White River Glacier | Steve Baldwin | geologist
The Melting Point
by
Jack Boulware
Guides get to climb to the summit of Mount Hood every week, he
says, so glacier tours are more fun for them.
We climb inside a Sno-Cat and chug up the permafrost of the Palmer
ski run, the treads easily navigating the crunchy snow. Halfway up
the trail, we encounter Bowker and some of the folks from
yesterday's class walking back down the slope with glum
expressions. "They turned back," observes Bates. I never find out
why.
Weather is often the key factor. My trip here was postponed for two
weeks because of snow and rain.
"You could come up," Steve Baldwin, the guide company's
codirector, had told me over the phone. "But it would be like
being inside a ping-pong ball."
Fortunately, today there are supposed to be clear skies. The
Sno-Cat stops at 8,500 feet, the top of the Palmer ski lift, and
lets us out. We hike up another 200 feet toward the summit and then
put on our crampons, cut across the slope laterally, and step onto
the White River Glacier.
I immediately notice the distinct odor of sulfur, which seeps from
fumaroles in the main crater above us; the gas stains the rocks
yellow. Although the mountain hasn't erupted in a few hundred
years, it's still technically a volcano - comforting thought.
I look back at the buildings far below. They look like Monopoly
pieces. Over time, the glacier has carved out four moraines of
churned-up dirt and rocks, which finger their way down to the tree
line. You don't have to be a geologist to realize that the ice mass
we're standing on was once two-thirds larger.
"The old-timers around here will tell you it used to go all the way
to the lodge," says Bates.
It's difficult to find someone at Mount Hood who doesn't believe in
global warming and glacial retreat, because everyone here is on
mountains every day, and they see it for themselves.
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