liustiku sulamisel jääst vabanenud setetest liustikuserva ette kujunevad liustikuservaga paralleelsed (marginaalsed) ja selle kuju jälgivad künnised, mille mõõtmed sõltuvad kujunemise aja kestusest ja sette hulgast liustikus, a winding ridge of unconsolidated debris (till) deposited at/in front of a glacier margin. They reflect the shape of the glacier terminus and the size depends on the length of it takes them to form. May be composed of debris ranging in size from silt-sized glacial flour to large boulders. Can be formed at the ice-sheet margins as well as in front of Alpine glaciers.
liustike kuhjatud, segakoostise ja -lõimisega, sorteerumata ja ümardumata osadest koosnev sete, unstratified drift, deposited directly by a glacier without reworking by meltwater, and consisting of a mixture of clay, silt, sand, gravel, and boulders ranging widely in size and shape, depósito glacial no estratificado ni clasificado que se presenta asociado al extremo del glacial y las acumulaciones de las morrenas terminales
moraine . Limnoloogia sõnastik. Eesti Keele Instituut, Sõnaveeb 2026. https://sonaveeb.ee/search/unif//lim/moraine/1/fra (20.06.2026)
