HOPS - Hopland Research and Extension Center
We operate broadband and borehole stations under the network code BK. The Berkeley Digital Seismic Network (BDSN) is a regional network of very broadband and strong motion seismic stations designed to monitor regional seismic activity as well as provide high quality data. The Berkeley borehole stations have borehole geophones or other seismic sensors and may have other geophysical instrumentation.
BARD is our GPS network for monitoring crustal deformation across the Pacific-North America plate boundary and in the San Francisco Bay Area for earthquake hazard reduction studies and rapid earthquake emergency response assessment
| Station Name | HOPS (HOPL) |
| In Operation | 1998/03/24 22:42:00 - Present |
| Latitude | |
| Longitude: | |
| Elevation: | 353.2323 meters |
| Instrumentation | Broadband GPS |
Location
HOPS is located at the Hopland Research and Extension Center of the University of California Agriculture and Natural Resources unit.Network
Berkeley Digital Seismic Network (BK)Bay Area Regional Deformation Network Network (BARD)
Geology
Cretaceous and Jurassic sandstone with smaller amounts of shale, chert, limestone, and conglomerate
Borehole Conditions
The instruments are located in a steel and concrete vault benched into a hillside with 2 meters of soil overburden. The vault is oriented north/south to minimize the effects of solar heating. The concrete pier is covered with 4" of insulation on the sides and 8" of insulation on the top. The datalogger and supporting equipment are in an adjacent room.GPS Monument Description
Deep-Drilled Braced
Table of Seismic Instrumentation
| Sensor | Datalogger | SEED Channels | Location | |
| Broadband | STS-7 | Q330HRS | BH?,HH?,LH?,VH? | 00 |
| Accelerometer | EPISENSOR ES-T | Q330HRS | HN? | 00 |
| Auxiliary | ANTENNACURRENT | Q330HRS | VE? | 00 |
| CLOCKPHASE | Q330HRS | LC?,VC? | 00 | |
| CLOCKQUALITY | Q330HRS | LC?,VC? | 00 | |
| SYSTEMCURRENT | Q330HRS | VE? | 00 | |
| VCOVALUE | Q330HRS | VC? | 00 | |
| CALIBRATIONINPUT | Q330HRS | LC? | EP | |
| INPUTVOLTAGE | Q330HRS | LE? | EP | |
| MODEL 270 | Q330HRS | LD? | EP | |
| SYSTEMHUMIDITY | Q330HRS | LI? | EP | |
| SYSTEMPRESSURE | Q330HRS | LD? | EP | |
| SYSTEMTEMPERATURE | Q330HRS | LK? | EP |
GPS Instrumentation
| Receiver | Antenna | Radome | - | |
| GPS | SEPTENTRIO POLARX5 | SEPTENTRIO SEPCHOKE_B3E6 | SPKE | - |
Waveforms and associated metadata, and GPS data, are available at the Northern California Earthquake Data Center (NCEDC).
Waveform Data
- BK Information Directory, including
- List of station locations
- List of available channels
- Instrument Response
- Querying the archives
- Download waveform data
GPS Data
- Site log: hopl.log
Data Type From To Low-rate raw -- -- Low-rate rinex 11/17/2022 present High-rate raw 2/6/2024 present High-rate rinex 2/6/2024 present
Noise Analysis
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GPS Data Quality
Completeness
Data completeness is defined both as "Completeness of observations" and "Cycle slips per observation". "Completeness of Obs." is the number of epochs in the final RINEX file normalized to the expected number. This percentage will go down if time is missing from the RINEX file. "Cycle slips per Obs." is the total number of detected cycle slip normalized to the total number of observations in the RINEX file. This number will increase as the receiver loses lock on satellites more frequently.
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Multipath
The effects of multipath on the data are estimated by parameters for L1 and L2 (MP1 and MP2 respectively); see Estey and Meertens (GPS Solutions, 1999) for derivation. The daily value is the RMS of MP1 and MP2 throughout the day and for all satellites. Higher values indicate a greater prevalence and/or strength of multipathing, i.e. objects on the ground are providing multiple reflection pathways from the satellite to antenna.
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Signal-to-Noise Ratio
The Signal-to-Noise ratios are the mean values above the QC elevation mask for L1 and L2 respectively.
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