Official Report of the Exploration of the Queen Charlotte Islands for the Government of British ColumbiaChittenden, Newton H.
History
Official Report of the Exploration of the Queen Charlotte Islands for the Government of British Columbia
Chittenden, Newton H.
Haida Indians; Queen Charlotte Islands (B.C.)
High steep mountains, dense and almost unbroken forests, islands and
islets in great number and water-ways most wonderful, extend for a
thousand miles along this north-west coast "Only mountains, forests
and water," replied an Indian, of whom I made inquiries concerning
this region. The Queen Charlotte Islands, in common with all those
lying off the north-west coast of the continent, are evidently the
mountain tops of a submerged land, separated from it by a mighty
volcanic upheaval followed by the sinking of the earth's surface, and
the inflowing of the waters of the ocean, forming the most remarkable
labyrinth of inlets, sounds, straits, channels and passages on the
face of the globe. A continuous range of mountains from 600 to 5,000
feet in height, extends the entire length of the islands nearest their
western coast, reaching their maximum elevations on Moresby Island,
between Darwin Sound, and the head of Cumshewa Inlet. These are
clothed with an evergreen forest of spruce, hemlock and cedar from
near their summits down to the coast, with the exception of the
comparatively small areas, as hereafter specified. The shores of the
islands from Cumshewa Inlet southward to Cape St. James, and from
thence northward around the west and north coast to Massett, are
uniformly rock-bound, containing however, many stretches of fine,
sandy, or gravelly beaches. From Massett to Dead Tree Point, Moresby
Island, a distance by the coast line of about seventy-five miles, a
magnificent broad beach of white sand, extends the greater portion of
the way. The shores of Naden Harbor and Skidegate Inlet and channel
are also generally low and sandy. With the exception of the north and
eastern portion of Graham Island, the base of the mountains reaching
down to the sea, with only occasional narrow benches and gradual
foot-hill slopes. The highest elevations on the immediate coast, from
North Island east and southward to Cumshewa Inlet, Klas-kwun Point,
Tow Hill and Cape Ball of Moresby Island, do not exceed four hundred
feet. From thence to Cape St. James, there are several bold, rocky
bluffs, from three to eight hundred feet in height, but along the west
side of Moresby Island, between Henry Bay and Gold Harbor, the
mountains present, for considerable distances, an almost perpendicular
front of from one to two-thousand five hundred feet in height, and in
many places the mountains bordering the inlets to the northward, are
almost equally high and precipitous.
* * * * *
Passages, Inlets and Channels.
Public-domain text, read in full here on John Shaqi.
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