Английская Википедия:Berthoud Pass
Шаблон:Short description Шаблон:Infobox mountain pass
Berthoud Pass (Шаблон:IPAc-en Шаблон:Respell; elevation Шаблон:Convert) is a high mountain pass in central Colorado, in the Front Range of the Rocky Mountains of the western United States.
The pass is located west of Denver, and provides a high route between upper Clear Creek Canyon to the upper valley of the Fraser River in Middle Park to the north. It traverses the continental divide at the Front Range, on the border between Clear Creek County and Grand County.
The pass is named for Edward L. Berthoud, the chief surveyor of the Colorado Central Railroad during the 1870s. Accompanied by Jim Bridger, Berthoud discovered the pass in July 1861 while surveying a possible route for the railroad. Berthoud concluded that the pass was suitable as a wagon road, but not as a railroad, and was then hired by the Central Overland California and Pikes Peak Express Company to survey a route over the pass to Salt Lake.[1]
The route of U.S. Highway 40 currently traverses the pass north of its junction with Interstate 70 in Clear Creek Canyon. It provides primary road access to Winter Park and a secondary route to Steamboat Springs from Denver and the Colorado Front Range. However, the pass is one of the most notoriously difficult passes in Colorado for motorists, based on its height as well as the steep grades on both sides (6.3%) and the large number of switchbacks on the southern side of the pass. At least 55 avalanche paths have been mapped on Berthoud Pass, some of them intersecting U.S. Highway 40 and some of those intersecting the roadway at multiple points on the pass.[2] In 2015, CDOT installed an automated propane-fueled avalanche mitigation system consisting of five units that create concussive blasts to mitigate snow slab buildup on avalanche path #5, Stanley.[3]
Geologic history
Berthoud Pass is found in a region of Middle Proterozoic granite that intruded through older schist and gneiss roughly 1.4 billion years ago.[4] It was carved out by a fault zone crossing the Continental Divide. The pass is capped by metasedimentary rock and surrounded by granite on both sides. [4]
The entire region was formed by continuing compression of the crust into the Routt and Berthoud plutonic suites. This compression led to the formation of volcanoes in New Mexico.[4]
Climate
Berthoud Pass has an extreme alpine subarctic climate (Köppen Dfc), bordering on an alpine climate (ETH), with short summers featuring comfortable days and cold nights, and long, extremely snowy winters. The average annual snowfall is Шаблон:Convert, and every month from November to May averages at least Шаблон:Convert of snow. In the year from July 1983 to June 1984 snowfall reached Шаблон:Convert, including Шаблон:Convert in December 1983. Actual snow depth can be expected to peak at over Шаблон:Convert and has exceeded Шаблон:Convert. Шаблон:Weather box
Wildlife
Berthoud Pass is known for the wide variety of wildflowers growing in the area.[5] It is also a known migratory route for a variety of animals,[6] including the Canada lynx.[7]
Human history
Berthoud Pass Ditch
In 1902, the 3.5 mile (5.6 km) Berthoud Pass Ditch began diverting water from the headwaters of the Fraser River over the continental divide into the basin of Clear Creek. Initially, this water was used for irrigation, but the cities of Northglenn and Golden purchased the ditch in the mid-1980s. The ditch has a capacity of 53.4 cubic feet per second (1.51 m3/s), [8]
The ditch was blocked in 1999 by the collapse of the tunnel under the parking lot at the summit of the pass, but it was repaired the next year.[9] In the decade since the repairs, the ditch has typically diverted on the order of 500 acre-feet (600,000 m3) per year.[10]
Berthoud Pass Ski Area
Once home to the now-defunct Berthoud Pass Ski Area, the pass is a destination for local backcountry skiers, snowboarders, and snowshoers due to its abundance of steep and challenging terrain and plentiful snow averaging 500 inches annually. The twisting road on both sides of the pass also makes "car shuttles" possible, eliminating the need for skiers and snowboarders to hike back to the top of the pass after each run.
The ski resort was closed in 2002 due to financial problems caused by lack of water and sewage at the top of the pass. In 2003 the lifts were taken down, while some people continued to ski using snowcats for lift transportation. In 2005 the Colorado DOT began using a fund to restore the area to its natural state. First on the list was the demolition of the historic lodge.
A new warming hut was opened at the top of the pass in May 2008, along with an expanded parking area, two scenic viewing areas and a new summit marker sign. The ski lodge and facilities had been in use since the early 1950s and the new warming hut includes modern features such as composting toilets, radiant floor heating and green construction.
Berthoud Ski resort is claimed by some to have been the first resort and lift in Colorado.Шаблон:Citation needed Some say it was the first resort to openly welcome snowboarders.Шаблон:Citation needed
The summit of Berthoud Pass is located at approximately Шаблон:Coord.[11]
References
External links
- Berthoud Pass, Colorado
- USGS TopoZone listing
- Friends of Berthoud Pass
- Berthoud Pass Ski Area's History
Шаблон:Colorado Шаблон:Authority control
- ↑ Шаблон:Cite book
- ↑ http://avalanchemapping.org/IMAGES/Bpastopoweb.pdf Шаблон:Bare URL PDF
- ↑ Шаблон:Cite web
- ↑ 4,0 4,1 4,2 Шаблон:Cite book
- ↑ Шаблон:Cite web
- ↑ Шаблон:Cite web
- ↑ Шаблон:Cite web
- ↑ John N. Winchester, A Historical View: Transmountain Development in Colorado Шаблон:Webarchive, 2000; retrieved July, 2015.
- ↑ PAW, “The Ditch” on Berthoud Pass, Clear Creek County Document Center, 2012, retrieved Aug. 2015.
- ↑ Appendix IX. Transbasin Diversions, HB 1278 Final Report: The South Platte River Alluvial Aquifer, Colorado State University, Dec. 31, 2013; retrieved Aug. 2015.
- ↑ Шаблон:Cite web
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