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Erosion is an important factor for the entrainment of pre-existing materials and objects, which include large-sized clasts external to the remobilized pyroclastic material. Size and density of the largest clasts embedded in the deposits can give an idea of the carrying capacity of the lahars. We grouped all deposit descriptions into representative lithofacies to more directly characterize both the primary pyroclastic and lahar deposits (Table 2 and Fig. 7). Given the amount of data and description of the studied areas, we used these lithofacies to characterize a number of macro-areas between the Somma–Vesuvius sector and the nearby Apennine valleys (Appendix C).

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The latter is represented by a discontinuous medium to fine ash layer, slightly laminated for contrasting grain size, up to 5 cm thick, with a gray to violet color, and containing dark pumice fragments and loose crystals of leucite, pyroxene, and biotite (Fig. C7). Its thickness variation is due to both slight internal variations (thickening in correspondence with depressions) and erosion by the following lahars. The latter are composed of one to three flow units (d1 in Fig. C7), with a cumulative total thickness varying from 10 to 45 cm. They are composed of massive fine and very cohesive ash and contain rare scattered dark pumice fragments similar to those of the 1631 eruption (lithofacies mM). Locally, thin ash beds of recent Vesuvius activity (like 1822, 1906) overlie the 1631 deposits. C1, above the primary deposit, there is an example of a well-exposed sequence composed of at least five units (c in Fig. C1).

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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. 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 automated trading bot evidence of a very short-term time span between the eruptions and the lahar events. Another interesting feature is the presence of multiple depositional flow units, as evidenced by grain-size changes, some clast alignments, and concave erosion surfaces in the lahar deposits.

It underlies a massive deposit with high thickness variations (max 20 cm) at the outcrop scale. It is composed of fine ash, is cohesive and vesiculated, and contains scattered small pumice fragments (lithofacies mM). The pumice fragments are vesicular, dark gray to blackish, and highly porphyritic with leucite, pyroxene, and feldspar crystals.

The work was also supported by the INGV project Pianeta Dinamico – Working Earth – Task V3 (MDV). We thank Ulrich Kueppers, Lucia Capra, an anonymous reviewer, and the editor Andrea Di Muro very much for their help in improving this paper in the revision process. Table 2Historical archive of lahar and alluvial events related to the four most significant Vesuvius eruption in the last 4 centuries and the municipalities affected by such events. This webshop is offering payment methods that can be considered reasonably safe such as credit card and Paypal. These companies usually offer the option to get your money back in case the merchant does not deliver or the product has been broken during transportation. Make sure you file a complaint in time and be careful with the limitations your credit card or payment methods have set.