Table 1 Summary of study site cliff-forming lithology, cliff erosion rate, and wave climatology.

From: Modeling future cliff-front waves during sea level rise and implications for coastal cliff retreat rates

Location

Cliff-forming lithology

Cliff erosion rate [m/year]

Wave climatology

Okakari point, Auckland (AK1)

Flysch (volcanic-rich) with alternating mudstone and sandstones*

< 0.0232

Intermediate wave energy with occasional tropical storm events

Red beach, Auckland (AK2)

Flysch (volcanic-poor) with alternating siltstones and sandstones*

< 0.0232

Low wave energy with occasional tropical storm events

Rothesay bay, Auckland (AK3)

Flysch (volcanic-poor) with alternating siltstones and sandstones*

< 0.0232

Low wave energy with occasional tropical storm events

Sunset cliff, San Diego (SD1)

Cretaceous sedimentary overlaid by Pleistocene terrace deposits33

0.06–0.4334

Seasonal winter-high and summer-low wave energy

Del Mar, San Diego (SD2)

Eocene sedimentary overlaid by weakly cemented sandy Pleistocene terrace deposits33

0.03–0.1034

Seasonal winter-high and summer-low wave energy

Nash point, Vale of Glamorgan (VG)

Jurassic Blue Lias Limestone, alternating bands of organic-rich, finely laminated shales and limestones35

0.06–0.0835

High energy storm wave

  1. *General rock hardness: AK1 > AK2 > AK3