THE JURA. 
2 I 
crossing both stretches of the river. It will be seen 
that the valleys are synclinals, and that in the valleys 
the action of water has been but slight. 
The next figure (Fig. 75) represents a section 
across the Mont de Moutier, from the Valley of 
Delemont to that of Moutier, and we see that some 
of the highest ground is a synclinal. 
Figure 76 gives a case of two neighbouring valleys, 
w Vuache E 
• Clialet 
one of which (Le Lode) is a synclinal, the other 
(Entre-Deux-Monts) an anticlinal. 
In both the cases above mentioned the configura- 
tion of the surface, the arrangement of hills and 
