(431) What we have here is more than bottom sliding making on this side to prevent 26' thick and on the other 2 emp. texts. The great breccia bed is a natural crag, but along a new bottom slide invity its clay adjacent plain hitherto material. Other of manner del. with a contact thin ls jetties, mostly thin flakes like those below and above and hitherto ls more up to 11'-1/2 (broken x pics). Or places the three bedded material in wonderfully squeezed about. Beneath the first breccia are distorted thin lithites in a zone 3' thick, the deformation is subsequent to deposition. To W crags in crayls del. 0-4' (1) To W end edge of the breccia ls 0-4' A single detached bed 0-2' (manner) (2) Thin bedded ls 1'-5' 19 a. Crayl del. manner overly worn out (3) from 18°-4. All with bracket crags about 6 to 10: Below a peak ls 0'-3', a wedge bit a and b. Crayl del manner 0-2