Earthquakes today in Cornuda
Today, within 30 km: no earthquakes recorded (updated at 11:29). Latest: M2.4 on 12 October 2026 at 06:17, 1 km South-West of Revine Lago, 10 km deep.
Latest earthquake within 30 km
1 km South-West of Revine Lago
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 Cornuda: zone 2
A zone where strong earthquakes are possible: new buildings follow strict anti-seismic criteria.
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 = 0.223 g (10% probability of exceedance in 50 years, rigid soil).
“Within 30 km”: epicentres less than 30 km from the centre of Cornuda. “In the town”: quakes whose nearest town to the epicentre is Cornuda.
The seismic history of Cornuda
The earthquakes that were actually felt in Cornuda over the centuries, with the intensity observed on site (Mercalli MCS scale).
- 2004IV12 July 2004
Moderate: felt by many indoors; glasses and dishes rattle.
Slovenia nord-occidentale earthquake (M5.1), epicentre 136 km away
- 2001III-IV17 July 2001
Moderate: felt by many indoors; glasses and dishes rattle.
Val Venosta earthquake (M4.8), epicentre 120 km away
- 1989IV13 September 1989
Moderate: felt by many indoors; glasses and dishes rattle.
Prealpi Vicentine earthquake (M4.8), epicentre 58 km away
- 1987NF2 May 1987
Imperceptible: only instruments record it.
Reggiano earthquake (M4.7), epicentre 153 km away
- 1897V-VI11 June 1897
Strong: felt by everyone, many get scared; objects fall, first light damage to buildings.
Asolano earthquake (M4.4), epicentre 3 km away
- 1895V10 June 1895
Rather strong: felt by almost everyone; hanging objects swing.
Prealpi Trevigiane earthquake (M4.8), epicentre 13 km away
- 1893F27 October 1893
Moderate: felt by many indoors; glasses and dishes rattle.
Bellunese earthquake (M4.4), epicentre 44 km away
- 1695VIII25 February 1695
Ruinous: partial collapses in ordinary buildings, widespread heavy damage.
Asolano earthquake (M6.4), epicentre 8 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 sits above this source area: the deep structure where this area's earthquakes can originate.
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?
Cornuda sits in one of the most seismically active areas of its province: quakes are a familiar presence here, almost always light.
Each quake is attributed to the town closest to its epicentre: the numbers describe the area, not the municipal territory alone.
Context
Province of Treviso1 event · last 30 daysVeneto region11 events · last 30 daysFrequently asked questions
Were there earthquakes near Cornuda today?
No, no quakes were recorded today within 30 km of Cornuda. The latest dates back to 12 October 2026.
Is Cornuda a seismic area?
Cornuda is classified in seismic zone 2 by the Civil Protection. A zone where strong earthquakes are possible: new buildings follow strict anti-seismic criteria.
What was the strongest earthquake near Cornuda?
In the INGV catalogue since 2015, the strongest earthquake within 30 km of Cornuda was magnitude 3.6, on 28 September 2021.
When was the last quake near Cornuda?
The last quake recorded within 30 km of Cornuda dates back to 12 October 2026, magnitude 2.4.
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)