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.

Article contributed by Abbott Fay

The railroaders graded and bridged the trails originally made by the Indians and expanded by the trappers, prospector and stage road builders that following in rapid succession. The

In another lost train story, the No. 3 westbound was seven hours late out of Denver because of a severe winter blizzard.  It crept out of the Fraser Canyon and whistled for the Granby Crossing.  The engineer parked the train intending to wait till daylight to continue on.  In the meantime, the No. 2 eastbound, 2 days late out of Craig reached Corona without passing the No. 3. In the morning, all were amazed to find the train parked "plumb center" of Granby's main street. Later investigation showed that the No. 3 train left the train tracks just east of Granby and traveled almost a mile over frozen highway.  The next day a Chinook wind came up and melted the frozen soil, sinking the train to it's axles in mud. It required the building of 1500 feet of special track to salvage the train. However, some longtime Granby residents say the locale of this incident was the Kremmling flats.

Sources: Roland L. Ives, Folklore of Middle Park Colorado,Journal of American Folklore, Vol. XXXIV, Nos. 211, 212, 1941; Levette J. Davidson & Forrester Blake, Rocky Mountain Tales, University of Oklahoma Press, 1947

 Though few, high altitude water ditches have had a major impact on Grand County's history and economy, there were many early valley ditches transporting this precious commodity from water-right sources to the owner's ranch. However, the threat of transporting great volumes of water from our county to Boulder County via high altitude ditches appeared back in 1889.  Certain interests east of the Divide talked the Legislature into appropriating $25,000, for surveying and developing a 20-mile-long canal over South Boulder Pass to South Boulder Creek.  Amazingly, neither Grand County residents nor very many others opposed this notion.  Luckily the state engineer found the terrain so difficult that not even $2000 was ever spent on the project.


The next effort occurred also in 1889.  This privately financed plan was to develop a two-branched canal system that would move 700 second feet of water to a half-mile tunnel just beneath Berthoud Pass at over 11,000 feet, thence down to Clear Creek and on to the Golden area.  Initial surveys were begun that fall and roads laid out the following year.  The effort bogged down but was resurrected in 1900 under the Agricultural Ditch Co., supplemented in 1902 with the Berthoud Canal Co.  The canal was partially completed by the Frank Church family ranching interests of Jefferson County by 1906.  The ditch, which can be walked today, runs from Second Creek to Berthoud Pass, though it no longer carries much water.  However, the Church Ditch water rights coming from Clear Creek still exist and today are owned by Northglenn.

Proposed in 1890 by the Water Supply and Storage Company of Fort Collins, a greater canal was to be built 1000 feet above the Kawuneeche Valley, that would tap the high tributaries of the North Fork of the Grand River, sending the water over Poudre Pass to a reservoir and then into the Cache La Poudre River and on to agricultural areas east of the Front Range.  The water company, later known as the Grand River Ditch Company, appropriated 525 second feet at the time of the initial diversion in 1892.  (When the Grand River was renamed the Colorado River in 1921, the company was changed to the Grand Valley Irrigation Company.)  The ditch was dug by hand, primarily by Japanese and Mexican laborers.  By 1900, water was flowing eastward.  

By 1906, this major canal, known as the Grand Ditch, and draining water from the Never Summer Range, had a capacity of nearly 358 second feet with 12 headgates within 8 miles, running from Baker Creek to the pass at 10,179 feet, plus a smaller canal carrying 183 second feet within 11 miles, coming from Specimen Mountain.  In 1936, using machinery, the ditch was lengthened to 14 miles.  The Grand Ditch is about 20 feet wide and 6 feet deep, though the water is rarely more than 3 feet deep, and this water irrigates some 40,000 acres in Weld and Larimer counties.

The National Park Service has argued against the allocation of all this water to the canal as it is needed to support plant life and animal habitat.  Becuase river water flow was cut in half, the immediate effect was a reduction in the fish population in the Colorado River.  More recently, a major washout in the ditch caused devastating damage to the slopes below the ditch and to the Colorado River itself.  Hikers climbing up from the valley use the Grand Ditch as a route to the high peaks and lake.  But as viewed from below, the Grand Ditch is often considered an ugly scar on the landscape.

While the origin of the names of many mountains in Grand County has been lost to history, we do know the source of many of the more notable mountains.  The name originations of some mountains of Grand County are as follows:   Adams Peak – Named for either Jay E. Adams who owned a cottage in Grand Lake or Alexander and Louise Adams, original owners of the Grand Lake Lodge.  

Mount Alice – 13,110 ft. – Named in 1911 by request of geologist Dr. William S. Cooper.  Who “Alice” was, was not explained.   Arapaho Peak – Named for the Arapaho Indian tribe who frequented Grand County during hunting season.   Arikaree Peak – Named for the Arikaree Indian tribe by James Grafton Rogers in 1955.   Baker Mountain – Named for John Baker from Indiana, a well known prospector and hunter of the 1850’s and 1860’s.  

Bills Peak – Named after an early settler in the area whose last name was not known.   Bottle Mountain – Named for the bottle shape of the mountain, three miles north of Byers Peak.   Byers Peak – 12,790 ft. – Named for William N. Byers, publisher and editor of the Rocky Mountain News and early promoter of Hot Sulphur Springs.   Mountain Cairns – 10,800 ft. – Named for James Cairns, first storekeeper at Grand Lake.   West Carter Peak and North Carter Peak– Believed to have been named for a member of the original U.S. Geological Survey team.   Cascade Mountain – Also known as Loder Mountain, popularly named for cascading stream.  

The Cleaver – Believed named by early settlers for location between two other peaks.   Coal Mountain – Named for visible coal seam.   Mount Cumulus – 12,725 ft. – Named for cloud formation resemblance.  One of three “cloud” peaks.   Diamond Mountain – Named for rumors of diamonds found there or its shape.  Located four miles East of Muddy Pass.   Mount Epworth – Believed named for a Methodist youth group founded in 1889.  Located east of Rollins Pass.  

Fairview Mountain – Named for scenic view.  Located ½ mile south of Parika Peak.   Mount Flora – Named for fields of flowers on mountain.   Mount George – 12,876 – Named for Dr. R.D. George, a geologist.  Its north spur is Lone Eagle Peak.   Green Mountain – Named for the green trees covering the mountain.   Grouse Mountain – Named for the grouse that inhabit the area.   Hallett Park – 12,713 – Named for William H. Hallett who lived from 1851 to 1947.  The mountain was named in 1887.  

Howard Mountain – Named for John Howard, a prospector.  The mountain was named in 1880.   Mount Irving Hale – Named for Brigadier General Hale who lead Colorado troops in the Philippines during the Spanish American War.  Hale was a member of the first graduating class at Denver High School and won an appointment to West Point.  Camp Hale, near Leadville, was a training site for World War II ski troops and was also named for him.