.V DEPTHS AND DEPOSITS OF THE OCEAN 203 



Among the metamorphic series there are representatives of crystalline 

 o-neisses and schists which could be matched from the Lewisian gneiss 



Fig. 145.— Glaciated Stone from "Michael Sars " Station 95. 



and Moine schist areas in the North-West Highlands of Scotland. 

 Associated with these are specimens indicatmg a low grade of meta- 

 morphism, such as phyllites and sheared greywackes and igneous rocks, 



