Holocene glacier fluctuations in the Italian Alps - Medclivar

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Niederjoch/Giogo Basso Gl.(Baroni & Orombelli, 1995)Ötzi(~ 5200 cal BP)The mummified corpse of theiceman rested directly on bedrock,suggesting that, after death, itbecame buried in snow on ice-freeground ~ 5.2 kyr BP and since thenremained continuously preservedin cold ice, frozen to bedrock at theupper edge of the Giogo Basso Gl.(EasternAlps).At about 5.2 kyr BP, for an abrupt climate change, GiogoBasso glacier started to re-form near the Tisa Pass in itsupper accumulation basin.
advancingre-formingCalderone glacierabsentIn the Apennines the CalderoneGlacier, possibly still presentduring the Late Glacial, disappea-red in the Early Holocene, , andre-formedat 4.5-4.34.3 kyr BP(Giraudiet al., 2011)possiblypresent
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 and 10: NLa MareGlacierMax LIA glacierexten
Page 11 and 12: The second period (10.2 ÷ 5 kyr BP
Page 13 and 14: 9 070 ±120÷ 4 945 ±6514 C yr BP~
Page 15: Miagelateral moraineCombal outwash
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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