Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8868090 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2018 | 53 Pages |
Abstract
Fuerteventura has been vertically stable since the last interglacial period, and the sedimentology of the deposits precludes an origin from tsunamis or storms. This island is in a far-field region in terms of glacial isostatic adjustment (GIA) processes. Here, we suggest that the deposits may be related to GIA and ice mass losses effects in the Southern Hemisphere.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
JoaquÃn Meco, Alejandro Lomoschitz, Ángel RodrÃguez, Antonio J.G. Ramos, Juan F. Betancort, Josep Coca,