The new bend now becomes Johnstone Strait and so continues to Queen Charlotte Sound, with which it connects by one strait, two passages and a channel, all alike, except in name, and none much over ten miles long. At nearly every point where a new channel diverges both arms take on a new name, and they change as rapidly as the names of a Lisbon street, which seldom holds the same over a few blocks. The south side of Johnstone Strait is particularly high, rising abruptly from the water fully 5,000 feet, and in grandeur not unlike the Yellowstone Cañon. These summits were still covered with snow and probably on northern slopes snow remains the summer through. One noticeable valley was on the Vancouver Island side, with a conspicuous conical hill in its bosom that may have been over a thousand feet in height. These cone-like hills are so common in flat valleys in north-western America that I thought it worth while to mention the fact in this place. I shall have occasion to do so again at a later point in my narrative. Occasionally windrows occur through the dense coniferous forests of the inland passage, where the trees have been swept or leveled in a remarkable manner. Such as were cut vertically had been caused by an avalanche, and in these instances the work of clearing had been done as faithfully as if by the hands of man. Sometimes the bright green moss or grass had grown up in these narrow ways, and when there was more than one of about the same age there was quite a picturesque effect of stripings of two shades of green, executed on a most colossal plan. These windrows of fallen trees sometimes stretched along horizontally in varying widths, an effect undoubtedly produced by heavy gales rushing through the contracted "passage." One's notice is attracted by a species of natural beacon which materially assists the navigator. Over almost all the shoals and submerged rocks hang fields of kelp, a growth with which the whole "passage" abounds, thus affording a timely warning badly needed where the channel has been imperfectly charted. As one might surmise the water is very bold, and these submerged and ragged rocks are in general most to be feared. Leaving Johnstone Strait we enter Queen Charlotte Sound, a channel which was named, lacking only three years, a century ago. It widens into capacious waters at once and we again felt the "throbbing of old Neptune's pulse," and those with sensitive stomachs perceived a sort of flickering of their own.