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Evidence for a “Little Ice Age” Glacial Advance within the Antarctic Peninsula - Examples from Glacially-Overrun Raised Beaches

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dc.contributor.authorDeWitt, Regina
dc.contributor.authorSimms, Alexander R.
dc.contributor.authorBentley, Michael J.
dc.contributor.authorSimkins, Lauren M.
dc.contributor.authorZurbuchen, Julie
dc.contributor.authorReynolds, Laura C.
dc.contributor.authorThomas, Elizabeth R.
dc.date.accessioned2022-10-25T14:03:56Z
dc.date.available2022-10-25T14:03:56Z
dc.date.issued2021-10-02
dc.identifier.doi10.1016/j.quascirev.2021.107195
dc.identifier.issn0277-3791
dc.identifier.urihttp://hdl.handle.net/10342/11658
dc.language.isoen_USen_US
dc.subjectNeoglacialen_US
dc.subjectAntarcticaen_US
dc.subjectClimate changeen_US
dc.titleEvidence for a “Little Ice Age” Glacial Advance within the Antarctic Peninsula - Examples from Glacially-Overrun Raised Beachesen_US
dc.typeArticleen_US
ecu.journal.nameQuaternary Science Reviewsen_US
ecu.journal.volume271en_US

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