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The lithic clasts are abundant for the coarser classes; they decrease with distance for the medium classes and increase again for the finer classes. In particular, the sampling was mostly made on the syn-eruptive lahar deposits, but also on the post-eruptive and, in a few cases, on the primary pyroclastic deposits. All lab analyses were performed in the laboratories of sedimentology and optical microscopy at the Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Napoli Osservatorio Vesuviano (INGV–OV).

Such occurrences of erosion and accumulation of multiple units were useful to inform the lahar modeling of de’ Michieli Vitturi et al. (2024). Petrological analysis of the syn-eruptive lahar deposits has not been performed because the lithology (color, texture, mineral content) of the components is the same as the juvenile material of the primary deposits described in Sulpizio et al. (2005). The loose crystals consist of sanidine, leucite, biotite, and pyroxene fragments. Based on the results of the grain-size analyses, the coarser classes are defined from −4 to −1 phi, the medium ones from −0.5 to 2.5 phi, and the finest one from 3 phi. The juvenile pumice clasts are a ubiquitous component of the lahar deposits (both syn- and post-eruptive), but they decrease with distance for the finer grain-size classes, while the crystal content increases with the same progression.

The uppermost unit always contains white pumice fragments of the Avellino eruption. With particular reference to the lahar deposits, the syn-eruptive ones occurred by relatively short-term (during or immediately after the eruption) events and were directly emplaced on the primary pyroclastic deposits for both the Pollena and 1631 eruptions. Also, there are no significant erosion surfaces or humification traces in the sequences due to prolonged exposure of the primary deposits, demonstrating that the secondary emplacement was quite immediate (max a few years; Sulpizio et al., 2006) after or even during the eruption. The syn-eruptive features are also evidenced by the absence of anthropogenic traces or humified surfaces at the base of or interbedded in the lahar deposits, as further evidence of a very short-term time span between the eruptions and the lahar events.

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The structure of the work consists of an integrated geological, geomorphological, stratigraphic, and sedimentological study, a paleomagnetic and sediment–mechanic impact assessment calculation, and a comprehensive discussion on the lahar problem in the Campanian Plain. I love this app but it needs some improvement on the tech side – the app seems to crash every time a paid pulse is launched, presumably because of the amount of people using the app. Immediate MaxAir 2.1 shines in both auto and manual trading, making the process straightforward for traders at any stage.

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The investigated area was affected many times by post-eruptive lahar events due to the presence of thick, variably weathered pyroclastic deposits mantling the steep slopes of Somma–Vesuvius and the Apennines. This catastrophic event involved an extension area of around 60 km2 and a volume of more than 2 × 106 m3 (40 % derived from materials eroded along the channels), harming 160 victims and causing severe damage to the mentioned towns (Di Vito et al., 2019a, and references therein). The trading bot it offers caters to both automatic trading and manual trading options, guaranteeing a seamless procedure for beginners and experienced traders in the same way. When navigating the markets with Immediate MaxAir 2V, understanding the pros and cons of this trading platform is essential. Despite its promise to connect you with high-quality brokerages and endless investment possibilities, it’s important to weigh the positives and negatives to make an informed decision.

For this purpose, particular attention was paid to the basal contacts between the deposits. In some areas like Nola (10–15 km from Apennine source valleys), the lahar deposits directly overlie the primary pyroclastic deposits (for both the 472 CE Pollena and 1631 eruption), while in other areas some pyroclastic units or the whole primary deposits are missing (eroded) or lacking. 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. The analysis of the internal structure marked by sharp changes in grain sizes, color, presence of erosional unconformities, or interposition of lenses of coarser material also permitted the identification of one or more flow units within the same individual deposit package. The macroscopic characteristics of the sequences permitted some inferences on the transport and depositional mechanisms, while the grain-size and componentry analyses provided information on the source deposits that were remobilized. This brings us to another important definition, syn-eruptive vs. post-eruptive lahars, according to the definition of Sulpizio et al. (2006) and Iverson and Vallance (2015), which applies during or soon after the eruption vs. several years to centuries after the eruption ended, respectively.

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