Frosta 1622 II. Beskrivelse av kvartærgeologisk kart - M 1:50 000 (med fargetrykt kart).

SKRIFTER
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75
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Forfattere
Reite, Arne J.
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Utgivelsesår
1986
Publikasjonstype
Utgivelsesår
1986
Summary
The superficial deposits occuring within the map-area are described and classified according to their genesis. In the mountains a discontinuous or thin cover of till dominates with peat in the depressions. In the lowland areas glaciomarine sediments were deposited at a sea-level situated c. 180 m above the present one. In Frosta and Skatval these sediments are overlain by till, deposited by a glacial advance during early Younger Dryas, reaching just to the west of the map-area. Marginal moraines from a late Younger Dryas glacial advance can be traced more or less continuously from Hegra in Stjørdal toowards Hoklingen and Alstahaug. During the shoreline displacement the sediments below the upper marine limit were influenced by fluvial erosion and slides. Short accounts are given on the potential for different utilization of the mapped superficial deposits.
Kommune
INDRE FOSEN
INDERØY
FROSTA
LEVANGER
STJØRDAL
Fylke
TRØNDELAG
Tilgjengelig
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