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Record #94787:

Morphogenetic features of talus cones in northwestern Wedel Jarlsberg Land, Spitsbergen / Jerzy Nitychoruk, Jan Dzierzek.

Title: Morphogenetic features of talus cones in northwestern Wedel Jarlsberg Land, Spitsbergen / Jerzy Nitychoruk, Jan Dzierzek.
Author(s): Nitychoruk, Jerzy.
Dzierzek, Jan.
Date: 1988.
In: Polish Polar Research. (1988.), Vol. 9(1) (1988)
Abstract: Three altitudinal zones of occurrence identified, dependent on influence of microclimate of adjacent glaciers. Zone A (<150 m a.s.l.) is not influenced by glacier, zone B (150 to 350 m a.s.l.) is influenced by glacier snouts, zone C (>350 m a.s.l.) is influenced by firn fields. Main development in this area occurred during Little Ice Age.
Notes:

Polish Polar Research. Vol. 9(1) :73-85 (1988).

Keywords: 551.435.646 -- Screes.
551.343.4 -- Rock glaciers.
E8 -- Glaciology: frost action and permafrost.
(*32) -- Svalbard.
(*324) -- Spitsbergen.
SPRI record no.: 94787

MARCXML

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100 1# ‡aNitychoruk, Jerzy.
245 10 ‡aMorphogenetic features of talus cones in northwestern Wedel Jarlsberg Land, Spitsbergen /‡cJerzy Nitychoruk, Jan Dzierzek.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1988.
300 ## ‡ap. 73-85 :‡bdiag., maps.
500 ## ‡aPolish Polar Research. Vol. 9(1) :73-85 (1988).
520 3# ‡aThree altitudinal zones of occurrence identified, dependent on influence of microclimate of adjacent glaciers. Zone A (<150 m a.s.l.) is not influenced by glacier, zone B (150 to 350 m a.s.l.) is influenced by glacier snouts, zone C (>350 m a.s.l.) is influenced by firn fields. Main development in this area occurred during Little Ice Age.
650 07 ‡a551.435.646 -- Screes.‡2udc
650 07 ‡a551.343.4 -- Rock glaciers.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(*32) -- Svalbard.‡2udc
651 #7 ‡a(*324) -- Spitsbergen.‡2udc
700 1# ‡aDzierzek, Jan.
773 0# ‡7nnas ‡tPolish Polar Research. ‡gVol. 9(1) (1988) ‡wSPRI-60789
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240225