legacy data

Real-time Data

Legacy Data	Real-Time Data

Raspberry Shake Data Center

Feed your research with high quality data

The Raspberry Shake Data Center (SDC) is online and ready to serve you. All (*) of the historical seismic data from the Raspberry Shake network is available for download using the SDC’s FDSN Web Service.

Data Center

Data from over 3,000 stations

Raspberry Shake operates the largest permanent real-time streaming seismic network in the world

200 TB of data

Since 2016, the SDC has collected over 60 TB of seismic and infrasound data, complete with instrument response files

Free access

All historical data is freely accessible via the SDC’s FDSN Web Service

Seismology’s first and only crowd sourced data center

Data from the Raspberry Shake network has grown enormously thanks to continuous real-time contributions from professional seismologists and citizen scientists alike. This is community science participation at its best.

FDSN Web Services

Use the SDC’s FDSNWS to access station metadata in FDSN StationXML, StationXML and SC3XML formats and time series data in miniSEED format. All (*) historical data all the way back to 2016 when Raspberry Shake was born is now online and available via FDSNWS.

IP to use for fdsnws queries:
https://data.raspberryshake.org/fdsnws/

(*) All historical data is available via the FDSN Web Service, except EN* channels (strong motion), which are limited to the past year.

Data Center

Examples

fdsnws-dataselect example via wget:

Copy to Clipboard

fdsnws-dataselect example via ObsPy:

Copy to Clipboard

Find all details in the manual

Peer reviewed publications

Scientific journals have already begun to publish original research that leverages data from the SDC. We have made the historical data freely accessible and easy to access. What hypotheses will you test?

Peer Reviews

Citizen seismology helps decipher the 2021 Haiti earthquake

A network of citizen seismometers installed in 2019 provided near-field data critical to rapidly understand the mechanism of the mainshock and monitor its aftershock sequence.