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Turned
furrows in the northern ridge as seen from the west (11th. century
AD). A layer of raw humus showing some stratification covers the ridge,
and the layer of shifting sand on top of it has traces from the old
surfaces. The circular markings in the layer of windblown sand were
probably created by oak roots, in which case they were originally
of dark colour. - Photo: Vagn Wonsbek. |
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| For
further detail, see Vejbaek, O., "Agre og miler ved Filsö",
Kuml, 2005, pp. 187-124. |
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