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Late Pleistocene Glacial Events in the Central Apennines, Italy

TitleLate Pleistocene Glacial Events in the Central Apennines, Italy
Publication TypeArticolo su Rivista peer-reviewed
Year of Publication1997
AuthorsGiraudi, C., and Frezzotti M
JournalQuaternary Research
Volume48
Pagination280-290
ISSN00335894
KeywordsApennines, Aquila, glaciation, Gran Sasso Massif, Italy, Last Glacial Maximum, Pleistocene (late)
Abstract

The study of glacial evidence in the Gran Sasso Massif of the Central Apennines, Italy, has allowed the last maximum advance and the subsequent stadial phases to be dated and the mean annual temperature and quantity of precipitation in the form of snow to be assessed for a number of periods. The glaciers probably reached their maximum extension (Campo Imperatore Stade) ca. 22,600 14C yr B.P. and started to retreat ca. 21,000 yr B.P., leaving behind three recessional moraines. After a first interstade (Fornaca Interstade), the Fontari Stade appears to have taken place shortly after 16,000 yr ago. Ca. 15,000 yr ago the glacier started retreating, leaving behind four more recessional moraines. An interstade (Venacquaro Interstade) preceded the Mount Aquila Stade, datable at ca. 11,000 yr B.P. A strong correlation is evident between the glacial phases on land and the isotopic variations in cores from the Tyrrhenian Sea. © 1997 University of Washington.

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URLhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-0031394035&partnerID=40&md5=a1ed008a717571ee975a6aa646bfb019
Citation KeyGiraudi1997280