skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View a record

Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.

Please search for material in iDiscover for up-to-date information about the library collection.


Record #139996:

Landslides and relict ice margin landforms in Adventdalen, central Spitsbergen, Svalbard / Takanobu Sawagaki, Takashi Koaze.

Title: Landslides and relict ice margin landforms in Adventdalen, central Spitsbergen, Svalbard / Takanobu Sawagaki, Takashi Koaze.
Author(s): Sawagaki, Takanobu.
Koaze, Takashi.
Date: 1996.
In: Polar Research. (1996.), Vol. 15(2) (1996)
Abstract: Landslides in middle ranges of Adventdalen comprise large-scale bedrock slumps which form hummocky surface; fourteen landslide blocks are recognised. Drainage channels consist of tributary rivers to Adventelva, either parallel or oblique to main river. Glacial deposits cover ridges between tributaries. Upper and lower landslide divisions may indicate former positions of ice surface. Results strongly suggest existence of stagnant ice or minor re-advance phases during deglaciation.
Notes:

Polar Research. Vol. 15(2) :139-152 (1996).

Keywords: 551.435.627 -- Landslides.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*32) -- Svalbard.
SPRI record no.: 139996

MARCXML

LDR 01282naa#a2200000#a#4500
001 SPRI-139996
005 20221004152609.0
007 ta
008 221004s1996####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-139996
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aSawagaki, Takanobu.
245 10 ‡aLandslides and relict ice margin landforms in Adventdalen, central Spitsbergen, Svalbard /‡cTakanobu Sawagaki, Takashi Koaze.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1996.
300 ## ‡ap. 139-152 :‡bill., diags., table, maps.
500 ## ‡aPolar Research. Vol. 15(2) :139-152 (1996).
520 3# ‡aLandslides in middle ranges of Adventdalen comprise large-scale bedrock slumps which form hummocky surface; fourteen landslide blocks are recognised. Drainage channels consist of tributary rivers to Adventelva, either parallel or oblique to main river. Glacial deposits cover ridges between tributaries. Upper and lower landslide divisions may indicate former positions of ice surface. Results strongly suggest existence of stagnant ice or minor re-advance phases during deglaciation.
650 07 ‡a551.435.627 -- Landslides.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*32) -- Svalbard.‡2udc
700 1# ‡aKoaze, Takashi.
773 0# ‡7nnas ‡tPolar Research. ‡gVol. 15(2) (1996) ‡wSPRI-64246
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221004