Silverthorne geology: A ‘trapdoor’ story | SummitDaily.com

Silverthorne geology: A ‘trapdoor’ story

BOB BERWYN
summit daily news
Summit County, CO Colorado

SILVERTHORNE ” With the sawtooth quartzite of the Gore Range as a backdrop, Silverthorne geologist Randall Streufert sweeps his hand across the reaches of the Lower Blue and describes the geologic origins of the Gore Range.

“It’s just a giant rock cork that keeps popping up,” he says, describing how the 1.7-billion-year-old rocks have been at the core of the Southern Rocky Mountains since the dawn of the continent.

“Every time there’s a compressional event, the Gore Range pops up. “It’s an old piece of crust that rides up high,” Streufert says.

The peaks that surround Silverthorne have been shaped by unimaginable forces, as great slabs of the Earth’s crust skated into each other, crumpling and heaving.

Careful research on Gore Range peaks shows an interesting story: The bones of the local mountains are much younger than scientists thought until recently.

Streufert explains how he and others use fission track dating to measure the age of exposed rocks. The newest evidence suggests that the valley may be part of a vast and recent rift system extending south into New Mexico, as the crust of the Earth spreads apart.

The landscape around Silverthorne has been shaped by two styles of tectonic deformation, Streufert says, explaining how the story of the present-day mountains bounding the Lower Blue goes back at least 70 million years.

About 40 million years ago, those ancestral Rockies had been flattened by erosion, although the foundational rocks were still in place. Then, in another major geologic episodes, the entire region ” including the Colorado Plateau ” was uplifted about 10 million years ago. That’s when the rivers and streams started their work of carving down through the rock in places like Gore and Glenwood canyons, where the Colorado River cuts through the very heart of the range, giving the landscape much of its current look.

“We’re not sure what caused that uplift,” Streufert says, explaining that the entire western United States was affected by that event, known as an epeirogeny. “That has allowed the streams to exhume what we see today.”

“Colorado was under intense compression,” Streufert says, pointing out the contrast between the steep escarpment of the Gore Range and the much more gentle slopes of the Williams Fork Range on the east side of the Valley.

“Those older rocks were pushed many miles westward,” Streufert says. The Williams Fork range was shaped by a thrust fault, as the ancient basement rocks were shoved up and over much younger sedimentary rocks.

Although it’s not always easy to see through the cover of vegetation, there are places where the contact zone between the dramatically different layers are apparent as you hike up the Williams Fork peaks. On the lower slopes, you’re walking on those younger rocks that were once at the bottom of a shallow sea. As you near the crest of the mountains, you suddenly encounter the much older crystalline rocks.

Much more recently, a different kind of force has been shaping the local hills, Streufert says, explaining how, instead of experiencing compression, the crust of the Earth now seems to be stretching and spreading apart in parts of the West. The Rio Grande Valley, the Arkansas Valley and the San Luis Valley are all signs of that tectonic extension, Streufert says.

“We’ve known about extension the West for some time. What’s new is how much it has extended into the Colorado Rockies,” Streufert says. The evidence has been uncovered through small-scale geologic mapping on a much more detailed level than what has been previously done.

That includes Streufert’s work with fission track dating in the Gore Range near Silverthorne. Hiking up the peaks and taking readings of radioactivity, geologists can determine how long those rocks have been exposed.

“The higher you go in the Gore Range, the longer the tracks,” he says.

Steufert says the essential definition of the Blue River valley is a “half-graben,” the technical term for a valley that is sinking on one side, as the crust spreads apart (along the Blue River fault the Gore side), but remains hinged on the Williams Fork side.

“Only the west side has down-dropped,” Streufert says, likening the geologic action to a trapdoor. Some of the down-dropping came as recently as five million years ago, a mere blink of an eye on the geologic time scale, he adds.

“We’re in a shallow, sediment-filled half-graben. Things are pretty stable right now.

We’re not sure if the extension is still going on,” Streufert says, explaining that those geologic processes don’t currently present any threat of surface upheavals or earthquakes.

“There’s been no recorded seismicity on any local faults,” he says.

The jumble of foothills along the base of the Williams Fork Range includes debris from giant landslides that oozed down the slopes, covering up deposits of cretaceous-age shales. And Silverthorne itself is built on deposits of Blue River alluvium, huge deposits of boulders and gravel washed down over eons.


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