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Howse Peak
Howse Peak
Howse Peak
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Howse Peak is the highest mountain in the Waputik Mountains, a subrange of the Canadian Rockies. It is located 5 km (3 mi) west of the Icefields Parkway, above Chephren Lake, on the continental divide between Alberta and British Columbia.[6] At 3,295 m (10,810 ft), it is the 46th highest peak in Alberta, and the 59th highest in British Columbia.

Key Information

Howse Peak's name comes from Howse Pass, which lies 5 km (3 mi) to the west. The pass was named by David Thompson, after the Hudson's Bay Company trader Joseph Howse, who crossed the pass in 1809. (Thompson had actually crossed the pass two years earlier.)

Climbing

[edit]

Howse Peak is a dramatic mountain, rising over 1,600 m (5,249 ft) above both the Mistaya River to the east and Howse Pass to the west, in only a few horizontal kilometres.[7] It is also a formidable climbing challenge. The easiest route requires a 25 km (16 mi) hike up the Howse River and then a climb up a glacier on the west side of the peak. In addition, at least two high-quality, difficult (Grade V/VI) technical routes exist on the east side of the mountain.[8][9]

The first ascent was made on August 14, 1902 by J. Norman Collie, Hugh Stutfield, G.M. Weed, and Herman Woolley, guided by Hans Kaufmann. Starting from their camp at the foot of the peak, they began the ascent with a tiring two hour jaunt through the woods, continuing onto a rocky ridge that led up to the peak. However, they soon ran into two precipitous rock faces along the ridge. The first was tackled with little difficulty, the second however proved a more formidable challenge. With much time and effort expended, Kaufmann and Woolley managed to descend a 50-foot perpendicular rock chimney. The rest of the group however decided to descend into the valley before re-attaining the ridge further along. After a long snow grind interrupted by a few crevasses, they reached the summit eight hours from their starting point. "The summit is formed of a most enormous snow cornice running along the ridge for a great distance, and overhanging the terrific precipices which line the western side of Bear Creek above Waterfowl Lake."[4]

Geology

[edit]

Like other mountains in Banff National Park, Howse Peak is composed of black limestone and yellow sedimentary rock laid down during the Precambrian to Jurassic periods.[10] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[11]

Climate

[edit]

Based on the Köppen climate classification, Howse Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers.[12] Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Howse Peak drains into the Mistaya River, Howse River, and the Blaeberry River.

Incidents

[edit]

On 16 April 2019, David Lama, Jess Roskelley and Hansjörg Auer were killed by an avalanche during their descent after having climbed the mountain's east face on a new route.[13][14][15][16]

[edit]
  • Howse Peak
    Howse Peak
  • Howse Peak above Chephren Lake
    Howse Peak above Chephren Lake

References

[edit]
[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia

Howse Peak

View on Grokipedia
from Grokipedia
Howse Peak is a 3,295-metre (10,810 ft) mountain straddling the Continental Divide on the Alberta–British Columbia border in Banff National Park, Canada, and is the highest summit in the Waputik Mountains, a subrange of the Canadian Rockies. Named after Joseph Howse, a 19th-century Hudson's Bay Company explorer who traversed nearby Howse Pass, the peak features a striking twin-tipped spire with a sheer 900-metre (3,000 ft) east face of sedimentary rock often streaked with snow and ice. Prominently visible from the Icefields Parkway approximately 5 km (3 mi) to the east, Howse Peak dominates the skyline alongside neighboring summits like Mount Chephren and , drawing hikers and climbers to its remote, glaciated terrain despite challenging access and lack of cell service. The mountain's first recorded ascent occurred in 1902, but it gained renown in circles for its formidable east face routes, including the extreme M-16 line, which saw its first complete ascent in 1999 by Steve House, , and Scott Backes after a grueling five-day push. Howse Peak achieved tragic notoriety in April 2019 when an avalanche claimed the lives of renowned alpinists , , and Hansjörg Auer during their attempt on the M-16 route or a variation. The trio, attempting a fast one-day ascent and descent from the base, summited amid deteriorating weather before the slide buried them on the lower slopes; their bodies were recovered five days later by search teams in a debris field below the glacier. This incident, one of the deadliest in modern alpinism, underscored the peak's hazardous conditions, including unstable cornices and seracs, while highlighting the climbers' elite status—Lama and Auer were Austrian prodigies, and Roskelley an American veteran of high-profile expeditions.

Geography

Location and Access

Howse Peak is located at coordinates 51°48′50″N 116°40′52″W, straddling the provincial border between and . As the highest summit in the Waputik Mountains, a subrange of the Canadian Rockies, it rises to an elevation of 3,295 meters (10,810 feet) on the continental divide. The peak lies within the boundaries of both in and in , contributing to the protected status of the surrounding wilderness area. Situated approximately 5 kilometers (3 miles) west of the Icefields Parkway (Highway 93), Howse Peak is visible from this major scenic route and is positioned near the Howse Pass trailhead, providing a key entry point to the region. The peak was named in 1902 during its by a expedition led by J. Norman Collie, honoring the nearby Howse Pass, which in turn commemorates Joseph Howse, a explorer who traversed the area in 1809–1810 while seeking routes to the watershed. Access to Howse Peak primarily involves a challenging approach hike of about 25 kilometers along the Howse River valley, starting from the trailhead on the Icefields Parkway near Saskatchewan Crossing. This route follows the David Thompson Heritage Trail through dense forest and open valley, gaining elevation gradually before reaching the base of the peak, often requiring multi-day travel for climbers due to the remote terrain. Visitors must obtain a national park pass for entry into , with additional backcountry permits needed for overnight stays or camping in the area.

Topography and Hydrology

Howse Peak reaches an elevation of 3,295 metres (10,810 feet) above and possesses a of 1,227 metres (4,026 feet), making it a significant in the Canadian Rockies. As the highest summit in the Waputik Mountains subrange, it lies astride the continental divide between and , embodying the rugged alpine character of the region. The peak's topography is defined by contrasting faces: its east face ascends steeply and dramatically from the Howse Valley, forming a sheer 900-metre wall of that challenges mountaineers with intricate and mixed routes. The west side, by comparison, presents gentler glacier-covered slopes that facilitate more straightforward approaches via snow and travel. Adjacent peaks include Mount Chephren to the north and approximately 3 kilometres to the north, contributing to a clustered skyline visible from the Icefields Parkway. In terms of hydrology, Howse Peak's meltwater and runoff diverge along the continental divide into distinct basins. Northern and eastern drainage feeds the Mistaya River and Howse River, respectively, both tributaries of the within the watershed. Western flows, including glacial melt from the slopes above Chephren Lake, contribute to the Blaeberry River, which joins the system en route to the . The surrounding terrain forms part of the extensive Waputik Range's glaciated high country, encompassing icefields, cirques, and ridgelines that transition below the treeline into alpine meadows and U-shaped valleys carved by past glaciation. This diverse landscape supports a network of seasonal streams and supports the peak's role in regional water dynamics.

Geology

Rock Composition

Howse Peak, located in the Waputik Range of , is primarily composed of sedimentary rocks ranging from shales at its base to limestones and forming the upper cliffs. These layers were deposited in ancient shallow seas over hundreds of millions of years, with the dominant black evident on the peak's steeper faces. Yellow sedimentary bands appear higher on certain routes, contributing to the peak's layered profile. The mineral composition includes prominent dolomite interbeds alongside shale layers within the limestone sequences, which create distinct fracture patterns due to differential weathering and bedding planes. Dolomite, a calcium-magnesium , adds to the durability of the cliff faces, while shales introduce softer, more friable zones that accentuate the stratified appearance visible from afar. These interbeds, primarily from Middle Cambrian formations, form the rugged cliffs characteristic of the Waputik Range. Visually, the eastern face of Howse Peak features dark, sheer cliffs of nearly black , forming a steep, monolithic wall with minimal layering exposure and white vein accents. In contrast, the western slopes exhibit lighter, more weathered sedimentary layers, including yellowish bands that erode into gentler terrain. This dichotomy highlights the peak's asymmetric profile, with the black dominating the imposing east side. The sedimentary layering influences the peak's stability by creating natural bedding planes that serve as weaknesses, facilitating slab avalanches in winter conditions, while providing reliable, incised holds for technical on routes like the Northeast . The interbedded shales and can lead to variable rock quality, with some sections offering solid protection and others prone to flaking. Overall, these compositional traits underscore the peak's challenging yet feature-rich structure for mountaineers.

Tectonic Formation

Howse Peak's tectonic formation is primarily attributed to the , a major mountain-building event that occurred between approximately 80 and 55 million years ago during the to early periods. This resulted from the and collision of the Farallon oceanic plate beneath the western margin of the North American plate, leading to compressional forces that deformed the continental crust across western , including the region now encompassing in the Canadian Rockies. The dominant process shaping Howse Peak involved thrust faulting within the Rocky Mountain , where older and rocks were displaced eastward along low-angle faults and overridden younger sedimentary strata, resulting in stacked thrust sheets and characteristic inverted . These structures formed through thin-skinned , with deformation concentrated in the overlying sedimentary cover rather than deep involvement, though basement rocks influenced the overall . Howse Peak, as part of this belt's Main Ranges, exemplifies the eastward propagation of these thrusts, which created the peak's rugged through folding and faulting over tens of millions of years. The foundational rocks of Howse Peak evolved from ancient seabeds, with carbonates and clastics deposited in marine environments before the orogenic compression. Subsequent Pleistocene glaciation, during the Ice Age from about 2.6 million to 11,700 years ago, further refined the peak's form through erosional sculpting by valley glaciers and ice sheets, enhancing its steep faces and cirques. Ongoing uplift in the region, driven by isostatic rebound following glacial unloading, proceeds at rates of approximately 0.1–0.3 mm per year (as of 2020), contributing to the continued elevation of the .

Climate

Weather Patterns

Howse Peak, situated in the Waputik Mountains of , experiences a classified as Köppen Dfc, characterized by long, cold winters spanning November to April and short, mild summers from June to . This reflects the region's cold, snowy conditions influenced by its high and position in the Canadian Rockies, where continental polar air masses dominate in winter and milder Pacific air moderates summers. Winters feature persistent subzero temperatures, with average lows at nearby Lake Louise reaching -21.4°C in , while summers see daytime highs around 15-20°C at higher elevations, though nights can dip below freezing. Precipitation in the Howse Peak area averages 800-1,000 mm annually, predominantly falling as due to moist Pacific air funneled eastward by the ' topography. Heavy winter snowfall results from , accumulating as a of 3-5 meters on exposed slopes and ridges by late winter, which supports regional through seasonal melt. Rainfall is more concentrated in summer months, but overall totals increase with , exceeding 1,000 mm on windward mountain slopes compared to lower valleys. Wind patterns are marked by frequent chinook winds during winter, which are downslope that cause rapid temperature fluctuations of up to 20-30°C in hours by compressing and warming as they descend the eastern Rockies. These events occur on about one in three winter days in the region, with average speeds of 20-40 km/h and gusts reaching 100 km/h on exposed ridges like those near Howse Peak, contributing to redistribution and risks. Prevailing westerly winds throughout the year average 10-15 km/h at mid-elevations but intensify at altitude, influencing local weather variability.

Environmental Conditions

The environmental conditions surrounding Howse Peak, located in the Waputik Mountains of , feature a diverse alpine ecosystem shaped by high elevation and harsh conditions. Above the treeline, the landscape transitions to , supporting hardy species adapted to short growing seasons and strong winds, such as whitebark pine () and subalpine fir (), which form scattered communities near the timberline. Lower slopes are dominated by lodgepole pine () forests, interspersed with meadows of wildflowers including alpine forget-me-not (), which bloom vibrantly in rocky soils during brief summer periods. These plant communities contribute to and provide critical forage for herbivores in this subalpine zone. Fauna in the Howse Peak area reflects the rugged terrain, with common species including grizzly bears (Ursus arctos horribilis), which across valleys and slopes, and (Oreamnos americanus), often observed on steep cliffs. Smaller mammals like pikas (Ochotona princeps) inhabit talus fields, collecting vegetation for winter haypiles, while golden eagles (Aquila chrysaetos) soar overhead, preying on rodents and carrion. Seasonal migrations are influenced by , as and other ungulates move to higher elevations for fresh exposed in early summer, though changing melt patterns due to warming temperatures are altering these rhythms. Howse Peak is near retreating glaciers in the Waputik Mountains, which have lost significant mass over recent decades, contributing to the formation of proglacial lakes like nearby Chephren Lake and exposing new terrain for colonization by pioneer plants. As of 2023, glaciers in the region have lost more than 20% of their ice volume since the 1980s, accelerating habitat changes. This glacial retreat drives habitat shifts, as meltwater alters riparian zones and creates dynamic mosaics of wetland and barren ground, affecting aquatic and terrestrial species distributions. The area falls within Banff National Park, providing legal protection for these ecosystems under Parks Canada's management framework, which emphasizes biodiversity preservation. However, climate change poses ongoing threats, including permafrost thaw in alpine soils that destabilizes slopes and releases stored carbon, alongside the spread of invasive species like cheatgrass (Bromus tectorum), which outcompete native vegetation in disturbed areas.

Mountaineering

Early History and First Ascents

The Howse Pass, through which Howse Peak rises prominently, served as a vital travel corridor for long before European arrival. The Ktunaxa (Kootenay) First Nation utilized the pass from at least the to access bison herds on the eastern plains, facilitating seasonal migrations and trade exchanges. European exploration of the region began in the early 19th century with fur traders seeking new routes westward. In 1810, explorer Joseph Howse traversed the pass, establishing a temporary and noting the dramatic mountain scenery, including the prominent peak that would later bear his name. Howse's journey marked one of the earliest documented European crossings, highlighting the pass's potential as a artery despite challenges from hostile encounters with Pikani (Peigan) peoples, which led to its abandonment by traders after 1811. The peak itself, while observed during these expeditions, remained unnamed and unclimbed amid the focus on overland transport. By the 1890s, systematic surveys of the Canadian Rockies, conducted by the Geological Survey of Canada, began mapping the Waputik Mountains, including the area around Howse Peak, to support boundary delineation and resource assessment. These efforts, led by figures like George M. Dawson, provided foundational topographic data that fueled later ventures. The peak received its formal name in 1902 from J. Norman Collie's expedition team, honoring the pass and its explorer. The first ascent of Howse Peak occurred on August 14, 1902, during this expedition, undertaken by J. Norman Collie, Hugh E. M. Stutfield, Hermann Woolley, G. M. Weed, and guide Hans Kaufmann. Starting from a camp in burnt timber on the western slopes, the party ascended via the west glacier route, navigating a bare-backed ridge intersected by precipices and steep slopes to reach the 3,295-meter summit by early afternoon. This climb exemplified the of Rocky Mountain exploration (circa 1890–1910), driven by British alpinists' pursuits of mapping unknown terrain, scientific observation, and peak conquests in the newly accessible national parks.

Notable Routes and Challenges

The standard route on Howse Peak ascends the west side via , classified as Class 3-4 with a 25 km approach hike along the Howse River, demanding navigation skills and rated PD (peu difficile) on the French alpine scale. This route serves as a benchmark for accessing the summit, emphasizing endurance over technical difficulty compared to steeper faces. East face routes represent some of the most demanding technical climbs on the peak, graded V/VI overall, with mixed and rock features up to 1,000 m in length. The seminal M-16 route, established in 1999 by , Scott Backes, and Steve House, spans approximately 15 pitches of WI6 to WI7+ and mixed terrain with A2 aid, pioneering extreme winter alpinism in the Canadian Rockies through fragile "snow-ice" formations and steep snow slopes. A landmark subsequent ascent, Howse of Cards, was completed in 2002 by , Kevin Mahoney, and Scott Semple as the first full east face traverse; this 1,065 m line (VI M7- WI6X) shares initial pitches with M-16 before diverging into thin, deteriorating , cruxes (M6+ X WI6 R), and snow-covered 5.7 rock, over two attempts amid fragile conditions. In 2019, , , and pioneered an unnamed new line on the east face, approximately 1,200 m of WI5 to WI6+ ice and M6 mixed climbing, starting on lower sections of M-16 before traversing left into a bowl above Life by the Drop and continuing via difficult mixed bands to the southwest ridge. This ascent exemplified modern lightweight alpinism trends, executed alpine-style with unroped sections and a rapid 1,340 m gain in under seven hours, prioritizing speed and minimal gear for high-alpine efficiency. Climbing Howse Peak's routes presents multifaceted challenges, including cornice collapses on ridges, rockfall from loose mixed terrain, and complex route-finding across sheer, variable faces that demand precise line selection. Success requires advanced mixed climbing proficiency for integrating ice tools with rock protection in poor conditions, alongside rigorous avalanche assessment to mitigate spindrift, unstable slopes, and overhead hazards in this remote, weather-exposed environment.

Incidents

2019 Avalanche Tragedy

On April 16, 2019, Austrian climbers and , along with American climber , attempted a new route on the east face of Howse Peak in , . The trio, all sponsored athletes of with extensive experience in high-altitude alpinism including multiple Himalayan expeditions, began their ascent around 6 a.m. after establishing a base camp the previous day. They summited before 1 p.m., having climbed approximately 1,340 meters in a fast-and-light alpine style without fixed ropes or supplemental oxygen. During their descent via the southwest ridge, the climbers were caught in a around 2 p.m., triggered by a likely collapse or wind-loaded snow on the slabs below. The , consisting of a relatively small but fast-moving slab, swept the three climbers into a , burying them under debris. (28), Auer (35), and Roskelley (36) were all confirmed deceased from asphyxiation due to the snow slide. Search efforts began on April 17 after the climbers failed to return, with their location pinpointed by debris and gear. The bodies were recovered on April 21 by rescuers using an dog and extraction, despite challenging weather and further risks. The incident highlighted the perils of committing descents on steep, snow-covered terrain, with the new east face line later documented in climbing records.

Safety and Rescue Operations

Following the 2019 avalanche on Howse Peak, initiated search and recovery operations on April 17, prompted by the climbers' overdue report. Helicopter teams conducted starting April 18, identifying avalanche debris and climbing gear at the base of the east face, but poor weather and high avalanche hazards prevented ground access until April 20. On , over 28 personnel, including Visitor Safety Specialists and an avalanche rescue dog and handler from the Canadian Avalanche Rescue Dog Association, executed the recovery using long-line helicopter extractions and probing techniques to retrieve the bodies from the debris field. Safety protocols for on Howse Peak emphasize preparation to mitigate risks, which are prevalent in Banff National Park's terrain. Climbers should consult avalanche forecasts through Avalanche Canada's Mountain Information Network, which provides real-time user-submitted observations and professional assessments for specific regions like the Canadian Rockies. Key recommendations include traveling with experienced partners for mutual checks, carrying essential rescue gear such as avalanche beacons, probes, and shovels, and avoiding the east face during spring when wind slabs—formed by strong winds redistributing snow—pose heightened instability. In response to the 2019 incident, the climbing community has placed greater emphasis on real-time weather monitoring via apps like those from and proactive sharing of route beta through platforms such as Mountain Project to inform hazard awareness. The American Alpine Club's post-incident analysis, based on recovered equipment and photographic evidence, highlighted the dangers of solo or unroped descents without transceivers, advocating for their consistent use even on ascents to facilitate rapid location in case of burial. Beyond , Howse Peak presents general hazards including falls on glaciated approaches and from sudden temperature drops and exposure. Climatic factors like persistent winds, which build unstable snow layers, further compound these dangers during winter and spring expeditions.

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