There was little in the way of building materials, so the families dug into the bluffs of the Jordan River for shelter. In 1849, Samuel and John Bennion and several other families moved south crossing the river on the ice in January. The first Mormon pioneer settlers, Joseph and Susanna Harker from England built a log cabin on the west side of the Jordan River in November 1848 on what was called then "the Church Farm" near 3300 South. Spanish and then Mexican land claims remained until the Treaty of Guadalupe Hidalgo which ended the Mexican War in 1853 and ceded the whole of northern Mexico to the United States including a few thousand Mormon settlers who had taken up residence in July 1847. The whole region was called "Teguayo" and "Lake Copalla" (Utah Lake) appear on maps of Spanish Nuevo Mexico. There are poorly documented suggestions that Spanish missionaries, soldiers, and explorers came through the area beginning in the mid-1600s. Whether the name is his creation or an approximation of something they said is unknown. At least one local settler called these people the "Yo-No'". Early settlers observed small encampments of Ute in the cottonwoods along the Jordan River. A well-used Ute trail wound along the west side of the river at approximately 1300 West which the Ute used in spring and fall. Most of the area was dry sagebrush-covered land without any natural water sources except the Jordan River. In more recent times Ute bands passed through the valley between the marshes of the Great Salt Lake and Utah Valley. A large Fremont settlement on City Creek used the land where Taylorsville is located as hunting and foraging especially along the river. Some of this region's first named visitors were Fremont people who used the area to hunt and gather food along the Jordan River more than a thousand years ago. Less than five miles (8 km) from Taylorsville evidence of people killing and eating a mammoth have been found. The first (unnamed) people in the region appeared during or after the last ice age on the shores of what remained of Lake Bonneville. Bennion Hill is the eastern end of a wide ridge that rises toward Farnsworth Peak in the Oquirrh Mountains to the west. Like most desert soils, it has little organic material and is hard to work.Ī broad, east-west running ridge called "Bennion Hill" rises perhaps a hundred and fifty feet above the surrounding area. As Lake Bonneville dried up over the past 14,000 years, the salt from the breakdown of rock remains, making the soil alkaline. Lake Bonneville shaped the topography of the area and deposited lake bottom clay and sand. The inactive Taylorsville Fault has been traced down the center of the Salt Lake Valley. Beneath the surface, Taylorsville sits on more than a kilometer of unconsolidated rock, sand, and clay. The land on which Taylorsville is located is part of an interconnected alluvial plain that was formed by the wearing down of the Wasatch and Oquirrh Mountains to the east and west. The city officially became the City of Taylorsville during the centennial anniversary of Utah's statehood in 1996. These communities incorporated through a vote of the people with over 70 percent approval in September 1995. The area called Taylorsville today is made up of two historic communities in the central part of Salt Lake County: Taylorsville and Bennion. It is located in the middle of the Salt Lake Valley. The city is located adjacent to Interstate 215 and Bangerter Highway. Taylorsville was incorporated from the Taylorsville–Bennion CDP and portions of the Kearns metro township on July 1, 1996. The population was 60,448 at the time of the 2020 census. It is part of the Salt Lake City metropolitan area. Taylorsville is a city in Salt Lake County, Utah.
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