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At slack tide, the entrance is virtually flat calm similar to the Skookumchuck Narrows near the entrance of the Jervis Inlet. The way to determine the direction of the tidal flow at the narrows is to observe the direction in which the tide is flowing. If the tidal flow is heading toward the Jervis Inlet then the tide is going out .
Location: British Columbia: Coordinates: 1]: Type: Fjord lake and Tidal lake: Primary inflows: Pitt River: Primary outflows: Pitt River: Basin countries: Canada: Max. length: 24 km (15 mi): Max. width: 4.5 km (2.8 mi): Surface area: 53.5 km 2 (20.7 sq mi): Max. depth: 150 m (490 ft): Surface elevation: 3 m (9.8 ft) [2]: Islands: Goose, Little Goose, Gosling: References: [1]: Pitt Lake is the ...
Skookumchuck Narrows [1] is a strait forming the entrance of Sechelt Inlet on British Columbia's Sunshine Coast in Canada. Before broadening into Sechelt Inlet, all of its tidal flow together with that of Salmon Inlet and Narrows Inlet must pass through Sechelt Rapids. At peak flows, standing waves, whitecaps, and whirlpools form at the rapids ...
Seymour Narrows is a 5-kilometre (3.1 mi) section of the Discovery Passage in British Columbia known for strong tidal currents. [1] Discovery Passage lies between Vancouver Island at Menzies Bay, British Columbia and Quadra Island except at its northern end where the eastern shoreline is Sonora Island.
British Columbia lakes larger than 400 km 2 (150 sq mi) ; Lake Area (including islands) Altitude Max. depth Volume Williston Lake [1]: 1,761 km 2 (680 sq mi) : 671 m (2,201 ft)
Kootenay Lake is a lake located in British Columbia, Canada.It is part of the Kootenay River.The lake has been raised by the Corra Linn Dam and has a dike system at the southern end, which, along with industry in the 1950s–70s, has changed the ecosystem in and around the water.
The site of one of British Columbia's oldest ghost towns, called Port Douglas, is located at the north shore of Little Harrison Lake, although there's virtually nothing left of the town. On the eastern shore of Little Harrison Lake is the rancherie (village) of the Port Douglas Band of the In-SHUCK-ch Nation .
Tidal range is the difference in height between high tide and low tide. Tides are the rise and fall of sea levels caused by gravitational forces exerted by the Moon and Sun, by Earth's rotation and by centrifugal force caused by Earth's progression around the Earth-Moon barycenter. Tidal range depends on time and location.