RETIREMENT TRIP #7
Interesting Adventures in Oregon
It was cold this morning when we got up in Christmas Valley. Not cool, but cold. Andy went to the local market for coffee and.
A young man said, “You’re a lot tougher than I am.” He had on a winter coat.
Andy, dressed in tee shirt and jeans, answered, “No, I’m just
dumb.” Even he agreed it was cold.
By the time we left the motel, the temperature had warmed to 50
degrees. We would be driving for a
while, so shirt sleeves would still suffice.
Historic wooden buildings, remnants of Homesteaders in the 1900's, are preserved near Fort Rock State Park. |
Fort Rock Valley Historical Society Homestead Museum, founded in 1984,
was closed. “Come see us in May,” said
the sign. Across the road from Fort Rock
State Park, the Homestead Museum preserved some of the wooden buildings of an
old Oregon town of the 1800’s. The
electrified fence protected the old buildings from would-be vandals, but we
could still take pictures and read a little of the history.
The Enlarged Homestead Act of 1909 fueled a land rush that had begun in
1862. It qualified individuals to claim
320 acres by building a residence and cultivating 40 acres.
The old General Store even has its original gasoline pump. |
Thousands headed west. More than 1.3 million claims were filed in
the U.S. before 1900, but less than half proved successful. The original law had allowed heads of
households, widows and all single people over 21 years old to purchase 160
acres at $1.25 an acre or by paying a $15 filing fee after five years of
residence and cultivation.
Farming came with the Homesteaders in the early 1900’s. Many first-time
Homesteaders in this region arrived after 1909. Life on the land was not
easy. Dryland farming was a laborious
and expensive venture, and many would-be-sod-busters simply left when their
backs gave out or their money ran out.
The advent of World War I saw many drafted into service, while others
left for “good jobs” in the city.
In the distance Fort Rock stands high above the flat plain where the town from olden days is on display. |
Deep plowing and sowing drought-resistant crops became the norm. The development of deep well irrigation
technology in the 1960’s made agriculture profitable. Today, locally grown alfalfa is highly prized
and shipped as far as Japan.
The sun and clouds cast shadows on Fort Rock across the road. It was a great view of the entire lava tuff,
a view we hadn’t seen from inside the state park yesterday.
At Hole-in-the-Ground, another enormous feature in Oregon’s Outback,
the floor of a crater sinks 490 feet below the surrounding ground level and the
rim rises 110 to 210 feet above the surroundings.
From where we stand on the rim of Hole-in-the-Ground crater, the distance across is about a mile. |
A mile across the crater, a trail traced an
arching path up to the rim. We walked
about half way down in the powdery, ashy dirt.
It had been 4.4 miles in, driving on a rutted gravel road without signs,
so we had almost turned back.
As we stepped back onto the rim, a jeep or truck crawled down what we
thought was only a trail on the other side.
“That’s just amazing,” said Andy.
“Look at how slow he’s going!
That road must be awful.”
Interested, we watched for a long time as the far-off explorer, just a
tiny dot even with the zoom lens, walked around the belly of the crater and let
his vehicle cool.
“What we thought was just a trail around the rim is actually a dirt
road,” said Andy. Our little car would
never make it, and we certainly weren’t going to try. But watching was fun.
Hole-in-the-Ground is between 13,500 and 18,000 years old. It was once under water but quite near the
shore of Fort Rock Basin’s ancient lake.
At first scientists suggested it was a meteorite impact crater, but study
showed Hole-in-the-Ground was volcanic, caused when Basaltic magma intruded
near the surface groundwater, turning the water to steam. The steam blew out overlaying rock and
soil. As the material slid back down the
sides, it closed the vent. But the
explosions repeated again and again with blocks as large as 26 feet being flung
as far as 2.3 miles. It’s quite a sight
and delightfully silent!
Paulina Falls in Deschutes National Forest gushes over soft igneous rock that crumbles and gives way. |
We pulled out onto Route #97, lined with traffic and logging trucks.
“We could have stayed at that motel,” said Andy, pointing to a
sprawling Best Western.
“I’m glad you chose the tiny Desert Inn in Christmas Valley. It was
clean and adequate,” I said.
“I like to see how others live,” he explained. “I try to experience different lifestyles to
understand. It also makes me very
grateful for what I have.”
I understood completely.
Ahead of us rose the Cascades, black silhouetted peaks against a
cloud-filled sky. Snow lingered in
patches. Soon there would be more. The weather was changing and cumulus clouds
were moving in.
A visitor from Atlanta captures Andy and Sue together at Paulina Falls. |
In Deschutes National Forest the Forest Service was selective thinning
to minimize the chance of fire. Piles
everywhere waited for burning once the winter snow covered the ground. “They could get snow out of those clouds,”
said Andy, looking at the sky. “They are
heavy enough and high enough in the mountains.”
He was thinking about our already cold morning in the Outback.
From the overlook in Deschutes National Forest, we could see the Three
Sisters and other snow- crowned peaks.
East Lake was cloud covered, but there were still rowboats on the
shore. A few cabins named Goose, Honker
and Gull were occupied, probably for the weekend, and a group of adults,
dressed for winter, picnicked at a table near the lake.
Undergrowth at Paulina Falls is tinged with color as autumn temperatures plummet at night. |
Paulina Falls had two major viewpoints.
We walked the 800 or so feet to the upper view and then tried without success to find a river crossing. The quarter-mile switchback trail to the lower falls looped back and forth to the basalt jumble near the base. Some visitors from Atlanta offered to exchange photographic opportunities. It was nice to get a quality picture of both Andy and me at a beautiful location without using the timer. But we held our collective breaths every time the sun disappeared. A couple sprinkles near the falls from a big grey cloud warned us of what could be.
Andy, Sue and our new friends from Atlanta hike down to the base of Paulina Falls. |
We walked the 800 or so feet to the upper view and then tried without success to find a river crossing. The quarter-mile switchback trail to the lower falls looped back and forth to the basalt jumble near the base. Some visitors from Atlanta offered to exchange photographic opportunities. It was nice to get a quality picture of both Andy and me at a beautiful location without using the timer. But we held our collective breaths every time the sun disappeared. A couple sprinkles near the falls from a big grey cloud warned us of what could be.
Paulina Falls is like a hydraulic jackhammer, pounding away at the
softer rock beneath. But since the
volcano that feeds the falls erupts about every thousand years, the solid rock
that the falls wears away is periodically replenished. Geologists think the falls was 200 feet
downstream about 2,000 years ago. Today
water tumbles over the falls at a rate of about 20 cubic feet per second.
Newberry Crater, a sleeping volcano, is one of few in the world to spew obsidian as a lava during an eruption. |
At the base of Paulina Peak, 7,984 feet in elevation, we took the
Obsidian Flow Trail into the crater.
Obsidian Dome is otherworldly. |
Newberry Crater, a 500-foot climb of stairs ad trail in the center of
the crater to the top of the spewed Obsidian Dome, was actually above the tops
of the Ponderosa pines. Wind whipped in
waves, but intermittently the sun broke through. The trail, a half-mile around the dome,
climbed to the top and circled the inner dome of lava and obsidian. “You wouldn’t want to fall here,” said
Andy. It would literally be falling on
glass.
Obsidian, actually formed from molten silica, is just superheated sand
with a drop of iron oxide. Sand is what
is used to make glass.
Climbing the trail is actually walking on glass. |
Ancient peoples treasured obsidian and used it as money, but it doesn’t
occur in many places of the world.
Here, the explosion that produced the Obsidian occurred about 1,300
years ago. Where people lived near
obsidian, their lives and cultures were transformed. They used the “glassy” volcanic rock to
manufacture tools, weapons, jewelry, sculpture and ceremonial objects.
To ancient Central American people, the importance of obsidian for their economies was similar to that of steel for the economies of modern industrial nations. I found the informative sign fascinating.
Life is tough on the rocks of Obsidian Dome. |
To ancient Central American people, the importance of obsidian for their economies was similar to that of steel for the economies of modern industrial nations. I found the informative sign fascinating.
We stopped once more at the overlook at 3:00 p.m. because the sun was
out with blue sky. The view showed
Lookout Mountain, Mount Bachelor and the Three Sisters far in the
distance. It’s beautiful country.
From inside the crater on the Obsidian Dome we can see the top of the old volcano rim. |
The Don McGregor Viewpoint memorializes a man who cared for and loved the natural world. |
At Big Tree in La Pine State Park, Oregon’s largest Ponderosa pine is
protected. A circle of wooden fencing
keeps visitors from further compacting the soil immediately around the roots of
the 500-year old giant. The age is an
estimate, but the height is measured at 162 feet.
Oregon does an incredible job of establishing and maintaining its state
parks. Other states could learn a lot!
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