The landlocked U.S. state of Utah is known for its natural diversity and is home to features ranging from arid deserts with sand dunes to thriving pine forests in mountain valleys. It is a rugged and geographically diverse state at the convergence of three distinct geological regions: the Rocky Mountains, the Great Basin, and the Colorado Plateau.
Utah covers an area of 84,899 sq mi (219,890 km2). It is one of the Four Corners states and is bordered by Idaho in the north, Wyoming in the north and east, by Colorado in the east, at a single point by New Mexico to the southeast, by Arizona in the south, and by Nevada in the west. Only three U.S. states (Utah, Colorado, and Wyoming) have exclusively latitude and longitude lines as boundaries. [1]
The northern border with Idaho is inherited from the Adams–Onís Treaty of 1819, which defined the boundary between the Louisiana Purchase and New Spain. The large size of the proposed State of Deseret was controversial. The Compromise of 1850 gave the Utah Territory five degrees of latitude, cutting the land east of the new state of California roughly in half. [1] The creation of the Colorado Territory in 1861 moved Utah's eastern border from the Rocky Mountains to the 109th western meridian, to give Colorado Territory seven degrees of longitude (like Oregon previously had and four more western states would later get). [2]
To secure the booming Comstock Lode area in western Utah Territory for the Union during the American Civil War against the uncertain loyalties of the Mormons of Utah, Congress created the Nevada Territory in 1861. The Nevada Territory's boundary with the Utah Territory was moved from the 116th to the 115th meridian as more mineral deposits were discovered. Congress moved it to the 114th meridian when Nevada was granted statehood, in order to include access to Colorado River tributaries. [1]
The northwestern notch in the Utah Territory was created with the formation of the Nebraska Territory in 1854. When the Wyoming Territory was created in 1868, the notch was expanded to give Wyoming seven degrees of longitude. The notch area is separated from Salt Lake City by the Uinta Mountains and the Wasatch Range, making it easier for Wyoming authorities to administer. Anti-Mormon sentiment may have also led to this area being assigned to Wyoming. It contained coal fields, various waterways, and parts of the Oregon Trail, California Trail, Overland Trail, transcontinental telegraph, stagecoach route, and future transcontinental railroad. [1]
One of Utah's defining characteristics is the variety of its terrain. Running down the middle of the state's northern third is the Wasatch Range, which rises to heights of almost 12,000 ft (3,700 m) above sea level. Utah is home to world-renowned ski resorts made popular by light, fluffy snow and winter storms that regularly dump up to three feet of it overnight. In the state's northeastern section, running east to west, are the Uinta Mountains, which rise to heights of over 13,000 feet (4,000 m). The highest point in the state, Kings Peak, at 13,528 feet (4,123 m), [3] lies within the Uinta Mountains.
At the western base of the Wasatch Range is the Wasatch Front, a series of valleys and basins that are home to the most populous parts of the state. It stretches approximately from Brigham City at the north end to Nephi at the south end. Approximately 75 percent of the state's population lives in this corridor, and population growth is rapid.
Western Utah is mostly arid desert with a basin and range topography. Small mountain ranges and rugged terrain punctuate the landscape. The Bonneville Salt Flats are an exception, being comparatively flat as a result of once forming the bed of ancient Lake Bonneville. Great Salt Lake, Utah Lake, Sevier Lake, and Rush Lake are all remnants of this ancient freshwater lake, [4] which once covered most of the eastern Great Basin. West of the Great Salt Lake, stretching to the Nevada border, lies the arid Great Salt Lake Desert. One exception to this aridity is Snake Valley, which is (relatively) lush due to large springs and wetlands fed from groundwater derived from snow melt in the Snake Range, Deep Creek Range, and other tall mountains to the west of Snake Valley. Great Basin National Park is just over the Nevada state line in the southern Snake Range. One of western Utah's most impressive, but least visited attractions is Notch Peak, the tallest limestone cliff in North America, located west of Delta.
Much of the scenic southern and southeastern landscape (specifically the Colorado Plateau region) is sandstone, specifically Kayenta sandstone and Navajo sandstone. The Colorado River and its tributaries wind their way through the sandstone, creating some of the world's most striking and wild terrain (the area around the confluence of the Colorado and Green Rivers was the last to be mapped in the lower 48 United States). Wind and rain have also sculpted the soft sandstone over millions of years. Canyons, gullies, arches, pinnacles, buttes, bluffs, and mesas are the common sights throughout south-central and southeast Utah.
This terrain is the central feature of protected state and federal parks such as Arches, Bryce Canyon, Canyonlands, Capitol Reef, and Zion national parks, Cedar Breaks, Grand Staircase–Escalante, Hovenweep, and Natural Bridges national monuments, Glen Canyon National Recreation Area (site of the popular tourist destination, Lake Powell), Dead Horse Point and Goblin Valley state parks, and Monument Valley. The Navajo Nation also extends into southeastern Utah. Southeastern Utah is also punctuated by the remote, but lofty La Sal, Abajo, and Henry mountain ranges.
Eastern (northern quarter) Utah is a high-elevation area covered mostly by plateaus and basins, particularly the Tavaputs Plateau and San Rafael Swell, which remain mostly inaccessible, and the Uinta Basin, where the majority of eastern Utah's population lives. Economies are dominated by mining, oil shale, oil, and natural gas-drilling, ranching, and recreation. Much of eastern Utah is part of the Uintah and Ouray Indian Reservation. The most popular destination within northeastern Utah is Dinosaur National Monument near Vernal.
Southwestern Utah is the lowest and hottest spot in Utah. It is known as Utah's Dixie because early settlers were able to grow some cotton there. Beaverdam Wash in far southwestern Utah is the lowest point in the state, at 2,000 feet (610 m). [3] The northernmost portion of the Mojave Desert is also located in this area. Dixie is quickly becoming a popular recreational and retirement destination, and the population is growing rapidly. Although the Wasatch Mountains end at Mount Nebo near Nephi, a complex series of mountain ranges extends south from the southern end of the range down the spine of Utah. Just north of Dixie and east of Cedar City is the state's highest ski resort, Brian Head.
Like most of the western and southwestern states, the federal government owns much of the land in Utah. Over 70 percent of the land is either BLM land, Utah State Trustland, or U.S. National Forest, U.S. National Park, U.S. National Monument, National Recreation Area or U.S. Wilderness Area. [5] Utah is the only state where every county contains some national forest. [6]
Utah features a dry, semi-arid to desert climate, [7] although its many mountains feature a large variety of climates, with the highest points in the Uinta Mountains being above the timberline. The dry weather is a result of the state's location in the rain shadow of the Sierra Nevada in California. The eastern half of the state lies in the rain shadow of the Wasatch Mountains. The primary source of precipitation for the state is the Pacific Ocean, with the state usually lying in the path of large Pacific storms from October to May. In summer, the state, especially southern and eastern Utah, lies in the path of monsoon moisture from the Gulf of California.
Most of the lowland areas receive less than 12 inches (305 mm) of precipitation annually, although the I-15 corridor, including the densely populated Wasatch Front, receives approximately 15 inches (381 mm). The Great Salt Lake Desert is the driest area of the state, with less than 5 inches (127 mm). Snowfall is common in all but the far southern valleys. Although St. George receives only about 3 inches (76 mm) per year, Salt Lake City sees about 60 inches (1,524 mm), enhanced by the lake-effect snow from the Great Salt Lake, which increases snowfall totals to the south, southeast, and east of the lake.
Some areas of the Wasatch Range in the path of the lake-effect receive up to 500 inches (12,700 mm) per year. This micro climate of enhanced snowfall from the Great Salt Lake spans the entire proximity of the lake. The cottonwood canyons adjacent to Salt Lake City are located in the right position to receive more precipitation from the lake. [8] The consistently deep powder snow led Utah's ski industry to adopt the slogan "the Greatest Snow on Earth" in the 1980s. In the winter, temperature inversions are a common phenomenon across Utah's low basins and valleys, leading to thick haze and fog that can last for weeks at a time, especially in the Uintah Basin. Although at other times of year its air quality is good, winter inversions give Salt Lake City some of the worst wintertime pollution in the country.
Previous studies have indicated a widespread decline in snowpack over Utah accompanied by a decline in the snow–precipitation ratio while anecdotal evidence claims have been put forward that measured changes in Utah's snowpack are spurious and do not reflect actual change. A 2012 study [9] found that the proportion of winter (January–March) precipitation falling as snow has decreased by nine percent during the last half century, a combined result from a significant increase in rainfall and a minor decrease in snowfall. Meanwhile, observed snow depth across Utah has decreased and is accompanied by consistent decreases in snow cover and surface albedo. Weather systems with the potential to produce precipitation in Utah have decreased in number with those producing snowfall decreasing at a considerably greater rate. [10]
Utah's temperatures are extreme, with cold temperatures in winter due to its elevation, and very hot summers statewide (with the exception of mountain areas and high mountain valleys). Utah is usually protected from major blasts of cold air by mountains lying north and east of the state, although major Arctic blasts can occasionally reach the state. Average January high temperatures range from around 30 °F (−1 °C) in some northern valleys to almost 55 °F (13 °C) in St. George.
Temperatures dropping below 0 °F (−18 °C) should be expected on occasion in most areas of the state most years, although some areas see it often (for example, the town of Randolph averages about fifty days per year with temperatures that low). In July, average highs range from about 85 to 100 °F (29 to 38 °C). However, the low humidity and high elevation typically leads to large temperature variations, leading to cool nights most summer days. The record high temperature in Utah was 118 °F (48 °C), recorded south of St. George on July 4, 2007, [11] and the record low was −69 °F (−56 °C), recorded at Peter Sinks in the Bear River Mountains of northern Utah on February 1, 1985. [12] However, the record low for an inhabited location is −49 °F (−45 °C) at Woodruff on December 12, 1932. [13]
Utah, like most of the western United States, has few days of thunderstorms. On average there are fewer than 40 days of thunderstorm activity during the year, although these storms can be briefly intense when they do occur. They are most likely to occur during monsoon season from about mid-July through mid-September, especially in southern and eastern Utah. Dry lightning strikes and the general dry weather often spark wildfires in summer, while intense thunderstorms can lead to flash flooding, especially in the rugged terrain of southern Utah. Although spring is the wettest season in northern Utah, late summer is the wettest period for much of the south and east of the state. Tornadoes are uncommon in Utah, with an average of two striking the state yearly, rarely higher than EF1 intensity. [14]
One exception of note, however, was the unprecedented Salt Lake City Tornado that moved directly across downtown Salt Lake City on August 11, 1999. The F2 tornado killed one person, injured sixty others, and caused approximately $170 million in damage; [15] it was the second strongest tornado in the state behind an F3 on August 11, 1993, in the Uinta Mountains. [15] [16] The only other reported tornado fatality in Utah's history was a 7-year-old girl who was killed while camping in Summit County on July 6, 1884. [15] The last tornado of above (E)F0 intensity occurred on September 8, 2002, when an F2 tornado hit Manti. [15]
| Climate data for Salt Lake City International Airport (1991–2020 normals, [a] extremes 1874–present) [b] | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Record high °F (°C) | 63 (17) | 69 (21) | 80 (27) | 89 (32) | 99 (37) | 107 (42) | 107 (42) | 106 (41) | 107 (42) | 92 (33) | 75 (24) | 69 (21) | 107 (42) |
| Mean maximum °F (°C) | 51.8 (11.0) | 58.8 (14.9) | 70.4 (21.3) | 80.2 (26.8) | 88.9 (31.6) | 97.9 (36.6) | 101.9 (38.8) | 99.6 (37.6) | 93.9 (34.4) | 82.0 (27.8) | 67.1 (19.5) | 54.3 (12.4) | 102.3 (39.1) |
| Mean daily maximum °F (°C) | 38.6 (3.7) | 44.7 (7.1) | 55.3 (12.9) | 61.9 (16.6) | 72.6 (22.6) | 84.1 (28.9) | 94.0 (34.4) | 91.7 (33.2) | 80.6 (27.0) | 65.5 (18.6) | 50.7 (10.4) | 39.0 (3.9) | 64.9 (18.3) |
| Daily mean °F (°C) | 31.4 (−0.3) | 36.6 (2.6) | 45.8 (7.7) | 51.8 (11.0) | 61.5 (16.4) | 71.6 (22.0) | 81.1 (27.3) | 79.1 (26.2) | 68.4 (20.2) | 54.6 (12.6) | 41.7 (5.4) | 32.2 (0.1) | 54.7 (12.6) |
| Mean daily minimum °F (°C) | 24.2 (−4.3) | 28.6 (−1.9) | 36.3 (2.4) | 41.8 (5.4) | 50.4 (10.2) | 59.1 (15.1) | 68.2 (20.1) | 66.6 (19.2) | 56.3 (13.5) | 43.6 (6.4) | 32.8 (0.4) | 25.3 (−3.7) | 44.4 (6.9) |
| Mean minimum °F (°C) | 6.5 (−14.2) | 9.2 (−12.7) | 21.0 (−6.1) | 28.7 (−1.8) | 34.8 (1.6) | 43.5 (6.4) | 54.9 (12.7) | 52.4 (11.3) | 39.7 (4.3) | 29.5 (−1.4) | 16.9 (−8.4) | 7.3 (−13.7) | 0.9 (−17.3) |
| Record low °F (°C) | −22 (−30) | −30 (−34) | 0 (−18) | 14 (−10) | 25 (−4) | 32 (0) | 40 (4) | 37 (3) | 27 (−3) | 14 (−10) | −14 (−26) | −21 (−29) | −30 (−34) |
| Average precipitation inches (mm) | 1.43 (36) | 1.30 (33) | 1.75 (44) | 2.16 (55) | 1.82 (46) | 0.95 (24) | 0.49 (12) | 0.58 (15) | 1.06 (27) | 1.26 (32) | 1.32 (34) | 1.40 (36) | 15.52 (394) |
| Average snowfall inches (cm) | 12.7 (32) | 10.7 (27) | 5.9 (15) | 2.9 (7.4) | 0.1 (0.25) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 0.5 (1.3) | 7.0 (18) | 12.1 (31) | 51.9 (132) |
| Average precipitation days (≥ 0.01 in) | 10.3 | 9.5 | 9.2 | 10.4 | 8.9 | 4.8 | 3.9 | 4.9 | 5.2 | 6.5 | 8.3 | 9.6 | 91.5 |
| Average snowy days (≥ 0.1 in) | 7.6 | 6.0 | 4.0 | 2.2 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.7 | 3.6 | 7.1 | 31.4 |
| Average relative humidity (%) | 74.0 | 69.8 | 60.2 | 53.2 | 48.7 | 41.4 | 35.9 | 38.5 | 45.6 | 55.7 | 66.3 | 74.3 | 55.3 |
| Average dew point °F (°C) | 19.9 (−6.7) | 24.1 (−4.4) | 27.1 (−2.7) | 31.1 (−0.5) | 36.9 (2.7) | 41.4 (5.2) | 45.7 (7.6) | 45.1 (7.3) | 39.9 (4.4) | 34.5 (1.4) | 28.4 (−2.0) | 21.7 (−5.7) | 33.0 (0.5) |
| Mean monthly sunshine hours | 127.4 | 163.1 | 241.9 | 269.1 | 321.7 | 360.5 | 380.5 | 352.5 | 301.1 | 248.1 | 150.4 | 113.1 | 3,029.4 |
| Percent possible sunshine | 43 | 55 | 65 | 67 | 72 | 80 | 83 | 83 | 81 | 72 | 50 | 39 | 68 |
| Average ultraviolet index | 1.7 | 2.7 | 4.6 | 6.6 | 8.4 | 9.8 | 10.4 | 9.0 | 6.6 | 4.0 | 2.2 | 1.4 | 5.6 |
| Source 1: NOAA (relative humidity and sun 1961–1990) [17] [18] [19] [20] [21] | |||||||||||||
| Source 2: UV Index Today (1995 to 2022) [22] | |||||||||||||
| Climate data for St. George (1991–2020 normals) | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Record high °F (°C) | 72 (22) | 84 (29) | 91 (33) | 100 (38) | 108 (42) | 115 (46) | 118 (48) | 113 (45) | 112 (44) | 107 (42) | 88 (31) | 75 (24) | 118 (48) |
| Mean maximum °F (°C) | 65 (18) | 70 (21) | 81 (27) | 90 (32) | 98 (37) | 106 (41) | 110 (43) | 107 (42) | 103 (39) | 92 (33) | 76 (24) | 64 (18) | 110 (43) |
| Mean daily maximum °F (°C) | 55.2 (12.9) | 60.1 (15.6) | 69.7 (20.9) | 76.4 (24.7) | 86.3 (30.2) | 97.4 (36.3) | 102.5 (39.2) | 101.0 (38.3) | 93.1 (33.9) | 79.8 (26.6) | 64.7 (18.2) | 53.9 (12.2) | 77.0 (25.0) |
| Daily mean °F (°C) | 42.8 (6.0) | 47.4 (8.6) | 55.5 (13.1) | 61.9 (16.6) | 71.6 (22.0) | 81.8 (27.7) | 87.8 (31.0) | 86.5 (30.3) | 78.0 (25.6) | 64.5 (18.1) | 50.8 (10.4) | 42.1 (5.6) | 63.1 (17.3) |
| Mean daily minimum °F (°C) | 30.7 (−0.7) | 34.7 (1.5) | 41.3 (5.2) | 47.4 (8.6) | 56.7 (13.7) | 66.1 (18.9) | 73.2 (22.9) | 72.0 (22.2) | 62.6 (17.0) | 49.2 (9.6) | 36.9 (2.7) | 30.3 (−0.9) | 49.2 (9.6) |
| Mean minimum °F (°C) | 21 (−6) | 25 (−4) | 31 (−1) | 38 (3) | 45 (7) | 55 (13) | 66 (19) | 64 (18) | 52 (11) | 38 (3) | 27 (−3) | 21 (−6) | 19 (−7) |
| Record low °F (°C) | −11 (−24) | 1 (−17) | 12 (−11) | 18 (−8) | 20 (−7) | 35 (2) | 41 (5) | 43 (6) | 25 (−4) | 20 (−7) | 4 (−16) | −4 (−20) | −11 (−24) |
| Average precipitation inches (mm) | 1.11 (28) | 1.39 (35) | 0.90 (23) | 0.61 (15) | 0.37 (9.4) | 0.18 (4.6) | 0.54 (14) | 0.75 (19) | 0.54 (14) | 0.65 (17) | 0.66 (17) | 0.77 (20) | 10.08 (256) |
| Average snowfall inches (cm) | 0.4 (1.0) | 0.5 (1.3) | 0.2 (0.51) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | trace | 0.1 (0.25) | 1.4 (3.6) |
| Average precipitation days (≥ 0.01 in) | 6 | 6 | 5 | 4 | 3 | 1 | 3 | 3 | 2 | 3 | 3 | 5 | 44 |
| Average snowy days (≥ 0.1 in) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
| Source: NOAA (extremes 1893–present) [23] | |||||||||||||
| Climate data for Cedar City (1971 to 2000) | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Record high °F (°C) | 70 (21) | 73 (23) | 77 (25) | 83 (28) | 96 (36) | 101 (38) | 105 (41) | 100 (38) | 97 (36) | 88 (31) | 75 (24) | 68 (20) | 105 (41) |
| Mean daily maximum °F (°C) | 41.8 (5.4) | 46.7 (8.2) | 53.5 (11.9) | 61.2 (16.2) | 71.1 (21.7) | 83.1 (28.4) | 89.4 (31.9) | 87.1 (30.6) | 78.9 (26.1) | 66.1 (18.9) | 51.6 (10.9) | 42.7 (5.9) | 64.4 (18.0) |
| Mean daily minimum °F (°C) | 18.5 (−7.5) | 22.8 (−5.1) | 28.4 (−2.0) | 33.7 (0.9) | 41.5 (5.3) | 50.1 (10.1) | 57.8 (14.3) | 56.8 (13.8) | 47.6 (8.7) | 36.0 (2.2) | 25.9 (−3.4) | 18.6 (−7.4) | 36.5 (2.5) |
| Record low °F (°C) | −26 (−32) | −24 (−31) | −1 (−18) | 6 (−14) | 21 (−6) | 26 (−3) | 40 (4) | 36 (2) | 23 (−5) | −7 (−22) | −7 (−22) | −23 (−31) | −26 (−32) |
| Average precipitation inches (mm) | 0.90 (23) | 0.97 (25) | 1.34 (34) | 1.00 (25) | 0.91 (23) | 0.45 (11) | 0.93 (24) | 1.15 (29) | 0.83 (21) | 1.30 (33) | 0.97 (25) | 0.65 (17) | 11.4 (290) |
| Average snowfall inches (cm) | 9.1 (23) | 9.0 (23) | 8.5 (22) | 5.2 (13) | 1.5 (3.8) | 0.1 (0.25) | 0 (0) | 0 (0) | 0.1 (0.25) | 2.3 (5.8) | 6.1 (15) | 6.0 (15) | 47.9 (121.1) |
| Average precipitation days (≥ 0.01 inch) | 6.4 | 6.5 | 8.8 | 6.6 | 6.1 | 3.2 | 5.3 | 6.4 | 4.7 | 5.8 | 5.6 | 5.8 | 71.2 |
| Average snowy days (≥ 0.1 inch) | 5.1 | 4.4 | 4.7 | 2.9 | 0.8 | 0.1 | 0 | 0 | 0.1 | 1.0 | 3.2 | 3.6 | 25.9 |
| Source: National Oceanic and Atmospheric Administration [24] | |||||||||||||
| Climate data for Provo (1991–2020 normals, extremes 1916–present) | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Record high °F (°C) | 63 (17) | 73 (23) | 84 (29) | 89 (32) | 98 (37) | 105 (41) | 108 (42) | 107 (42) | 101 (38) | 90 (32) | 77 (25) | 72 (22) | 108 (42) |
| Mean maximum °F (°C) | 55 (13) | 63 (17) | 74 (23) | 82 (28) | 90 (32) | 99 (37) | 103 (39) | 100 (38) | 94 (34) | 84 (29) | 70 (21) | 58 (14) | 103 (39) |
| Mean daily maximum °F (°C) | 41.0 (5.0) | 47.5 (8.6) | 58.3 (14.6) | 65.5 (18.6) | 75.5 (24.2) | 87.0 (30.6) | 95.0 (35.0) | 92.7 (33.7) | 82.9 (28.3) | 68.4 (20.2) | 53.0 (11.7) | 41.2 (5.1) | 67.3 (19.6) |
| Daily mean °F (°C) | 32.3 (0.2) | 37.4 (3.0) | 46.3 (7.9) | 52.5 (11.4) | 61.4 (16.3) | 70.9 (21.6) | 78.6 (25.9) | 76.7 (24.8) | 67.3 (19.6) | 54.5 (12.5) | 42.2 (5.7) | 32.7 (0.4) | 54.4 (12.4) |
| Mean daily minimum °F (°C) | 23.5 (−4.7) | 27.2 (−2.7) | 34.3 (1.3) | 39.5 (4.2) | 47.2 (8.4) | 54.7 (12.6) | 62.1 (16.7) | 60.8 (16.0) | 51.8 (11.0) | 40.7 (4.8) | 31.4 (−0.3) | 24.2 (−4.3) | 41.5 (5.3) |
| Mean minimum °F (°C) | 8 (−13) | 13 (−11) | 22 (−6) | 28 (−2) | 35 (2) | 43 (6) | 53 (12) | 52 (11) | 40 (4) | 28 (−2) | 17 (−8) | 10 (−12) | 5 (−15) |
| Record low °F (°C) | −20 (−29) | −20 (−29) | 0 (−18) | 12 (−11) | 27 (−3) | 29 (−2) | 35 (2) | 39 (4) | 21 (−6) | 11 (−12) | 3 (−16) | −30 (−34) | −30 (−34) |
| Average precipitation inches (mm) | 1.95 (50) | 1.59 (40) | 1.55 (39) | 1.95 (50) | 1.97 (50) | 0.93 (24) | 0.51 (13) | 0.77 (20) | 1.24 (31) | 1.59 (40) | 1.39 (35) | 1.81 (46) | 17.23 (438) |
| Average snowfall inches (cm) | 12.5 (32) | 8.5 (22) | 4.0 (10) | 3.1 (7.9) | 0.2 (0.51) | 0 (0) | 0 (0) | 0 (0) | 0 (0) | 0.6 (1.5) | 4.5 (11) | 12.0 (30) | 45.4 (114.91) |
| Average precipitation days (≥ 0.01 in) | 10 | 9 | 9 | 10 | 9 | 6 | 5 | 5 | 6 | 7 | 8 | 9 | 93 |
| Average snowy days (≥ 0.1 in) | 6 | 4 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 6 | 24 |
| Percent possible sunshine | 50 | 55 | 67 | 69 | 71 | 80 | 73 | 79 | 83 | 73 | 50 | 56 | 67 |
| Average ultraviolet index | 2 | 3 | 5 | 7 | 9 | 10 | 10 | 9 | 7 | 4 | 3 | 2 | 6 |
| Source 1: NOAA [25] | |||||||||||||
| Source 2: Weather Atlas [26] | |||||||||||||
Utah is home to more than 600 vertebrate animals [27] as well as numerous invertebrates and insects. [28]
Mammals are found in every area of Utah. Non-predatory larger mammals include the plains bison, [29] [30] elk, [31] moose, [32] mountain goat, [32] mule deer, [32] pronghorn, [33] and multiple types of bighorn sheep. [34] [35] [36] Non-predatory small mammals include muskrat, [32] and nutria. [37] Large and small predatory mammals include the black bear, [32] cougar, [32] Canada lynx, [38] bobcat, [32] fox (gray, red, and kit), [32] coyote, [32] badger, [32] black-footed ferret, [39] mink, [32] stoat, [32] long-tailed weasel, [32] raccoon, [32] and otter. [40]
The brown bear was formerly found within Utah, but has been extirpated. [41] There are no confirmed mating pairs of gray wolf in Utah, though there have been sightings in northeastern Utah along the Wyoming border. [42] [43]
As of January 2020, there were 466 species included in the official list managed by the Utah Bird Records Committee (UBRC). [44] [45] Of these, 119 are classed as accidental, 29 are classed as occasional, 57 are classed as rare, and 10 have been introduced to Utah or North America. Eleven of the accidental species are also classed as provisional.
Due to the miracle of the gulls incident in 1848, the most well known bird in Utah is the California gull, which is the Utah state bird. [46] [47] A monument in Salt Lake City commemorates this event, known as the "Miracle of the Gulls". [47] Other gulls common to Utah include Bonaparte's gull, [48] the ring-billed gull, and Franklin's gull.
Other birds commonly found include the American robin, [49] the common starling, finches (black rosy, [50] Cassin's, [51] and goldfinch), [52] the black-billed magpie, [53] mourning doves, sparrows (house, tree, [54] black-chinned, [55] black-throated, [56] Brewer's, [57] and chipping), [58] Clark's grebe, [59] the ferruginous hawk, geese (snow, cackling, [60] and Canada), [61] eagles (golden and bald), [62] California quail, [63] mountain bluebird, and hummingbirds (calliope, [64] black-chinned, [65] and broad-tailed). [66]
Utah is host to a wide variety of arachnids, insects, mollusks, and other invertebrates. Arachnids include the Arizona bark scorpion, [67] Western black widow spiders, [68] crab spiders, [69] hobo spiders (Tegenaria agrestis), [70] cellar spiders, American grass spiders, woodlouse spiders. [68] Several spiders found in Utah are often mistaken for the brown recluse spider, including the desert recluse spider (found only in Washington County), the cellar spider, and crevice weaving spiders. [71] [72] [73] The brown recluse spider has not been officially confirmed in Utah as of summer 2020 [update] . [74]
One of the most rare insects in Utah is the Coral Pink Sand Dunes tiger beetle, found only in Coral Pink Sand Dunes State Park, near Kanab. [75] It was proposed in 2012 to be listed as a threatened species, [76] but the proposal was not accepted. [77] Other insects include grasshoppers, [78] green stink bugs, [79] the Army cutworm, [80] the monarch butterfly, [81] and Mormon fritillary butterfly. [81] The white-lined sphinx moth is common to most of the United States, but there have been reported outbreaks of large groups of their larvae damaging tomato, grape and garden crops in Utah. [82] Four or five species of firefly are also found across the state. [83]
In February 2009, Africanized honeybees were found in southern Utah. [84] [85] The bees had spread into eight counties in Utah, as far north as Grand and Emery counties by May 2017. [86]
Several thousand plants are native to Utah, [89] including a variety of trees, shrubs, cacti, herbaceous plants, and grasses. As of 2018 [update] , there are 3,930 species of plants in Utah, with 3,128 of those being indigenous and 792 being introduced through various means. [90]
Common trees include pines/piñons (white fir, Colorado, single-leaf, Great Basin bristlecone, ponderosa, Engelmann spruce, Rocky Mountain white), and Acer grandidentatum, quaking aspen, bigtooth maple, Utah juniper, speckled alder, red birch, Gambel oak, desert willow, blue spruce, and Joshua trees. Utah has a number of named trees, including the Jardine Juniper, Pando, [87] [88] and the Thousand Mile Tree. Shrubs include a number of different ephedras (pitamoreal, Navajo, Arizona, Nevada, Torrey's jointfir, and green Mormon tea), sagebrushes (little, Bigelow, silver, Michaux's wormwood, black, pygmy, bud, and Great Basin), blue elderberry, Utah serviceberry, chokecherry, and skunkbush sumac. Western poison oak, poison sumac, and western poison ivy are all found in Utah. [91]
There are many varieties of cacti in Utah's varied deserts, especially in the southern and western parts of the state. Some of these include desert prickly pear, California barrel cactus, fishhook cactus, cholla, beavertail prickly pear, and Uinta Basin hookless cactus. Despite the desert climate, many different grasses are found in Utah, including Mormon needlegrass, bluebunch wheatgrass, western alkali grass, squirreltail, desert saltgrass, and cheatgrass.
Several invasive species of plants are considered noxious weeds by the state, including Bermuda grass, field bindweed, henbane, jointed goatgrass, Canada thistle, Balkan and common toadflax, giant cane, couch grass, St. John's wort, hemlock, sword grass, Russian olive, myrtle spurge, Japanese knotweed, salt cedar, and goat's head. [92]
Utah is a landlocked state in the Mountain West subregion of the Western United States. It is one of the Four Corners states, sharing a border with Arizona, Colorado, and New Mexico. It also borders Wyoming to its northeast, Idaho to its north, and Nevada to its west. In comparison to all the U.S. states and territories, Utah, with a population of just over three million, is the 13th largest by area, the 30th most populous, and the 11th least densely populated. Urban development is mostly concentrated in two regions: the Wasatch Front in the north-central part of the state, which includes the state capital, Salt Lake City, and is home to roughly two-thirds of the population; and Washington County in the southwest, which has somewhat more than 180,000 residents. Most of the western half of Utah lies in the Great Basin.
The Great Salt Lake is the largest saltwater lake in the Western Hemisphere and the eighth-largest terminal lake in the world. It lies in the northern part of the U.S. state of Utah and has a substantial impact upon the local climate, particularly through lake-effect snow. It is a remnant of Lake Bonneville, a prehistoric body of water that covered much of western Utah.
Wasatch County is a county in the U.S. state of Utah. As of the 2020 United States Census, the population was 34,788. Its county seat and largest city is Heber City. The county was named for a Ute word meaning "mountain pass" or "low place in the high mountains".
Uintah County is a county in the U.S. state of Utah. As of the 2020 United States Census the population was 35,620. Its county seat and largest city is Vernal. The county was named for the portion of the Ute Indian tribe that lived in the basin.
The Great Basin is the largest area of contiguous endorheic watersheds, those with no outlets to the ocean, in North America. It spans nearly all of Nevada, much of Utah, and portions of California, Idaho, Oregon, Wyoming, and Baja California. It is noted for both its arid climate and the basin and range topography that varies from the North American low point at Badwater Basin in Death Valley to the highest point of the contiguous United States, less than 100 miles (160 km) away at the summit of Mount Whitney. The region spans several physiographic divisions, biomes, ecoregions, and deserts.
The Wasatch Range or Wasatch Mountains is a mountain range in the western United States that runs about 160 miles (260 km) from the Utah-Idaho border south to central Utah. It is the western edge of the greater Rocky Mountains, and the eastern edge of the Great Basin region. The northern extension of the Wasatch Range, the Bear River Mountains, extends just into Idaho, constituting all of the Wasatch Range in that state.
The Colorado Plateau is a physiographic and desert region of the Intermontane Plateaus, roughly centered on the Four Corners region of the southwestern United States. This plateau covers an area of 336,700 km2 (130,000 mi2) within western Colorado, northwestern New Mexico, southern and eastern Utah, northern Arizona, and a tiny fraction in the extreme southeast of Nevada. About 90% of the area is drained by the Colorado River and its main tributaries: the Green, San Juan, and Little Colorado. Most of the remainder of the plateau is drained by the Rio Grande and its tributaries.
The Denver and Salt Lake Railway (D&SL) was a U.S. railroad company located in Colorado. It was incorporated in 1902 as the Denver, Northwestern and Pacific (DN&P) Railway with the goal of connecting Denver, Colorado with Salt Lake City, Utah. It underwent numerous reorganizations throughout its financially troubled history and, by the time it was acquired in 1931 by the Denver and Rio Grande Western Railroad, it had advanced only as far west as Craig, Colorado. After its acquisition, it was connected to the D&RGW main to give the D&RGW a more direct route to Denver via the eastern half of the DS&L. The portions of the D&SL still in use today comprise the Moffat Tunnel Subdivision of Union Pacific Railroad's Central Corridor, and Amtrak’s California Zephyr uses a portion of the former D&SL between Denver and Bond.
The Uinta Mountains are an east-west trending mountain range in northeastern Utah extending a short distance into northwest Colorado and slightly into southwestern Wyoming in the United States. As a subrange of the Rocky Mountains, they are unusual for being the highest range in the contiguous United States running east to west, and lie approximately 100 miles (160 km) east of Salt Lake City. The range has peaks ranging from 11,000 to 13,528 feet, with the highest point being Kings Peak, also the highest point in Utah. The Mirror Lake Highway crosses the western half of the Uintas on its way to Wyoming. Utah State Route 44 crosses the east end of the Uintas between Vernal and Manila.
Uinta National Forest is a national forest located in north central Utah, US. It was originally part of the Uinta Forest Reserve, created by President Grover Cleveland on 2 February 1897. The name is derived from the Ute word Yoov-we-teuh which means pine forest. Because of changes to the boundaries over the years, the Uinta Mountains are now located in the Wasatch-Cache National Forest. In August 2007 it was announced that the Uinta National Forest would merge with the Wasatch–Cache National Forest based in Salt Lake City, Utah, 50 miles (80 km) north of Provo, Utah.
The Uinta Basin is a physiographic section of the larger Colorado Plateaus province, which in turn is part of the larger Intermontane Plateaus physiographic division. It is also a geologic structural basin in eastern Utah, east of the Wasatch Mountains and south of the Uinta Mountains. The Uinta Basin is fed by creeks and rivers flowing south from the Uinta Mountains. Many of the principal rivers flow into the Duchesne River which feeds the Green River—a tributary of the Colorado River. The Uinta Mountains form the northern border of the Uinta Basin. They contain the highest point in Utah, Kings Peak, with a summit 13,528 feet above sea level. The climate of the Uinta Basin is semi-arid, with occasionally severe winter cold.
The Duchesne River, located in the Uintah Basin region of Utah in the western United States, is a tributary of the Green River. The watershed of the river covers the Northeastern corner of Utah. The Duchesne River is 115 miles (185 km) long, and drains a total land area of 3,790 square miles (9,800 km2).
Little Cottonwood Creek is one of the principal streams entering Salt Lake Valley from the east. The creek rises near the summit of the Wasatch Mountains, a short distance south of the ski resort town of Alta, and flows in a westerly direction through Little Cottonwood Canyon until it emerges into Salt Lake Valley about eleven miles from its source. Thence its course is north westerly through Sandy, Midvale and Murray, Utah until it empties into the Jordan River, about six miles south of Salt Lake City. Its whole length is nearly 27 miles (43 km). The headwaters of Little Cottonwood Creek are in Little Cottonwood Canyon, a glaciated canyon in Uinta-Wasatch-Cache National Forest and the Wasatch and Uinta Mountains eco-region. One of the main tributaries of the creek rises in Cecret Lake, a small sheet of water situated near Alta. The entire Little Cottonwood Creek drainage basin encompasses 46 square miles (120 km2), ranging in elevation from about 4,490 to 11,500 feet.
Big Cottonwood Creek is located in the Wasatch Mountains just east of Salt Lake City. It is part of the Big Cottonwood Creek Watershed, which ranges in elevation from 5,000 to 10,500 feet with the headwaters around 9,600 feet. The creek flows through the Big Cottonwood Canyon in a westerly direction until it emerges into Salt Lake Valley about eighteen miles (29 km) from its highest source. Thence its course is northwesterly through Cottonwood Heights, Holladay, and Murray, Utah for a little over twenty-four miles from the headwaters until it empties into the Jordan River about five miles (8.0 km) south of Salt Lake City. The water eventually flows into the Great Salt Lake. In the summer, its waters are all used for irrigation purposes. From its source to its original outlet in the Jordan River is about twenty-six miles.
The Mountain states form one of the nine geographic divisions of the United States that are officially recognized by the United States Census Bureau. It is a subregion of the Western United States.
The Uinta Basin Rail project is a proposed 100-mile (160 km) rail line to connect the shale oil rich Uinta Basin region of eastern Utah to the national rail network. Numerous proposals have been made, some as far back as 1902, that are still under consideration. The current effort is a public-private partnership between a coalition of 7 counties in Utah, the Rio Grande Pacific Corporation and Drexel Hamilton Infrastructure Partners. The railroad is also backed by the Ute Tribe who hold a 5% stake in the project. If the rail line is built it will be the first major greenfield rail line built in the United States since the Chicago and North Western’s line to the Powder River Basin was built in the early 1980s. The Surface Transportation Board approved construction of the line in December 2021, however, the approval is being challenged in court by various environmentalist groups. In 2024, the Supreme Court of the United States agreed to hear the case Seven County Infrastructure Coalition v. Eagle County, involving the approval to build the rail line.
And finally, false reports of brown recluse spiders incite fear in Utah residents (only the desert recluse spider, found in Washington County, exists in Utah).
