Earthquakes today in Pont-Saint-Martin
Today, within 30 km: no earthquakes recorded (updated at 13:17). Latest: M1.7 on 22 January 2026 at 14:23, 0 km North-East of Val di Chy, 9 km deep.
Latest earthquake within 30 km
Seismic activity within 30 km
30 km radiusINGV catalogue epicentres of the last ~12 years, within the given radius from the town centre.
How seismic is Pont-Saint-Martin: zone 3
Medium-low seismicity: strong quakes are rare, but not impossible.
Official Civil Protection classification (upd. 2025), used for building codes.
Hazard describes the long-term expected shaking: it is not a forecast. Technical value: ag = 0.050 g (10% probability of exceedance in 50 years, rigid soil).
Why the ground rarely shakes here
Pont-Saint-Martin sits in one of the most stable areas of Italy: far from the boundary between the Eurasian and African plates, on ancient, rigid crust that hardly accumulates tectonic stress any more.
That is why earthquakes here are rare and almost always weak: a small geological privilege.
“Within 30 km”: epicentres less than 30 km from the centre of Pont-Saint-Martin. “In the town”: quakes whose nearest town to the epicentre is Pont-Saint-Martin.
The seismic history of Pont-Saint-Martin
The earthquakes that were actually felt in Pont-Saint-Martin over the centuries, with the intensity observed on site (Mercalli MCS scale).
- 2005NF5 July 2005
Imperceptible: only instruments record it.
Canavese earthquake (M3.5), epicentre 32 km away
- 1996NF31 March 1996
Imperceptible: only instruments record it.
Valle d'Aosta earthquake (M4.2), epicentre 47 km away
- 1980III-IV5 January 1980
Moderate: felt by many indoors; glasses and dishes rattle.
Torinese earthquake (M4.8), epicentre 75 km away
- 1968V18 June 1968
Rather strong: felt by almost everyone; hanging objects swing.
Valle d'Aosta earthquake (M4.9), epicentre 10 km away
- 1892VI-VII5 March 1892
Very strong: hard to stand; chimneys and roof tiles fall, serious damage to weaker buildings.
Valle d'Aosta earthquake (M5.0), epicentre 3 km away
- 1887III23 February 1887
Light: felt by few people, like a passing truck.
Liguria occidentale earthquake (M6.3), epicentre 190 km away
Source: Italian Macroseismic Database DBMI15 (INGV, CC BY 4.0).
The great earthquakes in this area's history
Almost a thousand years of catalogues: the strongest documented events within ~50 km.
Source: Parametric Catalogue of Italian Earthquakes CPTI15 (INGV, CC BY 4.0).
The closest seismic structure
The town lies about 47 km from Western Monferrato, one of the seismic structures mapped by INGV geologists.
Faults are mapped to build better and understand the territory: knowing them says nothing about when an earthquake will occur, which remains unpredictable. Source: DISS 3.3 (INGV, CC BY 4.0).
Over time within 30 km
Earthquake map within 30 km
60 eventsLatest earthquakes within 30 km
Nearby towns
How does it compare with the surroundings?
Pont-Saint-Martin is about average for its province in recorded quakes.
Each quake is attributed to the town closest to its epicentre: the numbers describe the area, not the municipal territory alone.
Context
Province of Aosta39 events · last 30 daysAosta Valley region39 events · last 30 daysFrequently asked questions
Were there earthquakes near Pont-Saint-Martin today?
No, no quakes were recorded today within 30 km of Pont-Saint-Martin. The latest dates back to 22 January 2026.
Is Pont-Saint-Martin a seismic area?
Pont-Saint-Martin is classified in seismic zone 3 by the Civil Protection. Medium-low seismicity: strong quakes are rare, but not impossible.
What was the strongest earthquake near Pont-Saint-Martin?
In the INGV catalogue since 2015, the strongest earthquake within 30 km of Pont-Saint-Martin was magnitude 2.0, on 14 April 2025.
When was the last quake near Pont-Saint-Martin?
The last quake recorded within 30 km of Pont-Saint-Martin dates back to 22 January 2026, magnitude 1.7.
Tip. Click a nearby town to explore its seismicity.
Sources:INGV earthquake catalogueDBMI15 macroseismic historyCivil Protection seismic classification
Data: INGV — National Institute of Geophysics and Volcanology (CC-BY 4.0)