Give this article a quick listen!
knau.org
A dinosaur recently found in southern Utah has reshaped paleontologists’ ideas of the fierce group of carnivores known as tyrannosaurs.
Give this article a quick listen!
knau.org
A dinosaur recently found in southern Utah has reshaped paleontologists’ ideas of the fierce group of carnivores known as tyrannosaurs.
Here’s another installment of “Spot the Rock”! Can you guess where this is? Like us on FACEBOOK or follow us on TWITTER to participate!
UPDATE: Location Revealed
Crystal Geyser is located on the eastern bank of the Green River approximately 3.5 miles downstream from Interstate 70. It is a geologically unusual site to visit, as it is a cold-water, carbon-dioxide-driven geyser as opposed to the geothermal geysers you would see at Yellowstone. In the past, Crystal Geyser’s eruptions were notably higher and more frequent than what they are today. As seen in the video the entire area is draped with beautiful travertine (calcium carbonate) which makes it a gem of a place to put on your bucket list.
cbsnews.com
It was one of the biggest, scariest dinosaurs that ever roamed the Earth, a giant predator that prowled Europe millions of years ago.
The dino track recently stolen from Moab is not alone in the vandalism that happens in the area. The BLM is working to prevent theft and other vandalism from ruining the fossils and tracks in Moab. You can help in these efforts too!
ksl.com
This is an exciting new tool on the horizon for planning ahead.
hjnews.com
Developers and homeowners will have the opportunity to look at detailed, updated flood hazards along the Wasatch Front and in Cache County in a couple of years.
Little Cottonwood Canyon, Wasatch Range, Salt Lake County, Utah
Photographer: Mike Hylland; ©2011
The “”wrinkled” surface of a rock glacier on the floor of Maybird Gulch hints at the Ice Age glacial activity that carved this tributary to Little Cottonwood Canyon. Ice below the ground surface, now likely all melted away, once allowed the bouldery deposit to imperceptibly flow down the valley floor, forming the arcuate ridges at the ground surface.