Wells Gray Provincial Park

The boundaries of Wells Gray Park encompass 60 percent of the drainage basin of the Clearwater River, and most water that originates in the park flows into this river. The northern two-thirds of the park is extremely rugged with relief ranging from Clearwater Lake at an elevation of to at Mount Lyons on the northern park boundary, west of Mount Pierrway. These summits are part of the Cariboo Mountains, and most of the east boundary of the park follows the mountain divide between drainage into the North Thompson River and into the Clearwater River. Individual mountain groups dominate the topography of the northern park region and are separated by deep glacial valleys, several of which contain large lakes such as Clearwater, Azure and Hobson. The ruggedness of its features has ensured that northern Wells Gray remains little known except to the hardiest of backpackers. The southern third of Wells Gray Park is traversed by the Clearwater Valley Road, although large areas are accessible only by trail. The dominant topography features volcanic plateaus, lava flows and deep canyons which are crowned by several peaks over high. The waterfalls, for which Wells Gray is famous, usually result from the interaction of volcanic eruptions and glacial activity. The best known is Helmcken Falls, the fourth highest waterfall in Canada, which plunges over the edge of one of these volcanic plateaus. Highest mountains The eight highest mountains in Wells Gray Park are: 1) Mount Lyons, 2946 m. The first recorded ascent was made by Bill McKenzie and Roger Wallis on August 18, 2005. It is named after Chess Lyons, Wells Gray Park surveyor in 1940, naturalist, author, photographer, and explorer. 2) Mount Goodall, 2930 m. The mountain consists of 11 distinct summits and extends for nearly 8 km in a northwest to southeast direction. On the northeast side, an unbreached wall of rock and ice rises between 400 m and 1,300 m from the Goodall Glacier. The first ascent was achieved on August 21, 2006, by Roger Wallis, Don Chiasson, and Jim Lundy. They established its height, only 16 m lower than Mount Lyons. As of 2022, only four of Goodall's 11 summits have been conquered. Mount Goodall is one of six peaks in this area named in 1966 in honor of Canadian soldiers from the Quesnel area who were killed in action during World War II; it is named after Trooper Walter Henry Goodall, age 24. 3) Garnet Peak, 2876 m. This is a prominent landmark from many viewpoints in southern Wells Gray Park. It is located north of Azure Lake. The first ascent was by Hugh Neave, Tor Schmid and Barbara Hargreaves on August 29, 1974. It was long believed to be the park's highest mountain until expeditions to the north boundary found the above two peaks were higher. 4) Black Cone, 2861 m. This is the second highest summit of the Goodall group and has been unofficially called "The Black Cone". Its first ascent was on July 30, 2012, by Paul Geddes, Norm Greene, and Bill McKenzie. 5) Mount Pierrway, 2854 m. It was first climbed in 1969 by Art Maki and Art Wilder. The second ascent was in 1987 and the third in 2005. This honors another World War II casualty, Private Alfred Pierrway, age 22. 6) "Unnamed Peak, 2847 m, 3.7 km WSW of Mount Pierrway". It is located on the north park boundary near Mount Lyons. As of 2022, there is no record of this peak being climbed, therefore it is Wells Gray Park's highest unclimbed mountain. 7) Mount Hugh Neave, 2829 m. Located east of Hobson Lake and north of Garnet Peak. Hugh Neave, first to summit Garnet Peak, and Peter Cowan attempted to climb it in 1972 via Hobson Glacier to the east, but were forced to turn back by difficult terrain. It was named after Hugh Neave after his death in 1988. Two expeditions in the 1990s, two in 2015, and one in 2017 failed to reach the summit. The first successful ascent was on August 27, 2019, by JF Labranche and Travis Goodridge. 8) "Unnamed Peak, 2797 m, 3.1 km SE of Mount Beaman". ==History==

Prior to the arrival of Europeans, the Wells Gray area was a valued hunting ground to the Secwepemc (Shuswap), Tsilhqot'in (Chilcotin) and Canim Lake Indigenous People. This resulted in a conflict around 1875 over access to caribou herds. Geographic names like "Battle Mountain", "Fight Lake", "Battle Creek" and "Indian Valley" recall this period. In 2018 Sarlacc's Pit cave was discovered in the park. Notable for its size, the entrance pit measures some 100m x 60m, and a 61m waterfall on the pit wall is fed by snowpack and glacier meltwater. This stream emerges 2 km east and flows into Ovis Creek. Clearwater River dams The disastrous Fraser River flood of 1948 nearly changed the Clearwater River and Wells Gray Park. In November 1947, prior to the flood, the Federal Minister of Public Works had proposed the creation of a joint federal-provincial committee to study the Fraser River's water resources. The flood in the following spring made this project more urgent, and in late 1948 the Dominion-Provincial Board Fraser River Basin was established to report on power generation, fisheries, flood control, water supply and recreation. Between 1949 and 1954, the committee of ten collected data and filled in the gaps in other government studies. No report was produced, but in 1953, 12 detailed maps of the Clearwater River between Hemp Creek and the North Thompson River were published. These had a scale of 1 inch to 500 feet, and a contour interval of 20 feet. As of 2023, these sheets are still the most detailed and accurate topographic maps available of the lower Clearwater, although they are out-of-date regarding human developments. The Fraser River committee proposed two dams, one just upstream from Clearwater and one at Sabre Tooth Rapids. In 1955, the federal and provincial governments replaced this committee with a smaller one with only four members, the Fraser River Board, and directed it to determine what development of the Fraser River's water resources would be feasible, particularly regarding flood control and hydro-electric power. The Board published two preliminary reports, one about flood control in 1956, and one about hydro-electric developments in 1958. The idea of developing hydro power from the Clearwater River and its tributaries was not new to the Fraser River Board. In 1918, Helmcken Falls was studied as a source of power for Kamloops, but the needed transmission lines were prohibitively long. In the late 1940s, the Aluminum Company of Canada examined the power potential of Helmcken Falls, but chose Kitimat instead, thereby flooding northern Tweedsmuir Park instead of Wells Gray. In 1959, a comprehensive development of the Murtle River was proposed by the British Columbia Power Commission. These proposals paled in comparison to the final report of the Fraser River Board, issued in 1963. Although dams were proposed elsewhere such as on the Cariboo and McGregor Rivers and at the Grand Canyon of the Fraser, the Clearwater River attracted most of the attention with seven dams and five reservoirs recommended. The dams would be located upstream from the North Thompson confluence, at the lower end of Granite Canyon, at Sabre Tooth Rapids, near Myanth Falls (upper and lower dams), at the outlet of Hobson Lake and on the low pass between Hobson and Quesnel Lakes. Together, these dams would turn the Clearwater River into a 160 km long (100-mile long) series of reservoirs extending nearly to its glacial source above Hobson Lake. Each dam would back water almost to the foot of the next one, similar to the Columbia River today which has little free-flowing water. The dam at Sabre Tooth Rapids would be the highest at , flooding most of Helmcken Canyon, inundating Sylvia and Goodwin Falls, and submerging the bottom of Helmcken Falls. The plan for Baileys Chute envisaged two dams; the lower dam at Myanth Falls would divert the river into a power canal ending at Baileys Chute. Collectively, the proposal (including the other rivers) was called System E and the cost of construction was estimated at $398,503,500. There was little reaction to the Fraser River Board's report. The public was not too concerned about losing remote preserves such as Wells Gray Park, when British Columbia had so much wilderness land. The park may have been saved because the British Columbia government was preoccupied in the 1960s with planning and building (and paying for) the W.A.C. Bennett Dam on the Peace River and Mica Dam, Keenleyside Dam and Duncan Dam, all part of the Columbia River Treaty projects. In 1971, BC Hydro, the provincial power utility, revived the Fraser River Board's report and took a new look at the feasibility and costs of building the seven dams on the Clearwater River. In just a decade, the environmental movement had gained power and credibility in the province, and BC Hydro's interest in the Clearwater quickly caught the attention of the Shuswap-Thompson River Research and Development Association (STRRADA) and the newly formed Yellowhead Ecological Association based in Clearwater, BC. One of the undertakings was to offer bus tours of Wells Gray Park during the summer of 1972. The tours stopped at viewpoints where the volunteer guides urged passengers to imagine how the valley would look when flooded by the dams. The strategy was effective and succeeded in creating an uproar of protest about the dams. Within a year, the plan to dam the Clearwater River was quietly shelved, but BC Hydro retained its water rights until 1987 when the flooding reserve on the Clearwater was cancelled. ==Natural history==

Wells Gray Park is bordered on every side by different types of terrain and these merge within the boundaries to give the Park its splendid diversity. According to Tom Dickinson, Professor Emeritus at Thompson Rivers University, Wells Gray hosts about 1,050 species of trees, shrubs, and flowers; more than 1,000 species of lichens, several important for wildlife, especially mountain caribou; about 200 species of mushrooms; at least 275 species of mosses and liverworts; 15 species of fish; 56 species of mammals; 5 species of amphibians; 3 species of reptiles; over 275 species of birds with at least 75 being listed as rare or very rare; and several thousand species of invertebrates, including dragonflies, moths, butterflies, and of course mosquitoes. A variety of factors enrich the Park and these include the 1926 forest fire, the proximity of the Fraser Plateau westward, the Cariboo Mountains northeastward, the interior wet belt eastward, and the semi-desert zone to the south. Within the Park, micro-climates, altitude, soil type, and availability of water all have their effects and contribute to the existence of this amazing variety of plant and animal life. ==Wildlife==

This park is home to various birds as well as the mammalian species of grizzly bear, white-tailed deer, beaver, moose, mule deer, black bear and timber wolf. ==Climate==

Winters in the Clearwater Valley are severe, with an average of of accumulated snow at lower elevations and much more higher up. Snow may linger along the low elevation roads until mid-April and never completely disappears from the north sides of the mountains. Early May and most of June are often rainy and, during the summer, storms occur about once a week. Average annual precipitation at Clearwater is and this increases as one travels north into the park and closer to the mountains. Clearwater Lake receives over and Azure Lake about . Summer temperatures in the Clearwater Valley are often in the mid-20s Celsius, but may reach 30 degrees, and vary considerably according to altitude. September through mid-October usually features clear warm days, cool nights and colourful fall foliage. ==Access==

There are five roads that provide access to Wells Gray Park. Many volunteers and two local logging companies, Dale Miller Logging and Wadlegger Logging, stepped up to temporarily repair the road, but work couldn't get underway until April 2021, nine months after the washout, due to a lack of permits. When work began, it was quickly discovered that the damage was more extensive than initially believed - beyond the scope of volunteer repairs. During 2021 and 2022, alternate routes to the Clearwater River were discussed and engineers studied the washout. A proposal for building retaining walls at a cost of $1.1 million has been submitted to the Minister of Transportation, but no decision has been made as of April 2023. The event has hit Clearwater's tourism and recreation industry hard, as the road was very popular with campers, anglers, and used by three whitewater rafting companies - Interior Whitewater Expeditions, Liquid Lifestyles, and Riverside Adventures. Interior Whitewater Expeditions (IWE) has had to cancel all overnight trips, with their only trips now being on the lower part of the river - from the put-in points below the washout. As a result of the washout, IWE cancelled 100 overnight trips in summer 2021 and laid off nearly half of their workforce. • Mahood Lake Road. It starts from Highway 24 between 100 Mile House on Highway 97 and Little Fort on Highway 5. From the latter, it is to the end at Deception Point on Mahood Lake. There is a 37-unit campground at Mahood Lake. Attractions are Canim Falls, Mahood Lake beaches and Deception Falls. Most of the road is gravel. • Murtle Lake Road. It starts at Blue River on the Yellowhead Highway and climbs for to the pass. A short trail, designed for portaging canoes or kayaks, goes the rest of the way to Murtle Lake. Murtle is North America's largest paddle-only lake. The road is rough and high-clearance vehicles are recommended but not essential. • Flourmill Volcanoes Road. It starts at 100 Mile House on Highway 97. There is no signage to help at the many junctions; refer to Exploring Wells Gray Park for directions. The road is long, mostly gravel and dirt. From the end of the road, it is a hike of to the lava flow. ==Attractions==

The park is popular from mid-May through mid-October. Campgrounds are open and serviced from late May to mid-September. The park is open year-round, but in winter the Clearwater Valley Road is plowed only as far as Helmcken Falls. Following are the park's major attractions: • Helmcken Falls is the park's main tourist draw. The waterfall is Canada's fourth highest with a vertical drop of . A road leads to a viewing platform on the north side of the canyon and a trail goes to south side and the brink. In winter, an ice cone forms which sometimes grows halfway up the falls if it is very cold and snowy. • Spahats Falls is a tall waterfall on Spahats Creek where it drops into the Granite Canyon of the Clearwater River. • Trophy Mountain is on the south edge of Wells Gray Park and consists of nine summits. The meadows bloom in late June and again in late July to early August. There are many hiking trails and routes in the meadows and on the peaks. • Third Canyon has sidewalks on both sides of the road bridge for safe viewing of two waterfalls on the upstream side and an deep gorge on the downstream side. • Moul Falls on Grouse Creek is high. It is one of the park's most popular short hikes and it is the only waterfall that hikers can go behind. • Green Mountain has a road to the top. A viewing tower provides a panorama of southern Wells Gray Park. • Dawson Falls is on the Murtle River upstream from Helmcken Falls. It is high and wide. • The Mushbowl is a narrow canyon downstream from Dawson Falls. The Clearwater Valley Road bridges the Murtle River here. Some of Wells Gray Park's oldest rocks are seen here. • Ray Farm is an abandoned homestead. John Ray lived here from 1911 to 1947. He married Alice Ludtke in 1932 and they raised three children in the wilderness, Nancy, Douglas and Robert. • '''Bailey's Chute''' is a low waterfall on the Clearwater River. In late summer and fall, salmon can be seen trying to jump the falls. A continuation of this trail goes to Marcus Falls, Myanth Falls and West Lake. • Clearwater Lake is the end of the Clearwater Valley Road. Two large campgrounds are located here. Osprey Falls is a low waterfall that the lake empties over to become the Clearwater River. Boat tours, boat rentals and a public boat launching are available here and allow access deeper into Wells Gray Park via Clearwater Lake and Azure Lake. • Murtle Lake is a wilderness lake in the southeast part of the park. See access section above. • Canim Falls is in the far western end of the park, reached by Mahood Lake Road. The Canim River flows over a lava cliff that is high. • Mahood Lake is reached from the west via Mahood Lake Road. A campground and beach are at the west end of the lake. The lake is long. Waterfalls Wells Gray Park bears the nickname "Canada's Waterfalls Park" because 42 named waterfalls are found within its boundaries. There are actually many more if the numerous creeks that cascade down the mountainsides are included, but the following table lists the named waterfalls. Campgrounds ==Gallery==

File:Clearwater Lake Garnet Peak.jpg|Clearwater Lake and Garnet Peak File:DawsonFalls.WellsGray.jpg|Dawson Falls on the Murtle River File:Mount_Hugh_Neave.jpg|Mount Hugh Neave (centre) from Hobson Glacier File:Murtle_Lake_beach.jpg|West Arm of Murtle Lake File:Sheila Lake.jpg|Sheila Lake (R) on Trophy Mountain. Trophy Mountain summit is on far right. File:Clearwater River Wells Gray Park.jpg|Osprey Falls on Clearwater River File:Moul_Falls.jpg|Hikers behind Moul Falls File:Pyramid Mountain.jpg|Pyramid Mountain from Green Mountain File:Sylvia_Falls_Mahood_River.jpg|Sylvia Falls on Mahood River File:Raft_Mountain_from_Trophy_Mountain.jpg|Raft Mountain, taken from the flower meadows of Trophy Mountain File:Silvertip_Falls.jpg|Silvertip Falls, over 200 metres tall File:Sabre_Tooth_Rapids_Wells_Gray.jpg|Sabre Tooth Rapids on the Clearwater River File:Stitca_Falls.jpg|Sticta Falls on Falls Creek File:The_Kettle.jpg|The Kettle on the Clearwater River File:Triple_Decker_Falls.jpg|Triple Decker Falls on Candle Creek ==References==