Lake Chelan

Last updated • 8 min readFrom Wikipedia, The Free Encyclopedia
Lake Chelan
Stehekin Chelan.JPG
Lake Chelan with Stehekin on the lower left
USA Washington relief location map.jpg
Red pog.svg
Lake Chelan
Location Chelan County, Washington,
United States
Coordinates 47°50′28″N120°02′47″W / 47.84111°N 120.04639°W / 47.84111; -120.04639
Type Glacially overdeepened lake
Primary inflows Stehekin River, Railroad Creek
Primary outflows Chelan River
Catchment area 924 sq mi (2,390 km2)
Basin  countriesUnited States
Max. length50.5 mi (81.3 km)
Surface area52.1 sq mi (135 km2)
Average depth474 ft (144 m)
Max. depth1,486 ft (453 m)
Water volume4.66 cu mi (19.4 km3)
Residence time 10.6 years
Shore length1109.2 mi (175.7 km)
Surface elevation1,100 ft (340 m)
Settlementssee Cities
References [1] [2]
1 Shore length is not a well-defined measure.

Lake Chelan ( /ʃəˈlæn/ shə-LAN) is a narrow, 50.5 mi (81.3 km) long lake in Chelan County, north-central Washington state, U.S. [1] It is an overdeepened lake and resembles a fjord, with an average width of 1.3 mi (2.1 km). Near its upper end, the lake surface lies more than 6,600 ft (2,000 m) below peaks less than 3 mi (4.8 km) away. [3] [4] Before 1927, Lake Chelan was the largest natural lake in the state in terms of both surface area and water volume. [2] [5] Upon the completion of Lake Chelan Dam in 1927, the elevation of the lake was increased by 21 ft (6.4 m) to its present maximum-capacity elevation of 1,100 ft (340 m). [2]

Contents

With a maximum depth of 1,486 ft (453 m), Lake Chelan is the third deepest lake in the United States behind Crater Lake, the deepest, and Lake Tahoe, the second deepest. Because of overdeepening, the sides of this lake drop steeply to its bottom. The deepest part of Lake Chelan lies as much as 436 ft (133 m) below sea level. In places, the bedrock floor of the valley occupied by Lake Chelan, which is buried by Pleistocene glacial and lacustrine sediments, lies at least 1,529 ft (466 m) below sea level. Two communities lie on the southern end of the lake, and a third sits at the far north end, providing a gateway to North Cascades National Park. [3] [4]

Hydrology

On an annual basis, an average of 2,200 cubic feet per second (62 m3/s) flow into the lake. [6] Approximately 75% of the water that flows into the lake comes from two tributaries. [7] The Stehekin River alone contributes 65% of all water to Lake Chelan, averaging 1,401 cu ft/s (39.7 m3/s) annually. [8] The other major tributary, Railroad Creek, averages 202 cu ft/s (5.7 m3/s) annually. [6] The remaining water is added via a number of smaller tributaries as well as direct rain and snowfall.

With a maximum depth of 1,486 feet (453 m), [6] Lake Chelan is the third deepest lake in the United States, and the 25th deepest in the world. At its deepest, the lake bottom is 388 feet (118 m) below sea level. [9] The total watershed of the lake is 924 square miles (2,390 km2) [7] [10] [11] More than 90% of the watershed is forested land. The remainder of the basin is composed of the lake itself (5.6%) and agriculture (3.5%). [12]

Geology

The fjord-like topography of the Lake Chelan valley results from repeated glacial erosion and deposition (maybe nine or ten times) during the Pleistocene Period. [4] [13] The last episode of glacial erosion and deposition in the basin occurred during the Last Glacial Maximum about 21,000 years ago. At that time, in the upper Similkameen River valley of British Columbia, the Skagit Lobe split from the Okanogan Lobe of the Cordilleran ice sheet and advanced south into the Skagit River drainage. [14] Skagit ice passed through Fisher and Rainy passes, and down Bridge Creek into the Lake Chelan valley. The glacial lobe flowed down the Lake Chelan valley until meeting glacial ice of the main Okanogan Lobe advancing up the valley from the Columbia River drainage near Manson. The deposits of the northwestward advancing Okanagan lobe are characterized by large, basalt glacial erratics. [4] As the Skagit Lobe during the Last Glacial Maximum and glacial lobes during older glaciations flowed to the southeast down the Lake Chelan valley, they excavated the deep glacial trough that is now occupied by Lake Chelan. [14] The depth of the Lucerne Basin and the elevation of glacial till and moraines and glacier-scoured bedrock on the walls of the overdeepened Lake Chelan valley indicates that the thickness of the Skagit Lobe was over 1 mi (1.6 km). [3] [4]

Basins

Lake Chelan is composed of two basins. The lower basin, Wapato, is shallower and approximately a fourth the total length of the lake. The upper basin, Lucerne, is much deeper and extends for the remainder of the length of the lake. The two basins are separated by a sill rising to within 122 ft (37 m) of the surface, at a point known as the narrows, at which the lake is only 0.35 miles (0.56 km) wide. [9]

The lower basin, Wapato, reaches a maximum depth of only 400 feet (120 m). About 600 feet (180 m) of glacial sediment and rockslide deposits rest on top of the bedrock. [15] This section of the lake is 12 miles (19 km) long, and has an average depth of 190 feet (58 m). [16] Due to the relatively modest size of this basin, water resides in this basin for only 0.8 years, compared to 10 for Lucerne Basin. [17] The upper Lucerne basin is 38 miles (61 km) long with an average depth of 1,148 feet (350 m) and thus by far the larger of the two basins. [16] It is in this part of the lake that the maximum depth of 1,486 feet (453 m) is found. Lucerne basin contains 92% of the water in Lake Chelan and 74% of the surface area, leaving Wapato with only 8% of the total volume of water and 26% of the surface area. [8] [9] [15] The upper basin of Lake Chelan is surrounded by more mountainous terrain, resulting in few beaches along the shoreline. Approximately 50 miles (80 km) of the shoreline of this basin are in National Forest lands, and 12 miles (19 km) in National Park lands. [8]

Natural history

Climate

The climate of Lake Chelan's watershed is varied. From the southern end of the lake in the rain shadow of the Cascade Range, to the northern tip of the lake located in the eastern Cascades, the climate of Lake Chelan's watershed is as diverse as the lake is long. The south end's weather is notably dry, with Chelan averaging only 11.4 inches (29 cm) of rain per year, along with 21.8 inches (55 cm) of snow. Stehekin receives an average of 35.5 inches (90 cm) of rain per year, and 122.5 inches (311 cm) of snow. Other than precipitation trends, the climates are remarkably similar. Both locations average around 60 °F (16 °C) for a high, and 40 °F (4 °C) for a low throughout the course of the year.[ citation needed ]

Climate data for Chelan, Washington (south end of lake) (1991–2020 normals, extremes since 1891)
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record high °F (°C)62
(17)
63
(17)
74
(23)
88
(31)
98
(37)
111
(44)
109
(43)
106
(41)
97
(36)
88
(31)
72
(22)
65
(18)
111
(44)
Mean maximum °F (°C)48
(9)
52
(11)
63
(17)
75
(24)
86
(30)
90
(32)
99
(37)
99
(37)
89
(32)
75
(24)
58
(14)
48
(9)
100
(38)
Mean daily maximum °F (°C)34.3
(1.3)
41.7
(5.4)
51.9
(11.1)
62.1
(16.7)
71.9
(22.2)
77.9
(25.5)
86.6
(30.3)
87.0
(30.6)
77.2
(25.1)
62.2
(16.8)
45.7
(7.6)
34.9
(1.6)
61.1
(16.2)
Daily mean °F (°C)28.0
(−2.2)
33.0
(0.6)
41.1
(5.1)
49.8
(9.9)
59.0
(15.0)
65.4
(18.6)
72.8
(22.7)
72.5
(22.5)
63.2
(17.3)
50.5
(10.3)
37.6
(3.1)
28.7
(−1.8)
50.1
(10.1)
Mean daily minimum °F (°C)21.6
(−5.8)
24.3
(−4.3)
30.3
(−0.9)
37.5
(3.1)
46.2
(7.9)
53.0
(11.7)
59.1
(15.1)
58.1
(14.5)
49.2
(9.6)
38.8
(3.8)
29.5
(−1.4)
22.6
(−5.2)
39.2
(4.0)
Mean minimum °F (°C)11
(−12)
16
(−9)
24
(−4)
32
(0)
39
(4)
47
(8)
52
(11)
52
(11)
42
(6)
30
(−1)
21
(−6)
14
(−10)
7
(−14)
Record low °F (°C)−18
(−28)
−15
(−26)
4
(−16)
21
(−6)
28
(−2)
33
(1)
35
(2)
42
(6)
26
(−3)
3
(−16)
−3
(−19)
−18
(−28)
−18
(−28)
Average precipitation inches (mm)1.52
(39)
1.22
(31)
1.09
(28)
0.75
(19)
1.05
(27)
0.87
(22)
0.42
(11)
0.32
(8.1)
0.34
(8.6)
1.04
(26)
1.51
(38)
1.83
(46)
11.96
(303.7)
Average snowfall inches (cm)7.7
(20)
2.0
(5.1)
0.7
(1.8)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
1.4
(3.6)
8.7
(22)
20.5
(52.5)
Average extreme snow depth inches (cm)3
(7.6)
2
(5.1)
1
(2.5)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
1
(2.5)
2
(5.1)
4
(10)
Average precipitation days (≥ 0.01 inch)107756532269971
Source: National Oceanic and Atmospheric Administration [18]
Climate data for Stehekin, Washington (north end of the lake) (1991–2020 normals, extremes since 1906)
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record high °F (°C)55
(13)
59
(15)
70
(21)
85
(29)
101
(38)
103
(39)
107
(42)
105
(41)
98
(37)
88
(31)
67
(19)
62
(17)
107
(42)
Mean maximum °F (°C)42
(6)
48
(9)
59
(15)
74
(23)
86
(30)
92
(33)
99
(37)
98
(37)
89
(32)
72
(22)
52
(11)
42
(6)
100
(38)
Mean daily maximum °F (°C)32.3
(0.2)
37.8
(3.2)
46.5
(8.1)
57.5
(14.2)
68.6
(20.3)
74.4
(23.6)
84.3
(29.1)
83.3
(28.5)
72.5
(22.5)
55.8
(13.2)
40.0
(4.4)
32.3
(0.2)
57.1
(13.9)
Daily mean °F (°C)28.5
(−1.9)
31.9
(−0.1)
38.1
(3.4)
46.6
(8.1)
56.2
(13.4)
62.2
(16.8)
70.1
(21.2)
69.3
(20.7)
60.2
(15.7)
46.8
(8.2)
35.2
(1.8)
29.0
(−1.7)
47.8
(8.8)
Mean daily minimum °F (°C)24.8
(−4.0)
26.0
(−3.3)
29.8
(−1.2)
35.8
(2.1)
43.8
(6.6)
49.9
(9.9)
55.9
(13.3)
55.2
(12.9)
47.8
(8.8)
37.8
(3.2)
30.4
(−0.9)
25.6
(−3.6)
38.6
(3.7)
Mean minimum °F (°C)12
(−11)
15
(−9)
22
(−6)
28
(−2)
34
(1)
41
(5)
47
(8)
46
(8)
38
(3)
27
(−3)
21
(−6)
12
(−11)
8
(−13)
Record low °F (°C)−18
(−28)
−16
(−27)
−5
(−21)
19
(−7)
25
(−4)
28
(−2)
36
(2)
30
(−1)
22
(−6)
16
(−9)
0
(−18)
−11
(−24)
−18
(−28)
Average precipitation inches (mm)6.75
(171)
3.72
(94)
3.60
(91)
1.44
(37)
1.07
(27)
0.75
(19)
0.46
(12)
0.49
(12)
1.05
(27)
3.66
(93)
6.73
(171)
7.16
(182)
36.88
(936)
Average snowfall inches (cm)41.4
(105)
18.5
(47)
9.1
(23)
0.2
(0.51)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.2
(0.51)
9.7
(25)
50.6
(129)
129.7
(330.02)
Average extreme snow depth inches (cm)36
(91)
33
(84)
24
(61)
6
(15)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
6
(15)
27
(69)
41
(100)
Average precipitation days (≥ 0.01 in)171111866336111616114
Average snowy days (≥ 0.01 in)1153000000031133
Source: NOAA [19]

History

Etymology

The name Chelan is a Salish Indigenous word, "Tsi - Laan," meaning 'Deep Water'. [20]

Cities

Due to the isolated nature of Lake Chelan, especially at its northern reaches, there is not a large population that resides along the shore. Chelan, which had 4,222 residents at the 2020 census, [21] is currently the only incorporated city situated along the lake shore. The city is located at the southern terminus of the lake, adjacent to the Lake Chelan Dam and the Chelan River outflow. The census-designated place of Manson, which had 1,523 residents in 2020, [22] is also located at the southern end of the lake. The unincorporated community of Stehekin, [23] with approximately 75 residents, [24] is located at the northern terminus of the lake, adjacent to the Stehekin River inflow. At the mouth of the Railroad Creek sits Lucerne, a small community of private cabins served by commercial boats. [23] Lucerne is also the primary gateway to the community of Holden Village, a Lutheran retreat center located 11 mi (18 km) inland from the lake. With approximately 50 long-term residents, Holden includes one of the few remaining public K-12 two-room schools in the contiguous United States. [25]

Economy

Fishing

Fishing is a popular recreating activity on Lake Chelan. The following fish are or were native to the lake: Bull Trout, Westslope cutthroat trout, Largescale sucker, Longnose sucker, Bridgelip sucker, Northern pikeminnow, Peamouth, Redside shiner, Mountain whitefish, Pygmy whitefish. [26] [27]

In addition to these native species, six species have been introduced to the lake, primarily for sport fishing purposes: Yellowstone cutthroat trout, Rainbow trout, Kokanee, Brook trout, Chinook salmon, Lake trout [26] [27]

State records

In 2013, a 35.63 lb (16.16 kg) Lake Trout was caught, setting the state record. [28]

Winemaking

The Lake Chelan AVA surrounds the southernmost 12 miles of Lake Chelan. [29] A subzone of the larger Columbia Valley AVA, the Lake Chelan AVA is home to 31 tasting rooms. [30]

Protected lands

At the north end of the lake, surrounding the town of Stehekin, is Lake Chelan National Recreation Area (NRA). Bordering the Lake Chelan NRA is the Lake Chelan-Sawtooth Wilderness. The Wenatchee National Forest surrounds much of the lake on either side. Two state parks are located on the southern edge, not far from the city of Chelan. These state parks are Twenty-Five Mile Creek State Park and Lake Chelan State Park. [31]

In addition to the protected land located directly on the shores of Lake Chelan, Stehekin serves not only as a gateway to the Lake Chelan NRA, but also to the rest of the North Cascades National Park Complex, Stephen Mather Wilderness, and adjacent National Forest Wilderness Areas. [32] Approximately 87% of the Lake Chelan watershed is owned by either federal, state, or local entities, with the rest in private ownership. [12]

See also

Related Research Articles

<span class="mw-page-title-main">Puget Sound</span> Sound in Washington, United States

Puget Sound is a complex estuarine system of interconnected marine waterways and basins located on the northwest coast of the U.S. state of Washington. As a part of the Salish Sea, the sound has one major and two minor connections to the Strait of Juan de Fuca, which in turn connects to the open Pacific Ocean. The major connection is Admiralty Inlet; the minor connections are Deception Pass and the Swinomish Channel.

<span class="mw-page-title-main">North Cascades National Park</span> National Park in Washington, United States

North Cascades National Park is a national park of the United States in Washington. At more than 500,000 acres (200,000 ha), it is the largest of the three National Park Service units that comprise the North Cascades National Park Complex. North Cascades National Park consists of a northern and southern section, bisected by the Skagit River that flows through the reservoirs of Ross Lake National Recreation Area. Lake Chelan National Recreation Area lies on the southern border of the south unit of the park. In addition to the two national recreation areas, other protected lands including several national forests and wilderness areas, as well as Canadian provincial parks in British Columbia, nearly surround the park. North Cascades National Park features the rugged mountain peaks of the North Cascades Range, the most expansive glacial system in the contiguous United States, the headwaters of numerous waterways, and vast forests with the highest degree of flora biodiversity of any American national park.

<span class="mw-page-title-main">Chelan County, Washington</span> County in Washington, United States

Chelan County is a county in the U.S. state of Washington. As of the 2020 census, its population was 79,074. The county seat and largest city is Wenatchee. The county was created out of Okanogan and Kittitas Counties on March 13, 1899. It derives its name from a Chelan Indian word meaning "deep water," likely a reference to 55-mile (89 km)-long Lake Chelan, which reaches a maximum depth of 1,486 feet (453 m).

<span class="mw-page-title-main">Glacial Lake Missoula</span> Prehistoric proglacial lake in Western Montana

Lake Missoula was a prehistoric proglacial lake in western Montana that existed periodically at the end of the last ice age between 15,000 and 13,000 years ago. The lake measured about 7,770 square kilometres (3,000 sq mi) and contained about 2,100 cubic kilometres (500 cu mi) of water, half the volume of Lake Michigan.

<span class="mw-page-title-main">Lake Passaic</span> Former proglacial lake in New Jersey, U.S.

Lake Passaic was a prehistoric proglacial lake that existed in northern New Jersey in the United States at the end of the last ice age approximately 19,000–14,000 years ago. The lake was formed of waters released by the retreating Wisconsin Glacier, which had pushed large quantities of earth and rock ahead of its advance, blocking the previous natural drainage of the ancestral Passaic River through a gap in the central Watchung Mountains. The lake persisted for several thousand years as melting ice and eroding moraine dams slowly drained the former lake basin. The effect of the lake's creation permanently altered the course of the Passaic River, forcing it to take a circuitous route through the northern Watchung Mountains before spilling out into the lower piedmont.

<span class="mw-page-title-main">Skagit River</span> River in Canada and the United States

The Skagit River is a river in southwestern British Columbia in Canada and northwestern Washington in the United States, approximately 150 mi (240 km) long. The river and its tributaries drain an area of 1.7 million acres (690,000 hectares) of the Cascade Range along the northern end of Puget Sound and flows into the sound.

<span class="mw-page-title-main">Stehekin, Washington</span> Unincorporated community in Washington, United States

Stehekin is a small unincorporated community in Chelan County, Washington. The name "Stehekin" comes from a word in the Salishan language that means "the way through". Stehekin has somewhat more than 100 permanent residents, but vacationers and seasonal workers increase its population during the summer.

<span class="mw-page-title-main">Cascade Pass</span> Mountain pass in Washington

Cascade Pass is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.

<span class="mw-page-title-main">Lake Whatcom</span>

Lake Whatcom is located in Whatcom County, Washington, United States. It is the drinking water source for approximately 85,000 residents in the city of Bellingham as well as Whatcom County. It is approximately 10 miles (16 km) in length and 1 mile (1.6 km) in width at its widest. Lake Whatcom is located and managed within three political jurisdictions: the city of Bellingham, Whatcom County, and the Lake Whatcom Water and Sewer District. The lake is a popular area for motor boating, swimming, fishing, and other recreational activities.

<span class="mw-page-title-main">Stehekin River</span> River in Washington, United States

The Stehekin River is a river located in Washington state in the Pacific Northwest of the United States. It is the main river flowing into Lake Chelan. Miners arrived in Stehekin River Valley in the late 19th century. They were followed by homesteaders in the early 20th century. Today, the Stehekin River Valley is still a remote area that can only be reached by way of a 55-mile boat ride up Lake Chelan.

<span class="mw-page-title-main">Lake Chelan National Recreation Area</span> National recreation area in Chelan County

Lake Chelan National Recreation Area is a national recreation area located about 35 miles (56 km) south of the Canada–US border in Chelan County, Washington. It encompasses an area of 61,958 acres (25,074 ha) including the northern end of Lake Chelan and the surrounding area of the Stehekin Valley and the Stehekin River. The area is managed by the U.S. National Park Service as part of the North Cascades National Park Service Complex.

<span class="mw-page-title-main">Lake Crescent</span> Lake located in Olympic National Park, Washington, United States

Lake Crescent is a deep lake located entirely within Olympic National Park in Clallam County, Washington, United States, approximately 17 miles (27 km) west of Port Angeles on U.S. Route 101, near the small community of Piedmont. With an official maximum depth of 624 feet (190 m), it is officially the second deepest lake in the state of Washington. A lake-wide bathymetric survey was performed from 2013 to 2014 by Eian Ray and Jeff Engea and the results of this survey show the maximum depth as being 596 feet (182 m). Using GIS statistical analysis, this survey also estimated that the lake contains around 0.5 cubic miles (2.1 km3) of fresh water.

<span class="mw-page-title-main">Baker River (Washington)</span> River in Washington, United States

The Baker River is an approximately 30-mile (48 km), southward-flowing tributary of the Skagit River in northwestern Washington in the United States. It drains an area of the high North Cascades in the watershed of Puget Sound north of Seattle, and east of Mount Baker. With a watershed of approximately 270 square miles (700 km2) in a complex of deep valleys partially inside North Cascades National Park, it is the last major tributary of the Skagit before the larger river reaches its mouth on Skagit Bay. The river flows through Concrete, Washington, near its mouth and has two hydroelectric dams owned by Puget Sound Energy.

<span class="mw-page-title-main">Green Lake (Wisconsin)</span> Lake in Green Lake County, Wisconsin, USA

Green Lake — also known as Big Green Lake — is a lake in Green Lake County, Wisconsin, United States. Green Lake has a maximum depth of 237 ft (72 m), making it the deepest natural inland lake in Wisconsin and the second largest by volume. The lake covers 29.72 km2 and has an average depth of 30.48 m (100.0 ft). Green Lake has 43.94 km (27.30 mi) of diverse shoreline, ranging from sandstone bluffs to marshes.

<span class="mw-page-title-main">Lake Willoughby</span> Glacial lake (ice age) in Vermont, U.S.

Lake Willoughby is located in the town of Westmore in Orleans County in the Northeast Kingdom of Vermont, United States.

The Chelan are an Interior Salish people speaking the Wenatchi dialect, though separate from that tribe. The name derives from the traditional Wenatchi name Tsi-Laan meaning "deep water".

<span class="mw-page-title-main">Lake Sunapee</span> Lake in New Hampshire, United States

Lake Sunapee is located within Sullivan County and Merrimack County in western New Hampshire, the United States. It is the fifth-largest lake located entirely in New Hampshire.

<span class="mw-page-title-main">Suiattle River</span> River in Washington, United States

The Suiattle River is a river in the northern Cascade Mountains of western Washington, United States. It is a tributary of the Sauk River and by extension the Skagit River. Its source is located between Suiattle Glacier and Honeycomb Glacier on Glacier Peak, at an elevation of around 7,000 ft (2,100 m) above sea level. It descends through a 60-mile (97 km) course, lying mainly within the Mount Baker–Snoqualmie National Forest. It meets the Sauk northeast of Darrington, Washington, at an elevation of 400 ft (120 m). Snowmelt from Chocolate and Dusty Glacier gives the river silty water, with a suspended load over twice that of the upper Sauk or adjacent White Chuck.

<span class="mw-page-title-main">Buckner Mountain</span> Mountain in Washington (state), United States

Buckner Mountain is a tall peak in the North Cascades of Washington state and in the Stephen Mather Wilderness of North Cascades National Park. At 9,114 feet (2,778 m) in elevation it is the highest in Skagit County and one of about ten of Washington's non-volcanic peaks above 9,000 feet high. It is ranked as the 14th highest peak in the state, and the third highest peak in North Cascades National Park.

References

  1. 1 2 "TMDL Case Study: Lake Chelan, Washington". Environmental Protection Agency. January 1994. Retrieved 2015-01-17.
  2. 1 2 3 Kendra, Will; Singleton, Lynn (January 1987). "Morphometry of Lake Chelan" (PDF). Washington State Department of Ecology. Retrieved 2023-02-03.
  3. 1 2 3 Whetten, J.T. (1967). "Lake Chelan Washington: bottom and sub-bottom topography". Limnology and Oceanography. 12 (2): 253–259. doi: 10.4319/lo.1967.12.2.0253 .
  4. 1 2 3 4 5 Lillquis, Karl (2016). Moses Coulee to Chelan Field Trip, 12 June 2016. Ellensburg, Washington: Ellensburg Chapter, Ice Age Floods Institute. p. 39.
  5. Bortleson, G.C.; Dion, N.P.; McConnell, J.B.; Nelson, L.M. (1976). "Reconnaissance data on lakes in Washington -- Vol. 5, Chelan, Ferry, Kittitas, Klickitat, Okanogan, and Yakima Counties". Washington State Department of Ecology. Retrieved 2023-02-03.
  6. 1 2 3 "Chelan Watershed Initial Assessment" (PDF). Washington Department of Ecology. May 1985. Retrieved 2015-01-13.
  7. 1 2 Hillman, T.W.; Giorgi, A.E. (February 2000). "Historical Occurrences of Anadromous Salmonids in Lake Chelan, Washington" (PDF). Chelan Public Utilities District. BioAnalysts, Inc. Retrieved 2015-01-17.
  8. 1 2 3 Coots, Randy (June 2006). "Lake Chelan Watershed DDT and PCB Total Maximum Daily Load: Water Quality Improvement Report" (PDF). Washington State Department of Ecology. Retrieved 2015-01-19.
  9. 1 2 3 "Lake Chelan Wapato Basin Total Phosphorus Total Maximum Daily Load" (PDF). State of Washington Department of Ecology. November 2011. Retrieved 2015-01-18.
  10. "Chelan Watershed Initial Assessment" (PDF). Washington Department of Ecology. May 1985. Retrieved 2015-01-13.
  11. "Water Quality Improvement Project: Lake Chelan Area: Multi-Parameter". Department of Ecology - State of Washington. March 2013. Retrieved 2015-01-17.
  12. 1 2 "Draft In-Leau Fee Program Prospectus and Compensation Planning Framework for Lower Lake Chelan" (PDF). The Watershed Company. June 2010. Archived from the original (PDF) on 2015-09-09. Retrieved 2015-01-19.
  13. Freeman, O.W. (1944). "Glaciation and some human relationships at Lake Chelan". Northwest Science. 18 (3): 59–62.
  14. 1 2 Riedel, J.L. (2017). "Deglaciation of the North Cascade Range, Washington and British Columbia, from the last glacial maximum to the Holocene". Cuadernos de investigación geográfica/Geographical Research Letters. 43: 59–62.
  15. 1 2 "Discover Lake Chelan" (PDF). National Park Service. Retrieved 2015-01-14.
  16. 1 2 Chamberlain, William; Singleton, Lynn; Jay, Joe (1985-02-20). "Lake Chelan Project Proposal" (PDF). Washington State Department of Ecology. Retrieved 2015-01-19.
  17. Pelletier, Greg; Owes, Harper (January 1989). "Lake Chelan Water Quality Assessment" (PDF). Washington State Department of Ecology. Retrieved 2015-01-19.
  18. "NowData – NOAA Online Weather Data". National Oceanic and Atmospheric Administration . Retrieved August 7, 2022.
  19. "NowData – NOAA Online Weather Data". National Oceanic and Atmospheric Administration . Retrieved August 7, 2022.
  20. "Native American Legends" (PDF). USDA Forest Service - Pacific Northwest Region. Archived from the original (PDF) on April 11, 2006. Retrieved 2007-06-26.
  21. "Explore Census Data". data.census.gov. Retrieved 2022-03-23.
  22. "2020 United States Census Profile: Manson CDP, Washington". U.S. Census Bureau, American Factfinder. Retrieved March 15, 2023.
  23. 1 2 "Shoreline Inventory" (PDF). Chelan County. 2012-04-23. Retrieved 2015-01-19.
  24. Visit Stehekin. "Visit Stehekin, Washington". Archived from the original on 2015-01-01. Retrieved 2015-01-13.
  25. "Holden School". Holden Village. Archived from the original on 2015-05-01. Retrieved 2022-03-17.
  26. 1 2 Nelson, Mark C. (2012-01-20). "What Happened to Bull Trout in Lake Chelan? An Examination of the Historical Evidence" (PDF). U.S. Fish and Wildlife Service. Archived from the original (PDF) on 2015-09-24. Retrieved 2015-01-17.
  27. 1 2 Hillman, T.W.; Giorgi, A.E. (February 2000). "Historical Occurrences of Anadromous Salmonids in Lake Chelan, Washington" (PDF). Chelan Public Utilities District. BioAnalysts, Inc. Retrieved 2015-01-17.
  28. "Freshwater and Saltwater Records". Washington Department of Fish & Wildlife. Archived from the original on 2015-01-18. Retrieved 2015-01-17.
  29. "Federal Register :: Request Access". unblock.federalregister.gov. Retrieved 2023-06-21.
  30. "Facts and Figures – Lake Chelan Wine Valley". 2020-04-27. Archived from the original on 2020-04-27. Retrieved 2023-06-21.
  31. "Lake Chelan Area State Parks Management Plan". Washington State Parks and Recreation Committee. January 2009. Archived from the original on 2015-01-18. Retrieved 2015-01-17.
  32. "Stehekin". National Park Service. Retrieved 2015-01-17.