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Tuatara: Volume 2, Issue 2, July 1949
Fig. 2. An interpretation of New Zealand geography in the early Wanganui Epoch (? Early Pliocene). Marine fossiliferous rocks give positive evidence of the presence of sea in some areas, but the position of land and of coast lines must be deduced from indirect evidence of many kinds which is seldom conclusive
Fig. 2. An interpretation of New Zealand geography in the early Wanganui Epoch (? Early Pliocene). Marine fossiliferous rocks give positive evidence of the presence of sea in some areas, but the position of land and of coast lines must be deduced from indirect evidence of many kinds which is seldom conclusive.