Denver / New York / Canberra / Rome / Oshkosh Oshkosh / Orville / /
Company
Marshall Nunatak / Cambridge University Press / Kellogg / LeMay Group / Latady Formation / Thomson / Cambridge Cambridge University Press / Oshkosh / /
Continent
South America / Antarctica / /
Country
New Zealand / United States / /
Facility
Siple Station / University of Wisconsin Press / Columbia University / Geology University of Wisconsin / Botany University of Texas / University of Texas / I.W.D. DALZIEL* Lamont-Doherty Geological Observatory / University of Wisconsin / Byrd Station / University Palisades / /
IndustryTerm
volcanic conglomerate / /
NaturalFeature
Jone Mountains / Behrendt Mountains / Orville coast / Lassiter coast / Ellsworth Mountains / Jones Mountains / Mount Benkert / Merrick Mountains / Thurston Island / Bellingshausen Sea / Pacific Coast / Mount Harry / Whitmore Mountains/Thiel Mountains / Pensacola Mountains / Island British / Mount Peterson / Alexander Island / /
Organization
English Coast / Cambridge University / Columbia University / University of Wisconsin Press / University of Texas at Austin / National Science Foundation / National Science Foundation Division of Polar Programs / Columbia University / New York / C.T. GEE Department / T.S. LAUDON Department / Botany University / United States Navy / Australian Academy of Science / University of Wisconsin / International Association of Volcanology and Chemistry of the Earth / U.S. Government Printing Office / K.S. Kellogg / /
Person
T.S. Laudon / W.R. Vennum / Alexander Island British / Theodore Delevoryas / J.M. Boyles / P.D. Rowley / D.J. Lidke / Marshall Nunatak / Robert J. Pankhurst / K.L. Milliken / Carole T. Gee / P.L. Williams / Gondwanaland / Bryan C. Storey / Ian W. D. Dalziel / Anne Grunow / Ed Murton / /
Position
Captain / /
ProvinceOrState
Texas / Wisconsin / New York / Colorado / /
PublishedMedium
Journal of Paleontology / /
Region
antarctic / western Antarctica / East Antarctica / British Antarctic / West Antarctica / /
The channel-fill deposits at Mount Benkert appear to represent fluviatile sedimentary rocks derived from hyaloclastites; the huge channel forms that compose the main outcrop, the associated mesoscopic internal bedding fo