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2.6
light
EARTHQUAKE DETAILS

1 km North of Campegine

117 months ago · 3 Jan, 11:30

A light earthquake, rarely felt by people. Being deep, it is felt less at the surface.

Stronger than 96% of Italian events in the past year

Where

1 km North of CampegineEarthquakes in the province of Reggio EmiliaEarthquakes in Emilia-Romagna

How far away could it be felt?

A quake this small is usually not felt by people: only seismographs record it.

Statistical estimate from the Italian intensity attenuation model (INGV): actual perception depends on geology, buildings and depth. Very shallow events can be felt locally even below the threshold.

Earthquake map

1 events
Magnitude:lightweakmoderatestrong

The energy released

How much energy this quake unleashed, translated into everyday comparisons.

120kgof TNT equivalent
Less than the energy of a lightning bolt
M3
A magnitude 3 earthquake releases ×4 its energy
M2this quakeM4

Each extra magnitude unit releases about 32 times more energy: an M5 is not "a bit stronger" than an M4 — it is a different league.

Energy estimated with the standard Gutenberg–Richter relation; an average lightning bolt ≈ 1 billion joules. Indicative values.

The race of the seismic waves

Two waves set off from the hypocentre: the faster P wave arrives first with a sharp jolt; the S wave carries the actual shaking.

P waves — the first sharp jolt (~6 km/s)S waves — the strongest shaking (~3.5 km/s)
t ≈ 16 s

Animation sped up ~3× compared to reality.

  • Reggio nell'Emilia
    12 km from the epicentre
    first tremor in ~8 s
    main shaking in ~13 s
  • Parma
    15 km from the epicentre
    first tremor in ~8 s
    main shaking in ~13 s
  • Carpi
    31 km from the epicentre
    first tremor in ~9 s
    main shaking in ~15 s
  • Modena
    31 km from the epicentre
    first tremor in ~9 s
    main shaking in ~16 s

Theoretical times with average crustal speeds: real values vary with geology. The gap between P and S waves is what earthquake early-warning systems rely on.

How deep it was born

45 km
deep
5 times the height of Mount Everest

Being deep, it is felt less at the surface.

deeper than the area average (~21 km)

For the same magnitude, a shallow earthquake is felt much more than a deep one: the energy starts closer to the surface.

What kind of quake is this?

Isolated quake

In the 30 days around this event no other quakes were recorded within 30 km: a one-off episode, very common in Italy.

Activity in the area right now (30 km radius)
0
last 24 hours
0
last 7 days
0
last 30 days

No other quakes within 30 km in the 30 days around the event.

How often does it happen here?

about every ~14 days

Within 50 km of this epicentre, a magnitude ≥ 2.5 earthquake has occurred on average this often: 296 events in the last 12 years of the INGV catalogue.

An average computed on the recent past: it tells how used this area is to shaking, not when the next quake will come — earthquakes cannot be predicted.

The great earthquakes in this area's history

Almost a thousand years of catalogues: the strongest documented events within ~50 km.

15016.0
Modenese earthquake
5 June 1501 · 39 km from here
IXDestructive: many buildings partly or fully collapse.
20125.9
Pianura emiliana earthquake
29 May 2012 · 43 km from here
VIIIRuinous: partial collapses in ordinary buildings, widespread heavy damage.
14385.6
Parmense earthquake
11 June 1438 · 24 km from here
VIIIRuinous: partial collapses in ordinary buildings, widespread heavy damage.
19715.5
Parmense earthquake
15 July 1971 · 15 km from here
VIIIRuinous: partial collapses in ordinary buildings, widespread heavy damage.

Source: Parametric Catalogue of Italian Earthquakes CPTI15 (INGV, CC BY 4.0).

The closest seismic structure

Campegine-Correggio

The epicentre lies about 2 km from Campegine-Correggio, one of the seismic structures mapped by INGV geologists.

estimated maximum magnitude 6.6between 3 and 10 km deep

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).

Data: INGV — National Institute of Geophysics and Volcanology (CC-BY 4.0)

Estimates computed by Meteare on INGV data (Gutenberg–Richter relation; Italian macroseismic intensity attenuation model).

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