Results from geomorphological investigations in the catchment of Lago di Mezzano (VT) have been compared with data from a long sediment core sampled in the lake center. The palaeoenvironmental reconstruction was based on vegetation (deduced from pollen and microcharcoal) and hydrological (reconstructed through lake-level) changes .
|Pages (from-to)||129 - 131|
|Number of pages||3|
|Journal||Alpine and Mediterranean Quaternary|
|Publication status||Published - 2011|
All Science Journal Classification (ASJC) codes
- Earth-Surface Processes