| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1041663 | Quaternary International | 2014 | 4 Pages |
Abstract
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.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Margot Böse, Robert Hebenstreit, Jacob Hardt,