| _version_ | 1867168093323657216 |
|---|---|
| author | Zoltai, S C |
| author_facet | Zoltai, S C |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | A group of nine pingos occurs in the valley of a glacial meltwater river. The pingos rise from a plain of low-center polygons. Some pingos have a typical cone shape, but others are linear, apparently centered on ice wedges . The occurrence of most pingos at the junction of oversize ice wedge polygon ridges suggests that the injection of water and the segregation of ice occurred along pathways provided by the ice wedges. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_746730 |
| institution | PANGAEA |
| language | en |
| publishDate | 1983 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Tab. 1: Approximate dimension of the pingos Zoltai, S C 9Pingos; Bylot Island, North West Territories, Canada; Comment; Geological mapping; GEOMAP; Height; Length; ORDINAL NUMBER; Surface description; Width A group of nine pingos occurs in the valley of a glacial meltwater river. The pingos rise from a plain of low-center polygons. Some pingos have a typical cone shape, but others are linear, apparently centered on ice wedges . The occurrence of most pingos at the junction of oversize ice wedge polygon ridges suggests that the injection of water and the segregation of ice occurred along pathways provided by the ice wedges. |
| title | Tab. 1: Approximate dimension of the pingos |
| topic | 9Pingos; Bylot Island, North West Territories, Canada; Comment; Geological mapping; GEOMAP; Height; Length; ORDINAL NUMBER; Surface description; Width |
| url | https://doi.org/10.1594/PANGAEA.746730 |