The unrest and hard feelings between the Indians and settlers in Middle Park gave rise to an inevitable conflict the last week of August, 1878. About forty Utes, led by Piah and Washington, started to set up camp in William Cozens’ meadow, near Fraser, taking fence poles to make fires. Cozens drove them off, telling them to replace the poles and leave. The Utes moved down valley about five miles to a spring not far from Junction Ranch (named for the junction of the Rollins Pass and Berthoud Pass wagon roads).

There, Johnson Turner, who leased that land, became increasingly uneasy as the Indians were drinking heavily and expressing anger that Ouray given away their land in treaties with the white man. They wanted Turner to pay them for the hay he was cutting. They tore down his fences for firewood, turned their 100 horses into his meadow, and set up camp. They also laid out a race track on drier ground about a mile way.

Turner complained to the sheriff, Eugene Marker, who rounded up a posse of men, intending to remove the Indians or at least convince them to move on. Accompanying him, on September 1, were Frank Addison, a transient prospector, John Stokes, T.D. Livingston, and Frank Byers.  The posse found only women and children at the camp, since the Ute men were at the race course. Marker, the sheriff, ordered the encampment searched for firearms and when the Ute men returned, an angry confrontation ensued. 

Tabernash and Frank Addison exchanged threats, and Tabernash jumped from his horse and snatched one of the guns piled on the ground. Frank Addison immediately shot him. Tabernash tried to pull his rifle from its scabbard, but that it became entangled, and Addison then fired twice more. Tabernash slumped over the neck of his pony, which ran away through the willows. Apparently Addison recognized Tabernash as the Indian responsible for the killing several of his companions while trapping furs on Grizzly Fork in North Park six years earlier. 

After this bloodshed, the posse persuaded the rest of the Utes to leave, after they buried Tabernash’s body in a shallow grave. No one was ever sure where Tabernash was buried. There was a rumor that the slain Tabernash was buried in a draw not far from Junction Ranch, but when the Grand County Historical Association excavated the site, nothing was found.

A day later, September 3, on a Ranch near Kremmling, Abraham Elliott was shot while cutting wood, and his horses stolen.  In response, the posse moved north in the direction of the White River Reservation. 60 Utes met the posse, and explained that the culprits were Piah and Washington, neither of whom was a part of the White River band.  Ultimately, the Utes signed a council report, returned horses stolen from the Elliott ranch, while the  ranchers returned guns confiscated from the Utes at Junction Ranch.  The matter was considered legally settled, but outrage and fear continued among the settlers and the Utes of the area.

In 1902, E.A. Meredith, chief engineer for the Denver & Salt Lake Railroad, named the town that had grown up with the building of the railroad, after the slain Ute, Tabernash.

Most serious ranchers had more than one ditch and most built one or more reservoirs. Hilry Harris, Munroe C. Wythe, Samuel H. Burghard, and John A. Coulter entered the first water claim in the county on September 20, 1874. This came out of Sheep Creek above the head of Gore Canyon.

There usually was some natural irrigation; but the challenge of getting the water from the creek required laborious construction of diversion dams, headgates, and ditches, the earliest ditches being dug by hand and often taking up to four years to complete. Later, ditches were dug using teams and scrapers. The grade was figured out initially by simple gravity flow, letting a trickle of water move down the ditch. Soon ranchers refined the process, using a 16’ long board placed with a 1/8" slope, determined by a carpenter’s level. A.F. and Roy Polhamus surveyed a great many of the water ditches, especially those impressive ones in West Grand County, some of which even had tunnels involved. Most small ditches supplied just one ranch, but if a ditch had to cross another ranch, that rancher usually got a share. And some of these ditches were long!

For instance, Dr. Henry Hoagland, on the Blue River, anticipated getting water close at hand from Spruce Creek. Instead, he discovered an old timer had previous rights that forced him to go back into the mountains and build a 13-mile long ditch. Hoagland had figured on spending about $7000; in the end, the actual cost was $26,000! His crew dug the ditch around side hills and across valleys using flumes and siphons. Then his real troubles began. Terrible leaks and washouts occurred everywhere. Finally he hauled in adobe and put this in the bottom of the ditch, rented sheep, and drove them day after day up and down the ditch to pack it. After a couple of years of using this tamping process, the ditch held. Other ditches were even longer. The Church Ditch at Willow Creek and the Wheatley Ditch on the back Troublesome were both 16 miles long.

The Company Ditch (aka the Williams Fork Ditch), eight feet wide on the bottom, was another long one. Built between 1903 and 1907, it cost $44,000 and had a decree for 150 cubic feet / second. The ditch went uphill and down, requiring many flumes and bridges. One flume was actually 1200 feet long! Subsequent breakdowns, leaks, and slides were so frequent and repairs so extremely costly that old-timers have said the reason the Company Ranch went broke about 1920 was the expense of The Ditch. The Lyman Ditch (or the Curtis), started about 1891, was just as complicated as the Company Ditch. Crossing high above the Williams Fork River, the ditch eventually needed cement piers to carry the pipe (1928). This ditch had so many slides, leaks, and washouts, that it had to be inspected once or twice daily! Siphons were required over draws. Flumes, sometimes ¼ mile long, might be 25-30 feet high, and one flume was actually 177 feet high; but these heights were necessary to maintain the elevation.

Flumes, being of wood, rotted and were guaranteed to leak. Sometimes wind blew a portion of the flume down. Finally the county put in big pipes to help the ditches across the Williams Fork. It might be noted that, when water leaked out of ditches, a side benefit was that ranchers along the way could use the "lost" water. Along with the ditches came reservoirs.

Fred DeBerard had four reservoirs on the Muddy: the Albert, the Binco, Milk Creek, and a low one that flooded the Jones place near Kremmling. All were dirt, of course. The Hermosa Ranch on the Little Muddy had water rights through the Sylvan Ditch and Reservoir Company and they built the Sylvan Reservoir dam and the Hermosa Ditch starting in 1911 and completing it by the spring of 1916. The Stein Ditch, started in 1897, was another large ditch, this one later purchased by the Taussig family. These ditches were all built originally to provide water to meadows and fields for ranching purposes. For years, people hauled in water for baths and household use, but that gradually changed. Leon Almirall, near the Horseshoe Ranger Station on the Williams Fork, decided that he wanted water for his home, so he built a 1700’ pipeline to his house, added an inside bathroom, and was shocked when the line froze the first winter – it was only three feet deep. He called in workers who dug down and insulated the line with manure and straw. It froze again. Finally, Almirall gave up and buried the line six feet deep. Now he had his water!

On Ranch Creek in the east end of the county, E.D. Shew cut a ditch upstream from his house, placing it along the edge of the creek, but directing the water back into the main channel near his house. At that point, he put a little water wheel that pushed the water up the hill to his cabins -- and furnished electricity besides. Eventually he replaced the water wheel with a gas engine. There was a similar water wheel, used for the same purpose, up in Hideaway Park.

Water was used to transport lumber as well. A flume ran down the mountain into Monarch Lake, in the days when the Monarch Company was timbering there. There was a flume along St. Louis Creek, carrying lumber from the camps upstream. Perhaps the most ambitious flume ran from Western Box Sawmill. This area is now under Meadow Creek Reservoir. In 1906, the Deisher Lumber Company paid Nathan Hurd for a right of way through his land and built a flume with a 2% grade down Hurd Creek. Logs were placed in the flume and a horse harnessed to the last log. The horse then pushed the logs down the flume with the help of the water. Three years later, the mill was moved to "Sawmill Meadow" on Meadow Creek.

In 1911 construction on the seven-mile-long Vaver Flume began, with 117 cubic inches of water allotment. This flume ran down Meadow Creek and over to Tabernash, carrying partially processed logs for further manufacture. A flume rider checked along the way, making sure there were no jams, and phone line allowed the rider to report troubles. Hikers can see remnants of both the St. Louis Creek flume and that one coming down Meadow Creek today.

The prospect of discovering a remnant from a 10,000-year-old stone age society that inhabited Colorado's Middle Park so long ago seemed remote at best - while the suggestion that a prized Folsom point could somehow materialize before our very eyes appeared all but impossible.  For one thing, it was the last day of excavating for the summer at the Barger Gulch archaeological site and the ten member scientific team would soon be packing up and heading back to their ivory towers at the University of Wyoming and the University of Arizona.

Barger Gulch is a desolate spot that the federal Bureau of Land Management (BLM) oversees. It is hard, parched dirt dabbled with sagebrush as far as your eyes can see across the flat valley - a haven for all manner of bugs and other forms of native wildlife. In winter, the place turns to the opposite extreme as temperatures plunge to minus 40-degrees and howling winds whip up ghostly images of snow that swirl eerily across the land. This is Middle Park, a high mountain basin with roughly the same geo-political boundaries as Grand County. It encompasses some 1,100 square miles of unforgiving territory flanked on three sides by the formidable wall of the Continental Divide and its terrain soars high over the Great Plains into the thin, alpine air up to altitudes of 13,000 feet above sea level. What would induce these primitive Americans to trek all the way up here without so much as horses for transportation? How would they have survived the brutal winters with only primitive tools and clothing?  And why in the world would they ever want to settle in such a barren, god-forsaken place as Barger Gulch? 

This site could well prove to be one of the most significant archaeological discoveries of its kind in North America, according to BLM officials who oversee the project here. In just three years of work in a relatively small excavation area, investigators unearthed more than 18,000 artifacts - a staggering number ten times that discovered at typical Folsom sites. And this is only one of four sites in the same vicinity.  In addition to Barger Gulch and Upper Twin Mountain, discoveries include the Jerry Craig and Yarmony Pit House sites. Most of these were occupied by peoples described by archaeologists as Paleo-Indians, a catchall term for ancient humans that inhabited North America; Yarmony Pit House post dated Paleo-Indians by about 3,000 years.

But long before Paleo-Indians ever set foot on the Continent, Middle Park was a prehistoric menagerie; 20-million years ago, it was the stomping grounds for prehistoric rhinoceros, three-toed horses, camels, giant beavers, and even small horses. Creatures known as oreodonts also romped across the mountainous terrain. These vegetarians, ranging in size from small dogs to large pigs, fed on grasses and green, leafy plants. In fact, the skull of one of these animals was discovered recently in the vicinity of Barger Gulch. These long extinct, hoofed animals resembled sheep, but were actually closer to camels, and were common in the western U.S. This latest discovery is remarkably well preserved; while the bones have turned to stone, the smooth, hard enamel that encased the animal's teeth is still intact. 

Humans arrived in North America much later - about 12,000 years ago - as the last Ice Age of the Pleistocene Epoch made its exit. These first Americans crossed a land bridge from Siberia to Alaska and began populating the entire Continent; experts believe it is possible they also arrived on boats following the Continental Shelf into North America. Folsom people are best known as nomadic, big game hunters who chiseled out their spear points and finished them off with a distinctive, artistic flourish - a unique groove, or flute, that runs lengthwise along the face that has become the symbol of this Paleo-Indian culture. They honed the tips of these primitive weapons surprisingly sharp for killing frenzies that were necessarily up close and personal: they herded their prey into traps before launching their spears - and archaeologists suspect there was just such a bison ambush site near Barger Gulch. The quarry just over the rise is a gold mine of raw materials, including fine-grained Kremmling chert and abundant Windy Ridge quartzite, which provided a never-ending supply of top grade stone. "It makes sense," explains Todd Surovell. "You would want to camp where you could get as many raw materials as possible within a short distance. That's where you're going to park yourself for awhile."

The bulk of these tools originated with local material, but investigators have found some 200  "exotic" items noticeably out of place at Barger Gulch. One is a distinctive piece of yellow, petrified wood that came from 93 miles away as the crow flies, near the town of Castle Rock on the Colorado plains. Another is a large biface that was brought up from the Arkansas Valley, some 60 miles south. "They worked on it up here in one place and turned it into two, maybe three projectile points," notes Surovell. "One of them broke during manufacture and we have two pieces that fit exactly together."

Fitting these and thousands of other pieces together is what archaeologists do when they get back to the lab. The process begins on site where investigators photograph each find and record its exact location within the excavation block. This gives the team a visual reference to help recognize activity patterns - a way to connect the dots of Folsom society.  But the specks come to an abrupt stop, as if they suddenly run into a solid wall. "If we could figure out that this represented the wall of a structure, that would be really special," he explains. "Nobody's even been able to do that before in a site of this age in North America." Just then, a graduate student pops his head inside the door. "You want to be a camera man?" he asks Surrovell. "What do you got?" "A Folsom point," he replies with a broad grin. We rush over to the site where Waguespack has dug a narrow shaft down the north wall of the excavation pit and hit pay dirt - a Folsom point that remains half buried in the stratum of rich soil.

The mountains of Grand County may not boast any of the famous “fourteeners“ (14,000 feet and above), but Middle Park is defined by some of the most majestic ranges in the state. These include parts of the Front Range, Gore Range, Rabbit Ears Range, and the Williams Fork Mountains.  

The only range Grand County can call entirely it's own is The Never Summer Range.  It's highest point is Mount Richthofen (12,940 feet).  Other major peaks include: Mount Howard (12,810 feet), Mount Cirrus (12,797 feet), Mount Nimbus (12,706 feet), and Nokhu Crags (12,485 feet). The name Never Summer is translated from the Arapahoe name, Ni-chebe-chii, which means “the place of No Never Summer“.  The cloud names of Cirrus and Nimbus, and Stratus and Cumulus were the idea of James Grafton Rogers, a founder of the Colorado Mountain Club.  

The Never Summer Range stretches for ten miles from Cameron Pass to Bowen Mountain.  This range is darker and harder due the tremendous heat produced when the peaks were a localized center of volcanic activity.