616 
APPENDIX. 
[C. 
also Kater Island, in Montagu Sound. And the same 
rock appears to occur throughout the islands on this part 
of the coast.— (Narrative, i. p. 401.) 
Montagu Sound, about five-and-twenty miles south-west 
of Admiralty Gulf, (Narrative, i. p. 400.) — Greyish gra- 
nular quartz; like that of the Lickey Hill, in Worcestershire. 
Fine-grained quartzose sandstone^ of a purplish hue, re- 
sembling a rock on the banks of the Severn, near Bridge- 
north. Grey and reddish sand-stone; apparently composed 
of the debris of granite, and very nearly resembling that of 
Simms Island above-mentioned. 
Hunter’s River, falling into York Sound, on the north- 
east side. — Somewhat coarse reddish-white sand-stone ; like 
that of the coal formation, and some varieties of millstone 
grit. Fine-grained, reddish-grey quartzose sand-stone^ hav- 
ing the appearance of stratification, and resembling the 
rocks of Cambridge Gulf. 
Roe’s River, at the eastern termination of York Sound, 
(Narrative, i. p. 407, 408, 413,) runs between precipitous 
banks of sand-stone^ in nearly horizontal strata, which rise 
to the height of three hundred feet. 
Careening Bay, between York Sound and Prince Re- 
gent’s River, (Narr. i. p. 413; ii. 43, &c. See the plate, 
p. 418, vol. i.) — Crystalline epidote, and whitish quartz, ap- 
parently from a vein. Purplish-brown epidote, with small 
nests or concretions of green epidote and quartz ; forming a 
a sort of amygdaloid. Conglomerate^ containing angular 
fragments of yellowish-grey quartz-rock, in a base of com- 
pact epidote. A nearly uniform greenish compound of 
epidote intimately mixed with quartz, also occurs at this 
place. Flat lamellar calcedony. Very fine-grained red- 
