Station Overview

image
legend Overview at SMOE
Overview Location not available
Picture Gallery details...
Network CH
Station Code SMOE
Station Description Moudon, Ecole, VD
Latitude (WGS84) 46.6718
Longitude (WGS84) 6.80111
Station altitude (CH1903) 527.0
running from 2015-03-11
...until now
Waveform Access open
Sensor Types Accelerometer
Geological Unit Gravel and sand ("Schotter")
Site Morphology Class T1
T1: flat; T2: slope; T3: ridge and T4: steep ridge;
following Pessina and Fiorini (2014) A GIS procedure for fast topographic characterization of seismic recording stations, Soil Dynamics and Earthquake Engineering, 63, p248-258
Site Morphology Description Valley
Ground type EC8 B
Ground type SIA B
Basin Information Broye basin, interface at fundamental frequency at 15 m depth
Reference Michel Clotaire, Hobiger M., Fäh D., "Site Characterization Report SMOE: Moudon (VD) - Ecole", Swiss Seismological Service, ETH Zürich, 2016
Resonance Frequency (Hz) 10.01
Uncertainty Factor -
Vs 30 (m/s) 570
Location Map


Federal Office of Topograpy: National Map 1:25‘000
Topography Map


Federal Office of Topograpy: DHM25: Digital Height Model 1:25000
Geology Map

Federal Office of Topograpy: Geological map of Switzerland 1:500‘000

Sensor locations

Location Code (none)
Opening Date 11-03-2015
End Date -
Housing Class Free field
Housing Description SSMNet big pot
sensor depth below station 1.0 m
Distance to Building (m) -

Current Instrumentation

Location code (none)
On date 19-04-2023 10:00:00
Off date -
Sensor model EpiSensor ES-T
Sensor manufacturer Kinemetrics
Digitizer model Centaur
Digitizer manufacturer Nanometrics
Channels HGE , HGN , HGZ
Stream Noise (last week) HGE , HGN , HGZ
Location code (none)
On date 11-03-2015 06:40:58
Off date 2023-04-19 10:00:00
Waveform Access open
Sensor model EpiSensor ES-T
Sensor manufacturer Kinemetrics
Digitizer model Centaur
Digitizer manufacturer Nanometrics
Channels HGE , HGN , HGZ

Site Characterization

channel group
Empirical Amplification
CH.SMOE..HG not available

Obtained from spectral modeling of small earthquakes with constant update.

  • Top: Fourier amplification with elastic (dashed line) and anelastic (solid line) amplification functions;
  • Centre: 5% damped response spectra amplification (anelastic);
  • Bottom: Number of recordings used.

See Edwards et al. (2013), Determination of Site Amplification from Regional Seismicity: Application to the Swiss National Seismic Networks. Seismological Research Letters, 84(4), 611–621.

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Authoritative Site Characterization Analysis details...
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