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M. Clare

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Articles by M. Clare

Rapid submarine caldera collapse during the 2022 climactic eruption of Hunga volcano (Tonga)

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By M. Ribo, S. J. Cronin, M. Clare, S. J. Watson, Y. S. Choi, J. Jung, J. Yoo, B. Hutton, S. Alan Stern, M. Brenna, J. E. Hunt, K. Mackay, M. Manu, S-H. Park, J. Garvin, I. A. Yeo, S.-G. Kang, G. Sielfeld, D. A. Slayback, J. D. L. White, F. Latu’ila, N. Heni, P. Tuku’afu, T. Kula
| Nature Verified
Abstract Caldera-forming eruptions are among the most hazardous volcanic processes, particularly submarine ones. Yet, the dynamics of submarine caldera-forming eruptions and, thus, the hazards they pose are not well understood, owing to the relative inaccessibility of the resulting calderas and eruption products. Here we show the changes in geomorphology of Hunga volcano (Tonga) after the 15 January 2022 eruption.
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Benthic biology influences sedimentation in submarine channel bends: Coupling of biology, sedimentation and flow

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By J. Peakall, M. Clare, M. Azpiroz-Zabala, E. J. Sumner
| Wiley Online Library Verified
1 INTRODUCTION Submarine channels are distinctive large-scale sea floor features that funnel globally important volumes of sediment hundreds of kilometres from the shallow continental shelves into the deep sea (Khripounoff et al., 2003; Peakall & Sumner, 2015). These systems generally evolve from V-shaped canyons incised on the continental shelf (Kuenen, 1953; Wynn et al., 2007; Harris & Whiteway, 2011) to U-shaped channels with overbank deposits (Walker & Mutti, 1973; Clark & Pickering, 1996).
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Challenging the highstand-dormant paradigm for land-detached submarine canyons - Nature Communications

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By A. R. Gates, B. J. Bett, R. A. Hall, J. E. Hunt, I. A. Kane, M. Clare
| Nature Verified
Abstract Sediment, nutrients, organic carbon and pollutants are funnelled down submarine canyons from continental shelves by sediment-laden flows called turbidity currents, which dominate particulate transfer to the deep sea. Post-glacial sea-level rise disconnected more than three quarters of the >9000 submarine canyons worldwide from their former river or long-shore drift sediment inputs.
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