Late Quaternary fluvial terraces of the Romagna and Marche Apennines, Italy: Climatic, lithologic, and tectonic controls on terrace genesis in an active orogen

KW Wegmann, FJ Pazzaglia - Quaternary Science Reviews, 2009 - Elsevier
We synthesize a new fluvial terrace chronostratigraphy of the Bidente and Musone Rivers
cast within a broader European framework, which forms the basis of a terrace genesis and …

Morphotectonic evolution of the Adriatic piedmont of the Apennines: an advancement in the knowledge of the Marche-Abruzzo border area

M Della Seta, M Del Monte, P Fredi, E Miccadei… - Geomorphology, 2008 - Elsevier
This study focuses on the morphotectonic evolution of the Apennines Central Adriatic
piedmont, and in particular on the region along the Marche-Abruzzo border …

Unraveling tectonic and climatic controls on synorogenic growth strata (Northern Apennines, Italy)

KL Gunderson, FJ Pazzaglia, V Picotti… - …, 2014 - pubs.geoscienceworld.org
We develop a new high-resolution stratigraphic age model to unravel the contributions of
tectonic and climatic processes on early to late Pleistocene synorogenic growth strata. We …

Pleistocene sea-level changes, sapping processes and development of valley networks in the Apulia region (southern Italy)

G Mastronuzzi, P Sansò - Geomorphology, 2002 - Elsevier
The central area of the Apulia region is characterized by a network of valleys with peculiar
features, locally called 'gravine'or 'lame'. They are short, straight valleys, deeply incised in …

Alluvial terraces on the Ionian coast of northern Calabria, southern Italy: Implications for tectonic and sea level controls

G Robustelli, F Lucà, F Corbi, T Pelle, F Dramis… - Geomorphology, 2009 - Elsevier
In this paper we present the results of an integrated geomorphological, pedological and
stratigraphical study carried out along the Ionian coast of northern Calabria (southern Italy) …

[HTML][HTML] Transient landscape and stratigraphic responses to drainage integration in the actively extending central Italian Apennines

AH Geurts, AC Whittaker, RL Gawthorpe, PA Cowie - Geomorphology, 2020 - Elsevier
Drainage networks in continental rifts are generally reported as dynamic features that
produce transitions between endorheic and exorheic conditions. While this is of major …

Paleogeographic and paleodrainage changes during Pleistocene glaciations (Po Plain, northern Italy)

E Garzanti, G Vezzoli, S Andò - Earth-Science Reviews, 2011 - Elsevier
The Po Basin, a Pliocene marine gulf between the Alps and the Apennines, was filled
progressively from west to east and finally capped by fluvial sediments during the …

Middle Eocene to Early Miocene sedimentary evolution of the western Lombardian segment of the South Alpine foredeep (Italy)

A Di Giulio, B Carrapa, R Fantoni, L Gorla… - International Journal of …, 2001 - Springer
The main steps of the sedimentary evolution of the west Lombardian South Alpine foredeep
between the Eocene and the Early Miocene are described. The oldest is a Bartonian …

Quaternary evolution of the" Castelluccio di Norcia" basin (Umbro-Marchean Apennines, central Italy)

M Coltorti, P Farabollini - Alpine and Mediterranean Quaternary, 1995 - amq.aiqua.it
Castelluccio di Norcia is a closed depression, 12 km in length and 8 km in width, located in
the southern part of the Umbro-Marchean Apennines, westward from the highest reliefs of …

[HTML][HTML] The interplay between adjacent Adige and Po alluvial systems and deltas in the late Holocene (Northern Italy)

S Piovan, P Mozzi, M Zecchin - Géomorphologie: relief …, 2012 - journals.openedition.org
The alluvial plain behind the southern Venice Lagoon, in northern Italy, is characterised by
the presence of a complex network of alluvial ridges formed by the aggradation of channel …