Erosion of orogenic mountain ranges exhumes deeply buried rocks and controls
weathering, climate, and sediment production and transport at a variety of scales. Erosion …

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 …

Accurate thermochronologic interpretation of zircon (U-Th)/He dates requires a realistic and
practically useful understanding of He diffusion kinetics in natural zircon, ideally across the …

An outline of the geology of the Italian Northern Apennines, to accompany a geological map
at 1: 250,000 scale covering the Emilia-Romagna, Marche, Tuscany and Umbria regions, is …

Rock uplift rates can be difficult to measure over 103–105 yr time scales. If, however, a
landscape approaches steady state, where hillslope erosion and rock uplift rates are steady …

We integrate existing and new geologic data [REtreating TRench, Extension, and Accretion
Tectonics (RETREAT project)], particularly on the origin, growth, and activity of the mountain …

Much of our understanding of submarine sediment‐laden density flows that transport very
large volumes (ca 1 to 100 km3) of sediment into the deep ocean comes from careful …

The Casaglia Monte della Colonna (CMC) body, from the middle Miocene Marnoso-
arenacea Formation of the Northern Apennines, covering more than 350 square kilometers …

The topography of orogenic belts responds to several contributions operating at short and
long temporal and spatial (ie, wavelengths) scales, from the surface to the deep mantle …

The elevation of an orogenic belt is commonly related to crustal/lithosphere thickening.
Here, we discuss the Apennines as an example to show that topography at a plate margin …