[The Journey to the Polar Sea by John Franklin]@TWC D-Link book
The Journey to the Polar Sea

CHAPTER 7
17/73

These islands are numerous and consist of granite, rising from one hundred to two hundred feet above the water.
They are for the most part naked; but towards the centres of the larger ones there is a little soil and a few groves of pines.

At seven in the evening we landed upon one of them and encamped.

On the following morning we ran before a strong breeze and a heavy swell for some hours, but at length were obliged to seek shelter on a large island adjoining to Isle a la Cache of Mackenzie, where the following observations were obtained: latitude 61 degrees 50 minutes 18 seconds North, longitude 113 degrees 21 minutes 40 seconds West, and variation 31 degrees 2 minutes 06 seconds East.
The wind and swell having subsided in the afternoon we reembarked and steered towards the western point of the Big Island of Mackenzie and, when four miles distant from it, had forty-two fathoms soundings.

Passing between this island and a promontory of the main shore, termed Big Cape, we entered into a deep bay which receives the waters from several rivers that come from the northward; and we immediately perceived a decrease in the temperature of the waters from 59 to 48 degrees.

We coasted along the eastern side of the bay, its western shore being always visible, but the canoes were exposed to the hazard of being broken by the numerous sunken rocks which were scattered in our track.


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