166 DISTRIBUTION OF BEDDED LEADS 



fold, including Mooseland and Geg-ogan (Lawrencetown may 

 be on a westward continuation) ; (5) the Wine Harbour 

 fold, with Wine Harbour ; (6) The Montague-Isaacs Harbour 

 fold, with Montague, Gold Lake, Killag, Goldenville, and 

 Isaacs Harbour ; (7) the Moose River- Beaver Dam fold, with 

 Beaver Dam, Upper Seal Harbour, Ragged Falls, and Moose 

 River ; (8) the Waverley- Fifteen Mile Stream fold, with 

 Waverley at the west, running through Moose River, where it 

 parts company with 7, to Fifteen Mile Stream ; (9) The 

 Caribou fold, containing Caribou, Cameron Dam, Crow's Nest, 

 and Cochran Hill ; (10) the Oldham fold, with Oldham: (11) 

 the South Branch Musquodoboit fold, with an unnamed dome 

 and Little Liscomb Lake mine ; (12) the South Uniacke fold, 

 with South Uniacke ; and (13) the Mt. Uniacke fold, with Mt. 

 Uniacke and Renfrew. Thus exactly half the anticlines have 

 domes which are being worked, or which have been operated 

 in the past. 



It will be noted that there is a great variation, from one to 

 five, in the number of known domes on individual anticlines. 

 There is much difference, also, in the length of these anticlines 

 — from 4.5 miles, in the local Ecum vSecum axis, to about 105 

 miles in the Waverley-Moose River-Upper Seal Harbour fold. 

 Further, the variation in interval between adjacent domes on the 

 same axis is considerable. Tiie two nearest together, un- 

 separated by a fault, are Ecum Secum and Harrigan Cove, 

 about 6 miles apart. This is the only instance of its kind, 

 however, and Harrigan Cove has not a very good dome structure. 

 The two adjacent districts farthest apart without an intervening- 

 fault, are Goldenville and Killag, about 34 miles distant. 

 Mapping the domes upon one large sheet, so that the relations 

 can be seen at a glance, it at first sight looks as though there 

 were a tendency to an oblique northeast-southwest alignment 

 of domes, the districts lying slightly farther east on each suc- 

 cessive axis northward. Close inspection, however, shows that 

 the tendency is really present in but two cases, and may well be 

 accidental in these. To sum up, therefore, it appears that any 



