Longworth Peak

Last updated
Longworth Peak
Longworth Peak.jpg
Highest point
Elevation 2,091 m (6,860 ft)
Prominence 1,265 m (4,150 ft)
Parent peak Mount Sir Alexander
Isolation 27.65 km (17.18 mi)
to  Kisano Mountain
Coordinates 53°55′57″N121°21′52″W / 53.93250°N 121.36444°W / 53.93250; -121.36444
Geography
Canada British Columbia relief location map.jpg
Red triangle with thick white border.svg
Longworth Peak
Canada relief map 2.svg
Red triangle with thick white border.svg
Longworth Peak
Longworth Peak (Canada)
DistrictCariboo Land District
Parent range McGregor Plateau
Topo map NTS 93H14 Penny

Longworth Peak, is a 2,094-metre (6,870-feet) mountain in the McGregor Range of the McGregor Plateau in Northern British Columbia. [1] It is the highest peak in the McGregor Range.

Located between the Fraser River and the Torpy River, the peak is rocky with no glaciers.

The peak rises above the unincorporated hamlet of Longworth, BC and is a popular hiking destination. There is an abandoned fire lookout near the summit.

The BC Ministry of Environment operates an automated snow weather station on the south west side of the mountain at an elevation of 1,740m [2] which was installed in 2016.

Related Research Articles

<span class="mw-page-title-main">Geography of Lebanon</span> Geographical features of Lebanon

Lebanon is a small country in West Asia, located at approximately 34˚N, 35˚E. It stretches along the eastern shore of the Mediterranean Sea and its length is almost three times its width. From north to south, the width of its terrain becomes narrower. Lebanon's mountainous terrain, proximity to the sea, and strategic location at a crossroads of the world were decisive factors in shaping its history.

<span class="mw-page-title-main">Mount Waddington</span> Mountain in British Columbia, Canada

Mount Waddington, once known as Mystery Mountain, is the highest peak in the Coast Mountains of British Columbia, Canada. Although it is lower than Mount Fairweather and Mount Quincy Adams, which straddle the United States border between Alaska and British Columbia, Mount Waddington is the highest peak that lies entirely within British Columbia. It and the subrange which surround it, known as the Waddington Range, stand at the heart of the Pacific Ranges, a remote and extremely rugged set of mountains and river valleys.

<span class="mw-page-title-main">The Remarkables</span> Mountain range in New Zealand

The Remarkables are a mountain range and skifield in Otago in the South Island of New Zealand. Located on the southeastern shore of Lake Wakatipu, the range lives up to its name by rising sharply to create a remarkable backdrop for the waters. The range is clearly visible from the nearby town of Queenstown.

<span class="mw-page-title-main">Canadian Rockies</span> Mountain range in Canada

The Canadian Rockies or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico.

<span class="mw-page-title-main">Mount Garibaldi</span> Stratovolcano in British Columbia, Canada

Mount Garibaldi is a dormant stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has a maximum elevation of 2,678 metres and rises above the surrounding landscape on the east side of the Cheakamus River in New Westminster Land District. In addition to the main peak, Mount Garibaldi has two named sub-peaks. Atwell Peak is a sharp, conical peak slightly higher than the more rounded peak of Dalton Dome. Both were volcanically active at different times throughout Mount Garibaldi's eruptive history. The northern and eastern flanks of Mount Garibaldi are obscured by the Garibaldi Névé, a large snowfield containing several radiating glaciers. Flowing from the steep western face of Mount Garibaldi is the Cheekye River, a tributary of the Cheakamus River. Opal Cone on the southeastern flank is a small volcanic cone from which a lengthy lava flow descends. The western face is a landslide feature that formed in a series of collapses between 12,800 and 11,500 years ago. These collapses resulted in the formation of a large debris flow deposit that fans out into the Squamish Valley.

<span class="mw-page-title-main">Tararua Range</span> Mountain range in the North Island of New Zealand

The Tararua Range, often referred to as the Tararua Ranges or Tararua, is one of several mountain ranges in the North Island of New Zealand.

<span class="mw-page-title-main">Glacier National Park (Canada)</span> Canadian national park located in British Columbia

Glacier National Park is part of a system of 43 parks and park reserves across Canada, and one of seven national parks in British Columbia. Established in 1886, the park encompasses 1,349 km2 (521 sq mi), and includes a portion of the Selkirk Mountains which are part of the larger grouping of mountains, the Columbia Mountains. It also contains the Rogers Pass National Historic Site.

<span class="mw-page-title-main">Gold River, British Columbia</span> Village in British Columbia, Canada

Gold River is a village municipality located close to the geographic centre of Vancouver Island in British Columbia, Canada. In terms of the Island's human geography it is considered to be part of the "North Island", even though it technically is on the Island's west coast.

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

The term freshet is most commonly used to describe a snowmelt, an annual high water event on rivers resulting from snow and river ice melting. A spring freshet can sometimes last several weeks on large river systems, resulting in significant inundation of flood plains as the snowpack melts in the river's watershed. Freshets can occur with differing strength and duration depending upon the depth of the snowpack and the local average rates of warming temperatures. Deeper snowpacks which melt quickly can result in more severe flooding. Late spring melts allow for faster flooding; this is because the relatively longer days and higher solar angle allow for average melting temperatures to be reached quickly, causing snow to melt rapidly. Snowpacks at higher altitudes and in mountainous areas remain cold and tend to melt over a longer period of time and thus do not contribute to major flooding. Serious flooding from southern freshets are more often related to rain storms of large tropical weather systems rolling in from the South Atlantic or Gulf of Mexico, to add their powerful heating capacity to lesser snow packs. Tropically induced rainfall influenced quick melts can also affect snow cover to latitudes as far north as southern Canada, so long as the generally colder air mass is not blocking northward movement of low pressure systems.

<span class="mw-page-title-main">Geography of British Columbia</span> Overview of the geography of British Columbia

British Columbia is the westernmost province of Canada, bordered by the Pacific Ocean. With an area of 944,735 km2 (364,764 sq mi) it is Canada's third-largest province. The province is almost four times the size of the United Kingdom and larger than every United States state except Alaska. It is bounded on the northwest by the U.S. state of Alaska, directly north by Yukon and the Northwest Territories, on the east by Alberta, and on the south by the U.S. states of Washington, Idaho, and Montana. Formerly part of the British Empire, the southern border of British Columbia was established by the 1846 Oregon Treaty. The province is dominated by mountain ranges, among them the Canadian Rockies but dominantly the Coast Mountains, Cassiar Mountains, and the Columbia Mountains. Most of the population is concentrated on the Pacific coast, notably in the area of Vancouver, located on the southwestern tip of the mainland, which is known as the Lower Mainland. It is the most mountainous province of Canada.

Tweedsmuir South Provincial Park is a provincial park covering parts of the eastern Kitimat Ranges, northern Pacific Ranges, and the Rainbow Range in British Columbia, Canada. It was established on May 21, 1938 in the western interior of the province, to protect its important natural features. The park hosts a variety of recreation activities for visitors. This park encompasses a range of diverse species in this park including bears, moose, and various fish. There are also a few at risk species in this park.

<span class="mw-page-title-main">Geography of Arizona</span>

Arizona is a landlocked state situated in the southwestern region of the United States of America. It has a vast and diverse geography famous for its deep canyons, high- and low-elevation deserts, numerous natural rock formations, and volcanic mountain ranges. Arizona shares land borders with Utah to the north, the Mexican state of Sonora to the south, New Mexico to the east, and Nevada to the northwest, as well as water borders with California and the Mexican state of Baja California to the southwest along the Colorado River. Arizona is also one of the Four Corners states and is diagonally adjacent to Colorado.

The McGregor Range is a mountain range in the Central Interior of British Columbia, located between the main spine of the Rocky Mountains and the Fraser River on the northeast and southwest, and between the Torpy River on its southeast and the McGregor River on its northwest. Though adjacent to the Rockies and very mountainous, the McGregor Range is part of the McGregor Plateau, a subdivision of the Fraser Plateau.

<span class="mw-page-title-main">South Chilcotin Mountains Provincial Park</span> Provincial park in British Columbia, Canada

South Chilcotin Mountains Provincial Park is a provincial park in British Columbia, Canada, located on Highway 40 northwest of Lillooet, British Columbia. The park, which is 56,796 ha. in size, was established on April 18, 2001, and It was created out of a portion of the Spruce Lake Protected Area. The park is located on three Indigenous Nations: The Tsilhqot’in, St’at’imc, and Secwepemc.

The Triglav Lodge at Kredarica is the highest mountain hut in Slovenia and the highest meteorological station in the country. It stands on a small plateau just under the peak of Kredarica, an elevation in the ridge between Rjavina and Triglav. The Valentin Stanič Lodge stands to the northeast below Begunje Peak, and the Planika Lodge at Triglav stands to the south. In the vicinity there is also a chapel dedicated to Our Lady of the Snows, and a few metres away there is a small cave named Ivačič Cave.

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

McGregor Mountain is an 8,122-foot (2,476-metre) elevation massif located in the Stehekin Valley of the North Cascades, in Chelan County of Washington state. McGregor Mountain is situated northwest of Lake Chelan in the northern Methow Mountains, on the shared border of North Cascades National Park and Lake Chelan National Recreation Area. The closest community is Stehekin, and the nearest higher neighbor is Goode Mountain, 7.3 miles (11.7 km) to the northwest. Precipitation runoff from the mountain drains into tributaries of the Stehekin River. Topographic relief is significant since the southern aspect of the mountain rises 6,600 feet above this river in approximately two miles. The famous Pacific Crest Trail traverses the western base of this mountain, and the strenuous 7.7-mile (12.4 km) McGregor Mountain Trail gains 6,400 feet of elevation to take hikers within a half-mile of the summit. Reaching the summit requires exposed scrambling the final 1,100 feet, and an ice axe is needed if the trail remains covered by snowpack. The summit was the site of an old fire lookout cabin from 1923 until 1955, but now has a radio repeater for the National Park Service. The views from the top include Glacier Peak, Black Peak, Corteo Peak, Frisco Mountain, Tupshin Peak, Dome Peak, Glory Mountain, and many others. This mountain was named for Billy McGregor, a Stehekin Valley resident who had a cabin and homestead at the base of this mountain during the 1890s. In May 1901, Billy disappeared overnight from a boat docked in Lake Chelan, and was never seen or heard from again.

<span class="mw-page-title-main">Flathead Range (Canada)</span> Mountain range in British Columbia and Alberta, Canada

The Flathead Range is a mountain range of the Canadian Rockies in Alberta and British Columbia, Canada. It is located on the Continental Divide, east of Fernie, in the Kootenay Land District. It stretches 27 km (17 mi) lengthwise north–south from Crowsnest Pass to North Kootenay Pass. The range's toponym was officially adopted on 30 June 1912 by the Geographic Board of Canada, and was named in association with the Flathead River.

<span class="mw-page-title-main">Big Snow Mountain (British Columbia)</span> Mountain in the country of Canada

Big Snow Mountain is a 2,357-metre (7,733-foot) mountain summit located in British Columbia, Canada.

<span class="mw-page-title-main">Whitesaddle Mountain</span>

Whitesaddle Mountain is a summit located in British Columbia, Canada.

<span class="mw-page-title-main">Blackhorn Mountain</span>

Blackhorn Mountain is a summit located in British Columbia, Canada.

References

  1. "Longworth Peak". PeakBagger. Retrieved 2022-09-04.
  2. "BC Ministry of Environment". Automated Snow Weather System. Retrieved October 5, 2022.