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Numerical investigation of the refractive properties of near-horizontal rocky shore platforms and their effects on harmonic and stationary wave patterns

Geomorphology (Amsterdam, Netherlands), 2025-01, Vol.468, p.109491, Article 109491

2025

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Trapping of fine-grained sediment on a supply-limited intertidal shore platform at Kaikōura, New Zealand

Geomorphology (Amsterdam, Netherlands), 2023-12, Vol.442, p.108926, Article 108926

2023

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The consequences of uplift on wave transformation across a shore platform, Kaikōura, New Zealand

Marine geology, 2022-09, Vol.451, p.106888, Article 106888

2022

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Supratidal inundation on an incipient marine terrace

Geomorphology (Amsterdam, Netherlands), 2022-11, Vol.417, p.108443, Article 108443

2022

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Subaerial weathering versus wave processes in shore platform development: reappraising the Old Hat Island evidence

Earth surface processes and landforms, 2011-05, Vol.36 (5), p.686-694

2011

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Wave transformation on a sub-horizontal shore platform, Tatapouri, North Island, New Zealand

Continental shelf research, 2011-09, Vol.31 (14), p.1409-1419

2011

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Sea level and storm control on the evolution of a chenier plain, Firth of Thames, New Zealand

Marine geology, 2012-04, Vol.307-310, p.58-72

2012

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Effects of varied lithology on soft-cliff recession rates

Marine geology, 2014-08, Vol.354, p.40-52

2014

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Shore platform development around Lord Howe Island, southwest Pacific

Geomorphology (Amsterdam, Netherlands), 2006-06, Vol.76 (3), p.295-315

Dickson, Mark E.

2006

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Lithological control on the elevation of shore platforms in a microtidal setting

Earth surface processes and landforms, 2006-10, Vol.31 (12), p.1575-1584

2006

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The influence of rock resistance on coastal morphology around Lord Howe Island, southwest Pacific

Earth surface processes and landforms, 2004-05, Vol.29 (5), p.629-643

2004

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Defining shore platform boundaries using airborne laser scan data: a preliminary investigation

Earth surface processes and landforms, 2007-05, Vol.32 (6), p.945-953

2007

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Geomorphological Evolution of Lord Howe Island and Carbonate Production at the Latitudinal Limit to Reef Growth

Journal of coastal research, 2006-01, Vol.22 (1), p.188-201

2006

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Episodes of reef growth at Lord Howe Island, the southernmost reef in the southwest Pacific

Global and planetary change, 2005-12, Vol.49 (3), p.222-237

2005

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The development of talus slopes around Lord Howe island and implications for the history of island planation

Australian geographer, 2004-07, Vol.35 (2), p.223-238

Dickson, M. E.

2004

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Carbonate sedimentation on subtropical shelves around Lord Howe Island and Balls Pyramid, Southwest Pacific

Marine geology, 2002-08, Vol.188 (3), p.333-349

2002

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Rock Coasts

Reference Module in Earth Systems and Environmental Sciences, 2013

2013

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10.11 Rock Coasts

Treatise on Geomorphology, 2013, p.289-307

2013

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Nebraska University Poultry Exhibit

Journal of the American Association of Instructors and Investigators of Poultry Husbandry, 1917-01, Vol.3 (4), p.30-32

DICKSON, M.E.

1917

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The pH stability of the Wisconsin FXNO strain of egg-adapted distemper virus

American journal of veterinary research, 1955-10, Vol.16 (61 Part 1), p.616

1955

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Osmium isotope evidence for two pulses of increased continental weathering linked to Early Jurassic volcanism and climate change

Geology (Boulder), 2016-09, Vol.44 (9), p.759-762

2016

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Carbonate sedimentology

1, 2009

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Does large igneous province volcanism always perturb the mercury cycle? Comparing the records of Oceanic Anoxic Event 2 and the end-Cretaceous to other Mesozoic events

American journal of science (1880), 2018-10, Vol.318 (8), p.799-860

2018

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Sedimentary Mercury Enrichments as a Marker for Submarine Large Igneous Province Volcanism? Evidence From the Mid‐Cenomanian Event and Oceanic Anoxic Event 2 (Late Cretaceous)

Geochemistry, geophysics, geosystems : G3, 2017-12, Vol.18 (12), p.4253-4275

2017

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Water dispersible clay and micro-structure of soils from coastal plain sands, shale and false-bedded sandstones

Soil security, 2024-09, Vol.16, p.100137, Article 100137

2024

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Numerical investigation of the refractive properties of near-horizontal rocky shore platforms and their effects on harmonic and stationary wave patterns

Trapping of fine-grained sediment on a supply-limited intertidal shore platform at Kaikōura, New Zealand

The consequences of uplift on wave transformation across a shore platform, Kaikōura, New Zealand

Supratidal inundation on an incipient marine terrace

Subaerial weathering versus wave processes in shore platform development: reappraising the Old Hat Island evidence

Wave transformation on a sub-horizontal shore platform, Tatapouri, North Island, New Zealand

Sea level and storm control on the evolution of a chenier plain, Firth of Thames, New Zealand

Effects of varied lithology on soft-cliff recession rates

Shore platform development around Lord Howe Island, southwest Pacific

Lithological control on the elevation of shore platforms in a microtidal setting

The influence of rock resistance on coastal morphology around Lord Howe Island, southwest Pacific

Defining shore platform boundaries using airborne laser scan data: a preliminary investigation

Geomorphological Evolution of Lord Howe Island and Carbonate Production at the Latitudinal Limit to Reef Growth

Episodes of reef growth at Lord Howe Island, the southernmost reef in the southwest Pacific

The development of talus slopes around Lord Howe island and implications for the history of island planation

Carbonate sedimentation on subtropical shelves around Lord Howe Island and Balls Pyramid, Southwest Pacific

Rock Coasts

10.11 Rock Coasts

Nebraska University Poultry Exhibit

The pH stability of the Wisconsin FXNO strain of egg-adapted distemper virus

Osmium isotope evidence for two pulses of increased continental weathering linked to Early Jurassic volcanism and climate change

Carbonate sedimentology

Does large igneous province volcanism always perturb the mercury cycle? Comparing the records of Oceanic Anoxic Event 2 and the end-Cretaceous to other Mesozoic events

Sedimentary Mercury Enrichments as a Marker for Submarine Large Igneous Province Volcanism? Evidence From the Mid‐Cenomanian Event and Oceanic Anoxic Event 2 (Late Cretaceous)

Water dispersible clay and micro-structure of soils from coastal plain sands, shale and false-bedded sandstones

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