järsu nõlva jalamile varisenud materjalist kujunenud koonusekujuline kuhjatis
cone of fallen rock fragments/debris at the base of the cliff/slope; laterally joining cones can form talus (apron); 45deg is a maximum natural sloping of talus cone in unconsolidated sediments.
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Rusukoonuste külgepidi liitumisel võivad kujuneda ulatuslikud rusukalded; pudedates setetes ei saa rusukoonuse kallakus ületada 45o
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