A cast of part of the track slab showing several trackways of two different sizes of pterosaurs.

A 900 lb. slab of rock with some of the best preserved pterosaur (flying reptile) tracks ever recognized was discovered on State Land in the San Rafael Swell near the town of Ferron by a team from Marietta College (Ohio).  This slab of rock from the Jurassic Summerville Formation preserves at least 9 separate trackways of 2 different sizes of pterosaurs that were walking along a tidal flat near the shore of the Curtis Sea.  We know the tracks were made by pterosaurs because, in addition to the hind foot prints, there are tracks made by the wings.  So, unlike birds that walk bipedally on their hind feet while folding their wings against their bodies, pterosaurs walked quadrupedally using their folded up wings to support the front of their bodies.  This site and the tracks were documented in a scientific publication in 2004 (Mickelson and others, 2004).

Because of the scientific importance of this slab, a team from the Utah Geological Survey (UGS) collected it in 2004 so that it could be placed in the Natural History Museum of Utah (the repository for all of the fossils collected by the UGS from public lands in Utah).  Due to its large size, this slab has been stored at the UGS’s Utah Core Research Center since collection.

Recently, the Natural History Museum of Utah agreed to loan the slab to the American Museum of Natural History in New York City for display in a new exhibit on pterosaurs.  On November 14, a team from Terry Dowd Inc. (a fine art packing company) came to the UGS to package the slab in a custom crate so that it could be transported by truck to New York.  The slab was cradled in ethafoam so that it will be well protected during the long drive to New York which began on November 19.  Eventually, the slab will be returned to the Natural History Museum of Utah for display.

Twelvemile Canyon, Wasatch Plateau, Sanpete County, Utah.
Photographer: Rich Giraud

Island Lake at the head of Twelvemile Canyon, Wasatch Plateau, Sanpete County, Utah.

Mirror lake, Uinta Mountains, Duchesne County, Utah
Photographer: Ken Krahulec

Mirror Lake nestles among 11,000-foot peaks of the western Uinta Mountains. The rocks of the Uintas, consisting largely of sandstone and shale of the Precambrian-age Uinta Mountain Group, contain microscopic bacteria nearly 800 million years old that likely represent Utah’s oldest fossils.

By: Robert F. Biek and Janice M. Hayden

The Kanarraville quadrangle includes the southern part of Cedar Valley and parts of the adjacent Kolob Terrace, Harmony Mountains, and North Hills. It straddles a particularly instructive area of structural overlap between the Sevier fold thrust belt-represented by the overturned, east limb of the Kanarra anticline exposed at the west edge of the Kolob Terrace-and the Basin and Range physiographic province, whose east margin corresponds to the Hurricane fault zone at the base of the plateau. Regional ash-flow tuffs erupted from calderas in western Utah and eastern Nevada are present in the Harmony Mountains and North Hills; in the Harmony Mountains, these tuffs are involved in a large gravity slide shed off the nearby Stoddard Mountain laccolith, which erupted to produce an ash-flow tuff now partly buried by the gravity slide.

This CD contains the geologic map at 1:24,000 and a 31-page booklet describing the geology of the Kanarraville 7.5-minute quadrangle. All of the files are in PDF format. The latest version of Adobe Reader is required to view the PDF files.

GET IT HERE

 

Spring-fed Pruess Lake, Snake Valley, Millard County, Utah.
Photographer: Matt Affolter

Middle Springs, Fish Springs National Wildlife Refuge, Juab County, Utah
Photographer: Matt Affolter

Many of you may already know the Utah Geological Survey has a Facebook page. Well, did you know that you could win a 2014 Calendar of Utah Geology by liking our page? Now you do! We’re giving away one of our gorgeous 2014 calendars to the 2,000th person to like our Facebook page! We appreciate all our followers and want to say thank you for joining our Facebook group. By liking our page you’ll get the same great pictures, articles, and geology news you get right here on our blog, and you can quickly share them with all your Facebook friends. Plus, you can send us your favorite Utah geology picures, and connect with other fans of Utah geology. If you already like our page, tell your friends to like us, too! If one of your friends happens to be our 2,000th like, maybe they’ll share the calendar with you! After all, what are friends for?

AND if you happen to be a Twitter user, we’re also giving away a calendar to the 800th follower! Twitter is a great way to get geology pictures, info, and news quickly!

So, now it’s time for you to ask your friends, family, neighbors, coworkers, and the occasional friendly stranger to go online and like the UGS Facebook page or follow the UGS on Twitter. Our 2014 calendar is amazing and it could be yours for FREE! Keep an eye on the numbers and good luck!

Like us here: UGS Facebook

Find us on Twitter here: UGS Twitter

Info on the calendar here: 2014 Calendar of Utah Geology

nationalparkstraveler.com

What did the Colorado Plateau look like 250 million years ago? That’s a question geologists hope to shed some light on via an ambitious project that is pulling rock cores up from as much as 1.5 kilometers down into the plateau’s belly. The Colorado Plateau is an expansive region, taking in parts of Colorado, Utah, Arizona, and New Mexico. Within this geologic province are some of our most iconic national parks: Arches and Canyonlands, Bryce Canyon and Zion, the Grand Canyon and Petrified Forest to name the most recognizeable. What makes them so stunning is the geology from which they rise.

READ MORE

 

 

Great Salt Lake, Tooele County, Utah
Photographer: Tom Dempster

Solar evaporation pond at Great Salt Lake, Tooele County, Utah

Many of you may already know the Utah Geological Survey has a Facebook page. Well, did you know that you could win a 2014 Calendar of Utah Geology by liking our page? Now you do! We’re giving away one of our gorgeous 2014 calendars to the 2,000th person to like our Facebook page! We appreciate all our followers and want to say thank you for joining our Facebook group. By liking our page you’ll get the same great pictures, articles, and geology news you get right here on our blog, and you can quickly share them with all your Facebook friends. Plus, you can send us your favorite Utah geology picures, and connect with other fans of Utah geology. If you already like our page, tell your friends to like us, too! If one of your friends happens to be our 2,000th like, maybe they’ll share the calendar with you! After all, what are friends for?

AND if you happen to be a Twitter user, we’re also giving away a calendar to the 800th follower! Twitter is a great way to get geology pictures, info, and news quickly!

So, now it’s time for you to ask your friends, family, neighbors, coworkers, and the occasional friendly stranger to go online and like the UGS Facebook page or follow the UGS on Twitter. Our 2014 calendar is amazing and it could be yours for FREE! Keep an eye on the numbers and good luck!

Like us here: UGS Facebook

Find us on Twitter here: UGS Twitter

Info on the calendar here: 2014 Calendar of Utah Geology