Summary
The superficial deposits within the map-sheets are classified genetically and described. The icemarginal line "Bremsnestrinnet" is reconstructed from the positions of terminal moraines in the fjord areas. Radiocarbon dating of the younger event "Tingvolltrinnet" further to the east to some 12 000 years, indicates that the "Bremsnestrinnet" is somewhat older, but no more than 13 500 years, at which time the continental shelf of Norway still thought to be covered by glaciers. Short accounts of the distribution of glacifluvial and fluvial deposits are given. Diverse tests have been carried out and are summarized in the "Grusregister".
