Wednesday, September 14, 2011
Adventures with Tracy Vallier, August 2011, Hells Canyon near Oxbow, Oregon
On our first day we took two trucks up the Kleinschmidt Grade in Idaho. Steep, gravel switchbacks, a 4-wheel-drive road. Tracy rode in Charles’s truck, Dave & I behind. We stopped on the grade to talk to a couple, Tracy’s friends, from Cuprum, the town at the top. They were on their way out to photograph tombstones at Halfway, Oregon. They record gravesites and post pictures on findagrave for people who want to see where their ancestors are buried.
At the top of the grade we turned out onto Windy Ridge, back toward the south.There was a sign on a locked gate, “Road Closed.” With good reason! But Tracy had borrowed the key from the Forest Service, and we drove along the top of the world in progressively (or regressively) worse conditions. Rocks or trees had to be cleared in some places. At a spot only Tracy could recognize as a turn-off, we parked while they cleared brush out ahead.
Tracy explained that we were headed toward an old homestead that had burned out years ago. He had come across it in 1965, and found that the calendar on the kitchen wall showed the last day circled—and hence, the date that place was abandoned—as September 19, 1936—Tracy’s birthday! So he has a special affinity for the place.
The lane got worse & worse, and the 2 scariest places were sharp curves against the side of the hill, where I feared the trucks would tip over the mountain—bumpy, rough, brushy, and then your uphill side goes up, and you slew around the turn with tires spinning in the bumps and rocks, --I leaned as far uphill as I could. I thought we might be quickly finding our own graves at the bottom of the canyon! And we had to come back that way, too! How would we even turn around?
Finally we came to a point near the old homestead where we could park & eventually turn around, so we parked for the day. Springs still feed the gullies where the old orchards are summer home to Bears!
A lot could be seen from the ridge, before Tracy and Charles descended. What a view!
Dave and I spent the day reading in folding chairs, in the shade of a huge old red fir tree. From the amount of coyote scat at the base, we could assume there was a den under the roots, abandoned for the summer.
When Tracy & Charles climbed back up the mountain at the end of the day, I dreaded the return trip. But it was no worse than earlier—just as scary! Tracy rode with Dave up ahead; they wanted to hurry to the store for ice before it closed. I rode with Charles, and we picked up rocks and leaves and identified a few trees, but these stunning flowers were a mystery until I finally found them in an old book at home.
Rattler! It was on the road at a switchback, and we jumped out of the truck for a demonstration of how to catch a rattlesnake!
Charles had two tools for the job, ready at hand in the front seat. A (very) long- handled hook, to slow down the snake’s progress, and a (very) long- handled grabber, one in each hand. After pressing the hook gently but firmly on the snake’s back, he then squeezed the grabber by its handles, and picked up the snake by the midsection; and he could then raise it off the ground, hugged by the two sides of the grabber. It was a beauty (sorry, no camera), with 9 rattles on the tail, about 2 feet long.
That man was so quick, that the surprised snake never even rattled an alarm. He let me hold the (very) long-handled grabber! The snake squirmed & writhed, but he couldn’t get away, and he wasn’t hurt. When I let him down to the ground and released the grabber, he slithered across the road and into the ditch with never a look back. That was the first time I ever held a rattler.
Second Day. Oregon side of the canyon. We learned about Triassic rocks folding over Permian rocks, near the Snake River.
We drove up an even steeper road than the Kleinschmidt, to drop off Tracy and Charles at the top of the drainage they wanted to study, above Ashby Creek.
Dave & I drove back down to the river to await the descending geologists. Dave caught a few fish, and I read more books.
The blackberries there grew way up in the trees like vines—20 feet tall!—reaching for the sunlight. But knowing that the sweetest berries ripen in the shade, I reached under the leaves and ate all I wanted. I got plenty for a skilletful of blackberry dumplings for supper. And the little yellow plums from trees that have escaped from the homesteads are delicious and so beautiful—not a speck of insect damage (how is that?) I brought home a mess of them to make Canyon Plum Jam.
Friday was a day to rest, so Tracy showed us some beautiful high country in the Wallowa Whitman National Forest. The trail along a creek that he had hiked with Garry many years ago had been washed out, so we went up to Fish Lake, a most gorgeous pristine lake where the Valliers had camped during two summers of field work. Dave caught some fish there (released) and we ate lunch. In clearings at the high elevations we saw grand spreads of brilliant wildflowers. And we scrambled over several roches moutonnée. These are big boulders where geologists can see the marks of passing glaciers that scratched the rocks.
Back at the campground in the late afternoon, two little boys were looking for Tracy after their own day out exploring. When they spotted him at our table, they came running, clutching rocks in their little hands—“Tracy, Tracy! Look what I found!” When their mother came to get them, the little boys resisted, saying, “Tracy’s telling stories about the rocks!”
“Will you tell the story again?”
Old or young, we never tire of hearing the stories from the master story-teller, the super geologist, the lifelong teacher.
Diana Fredley
Thursday, August 4, 2011
Have You Noticed Effects of Climate Change in Hells Canyon?
I’m off next week (August, 2011) to continue geologic mapping in Hells Canyon and am writing this blog to encourage communication and possible action. Maybe you and I can be involved in useful dialogue about the canyon we appreciate and admire. Should we be active, also?
I’ve observed adaptations in Hells Canyon region that are possibly related, at least in part, to climate change. For example, Prickly Pear cacti have migrated steadily upstream from near Pittsburg Landing since the 1960s; noxious weeds are resolutely invading canyon slopes; plants like gooseberries seem to be at higher elevations than when I started working there in 1963; and I don’t drink water directly from creeks and river as I did before the mid-1970s.
I recently studied data and interpretations I found on a web site written by folks from the Union of Concerned Scientists (http://www.ucsusa.org). It is a science-based nonprofit organization, composed of scientists and other citizens who are working for a healthier environment. Look at the website to evaluate their integrity and criticisms of government agencies, Congress, and the current (and past) Executive Branch. I am impressed by their standards and attempts at public outreach. I find their articles and endeavors quite objective, but somewhat depressing because of the conclusions. I invite everyone to read and criticize, but please don’t count on me to be a defender. Communicate directly with the scientists.
Of current interest is a new website about climate change (global warming) at (www.climatehotmap.org) and the effects it’s having on many regions of the earth. Yes, I believe that climate is changing, but no one can definitely say whether the change is permanent and not reversible, or just a cyclical phenomenon. We can’t panic, but we should be deeply concerned about the next few generations of people who will be greatly impacted if changes in weather and ecosystems seen throughout the world are the first wave of a permanent (say a few hundred years) climate change. We should remain skeptical, question data and interpretations of scientists, corporations, and politicians, and become involved in what we think are people-caused influences on climate. Let’s not stick our heads in the sand like ostriches.
In my own field of research, I recall that it took about twenty years for the theory of plate tectonics to be accepted by last holdouts in the Earth Science community. And, we need to remember that there is still an active “Flat Earth Society” (www.theflatearthsociety.org).
If you, the reader, have noticed changes in Hells Canyon weather, water health of rivers, reservoirs, and creeks, and plant and animal ecosystems during the past few decades, let me know. Would Hells Canyon be a good place for scientists and others to set up weather stations and study areas that can be monitored for changes in plant and animal ecosystems? If so, where are the best places and how should we proceed?
Monday, July 25, 2011
The Union of Concerned Scientists
The Union of Concerned Scientists (http://www.ucsusa.org) is a science-based nonprofit organization, made up of scientists and other citizens, working for a healthy environment. Look at the website to evaluate their integrity and criticisms of governmental agencies, Congress, and the current (and past) Executive Branch.
I am impressed by their standards and attempts at public outreach. I find their articles and endeavors quite objective, but depressing because of the conclusions. I invite everyone to read and criticize, but don’t count on me to be a defender. Ask them to do that. Communicate directly with them.
Of current interest is a new website about climate change (mostly global warming) at (<www.climatehotmap.org>) and the effects it’s having on many regions of the earth. Yes, our climate is changing, but no one can say whether the change is permanent and not reversible, or just cyclical and the climate will come back toward the climate we’ve grown used to during the past century and a half. We can’t panic, but we should be deeply concerned for the next few generations of people who will be greatly impacted if changes seen throughout the world are the first wave of permanent changes. We should remain skeptical, question data and interpretations, but not stick our heads in the sand like an ostrich.
In my own field of research, I recall that it took twenty years for the theory of plate tectonics to be accepted by the last holdout in the Earth Science community. And, I have to remember that there is still an active “Flat Earth Society” (www.theflatearthsociety.org). Let’s hope that ultraconservatives and science-ignorant people don’t start a society against climate change. What could it be? Let’s see. How about this one (<climatechangedissenters.org>)?
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