Tag Archive for: Utah Geological Survey

Utah—putting the “Awe” in geology since the Precambrian.

High Uintas Wilderness, Summit County, Utah
Photographer: Chris DuRoss; © 2013

Ostler Peak (12,718 feet) is reflected in a meander bend of the Stillwater Fork of the Bear River in the Uinta Mountains. Thousands of years ago glaciers inundated much of the Uinta Mountains, leaving behind long glacier-carved valleys, steep-sided cirques, and jagged peaks.

Tune in at 12:15 PM today to hear several geologists talk about landslides and development. Jessica Castleton, one of our geologists here at the Utah Geological Survey, will be joining the discussion. Watch this online video chat at sltrib.com. You can also join the discussion by sending questions and comments to the hashtag #TribTalk on Twitter and Google+ or texting 801-609-8059.

sltrib.com

When is it safe to build on a hillside?

READ MORE

Listen to our Deputy Director, Kimm Harty, talk to KSL about the North Salt Lake landslide.

ksl.com

Three homes remain at risk from a landslide that pushed one home off its foundation and damaged a sports facility shortly before 6:30 a.m. Tuesday.

SEE IT HERE

By: William R. Lund

The Utah Geological Survey has revised and updated the Utah fault database used with the Federal Emergency Management Agency’s Hazus Earthquake Model. The Hazus Earthquake Model loss estimation software is designed to produce loss estimates for use by federal, state, regional, and local governments in planning for earthquake risk mitigation, emergency preparedness, response, and recovery. The model’s loss estimates are based on a scenario earthquake on a fault in an area of interest. This revised Hazus Utah fault database provides parameters for scenario earthquakes on significant Utah Quaternary-active faults statewide and for select faults/fault sections in adjoining states. The previous Utah Hazus fault database contained 27 Quaternary faults/fault sections taken largely from fault sources on the United States National Seismic Hazard Maps. This revised database expands the Utah Hazus fault database to include all known Late Quaternary and younger faults/fault segments capable of generating a ≥M 6.75 earthquake in Utah, and includes 82 Quaternary-active faults/fault segments, and nine credible multisegment rupture scenarios.

GET IT HERE

Bryce Canyon National Park from Rainbow Point, Garfield County, Utah
Photographer: Gregg Beukelman; © 2013

 

Arches National Park, Grand County, Utah
Photographer: Don DeBlieux; © 2013

Dissolution of subsurface salt caused the collapse of the Salt Valley anticline, forming vertical fractures in the Jurassic-age Entrada Sandstone. Weathering along the fractures has produced the spectacular fins, towers, and arches in the Devils Garden section of Arches National Park.

“Spot the Rock” is back this week with a riddle! What Utah-“rock” is rarer than diamonds, and more valuable than gold?

Check for updates next week to see the answer! Like us on FACEBOOK or follow us on TWITTER to participate!

UPDATE: Answer revealed

Last week’s “Spot the Rock” was definitely one for our rock hounding friends. And everyone guessed right! Red Beryl is found in Utah, is rarer than diamond, and more valuable than gold.

The gemstone has several different names: red beryl, red emerald, or bixbite. Originally, the mineral was named bixbite, but now red beryl is the most accepted designation. Red beryl is estimated to be worth 1,000 times more than gold and is so rare that one red beryl crystal is found for every 150,000 diamonds.

Read more about the mineral HERE

deseretnews.com

The Utah Geological Survey has released a publication containing 10 geologic hazard maps for an area of western Salt Lake Valley that includes portions of Herriman, West Jordan and South Jordan.

READ MORE

 

San Rafael Swell, Emery County, Utah
Photographer: Robert Ressetar; © 2013

Triassic-age sedimentary rocks in the San Rafael Swell, Emery County.

 

Snow Canyon State Park, Washington County, Utah
Photographer: Daniel King; © 2013

Eroded fragments of a dark ironstone layer contrast sharply against the pale-orange Jurassic-age Navajo Sandstone at Snow Canyon State Park. In places, the iron- and manganese-rich ironstone forms a resistant cap at the top of sandstone columns or pillars called hoodoos.