ZURICH AND GLARUS. 
1S3 
The Gdarnisch. 
The Glarnisch is another complicated case of 
foldings.* It is both orographically and geologically 
a trough. The strata are folded on one another like 
an S cut off at the two sides by the valleys of the 
Linth and the Klon. Baltzer gives the following 
table showing the sequence of the strata on the 
eastern Glarnisch: — 
Actual Sequence on 
Normal Sequence. eastern Glarnish. 
Eocene 
Urgonian 
TJrgonian 
Neocomian 
Neocomian 
Valenginian 
Valenginian 
Neocomian 
Upper Jura 
Urgonian 
Middle Jura 
Neocomian 
Lias 
Valenginian 
Trias 
Neocomian 
Dyas 
Upper Jura 
Middle Jura 
Lias 
Upper Jura 
Middle Jura 
Dyas 
Upper Jura 
Eocene 
* Baltzer, Der Glarnisch. 
