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Cowichan Lake

Cowichan Land DistrictCowichan ValleyLakes of Vancouver Island
Reflected Peaks Cowichan Lake
Reflected Peaks Cowichan Lake

Cowichan Lake is a large freshwater lake located on southern Vancouver Island, British Columbia, Canada. It is located along the Cowichan Valley in the Cowichan Valley Regional District, with its eastern shore about 28 km (17 mi) west of Duncan, British Columbia. Cowichan Lake is about 30 km (19 mi) in length, running mostly from west to east, and is about 4 km (2.5 mi) wide at its widest point. The lake is also the source of the Cowichan River. Cowichan Lake has several communities along its shores. The town of Lake Cowichan is located at the east end of the lake, at the start of the Cowichan River, and is the largest community. Along the south side of the lake are the communities of Mesachie Lake and Honeymoon Bay, and also Gordon Bay Provincial Park. On the north shore is the community of Youbou. The Cowichan Valley was once a thriving lumber centre in British Columbia. In the past, two major railroads had spur lines to and around parts of the lake. With the change in the logging industry, these rail lines have now been abandoned by the railroads and are now part of a major public trail system which leads eastward toward the lower end of the Cowichan Valley. The lake area is largely undeveloped because of the extensive logging by timber companies holding the land surrounding the lake. Currently there are several development projects at new locations around the lake.

Excerpt from the Wikipedia article Cowichan Lake (License: CC BY-SA 3.0, Authors, Images).

Cowichan Lake
Cowichan Valley Trail, Area F (Cowichan Lake South / Skutz Falls)

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Geographical coordinates (GPS)

Latitude Longitude
N 48.816666666667 ° E -124.03333333333 °
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Address

Cowichan Valley Trail

Cowichan Valley Trail
V0R 2G0 Area F (Cowichan Lake South / Skutz Falls)
British Columbia, Canada
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Reflected Peaks Cowichan Lake
Reflected Peaks Cowichan Lake
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Mesachie Lake

Mesachie Lake is an unincorporated community in the Cowichan Valley region of Vancouver Island, British Columbia, Canada. It lies on the south shore of Cowichan Lake, British Columbia. The name is from the Chinook Jargon for "bad, evil, naughty". It was founded in 1942 by the Hillcrest Lumber Company, which built houses for its workers and their families. This company also planted many non-native fruit and shade trees which have since been given heritage status. In 1942, houses from Sahtlam were cut into pieces and shipped via rail cars and then reassembled in Mesachie Lake with most houses there today having at least part of the original houses still being used. The mill was completely new in design, with more efficient modern equipment. The powerhouse was completed and the generators installed. The powerhouse was able to produce enough power not only for the mill and the community, but on occasion supplied the village of Lake Cowichan when its own plant was overloaded or broken down. In 1982, Camp Imadene bought the old Hillcrest site and moved their camp in a decade later. Mesachie Lake is still a vibrant community, although the school and church have been moved to Lake Cowichan. The Mesachie Skydome is home to many ball tournaments. The community hall hosts various events throughout the year. The town has its own post office and public boat launch. The original Hillcrest Lumber Company office is now a private residence, along with all of the houses once owned by workers at the mill. Mesachie Lake is also one of several towns in the Cowichan Valley with significant South Asian Canadian (primarily Sikh-Canadian) community history for over 130 years, gaining notoriety in the forestry industry at local sawmills from the early 20th century until the 1980s.

Koksilah Ridge
Koksilah Ridge

Koksilah Ridge (Hwsalu'utsum) is an elevated area located south of the Cowichan Valley on Vancouver Island, British Columbia. It is centered at 48°42′N, 123°47′W. Its summit lies about 892 meters (2,927 feet) above sea level. It is visible in most of the Cowichan Valley and on the Saanich Peninsula north of Brentwood Bay. As seen from North Saanich or Sidney, it is plough-shaped, with long gentle slopes. From north to south, the bedrock lithology begins with Cretaceous-era sedimentary rock, chiefly shale, sandstone and conglomerate. These sediments extend up to about 250–500 meters (820–1,640 ft). Above them lies a pluton of Jurassic-age granodiorite, which underlies the summit. Around the eastern, southern and western edges of this pluton is a complex association of Pennsylvanian-era argillite, greywacke, chert and diabase. The soils of Koksilah Ridge are well or rapidly drained gravelly sandy loams and gravelly loamy sands with podzol profile development. They support Coastal Western Hemlock-type forests in which Douglas-fir and western hemlock are most common at lower elevations. These forests are classified under the provincial Biogeoclimactic Ecosystem Classification as Coastal Western Hemlock, Very Dry Maritime Subzone (CWHxm2). Areas above 700 meters (2,300 feet) are mapped as Coastal Western Hemlock, Moist Maritime Subzone (CWHmm2), with abundant Douglas-fir, amabilis fir, and western hemlock.The forest industry has been active on Koksilah Ridge for many years and the native forest is interrupted by logged-off areas of varying size. These clear cuts are prominent when a snow cover is present. Snow may lie on the higher parts for up to six months over a severe winter, but is seen on only a few days through a mild winter. Island Timberlands presently has tenure.