MENU

Station Overview

image
legend Overview at SWYZ
Overview Location not available
Picture Gallery details...
Network CH
Station Code SWYZ
Station Description Schwyz Kantonsschule Kollegium, SZ
Latitude (WGS84) 47.02375
Longitude (WGS84) 8.65261
Station altitude (CH1903) 547.0
running from 2018-07-19
...until now
Waveform Access open
Sensor Types Accelerometer
Geological Unit Gravel, sand, silt, partly blocks (detritic cone)
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 Fluvial geomorphology: alluvial slope, plain, cone
Ground type EC8 B
Ground type SIA B
Basin Information In a sedimentary basin with 1D resonance and probable lateral propagation basin
Reference Panzera Francesco, Hobiger M. & Fäh D., "SITE CHARACTERIZATION REPORT SWYZ: Schwyz (SZ)", Swiss Seismological Service, ETH Zürich, 2019
Resonance Frequency (Hz) 1.21
Uncertainty Factor -
Vs 30 (m/s) 561
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 19-07-2018
End Date -
Housing Class Urban free-field
Housing Description SED big pot, concrete vault, sensor bolted to the Foundation
sensor depth below station 1.0 m
Distance to Building (m) -

Current Instrumentation

Location code (none)
On date 19-07-2018 18:00:00
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

Site Characterization

channel group
 Empirical Amplification
CH.SWYZ..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.

H/V pick image:
Authoritative Site Characterization Analysis details...
measurements nearby list...