A Short History of Logan River

Over fifteen thousand years ago, the glacially fed Logan River was flowing into Lake Bonneville which covered most of the NW quadrant of the state and completely filled Utah’s Cache Valley.

The river met the ancient Lake Bonneville some distance up Logan Canyon so it was much shorter. Animals that lived along the river included saber-toothed cats, woolly mammoths and giant ground sloths.

About ten thousand years later, after Lake Bonneville had disappeared, the Logan River meandered across the old lake bed and the Shoshone Native American tribe made Cache Valley their home.

Shoshone Women and Children. Photo taken in 1870, Unknown photographer. Courtesy USU Digital History Collections.
Shoshone Women and Children. Photo taken in 1870, Unknown photographer. Courtesy USU Digital History Collections.
Frank Howe, chairman of the Logan River Task Force, adjunct associate professor, and university liaison for Utah Division of Wildlife Resources said, “When people say ‘let’s return Cache Valley to how it was naturally’ they don’t realize the valley [had been] managed by the Shoshone for thousands of years before the settlers arrived.”

The Shoshone burned the valley frequently to drive the Bison and provide better forage for their horses. This impacted the vegetation across the valley and along the river. Instead of large stands of tall trees, the river was lined with shrubs which responded better to fire, hence the valley’s first name Willow Valley.

Water flowing in Right-hand Fork one of the tributaries of Logan River. Courtesy & Copyright Shauna Leavitt
Water flowing in Right-hand Fork one of the tributaries of Logan River. Courtesy & Copyright Shauna Leavitt
During this time the flow and movement of the Logan River was much different, in part because of the beaver families who built their homes and dams up and down the waterway. The dams created ponds whose waters seeped into the valley bottoms raising the water table and saturating the sponge. Joseph Wheaton, associate professor of the Department of Watershed Sciences in the Quinney College of Natural Resources explained, “the saturated ground increased resilience to drought, flood and fire.”

In the early 1800s trappers arrived in the valley.

Michel Bourdon was one of the earliest trappers to see Cache Valley around 1818. The river was, for a short time, named after him. A few years later, Ephraim Logan arrived in Cache Valley. He and many other trappers attended the Rocky Mountain Rendezvous along the Bourdon River in 1826. Shortly thereafter, Logan died during one of his outings and the area’s trappers decided to rename the river Logan, in his honor.

Trapping for the fur industry severely impacted the beaver population and the Logan River. The dam building beavers were almost trapped to extinction because of the European fashion demand. Luckily, fashion trends changed before beaver were extinct. However, the virtual elimination of beavers fundamentally changed the character of the Logan River to this day.

Man fly-fishing in Logan River, Logan Canyon, Utah, July 21, 1937. Courtesy of USU Digital History Collections.
Man fly-fishing in Logan River, Logan Canyon, Utah, July 21, 1937. Courtesy of USU Digital History Collections.
In the 1850s the first settlers arrived in Cache Valley. Their arrival had a large impact on Logan River. Within a year they began constructing the first canal for irrigation.

Logan’s Main Street about 1920, Courtesy of Darrin Smith
Logan’s Main Street about 1920, Courtesy of Darrin Smith
Around the turn of the 19th century it became apparent the grazing and timber need of the settlers had been hard on the Logan River and the surrounding landscape. Albert F. Potter surveying the Logan River watershed for President Theodore Roosevelt, reported the canyon had been overgrazed and its timber overcut. The timber, at the time, was used for railroad ties and to build Logan City.

Logan Canyon about 1910. Four waterways: the aquaduct which was used for power generation, the canal, a water way that ran behind the building which had been part of the old Hercules Power Plant, and the Logan River. Photographer H.G. Hutteballe, Courtesy of Darrin Smith Photo Collection
Logan Canyon about 1910. Four waterways: the aquaduct which was used for power generation, the canal, a water way that ran behind the building which had been part of the old Hercules Power Plant, and the Logan River. Photographer H.G. Hutteballe, Courtesy of Darrin Smith Photo Collection
As the valley’s population grew, so did the demand for Logan River water.

Color enhanced photo 1910 photo of Logan Canyon Courtesy Logan Library
Color enhanced photo 1910 photo of Logan Canyon
Courtesy Logan Library
Over the next few months, Wild About Utah will continue this series on the Logan River to tell the stories about its ecology, social value, and how humans have worked together to make it a community amenity not just a canal.

We hope you’ll join us as we learn more interesting facts about Logan River.

This is Shauna Leavitt and I’m wild about Utah.

Credits:
Photos: Courtesy & Copyright ©
Audio: Courtesy & Copyright © Friend Weller, Utah Public Radio
Text: Shauna Leavitt, USGS Utah Cooperative Fish and Wildlife Research Unit, Quinney College of Natural Resources, Utah State University
Co-Authored by: Frank Howe, chairman of the Logan River Task Force, adjunct associate professor, and university liaison for Utah Division of Wildlife Resources.

Sources & Additional Reading

Geologic Map of the Logan 7.5′ Quadrangle, Cache County, Utah, Utah Geological Survey, 1996, https://ugspub.nr.utah.gov/publications/misc_pubs/mp-96-1.pdf

Williams, Stewart J. Lake Bonneville: Geology of Southern Cache Valley, Utah, Geological Survey Professional Paper 257-C, US Department of the Interior, 1962, https://pubs.usgs.gov/pp/0257c/report.pdf

Biek, Bob; Willis, Grant; Ehler, Buck; Utah’s Glacial Geology, Utah Geological Survey, September 2010, https://geology.utah.gov/map-pub/survey-notes/utahs-glacial-geology/

Utah’s Desert Paradox

Utah's Desert Paradox: Upheaval Dome Courtesy Wikimedia Licensed under the Creative Commons Attribution-Share Alike 3.0 Unported license.
Upheaval Dome
Courtesy Wikimedia
Licensed under the Creative Commons Attribution-Share Alike 3.0 Unported license.
Have you ever wondered why the redrock landscape of Southeastern Utah ebbs and flows, why the exposed layers of sedimentary rock seem to rise and fall in crests and troughs like so many waves across the surface of the sea? Well, the answer, surprisingly enough, can be found through investigating the ancient seas that once covered vast swathes of Southeast Utah more than 300 million years ago.

Utah's Desert Paradox: Salt Diapir Courtesy Geology.com
Salt Diapir
Courtesy Geology.com
Back then, the allotment of Earth’s crust that would one day become the Beehive State was located along the western edge of a chain of islands that rose above a shallow, equatorial sea. 15 million years of sea level rise, recession, and evaporation left behind layer upon layer of salt deposits that would eventually measure nearly a mile thick. These salt deposits were subsequently covered and crushed by vast layers of sediment, rock, and debris eroded from the flanks of the Ancestral Rocky Mountains. Under the tremendous weight of these additional layers, the now lithified layers of salty stone softened and squirted west like toothpaste through a tube until they collided with deep tectonic faults. Here, they erupted upward, forcing the younger, denser rock layers into anticlinal arched domes, called diapirs, resembling the crests of waves. This phenomenon works much like a waterbed across the landscape: heavier rock layers squirting salt into thinner layers of rock that then bulge upward before they are subsequently squashed downward again by even more sediment, rock, and debris. The subterranean movement of salt through rock layers becomes a game of geologic whack-a-mole.

Utah's Desert Paradox: Cane Creek Anticline Canyonlands National Park Courtesy USGS, Public Domain, Photo id: 249988
Cane Creek Anticline
Canyonlands National Park
Courtesy USGS, Public Domain, Photo id: 249988
I recently visited Dead Horse Point State Park between the town of Moab and Canyonlands National Park. On the eastern edge of the rising mesa on which the park is located, one can look out across millions of years’ worth of sedimentary deposits toward the Cane Creek Anticline, an obvious salt diapir that seems to rise straight out of the Colorado River. Perhaps the most famous (and most contested) salt diapir in the area, though, is that of Upheaval Dome, located in Canyonlands National Park. An alternative theory to the creation of Upheaval Dome maintains that an ancient meteor impact created the crater where Upheaval Dome is located. However, the fracturing of the younger Wingate Sandstone that occupies the higher rock layers is indicative of a salt diapir formation. Yet, debate rages on!

Utah's Desert Paradox: Paradox Basin Overview Courtesy & Copyright Buffalo Royalties
Paradox Basin Overview
Courtesy & Copyright Buffalo Royalties
Funnily enough, the discovery of this layer of ancient salt deposits that wreaks so much havoc below the Earth’s surface was made in the collapsed center of an ancient salt diapir. In 1875, geologist and surveyor Albert Charles Peale, at the time yet unaware of the salt tectonics at work beneath the Colorado Plateau, noted the paradoxical course of the Delores River. As Peale and his colleagues would find out, the geography of the collapsed salt diapir caused the river to chart a perpendicular course through its valley as opposed to a parallel course as is most often taken by rivers. This paradox of fluvial geomorphology gave the place its name, Paradox Valley. Likewise, the subsequent discovery of an entire basin of ancient salt deposits borrowed the name “Paradox.” Now, we know the salty layer as the Paradox Formation of rocks found throughout the Paradox Basin of the Colorado Plateau.

Paradox Valley Courtesy & Copyright GJhikes.com
Paradox Valley
Courtesy & Copyright GJhikes.com
This paradox of fluvial geomorphology can also be found where the Colorado River cuts a perpendicular course across the Spanish Valley of Moab and is indicative of a vast layer of ancient salts below the surface, waiting to further morph the landscape into crests and troughs of rocky waves that ebb and flow across the landscape. The next time you venture into this part of our great state, stop and consider the remnants of ancient seas below your feet that project their image into the surface of the redrock above.

I’m Josh Boling, and I’m Wild About Utah.

Credits:

Photos: Paradox Basin Overview, Courtesy and Copyright Buffalo Royalties
Upheaval Dome Courtesy Wikimedia, https://commons.wikimedia.org/wiki/File:UpheavalDomePanorama.jpg
Salt Diapir Courtesy Geology.com, https://geology.com/stories/13/salt-domes/
Paradox Valley Courtesy GJhikes.com, https://www.gjhikes.com/2017/10/long-park.html
Cane Creek Anticline Courtesy USGS (Photo id: 249988 – Canyonlands National Park, Utah. Cane Creek anticline, looking northeast toward the La Sal Mountains from Dead Horse Point. The Colorado River cuts across the crest at the middle right, above which is Anticline Overlook. A jeep trail and part of Shafer dome lie below. Figure 13, U.S. Geological Survey Bulletin 1327. – ID. Lohman, S.W. 10cp – lswc0010 – U.S. Geological Survey – Public domain image)
Text: Josh Boling, 2018

Sources & Additional Reading

Davis, Jim, Glad You Asked: Why Does A River Run Through It?, Glad You Asked, Utah Geological Survey, https://geology.utah.gov/map-pub/survey-notes/glad-you-asked/why-does-a-river-run-through-it/

What is a Salt Dome?. Geology.com, https://geology.com/stories/13/salt-domes/

The Colorado Plateau

000000The Colorado Plateau: Colorado Plateaus Province US Physiographic Province Courtesy US National Park Service
US National Parksbr />
Colorado Plateaus Province
US Physiographic Province
Courtesy US National Park Service

If you have ever been to a museum you have witnessed historical items that may be hundreds, or thousands of years old. When we look outdoors at the natural geology of our planet earth, we may be witnessing things that are hundreds of thousands, or even millions of years old.

I realize that there are some people who disagree with the aging with which some scientists label various mountains and canyons, so let’s just settle on the fact that some of these places are very, very old.

There is only one place in the United States where a person can put his feet and hands in four different States at the same time, and that place is called The Four Corners. The story behind this incredible area deals with the formation of what is known as the Colorado Plateau. This area covers 130,000 square miles in Utah, Colorado, New Mexico, and Arizona. If you have ever been to any of Utah’s Mighty Five National Parks you are on the Colorado Plateau, but it’s much more than that. There are 3 national recreation areas, 10 national parks, and 16 national monuments all included in that amazing geologic formation.

Scientists say that millions of years ago tropical seas covered the Plateau region where layers of limestone, sandstone, silt and shale were continually deposited. When upheavals began to lift the plateau, and mountain-building events occurred, volcanic eruptions also accented the western area. Eras of various rivers, lakes, and inland seas continued to leave sediment deposits known as the Chinle, Moenave and Kayenta layers. Later, a huge desert formed the Navajo, Temple-Cap and Carmel formations.

Tectonic activity began to uplift the Plateau nearly two miles high and slightly tilt it to the west. Rivers and streams responded with increased downcutting and erosion which revealed scenic wonders from narrow slot-canyons to huge cuts in the earth’s surface. Perhaps you have heard the term “Grand Staircase” which describes the descent in altitude from Bryce Canyon down to Zion Canyon and further down to the Grand Canyon in Arizona. About ninety percent of the area is drained by just a few rivers including the Colorado, Green, San Juan, Little Colorado and the Rio Grand.

Why emphasize the geology? Besides climate, think how the soil and rock formations determine water retention and flow directions. How water and soil then determines the plant life in an area. And finally, how all three of those components determine what wildlife will exist in that same area.

So the next time you visit Utah’s Mighty Five: Arches, Bryce Canyon. Canyonlands, Capitol Reef, or Zion Canyon, try to picture yourself atop a huge natural table-top with incomparable scenery.

This is Ron Hellstern, and I am Wild About Utah.
 
Credits:

Images: Courtesy & Copyright
Audio: Courtesy and Copyright Kevin Colver
Text: Ron Hellstern, Cache Valley Wildlife Association

Additional Reading

Colorado Plateaus Province, Physiographic Provinces, National Park Service, https://www.nps.gov/articles/coloradoplateaus.htm

Geologic Provinces of the United States: Colorado Plateau Province, USGS Geology in the Parks, USGS, https://archive.usgs.gov/archive/sites/geomaps.wr.usgs.gov/parks/province/coloplat.html

Annerino, John, Colorado Plateau Wild and Beautiful, Farcounty Press, April 1, 2014, https://www.amazon.com/Colorado-Plateau-Wild-Beautiful-Annerino/dp/156037585X

The Canyon

The Canyon: Grand Canyon of the Colorado Courtesy Pixabay, Public Domain
Grand Canyon of the Colorado
Courtesy Pixabay, Public Domain
Here it’s just called, The Canyon, like there is no other. It’s a place we go to get away from, or get into, it. It’s a place that still lets us trust each other’s word, and have plans on when we should be back. For those waiting on The Canyon, we practice patience and balance with our expectations.

For those of us in The Canyon though, we have entered a different, older world. Out here, once up and away from the road, we find what keeps us out late, what drives us home early, and why we go back.

Free from the paved groan, the threshold is passed, and the stories are all in front of us now. We hike old trails, finding new turns, flowers, and shades. We scout new paths blazed by others, leading to timeless vistas, stands, and grounds. We hear strange ancient birds. We smell new familiar fires. We taste life’s grit.

The repetition is not the kind that gets old, going out and discovering; getting dirty, thirsty, hungry, bit up, rained on, or suddenly freezing mid-stride when you hear a branch snap in the wood aside from you and you like that you still have some of that good instinct left, especially in this age.

The Canyon as we know it though did not begin as it now is, nor will remain. In its long winding life thus far, The Canyon has been sculpted by water, want, and what some call westward expansion.

For some of us, we know the story like it was passed down every winter. For others, we quickly learn that it’s worth the stillness.

Trees now grow on what was once an oceanic graveyard: the floor of a great sea. The very stone and rock that lifts dramatically upwards is an elaborate crosscut in geologic history taking place over millions of years. We find deposits of shells, fish, and other oddities as we ascend The Canyon, travelling through time as if in some wonder of which all museums aspire to be.

On and into this grand mountainous slab came Guinavah, The River. The Canyon’s deep V-shape has been carved from Guinavah flowing water over the forgotten seabed once more, finely eroding a channel through, giving The Canyon it’s great bends; perfect for catching an eddied trout or fleeing a pesky cell signal.

The River has been essential for humans as well for thousands of years. When the valley was settled, this time by Easterners in the mid-19th century, Guinavah became known to these settlers eventually as Logan River.

Historically, these lush environs once donned The Canyon’s many great iconic mammals, but the iconic do not easily survive in the limelight. 100 years after Eastern settlement, the once-abundant bison, bighorn sheep, and brown bears were gone. To mark their absence, we have Ephraim’s grave and the imagination.

This said, there is certainly no general void of wildlife in The Canyon. Seeing another traveler is always a blending of curiosity at what they’re up to, and of gratitude that they’re out here too. From here our paths diverge. Some of us continue the hike. Some of us continue the hunt. Some of us back away slowly and keep an eye on the company.

This is the world of The Canyon, a product of its many stories. For us who see the Canyon but have yet to venture in, there are ways in all seasons to experience it. Try a trail, Fork, or any number of Hollows, and visit one of the last quiet places in any one of the unnamed corners of your 1.6 million acre backyard.

It’s a good place out here. Many go out to experience how The Canyon is now, many go out to experience how it All once was, this is an invitation to go and experience of how It can all still be tomorrow.

I’ll see you at the trailhead.

I’m Patrick Kelly and I’m Wild About Utah.
 
Credits:

Images: Grand Canyon Image Courtesy Pixabay, Public Domain
Audio: Contains audio Courtesy & Copyright Friend Weller, Utah Public Radio
Text:    Patrick Kelly, Director of Education, Stokes Nature Center, https://logannature.org
Included Links: Lyle Bingham, Webmaster, WildAboutUtah.org

Additional Reading

Strand, Holly, A Grand Old River, Wild About Utah, July 9, 2009, https://wildaboututah.org/a-grand-old-river/

Strand, Holly, Last Blank Spots on the Map, Wild About Utah, Oct 29, 2009, https://wildaboututah.org/last-blank-spots-on-the-map/

Grand Canyon National Park, US National Park Service, US Department of the Interior, https://www.nps.gov/grca/index.htm
Twitter: https://twitter.com/GrandCanyonNPS

Ross, John F., The little-known story of how one man turned the Grand Canyon into an icon, AZ Central, Phoenix Newspapers, Inc., Gannett…, https://www.azcentral.com/story/opinion/op-ed/2019/01/27/grand-canyon-national-park-icon-john-wesley-powell-history/2651251002/

Hikes, Colorado Plateau Explorer, Grand Canyon Trust, https://www.grandcanyontrust.org/hikes/