h 
or r grey sub-metamorphic limestone, which is in places di 
_ THE GEOLOGICAL FORMATIONS OF NEW ZEALAND. 
to a very large extent. White crystalline limestones are alo 
associated with these beds throughout the whole length of | 
district from Mount Owen to Motueka. ey 
The whole series is disturbed by eruptive mee 
syenitic rocks, which are probably of devonian 
Fossils have been found in two localities only, and th 
} 
stone and bituminou 8 schists o erlie. 
