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Record #143348:

Nowe fakty dotyczące genezy zagłȩbień wytopiskowych na sandrach przedpola lodowca Skeidarár (Islandia) / Paweł Molewski.

Title: Nowe fakty dotyczące genezy zagłȩbień wytopiskowych na sandrach przedpola lodowca Skeidarár (Islandia) / Paweł Molewski.
Translated title: New facts relating to the genesis of the kettle holes on the sandurs of the Skeidarár Glacier foreland (Iceland).
Author(s): Molewski, Paweł.
Date: 1997.
Language: Polish.
In: Przegląd Geograficzny. (1997.), LXVIII(3-4) (1997)
Abstract: Kettle holes are either isolated or form clumps. Shapes are very regular, most often conical or bowl shaped. Diameter can be from 0.5 m to over 60 m., slopes from 1 to 35 degrees. All kettle holes occur along main lines of water outflow, with largest in central part. Greatest concentration is in marginal part of sandurs. They are result of degradation of ice blocks transported during jökulhlaups. Author studied different sequence in case of holes in young sandurs.
Notes:

Przegląd Geograficzny. LXVIII(3-4) :405-426 (1997).

English summary p.425, English captions.

Keywords: 551.332.5 -- Glacial landforms.
551.332.55 -- Ice-contact features.
551.332.58 -- Outwash plains.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*35) -- Iceland.
SPRI record no.: 143348

MARCXML

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005 20221001145449.0
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035 ## ‡aSPRI-143348
040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡apol
100 1# ‡aMolewski, Paweł.
242 10 ‡aNew facts relating to the genesis of the kettle holes on the sandurs of the Skeidarár Glacier foreland (Iceland).‡yeng
245 10 ‡aNowe fakty dotyczące genezy zagłȩbień wytopiskowych na sandrach przedpola lodowca Skeidarár (Islandia) /‡cPaweł Molewski.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1997.
300 ## ‡ap. 405-426 :‡bill., table.
500 ## ‡aPrzegląd Geograficzny. LXVIII(3-4) :405-426 (1997).
500 ## ‡aEnglish summary p.425, English captions.
520 3# ‡aKettle holes are either isolated or form clumps. Shapes are very regular, most often conical or bowl shaped. Diameter can be from 0.5 m to over 60 m., slopes from 1 to 35 degrees. All kettle holes occur along main lines of water outflow, with largest in central part. Greatest concentration is in marginal part of sandurs. They are result of degradation of ice blocks transported during jökulhlaups. Author studied different sequence in case of holes in young sandurs.
546 ## ‡aIn Polish.
650 07 ‡a551.332.5 -- Glacial landforms.‡2udc
650 07 ‡a551.332.55 -- Ice-contact features.‡2udc
650 07 ‡a551.332.58 -- Outwash plains.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*35) -- Iceland.‡2udc
773 0# ‡7nnas ‡tPrzegląd Geograficzny. ‡gLXVIII(3-4) (1997) ‡wSPRI-11780
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221001