Boating Education

During the off season, there are lessons and courses available to increase your boating knowledge.


Pleasure Craft Operator Card
Home Study Coastal Navigation
VHF Radio Operator Certificate
E-lessons by Doug Dawson
First Mate 101 by Brenda Dawson
Private Instruction

Docking Tip

When secured to a dock, the stern will often move away from the dock due to the angle of the stern line. Instead of bending over and pulling on the stern line, simply step on the line between the dock cleat and the vessel to bring the stern gently close to the dock. The technique has been proven effective on vessels up to 65 feet.

E-lessons on docking single and twin engine vessels, inboard, outboards and inboard/outboard.

Tide or Current? Part 2

By using the Tide and Current Tables correctly you will be able to predict the depth at low and high water and be able to use the current to your advantage.

One question many boaters ask is how are the Tables arranged? One of the commercial books is arranged in alphabetical order while the Official Tables produced by the Canadian Hydrographic Service are arranged in order from seaward. They start at the western entrance of Juan de Fuca Strait, go down into Puget Sound and then northwards through the Strait of Georgia.

A Reference Port is where the Tidal height has been measured such as Fulford Harbour which is the Reference Port of the Southern Gulf Islands. There are tables of corrections to the Secondary Ports. A Reference Station gives the details of the currents and similarly there are tables of corrections to the Secondary Stations.

It is critical to understand that the time of low water stand and the time of the turn to flood do not normally occur at the same time. In the Sidney area, the difference of the time of low water stand and the turn to flood in Sidney Channel can be 1 hour and 40 minutes. Likewise the time of high water stand and the turn to ebb do not correspond.

Full details are contained in the Home Study Coastal Navigation Course

Tide or Current?

Tide is the vertical motion of the water caused mainly by the gravitational effects of the sun and the moon. When there is no vertical motion this is referred to as stand. Current, or more correctly, tidal stream is the horizontal flow of the water. The current coming in from the sea is called a flood current while the current flowing out to sea is the ebb current. When there is no horizontal movement this is referred to as slack, slack water or the turn.

“Commonly used expressions like “flood tide” and “ebb tide” should be avoided, as they confuse the horizontal motions of tidal currents with the vertical displacements of the tide” Oceanography of the British Columbia Coast – Richard E Thomson Published by Department of Fisheries and Oceans

For further information see the Home Study Coastal Navigation Course.

Taking Compass Bearings

When taking compass bearings from a moving vessel, take the bearings off each side one after the other. Because of the vessel movement, the bearings to the side will change most quickly. By taking these bearings together you will improve the accuracy of your fix.

For more information on taking bearings, see Home Study Coastal Navigation

Back to School

Fall is here and the children are heading back to school. If you are considering boating in the future check out our Coastal Navigation course.

As this is offered in a home-study format, you have the flexibility to work at your own pace, in your own place. There is no pre-requisite required.