| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1044171 | Quaternary International | 2008 | 9 Pages |
Abstract
Coarse-grained glacial, outwash and fluvial sediments (Colleretto Castelnuovo, S. Defendente, Case Musso, Pagliero, Serra and Piverone Alloformations) are described in the upper part of the continental succession. They consist of undeformed sediments deposited during Middle to Late Pleistocene. These sediments indicate the presence of small local glaciers along the current valley trends. The terracing ratios among the different units and their small thicknesses indicate subsequent differential uplift.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Maria Gabriella Forno, Simona Ferrando,