Iron Springs (Iron County, Utah)
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Iron Springs (Iron County, Utah)
Iron Springs, originally Cedar Springs, was a spring in the bed of Iron Springs Creek in what is now Iron County, Utah. The creek originally drained the western side of Cedar Valley before it was settled. Cedar Springs was located in the gap where the creek passed between the mountains of The Three Peaks and Granite Mountain. Cedar Springs was a camp for early travelers on the Mormon Road, after they had made the arduous passage from Johnson's Springs across the marshy and wooded Coal Creek. It was difficult to cross with wagons at that point in Cedar Valley. The road crossed Coal Creek midway across the valley between Johnson Springs and Cedar Springs. The travelers guide, Mormon Waybill described Cedar Spring "... wood plenty food short, Good camp". When Cedar City was established on the upper reach of Coal Creek in 1851, the road was diverted to the easy crossing there and then proceeded across the valley to Iron springs, a longer route but less arduous.
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Iron Springs Creek
Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in front of oxygen (32.1% and 30.1%, respectively), forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. In its metallic state, iron is rare in the Earth's crust, limited mainly to deposition by meteorites. Iron ores, by contrast, are among the most abundant in the Earth's crust, although extracting usable metal from them requires kilns or furnaces capable of reaching or higher, about higher than that required to smelt copper. Humans started to master that process in Eurasia during the 2nd millennium BCE and the use of iron tools and weapons began to displace copper alloys, in some regions, only around 1200 BCE. That event is considered the transition from the Bronze Age to the Iron Age. In th ...
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Iron County, Utah
Iron County is a county in southwestern Utah, United States. As of the 2010 United States Census, the population was 46,163. Its county seat is Parowan, and the largest city is Cedar City. The Cedar City, UT Micropolitan Statistical Area includes all of Iron County. History Evidence of Fremont culture habitation ranging from 750 to 1250 AD exists in present Iron County. Petroglyphs of differing periods were carved into the walls of Parowan Gap NW of Parowan. Paiutes roamed the Parowan Valley in the centuries before Euro-American exploration; their descendants are now represented by the Southern Paiute Indian Reservation, which is headquartered in Cedar City. The Domínguez–Escalante expedition traveled through the Iron County area on October 12, 1776. Fur trapper Jedediah Smith is the first recorded Anglo-American to pass through the area (1826). Settlement of the area began in 1851, when LDS President Brigham Young directed members from the northern colonies to move i ...
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Cedar Valley (Iron County, Utah)
The Cedar Valley of Iron County, Utah, United States is a long valley located in the southeast of the county, against the Hurricane Cliffs which border the Cedar Mountains and the Markagunt Plateau. Cedar Valley borders the southeast of the Escalante Desert, at its north and northwest. Cedar City, Utah lies in the valley's center and east, at the foothills of the Hurricane Cliffs. Description Cedar Valley is northeast trending. It narrows in the southwest, between mountain ranges; in this southwest section, the Harmony Mountains are west, and the Hurricane Cliffs are east, bordering the Kolob Terrace. The valley is mostly about wide, between mountains, or ranges, or the Hurricane Cliffs, to the east, which is a 75-mi long landform, from Hurricane, Utah at its southwest end. The valley's north and northwest terminus merges into the Mud Spring Wash–Rush Lake region at the southwest of the Black Mountains (Utah), (and the southeast perimeter of the Escalante Desert); ...
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Gap (landform)
A gap is a geological formation that is a low point or opening between hills or mountains or in a ridge or mountain range. It may be called a col, notch, mountain pass, pass, saddle (landform), saddle, water gap, or wind gap, and geomorphology, geomorphologically is most often carved by water erosion from a freshet, stream or a river. Gaps created by freshets are often, if not normally, devoid of water through much of the year, their streams being dependent upon the meltwaters of a snow pack. Gaps sourced by small spring (hydrology), springs will generally have a small stream excepting perhaps during the most arid parts of the year. Water gaps of necessity often cut entirely through a mountain chain, barrier barrier ridge, range and riverine gaps may create canyons such as the riverine gaps of the Danube River, Lehigh River Gorge, the Colorado River's Grand Canyon and the Genesee River. Such cuttings may expose millennia of strata in the local rock column writing the geologic reco ...
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The Three Peaks
''The'' () is a grammatical article in English, denoting persons or things that are already or about to be mentioned, under discussion, implied or otherwise presumed familiar to listeners, readers, or speakers. It is the definite article in English. ''The'' is the most frequently used word in the English language; studies and analyses of texts have found it to account for seven percent of all printed English-language words. It is derived from gendered articles in Old English which combined in Middle English and now has a single form used with nouns of any gender. The word can be used with both singular and plural nouns, and with a noun that starts with any letter. This is different from many other languages, which have different forms of the definite article for different genders or numbers. Pronunciation In most dialects, "the" is pronounced as (with the voiced dental fricative followed by a schwa) when followed by a consonant sound, and as (homophone of the archaic pron ...
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Granite Mountain (Iron County, Utah)
Granite Mountain may refer to: Mountains Canada *Granite Mountain (British Columbia), in the Rossland Range of the Monashee Mountains United States *Granite Mountain (Arizona), in Yavapai County *Granite Mountain (Arkansas), near Little Rock *Granite Mountain (California), in Anza-Borrego Desert State Park *Granite Mountain (Texas), in Burnet County *Granite Mountain (Salt Lake County, Utah), in the Wasatch Range *Granite Mountain (Washington), several peaks, including: **Granite Mountain (King County, Washington) **Granite Mountain (Wenatchee Mountains) **Granite Mountain (Whatcom County, Washington) Settlements *Granite Mountain, Alaska, a place in Alaska **Granite Mountain Air Station *Granite Mountain, a neighborhood in Little Rock, Arkansas Other uses *Granite Mountain charter school, Lucerne Valley, California, US * ''Only the Brave'' (2017 film) (working title ''Granite Mountain''), an American film See also *Granite Mountains (other) *Granite Peak Mountains nam ...
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Mormon Road
Mormon Road, also known to the 49ers as the Southern Route, of the California Trail in the Western United States, was a seasonal wagon road pioneered by a Mormon party from Salt Lake City, Utah led by Jefferson Hunt, that followed the route of Spanish explorers and the Old Spanish Trail across southwestern Utah, northwestern Arizona, southern Nevada and the Mojave Desert of California to Los Angeles in 1847. From 1855, it became a military and commercial wagon route between California and Utah, called the Los Angeles – Salt Lake Road. In later decades this route was variously called the "Old Mormon Road", the "Old Southern Road", or the "Immigrant Road" in California. In Utah, Arizona and Nevada it was known as the "California Road". Mormon Road 1847–1855 Jefferson Hunt and Mormon Veterans Expeditions 1847–1848 The wagon road later called the "Mormon Road" was pioneered by a Mormon party with pack horses, led by Jefferson Hunt, intent on obtaining supplies for the stru ...
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Enoch, Utah
Enoch is a mostly rural and agricultural city in Iron County, Utah, United States, and is located approximately northeast of Cedar City in the northeast part of Cedar Valley. The population was 5,803 at the 2010 census, up from 3,467 at the 2000 census. As of 2018 the estimated population was 7,039. Enoch was originally settled as part of an iron mission along with Cedar City and Parowan. The area was originally known as "Fort Johnson" and "Johnson Springs", after Joel H. Johnson, the earliest known white settler, who came to the area in 1851 with his family. In 1890, the area's name was changed to "Enoch", to avoid confusion with another settlement in Utah also named Johnson Springs. Enoch was officially incorporated on January 10, 1966, absorbing nearby Grimshawville, Stevensville, and Williamsville. The present name is after the Order of Enoch. History Enoch was founded by Joel H. Johnson. It was originally known as Johnson's Springs and Fort Johnson. Enoch was incorpo ...
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Coal Creek (Iron County, Utah)
Coal Creek is a stream in eastern Iron County, Utah, United States. Description The creek's mouth was at an elevation of in Cedar Valley in 1979, but that location is now a farm field, and its new terminus is located a little further upstream, northwest of Cedar City Cedar City is the largest city in Iron County, Utah, United States. It is located south of Salt Lake City, and north of Las Vegas on Interstate 15. It is the home of Southern Utah University, the Utah Shakespeare Festival, the Utah Summer Gam .... Its source is at the confluence of Crow Creek and Ashdown Creek, in Cedar Canyon, at the foot of Cedar Mountain at at an elevation of . Coal Creek passes through Cedar City on its way to Cedar Valley. See also * List of rivers in Utah References External links Rivers of Utah Rivers of Iron County, Utah {{Utah-river-stub ...
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Cedar City
Cedar City is the largest city in Iron County, Utah, United States. It is located south of Salt Lake City, and north of Las Vegas on Interstate 15. It is the home of Southern Utah University, the Utah Shakespeare Festival, the Utah Summer Games, the Simon Fest Theatre Co., and other events. As of the 2010 census the city had a population of 28,857, up from 20,257 in 2000. As of 2019, the estimated population was 34,764. History The presence of prehistoric people in the Cedar City area is revealed by rock art found in Parowan Gap to the north and Fremont sites dated to A.D. 1000 and 1300. Ancestors of the present-day Southern Paiute people met the Domínguez–Escalante expedition in this area in 1776. Fifty years later, in 1826, mountain man and fur trader Jedediah Smith traveled through the area, exploring a route from Utah to California. Cedar City was originally settled in late 1851 by Mormon pioneers originating from Parowan, Utah, who were sent to build an iron ...
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Roadometer (odometer)
The roadometer was a 19th-century device like an odometer for measuring mileage, mounted on a wagon wheel. One such device was invented in 1847 by William Clayton, Orson Pratt, and Appleton Harmon, pioneers of The Church of Jesus Christ of Latter-Day Saints. History Brass odometers were used by many pioneers making the westward trek in the 1840s. However, the design of Clayton, Pratt, and Harmon's odometer was new. In 1847, William Clayton accompanied the first expedition to the Utah Territory as a writer and record-keeper. He initially counted revolutions of a wagon wheel to calculate the distance they had travelled. He tired of counting wheel revolutions and wanted a device that could measure the distanced a wagon travelled. It is possible he was familiar with the English viometers that measured distance using gears. Clayton asked Orson Pratt if it would be possible to make such a device, and Pratt created the design. Harmon carved the gears out of wood and may have further re ...
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Iron Springs, Utah
Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in front of oxygen (32.1% and 30.1%, respectively), forming much of Earth's outer core, outer and inner core. It is the fourth most common abundance of elements in Earth's crust, element in the Earth's crust. In its metallic state, iron is rare in the Earth's crust, limited mainly to deposition by meteorites. Iron ores, by contrast, are among the most abundant in the Earth's crust, although extracting usable metal from them requires kilns or Metallurgical furnace, furnaces capable of reaching or higher, about higher than that required to smelting, smelt copper. Humans started to master that process in Eurasia during the 2nd millennium BC, 2nd millennium BCE and the use of iron tools and weapons began to displace list of copper alloys, copper ...
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