Eastport quadrangle notebook # 5, 1908
Page 172
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Transcription
7426 123 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 July 2 1908 A few rods east of the dam at the head of Roaring Lake, there occurs on the south side of the highway an exposure of thin gray shaly shale flanked on the east by a distance above the shale and underneath a rhyolite flow and inset a massive volcanic converting of more shale, rhyolite flow & tuff, then flows over a thick base lava, with a length of underlying tuff across the visible underlayment and tuff, rhyolite & acid flow. Ingers for details see section: see 8-5 13 notes on 7426, 7423, 7431, 2, 4, July with, 1908. The entire series strikes N. 20° E. and dips East about 40°. The fossiliferous gray shales in this highway contain: Lingula "striata" type Rare Orbiculoidea sp. " Chonetes cornutus Common Leptostropha ornata Common Prophonall (?) sp. Rather Rare Leptana rhomboidae " Stenoscisma cf. acinus Common vilsonia wilsoni Occasional Spirifer crispus (var.) " Atrypa reticularis Rare Meristella(?) sp. " Teronitella retroflexa " Eumphales (?) sp.) Occasional monotypella sp. Trails of Edmunds formation at Roaring Lake. 7426:4