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Vesuvius volcano, Italy: news & activity updates

Updated: Apr 30, 2025 22:36 GMT-

Vesuvius volcano (Italy): volcano continues its year-long slumber, no signs of wakening up

Mon, 8 Jul 2024, 12:40
Summary of volcanic activity at Vesuvius volcano in June 2024 (image: INGV OV)
Summary of volcanic activity at Vesuvius volcano in June 2024 (image: INGV OV)
The volcano remains calm. The volcano observatory in Naples (INGV OV) informed that no significant seismic, deformation or other activity has been detected during the past month. Acquired geochemical data indicate that the current multi-year trend of decrease in hydrothermal activity within the crater area of ​​Vesuvius has continued. Read all

Vesuvius volcano (Italy): tiny earthquakes are no reason to worry but normal

Tue, 26 Mar 2019, 07:10
Current earthquakes at Vesuvius
Current earthquakes at Vesuvius
Since about Oct last year (2018), the number of registered micro-quakes under the volcano seems to have increased. Small swarms of tiny quakes have been reported more frequently in various media and can be seen on the published data of the volcano observatory. Read all
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Vesuvius volcano
Stratovolcano 1281 m
Italy, 40.82°N / 14.43°E
Map of Vesuvius volcano Current status: normal or dormant (1 out of 5) Vesuvius volcano eruptions:
1796 - 1822, 1824 - 1834, 1835 - 1839, 1841 - 16 February 1850, 1854 - 1855, 1855 - 1861, 1864 - 1868, 1870 - 1872, 1875 - 1906, 1913 - 4 April 1944
Typical eruption style
Mainly explosive. I detail, Vesuvius has 4 typical types of eruptions:
1. Plinian (such as the 79 AD Pompeii eruption): extremely large explosive eruptions producing several to several tens of cubic km of magma in a very short time.
2. Sub-Plinian explosive eruptions (such as the 1631 eruption). They are similar in style, but smaller than true Plinian events.
3. Strombolian and Vulcanian eruptions (several examples during the 1631-1944 period, e.g. 1906 and 1944). Such eruptions produce local heavy tephra falls, small pyroclastic flows, as well as large fire fountains and lava flows.
4. The smallest, but most frequent type of activity observed at Vesuvius is persistent Strombolian to Hawaiian-style activity that prevailed during much of the period between 1631 and 1944. This activity is usually limited to the central crater, and sometimes to flank vents. Lava flows and lava fountains have been frequently observed during such periods of activity.
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