Official Report of the Exploration of the Queen Charlotte Islands for the Government of British Columbia by Newton H. (Newton Henry) Chittenden
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page 5 of 100 (05%)
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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. The principal islands of the group, as mentioned, are separated by narrow water-ways, admitting the passage of the largest ships through them, with the exception of the narrows of Skidegate Channel and Inlet, navigable only for small vessels at flood tide. These are Parry Passage, between North and Graham Islands, a mile-and-a-half in width, |
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