Tuesday, September 16, 2014
Not far from our campsite and just a short detour from our route
was the Sumpter Dredge State Heritage Area, so Tuesday morning we
drove up to the site. This part of the Sumpter River Valley had been
dredged for gold in the early 20
th century, just as the
valley stream in Virginia City, Montana had been. In fact, there are
places all over the west where these huge dredges chewed up stream
valleys leaving long hills of gravel, and totally blocking and
redirecting the streams. This park has an actual restored dredge.
Most were stripped and left to rot away in place. Wow! We had no idea
how huge these were! No wonder the results were so destructive. It
looks like a huge three story white boarded hotel on a barge. The
gravel gets scooped up in the front, put on a conveyor belt,
transported through the inside, where it gets sifted to smaller and
smaller sizes to find the gold, and the leftovers moved up a long
conveyor belt high up out the back end, and shot out the back and
redeposited into long rows. The dredge is always sitting in water
from the rearranged stream, and just floats along within the pond
that it makes for itself.
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The Sumpter Gold Dredge |
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Electric motors powered everything - winches, pumps, belts, chains |
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Tail end dump conveyor covered for preservation |
Of course no one did remediation, or stream restoration then, so
100 years later, the mess still remains. Slowly the vegetation,
birds, and animals have been reclaiming it, but it can never be
restored to its original configuration. Sad what we did to these
beautiful stream valleys in our thirst for gold.
The day was heating up and we continued on to the fossil beds.
After stops in the town of John Day for fuel and groceries, we
realized that the day was getting long, and we wouldn't have time to
hike once we got there. Besides, it was sunny and in the 90's! We
made the decision to go to the visitor center, get oriented and put
off the hikes until early the next morning. The monument is in three
non-contiguous units. We decided to visit the two closest ones.
The visit to the L Thomas Condon Paleontology Center with its
great exhibits of the fossils, geology, and history of the area was
very well done. We spent a long time there getting a handle on the
fossil record which runs from 50 million years ago to 5 million years
ago, essentially newer than the dinosaurs, it documents the Age of
Mammals. My one disappointment was that in the two units we chose to
visit there were no fossils to be seen along the trails. Fossil
digging is punishable, and they are vague about where fossils have
been found. The only legal place to dig is behind the high school in
the town of Fossil. Unfortunately, we weren't going that direction.
Greg isn't as interested in paleontology as in the geologic
structure, so he had to drag me out of the center when he got bored.
I love fossils! The idea of seeing something that was alive those
many million years ago is thrilling!
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Volcanic ash deposits of the John Day Fossil Beds - Sheep Rock Unit |
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Beautifully preserved Sycamore leaves from 44 million years ago |
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Palm leaf |
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Ancestral Easter Bunny! |
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Early elephant jaw |
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Fossilized egg |
Greg's Commentary – The John Day Fossil Beds consist mostly of
horizontal or gently dipping beds of volcanic ash with a few layers
of lava and ignimbrite (glowing hot ash and cinders that welded into
a hard rock) that erupted and fell over the landscape of forests and
grasslands at intervals of several thousand years during a span of 50
million years. Between ashfalls of a few to dozens of feet thick,
soils formed that supported a wide variety of plants and animals,
including some of the more charismatic mamalian megafauna like
mammoths, sabertooth cats, and ancestral bears, wolves, horses, and
many others. New ashfalls would kill many animals and preserve both
animal and plant fossils on the previous soil surface. These well
preserved and relatively easily excavated fossils were very
influential to the understanding of geology and evolution during the
early days of the science beginning about 1850. Later investigation
using more detailed and advanced methods, such as radiometric dating,
microfossil analysis (pollen, spores, etc.) yielded a better
understanding of entire ecosystems.
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Looking south at Picture Gorge below Sheep Mountain |
We still needed a place for the night, so we drove north through
the park along the John Day River until we reached the North Fork of
the John Day. Finding a very small BLM campground, Big Bend, along
the river banks we paid our $2.50 and settled in to the sounds of the
river and waited for the sun to set and cool things down.
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Our camp along the North Fork of the John Day |
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