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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #117034:

La gélivation des parois rocheuses dans une glaciére du Jura neuchâtelois / André Pancza.

Title: La gélivation des parois rocheuses dans une glaciére du Jura neuchâtelois / André Pancza.
Translated title: Freezing of the rock walls in a glacier of the Neuchâtel Jura.
Author(s): Pancza, André.
Date: 1992.
Language: French.
In: Permafrost and Periglacial Processes. (1992.), Vol. 3(1) (1992)
Abstract: Study of action of intense cold on water-saturated rock in ice cave of Monlési, French Alps. During Quaternary, it is possible that most karstic cavities in Jura mountains contained ice bodies, which suggests that karstic depressions are polygenetic in origin.
Notes:

Permafrost and Periglacial Processes. Vol. 3(1) :49-54 (1992).

English abstract, p. 49.

Keywords: 551.34 -- Geocryology. Frozen ground.
551.342 -- Frost shattering.
551.584.65 -- Microclimates in caves, mines and tunnels.
E8 -- Glaciology: frost action and permafrost.
(44) -- France.
(234.3) -- Alps.
SPRI record no.: 117034

MARCXML

LDR 01292naa#a2200000#a#4500
001 SPRI-117034
005 20240419044727.0
007 ta
008 240419s1992####xx#a##|##|###|0||#0|fre#d
035 ## ‡aSPRI-117034
040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡afre
100 1# ‡aPancza, André.
242 10 ‡aFreezing of the rock walls in a glacier of the Neuchâtel Jura.‡yeng
245 13 ‡aLa gélivation des parois rocheuses dans une glaciére du Jura neuchâtelois /‡cAndré Pancza.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1992.
300 ## ‡ap. 49-54 :‡bill., diags.
500 ## ‡aPermafrost and Periglacial Processes. Vol. 3(1) :49-54 (1992).
500 ## ‡aEnglish abstract, p. 49.
520 3# ‡aStudy of action of intense cold on water-saturated rock in ice cave of Monlési, French Alps. During Quaternary, it is possible that most karstic cavities in Jura mountains contained ice bodies, which suggests that karstic depressions are polygenetic in origin.
546 ## ‡aIn French.
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.342 -- Frost shattering.‡2udc
650 07 ‡a551.584.65 -- Microclimates in caves, mines and tunnels.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(44) -- France.‡2udc
651 #7 ‡a(234.3) -- Alps.‡2udc
773 0# ‡7nnas ‡tPermafrost and Periglacial Processes. ‡gVol. 3(1) (1992) ‡wSPRI-102743
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240419