244 Dr. C. A. Cotton—Later Geological 
The folds of this system have sometimes been regarded as trending 
uniformly north-east and south-west parallel with the elongation of 
the existing ranges in which the rocks occur,‘ and from this it might 
be inferred that they determine the north-east and south-west trend 
NORTH ISLAND 
Kaikoura 
lauuR. 
HurunuiR 
SOUTH ISLAND 
ky 
Lake . WaitakiR 
RR) Manso. Oamaru 
hate 
VE ora bd; Shag R. 
b4 
7 Tatert 2, 
Fic. 1.—Locality map of New Zealand. 
1 See, for example, P. Marshall, ‘“New Zealand and Adjacent Islands,’’ 
Handbuch der regionalen Geologie, Bd. vii, Abt. i, p. 58, Heidelberg, 1911 ; 
Geology of New Zealand, Wellington, 1912, p. 127. 
