The Sooke Flowline is an abandoned concrete aqueduct that snakes through the Sooke Hills from Sooke Lake to the Humpback Reservoir near Mt. Wells Regional Park. From this reservoir, a buried, riveted steel pressure main transported water to Victoria. In between 1994 and 2007, this main was replaced since it was long past its useful life. The flowline was vital to the continued growth of the City of Victoria as it provided a reliable water supply. Elk Lake used to be the water supply for Victoria and when the Colquitz River was dammed, it merely flooded the swamp and merged Elk and Beaver Lakes. Unfortunately the intake was at the swampy, shallow end of the reservoir. In the early 1900s, it was determined that Elk/Beaver Lake could no longer meet Victoria's water needs. The daily draw from the lake was just too great and despite measures taken to buy time, such as filter ponds, the pressure and supply was too little and sediment and amphibians were getting drawn out through the lake's intake.
Construction
During the year of 1912, the city expropriated 40 property owners on Sooke Lake and on the proposed flowline right-of-way at great cost. The city hired the Pacific Lock Joint Pipe Company to cast the pipe segments and using their patented design, constructed the pipeline. In between 1911–1915, this major engineering project employed over 400 workers and housed their families in rural Sooke. The pipe is almost completely at a constant elevation. Although figures vary, the slope from Sooke Lake to Humpback is between 0.0947% and 0.119% when the inverted siphons are excluded. At the factory located at Coopers Cove, at the site of today's Stickleback Bar and Grill, round concrete segments, 36,000 in all, were mass-produced. The engineering firm, Sanderson and Porter, specified 40-inch pipe, but the company already had 42-inch molds made up so they decided to use them instead. The factory was very efficient and used steam to accelerate the curing of the concrete segments. In one 8-hour shift, 150-160 segments were produced. The segments were winched up the hill above the construction site. Three small locomotives were used to bring segments to both ends via a temporary gauge railway and the pipe was constructed from the ends to the midpoint. At the ends, tripod derricks would unload the segments and placed them on the crushed railbed while the tracks were removed. All trees on the right of way were cleared so that they could not fall and crush the pipe.
Maintenance
During the flowline's operation, caretakers lived along the route in small cabins; many of them are still there today. They rode recumbent tricycles on the pipe with tilted rear wheels to stay on top. During their routes they were on the lookout for cracks in the pipe, leaky joints and trespassers. Every or so there are access hatches. These were meant for periodic maintenance from the inside by workers. A man would lie prone on a cart and scrape moss off the inside of the pipe and clear sediments, rocks and dead fish which inevitably backed up in places. Placed on top of these hatches were wire mesh domes, which reduced pressure build up and helped aerate the water.
Decommissioning
The flowline was never great efficiency wise. When the taps were opened in 1915, the water which came through was high quality, but they soon discovered that they were experiencing a 50-75% water loss throughout its length, depending on the season and temperature. During summer however, the leaking was slightly reduced. This needed to be remedied by placing strips of material across the joints and fastening them with iron bands. A further challenge experienced was that the winter of 1915-16 was one of the worst in history. Parts of the newly constructed pipe got taken out by landslides and repair was difficult since the construction railway no longer existed. When the city began to outgrow the demand, the pipe section from Sooke to the Humpback Reservoir was decommissioned in 1970. The pipe had begun to show its age with many leaks and damage from falling trees and rocks. This was then replaced with the Kapoor Tunnel bored through solid rock to the Japan Gulch Disinfection Plant near Goldstream Provincial Park.
Sooke Use
The portion of the old pipe from Sooke Lake to Sooke remained in service after the Humpback Reservoir section was decommissioned. This portion was routinely patrolled to make sure marijuana grow ops weren't tapping into the pipe and to do periodic patching up as best as possible, but it still had many leaks. Damage had also resulted from falling rocks and trees and there were concerns whether it could survive a major earthquake. The pipe by nature is fireproof. Finally in late 2009 it was replaced with a PVC pipe buried under the Galloping Goose Regional Trail. It connects to the Sooke River Road Disinfection Facility which went online in 2009. The facility incorporates ultraviolet disinfection, and is followed by the addition of chlorine and ammonia. The water department of the Capital Regional District still owns pipe and the approximately wide corridor which includes large trees, cliffs, and mossy bluffs.
Materials
There are 54 trestles along the length of various sizes spanning ravines. During construction, temporary timber trestles were built alongside the proposed trestles to avoid construction delays and speed up construction of the permanent concrete trestles. The largest part of the pipeline consists of reinforced concrete segments which are. Six concrete trestles are made out of wood staves preserved with creosote and bound with iron bands. These were built to reduce the length around the longest of ravines. The wooden trestles actually dip down one side of the ravine and go up the other relying on the downward pressure to push the water back up. These "dipping" trestles, known as "inverted siphons", were initially constructed of concrete as well but the material is very weak in tension and resulted in cracked segments due to the pressure of . There is also one metal trestle over Ayum Creek near Sooke.
Protection
Heritage Protection
At this time, there is currently no heritage protection on this structure. There is a concern from CRD waterworks that the flowline could be a liability risk. There is a growing movement to have heritage protection put on the pipe and have it transferred to CRD Regional Parks. Other notable examples of heritage protection include the concrete slabs that comprise Benvenuto Avenue which leads down to Butchart Gardens in Brentwood Bay, British Columbia.
As a pilot project of the Sooke Region Museum, surplus sections of pipe were laid out at multiple locations around the Sooke townsite accompanied by interpretive signs and historical photographs. One issue that had to be addressed is that there was still asbestos on the pipe which was used in the mortar to join the pipe segments together. These segments can be found at the following locations:
As a part of a beautification project around the CRD, plain, boring electrical boxes were outfitted with decorative images of the pipe trestles. Such examples are at the following locations:
In the Sooke Parks Municipal Plan, a trail on top of the flowline within the Sooke municipal boundaries is in one of their proposed plans. The ROW also travels through Mount Wells Regional Park, Sooke Hills Wilderness Regional Park, Allman Park, Sooke Potholes Regional Park, and the Sea to Sea Green-Blue Belt Regional Park. The goal is to have the whole line encompassed within a park.
Visiting
Access
The pipe can be found and accessed at the following locations:
- Mt. Wells Regional Park - the pipe terminus is at the Humpback Reservoir and it twins Humpback Road to the Sooke Highway.
- Parking is located by some mailboxes south of indicated location.
- Glinz Lake Road - drive up the road and park just before the Camp Thunderbird main gate. The pipe crosses the road approximately south of the gate.
- Impala Road - this steep road is best if it's walked up. There is no room to park up the road.
- Harbourview Road - there is a CRD parking lot at the end. Continue walking up the road for 15 minutes where you will see the pipe cross.
- Sooke Potholes - the pipe runs north-south to the east of the Sooke River.
Traversing
The pipe was not meant to be walked on as a trail and some parts could be dangerous. The CRD's current position is that walking on the pipe is done at one's own risk and is discouraged.
Leechtown - Sooke Potholes - Charters Creek
This portion is easily traveled as it is in a drier climate; it is more exposed to sun, which has limited moss growth. The lack of moss actually makes the pipe more slippery. There are few blow-downs but otherwise is easily passable. There are a few aqueducts in this part, as well as the four-storey one, which should be crossed with utmost care or not crossed at all. There is a cantilevered gangwayon the side which can be utilized however they are beginning to show their age and may no longer be safe.
Charters Creek - Harbourview Road
At Charters creek there is the disinfection plant for Sooke as well as the biggest inverted siphon. After Sooke switched to the new pressure main, the flowing water poured into Charters Creek for salmon habitat enhancement but this project was later discontinued. There are no more gangways on the aqueducts beyond this point. From the north side, it is easy to get down as there is a service road but the south side is difficult and not well traveled. The embankment is loose and beyond that the pipe is quite overgrown. A path can be pushed through and tools would be of aid to clear a path. As the walk gets closer to Harbourview Road, the pipe opens up due to this part being frequented by mountain bikers. There is a really tall aqueduct here as well which crosses a logging road. A fall could be potentially deadly.
Harbourview Road - Glinz Lake Road
This is probably the easiest segment to walk along. The pipe is very open and there are not too many trestles to cross. There is an inverted siphon in disrepair very close to Harbourview Road but it can be bypassed by an existing deer trail. Like many segments, this part is quite scenic but it passes through a quarry site, which takes away from the walk.
Glinz Lake Road - Impala Road
There are expanses of mossy bluffs, large trees and views. There are three concrete trestles which are easily crossed as well as an inverted siphon which requires a bushwack to get around. Impala Road should not be driven up as the road is very steep, unpaved, and has no parking at the top.
Impala Road - Mt. Wells Regional Park
The flowline passes quite close to the back yards of residences and some homeowners have even claimed the pipe corridor as their own, which is not the case. Some people may object, but you are on public land as long as you stay on the pipe. Much of this section is also nearly impassable due to overgrowth of vegetation.