liustikujõgede suubumisel jääjärves kuhjunud kruusast ja liivast koosnev, ümbritsevast alast kõrgemale ulatuv lainja pinnaga kaldtasandik
delta deposited in the proglacial lake by glacial rivers. Is a plain above surrounding terrain consisting of sand, gravel, pebbles and even boulders with the thickness of several tens of meters; having typically slightly inclined and undulating plain surface and steeply inclined forset beds dipping between 10-30deg.
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Ehituses on iseloomulikuks delta kasvamisel jääjärves kujunenud veeristest ja kruusast kallakkihiline kompleks, mida katavad rõhtsakihilised peenemad setted.
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