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(1887) The Date of the Ice Age. Geological Magazine, S. 3 Vol. 4 (11) 523-524 doi:10.1017/s0016756800190533

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Reference TypeJournal (article/letter/editorial)
TitleThe Date of the Ice Age
JournalGeological Magazine
Year1887 (November)Series:Volume3:4
Issue11
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800190533
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Mindat Ref. ID265287Long-form Identifiermindat:1:5:265287:4
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Full Reference(1887) The Date of the Ice Age. Geological Magazine, S. 3 Vol. 4 (11) 523-524 doi:10.1017/s0016756800190533
Plain Text(1887) The Date of the Ice Age. Geological Magazine, S. 3 Vol. 4 (11) 523-524 doi:10.1017/s0016756800190533
In(1887, November) Geological Magazine S. 3 Vol. 4 (11) Cambridge University Press (CUP)

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(1887) Re “Explosive Slickensides”. Geological Magazine, S. 3 Vol. 4 (11) 522-523 doi:10.1017/s0016756800190521
(1887) Dr. Hinde on the Origin of Carboniferous Chert. Geological Magazine, S. 3 Vol. 4 (11) 524-526 doi:10.1017/s0016756800190545
(1886) The Volcanic Eruption of New Zealand. Geological Magazine, S. 3 Vol. 3 (11) 523-524 doi:10.1017/s0016756800466811
(1866) To the Editor of the Geological Magazine. Geological Magazine, S. 1 Vol. 3 (29) 523-524 doi:10.1017/s0016756800198267
(1887) III.—The Work of Ice-Sheets. Geological Magazine, S. 3 Vol. 4 (4) 151-155 doi:10.1017/s0016756800196396
(1907) Nomenclature of Australian Silurian Ophicrids. Geological Magazine, S. 5 Vol. 4 (11) 523-524 doi:10.1017/s0016756800134004
(1893) IV.—Monographs and Bulletins of the United States Geological Survey. Geological Magazine, S. 3 Vol. 10 (11) 523-524 doi:10.1017/s001675680017431x
(1883) Continent Formation. Geological Magazine, S. 2 Vol. 10 (11) 523-524 doi:10.1017/s0016756800167135
(1895) Dr. Croll's Theory of the Ice Age. Geological Magazine, S. 4 Vol. 2 (3) 142 doi:10.1017/s0016756800006038
(1881) The “Lower Keuper Sandstone” or “Basement Beds.”. Geological Magazine, S. 2 Vol. 8 (11) 523-524 doi:10.1017/s0016756800129115
(1912) V.—Cambridge County Geographies. Geological Magazine, S. 5 Vol. 9 (11) 523-524 doi:10.1017/s0016756800115948
 
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