20 Transactions. 



watermark. This block bears the character of a rock from the Nelson 

 Province, and has no marks of hnman workmanship upon it. 



2. A boulder of garnet-schist from the same locality, five or six inches 

 long, and partially rounded or water-worn. The original locality of this 

 boulder would also appear to be the Nelson Province. 



A piece of decomposed micaceous granite was brought to me from the 

 Hutt some years ago, exact locality where found not known ; and in the 

 Museum there is a fragment of a piece of granite which was found near the 

 Tinakori Road, but of which, it having been broken up, 1 have not been able 

 to obtain sufficiently reliable intelligence to put in evidence. It appears, 

 however, that it is a New Zealand specimen, apparently from the west coast 

 of the South Island. 



There are at least three ways by which these foreign specimens may have 

 been carried. 



1. By canoe or ship. 



2. By seaweed. 



3. By floating ice. 



The dioritic blocks may have been carried by a fourth moWng power, viz., 

 by glacier ; but that power could hardly apply to the granite or schists, as 

 the distance whence they must have come is so great. 



To suppose the existence of a climate in these latitudes sufficiently cold to 

 infer the presence of glaciers and of floating ice, it is not necessary to bring- 

 in the idea of a secular cooling of the globe, nor even of a greatly increased 

 mass and height of mountains. A prolongation of the New Zealand plateau 

 as dry land in the direction of Mounts Erebus and Terror or other parts of 

 the Antarctic continent, would, by blocking and deflecting the polar current, 

 probably cause the refrigeration necessary to produce the e:ffiect. 



I shall not at present venture to decide upon the cause which has placed 

 either description of boulders in their present position. There is an absence 

 of marks of ice action on the rocks of our mountains, but the rocks are in 

 general too soft for us to expect in them the retention of striated marks ; 

 I am therefore not prepared to decide upon the effect of the action of ice. 

 The boulders from Lyall Bay were found some twelve or fourteen feet 

 above high watermark, and had they been deposited by seaweed, it must 

 have been when the land was at a lower level. They were also too far from 

 the water's edge to render it probable that they were brought as ballast, 

 either by canoe or by ship. 



I shall content myself by thus calling attention to the subject, in the hope 

 that, before long, fresh evidence may be procured. More boulders may be 

 found, and their nature and position carefully noted ; and probably strice 

 may yet be discovered. 



