liustiku ühtlasel taandumisel kujunev lainja pinnamoega moreenist koosnev tasandik
an extensive flat plain of glacial till that forms when a glacier gradually melts depositing the sediment it carried. Surface topography can be slightly undulating, hummocky or drumlinized. Thermokarst/glaciokarst kettles are common.
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Sõltuvalt pinnamoest liigitatakse lainjad-, künklikud-, voorestatud moreentasandikud. Sagedane on glatsiokarsti nähtusest tingitud sulglohkude esinemine.
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