| Lake Powell | |
|---|---|
 | |
  Lake Powell  Lake Powell  Lake Powell | |
| Location | Utah andArizona, United States |
| Coordinates | 36°56′10″N111°29′03″W / 36.93611°N 111.48417°W /36.93611; -111.48417 (Glen Canyon Dam) |
| Type | Reservoir |
| Primary inflows | |
| Primary outflows | Colorado River |
| Catchment area | 280,586 km2 (108,335 sq mi) |
| Basin countries | United States |
| Managing agency | National Park Service |
| Built | September 13, 1963 (1963-09-13) |
| Max. length | 186 mi (299 km) |
| Max. width | 25 mi (40 km) (maximum) |
| Surface area | 161,390 acres (65,310 ha) |
| Average depth | 132 ft (40 m) |
| Max. depth | 583 ft (178 m) |
| Water volume | |
| Residence time | 7.2 years |
| Shore length1 | 3,057 km (1,900 mi) |
| Surface elevation | |
| Website | www |
| 1 Shore length isnot a well-defined measure. | |
Lake Powell is areservoir on theColorado River inUtah andArizona, United States. It is a major vacation destination visited by approximately two million people every year. It holds 24,322,000 acre-feet (3.0001×1010 m3) of water when full, second in the United States to onlyLake Mead - though Lake Mead has fallen below Lake Powell in size several times during the 21st century in terms of volume of water, depth and surface area.[citation needed]
Lake Powell was created by the flooding ofGlen Canyon by theGlen Canyon Dam, which also led to the 1972 creation ofGlen Canyon National Recreation Area, a popular summer destination of public land managed by theNational Park Service. The reservoir is named forJohn Wesley Powell, a civil war veteran who explored the river via three wooden boats in 1869. It lies primarily in southern Utah, with a small portion in northern Arizona.
Lake Powell is a water storage facility for the Upper Basin states of theColorado River Compact (Colorado,Utah,Wyoming andNew Mexico). The Compact specifies that the Upper Basin states are to provide a minimum annual flow of 7,500,000 acre-feet (9.3 km3) to the Lower Basin states (Arizona, Nevada, and California).
According to US Geological Survey and the Bureau of Reclamation report, in addition to water loss, Lake Powell faced an average annual loss in storage capacity of about 33,270 acre-feet, or 11 billion gallons, per year between 1963 and 2018 because of sediments flowing in from theColorado andSan Juan rivers. Those settle at the bottom of the reservoir and decrease the total amount of water the reservoir can hold.[2] Environmentalists have pushed to drain Lake Powell and restore Glen Canyon to its natural, free-flowing state.[3][4][5]
In the 1940s and early 1950s, theUnited States Bureau of Reclamation planned to construct a series of Colorado River dams in the rugged Colorado Plateau province of Colorado, Utah, and Arizona. Glen Canyon Dam was born of a controversial damsite the Bureau selected inEcho Park, in what is nowDinosaur National Monument in Colorado. A small but politically effective group of objectors, led byDavid Brower of theSierra Club, succeeded in defeating the Bureau's bid, citing Echo Park's natural and scenic qualities as too valuable to submerge.
Glen Canyon Dam was built to solve the downstream delivery obligations of the Upper Basin states. Lake Powell is an "aquatic bank" built to fulfill the terms of the "Compact Calls" of Lower Basin.
Construction onGlen Canyon Dam began with a demolition blast keyed by the push of a button by PresidentDwight D. Eisenhower at his desk in theOval Office on October 1, 1956, which started clearing tunnels for water diversion. On February 11, 1959, water flowed through the tunnels so dam construction could begin. Later that year, the bridge was completed, allowing trucks to deliver equipment and materials for the dam and also for the new town ofPage, Arizona.
Concrete placement started around the clock on June 17, 1960. The last bucket of over 5 million cubic yards (4,000,000 m3) was poured on September 13, 1963. The dam is 710 feet (216 m) high and the surface elevation of the water at full-pool is approximately 3700 feet (1100 m). Construction cost $155 million, and 18 lives were lost. On September 22, 1966, Glen Canyon Dam was dedicated byLady Bird Johnson. From 1970 to 1980, turbines and generators were installed for hydroelectricity.
Upon completion of Glen Canyon Dam on September 13, 1963, the Colorado River began to back up, no longer being diverted through the tunnels. The newly flooded Glen Canyon formed Lake Powell. Sixteen years elapsed before the lake filled to the 3,700 feet (1,100 m) level on June 22, 1980. The lake level fluctuates considerably depending on the seasonal snow runoff from the Rocky Mountains.[6][7][8] The all-time highest water level was reached on July 14, 1983, during one of the heaviest Colorado River floods in recorded history, in part influenced by a strongEl Niño event. The lake rose to 3,708.34 feet (1,130.30 m) above sea level, with a water content of 25,757,086 acre-feet (31.770898 km3).[9] It lies primarily in parts ofGarfield,Kane, andSan Juan counties in southern Utah, with a small portion inCoconino County in northern Arizona. The northern limits of the lake extend at least as far as theHite Crossing Bridge.
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Colorado River flows have been below average since 2000 as a result of thesouthwestern North American megadrought, leading to lower lake levels. In winter 2005 (before the spring run-off) the lake reached its then-lowest level since filling, an elevation of 3,555.10 feet (1,083.59 m)[9] above sea level, which was approximately 150 feet (46 m) below full pool. After 2005, the lake level slowly rebounded, although it has not filled completely since then. Summer 2011 saw the third largest June and the second largest July runoff since the closure of Glen Canyon Dam, and the water level peaked at nearly 3,661 feet (1,116 m), 77 percent of capacity, on July 30.[9] However, water years 2012 and 2013 were, respectively, the third and fourth-lowest runoff years recorded on the Colorado River. By April 9, 2014, the lake level had fallen to 3,574.31 feet (1,089.45 m), largely erasing the gains made in 2011.[9]
Colorado River levels returned to normal during water years 2014 and 2015 (pushing the lake to 3,606 feet (1,099 m)) by the end of water year 2015.[9] The Bureau of Reclamation in 2014 reduced the Lake Powell release from 8.23 to 7.48 million acre-feet, for the first time since the lake filled in 1980. This was done due to the "equalization" guideline which stipulates that an approximately equal amount of water must be retained in both Lake Powell andLake Mead, in order to preserve hydro-power generation capacity at both lakes. This resulted in Lake Mead declining to the lowest level on record since the 1930s.
Long-term water level decline continued, forcing an emergency release of water from theFlaming Gorge Reservoir in July 2021.[10] and by April 22, 2022, Lake Powell was at 3,522.24 feet (1,073.58 m) in elevation – just22.88% of capacity. This marks the lowest water level for Lake Powell since it was filled in 1963.[11]
The capacity of Lake Powell has decreased by 7% since 1963 facing an average annual loss of 33,270 acre-feet of storage, due to the inflow of sediments from Colorado and San Juan rivers.[12]
Peer-reviewed studies indicate that storing water in Lake Mead rather than in Lake Powell would yield a savings of 300,000 acre feet of water or more per year, leading to calls by environmentalists to drain Lake Powell and restore Glen Canyon to its natural, free-flowing state.[3][4][5]
These data are for theWahweap climate station on Lake Powell just south of the Utah-Arizona border (Years 1961 to 2012).
| Climate data for Wahweap, AZ | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Record high °F (°C) | 69 (21) | 78 (26) | 85 (29) | 94 (34) | 104 (40) | 110 (43) | 120 (49) | 115 (46) | 105 (41) | 96 (36) | 80 (27) | 70 (21) | 120 (49) |
| Mean daily maximum °F (°C) | 47.2 (8.4) | 53.8 (12.1) | 63.0 (17.2) | 72.8 (22.7) | 83.8 (28.8) | 94.1 (34.5) | 98.8 (37.1) | 95.7 (35.4) | 87.7 (30.9) | 73.7 (23.2) | 58.3 (14.6) | 47.1 (8.4) | 73.0 (22.8) |
| Mean daily minimum °F (°C) | 26.9 (−2.8) | 31.8 (−0.1) | 37.8 (3.2) | 44.6 (7.0) | 54.9 (12.7) | 64.1 (17.8) | 71.3 (21.8) | 69.3 (20.7) | 60.7 (15.9) | 48.9 (9.4) | 36.9 (2.7) | 27.4 (−2.6) | 47.9 (8.8) |
| Record low °F (°C) | −2 (−19) | 4 (−16) | 21 (−6) | 16 (−9) | 29 (−2) | 40 (4) | 48 (9) | 51 (11) | 36 (2) | 24 (−4) | 15 (−9) | 3 (−16) | −2 (−19) |
| Averageprecipitation inches (mm) | 0.59 (15) | 0.56 (14) | 0.63 (16) | 0.37 (9.4) | 0.36 (9.1) | 0.17 (4.3) | 0.51 (13) | 0.75 (19) | 0.59 (15) | 0.85 (22) | 0.57 (14) | 0.41 (10) | 6.36 (160.8) |
| Average snowfall inches (cm) | 0.2 (0.51) | 0.2 (0.51) | 0 (0) | 0 (0) | 0 (0) | 0 (0) | 0 (0) | 0 (0) | 0 (0) | 0 (0) | 0 (0) | 0.3 (0.76) | 0.7 (1.78) |
| Source:http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?az9114 | |||||||||||||
Glen Canyon was carved bydifferential erosion from the Colorado River over an estimated 5 million years. TheColorado Plateau, through which the canyon cuts, arose some 11 million years ago. Within that plateau lie layers of rock from over 300 million years ago to the relatively recent volcanic activity.Pennsylvanian andPermian formations can be seen inCataract Canyon andSan Juan Canyon. TheMoenkopi Formation, which dates from 230 million years ago (Triassic Period), and theChinle Formation are found at Lees Ferry and the Rincon. Both formations are the result of the ancient inland sea that covered the area. Once the sea drained, windblown sand invaded the area, creating what is known asWingate Sandstone.
The more recent (Jurassic Period) formations includeKayenta Sandstone, which produces the trademark blue-black "desert varnish" that streaks down many walls of the canyons. Above this isNavajo Sandstone. Many of the arches, including Rainbow Bridge, lie at this transition point. This period also includes light yellowEntrada Sandstone, and the dark brown, almost purpleCarmel Formation. These latter two can be seen on the tops of mesas aroundWahweap, and the crown of Castle Rock andTower Butte. Above these layers lie thesandstone,conglomerate andshale of theStraight Cliffs Formation that underlies theKaiparowits Plateau andSan Rafael Swell to the north of the lake.
The confluences of theEscalante,Dirty Devil andSan Juan rivers with the Colorado lie within Lake Powell. The slower flow of the San Juan river has producedgoosenecks where 5 miles (8.0 km) of river are contained within 1-mile (1.6 km) on a straight line.
The lake's main body stretches up Glen Canyon, but has also filled many (over 90) side canyons. The lake also stretches up the Escalante River and San Juan River where they merge into the main Colorado River. This provides access to many natural geographic points of interest as well as some remnants of theAnasazi culture.
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Access to the lake is limited to developed marinas because most of the lake is surrounded by steep sandstone walls:
The following marinas are accessible only by boat:
Glen Canyon National Recreation Area draws more than two million visitors annually. Recreational activities includeboating,fishing,waterskiing,jet-skiing, and hiking. Prepared campgrounds can be found at each marina, but many visitors choose to rent ahouseboat or bring their own camping equipment, find a secluded spot somewhere in the canyons, and make their own camp (there are no restrictions on where visitors can stay).
The Castle Rock Cut is one of the most important navigational channels in the lake; it was blasted as early as the 1970s to allow boaters to bypass the winding canyons between the Glen Canyon Dam and reaches of Lake Powell further upstream – saving, on average, one hour of travel time. The cut has been deepened several times since then, to allow the use of the channel during droughts.[13] During the protracted 21st-century drought, however, the lake has dropped so quickly on several occasions that the cut dried up during the summer tourist season, most recently in 2013. Continued deepening of the Castle Rock cut has been criticized for its high cost, but boaters and the National Park Service argue that it improves safety, saves millions of dollars in fuel, and improves emergency response time.[14] In September 2021 the level of Lake Powell was 45 feet below the bottom of the Castle Rock cut.[15]
Currently,[when?] most marinas on the lake don't haveAutomatic Identification System monitoring stations that transmit boat positions to the AIS websites for the boating community. A substantial number of vessels on the lake do not have AIS transponders as there currently[when?] are no mandatory requirements for AIS usage for this body of water. Extra precautions must be taken with respect to boating safety, as thefractal nature of the lake's hydrologic surface area can allow vessels with limited charting equipment to become easily lost.
The burying of human (and pet) waste in Glen Canyon National Recreation Area is prohibited. Anyone who camps farther than a quarter of a mile from a marina must bring aportable toilet. Pet waste must also be packed out.
The southwestern end of Lake Powell in Arizona can be accessed viaU.S. Route 89 andState Route 98.State Route 95 andState Route 276 lead to the northeastern end of the lake in Utah.
Some of these fish species are on the US Endangered Species List. Currently most native species on the Colorado River Basin are subject to ongoing restoration efforts of some kind.
Bass
Carp, pike and others
 | This section needs to beupdated. Please help update this article to reflect recent events or newly available information.(February 2020) |
Zebra andquagga mussels first appeared in the United States in the 1980s.[16]
The mussels were initially brought to the United States through the ballast water of ships entering the Great Lakes. These aquatic invaders soon spread to many bodies of water in the Eastern United States and have even made their way to the western United States. In January 2008,[17][18] Zebra mussels have been detected in several reservoirs along the Colorado River system such as Lakes Mead, Mojave, and Havasu.
By the early 2000sArizona,California,Nebraska,Kansas,Colorado,Nevada andUtah have all confirmed the presence of larval zebra mussels in lakes and reservoirs.
Zebra and quagga mussels can be destructive to an ecosystem due to competition for resources with native species. The filtration of zooplankton by the mussels can negatively impact the feeding for some species of fish. Zebra and quagga mussels can attach to hard surfaces and build layers on underwater structures. The mussels are known to clog pipes including those in hydroelectric power systems, thus becoming a costly and time-consuming problem for water managers in the West.
Control policies have recently been introduced to alleviate the hydroelectric problems as well as ecological problems faced by Western infestation. Beginning in 1999 Lake Powell began to visually monitor for the mussels.
In 2001 hot water boat decontamination sites were established at Wahweap, Bullfrog, and Halls Crossing marinas. In January 2007, zebra mussels were detected in Lake Mead and new action plans were announced to prevent the spread of mussels to Lake Powell. In August 2007, preliminary testing was positive for zebra or quagga larvae in Lake Powell. These tests were deemed false positives, but adult quagga mussels were found in 2013.
In August 2010, Lake Powell was declared mussel free.[citation needed] Lake Powell introduced a mandatory boat inspection for each watercraft entering the reservoir beginning in June 2009. Effective June 29, 2009, every vessel entering Lake Powell must have a mussel certificate, although boat owners were allowed to self-certify. These measures were intended to help prevent vessels from transporting Zebra mussels into Lake Powell.
Despite these measures, quagga mussel DNA was detected in 2012 and live mussels were found at a number of sites including the Wahweap Marina in Spring and Summer 2013. In June 2013 the NPS was attempting a diver-based eradication program to find and remove mussels before the lake became infested.[citation needed]
TheWashington County Water Conservancy District has proposed building theLake Powell Pipeline, which would have the capacity to extract up to 83,756 acre-feet (103,312,000 m3) per year from Lake Powell for distribution to municipal drinking water systems in the county.[19]
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