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Taylorsville High School

1981 establishments in UtahEducational institutions established in 1981Public high schools in UtahSchools in Salt Lake County, Utah
Taylorsvillehigh
Taylorsvillehigh

Taylorsville High School is a public high school established in 1981, located in Taylorsville, Utah, United States. The principal is Mrs. Emily Liddell. The mascot is the Wilbur the Warrior. The current enrollment is around 2,900 students and represents many different ethnic groups. Taylorsville High is one of eight high schools in Granite School District. Taylorsville High is located in the central part of the Salt Lake Valley and was built in 1981 to serve the growing population of the Taylorsville area. School boundaries are roughly Jordan River to 3100 West and 4100 South to 6600 South (excluding the area between 4500 S and 4700 S and approximately Jordan River and 950 W). Taylorsville has immense pride in its history and continues to strive to improve, grow, and excel academically. Taylorsville has successful programs for AVID (Advancement Via Individual Determination), JROTC and Latinos in Action, along with large AP program.

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Taylorsville High School
Redwood Road,

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N 40.655555555556 ° E -111.93666666667 °
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Taylorsville High School

Redwood Road 5225 S
84123
Utah, United States
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Utah's 4th congressional district

Utah's 4th congressional district is a congressional district created by the state legislature as a result of reapportionment by Congress after the 2010 Census showed population increases in the state relative to other states. Prior to 2010 reapportionment, Utah had three congressional districts.Some 85 percent of the new district is concentrated in Salt Lake County and it includes a portion of Salt Lake City, which is shared with the 2nd and 3rd districts; it also includes parts of Utah, Juab, and Sanpete counties. Candidates first appeared on the 2012 ballot. As a result of redistricting, the 2012 party candidates included Democratic U.S. Congressman Jim Matheson, who had previously represented Utah's 2nd congressional district from 2001 to 2013. The Republican nominee was Mia Love, mayor of Saratoga Springs and running for Congress for the first time. She won the Republican nomination in 2012 over two state representatives, Stephen Sandstrom and Carl Wimmer, at the Republican state convention. Democratic candidate Matheson narrowly won the election against Love on November 6, 2012, and represented Utah's 4th congressional district until January 2015. He decided not to seek re-election. In 2014, Mia Love ran again for the seat and won in the general election, defeating Democratic candidate Doug Owens. She became the first Haitian American and the first black female Republican elected to Congress, as well as the first black person of either sex elected to Congress from Utah. In the 2018 elections, Love ran for a third term, losing to Salt Lake County mayor Ben McAdams by 694 votes out of almost 270,000. As a result of McAdams's election, the district became the most Republican district in the country to be represented by a Democrat. In 2020, Republican Burgess Owens narrowly defeated McAdams to regain the congressional seat for the Republican Party.

Little Cottonwood Creek (Salt Lake County, Utah)
Little Cottonwood Creek (Salt Lake County, Utah)

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 (1,370 to 3,510 m).Communities were founded around the creek soon after the pioneer settlement of Salt Lake Valley in 1847 and supported agricultural activities. Following the discovery of gold, silver, copper, and lead in nearby canyons in the 1870s, ore-refining activities brought an influx of people to these communities. During the mid-to the late 1900s, residential land use replaced agriculture as the dominant land-use type in the lower Little Cottonwood Creek drainage basin as the population of Salt Lake Valley expanded.Land cover upstream from the mouth of Little Cottonwood Canyon is 60 percent forest land and 33 percent rangeland. The watershed in Little Cottonwood Canyon is protected as a drinking water source but receives extensive recreational use. The urbanized part of the Little Cottonwood Creek drainage basin includes that part from the mouth of Little Cottonwood Canyon to the confluence with the Jordan River. The stream provides electrical power generation for Murray City. The first legitimate mining operation in Little Cottonwood Canyon was established in 1865. The ore deposits in Little Cottonwood Canyon yielded principally silver and lead with some copper, gold, and zinc. These ore deposits were formed mainly in shale, limestone, and dolomite. Galena or lead sulfide was the common primary lead mineral of the area. Argentite was found in most primary ores and was probably an abundant primary silver mineral. Ore production varied with time because of the nature of the deposits and the scattered control of holdings. The 1870s were especially productive when rich deposits were mined. Several smelters operated along Little Cottonwood Creek during the 1870s. Smelting operations produced a variety of by-products that included arsenic, matte, arsenical speiss, and slag. Past mining activities and ore-smelting operations continue to influence the water chemistry of the stream. Mine and smelter tailings in the Little Cottonwood Creek drainage basin can contribute trace metals to the stream. Metals from fluvial tailings deposits in the stream can be re-suspended and dissolved in the stream. Currently, the greatest threat to the streams ecosystem is pesticides from residential run-off.

William McLachlan Farmhouse

The William McLachlan Farmhouse, at 4499 S. 3200 West, in what is now West Valley City, Utah in Salt Lake County, Utah, listed on the National Register of Historic Places in 1980.It was built originally as a 22 by 21 feet (6.7 m × 6.4 m) brick and adobe house, during 1884–1885. The two rooms are adobe lined underneath plaster. The masonry work was done by Ed Ashton, and according to McLachlan's journal a man named Bridge did the plastering.The house was built by William McLachlan, a polygamist, who was "like many of the less wealthy polygamists of the period, extremely distressed by the consequences of anti-polygamy raids. In order that his wives not be left penniless should he be arrested and imprisoned, McLachlan purchased land and built this home in a then-remote area "over Jordan". When it was completed in March 1885 it became home for Maggie Naismith, his second wife, and her five children. McLachlan himself vanished into the underground for nearly eight years. Part of the time he was employed as a carpenter on the Manti temple and used his earnings there to support his families. His wives were visited as often as it was safe, and Margaret received title to her house in 1886 to protect her and her husband from loss of property should he be caught and prosecuted. Fortunately, McLachlan was never brought to trial." However, he was unable to complete the construction of this house, and death by diphtheria of three sons in 1894 contributed to his failure to make a success of the farm.