How is Bear Lake filled?

In 1911 the majority of the flow of the Bear River was diverted into Bear Lake via Mud Lake and a canal from Stewart Dam, ending 11,000 years of separation between the lake and that river system.



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Specifically, a lack of nitrogen and phosphorous severely limits algal growth in Bear Lake, keeping its water clean and blue.

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Bear Lake contains abundant suspended microscopic particles of white-colored calcium carbonate (lime) that reflect the water's natural blue color back to the surface, giving the lake its intense turquoise-blue color.

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It was formed by fault subsidence that continues today, slowly deepening the lake along the eastern side. In 1911 the majority of the flow of the Bear River was diverted into Bear Lake via Mud Lake and a canal from Stewart Dam, ending 11,000 years of separation between the lake and that river system.

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Known for its intense turquoise colored water, the lake is often called the Caribbean of the Rockies. A gradual slope to the lake bottom provides an enormous swimming area in the summer. In the winter, those with buckets and nets can ice fish for the Bonneville cisco, a fish found nowhere else on earth.

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Bear Lake is stratified in summer-spring where lighter water overlies denser water. During the winter months the mixing processes of winds and surface cooling break down the layers and the lake freezes over. Bear Lake does not completely freeze over every year but typically three out of five years.

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Bear Lake is a natural freshwater lake covering more than 112 square miles of land that straddles the Utah-Idaho border. It is often called the “Caribbean of the Rockies” for its unique turquoise-blue color, which is due to the reflection of limestone deposits suspended in the lake.

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It's high elevation makes this region one of the coldest areas in the state. The intense inversion also accounts for some extremely cold temperatures in winter. The coldest temperature on record, 50°F below zero, was recorded at Woodruff in February of 1899.

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Bear Lake is a natural freshwater lake on the Idaho–Utah border in the Western United States. About 109 square miles in size, it is split about equally between the two states; its Utah portion comprises the second-largest natural freshwater lake in Utah, after Utah Lake.



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Bear Lake is a natural freshwater lake on the Idaho–Utah border in the Western United States. About 109 square miles in size, it is split about equally between the two states; its Utah portion comprises the second-largest natural freshwater lake in Utah, after Utah Lake.



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The shells have lasted this long because of the calcium chemistry in Bear Lake water. Some that do get crushed become part of our sand. According to a U.S. Geological Survey study, the shells were in great abundance in the shallows of Bear Lake when the lake was around 50 feet higher and filled the whole valley.

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The decline has for years forced crews to push the docks forward to reach the lake's receding shoreline. The lake is still more than 14.5 feet below its capacity and hasn't been full since 2011, according to the water district.

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This was the first recorded account of Europeans seeing the beautiful lake. He attended one of the Native American gatherings at the south end of Bear Lake in 1819, aptly naming the area Black Bear Lake after the abundance of black bears in the area. This was later shortened to Bear Lake.

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There are no current health advisories for this water body. Conditions may change quickly. Check before entering the water and know how to spot a harmful algal bloom.

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There are no current health advisories for this water body. Conditions may change quickly. Check before entering the water and know how to spot a harmful algal bloom.

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Located near St. Charles, Idaho, Bear Lake North Beach just might be the best beach at Bear Lake. It's definitely one of the most popular, so make sure you get there early before they stop letting people in. Spend your time with friends and family swimming, kayaking, or water skiing.

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The volume is 187,800 cubic meters (153 acre-feet). The penetration of solar radiation into a lake is of fun- damental importance to the organisms dwelling there. Solar radiation is the overwhelming source of heat to warm the waters of Bear Lake.

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The decline has for years forced crews to push the docks forward to reach the lake's receding shoreline. The lake is still more than 14.5 feet below its capacity and hasn't been full since 2011, according to the water district.

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Blue-Green Algae is in fact not an algae at all, it is a bacteria (cyanobacteria). This type of bacteria is found in many lakes, ponds, and reservoirs across the world. They are usually present in low numbers, but can become very abundant in warm, shallow, undisturbed surface water that receives a lot of sunlight.

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If you plan to camp overnight, please use one of the many public and private camping areas around the lake (see map). No camping after 10 p.m. on the public beaches or exposed bed of Bear Lake.

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You want to jump in but watch out for leeches - Review of Bear Lake, Rocky Mountain National Park, CO - Tripadvisor.

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