Soils of some former Norse settlements in southwestern Greenland were
investigated and found to have well-developed, brightly coloured soil
profiles in spite of the high latitude. The soils are generally acidic
, sandy, strongly organic and high in exchange cations. Iron extractio
n data suggest a moderate degree of pedologic activity. The presence o
f smectite and interstratified hydroxy-aluminum vermiculite is likely
representative of an early stage of neomineral formation in an area wh
ich has probably been ice-free for at least 8000 years. In the areas v
isited, there was no evidence in the soil to suggest that extensive so
il erosion was responsible for the abandonment of these settlements.