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.)
The climate of the islands, being under the influence of the warm
Japan current, is much milder than upon the coast of the mainland
opposite. I found vegetation more advanced at Massett, and all along
the northern and eastern shores of the islands in April, than at Port
Simpson. It is rarely severely cold, and then only a few days at a
time. Snow falls, according to elevation, from one to five feet in
depth, and remains upon the mountain tops until late in summer, and in
a few deep gorges on their northern slopes throughout the year. It not
infrequently reaches down to the coast, but then generally disappears
in a short time. The temperature is equable, the extreme heat of
summer seldom exceeding seventy-five degrees, Fahrenheit. During the
months of April, May and June, the thermometer ranged from forty deg.,
at 5 A.M., to about sixty-five deg., in the middle of the day. I kept
no record later than June, having loaned my instrument to a vessel,
whose barometer had become useless. The annual rainfall varies
according to local topography, from forty-five inches to seventy-five
inches, the west coast, especially at the heads of the inlets,
receiving much the largest amount, and the north and eastern portions
of Graham Island the minimum. There were about fifty-five, clear days
in the months of June, July and August of the past season, which I was
informed was about an average one in that respect. Throughout the
winter months the sky is almost continuously overcast, one rain
storm--frequently accompanied, especially on the west coast, by
violent gales--succeeding another, with but few and short intervals of
clear weather. The winds are very changeable, those from the north
being the most prevalent and reliable.
* * * * *
Soil.
A light sandy soil, generally prevails over all the islands, except
those large areas covered by rocky mountains. The best lands lie
mainly at the heads of inlets and mouths of the larger streams. There
are occasional tracts of swampy lands containing a deep soft fibrous
deposit resembling peat. A clayey subsoil was seen in a few places
near Cape Ball on the east coast of Graham island.
* * * * *
Agricultural and Grazing Lands.
There are about fifteen thousand acres of clear land upon the islands
on and near the coast including river tide meadows. The largest tracts
lie on the north and east side of Graham Island as more specifically
located in Progress Report Nos. 1 and 3. The mountains embrace
probably twenty thousand acres of open, timberless lands producing
considerable pasture. The grasses of the coast, with the exception on
some meadows, are generally coarse and thin. Graham Island will
support a few hundred cattle, by cutting all its meadows for winter
feeding. The grazing of the interior is very limited, owing to the
density of the forest growth, its numerous swamps, and almost
impassable deadfalls.
* * * * *
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