A deformation till at Hohuan Shan, Taiwan
At the Hohuan Shan, a mountain massif well above 3400 m in altitude in northern Taiwan, a glacial deformation till has been observed in the uppermost part of the catchment of the Hohuan River. The sediment sequence above the slate bedrock is evidence of a late Pleistocene to early Holocene glaciatio...
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| Veröffentlicht in: | Quaternary international 2014-02, Vol.321, p.55-58 |
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| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | eng |
| Online-Zugang: | Volltext |
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| Zusammenfassung: | At the Hohuan Shan, a mountain massif well above 3400 m in altitude in northern Taiwan, a glacial deformation till has been observed in the uppermost part of the catchment of the Hohuan River. The sediment sequence above the slate bedrock is evidence of a late Pleistocene to early Holocene glaciation as dated in neighbouring mountain massifs, and is discussed in context with the results from a nearby outcrop with dated Holocene slope sediments. |
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| ISSN: | 1040-6182 1873-4553 |
| DOI: | 10.1016/j.quaint.2013.11.019 |