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Fig. s.—Dorrigo Plateau, N.S.W. Generalised catenary sequence of soils on basalt. Even higher rainfall at Dorrigo (inset) produces some gleying where there is interference from the ground-water table, but these soils otherwise have very little catenary differentiation.

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Permanent link to this item

https://paperspast.natlib.govt.nz/periodicals/TRSES19700806.2.2.5

Bibliographic details

Transactions of the Royal Society of New Zealand : Earth Sciences, Volume 7, Issue 6, 6 August 1970, Page 93

Word Count
37

Fig. 5.—Dorrigo Plateau, N.S.W. Generalised catenary sequence of soils on basalt. Even higher rainfall at Dorrigo (inset) produces some gleying where there is interference from the ground-water table, but these soils otherwise have very little catenary differentiation. Transactions of the Royal Society of New Zealand : Earth Sciences, Volume 7, Issue 6, 6 August 1970, Page 93

Fig. 5.—Dorrigo Plateau, N.S.W. Generalised catenary sequence of soils on basalt. Even higher rainfall at Dorrigo (inset) produces some gleying where there is interference from the ground-water table, but these soils otherwise have very little catenary differentiation. Transactions of the Royal Society of New Zealand : Earth Sciences, Volume 7, Issue 6, 6 August 1970, Page 93

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