rannajärsaku jalamile selle järk-järgulisel nihkumisel maismaa suunas kujunenud lauge rannanõlvaga madalaveeline rannikuosa (kulutusala)
subhorisontal plain off-shore at the cliff foot, formed when the roof of wave-cut notch collapses resulting the cliff retreating landward and the base of the wave-cut notch forms wave-cut platform. Can emerge while water-level drops forming a coastal terrace.
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Veetaseme alanedes võivad kerkida veetasemest kõrgemale moodustades rannaterrassi.
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