(Table 4) Clast lithology and weathering characteristics of Reedy Glacier deposits
| Cobertura |
MEDIAN LATITUDE: -85.955000 * MEDIAN LONGITUDE: -129.275000 * SOUTH-BOUND LATITUDE: -85.990000 * WEST-BOUND LONGITUDE: -132.500000 * NORTH-BOUND LATITUDE: -85.920000 * EAST-BOUND LONGITUDE: -126.050000 * MINIMUM ELEVATION: 1400.0 m * MAXIMUM ELEVATION: 2160.0 m |
|---|---|
| Data(s) |
26/02/2010
|
| Formato |
text/tab-separated-values, 360 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.808063 doi:10.1594/PANGAEA.808063 |
| 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 | #Clasts; Description; Elevation of event; Event label; Latitude of event; Lithologic unit/sequence; Lithology/composition/facies; Longitude of event; MULT; Multiple investigations; Polygon_Spur; Quartz_Hills; Transantarctic Mountains; Ventifacts |
| Tipo |
Dataset |
