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Abstract:
The evolution of topography in forearc regions results from the complex interplay of crustal and
mantle processes. The Southern Apennines represent a well‐studied forearc region that experienced several
tectonic phases, initially marked by compressional deformation followed by extension and large‐scale uplift.
We present a new structural, geomorphic and fluvial analysis of the Pollino Massif and surrounding
intermontane basins (Mercure, Campotenese and Castrovillari) to unravel their evolution since the Pliocene. We
constrain multiple tectonic transport directions, evolution of the drainage, and magnitude and timing of long‐
term incision following base level falls. Two sets of knickpoints suggest two phases of base level lowering and
allow to estimate ∼500 m of long‐term uplift (late Pleistocene), as observed in the Sila Massif. On a smaller
spatial scale, the evolution and formation of topographic relief, sedimentation, and opening of intermontane
basins is strongly controlled by the recent increase in rock uplift rate and fault activity. At the regional scale, an
along‐strike, long‐wavelength uplift pattern from north to south can be explained by progressive lateral slab
tearing and inflow of asthenospheric mantle beneath Pollino and Sila, which in turn may have promoted
extensional tectonics. The lower uplift of Le Serre Massif may be explained as result of weak plate coupling due
to narrowing of the Calabrian slab. The onset of uplift in the Pollino Massif, ranging from 400 to 800 ka, is
consistent with that one proposed in the southern Calabrian forearc, suggesting a possible synchronism of uplift,
and lateral tearing of the Calabrian slab.
