A sedimentological study on the formation of a hummocky moraine at Törnåkra in Småland, southern Sweden
En detaljerad sedimentologisk studie har gjorts på en sektion längs med en moränkulle vid Törnåkra i Småland, södra Sverige. Två sedimentära enheter, enheterna A och B, identifierades baserat på deras sedimentologiska särdrag. Den understa enheten (A) bildades genom vertikal pålagring av gravitationsdrivna sedimentflöden (diamiktona lager), kombinerat med att smältvatten dissaggregerade en stor deA detailed sedimentological study was made on a section along the side of a moraine hummock at Törnåkra in Småland, south Sweden. Two sedimentary units, A and B, were identified, based on their sediment characteristics. Unit A, the lower one, was formed due to vertical stacking of sediment gravity flow deposits (diamict beds) in combination with melt water disaggregation of such beds, leaving resi
