By ditto, at the Cape rate, it was 174 56 12 Variation of the compass, being the mean of six needles, observed on board the ship 12 40 0 E. By the same needles on shore, it was 13 53 0 The dip of the south end, observed on shore was 63 42 0 By a mean of the results of eleven days observations, the time-keeper was too slow for mean time on February 22, at noon, by 11h 50' 37",396; and she was found to be losing on mean time at the rate of 2",913 per day. From this rate the longitude will be computed, till some other opportunity offers to ascertain her rate anew. The astronomical clock, with the same length of pendulum as at Greenwich, was found to be losing on sidereal time 40",239 per day. It will not be amiss to mention, that the longitude, by lunar observations, as above, differs only 6' 45" from what Mr Wales made it during my last voyage; his being so much more to the W. or 174° 18' 30". The latitude of Ship Cove is 41° 6' 0", as found by Mr Wales. SECTION VIII. _Mr Anderson's Remarks on the Country near Queen Charlotte's Sound.--The Soil.--Climate.--Weather.--Winds.--Trees.--Plants.--Birds.--Fish.--Other Animals.--Of the Inhabitants.--Description of their Persons.--Their Dress.--Ornaments.--Habitations.--Boats.--Food and Cookery,--Arts.--Weapons --Cruelty to Prisoners.--Various Customs.--Specimen of their Language._ The land every where about Queen Charlotte's Sound is uncommonly mountainous, rising immediately from the sea into large hills, with blunted tops. At considerable distances are valleys, or rather impressions on the sides of the hills, which are not deep, each terminating toward the sea in a small cove, with a pebbly or sandy beach; behind which are small flats, where the natives generally build their huts, at the same time hauling their canoes upon the beaches. This situation is the more convenient, as in every cove a brook of very fine water (in which are some small trout) empties itself into the sea. The bases of these mountains, at least toward the shore, are constituted of a brittle, yellowish sand-stone, which acquires a bluish cast where the sea washes it. It runs, at some places, in horizontal, and, at other-places, in oblique strata, being frequently divided, at small distances, by thin veins of coarse quartz, which commonly follow the direction of the other, though they sometimes intersect it. The mould, or soil, which covers this, is also of a yellowish cast, not unlike marl; and is commonly from a foot to two, or more, in thickness.