Parleys Canyon
Description
Parleys Canyon begins where I-215 merges into I-80 in Salt Lake City and ends at Parleys Summit. The lower part of the canyon is relatively twisty and narrow and had to be dynamited to make way for I-80. Despite this, the interstate remains six or more lanes wide throughout the canyon; it is built over Parleys Creek in many places. Work is also underway to extend the Parleys Trail multi-use path through this segment to improve non-motorized access.
The canyon widens dramatically near Mountain Dell Dam and Utah State Route 65 (SR-65) splits from the freeway (which turns southeast temporarily) to provide access to Morgan County to the northeast. SR-65 also provides a connection to a local road leading over the ridge to Emigration Canyon in the same area where the Mormon trail crossed into that canyon. Little Dell Dam can be seen higher up on the side of Parleys Canyon in this area. As the freeway turns back toward the east, there is also an exit for the road leading up Lambs Canyon (a side canyon of Parleys Canyon).
The area around Parleys Summit is part of the Summit Park census-designated place (CDP). However, this area is more commonly referred to as Jeremy Ranch or Parleys Summit. A $5m wildlife overpass was completed in December 2018 to allow wildlife to cross I-80 safely. The overpass is 50 feet wide and 320 feet long; animals near that location by exit 140 are funneled onto the overpass with 3.5 miles of fencing. Here the canyon is wide enough to form large communities along the sides of the freeway along the gentle mountain slopes. On the other side of the summit the freeway continues into the Snyderville Basin, which is where the popular resort town of Park City is located. Also within the basin is the ski jump built for the 2002 Winter Olympic Games and the large shopping district at Kimball Junction.
Climate
Climate data for Parley's Summit, Utah, 2004–2020 normals: 7500ft (2286m) | |||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
Record high °F (°C) | 64 (18) |
58 (14) |
69 (21) |
74 (23) |
81 (27) |
87 (31) |
88 (31) |
88 (31) |
84 (29) |
77 (25) |
66 (19) |
57 (14) |
88 (31) |
Mean maximum °F (°C) | 48.9 (9.4) |
49.6 (9.8) |
57.7 (14.3) |
64.4 (18.0) |
72.6 (22.6) |
78.9 (26.1) |
84.8 (29.3) |
83.2 (28.4) |
78.2 (25.7) |
68.1 (20.1) |
57.9 (14.4) |
48.8 (9.3) |
85.3 (29.6) |
Mean daily maximum °F (°C) | 34.5 (1.4) |
36.0 (2.2) |
43.9 (6.6) |
48.8 (9.3) |
56.7 (13.7) |
67.0 (19.4) |
76.4 (24.7) |
75.4 (24.1) |
66.2 (19.0) |
52.3 (11.3) |
42.0 (5.6) |
32.5 (0.3) |
52.6 (11.5) |
Daily mean °F (°C) | 27.2 (−2.7) |
28.0 (−2.2) |
35.2 (1.8) |
39.7 (4.3) |
47.5 (8.6) |
56.8 (13.8) |
65.6 (18.7) |
64.6 (18.1) |
56.2 (13.4) |
43.9 (6.6) |
34.6 (1.4) |
25.6 (−3.6) |
43.7 (6.5) |
Mean daily minimum °F (°C) | 19.8 (−6.8) |
20.0 (−6.7) |
26.4 (−3.1) |
30.6 (−0.8) |
38.4 (3.6) |
46.6 (8.1) |
54.8 (12.7) |
53.8 (12.1) |
46.3 (7.9) |
35.6 (2.0) |
27.1 (−2.7) |
18.7 (−7.4) |
34.8 (1.6) |
Mean minimum °F (°C) | 1.4 (−17.0) |
3.4 (−15.9) |
13.6 (−10.2) |
18.2 (−7.7) |
27.4 (−2.6) |
33.2 (0.7) |
46.4 (8.0) |
44.2 (6.8) |
32.2 (0.1) |
20.0 (−6.7) |
8.8 (−12.9) |
1.1 (−17.2) |
−4.2 (−20.1) |
Record low °F (°C) | −9 (−23) |
−15 (−26) |
2 (−17) |
10 (−12) |
20 (−7) |
24 (−4) |
38 (3) |
35 (2) |
26 (−3) |
−2 (−19) |
−2 (−19) |
−12 (−24) |
−15 (−26) |
Average precipitation inches (mm) | 3.95 (100) |
3.48 (88) |
3.63 (92) |
4.00 (102) |
2.70 (69) |
1.37 (35) |
0.82 (21) |
1.16 (29) |
1.98 (50) |
2.83 (72) |
3.42 (87) |
3.85 (98) |
33.19 (843) |
Average snowfall inches (cm) | 34.00 (86.4) |
25.50 (64.8) |
20.90 (53.1) |
15.70 (39.9) |
3.10 (7.9) |
0.50 (1.3) |
0.00 (0.00) |
0.00 (0.00) |
0.90 (2.3) |
5.70 (14.5) |
15.50 (39.4) |
31.10 (79.0) |
152.9 (388.6) |
Source 1: XMACIS2 | |||||||||||||
Source 2: NOAA (Snyderville snowfall) |
History
The canyon receives its name from Parley P. Pratt who was assigned to explore the canyon, called Big Canyon at the time, and to build a toll road, called the Golden Pass Toll Road. Construction on the road started in 1848 and was completed in 1850. The road through Parleys Canyon became the primary route into the Salt Lake Valley, surpassing the original route through Emigration Canyon. The canyon was used by a narrow gauge branchline owned by the Denver & Rio Grande Western Railway from Salt Lake to Park City (the Salt Lake and Park City Railway). However, with its steep grades the line struggled to compete with the Union Pacific's line (via Coalville, connecting to the UP main at Echo). The line was eventually rebuilt to standard gauge by the Rio Grande Western who along with their successor the Denver & Rio Grande Western Railroad, operated trains up into the canyon until 1956. Some remnants of the Rio Grande line through Parleys Canyon, namely the cuts for the horseshoe curves, are in use by local roads and visible off the shoulder of the freeway. A lower portion of the same railroad line outside of Parley's Canyon, remains in use in the present day as the right of way for the UTA S-Line streetcar.
References
- ^ U.S. Geological Survey Geographic Names Information System: Parleys Canyon
- ^ Pierce, Scott (June 23, 2019). "New $5 million, animals-only overpass at Parleys Summit is saving wildlife (and drivers) already". The Salt Lake Tribune. Retrieved June 23, 2019.
- ^ "xmACIS2". National Oceanic and Atmospheric Administration. Retrieved November 15, 2023.
- ^ "Parley's Summit, Utah 1991-2020 Monthly Normals". Retrieved November 15, 2023.
- ^ "Snyderville, Utah 1991-2020 Monthly Normals". Retrieved November 15, 2023.
- ^ Arave, Lynn (5 Jan 2006). "Tidbits of history — Unusual highlights of Salt Lake County". Deseret Morning News. Salt Lake City: Deseret Digital Media. pp. S1–S2. Archived from the original on September 18, 2012. Retrieved 30 Jan 2017.
- ^ Strack, Don (12 Sep 2004). "The Golden Pass: Parleys Canyon, Utah". utahrails.net. Retrieved 30 Jan 2017.