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Record #170814:

Drainage of ice-contact Miage lake (Mont Blanc massif, Italy) in September 2004 / Philip Deline, and 6 others.

Title: Drainage of ice-contact Miage lake (Mont Blanc massif, Italy) in September 2004 / Philip Deline, and 6 others.
Author(s): Deline, Philip.
Date: 2003.
In: Geografia Fisica e Dinamica Quaternaria. (2003.), Vol. 27(2) (2003)
Abstract: Reports topographic survey and preliminary observations made immediately after drainage of ice-contact lake Miage in September 2004. Describes morphologies of lake bed and ice dam and recent evolution of lake, which has existed at least since 18th Century. Uses DEM to illustrate drainage event and constructs chronology. Concludes drainage occurred in two stages. Initial rapid water loss was due to increased outflow between glacier sole and till substrate. Lowering of lake surface left separate ponds isolated from subglacial drainage route and subsequent slower leakage took place over weeks through permeable till. Does not believe such events pose hazard.
Notes:

Geografia Fisica e Dinamica Quaternaria. Vol. 27(2) :113-119 (2003).

Italian abstract.

Keywords: 551.32 -- Glaciology.
551.332.56 -- Lakes, ice-dammed. Glacial lakes. Disruption of water drainage.
556.555.3 -- Lakes, inflow and outflow.
551.324.22 -- Glaciers: Glacier de Miage.
551.324.86 -- Glacier streams.
551.332.2 -- Drift, glacial. Deposits.
528.93 -- Cartography, topographical.
E11 -- Glaciology: glaciohydrology.
(45) -- Italy.
(234.3) -- Alps.
SPRI record no.: 170814

MARCXML

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100 1# ‡aDeline, Philip.
245 10 ‡aDrainage of ice-contact Miage lake (Mont Blanc massif, Italy) in September 2004 /‡cPhilip Deline, and 6 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2003.
300 ## ‡ap. 113-119 :‡bill., maps.
500 ## ‡aGeografia Fisica e Dinamica Quaternaria. Vol. 27(2) :113-119 (2003).
500 ## ‡aItalian abstract.
520 3# ‡aReports topographic survey and preliminary observations made immediately after drainage of ice-contact lake Miage in September 2004. Describes morphologies of lake bed and ice dam and recent evolution of lake, which has existed at least since 18th Century. Uses DEM to illustrate drainage event and constructs chronology. Concludes drainage occurred in two stages. Initial rapid water loss was due to increased outflow between glacier sole and till substrate. Lowering of lake surface left separate ponds isolated from subglacial drainage route and subsequent slower leakage took place over weeks through permeable till. Does not believe such events pose hazard.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.332.56 -- Lakes, ice-dammed. Glacial lakes. Disruption of water drainage.‡2udc
650 07 ‡a556.555.3 -- Lakes, inflow and outflow.‡2udc
650 07 ‡a551.324.22 -- Glaciers: Glacier de Miage.‡2udc
650 07 ‡a551.324.86 -- Glacier streams.‡2udc
650 07 ‡a551.332.2 -- Drift, glacial. Deposits.‡2udc
650 07 ‡a528.93 -- Cartography, topographical.‡2udc
650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local
651 #7 ‡a(45) -- Italy.‡2udc
651 #7 ‡a(234.3) -- Alps.‡2udc
773 0# ‡7nnas ‡tGeografia Fisica e Dinamica Quaternaria. ‡gVol. 27(2) (2003) ‡wSPRI-57546
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917 ## ‡aUnenhanced record from Muscat, imported 2019
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