Ricks Spring
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Ricks Spring is a
karst spring A karst spring or karstic spring is a Spring (hydrology), spring (exsurgence, outflow of groundwater) that is part of a karst hydrological system. Description Because of their often conical or inverted bowl shape, karst springs are also known i ...
, a natural water outflow from a cave in
Logan Canyon Logan Canyon is a canyon in the western United States in northeastern Utah, which cuts its way through the Bear River Mountains, a branch of the Wasatch Range. It is popular for both summer and winter activities, especially rock-climbing, hi ...
within the Wasatch-Cache National Forest in northeast
Utah Utah is a landlocked state in the Mountain states, 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 the northea ...
. The spring is not an artesian source, but comes from the
Logan River The Logan River (Yugambeh dialect, Yugambeh: ''Dugulumba'') is a perennial river in the Scenic Rim Region, Scenic Rim, City of Logan, Logan and City of Gold Coast, Gold Coast local government areas of the South East Queensland, South East region ...
. Ricks Spring is the best known of several springs in an underground water network of the area.


History

Thomas E. Ricks settled in the nearby
Cache Valley Cache Valley ''( Shoshoni: Seuhubeogoi, “Willow Valley”)'' is a valley of northern Utah and southeast Idaho, United States, that includes the Logan metropolitan area. The valley was used by 19th century mountain men and was the site of th ...
in 1859. Logan Canyon was an area rich with timber and other resources for nearby settlements, his explorations of which being some of the first documentations of the area. At the recommendation of
Brigham Young Brigham Young ( ; June 1, 1801August 29, 1877) was an American religious leader and politician. He was the second President of the Church (LDS Church), president of the Church of Jesus Christ of Latter-day Saints (LDS Church) from 1847 until h ...
, Ricks and others in the community began constructing a road to Bear Lake Valley. The road to Ricks Spring was the first section to be completed before winter, and within a decade, the area became a popular excursion point for camping and automobiling. The road is now part of the Logan Canyon Scenic Byway, part of US Route 89.


Hydrology

Since its discovery, people visiting the spring often drank from it, bringing home jugs and barrels of the "fresh spring water" under the assumption it came from a deep aquifer. They often became sick with
giardia ''Giardia'' ( or ) is a genus of anaerobic flagellated protozoan parasites of the phylum Metamonada that colonise and reproduce in the small intestines of several vertebrates, causing the disease giardiasis. Their life cycle alternates be ...
indicating the water was not from an artesian source. In the 1950s hydrogeologists noticed a pattern between the flows of the Logan River and theorized a connection between them. In 1972, a severe winter froze the river, jamming it in some locations causing water to fill upstream. Ricks Spring began to flow early that year, and then subsided when the river level dropped again confirming the link between the river and the spring. Later that summer dye tracing was used in the Logan River and the dye was found in Ricks Spring, confirming the water source of the spring. Further dye tracing found that the Logan River is not the only source for Ricks Spring. Several minor streams, located as far as five miles away, and up to 2600 feet higher in elevation, also feed into the underground network that feeds Ricks Spring. Water from Tony Grove Lake also contributes to Ricks Spring. Ricks Spring is only the most well known of several springs in the Logan Canyon area. The other springs, Dewitt Spring, Wood Camp Hollow Spring, Logan Cave Spring, and Benchmark Spring, all have water sources that overlap with at least one of the other springs. Dewitt Spring is a water source for the city of Logan, the other springs, including Ricks Spring all recharge the Logan River.


Geology

The local rock is made up of
sedimentary Sedimentary rocks are types of rock formed by the cementation of sediments—i.e. particles made of minerals (geological detritus) or organic matter (biological detritus)—that have been accumulated or deposited at Earth's surface. Sedime ...
layers. Pressure and earthquakes have caused the rock to fold and fracture exposing weak points. Over time water flowing through these points eroded through the limestone creating a path from the river and other inflows at high elevation to flow and emit from the spring. There are two caves at Ricks Spring. An above water cave extends into the rock about 25 feet. The second cave is an extensive network of both wet and dry passages that is only accessible by
cave diving Cave-diving is underwater diving in water-filled caves. It may be done as an extreme sport, a way of exploring flooded caves for scientific investigation, or for the underwater search and recovery, search for and recovery of divers or, as in th ...
. , it has been explored to about 2200 feet.


References


External links

{{coord, 41, 50, 38, N, 111, 35, 33, W, region:US-UT_type:landmark, display=title Bodies of water of Cache County, Utah Springs of Utah Caves of Utah Underwater diving sites in the United States