. Transactions and proceedings of the New Zealand Institute . SECr/O/V THffOUC/i TNE ME/IA/££ FLATS NAP/EH. i. ^lzov£a/l sojz^. tru-Ti/Tos of IrMJ. (Toiarn/. 2^a3ca,.) J. Shelly IzTTiMton^.a. Soft Siue sTuiZe,. TfiST!/ A. CoU sjrrin^) Warm, springs^ wz^ Jferoii/yD. Cold sprlT^yi G. Wcunn Sprma, w^Ji^cufj. r. w:StMm- AtZ. J^. /lit/ SKETC/^ of some. NOT SPRINGS n&a,7 ihe, BAV of JSL/I/VOS. yPnrAJ at&t*.St^^^Press 249 series increases in thickness from Port Waikato southwards, the Papakuraseries increases in thickness from Papakura northwards. Professor Hochs


. Transactions and proceedings of the New Zealand Institute . SECr/O/V THffOUC/i TNE ME/IA/££ FLATS NAP/EH. i. ^lzov£a/l sojz^. tru-Ti/Tos of IrMJ. (Toiarn/. 2^a3ca,.) J. Shelly IzTTiMton^.a. Soft Siue sTuiZe,. TfiST!/ A. CoU sjrrin^) Warm, springs^ wz^ Jferoii/yD. Cold sprlT^yi G. Wcunn Sprma, w^Ji^cufj. r. w:StMm- AtZ. J^. /lit/ SKETC/^ of some. NOT SPRINGS n&a,7 ihe, BAV of JSL/I/VOS. yPnrAJ at&t*.St^^^Press 249 series increases in thickness from Port Waikato southwards, the Papakuraseries increases in thickness from Papakura northwards. Professor Hochstetter, when assigning a position to the Papakura series,appears to have been too much influenced by the apparently intermediatecharacter of its fossils, between those of the Aotea and Waitemata series, so thatwhen, in his lecture, he placed the Waitemata series in its true position, hemade the Papakura series younger than parts of the Aotea series, and whenhe subsequently classed the Waitemata series with the Brown coal, he placedthe Papakura series in its pi-obably true position below the Aotea series. The connection between the Papakura and Waitemata series was supposedto consist in the occurrence of Pecten Fischeri, Pecten,


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