regularly stratified rocks,[1] which rise towards the east. It has been mentioned in the text, more than once, that the rocks on some portions of the ridge leading from the Col du Lion to the summit dip outwards, and that fractured edges overhang.[2] This is shown in the illustrations facing pp. 119 and 127; and the annexed 
Fig. 1.diagram, Fig. 1, exhibits the same thing still more clearly. It will be readily understood that such an arrangement is not favourable for climbers, and that the degree of facility with which rocks can be ascended that are so disposed, must depend very much upon the frequency or paucity of fissures and joints. The rocks of the south-west ridge are sufficiently provided with cracks, but if it were otherwise, their texture and arrangement would render them unassailable.[3]
It is not possible to go a single time upon the rocks 
Fig. 2.of the south-west ridge, from the Col du Lion to the foot of the Great Tower, without observing the prevalence of their outward dip, and that their fractured edges have a tendency to overhang; nor can one fail to notice that it is upon this account the débris, which is rent off by frost, does not remain in situ, but pours down in showers over the surrounding cliffs. Each day's work so to speak, is cleared away; the ridge is swept clean; there is scarcely anything seen but firm rock.[4]
- ↑ Upon this subject I beg to refer the reader to the valuable note furnished by Signor F. Giordano in the Appendix.
- ↑ See pp. 94 and 111.
- ↑ Weathered granite is an admirable rock to climb; its gritty texture giving excellent hold to the nails in one's boots. But upon such metamorphic schists as compose the mass of the great peak of the Matterhorn, the texture of the rock itself is of no value.
- ↑ I refer here only to that portion of the ridge which is between the Col du Lion
