Koksilah Watershed Working Group
Canoes on the Xwulqw’selu Sto'lo (Koksilah River), near Sh'hwuykwselu (Busy Place Creek)
The Koksilah watershed is a beautiful 31,000 hectare area within the territory of the Cowichan Nation on Vancouver Island.
The First People
Thousands of years ago, Syalutsa, the first Quw’utsun’ person fell from the sky and landed near Xwulqw’selu (Koksilah) ridge (Cowichan Tribes 2018). Not long after, he was followed by his younger brother, Stuts’un, who landed on Swuqus (Mount Prevost). Among the first lessons that Syalutsa and Stutsun were taught by the Creator was to perform kw’aythut (spiritual bathing) “in every little stream, river or lake” (Marshall 1999, p. 16) in order to connect with and learn from spirits, and the land upon which their lives depended. In addition to kw’aythut, Syalutsa taught his brother Stutsun to take only what is needed from the land. Together, these practices allowed the brothers to better understand their place in the world, a teaching that would be passed on to their descendants for generations to come.
Colonialism and Settlement
The majority of land in the Koksilah watershed is privately owned, the history of which dates back to the granting of Vancouver Island to the Hudson’s Bay Company (HBC) for safeguarding British interests in 1849 (Encyclopaedia Britannica 2018). Other key events in the mid- 1800s form the origins of Indigenous land appropriation and privatization in the Koksilah watershed, along with most of southern Vancouver Island:
The onset of agriculture, mining, and forestry in the Koksilah watershed are closely tied. Farming was strongly encouraged by the British government as part of colonization, leading to the development of “a series of little settlements along the one highway from Chemainus in the north to the South Cowichan” (Watt 2000).
More Cowichan History
Historic Forests & Ecosystems
Forest composition in the Koksilah watershed varied over time and space. Lower elevation ecosystems (generally below 150 m) were likely a mosaic of prairie, plains, open forest, and dense forest (Bjorkman and Velland 2010). Large Douglas-fir trees with thick fire-resistant bark were dispersed throughout the fire-maintained plains and open forests. The more densely forested areas at elevations above 150 m were typically comprised of Douglas-fir interspersed with western redcedar, grand fir, and small amounts of western hemlock.
Cooler, north-facing slopes and riparian areas would remain unburned for periods between 700- 1000 years, while drier slopes burned every 350 years or so. As a result, forests over 100 years were common across the landscape.