[
    {
        "id": "authors:echnm-d6q44",
        "collection": "authors",
        "collection_id": "echnm-d6q44",
        "cite_using_url": "https://resolver.caltech.edu/CaltechAUTHORS:20140808-160110331",
        "type": "article",
        "title": "Additions to classical sequence of Pleistocene glaciations, Sierra Nevada, California",
        "author": [
            {
                "family_name": "Sharp",
                "given_name": "Robert P.",
                "clpid": "Sharp-R-P"
            },
            {
                "family_name": "Birman",
                "given_name": "Joseph H.",
                "clpid": "Birman-J-H"
            }
        ],
        "abstract": "Two additions are proposed to Black-welder's classical sequence of four Pleistocene glaciations (Tioga, Tahoe, Sherwin, and McGee) of the Sierra Nevada. The younger, the Tenaya, lies between Tioga and Tahoe, giving a three-fold subdivision of the Wisconsin. The older, named Mono Basin, fills the long-recognized gap between Tahoe and Sherwin; it is possibly Illinoian. Evidence for the Mono Basin glaciation is scanty because its ice streams were less extensive than the subsequent Tahoe glaciers.",
        "doi": "10.1130/0016-7606(1963)74[1079:ATCSOP]2.0.CO;2",
        "issn": "0016-7606",
        "publisher": "Geological Society of America",
        "publication": "Geological Society of America Bulletin",
        "publication_date": "1963-08",
        "series_number": "8",
        "volume": "78",
        "issue": "8",
        "pages": "1079-1086"
    }
]