{{Infobox river | name = Incomappleux River | name_native = | name_native_lang = | name_other = | name_etymology = <!---------------------- IMAGE & MAP --> | image = Interior Rainforest (4495547683).jpg | image_caption = Incomappleux inland rainforest | map = | map_size = | map_caption = | pushpin_map = British Columbia | pushpin_map_size = | pushpin_map_caption= Location in British Columbia <!---------------------- LOCATION --> | subdivision_type1 = Country | subdivision_name1 = Canada | subdivision_type2 = Province | subdivision_name2 = British Columbia | subdivision_type3 = District | subdivision_name3 = Kootenay Land District | subdivision_type4 = | subdivision_name4 = | subdivision_type5 = | subdivision_name5 =
<!---------------------- PHYSICAL CHARACTERISTICS --> | length = | width_min = | width_avg = | width_max = | depth_min = | depth_avg = | depth_max = | discharge1_location= near Beaton<ref name=wsc>{{cite web|title=Archived Hydrometric Data Search |publisher=Water Survey of Canada |url=http://www.wsc.ec.gc.ca/hydat/H2O/index_e.cfm?cname=main_e.cfm |accessdate=October 19, 2008 |url-status=dead |archiveurl=https://web.archive.org/web/20090221205328/http://www.wsc.ec.gc.ca/hydat/H2O/index_e.cfm?cname=main_e.cfm |archivedate=February 21, 2009 }} Search for Station 08NE001 Incomappleux River near Beaton</ref> | discharge1_min = {{convert|4.76|m3/s|cuft/s|abbr=on}} | discharge1_avg = {{convert|55.8|m3/s|cuft/s|abbr=on}}<ref name=wsc>{{cite web|title=Archived Hydrometric Data Search |publisher=Water Survey of Canada |url=http://www.wsc.ec.gc.ca/hydat/H2O/index_e.cfm?cname=main_e.cfm |accessdate=October 19, 2008 |url-status=dead |archiveurl=https://web.archive.org/web/20090221205328/http://www.wsc.ec.gc.ca/hydat/H2O/index_e.cfm?cname=main_e.cfm |archivedate=February 21, 2009 }} Search for Station 08NE001 Incomappleux River near Beaton</ref> | discharge1_max = {{convert|570|m3/s|cuft/s|abbr=on}} <!---------------------- BASIN FEATURES --> | source1 = Illecillewaet Neve | source1_location = Selkirk Mountains | source1_coordinates= | source1_elevation = | mouth = Columbia River | mouth_location = Upper Arrow Lake | mouth_coordinates = {{coord|50|44|48|N|117|42|47|W|display=inline,title}}<ref>{{BCGNIS|1278|Incomappleux River}}</ref> | mouth_elevation = | progression = Incomappleux Valley | river_system = | basin_size = {{convert|1020|km2|abbr=on}}<ref name=wsc/> | tributaries_left = | tributaries_right = | custom_label = | custom_data = | extra = }} The '''Incomappleux River''' is in the West Kootenay region of southeastern British Columbia, Canada. Entering the Beaton Arm of Upper Arrow Lake, the river is a major tributary of the Columbia River. The upper reaches of the Incomappleux valley are home to some of the only inland temperate rainforest in the world.
The area has been studied since 2000 by Valhalla Wilderness Society as a part of their Inland Temperate Rainforest campaign, and the upper Incomappleux was included in the Selkirk Mountain Caribou Park proposal after groundbreaking biodiversity research by biologists Toby Spribille and Curtis Björk, sponsored by Valhalla Wilderness Society, found over 300 species of lichens in the Incomappleux, most of them in the ancient forest. This included seven species new to science. The Incomappleux Valley has been the subject of two films, one by Riel Marquardt, and more recently the VWS film ''Primeval: Enter the Incomappleux'', by award winning documentary filmmaker, Damien Gillis. VWS Director Craig Pettitt and biologist Amber Peters toured the province with the film. The Incomappleux Valley was declared a conservancy in 2023 but the remainder of the Selkirk Mountain Caribou Park proposal, containing critical old growth inland rainforest corridors still remains unprotected. The valley is in the traditional territory of the Sinixt First Nation and its protection was supported by the autonomous Sinixt.
==First Nations== The name "Incomappleux" is derived from the nsyilxcn word ''nk'mapeleqs'', meaning "point at end (of lake)". This refers to the northeastern tip of Upper Arrow Lake into which the river empties. The names of the creek and adjacent mountain are also derived from this word. A Sinixt village by this name formerly existed somewhere in the confluence area.<ref name=1Dec13>{{Cite web |url=https://www.nelsonstar.com/community/comaplix-comes-from-sinixt-word |title=Nelson Star |date=1 Dec 2013 |website=www.nelsonstar.com}}</ref>
==European presence== Europeans referred to the valley and river by various English spellings of the word, but Fish Creek/River was also common.<ref name="1Dec13" /> However, local lore has it that the word is a corruption of the Sinix't word for Fish.<ref>This was told by a Sinix't, or Lakes Person, as he described himself, who lived in Nakusp, to Lee Harding, who built a cabin at Galena Bay on Arrow Lake in 1970, once owned a house and lot in Camborne, and still has property nearby.</ref> In 1865, James Turnbull, surveyor and mapmaker, explored the Incomappleux Valley.<ref name="1Dec13" /> After the mid-1880s, visitors could enter the valley from the Canadian Pacific Railway (CP) main line, moving southward through the Glacier National Park area into the valley and following the river to its mouth, but this involved a long climb up and over a high mountain and a long trek down to the river.<ref name=MoL22>{{Cite web | url=https://open.library.ubc.ca/viewer/bcsessional/1.0225861#p67z-3r0f:%22Incomappleux%22 |page=68 (K64) |title=Minister of Lands annual report, 1922 |website=library.ubc.ca}}</ref> In 1889, the report of the Gold Commissioner at Farwell reported, "By 1889, ten locations [staked mine sites] had been made on the Northeast area of Upper Arrow Lake. Several claims, including the Fish Creek mines, had been worked on the upper reaches of Incomappleux river..." alt=Beatrice Mine|thumb|Beatrice Mine buildings above the town of Camborne in the Incomappleux River valley, B.C. alt=Battle Range|thumb|Battle Range viewed from the left (west) side of the Incomappleux River valley, looking north, 1996. Glacier National Park is beyond the Battle Range. The area around Roger's Pass was surveyed by Arthur O. Wheeler in 1902, using a photographic triangulation method that involved setting up a heavy camera on a tripod on a mountain peak and photographing all the other peaks within sight; and doing this again for all the peaks in the survey area. This survey provided the first topographic maps of Glacier National Park, the Battle Range that borders the park on the south, and the area of the upper Incomappleux River valley.<ref name=":1">Wheeler, A. O. 1905. The Selkirk Range, British Columbia. Government Printing Bureau, Ottawa. Volume 1 (text) and Volume 2 (map folio).</ref>
Access was from the south end through a deep, narrow, steep-sided gorge where the miners built a roadway about 0.5 km long out of timbers perched on the side of the cliff and anchored into rock crevices. In winter, horses pulling wagons were fitted with snowshoes for the deep snow. The timber/plank road was still in place and drivable in 1970, although some of the timber supports had fallen away, planks were broken and a sign warned, "ROAD CLOSED". In 1974, Celgar, the logging company based in Nakusp, blasted a solid road through the gorge, destroying the old timber/plank road.
== Mines == From the 1890s, mining claims staked upstream (removed from the mouth) were along Pool Creek at {{convert|6|mi|km|0|order=flip}},<ref>{{Cite web | url=https://open.library.ubc.ca/viewer/xrevherald/1.0186931#p3z-3r0f:%22Pool%22 |page=4 |title=Revelstoke Herald |date=2 Mar 1898 |website=library.ubc.ca}}</ref> Sable Creek at {{convert|11|mi|km|0|order=flip}}, and Boyd Creek at {{convert|16|mi|km|0|order=flip}}. Although most claims were accessed from the south, the Dunvegan group, at the headwaters of the river,<ref name="3Aug95">{{Cite web | url=https://open.library.ubc.ca/viewer/xkootmail/1.0181090#p3z-1r0f:%22Fish%22 |page=4 |title=Kootenay Mail |date=3 Aug 1895 |website=library.ubc.ca}}</ref> was reached by a {{convert|10|mi|adj=on|0|order=flip}} trail from the CP station at Albert Canyon.<ref>{{Cite web | url=https://open.library.ubc.ca/viewer/bcsessional/1.0059813#p196z-3r0f:%22Dunvegan%22 |page=197 (F182) |title=Minister of Mines annual report, 1917 |website=library.ubc.ca}}</ref> alt=Ore concentrator|thumb|Ore concentrator building at Camborne, 1973. The town of Camborne was built in 1902 in the lower valley, just upstream from the gorge, to service the mines. The principal mine was the Beatrice Mine, about 9.7 km up a steep trail from the town. Its owners built an ore concentrator at the upper end of the town site; horse-drawn ore carts would dump their loads into a sort of chute at the last switchback above the concentrator. The town was occupied until about 1954.<ref>When Lee Harding bought a lot from a woman then living in Revelstoke, in 1974, he was treated to her photo album and her memories of growing up there.</ref>
Nearby towns were Beaton on the Northeast Arm, just below the mouth of the Incomapplex; Galena Bay on the main lake to the south; and Trout Lake, over Galena Pass to the northeast, in the Lardeau River valley.
==Source== Formed in the Selkirk Mountains southeast of Glacier,<ref name=Hydro14>{{Google books|taI5AQAAMAAJ |Dept of the Interior, BC Hydrographic Survey, 1914|page=RA2-PA466}}</ref> the Illecillewaet Glacier near Rogers Pass is the source of the Illecillewaet River on the northwestern slope. However, the Illecillewaet Neve, which feeds the glacier, primarily flows south into the Incomappleux River.<ref>{{Cite web | url=https://www.worldwaterfalldatabase.com/waterfall/Illecillewaet-Glacier-Falls-2443 |title=Illecillewaet Glacier Falls |website=www.worldwaterfalldatabase.com}}</ref>
==Course== alt=Incomappleux River valley|thumb|Incomappleux River valley looking downriver; Boyd Creek entering from the left. 1974. The Incomappleux is about {{convert|42|mi|km|0|order=flip}} long,<ref name="Hydro14" /> with four large tributaries flowing {{convert|12|to|20|mi|km|0|order=flip}}.<ref name="3Aug95" /> Following a due south course, the swift, unnavigable river is {{convert|30|to|50|ft|m|0|order=flip}} wide.<ref name="Hydro14" /> Around {{convert|200|ft|m|0|order=flip}} high,<ref name="3Aug95" /> the narrow canyon, which is about {{convert|3|mi|km|0|order=flip}} from the mouth, funnels the glacial waters. Above the canyon, the valley widens to as much as {{convert|1|mi|km|0|order=flip}}.<ref name="MoL22" />
===2003 river incident=== In 2003, two experienced alpinists (Michel Bastien and Yves Laforest), a videographer (Aurélie Chabaud) and a multimedia student (Martin Champagneur) set out to climb Mount Hope for a childhood cancer charity then descend the Incomappleux River by kayak to Upper Arrow Lake at Beaton, British Columbia.<ref>{{Cite web|url=https://www.theglobeandmail.com/news/national/three-kayakers-missing-after-spill-in-bc-river/article25288608/|title=Three kayakers missing after spill in B.C. river|date=Aug 6, 2003|accessdate=Oct 24, 2024|via=www.theglobeandmail.com}}</ref><ref>{{Cite web |date=2014-09-15 |title=Aventuriers du Mont Hope - Sommet de l'Espoir |url=http://idedegenie.free.fr/html/aventuriers_mont_hope.html |access-date=2024-10-25 |archive-url=https://web.archive.org/web/20140915231033/http://idedegenie.free.fr/html/aventuriers_mont_hope.html |archive-date=2014-09-15 }}</ref> Just hours into the river journey, their kayaks were swept away by the rapids.<ref name="MontHope">{{Cite web |date=2017-07-06 |title=Mont Hope - sommet de l'Espoir - Expedition Yves Laforest |url=http://idedegenie.free.fr/html/histoire_mont_hope.html |access-date=2024-10-25 |archive-url=https://web.archive.org/web/20170706043956/http://idedegenie.free.fr/html/histoire_mont_hope.html |archive-date=2017-07-06 }}</ref> Of the four adventurers, only Champagneur survived and was found by rescuers six days after the incident occurred. Searches continued for two weeks until being called off by national park wardens and RCMP.<ref name="MontHope"/><ref>{{Cite web |date=August 10, 2003 |title=Mounties suspend search for missing kayakers |url=https://www.cbc.ca/news/canada/mounties-suspend-search-for-missing-kayakers-1.391617 |access-date=2024-10-24 |website=CBC News}}</ref>
==Forestry== The valley is heavily timbered and unsuited to agriculture.<ref name="Hydro14" /> This inland temperate rainforest comprises a wide range of cottonwood and spruce. The accessible conifer-dominated forest has been largely harvested over the decades.<ref>{{Cite web | url=http://www.sgrc.selkirk.ca/bioatlas/pdf/Endangered_Forests_of_the_Inland_Temperate_Rainforest.pdf#page=9 |page=9 |title=Endangered Forests of the Inland Temperate Rainforest: An inventory of old-growth in Trout Lake and the Incomappleux |date=Feb 2006 |website=www.sgrc.selkirk.ca}}</ref> Active logging returned in 1974, but environmental protests have restricted harvesting since the early 2000s.<ref>{{Cite web | url=http://valleyvoice.ca/_pdf/050914.pdf#page=1 |page=1 |title=Valley Voice |date=14 Sep 2005 |website=valleyvoice.ca}}</ref> In 2022, a moratorium was placed upon logging for at least two years.<ref>{{cite web |last1=Connelly |first1=Joel |title=The "Brazil of the North" Grapples with Cutting its Old Growth Forests |url=https://www.postalley.org/2022/11/08/the-brazil-of-the-north-grapples-with-cutting-its-old-growth-forests/ |website=www.postalley.org |date=8 November 2022}}</ref>
thumb|left|700px|Incomappleux Inland Rainforest, BC, 2010.
==Ferries and bridges across the river== In 1892, a {{convert|250|ft|adj=on|order=flip}} bridge existed at the river mouth, and a {{convert|46|ft|adj=on|order=flip}} one {{convert|20|mi|km|0|order=flip}} upstream near McDougal Creek.<ref>{{Cite web | url=https://open.library.ubc.ca/viewer/bcsessional/1.0065838#p86z-3r0f:%22Fish%22 |pages=87–88 (391–392) |title=Commissioner of Land and Works annual report, 1892 |website=library.ubc.ca}}</ref><ref>{{Cite web | url=https://open.library.ubc.ca/viewer/xrevherald/1.0186828#p0z-3r0f:%22Fish%22 |page=1 |title=Revelstoke Herald |date=22 Sep 1897 |website=library.ubc.ca}}</ref> After the one at the mouth connecting to Lardeau City was washed out, a temporary {{convert|18|by|40|ft|m|adj=on|0|order=flip}} cable ferry commenced in June 1893.<ref>{{Cite web | url=https://open.library.ubc.ca/viewer/kootstar/1.0310256#p0z-3r0f:%22ferry%22 |page=1 |title=Kootenay Star |date=3 Jun 1893 |website=library.ubc.ca}}</ref><ref>{{Cite web | url=https://open.library.ubc.ca/viewer/kootstar/1.0310255#p0z-3r0f:%22ferry%22 |page=1 |title=Kootenay Star |date=17 Jun 1893 |website=library.ubc.ca}}</ref> A replacement bridge destroyed by the 1894 flood<ref>{{Cite web | url=https://open.library.ubc.ca/viewer/xkootmail/1.0181697#p2z-1r0f:%22gone%22 |page=3 |title=Kootenay Mail |date=23 Jun 1894 |website=library.ubc.ca}}</ref> was in turn replaced.<ref>{{Cite web | url=https://open.library.ubc.ca/viewer/xrevherald/1.0187001#p0z-3r0f:%22bridge%22 |page=1 |title=Revelstoke Herald |date=29 Jun 1898 |website=library.ubc.ca}}</ref> A ferry was built in summer 1896, but its placement is unclear.<ref>{{Cite web | url=https://open.library.ubc.ca/viewer/xkootmail/1.0181671#p0z-1r0f:%22ferry%22 |page=1 |title=Kootenay Mail |date=13 Jun 1896 |website=library.ubc.ca}}</ref>
The lower bridge provided a connection in 1898,<ref>{{Cite web | url=https://open.library.ubc.ca/viewer/bcsessional/1.0064103#p96z-3r0f:%22Pool%22 |page=97 (823) |title=Commissioner of Land and Works annual report, 1898 |website=library.ubc.ca}}</ref> when the wagon road up the west side of the river was completed as far as the Camborne ferry.<ref>{{cite book |last=Parent |first=Milton |page=38 |title=Silent Shores and Sunken Ships |year=1997 |publisher=Arrow Lakes Historical Society |isbn=0-9694236-2-4}}</ref> That year, a ferry was installed across the river at Boyd Creek, which could carry six loaded packhorses.<ref>{{Cite web | url=https://open.library.ubc.ca/viewer/xrevherald/1.0186966#p3z-3r0f:%22ferry%22 |page=4 |title=Revelstoke Herald |date=20 Apr 1898 |website=library.ubc.ca}}</ref><ref>{{Cite web | url=https://open.library.ubc.ca/viewer/bcsessional/1.0064014#p78z-3r0f:%22ferry%22 |page=79 (357) |title=Commissioner of Land and Works annual report, 1899 |website=library.ubc.ca}}</ref>
In 1904, the wagon road was extended up the west side of the river from Camborne, and a bridge replaced the ferry at Boyd Creek.<ref>{{Cite web | url=https://open.library.ubc.ca/viewer/xrevherald/1.0187362#p0z-3r0f:%22Boyd%22 |page=1 |title=Revelstoke Herald |date=21 Jan 1904 |website=library.ubc.ca}}</ref><ref>{{Cite web | url=https://open.library.ubc.ca/viewer/evewoross/1.0226883#p0z-3r0f:%22Boyd%22 |page=1 |title=Evening World |date=1 Mar 1904 |website=library.ubc.ca}}</ref> At the 12-mile point, a wagon road bridge existed in the 1910s.<ref>{{Cite web | url=https://open.library.ubc.ca/viewer/bcsessional/1.0059901#p274z-3r0f:%22twelve-mile%22 |page=275 (K245) |title=Minister of Mines annual report, 1914 |website=library.ubc.ca}}</ref> The only remaining bridge, {{convert|2.4|km|mi|1}} north of Camborne, was a wooden timber bridge that had washed out by 1971. Celgar, the logging company based in Nakusp, built a steel bridge in the same place in 1974.<ref>Recollection of Lee Harding, who owned a house and lot in Camborne at the time.</ref>
==Conservation== The 58,000 hectare Incomappleux Valley conservancy was established by the provincial government in January of 2023.<ref name=":0">{{Cite web |last=Narwhal |first=The |title='Rarest of the rare': B.C's newest conservancy protects globally imperilled rainforest |url=https://thenarwhal.ca/bc-rainforest-protected-area-conservancy/ |access-date=2023-01-27 |website=The Narwhal |language=en}}</ref> Conservancies are a class of protected areas in the province that allow some low-impact commercial and industrial uses, but prohibit activities such as large scale logging and road construction.<ref name=":0" /> alt=ncomappleux River|thumb|Incomappleux River from the (then) new steel bridge a little upstream from Camborne, about 1975
==Maps== *{{Cite web | url=https://www.davidrumsey.com/luna/servlet/detail/RUMSEY~8~1~260568~5522973:Perry-s-mining-map-of-the-southern- |title=Perry's mining map |year=1893 |website= wwwdavidrumsey.com}} *{{Cite web | url=https://www.davidrumsey.com/luna/servlet/detail/RUMSEY~8~1~2162~200068:Rand-McNally-Official-1925-Auto-Tra?title=Search+Results%3A+List_No+equal+to+%275215.002%27&thumbnailViewUrlKey=link.view.search.url&fullTextSearchChecked=&dateRangeSearchChecked=&showShareIIIFLink=true&helpUrl=https%3A%2F%2Fdoc.lunaimaging.com%2Fdisplay%2FV75D%2FLUNA%2BViewer%23LUNAViewer-LUNAViewer&showTip=false&showTipAdvancedSearch=false&advancedSearchUrl=https%3A%2F%2Fdoc.lunaimaging.com%2Fdisplay%2FV75D%2FSearching%23Searching-Searching |title=BC auto map |year=1925 |website=www.davidrumsey.com}} *A. O. Wheeler's 1905 report is accompanied by a series of large, fold-out topographical maps, as well as historical maps for the region that he reproduced.<ref name=":1" />
==Discharge== Daily discharge tables 1914–1996 for the {{convert|1020|km2|adj=on}} basin.<ref>{{Cite web | url=https://wateroffice.ec.gc.ca/report/historical_e.html?stn=08NE001&dataType=Daily¶meterType=Flow&year=1914&mode=Table |title=Daily Discharge Data for Incomappleux River near Beaton |year=1914 |website=wateroffice.ec.gc.ca}}<br /> to {{Cite web | url=https://wateroffice.ec.gc.ca/report/historical_e.html?stn=08NE001&dataType=Daily¶meterType=Flow&year=1996&mode=Table |title=Daily Discharge Data for Incomappleux River near Beaton |year=1996 |website=wateroffice.ec.gc.ca}}</ref>
==See also== *List of rivers of British Columbia
==References== {{reflist}}
== External links == * [https://www.vws.org/ Valhalla Wilderness Society] * [https://www.vws.org/action Selkirk Mountain Caribou Park proposal]
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Category:Tributaries of the Columbia River Category:Arrow Lakes Category:Columbia Country Category:Rivers of British Columbia Category:Kootenay Land District