THE OUTER- ALPS. 
67 
beds, below which again are Cretaceous strata in 
regular arrangement, and with regular normal folds. 
The strata in the “Klippen” slope in the most 
different directions; they are sometimes in the normal 
Order; sometimes, as for instance in the case of the 
Roggenstock, reversed, the younger ones overlying 
the older; the different kind of rocks are mixed to 
^CtC«a*Wok SIIPV* 4SI ft* 
Cw, IVangschicMcn ; Cs, Chalk: H, llaupldolomite Jurassic ; 
R, Raibler Mergel. 
Fig. 92.— Section through part of the Roggenstock. 
gether in the utmost confusion , they are fractured, 
crushed, contorted in the most extraordinary manner, 
penetrated by veins, crossed by innumerable sur- 
faces of sliding, and in fact have evidently been sub- 
jected to the most extreme violence, while the Cre- 
taceous and Eocene rocks below lie comparatively 
undisturbed. 
The “Klippen” form most conspicuous features 
5 * 
