Introduction
Marche is a region in central Italy, situated in the external sector of the Adriatic side of the Umbria-
Marche Apennines, a trust-and-fold chain rising up since Miocene. It is characterised by short rivers
with several orders of terraces, deep gullies and narrow alluvial plains. The Cesano and Misa rivers,
including the Nevola torrent, are situated in the northern part of the region and flow orthogonally
to the coastline. The landscape of the Marche region is subjected to continuous changes, which can
be monitored by studying old and modern remote sensing data. The terraces originated during the
uppermost Pleistocene-Holocene, due to the dissection of the alluvial fill (Dall’Aglio, et al., 2012).
During the 3rd century BC, the Romans operated a division of the agri Picenus et Gallicus (lex
Flaminia, 232 BC), which resulted in a massive and growing network of drainage that caused a deep
transformation of the landscape (e.g., the meandering configuration of the rivers). The landscape
started to change again in the 5th and 6th centuries AD, when the Cesano and Misa valleys went
through a process of depopulation (Dall’Aglio, et al., 2012). Caused by both natural (e.g., a climate
cooling) and human factors (e.g., the Gothic Wars in AD 535-553), it led to waterlogging, wasteland,
and hydraulic disruption (Dall’Aglio, et al., 2012). As a consequence, the cultivated area was
replaced by woods and swamps. Eventually, the braided configuration of the rivers in the Cesano
and Misa valleys was restored. In the recent years, the changing rhythm is accelerating due to more
invasive ploughing techniques and a shift in cultivation, from olives and wine to cereals (Boschi,
2020).
In the central-southern area of Marche, many pre-Roman necropolises and settlements were
mapped in the hilltops of the Potenza and Esino valleys, around Ancona and the Conero promontory.
The Cesano, Misa, and Nevola river-valleys, instead, seemed to be less populated. In the Cesano
valley, while traces of settlements have been found on top of plains or river ridges (e.g., Montedoro,
Miralbello), the data about the necropolises is lacking. On the other hand, in the Misa and Nevola
valleys, data about necropolises is abundant, whereas the settlements are still to be mapped
(Boschi, 2022). However, scholars believe this could be related to a lack of systematic studies
(Boschi, 2020).
This project aims at mapping and detecting hilltop Picenian settlements in the river-valleys of the
Cesano, Misa, and Nevola. They will be then connected with known necropolises in the area. To do
so, a holistic approach will be applied, involving the study of cartography, geomorphology, LiDAR,
satellite imagery, and aerial photos. Moreover, this project will focus on identifying markers for the
detection of Picenian settlements, as has been done for the necropolises by Professor Federica
Boschi. To do so, a comparison with geomorphologically similar valleys will be made (e.g., the
Potenza valley). Eventually, field-walking surveys will be conducted to verify promising sites.