DRGW History and Information  

  Trip Report: Ghosts of the Uintah Railway - Chapter 1
  Mack to Carbonera
Uintah Milepost 0.0 to 20.0
  From: Ghosts of the Uintah Railway
Dates: Nov 29, 2007 Author: Nathan Holmes

Uintaite, or more commonly known by its trademarked name, Gilsonite, is a natural asphalt that, for all intents and purposes, looks very much like coal in its natural form. Unlike coal, however, it is resinous substance with a low melting point. Some early reports of its discovery describe trying to use it as coal, only to find that it burned poorly and would melt, sending flaming streams of liquid hydrocarbons in all sorts of undesirable directions. It occurs in only one place in the world - the Uintah Basin of eastern Utah and western Colorado. While similar substances are found elsewhere, uintaite is unique, differentiated by its specific gravity and low melting point. Found in deep, vertical, nearly-pure veins, geologists believe that uintaite is the result of petroleum from the region's underlying oil sands seeping up through cracks in the overlying sandstone. Over time, the more volatile elements would evaporate, leaving a solid asphaltic resin.

The story of the Uintah Railway really begins in 1885, eighteen years before the line was actually constructed. Samuel Gilson, having received samples of an unusual substance found within the Ute Indian Reservation of eastern Utah, quickly realized that this natural asphalt had commercial potential in a variety of applications. The only problem was that the reserves were inside the reservation. Through a good deal of lobbying, Gilson's interests had the ore-rich lands removed from the reservation through an 1888 act of Congress. The Gilson Manufacturing Company began large scale commercial extraction in September of that year, with some 3000 tons shipped by wagon to Price, Utah, where it was hauled to market via the Rio Grande Western's narrow gauge trains.

The substance proved so useful, and thus commercially valuable, that wagons were too slow and inefficient to meet demand the early 1900s. Gilson's mining concerns needed a railroad. They initially approached the Denver & Rio Grande about building a branch, but were turned down, as the D&RGW deemed it too risky a venture to build such a long branch that would be completely dependent upon a single commodity. Having few other options, they decided to go ahead with their own line, and in 1903, the Uintah Railway Company was born.

The route would connect with the Rio Grande Western at a point near Crevasse, Colorado (the point would become Mack, CO), and proceed northwesterly over Baxter Pass to the Black Dragon uintaite vein, some 50 miles away. The Black Dragon vein was chosen due to its significant size and proximity to the railhead. In light of the grades and curvature of the proposed route, the Uintah was to be constructed as a narrow gauge (3 foot) railway, despite the fact that all of the connecting roads had been standard gauged thirteen years earlier. By October of 1904, all 53.3 miles of the originally planned railway were in place, and the Uintah commenced operation doing what it was intended to do - hauling out uintaite.

To say that the Uintah is steep and curvy is a disservice to those who designed and built it. To say that it approaches the physical limits of adhesion (ie, non-cog) railways, and possibly the limits of sanity as well, would be significantly more accurate. In the six miles from the railroad's shops at Atchee to the summit of Baxter Pass, some 5 miles of that are unrelenting 7.5% grade. The back side of the pass is somewhat better - six miles of 5% grade. Within this section, there were two curves exceeding 65 degrees of curvature, and several more exceeding 60. (65 degrees of curvature is an effective radius of about 87 feet, for reference... Some sources say the Moro Castle curve may have been 75-80 degrees initially, and enlarged when the railroad realized that they simply could not operate on that.)

At least until 1926, the railroad operated as three parts, with normal rod-type steam locomotives operating from Dragon to Wendella (the northern end of the 5% climb). Power was then changed to one of the railroad's two-truck Shay locomotives - a type reknown for their pulling power - for the trip over Baxter Pass to Atchee. South of Atchee to Mack, the grade and curvature moderated and rod type engines were again used. Even the mighty Shays were only rated for 60ish tons over the hill, and rod engines could barely make the trip at all.

The first major change to the Uintah came in 1911, when the route was extended further north to Watson, UT, and a branch run westward to new mines near Rainbow, UT. Over the next decade, these steel tendrils would be extended a few more miles as more mines came online, such as the Barlow, Colorow, and Thimble Rock mines in 1918, and later the China Wall Mine in 1927. This would be the final extent of the Uintah. While there were plans drawn up for extending the railroad towards new deposits at Bonanza and perpetual talk of reaching Vernal for general freight, these never panned out. A combination of better roads and trucks, as well as improved standard gauge service at Craig, CO, due to the completion of the Moffat Tunnel, unwittingly conspired to limit any further growth of the Uintah.

The road, facing financial problems in the 1920s due to higher labor costs and aging equipment, decided that new motive power was the answer. In 1926, the railroad asked Baldwin for a solution - an engine that could operate around the railroad's tight curves, pull tonnage over the steep grades, and do it better than the aging Shays. What they got was #50, an articulated 2-6-6-2T that weighed in at 236,000 pounds and produced around 42,000 pounds of tractive effort. It could operate at reasonable speeds over the entire line, best a Shay in tonnage by at least 50% on the grades of Baxter Pass while only taking half the time, and reportedly did it all with maintenance costs less than one Shay. (Note: Although often referred to as such, they are not Mallets. Each of the four main cylinders was directly fed with high pressure steam, rather than recycling high pressure exhaust through low pressure cylinders in a true Mallet.) Within a few months of 50 proving itself, a second 2-6-6-2T was ordered - 51. Ten-thousand pounds heavier than 50, this unit would take the title of being the largest and heaviest narrow gauge steamer built.

Even the mighty 2-6-6-2Ts could not save the Uintah from lean revenue during the Great Depression and increased competitive pressure from trucks and the D&SL connection at Craig. To add to it all, the mines served by the railroad were starting to play out, with new deposits located on the north side of the rugged White River Canyon. On 24-Aug-1938, the railroad petitioned the Interstate Commerce Commission for abandonment of the route. By 1939, only a single train each week would ply the line, and on 8-Apr-1939, abandonment was approved. The last revenue train left Mack northbound at 0810h on 16-May-1939, concluding nearly thirty five years of operation. By August of that same year, the scrappers were already working their way south from Watson, and by early 1940, the railway was just a memory.

For those unfamiliar with the route, I've put together an interactive map of the line to help you acquaint yourself with it.

Today, much of the old grade has become a public road, and in dry weather, can easily be explored by any vehicle with good ground clearance and reasonably deep tire tread (due to the loose silty dirt that forms much of the road surface). This is something best done only after some period of dry weather, though, as my guess is the road surface can quickly turn into a muddy quagmire after rain. Don't expect any great speed, though - the road is narrow, steep, winding, and in places, hideously rough and deeply rutted. I'd strongly recommend printing off a copy of Bill Pratt's excellent Uintah tour guide. This is what I used to start planning my trip, and found it invaluable. You'll also want to consider taking a Delorme topo map (or similar) and possbily Rodger Polley's "Uintah Railway Pictorial", volumes 1 and 2, along with you, as these will help you figure out exactly where you are, and what railroad-related sites may be around you. As a final note, fill your gas tank before you leave Mack, make sure you have a good spare tire, and take food and water with you. Much beyond Mack, there's no cellphone service, so you'll need to be able to handle whatever comes up out there on your own. Don't let that scare you off, though - exploring the Uintah is a relaxing, interesting all-day trip along one of Colorado's most unique narrow gauge routes.

Although I've never met any of these individuals, I'd like to take a few lines to offer thanks the following: To Mr. Henry Bender, for capturing my interest in the Uintah with his original book, "Uintah Railway - The Gilsonite Route". To Mr. Rodger Polley for his two wonderful volumes, "Uintah Railway Pictorial", Volumes 1 and 2 - their included maps, photos, and town layouts were invaluable in indentifying things I was seeing along the way. To Mr. Bill Pratt, with his detailed driving tour guide to the Uintah, without which I likely would have spent much more time fumbling around with the map and missed half the stuff I was out there looking for. Thank you all for the efforts you've put into teaching us newcomers about the Uintah Railway - when I say this trip wouldn't have happened without you, I mean it.



Photo 1
This is what it's all about - deposits of natural asphaltic hydrocarbons known as uintaite (or by its more common trademarked name, Gilsonite), useful for making all sorts of stuff.
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Photo 2
The Uintah/Rio Grande narrow gauge grade is visible to the north side of old US Highway 6 west of Mack. This is just west of town, looking back east in the early morning.
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Photo 3
Another view of the grade profile, as it passes through a streambed west of Mack, CO. While railroads shared the same grade for a few miles west of Mack, the D&RG/RGW narrow gauge was long gone by the time the Uintah was built.
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Photo 4
Looking south, towards where the Uintah split off to head north from the old D&RG/RGW narrow gauge grade. The Uintah grade can be seen running diagonally towards the photographer in the center of the picture - the old D&RG/RGW grade is indiscernable, but in the background.
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Photo 5
Looking north along the Uintah grade from a point just north of where it diverged from the D&RG/RGW grade.
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Photo 6
From the same point as the previous two shots, you can see the old D&RG/RGW grade headed west across the desert towards Utah. When the route was standard gauged in 1890, this section of sharp curves and steep grades was eliminated in favor of the current route through the Colorado River canyon between Mack, CO, and Whitehouse, UT.
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Photo 7
The road north over Baxter Pass joins the old Uintah Railway grade at Uintah milepost ~6.4.
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Photo 8
At numerous points along the route, the road diverges from the old grade, typically to bypass missing trestles. This is one of those points, somewhere between MP 6.4 and 9.0. I'm on the road, and you can see the grade heading across the streambed across the middle of the frame.
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Photo 9
The road, running alongside the Uintah grade (raised to the right) at approximately milepost 9.
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Photo 10
There's not a lot left of the Uintah out here, aside from a lump in the dirt. I'm standing atop the grade, looking north towards Atchee and the Book Cliffs at around milepost 9.
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Photo 11
The north end of bridge 9-A (I think...) The south end is long gone, cut away by a large amount of erosion.
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Photo 12
Looking north along the road (built over the grade here) near milepost 10.
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Photo 13
The remains of bridge 11-B. There was a small (600 ft) siding near here, called either Salt Wash or Sprague, depending on the era.
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Photo 14
Looking south from on the grade at approximately milepost 12, where the road and grade come back together.
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Photo 15
Around where Uintah milepost 15 would have been, there's a view of Public Service Corp's Baxter Compressor Station, which handles the natural gas pipelines that run along the Uintah's general route today.
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Photo 16
As seen at milepost 15.3, we're starting to leave the high deserts and head up into the Book Cliffs, via the Salt Creek canyon.
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Photo 17
A rock formation to the west of the route known as the Crow's Nest. My notes scribbled down while driving only said: Don't remember why it's important, but I remember seeing it in Polley's book.
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Photo 18
Looking northward around milepost 17.5 (just north of trestle 17-A, according to my notes)
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Creative Commons License This work is copyright 2007 by Nathan D. Holmes (maverick@drgw.net), but licensed under a Creative Commons License. This allows and encourages others to copy, modify, use, and distribute my work for non-commercial purposes (only), without the hassle of asking me for explicit permission or fear of copyright violation. I encourage others to consider CC or other Open Content-style licensing of their original works.

All photographs in this trip report were taken with a Canon EOS 40D using either a Canon 24-105mm F4 L IS/USM or a Canon 100-400mm f4.5-5.6L IS/USM.