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Record #158874:

Late Glacial to Holocene deglaciation of the Colle del Vei del Bouc-Colle del Sabbione area (Argentera massif, Maritime Alps, Italy-France) / Walter Finsinger, Adriano Ribolini.

Title: Late Glacial to Holocene deglaciation of the Colle del Vei del Bouc-Colle del Sabbione area (Argentera massif, Maritime Alps, Italy-France) / Walter Finsinger, Adriano Ribolini.
Author(s): Finsinger, Walter.
Ribolini, Adriano.
Date: 2001.
In: Geografia Fisica e Dinamica Quaternaria. (2001.), Vol. 24(2) (2001)
Abstract: Italian and French summaries. Finds through geomorphological mapping and pollen analysis three pre-Little Ice Age glacial phases and two rock-glacier generations in area of French-Italian Alps and relates them to global climatic oscillations. Proposes quantitative reconstruction of climate during glacier advances. Permafrost still characterises Subboreal rock glaciers and flow units above 2600 m, formed during Younger Dryas.
Notes:

Geografia Fisica e Dinamica Quaternaria. Vol. 24(2) :141-156 (2001).

Keywords: 551.336 -- Ice ages.
551.794 -- Holocene.
551.32 -- Glaciology.
551.324 -- Land ice.
551.324.63 -- Land ice, advance and retreat.
551.343.4 -- Rock glaciers.
551.345 -- Permafrost. Cryopedology.
551.321 -- Glaciological methods and instruments.
581.081.3 -- Pollen analysis.
551.4 -- Geomorphology.
E7 -- Glaciology: glacial geology and ice ages.
(44) -- France.
(45) -- Italy.
(234.3) -- Alps.
SPRI record no.: 158874

MARCXML

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245 10 ‡aLate Glacial to Holocene deglaciation of the Colle del Vei del Bouc-Colle del Sabbione area (Argentera massif, Maritime Alps, Italy-France) /‡cWalter Finsinger, Adriano Ribolini.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2001.
300 ## ‡ap. 141-156 :‡bill., diags., tables, map.
500 ## ‡aGeografia Fisica e Dinamica Quaternaria. Vol. 24(2) :141-156 (2001).
520 3# ‡aItalian and French summaries. Finds through geomorphological mapping and pollen analysis three pre-Little Ice Age glacial phases and two rock-glacier generations in area of French-Italian Alps and relates them to global climatic oscillations. Proposes quantitative reconstruction of climate during glacier advances. Permafrost still characterises Subboreal rock glaciers and flow units above 2600 m, formed during Younger Dryas.
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc
650 07 ‡a551.343.4 -- Rock glaciers.‡2udc
650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc
650 07 ‡a551.321 -- Glaciological methods and instruments.‡2udc
650 07 ‡a581.081.3 -- Pollen analysis.‡2udc
650 07 ‡a551.4 -- Geomorphology.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(44) -- France.‡2udc
651 #7 ‡a(45) -- Italy.‡2udc
651 #7 ‡a(234.3) -- Alps.‡2udc
700 1# ‡aRibolini, Adriano.
773 0# ‡7nnas ‡tGeografia Fisica e Dinamica Quaternaria. ‡gVol. 24(2) (2001) ‡wSPRI-57546
917 ## ‡aUnenhanced record from Muscat, imported 2019
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