ksl.com

Leslee Maki says she can’t believe what happened to her property after a storm moved into the area Monday night and a debris flow shut down part of U.S. 6.
“We still don’t know where everything is,” Maki said. “Forty-five minutes is all it took.”

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deseretnews.com

sltrib.com

The gash in the hillside recedes from a dusty road in 20-foot steps, revealing a towering bounty of hydrocarbons embedded in stone deposited 50 million years ago when algae-filled Lake Uinta covered northeastern Utah.

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In Christchurch, New Zealand in February, 2011, a magnitude 6.3 earthquake struck six miles from the city center. The sandy type of soil present in the area caused the ground to basically liquefy during shaking.

UGS Geologist Chris DuRoss is interviewed by KCPW: Explore Utah Science to discuss the hazard of liquefaction we face right here in the the Salt Lake Valley.

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Earthquake Risk in the Salt Lake Valley

Michael Hylland, a geologist at the Utah Geological Survey, examines disruptions in the subsurface soil at a trench dug through a section of the Wasatch Fault

 

deseretnews.com

Residents and agencies are racing to fight debris and water flow caused by an unusually wet “monsoon season” in Utah that has caused slides and the threat of slides from Huntington to Alpine and across the Wasatch Front.

Salt Lake City averages 0.61 inches of rain in July, according to National Weather Service readings taken at Salt Lake airport. As of July 17, readings there totaled 1.15 inches and the month has weeks to go.

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deseretnews.com

For the third time in five years, a Grand Staircase-Escalante National Monument employee was honored by having a newly discovered dinosaur named for them.

The British scientific journal Proceedings of the Royal Society announced Wednesday that a new species of horned dinosaur unearthed at the monument is called Nasutoceratops titusi.

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sltrib.com

sunews.net

Bureau of Land Management has rescheduled the presentation “Microbes, Mars & Moqui Marbles” on Tuesday, July 16. The program is a special Grand Staircase-Escalante National Monument (GSENM) Walks and Talks Lecture Series presentation to be held at the BLM Kanab Visitor Center, located at 745 East Hwy 89, in Kanab, Utah.

Beginning at 7 p.m., Dr. David Loope will reveal new insights into how microbes affect geology. Based on his recent research on the Navajo Sandstone within GSENM, Dr. Loope will explain how microbes, that have lived just below Earth’s surface for at least three billion years play an important part in the development of Moqui Marbles on Earth, as well as other planets, including Mars.

 

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sltrib.com

Early explorers and pioneers often found precisely the right words to describe land formations as they named features they encountered while trekking west.

On July 27, 1850, for example, Robert Chalmers led a group of about 300 gold miners headed to California across the Bonneville Salt Flats using the Hastings Cutoff. Seeing a mountain range devoid of perennial streams and with sparse vegetation, he called them the Barren Mountains.

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deseretnews.com

An Estonia company that claims it has perfected turning oil shale into fuel oil during the past 30 years wants to mine rock from a remote region of the Uintah Basin, tapping 2.6 billion barrels of oil in the decades to come.

That staggering production, 50,000 barrels of oil per day, would represent one-third of Utah’s liquid fuel consumption and is touted to emerge from a processing and refining plant that would put power back into the energy grid.
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aapg.org

Geologic intervals that may have looked a bit ho-hum when pierced by the drill bit on its way to the Real Target can, on second look, yield some pleasant surprises.

The Uteland Butte Member of the Eocene Green River Formation in the Uinta Basin in Utah is one of these.

It’s the basal member of the Green River, above the Upper Paleocene to Lower Eocene Wasatch Formation, which is predominantly a sandstone with red, green and gray shales deposited in a fluvial setting.

In contrast, the Uteland Butte is indicative of a lacustrine environment and is mainly limestone, dolomite, organic rich calcareous mudstone and siltstone, with some thin sandstones, according to AAPG member Michael Vanden Berg.

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