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Station Overview

Overview Location not available
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Network CH
Station Code SBAE
Station Description Basel, Lange Erlen, BS
Latitude (WGS84) 47.5744
Longitude (WGS84) 7.6107
Station altitude (CH1903) 302.0
running from 1997-09-18
...until 2007-03-21
Waveform Access open
Sensor Types Accelerometer
Geological Unit Alluvium (Holocene)
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 Plain (Rhine river)
Ground type EC8 B
Ground type SIA C
Basin Information Rhine basin
Reference Havenith Hans-Balder, Fäh D., "SBAE: Bestimmung eines Wellengeschwindigkeitsprofils", Swiss Seismological Service, ETH Zürich, 2006
Resonance Frequency (Hz) .64
Uncertainty Factor -
Vs 30 (m/s) 375
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 18-09-1997
End Date 2007-03-21
Housing Class Urban free field
Housing Description Basement of a masonry house (concrete slab)
sensor depth below station 0.0 m
Distance to Building (m) -

Current Instrumentation

No open epochs

Location code (none)
On date 01-01-2003 00:00:00
Off date 2007-03-21 16:45:39
Waveform Access open
Sensor model AC-53
Sensor manufacturer GeoSIG
Digitizer model
Digitizer manufacturer
Channels HGE , HGN , HGZ
Location code (none)
On date 18-09-1997 00:00:00
Off date 2002-12-31 00:00:00
Waveform Access open
Sensor model AC-53
Sensor manufacturer GeoSIG
Digitizer model
Digitizer manufacturer
Channels HGE , HGN , HGZ

Site Characterization

channel group
 Empirical Amplification
CH.SBAE..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...
measurements nearby list...