Age constraints on surface deformation recorded by fossil shorelines at Cape Range, Western Australia: Reply

Author:

Sandstrom Michael R.1,O’Leary Michael J.2,Barham Milo3,Cai Yue1,Rasbury E. Troy4,Wooton Kathleen M.4,Raymo Maureen E.1

Affiliation:

1. Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W, Palisades, New York 10964, USA

2. School of Earth Sciences, The University of Western Australia, 35 Stirling Highway, Perth, 6009 WA, Australia

3. Timescales of Mineral Systems Group, School of Earth and Planetary Sciences, Curtin University, Perth, 6845 WA, Australia

4. Department of Geosciences, Stony Brook University, Stony Brook, New York 11794, USA

Abstract

Whitney et al. (2021) challenge our conclusions about rates of deformation and amount of uplift along the Cape Range, Western Australia, particularly the elevation constraints we place on the last interglacial shoreline along the northern half of Cape Range. They selectively focus almost entirely on the northern half of Cape Range, completely omitting our extensive analysis of the southern section, which provides the bulk of our paleo−sea-level interpretations. They also raise concerns about some of the nomenclature and methodology used. We thank them for the opportunity to clarify our results on the minor section of our paper they take issue to, and address their concerns below point by point.

Publisher

Geological Society of America

Subject

Geology

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