Fig. 3.—Near Armidale, N.S.W. Generalised catenary sequence of soils on basalt. As in Fig. 1, the shallow soils have numerous basalt “ floaters ” in the higher positions, while there are reddish-chocolate soils on the slopes. In contrast with the two New Zealand examples (Figs. 1 and 2) the rainfall at Armidale (inset) differs in seasonality and amount, and temperatures are less equable.
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Transactions of the Royal Society of New Zealand : Earth Sciences, Volume 7, Issue 6, 6 August 1970, Page 92
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61Fig. 3.—Near Armidale, N.S.W. Generalised catenary sequence of soils on basalt. As in Fig. 1, the shallow soils have numerous basalt “ floaters ” in the higher positions, while there are reddish-chocolate soils on the slopes. In contrast with the two New Zealand examples (Figs. 1 and 2) the rainfall at Armidale (inset) differs in seasonality and amount, and temperatures are less equable. Transactions of the Royal Society of New Zealand : Earth Sciences, Volume 7, Issue 6, 6 August 1970, Page 92
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