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Missing From The System? Utah's San Rafael Swell

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The view from the Cedar Mountain Overlook on the northern end of the San Rafael Swell exposes just some of the reasons why the Swell has been mentioned worthy of national park status down through the decades. Emery Country Travel Bureau photo.

Editor's note: Across the country, there are many spectacular landscapes that would fit appropriately within the National Park System. This article is the latest in an occasional series that looks at some of these places.

In places, the brush strokes are delicate, exquisitely formed, the work of a master. Others, though, are more roughly fashioned, in some cases pecked or scratched into the rock face's thin veneer.

The images, dating back thousands of years, are priceless. So, too, is the scenery in the landscape within which these pictographs and petroglyphs exist. It is a landscape of staggering natural beauty expressed by soaring cliffs, canyons compared to the grandest one in the country, minarets, and reefs of rock that tell a fascinating geologic story.

The plein aire art museum where you can find these works? Central Utah's San Rafael Swell.

Near-Perfect Preservation Conditions

The general aridness of central Utah gets the credit for preserving the rock art forms that, perhaps, date back 7,000 years, and which have been referred to as the state's Sistine Chapel. Though some appear childish, and others have been covered with images from nomadic cultures that followed the original artists through the millennia, the figures tell intriguing, at times hard-to-cipher, stories that still beg explanation.

The images inspired some intriguing names: "Head of Sinbad" was attached to a figure topped by a wriggling snake, while "Black Dragon" was spawned by a pictograph that some think looks much like a winged dragon.

Some of the oldest images fall under the category of "Barrier Canyon" rock art, a folder Dr. Polly Schaafsma, one of the country's most-renowned experts on Native American rock art, assigned the images to in the 1960s when she was part of an effort to catalog what existed in the southern Utah canyons that the pending Lake Powell were about to inundate.

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Rock art at Buckhorn Wash in the Swell. Photo courtesy of Emery Country Travel Bureau.

While researching a story for Smithsonian magazine some years ago, I learned that some archaeologists who have studied the Barrier Canyon images believe they were created between 1900 B.C.and A.D. 300. But Alan Watchman, a research fellow at Australian National University, told me his radiocarbon analysis dates some of them to the Early Archaic period, from about 7430 B.C. to 5260 B.C.

Another archaeologist, Phil Geib, also was of the opinion that the earliest image might date to the Archaic period of roughly 8,000 B.C. to 1,000 B.C. He notes that a figurine similar in style to Barrier Canyon rock art was recovered in a cave in Utah above a layer of soil dating to around 7500 B.C. A distinctive style of sandals directly associated with the figurine, he says, dates to around 5400 B.C.

While some Barrier Canyon images can be found in Canyonlands National Park, as well as Glen Canyon National Recreation Area, the San Rafael Swell is rife with them. Though many are not easily found.

 

But Archaic-era images aren't the only ones within the Swell. There are some from the Fremont Culture that lived in the area from about 700 A.D. to 1300 A.D., and more recent images crafted by Ute artists and Spanish explorers, and even an inscribed name purportedly made by that 19th Century criminal, Butch Cassidy. 

More modern history counts structures and roads built by the Civilian Conservation Corps, overly ambitious ranchers trying to coax a living from the spare landscape, remnants of uranium mines tapped during the Cold War.

Taken together, this history -- modern and prehistory -- tell wondrous stories in a demanding landscape.

Spectacular Landscape

Surrounding this graphic history is a landscape that is jaw-dropping. 

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Within the Swell you'll find some spectacular scenery thanks to its underlying geology. Photo via Big Stock Photo.

The San Rafael Swell is an 80-mile by 30-mile bulbous protuberance of rock in south-central Utah that was ratcheted into place by geologic machinations some 60 million years ago. The resulting geology is an open-air classroom, a layer-cake of strata named Coconino Sandstone, Kaibab Limestone, the Triassic Age Moenkopi and Chinle Formations, Wingate, Kayenta, and Navajo Sandstones.

These rockbeds deposited over millions of years have colored the Swell with buffs, reds, tans, greys, blues, yellows, whites, and oranges. And within some of those formations are paleontological treasures -- the Cleveland Lloyd Dinosaur Quarry, which holds a rich cache of fossilized prey and predator dinosaur remains, lies near the northern end of the Swell, and field research elsewhere in the Swell has turned up amazing finds. 

 

According to the Utah Geological Survey, remains of Acrocanthosaurus, a giant carnivore of the Early Cretaceous that was nearly as large as Tyrannosaurus, turned up in the Cedar Mountain Formation not far from Cleveland Lloyd. It possessed "enormous teeth adapted for cutting flesh," the Geological Survey notes.

As the landscape rose, it was transformed into a maze of sorts by erosion. So cut, twisted, and inhospitable appearing is the Swell that when mountain man Jedediah Smith peered into it briefly in 1826, he figured there was no reason to explore it further and kept on going. What the mountain man found to be a barren wasteland is viewed to many today as spectacular.

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Rock art in Black Dragon Canyon. Photo courtesy of Emery County Travel Bureau.

It was back in 1935 that many Utahans felt the same way, and at the time the Utah State Planning Board briefly lobbied for creation of a "Wayne Wonderland" national park, a 360,000-acre park named after Wayne County, one of the counties that the Swell is found in. 

In 1936 Bob Marshall, founder of The Wilderness Society, identified nearly 2 million acres of roadless area in the general vicinity of the Swell that should be protected, and in 1980 the Interior Department identified seven potential National Natural Landmark sites in the same area. More recently, the Emery County Development Council at one point proposed that 210,000 acres of the Swell be set aside as a national park. About in the early 2000s, then-Gov. Mike Leavitt proposed that 620,000 acres be set aside as a national monument.

But the movement never could gain traction in Utah, where 67 percent of the landscape is owned by the federal government, a percentage that in the state's political circles spurs contempt. 

Today part of the U.S. Bureau of Land Management landscape, the San Rafael Swell might not carry the "national park" imprimatur as do nearby Capitol Reef and Canyonlands national parks, but it is no less worthy of tag.  Those who believe the Swell needs greater protection, perhaps as a unit of the National Park System or else as officially designated wilderness (it currently contains seven Wilderness Study Areas), cite mining, grazing, and off-road vehicle impacts as threats to the landscape. Some rock art panels have served as shooting targets. 

Recreational Opportunities Abound

But the lack of a more protective land-management status hasn't prevented recreation in the Swell. Indeed, near the southern end of the Swell stands Goblin Valley State Park, and on BLM lands nearby the beautifully eroded Little Wildhorse and Bell slot canyons wiggle through the Swell.

Along with designated ORV routes, the Swell offers endless miles for horseback use, backpacking edens, mountain biking, and a river -- the San Rafael -- popular with paddlers when runoff swells it, usually from May into mid-June, depending on the previous winter's snowpack. The Green River, which runs through a portion of the Swell, is much more reliable for white-water cowboys and cowgirls looking to buck the rapids.

 

There's a wonderful BLM campground near the brink of the Wedge Overlook, which looks over a jagged canyon nearly 1,000 feet deep and which is locally referred to as the Little Grand Canyon.

Rock art aficionados appreciate the Swell for being home to some of the Southwest's most curious rock art, such as the renowned Buckhorn Wash Panel, the Head of Sinbad images, the Rochester Panel, or the collection of images found in Black Dragon Canyon.

Venture into the Swell and you'll find buttes and mesas, stone arches and minarets, grassy meadows and box canyons, streams and springs, and possibly be able to retrace routes Butch Cassidy took while fleeing posses.  Too, the Swell is home to more than 200 desert bighorn sheep, peregrine falcons, feral horses and burros, Bald and Golden eagles, red-tailed hawks, and prairie falcons.

The prominence of the Swell -- its landscapes and rich archaeological and paleontological resources --  came up when the Obama administration was considering prospective landscapes for protection under the Antiquities Act. That Act allows presidents, without congressional approval, to designate landscapes for protection as national monuments.

"... the San Rafael Swell is a .. . giant dome made of sandstone, shale and limestone -- one of the most spectactular displays of geology in the country. The Swell is surrounded by canyons, gorges, mesas and buttes, and is home to eight rare plant species, desert bighorns, coyotes, bobcats, cottontail rabbits, badgers, gray and kit fox, and the golden eagle," reads an internal draft document prepared for Interior Department officials.

"Visitors to the area can find ancient Indian rock art and explore a landscape with geographic features resembling those found on Mars."

While political push-back from Republicans in the U.S. House of Representatives seems to have squelched the administration's consideration of the Swell, and any other landscapes, for protection as national monuments, it hasn't lessened any of the wonders that you'll find in the Swell.

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Comments

Appearances can be deceiving, Anon.  Come out here.  Spend some time.  Learn more.

Remember, there are wise, sound, less harmful ways to use our resources properly.  That's all any of on this side of the fence are asking.


Back to the topic at hand...It would be great if the area got Wilderness designation. But at least the WSA's help protect the land in the interim. I, for one, don't think it should be made a National Park. If the BLM is managing the area well and protecting it, then why change it?
The Park Service is stretched thin as it is. They also tend to over-develop their lands to make them accessible to everyone. A surprising portion of National Park visitors only come to get their stamp or drive through. They spend an hour, simply so they can check ‘seeing’ another National Park off their to-do list. Would increasing this type of visitation to the San Rafael Swell help it at all?
This is a special place, however, the National Park Service aren’t the only ones who can care for it properly.


Lee Dalton:
Appearances can be deceiving, Anon. Come out here. Spend some time. Learn more.

Remember, there are wise, sound, less harmful ways to use our resources properly. That's all any of on this side of the fence are asking.

 All one needs to do is read the history of Utah towns or even look at the names of two counties to get a better idea. Would there be a "Carbon County" without extensive coal mining? Or "Iron County" without iron mining. Moab and Park City are historic mining towns.

Yeah - there are wide swaths of nothingness, but the state does have lots and lots of open pit mines throughout.


Moab and Park City are historic mining towns.

 So in your opinion, Moab and Park City are "pillaged"? 


It would be too much to say either were pillaged -- and indeed, you're twisting words a bit -- but Park City came close to having a Superfund designation due to mine tailings, and Moab has a Superfund site due to mine tailings.


Kurt Repanshek:
It would be too much to say either were pillaged -- and indeed, you're twisting words a bit -- but Park City came close to having a Superfund designation due to mine tailings, and Moab has a Superfund site due to mine tailings.

          I'm pretty sure that Lee's use of "pillage" was tongue and cheek.

However, there are some rather long term implications whenever there is mining - especially uranium mining like there was in the Moab area. I understand the cleanup of the Atlas Uranium Mill (now known as the Moab Tailings) is going to be upwards of $700 million. I'm thinking there could be some closed mines that can have their cleanup delayed because there are higher priority sites, but this one is urgent because of the potential for the radioactive materials to leach into the Colorado River. That would be absolutely disastrous if there was a wholesale leach which included uranium. And yes - that water you see right next [about 800 ft] to the pile (with all its leaching radon and other radioactive materials) is the Colorado River.

Here's a different angle, where the height of the pile is more readily noticed:

Here's the site on Google Maps. Just play around with the settings - especially satellite and/or zooming out to see how close this is to Moab and Arches NP. It's maybe a mile from the entrance to Arches NP.

http://maps.google.com/maps?q=38.599727N,109.597612W&hl=en&sll=38.599183...

Park City has issues too, as Kurt said.

http://www.epa.gov/region8/superfund/ut/richardsonflat/index.html


I'm pretty sure that Lee's use of "pillage" was tongue and cheek.

No doubt there were isolated examples of non-envionmentally friendly practices in the past - mostly out of ignorance.  But your example of a uranium mine that was closed nearly 30 years ago is hardly supportive of Lee's contention that the current mindset in Utah is to "multiply, multiply and pillage"  In fact, turning the mine over to the DOE and working on moving the tailings to a safer place suggests just the opposite. 
The fact is that Utah is one of the least developed states in the nation.


To help with the argument of mines in Utah.   Lets just look at active mines only, you can just go to a handy site that pulls data from the USGS.  http://active-mines.findthedata.org/d/d/Utah     I think it listed 131 active mines,  For Inactive mines its only estimates but

Approximately 10,697 abandoned hardrock mines exist in Utah according
to the Bureau of Land Management and Forest Service estimates. For more information visit: State of Utah, Department of Natural Resources/Division of Oil, Gas, and Mining
I would say there is plenty of mining in Utah or has been.  The only other states that look to be in the same league are Arizona, Nevada, California and possibly Idaho.   http://www.abandonedmines.gov/mapdata.html
These just cover counts and dont' discuss impacts of mining like tailings, potential water pollution etc.  If you wander any of those states listed above and make the claim there hasn't been much resource exploitation, you just aren't paying attention. 


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