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Great Salt Lake Throughout the Year
Mountain Resorts. South Valley. Southwest Valley. West Valley. Great Salt Lake. Getting Around. Ground Transportation. Public Transportation. GreenBike SLC. Fremont in On that expedition, Kit Carson visited one of the lake's islands and carved a cross near the summit of an island that is now called Fremont Island. Members of the Church of Jesus Christ of Latter-day Saints or Mormons arrived in the area in and used the islands for grazing cattle and also enjoyed swimming in the lake and holding picnics on its shores.
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- Surface features and chemistry;
- Bonneville Salt Flats?
- Bonneville Salt Flats?
Though momentous, this wedding of the rails was not efficient; Great Salt Lake had caused the engineers to build a detour onto the rugged mountains of the peninsula. In the wooden trestle was replaced with a rock-fill causeway that is still in use today. As Lake Bonneville shrank, all of the minerals in it — including salt — concentrated into steadily less water. Every year, 2. A terminal lake holds everything that has ever entered the lake except water, which can leave by evaporation.
Great Salt Lake is a sodium chloride lake, said Baxter. The hypersaline northern arm also called Gunnison Bay is about 30 percent salt. The southern portion of the lake also called Gilbert Bay fluctuates between 6 and 27 percent salinity. About 4.
These rivers carry fresh water from melted snow in the Wasatch Mountains into the eastern area of the lake. Sixty-six percent of fresh water entering the lake comes from these rivers. Additional fresh water comes from rainfall, groundwater and springs, according to Great Salt Lake Ecosystem Program. No feeders reach Gunnison Bay in the northwestern part of the lake. The western part of the Great Salt Lake watershed is desert and does not bring water into the lake except in very wet years.
Gunnison Island is home to a large population of pelicans. Several of the larger islands in the southern part of Great Salt Lake, including Antelope Island, become peninsulas when the water level is low. The area was separated from Great Salt Lake in and is now a state park. Earthwork artist Robert Smithson built it in Smithson used more than 6, tons 5, metric tons of black basalt rocks and earth dug up from the site to create a 1,foot-long m spiral that extends into the water, according to Dia Art.
The largest salt water lake in the Western Hemisphere
It is visible when the water level is below 4, feet 1, m altitude. The Union Pacific Railroad Northern Causeway is 21 miles 33 km long and was built as a railroad shortcut. Human-built features like causeways and dykes impede water flow, which creates microenvironments, said Jaimi Butler, coordinator of the Great Salt Lake Institute. The clearest example of this is in the far north of the lake, where the Union Pacific Railroad Northern Causeway blocks freshwater flow and has created a super-saturation of salt and an extreme environment.
Mineral extractionis a major economic feature of Great Salt Lake, said Butler. According to USGS, five businesses extract salt and other minerals from the lake through solar evaporation ponds. No food-grade salt comes from the lake; Great Salt Lake salt is used for deicers, road salt, water softeners and salt licks for livestock. Additionally, said Butler, a massive brine shrimp harvest occurs every fall. The brine shrimp are primarily sent to Asia and South America where they are used as feeders for commercially grown prawn and fish. Among Utah residents, Great Salt Lake is famous for occasionally emitting a stench like rotten eggs.
In , John C. Fremont led the first scientific expedition to the lake, but with winter coming on, he did not take the time to survey the entire lake. That happened in under the leadership of Howard Stansbury Stansbury discovered and named the Stansbury mountain range and Stansbury island. Stansbury also published a formal report of his survey work which became very popular. His report of the area included a discussion of Mormon religious practices based on Stansbury's interaction with the Mormon community in Great Salt Lake City , which had been established three years earlier in Beginning in November , artist and author Alfred Lambourne spent a year living on the remote Gunnison Island , where he wrote a book of musing and poetry, Our Inland Sea.
From November to March , he was alone.
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In March, a few guano sifters arrived to harvest and sell the guano of the nesting birds as fertilizer. Lambourne included musings about these guano sifters in his work. Lambourne left the island early in the winter of along with the first group of guano sifters. Salt Lake City and its suburbs are located to the south-east and east of the lake, between the lake and the Wasatch Mountains , but land around the north and west shores are almost uninhabited.
- The largest salt water lake in the Western Hemisphere;
- Salt Lake Desert?
- Winter: November-March;
The Great Salt Lake is fed by three major rivers and several minor streams. The three major rivers are each fed directly or indirectly from the Uinta Mountain range in northeastern Utah. The Bear River starts on the north slope of the Uintas and flows north past Bear Lake , into which some of Bear River's waters have been diverted [14] via a man-made canal into the lake, but later empty back into the river by means of the Bear Lake Outlet.
The river then turns south in southern Idaho and eventually flows into the northeast arm of the Great Salt Lake. The Weber River also starts on the north slope of the Uinta Mountains and flows into the east edge of the lake. The Jordan River does not receive its water directly from the Uintas, rather it flows from freshwater Utah Lake , which itself is fed primarily by the Provo River ; the Provo River does originate in the Uintas, a few miles from the Weber and Bear.
Due to its shallowness, the water level can fall dramatically in dry years and rise during high-precipitation years, thereby reflecting prolonged drought or wet periods. The change in the level of lake level is strongly modulated by the Pacific Ocean through atmospheric circulations that fluctuate at low frequency. The mostly solid causeway supporting the railway divides the lake into three portions: the north-east arm, north-west arm, and southern. Because no rivers, except a few minor streams, flow directly into the north-west arm, Gunnison Bay , it is substantially saltier than the rest of the lake.