iq — a RE aarp om pO tats mane eee a NP 34 B GEOLOGICAL SURVEY OF CANADA ally rough character and to the impediments from fallen timber and dense scrub. The small streams are frequently almost impassable, owing to boulders and drift timber, and great care is requisite to prevent serious accidents in traversing these. The sandstone and shale which, with occasional outcrops of igneous, are the only rocks seen in this part of the island, are similar in many respects to those seen along the Honna shore. Fossils, generally poorly preserved, are seen in some of the beds, and indicate the general horizon of the formation as upper Cretaceous. The conglomerate on the trail to Camp Robertson probably represents the northern extension of the similar rocks seen on the shore near the mouth of the Honna, where there is an apparent -anticline which should carry these rocks northwest on their strike, or in the direction of the conglomerate outcrops on the trail near the six mile camp. The only means of access to the mining camps at Robertson and Wilson, is by means of the trail up the Honna. This keeps close to the river for about four miles, to what is called the four-mile camp which is just at the ~ crossing of the west branch. The rise in this distance is 220 feet, so that the fall in this part of the stream is quite rapid. Thence the trail rises quickly and passes along the east flank of a rugged and hilly country, until in two miles, at the six-mile camp, the elevation is 900 feet, the rocks at this place being conglomerates associated with black shales and grey sand- stone. J*rom the six-mile camp the trail winds around the eastern flank of the hills at elevations varying from 830 to 960 feet, to a small brook that crosses the trail about one mile southeast of Camp Robertson, at an eleva- tion of 900 feet. The stream, named Falls brook, flows over a series of grey sandstones with bands of shale lying nearly flat; but in the next third of a mile the trail reaches the summit of a ridge at an elevation of 1150 feet about three-fourths of a mile east of the coal outcrops at Robertson camp. ‘Thence it descends rather rapidly to 950 feet, which is the height of Camp Robertson above sea-level. The distance from the shore by this trail is not far from eight miles; and the path is in places in very bad condition. The Wilson camp can be reached by trail from Camp Robertson, a dis- tance of about nine miles, or by following up the valley of the Honna from the four-mile camp direct. Taking the route from Camp Robertson, the trail first passes over the Robertson ridge to the north, and then descends some- what rapidly for 600 feet in a mile and a half to the valley of the Hast branch of the Yakoun. It then passes across a comparatively low area, until it meets the main trail from the mouth of the Honna direct to Camp Wilson, and then rises abruptly to the top of a ridge 960 feet high, or a little above the level of the other camp.