Most of the mountain is comprised of the Oquirrh Group, a series of Pennsylvanian-Permian age limestones and sandstones that were deposited in the ocean about 300 million years ago when Utah was at the edge of the North American continent. The rocks have since had an interesting history including deep burial, uplift, and erosion to form them into the current spectacular mountain. Several of the photos here were taken from my backyard and others as I have traveled around the mountain.
Showing posts with label Permian. Show all posts
Showing posts with label Permian. Show all posts
Sunday, April 21, 2013
The Mountain in Our Backyard -- Mount Timpanogos
Here are a few shots I have taken over the years of one of nature's most beautiful mountains: Mount Timpanogos in the Wasatch Mountains of Utah. Even though Timp is only 11,752 feet high, it rises abruptly from Utah Valley, with an elevation difference of over 5,000 feet. The upper parts of the mountain were glaciated during the last ice age, carving the top into its present form.
Most of the mountain is comprised of the Oquirrh Group, a series of Pennsylvanian-Permian age limestones and sandstones that were deposited in the ocean about 300 million years ago when Utah was at the edge of the North American continent. The rocks have since had an interesting history including deep burial, uplift, and erosion to form them into the current spectacular mountain. Several of the photos here were taken from my backyard and others as I have traveled around the mountain.
Most of the mountain is comprised of the Oquirrh Group, a series of Pennsylvanian-Permian age limestones and sandstones that were deposited in the ocean about 300 million years ago when Utah was at the edge of the North American continent. The rocks have since had an interesting history including deep burial, uplift, and erosion to form them into the current spectacular mountain. Several of the photos here were taken from my backyard and others as I have traveled around the mountain.
Labels:
Geologic Timescale,
Geology,
Midway,
Mount Timpanogos,
Pennsylvanian,
Permian,
Provo,
Utah,
Wasatch Mountains
Monday, October 1, 2012
Elephant Toes and other great spots in Dinosaur National Monument
There is more to see in Dinosaur National Monument than the dinosaur bones.
Elephant Toes, an erosional oddity in the Nugget Sandstone of Dinosaur National Monument along the Cub Creek road.
The Green River at Split Mountain campground and picnic area in Dinosaur National Monument. The red rocks in the middle of the photo are the Triassic Moenkopi Formation. The large white rounded mountain to the left is Permian Weber Sandstone, and the ridge of sandstone on the right above the red beds is the Garta Member of the Triassic Chinle Formation.
Here in the foreground the prominent sandstone outcrops on the left side belong to the Gartra Member of the Chinle Formation. The central reddish saddle is the upper unnamed member of the Chinle Formation (lower half of the saddle) and what we are calling the Bell Springs Formation (upper half of saddle). The prominent sandstone on the right that caps the red beds is the Nugget Sandstone.
Tan Nugget Sandstone contrasts with the whiter Weber Sandstone in this photo taken along the Cub Creek Road in Dinosaur National Monument.
Permian Weber Sandstone outcrops along the Green River at Split Mountain campground and picnic area in Dinosaur National Monument.
Triassic Gartra Member of Chinle Formation along road to Split Mountain campground, Dinosaur National Monument.
These last three photos were taken in 2002 on an earlier trip to Dinosaur and are re-posted here from an earlier blog.
Folded Weber Sandstone as viewed from the Blue Mountain road just south of Dinosaur National Monument.
View of Echo Park, the junction of the Yampa and Green Rivers, from Harper's Corner in Dinosaur National Monument.
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