Beardmore Glacier

Results: 35



#Item
1

PDF Document

Add to Reading List

Source URL: antarcticanz.govt.nz

Language: English - Date: 2013-08-06 00:53:12
2fern possesses a mesarch, amphiphloic siphonostele embedded in a parenchymatous cortex. The pith is often scierified. In these stems there is relatively little support tissue. Only the vascular strand and thickened cells

fern possesses a mesarch, amphiphloic siphonostele embedded in a parenchymatous cortex. The pith is often scierified. In these stems there is relatively little support tissue. Only the vascular strand and thickened cells

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 15:38:50
3silts tone/mudstone and interbedded fine-grained sandstone. Internally, the coarser sandstone units consist of scour-bounded cosets of 0.2- to 0.5-meter thick trough cross-beds. In some cases, thin siltstone drapes have

silts tone/mudstone and interbedded fine-grained sandstone. Internally, the coarser sandstone units consist of scour-bounded cosets of 0.2- to 0.5-meter thick trough cross-beds. In some cases, thin siltstone drapes have

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 18:12:12
4From what can be seen, however, it is apparent that the collection contains at least the top portion of a skull, over 20 vertebrae, numerous ribs, portions of at least eight limb bones including a humerus and part of a f

From what can be seen, however, it is apparent that the collection contains at least the top portion of a skull, over 20 vertebrae, numerous ribs, portions of at least eight limb bones including a humerus and part of a f

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 20:35:19
5canic detritus, derived from a caic-alkaline arc along the paleoPacific margin, became the principal component in sandstone. This change from cratonic to orogenic provenance was the result of a shift in the basin axis to

canic detritus, derived from a caic-alkaline arc along the paleoPacific margin, became the principal component in sandstone. This change from cratonic to orogenic provenance was the result of a shift in the basin axis to

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 07:07:21
6VXE-6 and the ITT/Antarctic Services, Inc., personnel at the Beardmore Camp. We would also like to thank Richard Arculus for his assistance with the X-ray fluorescence analyses which were performed at the University of M

VXE-6 and the ITT/Antarctic Services, Inc., personnel at the Beardmore Camp. We would also like to thank Richard Arculus for his assistance with the X-ray fluorescence analyses which were performed at the University of M

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 07:02:24
7water or moisture was available for plant survival during these episodes. The apparently low number of surviving species probably represents the last vestiges of land-plant vegetation in Antarctica before the Pleistocene

water or moisture was available for plant survival during these episodes. The apparently low number of surviving species probably represents the last vestiges of land-plant vegetation in Antarctica before the Pleistocene

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 18:12:45
8We wish to express our sincere appreciation to the other members of the Vanderbilt/Ohio State University research team, our fellow scientists from the Beardmore South camp, and the civilian and military support personnel

We wish to express our sincere appreciation to the other members of the Vanderbilt/Ohio State University research team, our fellow scientists from the Beardmore South camp, and the civilian and military support personnel

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 18:12:34
9Laird, M.G., G.D. Mansergh, an J.M. ChappellGeology of the central Nimrod Glacier area, Antarctica. New Zealand Journal of Geology and Geophysics, 14(3), Rees, M.N., A.J. Rowell, and B.R. PrattTh

Laird, M.G., G.D. Mansergh, an J.M. ChappellGeology of the central Nimrod Glacier area, Antarctica. New Zealand Journal of Geology and Geophysics, 14(3), Rees, M.N., A.J. Rowell, and B.R. PrattTh

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 18:13:55
10References Barrett, P. JStratigraphy and petrology of the mainly flu viatile Permian and Triassic Beacon rocks, Beardmore Glacier area Antarctica. (Institute of Polar Studies Report 34.) Columbus: Ohio State Univ

References Barrett, P. JStratigraphy and petrology of the mainly flu viatile Permian and Triassic Beacon rocks, Beardmore Glacier area Antarctica. (Institute of Polar Studies Report 34.) Columbus: Ohio State Univ

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 05:13:37