<p>There are lot of studies on the past activity of Mount Vesuvius. Eruptive deposits have been studied and dated in order to reconstruct the type and timing of past eruptions. This can give some indication of what to expect even if, and I cannot stress this enough, <em>past activity patterns of a given volcano do not predict its future activity</em>. It can give a tendency, but volcanoes remain unpredictable, as shown by recent examples in well-monitored countries like Japan (<a href="https://en.wikipedia.org/wiki/2014_Mount_Ontake_eruption" rel="nofollow noreferrer">Mount Ontake 2014 eruption</a>) or Italy (paroxysmal eruptions at Stromboli in summer 2019).</p>
<p>That being said, a study by <a href="https://doi.org/10.1016/j.jvolgeores.2008.04.024" rel="nofollow noreferrer">Cioni et al. (2008)</a> came up with some interesting results. They found that there is a positive correlation between the magnitude of an eruption and the repose time before this eruption, i.e., the longer we wait before an eruption of Vesuvius, the larger the eruption will be. It's their figure 6:</p>
<p><a href="https://i.sstatic.net/fK2el.jpg" rel="nofollow noreferrer"><img src="https://i.sstatic.net/fK2el.jpg" alt="Figure 6 from Cioni et al. 2008" /></a></p>
<p>You can see that Strombolian (= small) eruptions happen after a few years of repose while sub-Plinian and Plinian (= large, like the one that destroyed Pompei) eruptions are preceded by long repose periods. However there is some scattering, especially in the zone shown by a red box:</p>
<blockquote>
<p>In particular, a large variability in the magnitude and eruption style of the past eruptions is apparent for a window of repose time from dozens to hundreds of years.</p>
</blockquote>
<p>And now we are exactly in this box: the last eruption of Vesuvius was in 1944, 77 years ago. So according to this study, and <em>assuming the volcano will keep following this pattern</em> (which is not sure), if Vesuvius does erupt tomorrow, it could be up to a violent Strombolian eruption. This type of eruption would not be a major threat to the local population; the main threat is pyroclastic density currents, which happen mostly with sub-Plinian and Plinian eruptions (their Table 2). The last eruption (1944) falls in the &quot;violent Strombolian&quot; category; lava flows destroyed several villages, but no one was killed.</p>

CC BY-SA 4.0
2021-09-18T10:16:44.107Z
So you're also indicating... if it doesn't erupt for another few decades and especially century... it starts getting a bit more nervous as a general idea as it shifts towards the sub-plinian region of the graph?
JeopardyTempest
CC BY-SA 4.0
2021-09-20T08:40:28.273Z
@JeopardyTempest Exactly, that's the idea, but again, only *assuming the volcano will keep following this pattern*. These cycles are not infinite, we could imagine that at some point the magmatic system would shift to another vent, or even stop being recharged, ending the activity in the region.
Jean-Marie Prival
CC BY-SA 4.0
2020-01-06T17:01:21.230Z
2021-09-17T08:30:37.003Z
2021-09-17T08:30:37.003Z
Jean-Marie Prival
<p>How much of a risk does Mount Vesuvius pose for the population of the surrounding area?</p>

CC BY-SA 3.0
2016-04-27T10:31:03.703Z
Welcome at EarthScience.SE! Which research did you do on your own on that topics? How far is 'surrounding area'? Are you asking for the probability of an eruption of the magnitude that destroyed Pompei?
daniel.heydebreck
CC BY-SA 3.0
2016-04-27T10:43:00.630Z
Because in Italy since many decades of years Marco Pannella and Radical Party are warning public opinion on this risk, and too many houses are on and too near Vesuvio. So it could be interesting in this geological community, the opinion and in particular the  results of research
d.pensopositivo
CC BY-SA 3.0
2016-04-27T11:28:03.770Z
@d.pensopositivo I recommend combining your comment, which seems like relevant context, into your question. You might add anything else you know or have heard about the risk posed by volcanos — a little research can make a high quality question.
Matt Hall
CC BY-SA 3.0
2016-04-27T12:51:02.447Z
Valid question IMHO, although it leaves some room for interpretation, but could use a bit more context.
Semidiurnal Simon
<volcanology><volcanic-hazard><natural-disasters>
How big a risk is Mount Vesuvius for the local population?
d.pensopositivo
# How big a risk is Mount Vesuvius for the local population?

(Asked by: username_0 on 2016-04-27)

How much of a risk does Mount Vesuvius pose for the population of the surrounding area?

**Tags:** volcanology, volcanic-hazard, natural-disasters

> **Comments:**
> **username_1**: Welcome at EarthScience.SE! Which research did you do on your own on that topics? How far is 'surrounding area'? Are you asking for the probability of an eruption of the magnitude that destroyed Pompei?  
> **username_0**: Because in Italy since many decades of years Marco Pannella and Radical Party are warning public opinion on this risk, and too many houses are on and too near Vesuvio. So it could be interesting in this geological community, the opinion and in particular the  results of research  
> **username_2**: @username_0 I recommend combining your comment, which seems like relevant context, into your question. You might add anything else you know or have heard about the risk posed by volcanos — a little research can make a high quality question.  
> **username_3**: Valid question IMHO, although it leaves some room for interpretation, but could use a bit more context.  

---

## 1 answers

### Answer by username_4 on 2020-01-06. Score: 5

There are lot of studies on the past activity of Mount Vesuvius. Eruptive deposits have been studied and dated in order to reconstruct the type and timing of past eruptions. This can give some indication of what to expect even if, and I cannot stress this enough, *past activity patterns of a given volcano do not predict its future activity*. It can give a tendency, but volcanoes remain unpredictable, as shown by recent examples in well-monitored countries like Japan ([Mount Ontake 2014 eruption](https://en.wikipedia.org/wiki/2014_Mount_Ontake_eruption)) or Italy (paroxysmal eruptions at Stromboli in summer 2019).

That being said, a study by [Cioni et al. (2008)](https://doi.org/10.1016/j.jvolgeores.2008.04.024) came up with some interesting results. They found that there is a positive correlation between the magnitude of an eruption and the repose time before this eruption, i.e., the longer we wait before an eruption of Vesuvius, the larger the eruption will be. It's their figure 6:

[![Figure 6 from Cioni et al. 2008](https://i.sstatic.net/fK2el.jpg)](https://i.sstatic.net/fK2el.jpg)

You can see that Strombolian (= small) eruptions happen after a few years of repose while sub-Plinian and Plinian (= large, like the one that destroyed Pompei) eruptions are preceded by long repose periods. However there is some scattering, especially in the zone shown by a red box:

> In particular, a large variability in the magnitude and eruption style of the past eruptions is apparent for a window of repose time from dozens to hundreds of years.

And now we are exactly in this box: the last eruption of Vesuvius was in 1944, 77 years ago. So according to this study, and *assuming the volcano will keep following this pattern* (which is not sure), if Vesuvius does erupt tomorrow, it could be up to a violent Strombolian eruption. This type of eruption would not be a major threat to the local population; the main threat is pyroclastic density currents, which happen mostly with sub-Plinian and Plinian eruptions (their Table 2). The last eruption (1944) falls in the "violent Strombolian" category; lava flows destroyed several villages, but no one was killed.

> **Comments:**
> **username_5**: So you're also indicating... if it doesn't erupt for another few decades and especially century... it starts getting a bit more nervous as a general idea as it shifts towards the sub-plinian region of the graph?  
> **username_4**: @username_5 Exactly, that's the idea, but again, only *assuming the volcano will keep following this pattern*. These cycles are not infinite, we could imagine that at some point the magmatic system would shift to another vent, or even stop being recharged, ending the activity in the region.  

---

