(Table 3) Sedimentology and weathering characteristics of drift units at Reedy Glacier
| Cobertura |
MEDIAN LATITUDE: -85.992233 * MEDIAN LONGITUDE: -129.850000 * SOUTH-BOUND LATITUDE: -86.066700 * WEST-BOUND LONGITUDE: -132.500000 * NORTH-BOUND LATITUDE: -85.920000 * EAST-BOUND LONGITUDE: -126.050000 * MINIMUM ELEVATION: 800.0 m * MAXIMUM ELEVATION: 2160.0 m |
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| Data(s) |
26/02/2010
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| Formato |
text/tab-separated-values, 154 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.808061 doi:10.1594/PANGAEA.808061 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.808064 Bromley, Gordon RM; Hall, Brenda L; Stone, John O; Conway, Howard; Todd, Claire E (2010): Late Cenozoic deposits at Reedy Glacier, Transantarctic Mountains: implications for former thickness of the West Antarctic Ice Sheet. Quaternary Science Reviews, 29(3-4), 384-398, doi:10.1016/j.quascirev.2009.07.001 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Caloplaca_Hills; Comment; Depth, relative; Description; Elevation of event; Event label; Latitude of event; Layer thickness; Lithologic unit/sequence; Lithology/composition/facies; Longitude of event; MULT; Multiple investigations; Observation; Polygon_Spur; Quartz_Hills; Transantarctic Mountains |
| Tipo |
Dataset |
