Vote for your favorite mineral in #MinCup25! - Baryte vs. Hematite
It's a heavyweight match between industrial powerhouses as soft #baryte competes against rusty red #hematite.
Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Osborn, Henry Fairfield (1922) Pliocene (Tertiary) and Early Pleistocene (Quaternary) Mammalia of East Anglia, Great Britain, in Relation to the Appearance of Man. Geological Magazine, 59 (10) 433-441 doi:10.1017/s0016756800109227

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitlePliocene (Tertiary) and Early Pleistocene (Quaternary) Mammalia of East Anglia, Great Britain, in Relation to the Appearance of Man
JournalGeological Magazine
AuthorsOsborn, Henry FairfieldAuthor
Year1922 (October)Volume59
Issue10
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800109227
Generate Citation Formats
Mindat Ref. ID280189Long-form Identifiermindat:1:5:280189:0
GUID0
Full ReferenceOsborn, Henry Fairfield (1922) Pliocene (Tertiary) and Early Pleistocene (Quaternary) Mammalia of East Anglia, Great Britain, in Relation to the Appearance of Man. Geological Magazine, 59 (10) 433-441 doi:10.1017/s0016756800109227
Plain TextOsborn, Henry Fairfield (1922) Pliocene (Tertiary) and Early Pleistocene (Quaternary) Mammalia of East Anglia, Great Britain, in Relation to the Appearance of Man. Geological Magazine, 59 (10) 433-441 doi:10.1017/s0016756800109227
In(1922, October) Geological Magazine Vol. 59 (10) Cambridge University Press (CUP)
Abstract/NotesIn studying the evolution and distribution of the Proboscidea and the arrival of man in Great Britain (Osborn, 1922, 1922a, 1922b), the writer has recently had occasion to review the faunal researches of Lydekker and Newton, and the collection of Mr. A. C. Savin, in connexion with the very interesting question of the geologic correlation of Great Britain with the Upper Pliocene fauna of Europeto the south-east, and of the Scandinavian Glaciation I on the north, with the advent of the northern forest, the boreal, and the Arctic mammal fauna of Great Britain.


See Also

These are possibly similar items as determined by title/reference text matching only.

 
and/or  
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2025, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: September 19, 2025 13:18:55
Go to top of page