. Transactions and proceedings of the New Zealand Institute . f the land that has been made by deposition fromflooded rivers, but the facts are not available. 436 Transactions. Map fig. 4 sliows the east coast as it is to-day, with the several riversrunning into Poverty Bay and Hawke Bay respectively. The plains arenot to be distinguished from the other portions of the land-area, for natureheals wounds, and only leaves remnants of a past, after the manner of acamping-ground in the case of Natives or a party of picknickers. In a former paper on Artesian-water Basins of Heretaunga Plain (Trans.
. Transactions and proceedings of the New Zealand Institute . f the land that has been made by deposition fromflooded rivers, but the facts are not available. 436 Transactions. Map fig. 4 sliows the east coast as it is to-day, with the several riversrunning into Poverty Bay and Hawke Bay respectively. The plains arenot to be distinguished from the other portions of the land-area, for natureheals wounds, and only leaves remnants of a past, after the manner of acamping-ground in the case of Natives or a party of picknickers. In a former paper on Artesian-water Basins of Heretaunga Plain (Trans. Inst., vol. xxxvii, p. 432), sections are shown to illustrate thegrowth of the plain, and reference is made to the Great Wairarapa that flowedover the area long before the plain was formed. At that time my inquirieshad not extended to Poverty Bay, but the sections (figs. -5, 6, 7, and 8) givein regular sequence the geological events and proofs such as are given in theabove paper with respect to the Heretaunga Plain. \T£,tC kAAA /J/ \HAlt€/fATAHJ S-^.
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