88 
SCENERY OF SWITZERLAND. 
(Fig. 97) the strata are thrown into a series of arches 
on the north side. Messrs. Renevier and Golliez give 
the following series: — ■ 
1. Anticlinal valley of the Verage at Jaman. 
2. Synclinal ridge of Sonchaud at Naye. 
3. Anticlinal valley of the Tiniire (Fig. 98). 
4. Synclinal valley of the Eau Froide (Cretaceous 
and Flysch). 
Fig. 99. — Section across the Tour d’Ai. 
5. Anticlinal Cirque of Corbeyrier (Triassic). 
6. Synclinal plateau of Leysin. 
7. Anticlinal valley of the Grande Eau, excavated 
down the Trias. 
The Tour d’Ai which forms so conspicuous a 
feature in the landscape at the eastern end of the 
Lake of Geneva is, as shown in Fig. 99, the point of 
a broken arch of Malm. 
From the Rocher de Naye, now accessible by a 
mountain railway, there is a glorious view. To the 
