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Record #179585:
- #179585
Main publication details
MARC recordDepositional origin of an adverse delta surface slope at Altermarka, northern Norway / K. Gustavson, L. Olsen.
| Title: | Depositional origin of an adverse delta surface slope at Altermarka, northern Norway / K. Gustavson, L. Olsen. |
| Author(s): | Gustavson, K. Olsen, L. |
| Date: | 2006. |
| In: | Norsk Geografisk Tidsskrift. (2006.), Vol. 60(2) (2006) |
| Abstract: | Presents reinvestigation of Altemarka delta, finding no evidence that glacier overrode surface. Notes that topset beds remain intact and no appreciable till was found. Locates sediments resembling samples originally taken from Altermarka, but suggests that soil processes and other sedimentary processes could easily account for wide grain-size distributions. Cautions against using grain-size analysis, on its own, to interpret genesis of sediments. |
| Notes: | Norsk Geografisk Tidsskrift. Vol. 60(2) :129-138 (2006). |
| Keywords: | 551.3.051 -- Sedimentation and stratification. 551.332.2 -- Drift, glacial. Deposits. 551.332.212 -- Till or boulder clay. 551.332.25 -- Glacio-marine deposits. 551.4 -- Geomorphology. 551.4.037 -- Slopes. 551.7 -- Stratigraphy. B -- Geology and soil sciences. (*3) -- Arctic regions. (*58) -- Norway. |
| SPRI record no.: | 179585 |
LDR 01657naa#a2200000#a#4500 001 SPRI-179585 005 20230328043451.0 007 ta 008 230328s2006####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-179585 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aGustavson, K. 245 10 ‡aDepositional origin of an adverse delta surface slope at Altermarka, northern Norway /‡cK. Gustavson, L. Olsen. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2006. 300 ## ‡ap. 129-138 :‡bill., diag., table, map. 500 ## ‡aNorsk Geografisk Tidsskrift. Vol. 60(2) :129-138 (2006). 520 3# ‡aPresents reinvestigation of Altemarka delta, finding no evidence that glacier overrode surface. Notes that topset beds remain intact and no appreciable till was found. Locates sediments resembling samples originally taken from Altermarka, but suggests that soil processes and other sedimentary processes could easily account for wide grain-size distributions. Cautions against using grain-size analysis, on its own, to interpret genesis of sediments. 530 ## ‡aAlso issued online ‡uurn:doi:10.1080/00291950600723096‡uhttps://dx.doi.org/10.1080/00291950600723096 650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc 650 07 ‡a551.332.2 -- Drift, glacial. Deposits.‡2udc 650 07 ‡a551.332.212 -- Till or boulder clay.‡2udc 650 07 ‡a551.332.25 -- Glacio-marine deposits.‡2udc 650 07 ‡a551.4 -- Geomorphology.‡2udc 650 07 ‡a551.4.037 -- Slopes.‡2udc 650 07 ‡a551.7 -- Stratigraphy.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*58) -- Norway.‡2udc 700 1# ‡aOlsen, L. 773 0# ‡7nnas ‡tNorsk Geografisk Tidsskrift. ‡gVol. 60(2) (2006) ‡wSPRI-13025 916 ## ‡aJW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230328 ‡bJW