago and about 12,000
years ago the effects of this cold interval were profound
on this area. Glacial ice is probably the most effective agent
to wear and grind down rock ever devised by nature.
The ice ages saw incredible amounts of material being flushed
into the valley from the east out of the Cascades. As this
great mass of sand, silt and gravel flowed into the valley
born on streams it began to clog and plug the natural stream
system creating a network of shallow ponds, lakes and wetlands.
Along with this changed physiography came a lush vegetation
that would support a rich assemblage of mammals from mice
to elephants.
In the past 100 years any deep excavation or similar construction
in the Willamette Valley would often turn up the bones of
mammoth, mastodon and prehistoric bison. Dr Thomas Condon
began a collection of these large mammals and later Dr Earl
Packard similarly collected and published on this ice age
fauna. The latter paleontologist began to construct the rudiments
of a mammalian food chain from smaller organisms as beaver
and other rodents up to predators as wolves, fox, bears and
cats.
In the 1980s William Orr, director of the Condon museum of
paleontology in Eugene added to the collection with the remains
of muskrat and several more bones of bison, elephants and
ground sloths.
During the mid 1990s archaeologists began a series of excavations
in the Woodburn area in an attempt to find human cultural
material associated with the large mammalian remains. Under
the direction of Dr Alison Stenger those efforts were richly
rewarded in a series of archaeological digs conducted over
several summers into the millennium.
In 2002, several thousand bones have been extracted from the
Woodburn bog sites as well as fossil bird shell and bone,
insects, amphibians and a wealth of vegetable material including
leaves wood and fossil pollen. The center piece of their labor
however is several strands of human hair that date back to
between 11,000 and 12,000 years into the past.
Now ,at last, a complete picture of the Willamette Valley
Pleistocene or "ice age" environments is emerging.
The localities and fossils have attracted international attention
and a team of paleontologists and archaeologists are engaged
in unraveling this most interesting chapter of Oregon pre-history.
Written by Dr. William Norton Orr, July, 2002
Bibliography:
Excerpts from Dr. Orrs presentation on prehistoric animals
in the Willamette Valley, June 2002, at the Salem Public Library
with his permission, and from excavation work at the Woodburn
bog mentioned in the article above.
|