Curious Nature: A tale of two ranges continued | VailDaily.com
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Curious Nature: A tale of two ranges continued

An epic history

Nathan Boyer-Rechlin
Curious Nature
Traversing a high ridgeline between the Spider and the Fly, above the Booth Creek drainage in the Gore Range.
Nathan Boyer-Rechlin/Courtesy photo

“Hi, my name is Randall Streufert from Summit Geology, and I’m here to answer all your questions.”

I’ve never received such an intriguing voicemail. Not even those targeted Facebook ads promise something so grand. Remarkably, in this case it turned out to be true.

A few months ago I set out to write an article about the geology of our two local mountain ranges, the Gore and the Sawatch. I was curious why the Gore is so steep and jagged while the Sawatch resembles the northern remnants of the Great Wall. Much to my frustration, even the internet couldn’t yield definitive answers, and I was just left with more questions, which brings us back to that voicemail.



What followed was a deep dive into geologic history that felt more like reading a fantasy novel than my college textbooks. After a call back and another hour of geologic storytelling, I did indeed have answers.

If you’ve been taught anything about Colorado’s geologic history, it probably went something like this: 265 million years ago the ancestral Rockies rose to heights rivaling, and perhaps exceeding, today’s peaks. In the following 150 million years these mountains quickly eroded and inland seas advanced and receded, depositing the sandstone and limestone we see throughout the Eagle River Valley, until 60-70 million years ago when the Laramide Orogeny formed the modern Rocky Mountains. Shortly thereafter, Vail erected Gondola One and here we are.



While not completely wrong, that synopsis is similar to recapping the “Lord of the Rings” trilogy in three words. You’ll get the gist but miss the story.

In the tens of millions of years since the modern Rockies first rose (and not even close to the heights they reach today), antecedent rivers have cut dramatic canyons through rising ranges, entire regions rose thousands of feet, volcanoes erupted, a mountain range was lost only to re-emerge, and glaciers sculpted dramatic landscapes from previously rolling peaks.

Looking out over the Upper Piney drainage in the northern Gore Range.
Nathan Boyer-Rechlin/Courtesy photo

In only 50 million years, the ancestral Rockies rose and completely eroded. After 70 million years, our modern Rockies are as high as ever.

Like the rest of Colorado’s peaks, the Sawatch was formed in the Laramide. Then, 30 million years ago, the activity along the faults that shaped these peaks halted. Subsequent uplift heightened the entire Colorado Plateau and made mountains out of molehills, giving the Sawatch more than its fair share of 14ers, but the core of these peaks remained unchanged.

The granite that forms the Sawatch was eventually buried under thousands of feet of sedimentary rock, only to be re-exposed through millions of years of erosion, revealing the broad summits of crumbling rock we see today. Recent glaciation sculpted wide bowls and cirques, but these features are predominantly confined to northeastern aspects, a result of prevailing winds depositing snow and feeding glaciers there.

The Gore Range is less tame. These peaks rose along faults left over from the ancestral Rockies and have remained active since. Even 20 million years ago the Gore’s jagged peaks may have looked much like they do today.

Members of the Walking Mountains Hiking Club climbing the slopes of Mt. Huron in the Sawatch Mountain Range, near Leadville.
Nathan Boyer-Rechlin/Courtesy photo

The spine of this range is a horst, a sharply raised block bounded by the Blue River and Gore faults on either side. While the anticline that forms the Sawatch has been dormant for 30 million years, recent uplift along these faults has been measured at only 5 million years old. The steepness of the horst and fault-block formation combined with continual uplift and recent glaciation has resulted in the solid rock and steep, jagged appearance that defines these peaks.

At its most simplistic, the difference between these two ranges is age. As Randall likes to say “What’s really outrageous” is that everything we see in Colorado today looks like it does because of a 10-million-year-old uplift. And “10 million years just ain’t [anything] in geologic time.”


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