"Gefuegerelief" illustrated by "schist tor" topography in central Otago, New Zealand
- 1 November 1952
- journal article
- Published by American Journal of Science (AJS) in American Journal of Science
- Vol. 250 (11) , 802-807
- https://doi.org/10.2475/ajs.250.11.802
Abstract
Isolated blocky outcrops of schist in central Otago, New Zealand, are elongated and aligned in a northwest direction which parallels the lineation of the schist, and are thought to reflect the effect of differential weathering controlled by the rock fabric.Keywords
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