Flagstaff Lake is located in Somerset County and Franklin County, Maine, in the United States. The North Branch Dead River and South Branch Dead River join in the lake, forming the Dead River.

Flagstaff Lake
Flagstaff Lake seen from Mount Bigelow
Location of Flagstaff Lake in Maine, USA.
Location of Flagstaff Lake in Maine, USA.
Flagstaff Lake
Location of Flagstaff Lake in Maine, USA.
Location of Flagstaff Lake in Maine, USA.
Flagstaff Lake
LocationNorthwest Somerset, Somerset County, and Eustis, Franklin County, Maine, US
Coordinates45°11′38.9″N 70°18′52.4″W / 45.194139°N 70.314556°W / 45.194139; -70.314556
Typeeutrophic, reservoir, Man Made Lake, Its a flooded village, once known as Flagstaff Village.
Primary inflowsNorth Branch Dead River; South Branch Dead River
Primary outflowsDead River
Catchment area516 sq mi (1,340 km2)
Basin countriesUnited States
Surface area20,300 acres (8,200 ha)
Average depth18 ft (5.5 m)
Max. depth48 ft (15 m)
Water volume261,365 acre⋅ft (322,389,000 m3)
Residence time6 months
Shore length1147.2 mi (236.9 km)
Surface elevation1,146 ft (349 m)
1 Shore length is not a well-defined measure.
Flagstaff Lake in September 2018

The lake's surface area is 20,300 acres (82 km2), and it has a storage capacity of about 275,482 acre-feet (339,802,000 m3). It is extremely shallow (more so during drought years). Its deepest point is 48 feet (15 m).[1] Landlocked salmon and brook trout can be caught. Some points on the lake are very marshy and have to be negotiated with a canoe or kayak; even then, wading may be necessary in the marshy areas to get through to the rest of the lake.

Bigelow Mountain Range overlooks from the lake's southern shore, which makes the lake popular for outdoor activities. The lake is mostly undeveloped with relatively few boats and is optimal for kayaking.

Flagstaff Lake and Bigelow Mountains viewed from Flagstaff Road, Eustis, Maine

Long Falls Dam

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Flagstaff Lake was a smaller natural lake when the Long Falls Dam impounded the Dead River in 1950,[2] enlarging the lake and turning it into a reservoir used for hydropower electricity production by regulating the flow of the Dead River into the Kennebec River.[3] At the time, the river drive was still a primary means of delivering timber to the pulp mills downstream. Improved highways and the trucking industry have replaced the river drive.

Construction was controversial dating back to 1923, pitting the president of Central Maine Power Company, Walter Wyman, against state legislator and future Maine governor Percival Proctor Baxter.[4] Flagstaff Lake occupies parts of the abandoned and now submerged townships of Flagstaff, Bigelow, Dead River and Carrying Place.[5]

The dam is 45 feet (14 m) high, 1,339 feet (408 m) long at its crest, and consists of a 450 feet (140 m) concrete spillway, a 125 foot (38 m) long concrete section containing five 20 feet (6.1 m) wide Tainter gates, a 70 foot (21 m) long concrete section containing two Broome gates, and a log sluice, and a 694 foot (212 m) long earthen dike.[6] The dam is owned and operated by Brookfield Renewable Energy, [7] but no electricity is generated here. The dam is operated to regulate and augment flows that are used by eight downstream mainstem Kennebec River hydropower projects, and to control flooding.[8] [citation needed]

Climate

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Climate data for Long Falls Dam, Maine 1991–2020 normals, extremes 1951-2020: 1160ft (354m)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °F (°C) 56
(13)
60
(16)
78
(26)
83
(28)
90
(32)
93
(34)
94
(34)
98
(37)
94
(34)
82
(28)
68
(20)
63
(17)
98
(37)
Mean maximum °F (°C) 45
(7)
44
(7)
54
(12)
69
(21)
81
(27)
86
(30)
87
(31)
86
(30)
83
(28)
73
(23)
60
(16)
48
(9)
90
(32)
Mean daily maximum °F (°C) 23.2
(−4.9)
26.2
(−3.2)
34.7
(1.5)
47.3
(8.5)
62.1
(16.7)
71.5
(21.9)
76.7
(24.8)
75.5
(24.2)
68.1
(20.1)
53.7
(12.1)
40.4
(4.7)
29.2
(−1.6)
50.7
(10.4)
Daily mean °F (°C) 13.7
(−10.2)
15.5
(−9.2)
24.4
(−4.2)
37.6
(3.1)
51.0
(10.6)
60.6
(15.9)
65.9
(18.8)
64.2
(17.9)
56.8
(13.8)
44.6
(7.0)
32.8
(0.4)
21.4
(−5.9)
40.7
(4.8)
Mean daily minimum °F (°C) 4.3
(−15.4)
4.9
(−15.1)
14.0
(−10.0)
27.8
(−2.3)
39.9
(4.4)
49.7
(9.8)
55.1
(12.8)
52.9
(11.6)
45.5
(7.5)
35.4
(1.9)
25.2
(−3.8)
13.6
(−10.2)
30.7
(−0.7)
Mean minimum °F (°C) −19
(−28)
−16
(−27)
−9
(−23)
14
(−10)
28
(−2)
37
(3)
44
(7)
41
(5)
31
(−1)
23
(−5)
9
(−13)
−7
(−22)
−21
(−29)
Record low °F (°C) −37
(−38)
−37
(−38)
−23
(−31)
−9
(−23)
20
(−7)
29
(−2)
34
(1)
30
(−1)
20
(−7)
14
(−10)
−9
(−23)
−26
(−32)
−37
(−38)
Average precipitation inches (mm) 2.79
(71)
2.43
(62)
3.04
(77)
3.79
(96)
3.61
(92)
4.45
(113)
3.96
(101)
3.57
(91)
3.23
(82)
4.61
(117)
3.80
(97)
3.76
(96)
43.04
(1,095)
Average snowfall inches (cm) 22.70
(57.7)
22.90
(58.2)
22.20
(56.4)
7.60
(19.3)
0.00
(0.00)
0.00
(0.00)
0.00
(0.00)
0.00
(0.00)
0.00
(0.00)
2.60
(6.6)
7.20
(18.3)
23.90
(60.7)
109.1
(277.2)
Source 1: NOAA[9]
Source 2: XMACIS (temp records & monthly max/mins)[10]

1959 Air Accident

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A 37th Squadron F-102 like the one in Flagstaff Lake.
 
The other aircraft destroyed by the collision was similar to this T-33A.

A mid-air collision occurred over the lake during a United States Air Force exercise on the evening of 3 November 1959. A Lockheed T-33 Shooting Star simulated an enemy aircraft approaching from the east while ground-controlled interception directed Convair F-102 Delta Daggers of the 37th Fighter-Interceptor Squadron from Burlington International Airport to intercept it. One of the F-102s pressed a simulated firing run too close as the interception occurred over the lake, and the F-102 delta wing cut the tail off the T-33. The T-33 crew ejected successfully, but the rear seat crewman died when he became tangled in his parachute and landed upside down near the front section of the T-33. The front half of the T-33 was discovered in 1959, and the back half was discovered a few years later. The F-102 aircraft was discovered in Flagstaff Lake in 1979, but the pilot was never found.[11]

References

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  1. ^ Maine Fishing Depth Maps: Lakes & Ponds by County. DeLorme. 2007. ISBN 978-0-89933-350-2.
  2. ^ Patrick, Ruth (1994). Rivers of the United States: The eastern and southeastern states; Volume 3 of Rivers of the United States. John Wiley and Sons. p. 74. ISBN 978-0-471-30346-6.
  3. ^ "The Northern: The Way I Remember" (PDF). John E. Mcleod. Archived from the original (PDF) on 2013-08-13. Retrieved 2012-12-19.
  4. ^ Lost Villages of Flagstaff Lake, bBy Alan L. Burnell, Kenny R. Wing, page 9
  5. ^ "Flagstaff, "Man Made Lake" - Maine Folklife Center - University of Maine".
  6. ^ "Federal Register, Volume 61 Issue 175 (Monday, September 9, 1996)".
  7. ^ "Conservation group accuses DEP of intentionally relinquishing oversight of Flagstaff Lake". 4 January 2012.
  8. ^ Maine's Multiple Use River: Kennebec River, Past and Present. Kennebec Water Power Co. Lewiston, Maine
  9. ^ "Long Falls Dam, Maine 1991-2020 Monthly Normals". Retrieved October 26, 2023.
  10. ^ "xmACIS". National Oceanic and Atmospheric Administration. Retrieved October 26, 2023.
  11. ^ "T-33A crash mystery". Pete Noddin. Archived from the original on 2007-12-11. Retrieved 2012-01-20.