Abstract
Upper Pleistocene (MIS 4-2) loess sequences occur in most of continental Europe and in Northern Italy along the Po Plain Loess Basin. Loess is distributed along the flanks of the Po Plain and was deposited on glacial deposits, fluvial terraces, uplifted isolated hills, karst plateaus, slopes and basins of secondary valleys. Loess bodies are generally tiny and affected by pedogenesis, being locally slightly reworked by slope processes and bioturbation. Notwithstanding, loess in the Po Plain is an important archive of paleoenviron-mental record and its mapping provides new insights in paleoenvironmental and palaeoseismic reconstructions of Northern Italy.
Original language | English |
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Pages (from-to) | 253-256 |
Number of pages | 4 |
Journal | Alpine and Mediterranean Quaternary |
Volume | 31 |
Issue number | 1 |
State | Published - 2018 |
Externally published | Yes |
Bibliographical note
Publisher Copyright:© 2010 AIQUA - Associazione Italiana per lo Studio del Quaternario e EMMEVI - Servizio Congressi SPA.
Keywords
- Loess
- Mapping
- Po Plain loess basin
- Upper Pleistocene