ANTWERPEN (BE)

Controlled explosion1 July 2018

Magnitude
1.7ML
Depth
–
Belgian time
19:00:232018-07-01
UTC
17:00:232018-07-01

Main parameters

Date and time2018-07-01 17:00:23 UTC
2018-07-01 19:00:23 Belgian time
MagnitudeML 1.7
Epicentral coordinates51.238° N, 4.423° E
Uncertainty ± 5.5 km
Event IDROB 6830

Data source : ROB (Royal Observatory of Belgium)
Last update : 2018-07-05 14:14:50 Belgian time

Location map

  • Epicentre
  • Station that recorded the event

Macroseismic inquiry

Intensities derived from the answers to the online questionnaire “Did you feel an earthquake?”, grouped by municipality (former municipalities included). The map and the chart give the intensity of each municipality.

Answers
16
Municipalities
1
Farthest municipality
3km · ANTWERPEN
Countries
Belgium
Grouping
Show
Intensity of the municipality (CII)
  • I
  • II
  • III
  • IV
  • V
  • VI
  • VII+
Answers per municipality
  • 3–4
  • 5–9
  • 10–19
  • 20–49
  • ≥ 50
  • Epicentre

Answers by intensity

IntensityAnswers
I1
II0
III7
IV7
V1
Total16

Intensity against distance

  • Intensity of the municipality (CII)

Warning: the intensities derived from the inquiry are raw, unverified data.

Notes and method

Intensity of a municipality or a cell (CII, Community Internet Intensity) is computed as follows:

  • I if no answer reports that the earthquake was felt;
  • II–IX computed from 3 answer(s) kept: CII = 3.40 ln(CWS) − 4.38 (Wald et al., 1999), applied to the weighted sum (CWS) of the mean indexes of the answers; at least II if felt, at most IX.

Answers kept (USGS method, as applied by the ROB): reliability of 80 or more, given on the ground floor up to the 4th floor (or unknown floor), without those more than two standard deviations from the mean. The “felt” index is weighted by the answer to “Did others nearby feel it?”.

Distribution by intensity: macroseismic intensity (MI) recorded for each answer.

Cells: 5 or 10 km squares of the Belgian Lambert 72 grid, each answer placed at its geocoded address or at the point it placed on the map, otherwise at the centre of its municipality. The positions of the answers are published only rounded to about 1 km, in “Arrival of the answers”. Grid cell method: Van Noten et al. (2017), Solid Earth 8, 453–477, doi:10.5194/se-8-453-2017.

Depth not determined: distances measured from the epicentre.

Answers read on 2026-11-09 09:53.

Arrival times at the stations

Each station first records the P wave, the fastest, then the S wave. The farther a station is from the epicentre, the later the waves reach it and the wider the gap between the two.

Stations
14
Epicentral distance
46.4 – 148.7km
Mean velocity, P wave
5.9km/s
  • P wave
  • S wave
  • Curve fitted to the measurements
Notes and method

Curves: travel time of a direct wave in a homogeneous medium. The velocity of each wave and an origin-time shift, common to both, are fitted to the measurements by least squares. Depth not determined: hypocenter placed at the surface for the calculation. P wave: 10 measurements, root-mean-square deviation 0.87 s.

Stations farther than 120 km are left out of the fit: the first waves to reach them have travelled beneath the crust, through the mantle, where they propagate faster.

Table of measurements

Station measurements

P- and S-wave arrivals and ground displacement measured at each station. Click a column heading to change the order.

km°UTCUTCs
Belgian seismic network (Royal Observatory of Belgium)14 stations
MOLTMol46.49317:00:31.54+8.35 s––
SKQSteenkerque69.820017:00:34.52+11.33 s––
LESLessines71.321517:00:35.58+12.39 s––
RQRRonquières71.619117:00:36.01+12.82 s––
OPTOpitter86.09917:00:40.71+17.52 s––
BRQBracquegnies86.619417:00:38.46+15.27 s––
BOUBougnies100.220017:00:40.75+17.56 s––
GESGesves105.815317:00:41.57+18.38 s––
MRDMaredsous106.916717:00:41.00+17.81 s––
CLAClavier110.214517:00:42.43+19.24 s––
DOUDourbes127.717417:00:44.91+21.72 s––
MEMSMembach131.712117:00:45.31+22.12 s––
MRGMont Rigi141.612417:00:47.22+24.03 s––
HOUHouvegnez148.713117:00:47.68+24.49 s––
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