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Record #115524:

Colonisation végétale et géodynamique des versants en milieu polaire océanique (Svalbard, 79°N) / Marie-Françoise André.

Title: Colonisation végétale et géodynamique des versants en milieu polaire océanique (Svalbard, 79°N) / Marie-Françoise André.
Translated title: Plant colonisation and slope processes in a Polar oceanic environment (Svalbard, 79°N).
Author(s): André, Marie-Françoise.
Date: 1991.
Language: French.
In: Inter-Nord. (1991.), Vol. 19 (1991)
Abstract: Plant colonization and lichenometry researches yielded new insights into slope processes on Svalbard: major stages in slope evolution during Holocene have been identified and 3500-2000 BP neoglacial period is suggested as starting point of formation of lobate rock glaciers; estimates of frequency of episodic meteorological events indicate recurrence interval of rainfall-triggered debris flows and slush avalanches of 70-600 years; active and stable slope deposits were distinguished and importance of run-off during spring thaw and hypodermic drainage later in summer are implied.
Notes:

Inter-Nord. Vol. 19 :415-425 (1991).

English abstract p.415.

Keywords: 550.93 -- Geochronology.
551.32 -- Glaciology.
551.324.5 -- Land ice, flow.
551.332.5 -- Glacial landforms.
551.5 -- Meteorology.
574 -- Ecology.
582.29 -- Lichens.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*32) -- Svalbard.
(*324) -- Spitsbergen.
SPRI record no.: 115524

MARCXML

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040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡afre
100 1# ‡aAndré, Marie-Françoise.
242 10 ‡aPlant colonisation and slope processes in a Polar oceanic environment (Svalbard, 79°N).‡yeng
245 10 ‡aColonisation végétale et géodynamique des versants en milieu polaire océanique (Svalbard, 79°N) /‡cMarie-Françoise André.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 415-425 :‡bill., tables, map.
500 ## ‡aInter-Nord. Vol. 19 :415-425 (1991).
500 ## ‡aEnglish abstract p.415.
520 3# ‡aPlant colonization and lichenometry researches yielded new insights into slope processes on Svalbard: major stages in slope evolution during Holocene have been identified and 3500-2000 BP neoglacial period is suggested as starting point of formation of lobate rock glaciers; estimates of frequency of episodic meteorological events indicate recurrence interval of rainfall-triggered debris flows and slush avalanches of 70-600 years; active and stable slope deposits were distinguished and importance of run-off during spring thaw and hypodermic drainage later in summer are implied.
546 ## ‡aIn French.
650 07 ‡a550.93 -- Geochronology.‡2udc
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324.5 -- Land ice, flow.‡2udc
650 07 ‡a551.332.5 -- Glacial landforms.‡2udc
650 07 ‡a551.5 -- Meteorology.‡2udc
650 07 ‡a574 -- Ecology.‡2udc
650 07 ‡a582.29 -- Lichens.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*32) -- Svalbard.‡2udc
651 #7 ‡a(*324) -- Spitsbergen.‡2udc
773 0# ‡7nnas ‡tInter-Nord. ‡gVol. 19 (1991) ‡wSPRI-35278
917 ## ‡aUnenhanced record from Muscat, imported 2019
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