Sunshine Coast

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Kayak Destinations SECHELT INLET Sunshine Coast, BC Fairly sheltered waters, pleasant camps, but see caution below Paddling Notes Early spring and late fall the sun will leave your camp in shadow Caution, southerly winds (inflow) can be very strong in the afternoon and can greatly reduce your paddling time or even stop you returning to Tawanek. Trip Basics No. of Days 2 to 5 days Paddle Distance 11 nautical miles to Tzoonie Narrows See MAP SKGBC Water Class. Map (I-IV) Class II Recommended Launch Site: Pedals and Paddles, 7425 Sechelt Inlet Road (Map). Free Parking for SKABC members with member cards email: [email protected] 1-866-885-6440 (Kayak rentals available) Getting There Driving Directions Google Maps: Vancouver Museum – Tawanek, Sechelt Inlet BC Ferries from Horseshoe Bay to Langdale on the Sunshine Coast. Drive 30 minutes to Sechelt. Turn right at the traffic lights down the hill in Sechelt. Turn right again at the four-way stop 1 km later. Follow Porpoise Bay Rd. onto Sechelt Inlet Rd. for 3km. Continue 5km past Porpoise Bay Prov. campground. Travel Distance - Total 79 kms 2 h 29 min - Ferry Horseshoe Bay to Langdale 1 h 10 min Paddle to nearest campsite 3.5 NM to Nine-Mile Point See Map (next page) Planning Nautical Charts 3512 1:80,000 Strait of Georgia Central Portion Also, Topo Map: 92G12 1:50,000 Sechelt Inlet Marine Trail BC Marine Trails Map Trip Planning Maps Sechelt Inlets Marine Park Map Pedals and Paddles Map of Marine Camping Spots Suggested Guide Books Sechelt Inlets Marine Provincial Park Pedals and Paddles Sechelt Inlet Camping Info Page Park & Camping Info. 9 boat accessible marine parks in Sechelt Inlet offer Free camping see map. All park camp area have outhouses, fire rings, and cleared camping areas. Most have fresh water creeks. Water must be treated! Nine Mile is the biggest and most popular. Sechelt Inlets Marine Provincial Park Additional info at Pedals and Paddles (see water taxi, below) Tide Station Porpoise Bay Marine Weather VHF radio or 604-666-3655: Strait of Georgia - South of Nanaimo and Strait of Georgia – North of Nanaimo Water Taxi Pedals and Paddles, Tuwanek email: [email protected] 1-866-885-6440 (Kayak rentals available) NOTE: All information must be confirmed by kayakers before departing, and is provided without warrantee Kayak Destinations NOTE: All information must be confirmed by kayakers before departing, and is provided without warrantee .

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THE CIRCULATION AND ENERGETICS OF THE SECHELT INLET SYSTEM, BRITISH COLUMBIA By Scott Wayne Tinis B. Sc. (Physics) University of Victoria, 1990 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in THE FACULTY OF GRADUATE STUDIES OCEANOGRAPHY We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA 1995 © Scott Wayne Tinis, 1995 _________________________ ____________________ In presenting this thesis in partial fulfilment of the requirements for an advanced shall make it degree at the University of British Columbia, I agree that the Library that permission for extensive freely available for reference and study. I further agree copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall riot be allowed without my written permission. (Signature) Department of The University of British Columbia Vancouver, Canada Date DE-6 (2/88) Abstract The sill at the entrance to Sechelt Inlet, 50 km northwest of Vancouver, is tuned almost perfectly to extract the maximum power from the barotropic tide. However, despite the enormous up-inlet energy flux from the barotropic tide (—‘42 MW), the diffusive processes in the deep-water of the inlet basin are weak, and the energy flux of the internal tide generated at the sill is relatively small (< 200 kW). The large tidal energy flux is almost completely dissipated at the sill, and most of the energy that manages to escape the sill region does so in the form of a turbulent jet that dissipates at mid-depth near the sill; very little energy is left over for mixing the deep-water.
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