. The geology of the Oamaru district, North Otago (Eastern Otago division). James Park, plmtn.]A. FOSSILIFKKOCS LiMESTOXK VkIX IX r.\ J{ni;CCIA, SKAU HltKAKWATKH, A. C. Giffori/, /i/mto.] B. FOSSILIFKHOLS LiMESTONE Veix IX TaCHYLITIC Breccia, near Breakwatkr, Oamaru. Geol. Bull. No. 20.\ [7o face p(ige 76. Page Page 77 Glauconitic Sandst one—ro /(/ / n iied. 77 Upper Tari;et Gully Sections 82 78 Section on East Side of Target (iully 82 78 Section across Target (Jully above 79 Town Belt 82 79 Section South of 83 80 Section at Otiake 83 81 Section on Left Bank of Wai
. The geology of the Oamaru district, North Otago (Eastern Otago division). James Park, plmtn.]A. FOSSILIFKKOCS LiMESTOXK VkIX IX r.\ J{ni;CCIA, SKAU HltKAKWATKH, A. C. Giffori/, /i/mto.] B. FOSSILIFKHOLS LiMESTONE Veix IX TaCHYLITIC Breccia, near Breakwatkr, Oamaru. Geol. Bull. No. 20.\ [7o face p(ige 76. Page Page 77 Glauconitic Sandst one—ro /(/ / n iied. 77 Upper Tari;et Gully Sections 82 78 Section on East Side of Target (iully 82 78 Section across Target (Jully above 79 Town Belt 82 79 Section South of 83 80 Section at Otiake 83 81 Section on Left Bank of Waitaki River, Wharekuri 84 c gr 3ensands. (c) Conglomerate, mainly basaltic. 77 CHAPTER STAGE. Conglomerate Fauna of Conglomerate(Jlauconitic Greensands Fauna of Glauconitic GreensandsGlauconitic SandstoneTarget Ciiilly Sections Section at Target CJuUy at Ardgowan Shell-bed (a) Glauconitic sandstone. (b) Glauconi Hutchinsonian consists of two well-marked members—namely, glauconitic sands (theLower Hutchinsonian) and a glauconitic sandstone (the Upper Hutchinsonian= Waitaki stone). The conglomerate is
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Keywords: ., bookcentury1900, bookdecade1910, booksubjectgeology, bookyear1918
