Malarás

Langur ás gerður úr samsíða lögum af sandi og möl með öldulaga formi (mynd 1) eða nokkrar lengjur af hæðum sem verða til þegar leysingavatn flæðir undan jöklum (hæðir undir jöklum) eða rásir ofan jökla sem leysingavatn rennur eftir í opnum sprungum (ofanjökla hæðir).

Hæðir undir jöklum eru oft staðsettar innan dælda undir jöklum. Oftast eru hæðirnar hornréttar á jökulsporðinn sem býr þær til.

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