| OCR Text |
Show the escarpment is dark green, very fine-grained, well foliated phylliteQ tact with is Paleozoic gradational A to the be composed of cloudy chlorite Some with siliceous black, are A grey 25, in coarse mostly in green rocks is mass and as small To 27 No, color, grained and in 66 Wo fine to are deformation and It grey, of soft, in the is well to of and recrystallization the rock feathery weathering In Chlorite south are are and quartz planeso half of foliated, the to grey places abundant pyrite foliation quartz, muscovite, fissile, phyllites 65 Wo, associated The rock, and very to the many is thus east. layers can be found. shale in that sericite nearly dark to phyllite but 24 sections light equivalent layers most con presento were Ro medium-grainedo comparison shows fibrous, mineral granules along quartz compose consisting mostly layers R. of beddedQ tin occurs phyllite 27 No, mostly dark the in 90 per cent of the miera18o opaque 5, To between is feeto about up section phyllite outcrop Chlorite and Some of the an contact the'dominant mineral constituentsQ occurs, and of and fine-grained, very tens which makes phyllite The lepidioblastic a quartz, sericite9 The rockso section fissile, places the green phyllite several over thin single In soft, minor. Correlation and Thickness Dolomite, which crops out between lite is the two large expanses near of discontinuously exposede the pink and grey mottled dolomite 40 the Good Fortune phyllite outorop Both and mine, and the occurs phyl phyllite outcrops overli this feature provides the |
