2026 SCEC Fault Creep Workshop

Leverage decades of Bay Area fault‑creep observations to unlock new insights into earthquake behavior and join the community effort to modernize and expand long‑term creep monitoring

Date: March 3-6, 2026
Location: San Jose State University, San Jose, CA
Workshop Organizers: Elizabeth Madden (SJSU), Christie Rowe (UNR)
SCEC Award: 26025

Workshop applications closed on February 4, 2026

Overview

The San Francisco Bay Area is cut by a network of faults, many of which are creeping. Creep has been measured since the 1970s by survey measurements of 89 alignment arrays and this extraordinary dataset provides evidence for creep transients, some triggered by regional earthquakes, which propagate along strike over days to years. Currently there is no plan for continuing alignment array measurements, a time-consuming task which may be best shared across the research community. In addition, considering these data alongside alternative methods for observing creep is critical to advance understanding of loading conditions and stress transfer patterns in space and time that underlie fault mechanics, seismic cycling and earthquake rupture dynamics. Limited understanding of how creep influences seismic hazard further underscores the need to focus collaborative research in this area and reconsider long term monitoring of creep. With the expansion to Northern California, the Statewide California Earthquake Center is well positioned to facilitate this collaboration. Workshop goals:

  • Develop a community plan for alignment array measurement
  • Evaluate array locations, restore lost stations and consider new fault mapping to confirm/expand coverage
  • Share alternative creep observation methods complementary to alignment arrays
  • Plan how to best capture creep-related deformation into the future, including setting specific targets for spatial and temporal resolution to maintain or increase quality of creep records
  • Discuss incorporation of creep measurements into SCEC Community Earth Models (e.g. CGM)
  • Define community goals for data continuity in time and space that would allow replacement of alignment array measurements with other more efficient methods

We welcome applications from individuals interested in the interaction of transient and long-term fault creep on seismic hazard, the use of creep observations to constrain timescales of locking and slip, stress transfer, and fault interactions, geodetic, geophysical and geologic methods for constraining fault creep and understanding its mechanisms, and those interested in expanding an interdisciplinary consortium for longer term monitoring in northern and central California.

Workshop Costs

The workshop registration fee is $150, covering meals and transportation during the field trip on March 4.  Costs to participants may also include meals on other days (not included in the registration fee) transportation to/from San Jose (SJC), and parking at SJSU.

For supported out-of-town participants, lodging will be arranged at the Signia Hotel walking distance to the meeting room on San Jose State’s campus. Additional SCEC travel support may be available based on financial need, with priority given to students, early-career researchers, and those without institutional funding. Additional support may cover the registration fee only or may include additional travel expenses.

Applicants should complete the travel support section carefully when applying. Accepted participants will be notified by February 10, 2026, with details on registration payment, hotel reservations, and additional travel support if applicable.

All times are Pacific Standard Time (UTC-8). 

March 3, 2026

TimeDescriptionPresenter
Session 1: Creep and creep measurements
Clarify what we do we know about Bay Area creep. Identify what we should know about Bay Area creep to advance fundamental science and better mitigate seismic hazard.
12:30 - 13:00IntroductionChristie RoweAhmed Elbanna
13:00 - 13:20Decades of Alignment Array MonitoringF. McFarland
13:20 - 13:40Geologists measuring creep in the Bay area - brief history and future possiblitiesStephen DeLong
13:40 - 14:00An overview of the USGS Creepmeters along the San Andreas, Calaveras, and Hayward faultsTodd Ericksen
14:00 - 14:20Recent innovations in the measurement of fault creepRoger Bilham
14:20 - 14:40What surface data obscure: Measuring fault creep below the water tableJosie Nevitt
14:40 - 15:00Implementing Creep Measurements in US National Seismic Hazard ModelsKaj Johnson
15:00 - 16:15Breakout 1
  • What do we think we know from creep data?
  • What can we learn from continued monitoring of creep, ie what are the key research opportunities associated with these data?
  • What do we need from the dataset to better mitigate seismic hazard?
  • What is solid from the current dataset or monitoring methods? (what do we want to keep)
  • What is missing from the current dataset or monitoring methods? (what do we need to add)
  • What is no longer relevant from the current dataset or monitoring methods? (what do we need to remove)
16:15 - 16:45Field trip previewStephen DeLongJosie Nevitt / Todd Ericksen / Roger Bilham
16:45Adjourn Day 1

March 4, 2026

TimeDescriptionPresenter
Session 2: Measuring Creep in the Field
Ensure that all participants understand the current creep monitoring technology and discuss its limitations, advantages and future. Discuss new/potential creep assessment tools.
08:30Meet for all day field trip
Site 1/2Visit one or two alignment array sites and take measurementsStephen DeLong
Site 3Visit Gallegos Winery in Fremont, location of creepmeter CFW and a subsurface in-place inclinometer system across the Hayward fault.Josie NevittRoger Bilham / Todd Ericksen
18:00Workshop Dinner (San José)

March 5, 2026

TimeDescriptionPresenter
Session 3: Deep dive on comparison of alignment arrays and other monitoring methods
Critique current creep dataset and highlight challenges of data collection. Consider alternative/complementary monitoring strategies (microseismicity, remote sensing, creepmeters, structure from motion, lidar, etc). Highlight spatial and temporal resolutions provided by current and alternative methods.
09:00 - 09:30Introduction & field trip reviewStephen DeLongJosie Nevitt
09:30 - 09:45Implications of decadal changes in fault creep on Hayward faultRoland Burgmann
09:45 - 10:00Quantifying creep rates along the Central San Andreas Fault from repeat high-resolution topographyChelsea Scott
10:00 - 10:15Small-scale propagation of shallow creep events and environmental effects on the San Andreas fault, central CaliforniaHeather Crume
10:15 - 10:30Monitoring creep with coda wave interferometryThomas Luckie
10:30 - 10:45Reports on the Sargent Fault from alignment array data and trenching the creepy San AndreasBelle Philibosian
10:45 - 11:00Break
11:00 - 11:15Fault zone geodesy at USGS ESC: Challenges and Future DirectionsAndrew Barbour
11:15 - 11:30Structure, Deformation, and Rheology of the Hayward Fault: Where the Urban Fault Meets the RoadEric Fielding
11:30 - 11:45Multi-decadal GPS data set developed by the USGS Earthquake Science Center for measuring and modeling interseismic creep on faults in central and northern CaliforniaJessica Murray
11:45 - 12:00Perspectives on monitoring and modeling creep using InSAR, GNSS and repeating earthquakesGareth Funning
12:00 - 12:15The Pros and Cons of Air- and Space-based Remote Sensing of Creep in Northern CaliforniaKatherine Guns
12:15 - 13:15Lunch
13:15 - 14:23Thunder talks -- 4 minutes -- No "Minson" words! Pop up where you are sitting
13:15Evidence of creep on the San Gregorio Fault?Kim Blisniuk
13:19Repeat LiDAR along the San Gregorio Fault to monitor creepAshley Walsh
13:23Integrating LiDAR to identify 3D fault geometry along the Central Calaveras FaultKaren Castaneda
13:27Geomorphic characterization of fault creep along the Calaveras FaultHannah Martin
13:31The Concord fault - new trace and Alquist-Priolo mappingDanielle Madugo
13:35Updating creep measurements on the Hayward FaultEvan Agbayani
13:39Aseismic creep monitoring for linear utility assetsChristopher Madugo
13:43Updated high-resolution creep rates along the central SAF from repeat lidar differencingCatherine Hanagan
13:47Mapping the creeping section of the Bartlett Springs FaultRezagene Milani
13:51Observational implications of geometric influences on fault creep variabilityJaeseok Lee
13:55Northern California repeating earthquake mapTaka'aki Taira
13:59Fault based inversion modeling for the Bay Area: Assessing slip rates and off fault deformationCate Sloat
14:03Observing coseismic deformation using optical remote sensingSolène Antoine
14:07Laboratory attempts to measure the bulk viscous rheology of porous rocks at shallow depth conditionsHiroki Sone
14:11Spatiotemporal patterns and predictability of shallow slow slip sequences on the Superstition Hills fault Junle Jiang
14:15How is surface creep related to deep structure? A depth-dependent geometric complexity study of the Creeping San Andreas FaultTravis Alongi
14:19 - 14:40Break
14:40 - 15:10

Breakout 2

  • What can we learn from creep data? Does the dataset reveal fault loading cycles, absolute stress, patterns of strain partitioning, etc.? How can we best use the data to mitigate seismic hazard?
  • Does the total set cover the necessary areas to realize the research opportunities defined when answering the previous questions? If not, what additions, modifications, and/or restorations to the arrays are needed? What is the ideal dataset and how might it be collected?
  • How does array data dovetail with complementary datasets, or is there processing or organization that could facilitate this?
15:10 - 15:40Reconvene in larger group to share reflections and meet objectives.
Session 4: Planning for the future of creep monitoring
Build plans for maintaining current alignment array collection including criteria for measurement site priorities and benchmarks for site abandonment. Considering needed spatial and temporal collection scales, plan replacement or integration with other measurement methods. Plan for post-seismic measurements and operationalizing afterslip forecasting.
15:40 - 15:55Community Geodetic ModelMike Floyd & Katia Tymofyeyeva
15:55 - 16:10Migrating USGS fault creep measurements and processing workflows to the cloudCurtis Baden
16:10 - 16:25Fault creep information and dynamic rupture simulationsRuth Harris
16:25 - 16:40Break
16:40 - 17:10Breakout 3
  • What other observations/instrumentation contribute to the broad creep picture in time and space?
  • Are there opportunities that we should take advantage of for replacing or complementing alignment arrays with other datasets?
  • Are there efficiencies to realize in the workplan for upkeep?
  • What are ideal spatial collection scales?
  • Which improvements (e.g. densification near the creeping strands or targeting specific fault connections points, like the Hayward/Calaveras) should be considered?
  • What is needed for successful post-seismic investigations?
  • What is needed to operationalize afterslip forecasting?
17:10 - 17:40Reconvene in larger group to share reflections and meet objectives.
17:40End

March 6, 2026

TimeDescriptionPresenter
08:30 - 12:00Session 5: Workplan writing
Plan for draft report summarizing state of the art in measurement approaches and hazard applications for fault creep. Define community goals for data continuity in time and space that would allow for continued collection or replacement of alignment array measurements with more efficient or precise methods.
08:30 - 09:00Introduction to community synthesis on critical topics for planning the future of the alignment arrays (AA)
09:00 - 09:30Topic 1: State of the AA network - tabulation of which AA sites are in good shape, which need updates or additions, which are poorly documented
09:30 - 10:00Topic 2: Considering different faults and/or regions, which are in locations that we should continue to monitor or abandon? Under what criteria can we consider the AA obsolete? Are there any regions where we are approaching that threshold?
10:00 - 10:20Break
10:20 - 11:00Topic 3: What is the value of alignment arrays? Where do the data overlap with other methods that should be prioritized over AA monitoring?
11:00 - 11:40Topic 4: Community action - what efforts are necessary vs. aspirational to maintain utility of the AA dataset? How will the community accomplish this through coordination?
11:40 - 12:00Wrap-up and conclude

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