After taking lumber out of Pleasant Creek Canyon in late 1851, a band of Mormon colonists from Manti led by Madison D. Hambleton returned in the spring of 1852 to establish the Hambleton Settlement near the present site of Mt. Pleasant. During the Walkara (Walker) Indian War, the small group of settlers relocated to Spring Town (Spring City) and later to Manti for protection. The old settlement was burned down by local Native Americans, so when a large colonizing party from Ephraim and Manti returned to the area in 1859, a new, permanent townsite was laid out in its present location—one hundred miles south of Salt Lake City and twenty-two miles northeast of Manti.
Among the founding settlers were Mormon converts from Scandinavia, the United Kingdom, and the eastern United States. By 1880, at which time Mt. Pleasant was the county’s largest city, with a population of 2,000, more than 72 percent of its married adults were foreign born. This ethnic diversity had an important impact on village life during the nineteenth and early twentieth centuries. For decades, five languages were commonly spoken in town, creating confusing and sometimes amusing communication problems.
Indianola is in Sanpete County, Utah. It is located just off Highway 89 between Birdseye and Fairview, near Hideaway Valley. It is the former site of an Indian village.
We stopped by the Fairview Museum of History and Art to look around, it was two buildings, it was a holiday (July 4th) and I was surprised they were even open, they offered to open up the North building for us but we decided to save it for another time and just check out the South building.
I had wanted to come see the Mammoth for years since I had many times stopped at the site where it was found up the canyon (see this post.)
I was driving through Fairview and saw this gorgeous old mill and snapped a photo.
I later stopped in at the Museum in town and saw several paintings of the same Mill, I thought I’d post those here.
The historic Fairview Roller Mill has always been my favorite thing to see in Fairview. It was not in great shape but in 2016 the Utley family puchased it and fixed it up while converting it into a home.
Members of the Church of Jesus Christ of Latter-day Saints (LDS or Mormon Church) first explored and settled the Sanpete Valley in central Utah in 1849, but because of skirmishes between settlers and indigenous Ute tribal members, more than a decade passed before the various communities became established. Fairview (originally known as North Bend), at the north end of the valley, was one of the last to be settled. It was surveyed in 1859 and a fort constructed the next spring in response to regional Anglo/Indian conflicts. Life in the settlement was not “all work and no play.” A large log schoolhouse built in the center of the fort was dedicated December 9, 1860. It served as a school, church, and community center. Dances were held in this building from the beginning and soon a stage was built in one end for community drama productions. (*)
A few of my posts related to Fairview are listed here:
In 1864 a post office was established and by 1880, with one thousand residents, Fairview was the fourth largest settlement in the valley. The full-time population would exceed 1,700 in 1910 and again in 1940, but currently sits at under 1,000; there are several reasons for this. The primary occupations in Fairview are in the livestock and agricultural industries, with sheep and cattle being the main stock. Other industries were established in the twentieth century, mainly in coal mining and dairy operations, but because major traffic routes bypass the Sanpete Valley, little growth in either industry or population has occurred in the past several decades. The isolation and lack of growth in industry and population has allowed for the retention of a majority of historic buildings and structures, not only in Fairview, but also in the entire Sanpete Valley.
Welcome to Joe’s Valley, a 75-mile long, north-south trending depression graben, what’s a graben you ask?
Horsts and Grabens
A graben is a depressed block of land bordered by parallel faults. Graben is German for ditch.
A graben is the result of a block of land being downthrown producing a valley with a distinct scarp on each side. Grabens often occur side-by-side with horsts. Horst and graben structures are indicative of tensional forces and crustal stretching.
Graben are produced from parallel normal faults, where the hanging wall is downthrown and the footwall is upthrown. The faults typically dip toward the center of the graben from both sides. Horsts are parallel blocks that remain between grabens, the bounding faults of a horst typically dip away from the center line of the horst.
A single graben or multiple grabens can produce a rift valley.
(Horsts are up thrown blocks bounded on either side by parallel normal faults.)
(Grabens are downthrown blocks bounded on either side by parallel normal faults.)
Half-Graben
Half-grabens develop when parallel faults on either side of a block develop, but the block becomes tilted instead of dropping down as in a graben.
A beast who roamed Huntington Canyon 11,000 years ago is still a cause for excitement and interest these many years later. The mammoth was discovered at the Huntington Reservoir in Huntington Canyon on 8-8-88 by Nielson Construction backhoe operator, Chris Nielson.
At first they thought they had dug up an old tree or something, but closer examination revealed the ancient creature. Authorities were notified and an official removal process began.
Visitors again gathered at the site of the mammoth discovery on Friday to dedicate the new kiosk and information center recently constructed at the site. The event brought back many memories of the discovery. The Huntington/Eccles Scenic Byway is a diverse route with magnificent scenery which happens to go past the mammoth discovery site. Jana Abrams is the Energy Loop Byways Coordinator and instrumental in garnering the funds for this mammoth project. She said, “This kiosk is a new visitor attraction. We want visitors to stay a little longer in our communities. We have such a diverse community here along the Energy Loop and Huntington and Eccles Canyons. This byway ties everything together, mining, farming, travel and recreation. This kiosk was made possible with a grant from the Federal Highway division. Bill Broadbear from the US Forest Service worked on the trail down to the kiosk and the slope is ADA accessible. We have had a great partnership with the forest service.”
Abrams pointed out the long process of information gathering and photo gathering of the actual mammoth find to go on the information panels. She appreciates artist Joe Venus for the painted mural which depicts how the area may have looked when the mammoth roamed the country; this painted mural is on one of the panels.
Abrams thanked Dawnette Tuttle from Orangeville for the use of her pictures and the newspaper clippings from the time of the discovery. A second part of the kiosk project has been the installation of low wattage radio antennas which will broadcast information about the area. Information will include: camping info, weather conditions, special activities, etc. This station will be AM 1610.
Abrams introduced the speakers for the program-ribbon cutting ceremony which included: Martha Hayden, Utah Geologic Survey; Don Burge, retired curator for the College of Eastern Utah Prehistoric Museum; Bill Broadbear, Manti-LaSal National Forest Service; Carlos Machado, Federal Highways Administration Utah Division; and Gael Hill, State Scenic Byway coordinator.
Hayden was called to the site of the discovery on Aug. 8, 1988. She worked with Dave Madsen and Dave Gillette in the mammoth removal process. The bones were wrapped in burlap to prevent them from drying out. The bone unearthed by Nielson was a tusk or humerus bone. It was lying on the ground. She said there was great cooperation with Nielson Construction, the forest service and the volunteers at the site. At least 5,000 people visited the site during the time of excavation. She described the find as one of the greatest ice age fossil finds ever as the mammoth was 95 percent complete in its location. A short faced bear was also located at the site. The site had been a bog which was created by a glacier slide and became the mammoth’s resting spot. He was deposited at the end of the ice age and was a very old male, 60-65 years old, at the end of his life. Fur needles were preserved inside his stomach. Which is a poor diet for a mammoth of this size and the mammoth was found to have arthritis.
Burge spoke next saying next August will mark the 20 year anniversary of the mammoth discovery. He said, “The discovery has changed the course of the CEU museum. There have been more than 30 casts made of this mammoth. The South Dakota Mammoth site even has one of our mammoths. There are two in Japan, one in a Los Angeles museum and one in Canada.”
Burge said some of the bones were kept in kiddie pools around the museum to keep them from drying out. There were arguments at first of who owned the mammoth. Who did he belong to? The CEU museum became accredited so it could serve as a repository for the mammoth bones. Burge said the so called experts originally identified the beast as a mastodon and he was glad to point out to them the real identity of the creature. A mammoth has teeth similar to elephant teeth and mastodon teeth are more like human molars. A mammoth cast is at the CEU museum and the original mammoth skeleton is there and available for public viewing. It is stored in a conservation lab where the relative humidity is kept at 30 percent and the room temperature 68 degrees. Burge said that’s hard to do here where the air is so dry. “We did more things right than wrong and the bones are still in good condition,” said Burge.
Broadbear said one day during the discovery period a reporter from the New York Times showed up and wanted to do a story about the mammoth. Interest in the mammoth discovery went worldwide. Broadbear said he is impressed with the kiosk and the informative panels to tell the story of the discovery so visitors to the site come away with an appreciation of the site and the mammoth.
Machado said he works with the scenic byways to help them with grants to do projects. He enjoys these partnerships and the work they do to be good stewards of the natural resources. He believes the scenic byways are the heart and soul of America. He described scenic byways as an extensive collection of special places. He is working to bring additional funds to Utah for projects. “I have never been here before and am surprised with the scenic views.” The Utah Division since 1992, has had $7.3 million procured for 84 projects.
Hill rounded out the program with her description of the scenic byways program. “The byways connect our country. Utah has better byways than many states.” She is proud of the mammoth project and the Scenic highway 89 project from Manti to Kanab.
Abrams encouraged tourists to visit the mammoth kiosks and enjoy the discovery of the mammoth.
Wayne Nielson from Nielson Construction said they were working on a new dam at the time of the discovery. The old dam had begun to leak and was being replaced. His cousin Chris Nielson was excavating when he brought up a bone, it was 50-60 feet down, kind of in a bowl area. The bog area acted as a refrigerator for the skeleton and the cool mud kept it preserved for approximately 11,000 years.
The mammoth and its story will continue to be an asset to the Castle Valley region as its notoriety extends worldwide.
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This is at the site of a discovery very important to helping us understand the Ice Age period. This post focuses on how the earth can preserve bones, plant life, and even whole forests for thousands of years only to be discovered later and teach us of the past. Long ago this land was much different, what was it like?
The Ice Age is also known as the Pleistocene Epoch, which lasted from about 2 million to 10,000 years ago, and was a period of recurring widespread glaciations. Ice ages have actually occurred periodically throughout the history of the Earth. The Pleistocene is the most recent of these ice ages.
Glaciers covered most of the high mountains of Utah periodically during the Ice Age.
Lake Bonneville, a large fresh-water lake, covered most of western Utah from 30,000 to 12,000 years ago. The Great Salt Lake is the remnant of this Ice Age lake.
The animals that lived in Utah during the Ice Age included many of the same animals that we find here today, as well as many extinct forms such as mammoths, mastodons, ground sloths, and saber-toothed cats.
Many of the extinct Pleistocene animals were very large and have living relatives who are usually much smaller. These large, extinct animals are referred to as the “Pleistocene Megafauna”. They became extinct at the end of the Ice Age, about 10,000 years ago.
Mammoths and Mastodons are two types of elephants that lived in Utah during the Ice Age. They differ in the shape and function of their teeth and in the shape of other bones, including the skull. They are related to modern elephants that live in Africa and Asia.
Gravel quarries along the Wasatch Front contain the bones of many Ice Age animals. These gravels were deltaic deposits formed in Lake Bonneville. The animals that roamed the shores of Lake Bonneville included big-horn sheep (Ovis), horses (Equus), and bison (Bison), whose living relatives are found in Utah today, as well as animals such as musk oxen (Bootherium bombifrons), camels (Camelops hesternus), and giant ground sloths (Megalonyx jeffersoni), who have living relatives in other parts of the world.
Early in the Tertiary Period, not long after dinosaurs became extinct, mammals began a long and colorful evolution in North and South America. By late Tertiary time, two million years ago, our continent was occupied by camels, mastodons, horses, ground sloths, armadillos, saber tooth cats, giant wolves, giant beavers, giant bears, and many other exotic animals. The landscape from a distance looked more like today’s Africa than modern North America.
By the late Tertiary, glacial conditions in high latitudes intensified. Enormous quantities of water were bound up by the glaciers, and sea levels fluctuated with each shortlived glacial episode.
About 1,600,000 years ago, the first mammoths emigrated to North America from Asia during one of the low stands of sea level. That event marks the arbitrarily defined beginning of the Pleistocene Epoch of the Quaternary Period. The Ice Age was in full swing.
Glaciation
Mammoths evolved for more than 1.5 million years in North America, adjusting to the fluctuating conditions of the Ice Age. With each cycle of glaciation and deglaciation, habitats were disrupted first, then stabilized, and then disrupted again with renewed glaciation.
Each time the glaciers formed, they coalesced into enormous sheets of ice over central and eastern Canada, eventually pushing southward. These ice sheets, or continental glaciers, were as thick as two miles. They often moved so rapidly that they crushed standing forests.
Climatic Fluctuation
Climatic effects during the Ice Age became drastic by the end of the Pleistocene. Populations of animals and plants that lived in Canada were pushed southward thousands of miles. Intermountain valleys in the West became home to forests, rather than the deserts we have today. Between glacial episodes, forests retreated to higher elevations and desert vegetation returned, only to be replaced with the next glacial episode.
Especially during the latter part of the Ice Age, animals and plants that lived in northern Utah left a wonderful legacy of their history. With each fluctuation of the climate, some old species returned, and some new ones appeared. Some of those animals have been preserved as fossils in sediments deposited during their existence.
The Discovery of an Ice Age Mammoth
New discoveries of fossil vertebrates in northern Utah include several of the extinct megafauna. A nearly complete skeleton of the Colombian mammoth, preserved perfectly, was discovered here in 1988.
This sacred plot, laid out by Joseph Gaston Garlick, was first used in 1860. Three small children, Maria Terry, Henry Weeks Sanderson, jr., and Lucy Jones were the first buried here. Later, John givens, his wife, Eliza, and their son and three small daughters were buried in the cemetery. The graves of Lauritz Jens Larsen, David Jones, killed by Indians during the Black Hawk War, are also located here.
The cemetery was originally liad out in a rectangular shape. In the late 1800s, a flood from the west draw washed out several graves in the northeast section of the cemetery, causing burial to cease in that section.
Many of the headstones, the oldest of native limestone, mark the graves of mothers and their children who died of disease, childbirth complications, and accidents. Entire families were liad to rest here, having worn out their lives making the desert “blossom as a rose.” In turn, an honorable legacy was left.
Fairview, settled in 1859, was first named North Bend. Because of the incomparable scenery of the mountains to the east, blanketed with pines, aspens, and wild flowers in Perfusion, the name was changed in 1864.
The Stone used to build this monument was the original stone from the Fairview Fort, built in the 1860s. During the Black Hawk War of the mid-1860s, some Fairview residents moved to nearby Mt. Pleasant for protection. Those who remained complied with leader Brigham Young’s instructions to build a fort. By the end of 1866, a thick, ten-foot-high rock wall enclosed the center of town.
In the spring of 1865 John Given with his wife Eliza and their four children, John Jr., Mary, Anna, and Martha settled in the meadow land about 110 feet west of here. They built a cabin and willow shanty. Charles Brown and Charles W. Leah were helping them plow and plant crops. Early in the morning of May 26th they were attacked by a band of Indians. Brown and Leah escaped and ran six miles for help, which came too late. The entire Given family was massacred and their cattle and household furnishings taken. The murdered people were buried in Fairview.
Check out all of the historic markers placed by the Daughters of Utah Pioneers at JacobBarlow. com/dup
In 1859, a small group from Mt. Pleasant laid out a townsite here called North Bend. Later the name was changed to Fairview. During the winter rock was quarried and hauled to build a fort, and in 1860 walls of three sides were finished; the other side was made by the backs of log houses abutting at the end. Portholes in top walls were for watcher. Inside the fort were rows of houses, a tithing office, and a schoolhouse which also served as church. James N. Jones was presiding Elder. In 1868 Fairview was made an L.D.S. Ward with Amasa Tucker as Bishop.
