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
ABSTRACT The upper Pleistocene loess-paleosol sequence of Val Sorda (northeastern Italy
The interactions among Quaternary (paleo-) soil-forming, erosion, re-deposition and geomorphic proce...
Upper Pleistocene loess/palaeosol sequences provide excellent high-resolution terrestrial archives o...
Upper Pleistocene (MIS 4-2) loess sequences occur in most of continental Europe and in Northern Ital...
Upper Pleistocene (MIS 4\u20132) loess sequences occur in most of continental Europe and in Northern...
Loess represents one of the main paleoenvironmental archives recording Quaternary environmental chan...
Purpose At the northern fringe of the Po Plain (northern Italy), several isolated hills exist, corre...
The significance of two loess profiles located in the Ghiardo area (Reggio Emilia, northern Italy) a...
Loess deposits at the Apennine fringe lie on the of terraces cut into early-Middle Pleistocene conti...
The significance of two loess profiles located in the Ghiardo area (Reggio Emilia, northern Italy) a...
The Bagaggera sequence consists of two Late Pleistocene loesses superimposed on the top of Middle Pl...
Purpose At the northern fringe of the Po Plain (northern Italy), several isolated hills exist, corr...
A representative loess-paleosol sequence has been identified and studied by mineralogical and microm...
In the Castenedolo hill a stratigraphic sequence ranging from the Early Pleistocene to the Upper Ple...
ABSTRACT The upper Pleistocene loess-paleosol sequence of Val Sorda (northeastern Italy
The interactions among Quaternary (paleo-) soil-forming, erosion, re-deposition and geomorphic proce...
Upper Pleistocene loess/palaeosol sequences provide excellent high-resolution terrestrial archives o...
Upper Pleistocene (MIS 4-2) loess sequences occur in most of continental Europe and in Northern Ital...
Upper Pleistocene (MIS 4\u20132) loess sequences occur in most of continental Europe and in Northern...
Loess represents one of the main paleoenvironmental archives recording Quaternary environmental chan...
Purpose At the northern fringe of the Po Plain (northern Italy), several isolated hills exist, corre...
The significance of two loess profiles located in the Ghiardo area (Reggio Emilia, northern Italy) a...
Loess deposits at the Apennine fringe lie on the of terraces cut into early-Middle Pleistocene conti...
The significance of two loess profiles located in the Ghiardo area (Reggio Emilia, northern Italy) a...
The Bagaggera sequence consists of two Late Pleistocene loesses superimposed on the top of Middle Pl...
Purpose At the northern fringe of the Po Plain (northern Italy), several isolated hills exist, corr...
A representative loess-paleosol sequence has been identified and studied by mineralogical and microm...
In the Castenedolo hill a stratigraphic sequence ranging from the Early Pleistocene to the Upper Ple...
ABSTRACT The upper Pleistocene loess-paleosol sequence of Val Sorda (northeastern Italy
The interactions among Quaternary (paleo-) soil-forming, erosion, re-deposition and geomorphic proce...
Upper Pleistocene loess/palaeosol sequences provide excellent high-resolution terrestrial archives o...