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It is possible to evaluate the effects of the lahars on building in the Roman Villa di Lauro, at Taurano, where a 70 cm thick fallout is overlain, without paleosol, by syn-eruptive lahars which immediatemax-air.com engulfed and transported pieces of walls, bricks, and potteries. The lahar deposits are matrix-supported, are composed of fine to coarse ash, and contain abundant pumice lapilli (all similar to the Pollena fallout deposits). They are massive and cohesive and have a thickness up to about 1 m, thickening in depressions and near barriers (Fig. C11). The top is almost always horizontal due to erosion related to modern anthropogenic activity, and only in a few exposures it is capped by a paleosol, with traces of human presence of Medieval times and of the deposits of the 1631 eruption as well. The base of this latter deposit is a centimeter-thick fine ash bed with an internal plane-parallel layering emplaced by fallout.

Such an approach enabled us to cross-check geological and archeological evidence, allowing us to accurately fix the age of events. Conversely, the presence of well-dated primary pyroclastic deposits can define the age of human traces otherwise not easily datable. Furthermore, the identification of the “primary” deposit (fallout and pyroclastic current, along with the archeological findings) can give the absolute age (ante or post quem) of a given deposit. The definition of isochronic paleosurfaces can also contribute to the reconstruction of the paleo-environments affected by the deposition and of the variations that occurred during depositional processes. For this purpose, particular attention was paid to the basal contacts between the deposits. Only correlation with the nearby areas permitted us to determine whether the emplacement of the lahars partly or significantly the eroded underlying primary deposits; in contrast, complete absence in the emplacement areas could also be due to the distribution of the latter.

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It should be noted that the distribution of the data can be affected by the different urbanization over time and by the presence of damage to people, infrastructure, and goods, as well as economic activities and settlements. We identified about 500 individual reports, covering events between the sixteenth century CE and 2005 that took place in 97 different municipalities. The data were organized in a geospatial database so that it was possible to define different areas affected by frequent syn-eruptive floods and lahars, concomitant with or related to the sub-Plinian eruption of 1631, to be used as a benchmark for the main geological analyses. We could not add the Pollena eruption to this historical data set, as there are no available sources for similar occurrences other than documents derived from archeological excavations (see next sections). The post-eruptive lahar deposits of the Pollena eruption are more distributed in the Avella and Lauro valleys and in the plain north of the volcano close to the apron area (low-angle edifice outer slopes) (Figs. 1 and 9). Their deposits contain fragments from both the Pollena eruption and from preceding eruptions, suggesting that pyroclastic deposits of the older sequences were progressively eroded and involved in remobilization processes over time.

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This system is designed to maximize profitability by identifying optimal entry and exit points for trades, thereby enhancing the success rates of transactions. The overlying lahar deposits are massive and matrix-supported, composed of fine to coarse ash, and contain abundant pumice fragments of the primary deposit. 11, minor post-eruptive lahar deposits of the 1631 eruption are reported, with a preferential distribution to the E quadrants of the volcano from N to S both on the plain and in the valleys. These deposits are still significant, with a thickness of around half a meter to a meter or more at a few points.

This can be argued by the generally massive facies of each flow unit in the deposits and by the presence of water escape structures that vertically cross the entire deposit sequences. The latter evidence demonstrates rapid water loss through vertical escape “pipes” during or soon after the aggradation of the sequences. Figure C1Nola (10–15 km from Apennine source valleys); Pollena fallout deposits overlain by at least five lahar units.

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It is overlain by lahar deposits (b in Fig. C9) composed of several units and characterized by contrasting grain sizes. The deposits are composed of medium ash, are massive and matrix-supported, and contain abundant scattered millimeter- to centimeter-sized pumice fragments (all with the same lithology of the primary deposits) and sometimes vegetal remain traces (lithofacies Gms). The top of this paleosol is undulated and covered by the primary deposit of the 1631 eruption (d in Fig. C7).