This past weekend I climbed Oregon's Mt. Jefferson with some friends and was reminded of how quickly the past recedes. Twelve years ago I'd climbed the same route but it had looked completely different. Back then the routefinding had been straightforward and direct, right up the center of the glacier. Now twelve years later the crevasses are larger and the route zigzags around them. Most impressively, the upper bergschrund where Jefferson Park Glacier attaches to the mountain has tripled in size. The route used to depend on snow ramps and bridges to get across it. Now the glacier has shriveled like pruned skin and no snow bridge could surmount it. The route goes far right, and up a small headwall into the glacial moat above the schrund. At the current rate of melt, I expect this headwall will be gone within 10 years. After that, who knows if the route will exist?
I expect that within 50 years, there will be very few glaciers in Oregon and photographs like the ones below will seem like something out of a fairy tale. I think that if I live that long and look back on these photos, part of me will feel as if it has melted.
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If this blog is still around in 2058, check back in and see how the photos look from a future perspective. Upon doing so, feel free to let your heart melt...
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