Holocene glacier fluctuations in the Italian Alps - Medclivar

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Ruitor gl.was smallerthan now10.3-1010 Kyr BPBuried peat bognear the glacierfront*2510 m a.s.l.*Basalpeat10 270 – 9 950cal yr BPmax Little Ice Ageglacier extent(1820 ?)N1 km2003
The second period (10.2 ÷ 5 kyr BP)was characterized by a generally reducedglacier activity.In many mountain chains (NorthernH.)glaciers where in a prevailing retreatedcondition and locally they entirelydisappeared.In the Italian Alps a representative sectionis present near the front of the Ruitor Glacier(Western Alps),where a peat bog buried byglacigenic sediments has been found at2510 m a.s.l.
Page 1 and 2: Mediterranean Climate: from Past to
Page 3 and 4: Mountain glaciers, mainly composed
Page 5 and 6: Subdivisions of the HoloceneOn the
Page 7 and 8: 10 Be weighted mean age: : 11 340
Page 9: NLa MareGlacierMax LIA glacierexten
Page 13 and 14: 9 070 ±120÷ 4 945 ±6514 C yr BP~
Page 15 and 16: Miagelateral moraineCombal outwash
Page 17 and 18: advancingre-formingCalderone glacie
Page 19 and 20: The Little Ice Age in the Italian A
Page 21 and 22: The Little Ice Age in the AlpsThree
Page 23 and 24: The Little Ice Age in the Italian A
Page 25 and 26: Holocene fluctuations of Italian gl

Holocene glacier fluctuations in the Italian Alps - Medclivar

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