Støren. Beskrivelse til kvartærgeologisk kart 1621 III - M 1 : 50 000 (med fargetrykt kart).
SKRIFTER
65
Publikasjonstype
Utgivelsesår
1985
Summary
The superficial deposits occurring within the map-area are described and classified according to their genesis. In the mountains, till and organic deposits dominate. In the lowland areas glaciofluvial and glaciomarine sediments were deposited at a sea-level situated c. 175 m above the present one. During the shoreline displacement these sediments were strongly influenced by fluvial erosion and slides. The ice recession was interrupted by a glacial advance which took place dUring the first half of the Younger Dryas Chronozone, reaching just to the north of the map-area. Another glacial advance can be traced from the southwestern part of the map towards Reinsfjell and possibly to the western part of the lake Selbusjøen. These marginal moraines were deposited during late Younger Dryas. Short accounts are given on the potential for different utilization of the superficial deposits.
Forfattere
Reite, Arne J.
Kommune
TRONDHEIM
MELHUS
MIDTRE GAULDAL
Fylke
TRØNDELAG
Tilgjengelig
NGU-biblioteket