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Station Overview

Overview Location
Picture Gallery details...
Network CH
Station Code EMMET
Station Description Emmethof, AG
Latitude (WGS84) 47.43757
Longitude (WGS84) 8.01358
Station altitude (CH1903) 740.0
running from 2012-08-16
...until now
Waveform Access open
Sensor Types Velocimeter
Geological Unit Limestone of Triassic age (Hauptmuschelkalk)
Site Morphology Class T2
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 Jura plateau
Ground type EC8 A
Ground type SIA A
Basin Information not in a sedimentary basin with possible 2D/3D effects
Reference Poggi Valerio, Fäh D., "Emmethof, Switzerland (EMMET) Report on site characterization", Swiss Seismological Service, ETH Zürich, 2014
Resonance Frequency (Hz) 1.71
Uncertainty Factor -
Vs 30 (m/s) 839
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 16-08-2012
End Date -
Housing Class Free field
Housing Description SED big pot on edge of forest in soil.
sensor depth below station 1.0 m
Distance to Building (m) -

Current Instrumentation

Location code (none)
On date 24-04-2024 13:18:00
Off date -
Sensor model Trillium Compact 120s
Sensor manufacturer Nanometrics
Digitizer model Taurus
Digitizer manufacturer Nanometrics
Channels HHE , HHN , HHZ
Stream Noise (last week) HHE , HHN , HHZ
Location code (none)
On date 16-08-2012 00:00:00
Off date 2024-04-24 13:18:00
Waveform Access open
Sensor model Trillium Compact 120s
Sensor manufacturer Nanometrics
Digitizer model Taurus
Digitizer manufacturer Nanometrics
Channels HHE , HHN , HHZ

Site Characterization

channel group
 Empirical Amplification
CH.EMMET..HH 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...
measurements nearby list...