THE GREAT MARLBOROUGH CONGLOMERATE 



349 



of the conglomerate are not of local origin because local outcrops 

 of similar rock in place have not yet been found. 



The same conglomerates have been described as glacial moraines 

 by Park/ who assumes extensive glaciation in Eastern Marlborough 

 in the Pleistocene period. 



1-*^ I Great Marlborough Conglomerate. 



I. I Grey Marl and 1 r ,(■ . -,- 



^ Amuri Series ) C-«ta.ceous and Tertiary. 



^^^ Pre-Cretaceous (Maitai") 



\C.Canf)l>tU, 



KAIKOURA t- 



Scale of Miles 



1^ . gf > 



Fig. I. — Locality map of Eastern Marlborough, New Zealand. Geology after 

 McKay. 



The writer has examined several outcrops in the neighborhood 

 of Kekerangu, that forming Deadman's Hill, and also, at a number 

 of points, the strip which follows the line of the Middle Clarence 

 Valley. The outcrop near Cape Campbell was, however, in the 

 limited time available, not found, although a great part of the 



'J. Park, Trans. N.Z. Inst., XLIII, 520-24, 1910; Geology of New Zealand, 

 pp. 201-S, 1910. 



