Earthquake with magnitude of Md 3.1 on date 18-01-1986 and time 15:48:23 (Italy) in region 3 km NE Miranda (IS)

A magnitude Md 3.1 earthquake occured in region: 3 km NE Miranda (IS), on

  • 18-01-1986 14:48:23 (UTC)
  • 18-01-1986 15:48:23 (UTC +01:00) Italian time

and geographic coordinates (lat, lon) 41.6740, 14.2620 at 10 km depth.

The earthquake was located by: Bollettino Sismico Italiano INGV.

Search earthquakes: Any within 30 km radius

The values of hypocentral coordinates and magnitude may be revised at a later time as more information becomes available.

Municipalities within 20 km from the epicenter

Distances are determinated based on the geographic coordintes of the (Istat).
Municipality Region Dist Inh Cum Inh
Miranda IS 4 1047 1047
Roccasicura IS 4 550 1597
Carovilli IS 5 1359 2956
Pescolanciano IS 6 855 3811
Sessano del Molise IS 7 727 4538
Forlì del Sannio IS 7 675 5213
Pesche IS 7 1661 6874
Acquaviva d'Isernia IS 9 425 7299
Isernia IS 10 21842 29141
Chiauci IS 10 233 29374
Carpinone IS 11 1157 30531
Rionero Sannitico IS 11 1118 31649
Pettoranello del Molise IS 11 460 32109
Vastogirardi IS 11 704 32813
Civitanova del Sannio IS 12 945 33758
Fornelli IS 12 1909 35667
Cerro al Volturno IS 13 1281 36948
Pietrabbondante IS 14 759 37707
San Pietro Avellana IS 14 503 38210
Castelpetroso IS 14 1680 39890
Macchia d'Isernia IS 15 1035 40925
Sant'Agapito IS 15 1496 42421
Colli a Volturno IS 15 1349 43770
Rocchetta a Volturno IS 16 1113 44883
Castelverrino IS 16 115 44998
Santa Maria del Molise IS 16 665 45663
Duronia CB 17 405 46068
Castel San Vincenzo IS 17 516 46584
Bagnoli del Trigno IS 17 735 47319
Montenero Val Cocchiara IS 17 538 47857
Longano IS 17 690 48547
Montaquila IS 17 2456 51003
Castelpizzuto IS 17 155 51158
Poggio Sannita IS 17 702 51860
Agnone IS 17 5139 56999
Macchiagodena IS 18 1854 58853
Frosolone IS 18 3170 62023
Castel di Sangro AQ 18 6538 68561
Capracotta IS 18 903 69464
Scapoli IS 18 680 70144
Monteroduni IS 18 2264 72408
Pizzone IS 19 329 72737
Molise CB 20 167 72904
Cantalupo nel Sannio IS 20 739 73643

Municipalities with at least 50000 inhabitants

An earthquake occurred to
67 Km N of Caserta (76326 inhabitants)
74 Km NW of Benevento (60091 inhabitants)
76 Km S of Chieti (51815 inhabitants)
78 Km N of Aversa (53047 inhabitants)
81 Km N of Acerra (59573 inhabitants)
83 Km N of Giugliano in Campania (122974 inhabitants)
84 Km N of Afragola (65057 inhabitants)
85 Km N of Casoria (77642 inhabitants)
86 Km N of Marano di Napoli (59874 inhabitants)
88 Km S of Pescara (121014 inhabitants)
93 Km N of Napoli (974074 inhabitants)
93 Km W of San Severo (53905 inhabitants)
93 Km N of Pozzuoli (81661 inhabitants)
94 Km S of Montesilvano (53738 inhabitants)
95 Km N of Portici (55274 inhabitants)
96 Km NW of Avellino (54857 inhabitants)
96 Km N of Ercolano (53709 inhabitants)
99 Km N of Torre del Greco (86275 inhabitants)
Recent and historical seismicity

These maps show the seismic activity in different time intervals, before the seismic event to which they refer. Data reported in the first two maps come from the analysis carried out in real time by the personnel of the INGV Operating Rooms, immediately after each earthquake. The third map shows data from 1985 to the date of the earthquake: the locations are reviewed by the seismological analysts of the INGV Italian Seismic Bulletin (Bollettino Sismico Italiano dell’INGV). The localization parameters (hypocentral coordinates and magnitude) are the best possible estimate with the data available to the INGV, but are constantly updated according to further data that become available. The location and magnitude parameters, subsequently reviewed by seismological analysts, may vary.

Earthquakes of the 3 days preceding this event

Earthquakes of the 3 days preceding this event

This map shows the earthquake epicenters with magnitude ≥ 0.0, localized with data recorded by the National Seismic Network and other collaborative networks both in Italy and in neighboring countries, in the 72 hours preceding this event. The size of the circle indicates the different classes of magnitude. The colors indicate the different time intervals preceding the seismic event. The black and white star is the epicenter of the current earthquake.
Earthquakes of the 90 days preceding this event

Earthquakes of the 90 days preceding this event

This map shows the earthquake epicenters with magnitude ≥ 2.0, localized with data recorded by the National Seismic Network and other collaborative networks both in Italy and in neighboring countries, in the 90 days preceding this event. The size of the circle indicates the different classes of magnitude. The colors indicate the different time intervals preceding the seismic event. The black and white star is the epicenter of the current earthquake.
Earthquakes from 1985 to the date of the event

Earthquakes from 1985 to the date of the event

This map shows the earthquake epicenters with magnitude ≥ 3.0, localized with data recorded by the National Seismic Network and other collaborative networks both in Italy and in neighboring countries, from 1985 to the date of this event. The size of the circle indicates the different classes of magnitude. The colors indicate the different time intervals preceding the seismic event. The black and white star is the epicenter of the current earthquake.
Earthquakes since 1000 AD until 2019

Earthquakes since 1000 AD until 2019

This map shows the epicenters of the historical earthquakes catalogue CPT15 (Catalogo Parametrico dei Terremoti Italiani, 2015 version 3.0, https://doi.org/10.13127/cpti/cpti15.3) since 1000 AD until 2019. The size of the square indicates the different classes of magnitude. For earthquakes with magnitude ≥ 6.0, it is also shown the year of occurrence and the magnitude value. The black and white star is the epicenter of the current earthquake.
Seismic hazard

Seismic hazard maps provide probabilistic estimates of the earthquake ground shaking exceeding a given threshold in a given geographic region within a given time window. Thus, it is not a deterministic prediction - a target that may be never reached given the complexity of the earthquake physical phenomenon - nor of the maximum expected earthquake since this has extremely low probabilities to occur.

In 2004, it was published the seismic hazard map of Italy (http://zonesismiche.mi.ingv.it) that provides a picture of the most hazardous geographic regions. The seismic hazard map of Italy (GdL MPS, 2004; rif. Ordinanza PCM del 28 aprile 2006, n. 3519, All. 1b) provides the 10% probability of exceedance in 50 years of the horizontal acceleration at rock sites (i.e., Vs30>800 m/s; cat. A, 3.2.1 of the D.M. 14.09.2005).

The colours indicate the various values of the ground acceleration that have 10% to be exceeded within 50 years. In general, the colours associated to low values of acceleration refer to areas that are less hazardous and stronger earthquakes repeat less frequently although they may still occur.

Seismic hazard map

Seismic hazard map

This map shows the seismic hazard map of Italy for the region where the earthquake occurred.
Shakemap
Felt maps
Locations history
Type Magnitude Date and Time (UTC) Latitude Longitude Depth (km) Published time (UTC) Author Location ID
Bulletin
Rev1000
Md 3.1 1986-01-18
14:48:23
41.674 14.262 10 2013-07-15
08:40:51
Bollettino Sismico Italiano INGV 21239
Preferred location and magnitude until now.
Origin information

Origin

Field Value
Time (UTC) 1986-01-18 14:48:23 ± 0.33
Latitude 41.6740 ± 0.0306
Longitude 14.2620 ± 0.0266
Depth (km) 10 ± 6 (from location)
Evaluation mode of Origin manual
Evaluation status of Origin reviewed
Version 1000 -> BULLETIN-VAX
Event type earthquake
Origin ID 21239

Uncertainty

Field Value
Preferred uncertainty description horizontal uncertainty
Semi-major axis of confidence ellipse (meter)
Semi-minor axis of confidence ellipse (meter)
Azimuth of major axis of confidence ellipse. Measured clockwise from South-North direction at epicenter (gradi)
Circular confidence region, given by single value of horizontal uncertainty (meter) 4058.4
Confidence level of the uncertainty (%) 68

Quality

Field Value
Largest azimuthal gap in station distribution as seen from epicenter (degree) 138
Number of associated phases, regardless of their use for origin computation 9
Number of defining phases 9
RMS of the travel time residuals of the arrivals used for the origin computation (sec) 0.3
Epicentral distance of station closest to the epicenter (degree) 0.00130
Epicentral distance of station farthest from the epicenter (degree) 0.01222
Number of stations at which the event was observed 8
Number of stations from which data was used for origin computation 8
Magnitude information

Md:3.1

Field Value
Value 3.1
Uncertainty
Num. used stations 2
Type of magnitude Md
Reference to an origin 21239
Agency INGV
Autore Bollettino Sismico Italiano INGV
Time of creation (UTC) 2013-01-04 17:23:39
Picking and Arrival
SCNL Time Uncertainty Polarity Evaluation_mode Phase Azimuth Distance(km) Takeoff_angle Residual Weight
--.SGO.Z. 1986-01-18T14:48:48.50 10.0 undecidable manual PN 144 1.3542 0.15 0.6
--.SOR.Z. 1986-01-18T14:48:44.50 10.0 undecidable manual PN 177 1.0878 -0.13 0.7
--.AQU.Z. 1986-01-18T14:48:42.00 10.0 undecidable manual PG 317 0.9213 0.01 0.8
--.OVO.Z. 1986-01-18T14:48:42.70 10.0 undecidable manual PG 173 0.8436 2.16 0
--.SD1.Z. 1986-01-18T14:48:36.00 10.0 undecidable manual SG 276 0.333 -0.41 0.3
--.MSC.Z. 1986-01-18T14:48:34.40 10.0 negative manual PG 204 0.5217 -0.13 1.9
--.SD1.Z. 1986-01-18T14:48:31.00 10.0 negative manual PG 276 0.333 0 1.9
--.SGG.Z. 1986-01-18T14:48:29.20 10.0 positive manual PG 163 0.2997 -1.09 0.7
--.DUI.Z. 1986-01-18T14:48:27.50 10.0 positive manual PG 96 0.1443 0.05 1.9
TDMT - Time Domain Moment Tensor
Fault Plane solutions in the area
Fault Plane solutions

Fault Plane solutions

The map reports the fault plane solutions for earthquakes in the region from 1977 to the date of this event. Red moment tensors are determined using the Regional Centroid Moment Tensor technique (RCMT, http://www.bo.ingv.it/RCMT) applied for earthquakes with magnitude larger than 4.5 in the Euro-Mediterranenan area. Occasionally, when a station azimuthal coverage exists RCMTs can be obtained also for earthquakes with magnitude down to 4.0. The gray moment tensors are obtained with the Time Domain Moment Tensor method (TDMT, /tdmt). This technique is applied to earthquakes with magnitude ML greater than 3.2, when it is possible. The size of symbols scales with the calculated moment magnitude Mw.
Download
Type Description Link
QuakeML - small Event, Origin, FocalMechanism Download
QuakeML - full Event, Origin, FocalMechanism, Amplitude, Arrival, Pick, Station Magnitude Download