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

Summary

The 2026 SCEC workshop on Fault Creep Rates in the San Francisco Bay Area brought together researchers studying fault creep through field observations, geodetic measurements, remote sensing, laboratory experiments, and numerical modeling to evaluate the future of fault creep monitoring in California and its applications to earthquake science. The workshop was motivated by the unique record of fault creep measurements collected since the 1970s from nearly 90 alignment arrays across the San Francisco Bay Area—a remarkable dataset that has documented creep transients, some triggered by regional earthquakes, but for which no long-term monitoring plan currently exists. Participants examined how these observations, together with complementary techniques such as creepmeters, GNSS, InSAR, lidar, structure-from-motion photogrammetry, and coda wave interferometry, can improve understanding of fault loading, stress transfer, seismic cycling, earthquake rupture dynamics, and seismic hazard.

Through field demonstrations, invited presentations, breakout discussions, and collaborative planning, participants developed a community roadmap for sustaining and modernizing California’s fault creep observing system. The workshop established priorities for integrating long-term alignment array measurements with emerging monitoring technologies, preserving and expanding community access to fault creep datasets through SCEC Community Earth Models, and advancing collaborative research on the role of fault creep in earthquake mechanics and seismic hazard. The meeting also launched a community white paper reviewing current and emerging creep monitoring methods and outlining recommendations that will guide future research, data stewardship, and coordinated community activities.

The Fault Creep Workshop combined scientific presentations with a full-day field excursion and a concluding community workplan and white paper writing session. This intentional format enabled participants to compare fault creep monitoring methods in the field before developing shared priorities for future monitoring, data stewardship, and collaborative research. SEE PHOTOS

Key Outcomes

The workshop produced several important scientific and community outcomes that will guide future research on fault creep and its role in earthquake mechanics and seismic hazard. Highlights are summarized below, with additional detail available in the workshop report.

  1. A community roadmap for sustaining California’s fault creep observing system: One of the workshop’s most significant outcomes was the development of a community roadmap for the future of fault creep monitoring in California. Participants evaluated the long-term alignment array measurements that have documented fault creep in the San Francisco Bay Area since the 1970s alongside emerging observational technologies, recognizing the unique scientific value of this decades-long dataset and the need for a coordinated community effort to sustain and expand fault creep monitoring. The workshop highlighted the importance of integrating long-term observations with new measurement approaches to better understand fault loading, stress transfer, seismic cycling, and earthquake rupture dynamics.
  2. Priorities for advancing fault creep observations and earthquake science: Participants compared the capabilities of alignment arrays, creepmeters, GNSS, InSAR, lidar, structure-from-motion photogrammetry, coda wave interferometry, laboratory experiments, and other emerging approaches for monitoring fault creep. Discussions emphasized that these complementary methods provide new opportunities to characterize spatial and temporal variations in creep, improve understanding of fault mechanics, and evaluate the role of fault creep in earthquake rupture and seismic hazard. The workshop also identified important scientific questions requiring future investigation, including the relationship between creep and fault loading through the seismic cycle, the influence of creep on seismic hazard, and the controls on creep at depth.
  3. Priorities for community datasets and cyberinfrastructure: Participants identified opportunities to better organize, preserve, and share fault creep observations through SCEC community resources. Discussions focused on incorporating alignment array measurements and other creep datasets into the SCEC Community Geodetic Model, Community Fault Model, and Fault Slip Rate Database, while preserving the extensive historical records and metadata associated with long-term monitoring sites. These community resources will improve accessibility of fault creep observations and support future research on fault behavior, earthquake mechanics, and seismic hazard.
  4. Launching collaborative community products and future initiatives: The workshop initiated several collaborative efforts that will extend its impact beyond the meeting itself. Participants launched preparation of a community white paper reviewing current and emerging methods for monitoring fault creep and comparing the performance of 31 observational approaches. The workshop also established broad recommendations for future monitoring, data stewardship, and scientific priorities, providing a foundation for future proposals, including development of a SCEC Technical Activity Group (TAG) focused on a coordinated community workplan for fault creep research.
  5. Building an interdisciplinary fault creep research community: The workshop brought together 58 scientists from universities, federal and state agencies, national laboratories, and industry to evaluate the future of fault creep monitoring and its applications to earthquake science. The program combined field demonstrations, invited presentations, lightning talks, and breakout discussions that brought together researchers working across observational, experimental, and modeling disciplines. By fostering collaboration among scientists using diverse approaches to measuring and interpreting fault creep, the workshop established a shared scientific agenda for advancing long-term fault creep observations and their application to earthquake mechanics and seismic hazard.

References

Madden, E. H., & Rowe, C. D. (2026). 2026 Fault creep rates in the San Francisco Bay Area Workshop Report: Statewide California Earthquake Center. SCEC Contribution 15186

Presentation materials may be viewed by clicking the links below. PLEASE NOTE: Files are the author’s property. They may contain unpublished or preliminary information and should only be used for reviewing the talk. Only the presentations for which SCEC has received permission to post publicly are included below.

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

March 3, 2026

TimeDescriptionPresenter

Session 1: Creep and creep measurements
Clarify what we know about fault creep in the San Francisco Bay Area. Identify what we still need to understand to advance fundamental science and improve seismic hazard assessment.

12:30 - 13:00
  • Introduction
Christie Rowe / Ahmed Elbanna
13:00 - 13:20
  • Decades of Alignment Array Monitoring
F. McFarland
13:20 - 13:40
  • Geologists measuring creep in the Bay area - brief history and future possibilities (PDF)
Stephen DeLong
13:40 - 14:00
  • An overview of the USGS Creepmeters along the San Andreas, Calaveras, and Hayward faults
Todd Ericksen
14:00 - 14:20
  • Recent innovations in the measurement of fault creep (PDF)
Roger Bilham
14:20 - 14:40
  • What surface data obscure: Measuring fault creep below the water table
Josie Nevitt
14:40 - 15:00
  • Implementing Creep Measurements in US National Seismic Hazard Models
Kaj Johnson
15:00 - 16:15

Breakout 1

  • What have we learned from existing fault creep observations?
  • What are the highest-priority research opportunities enabled by continued fault creep monitoring?
  • What additional observations or datasets are needed to better understand and mitigate seismic hazard?
  • Which aspects of the current datasets and monitoring methods are most valuable and should be maintained?
  • What important observations or capabilities are missing from the current datasets and monitoring methods?
  • Which datasets, measurements, or monitoring approaches are no longer effective or should be modernized?
16:15 - 16:45Field trip previewStephen DeLong / Josie 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 current fault creep monitoring technologies and discuss their advantages, limitations, and future applications. Explore emerging and potential new approaches for measuring fault creep.

08:30Meet for all day field trip
Sites 1 and 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 Nevitt / Roger 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
Evaluate the strengths and limitations of current fault creep datasets and monitoring methods, with particular emphasis on alignment arrays. Compare alternative and complementary approaches—including microseismicity, remote sensing, creepmeters, structure-from-motion photogrammetry, and lidar—and assess their relative spatial and temporal resolution, data quality, and long-term monitoring potential.

09:00 - 09:30
  • Introduction & field trip review
Stephen DeLong / Josie Nevitt
09:30 - 09:45
  • Implications of decadal changes in fault creep on Hayward fault (PDF)
Roland Burgmann
09:45 - 10:00
  • Quantifying creep rates along the Central San Andreas Fault from repeat high-resolution topography (PDF)
Chelsea Scott
10:00 - 10:15
  • Small-scale propagation of shallow creep events and environmental effects on the San Andreas fault, central California
Heather Crume
10:15 - 10:30
  • Monitoring creep with coda wave interferometry (PDF)
Thomas Luckie
10:30 - 10:45
  • Reports on the Sargent Fault from alignment array data and trenching the creepy San Andreas
Belle Philibosian
10:45 - 11:00
  • Break
11:00 - 11:15
  • Fault zone geodesy at USGS ESC: Challenges and Future Directions
Andrew Barbour
11:15 - 11:30
  • Structure, Deformation, and Rheology of the Hayward Fault: Where the Urban Fault Meets the Road
Eric Fielding
11:30 - 11:45
  • Multi-decadal GPS data set developed by the USGS Earthquake Science Center for measuring and modeling interseismic creep on faults in central and northern California (PDF)
Jessica Murray
11:45 - 12:00
  • Perspectives on monitoring and modeling creep using InSAR, GNSS and repeating earthquakes (PDF)
Gareth Funning
12:00 - 12:15
  • The Pros and Cons of Air- and Space-based Remote Sensing of Creep in Northern California
Katherine Guns
12:15 - 13:15Lunch
13:15 - 14:23Thunder talks: 4 minute presentations. No "Minson" words! Pop up where you are sitting and share your work.
13:15
  • Evidence of creep on the San Gregorio Fault?
Kim Blisniuk
13:19
  • Repeat LiDAR along the San Gregorio Fault to monitor creep
Ashley Walsh
13:23
  • Integrating LiDAR to identify 3D fault geometry along the Central Calaveras Fault
Karen Castaneda
13:27
  • Geomorphic characterization of fault creep along the Calaveras Fault (PDF)
Hannah Martin
13:31
  • The Concord fault - new trace and Alquist-Priolo mapping
Danielle Madugo
13:35
  • Updating creep measurements on the Hayward Fault
Evan Agbayani
13:39
  • Aseismic creep monitoring for linear utility assets
Christopher Madugo
13:43
  • Updated high-resolution creep rates along the central SAF from repeat lidar differencing (PDF)
Catherine Hanagan
13:47
  • Mapping the creeping section of the Bartlett Springs Fault
Rezagene Milani
13:51
  • Observational implications of geometric influences on fault creep variability
Jaeseok Lee
13:55
  • Northern California repeating earthquake map
Taka'aki Taira
13:59
  • Fault based inversion modeling for the Bay Area: Assessing slip rates and off fault deformation
Cate Sloat
14:03
  • Observing coseismic deformation using optical remote sensing (PDF)
Solène Antoine
14:07
  • Laboratory attempts to measure the bulk viscous rheology of porous rocks at shallow depth conditions
Hiroki Sone
14:11
  • Spatiotemporal patterns and predictability of shallow slow slip sequences on the Superstition Hills fault
Junle Jiang
14:15
  • How is surface creep related to deep structure? A depth-dependent geometric complexity study of the Creeping San Andreas Fault
Travis Alongi
14:19 - 14:40Break
14:40 - 15:10

Breakout 2

  • What can we learn from fault creep data? Does the existing dataset reveal fault loading cycles, absolute stress, patterns of strain partitioning, or other key processes? How can these observations best inform seismic hazard assessment?
  • Does the current monitoring network adequately address the research opportunities identified in Breakout 1? If not, what additions, modifications, or restoration of alignment arrays are needed? What would an ideal fault creep monitoring dataset look like, and how might it be achieved?
  • How can alignment array measurements be integrated with complementary datasets? What improvements in data processing, organization, or accessibility would facilitate integration with other fault creep observations and support future research?
15:10 - 15:40Reconvene in larger group to share reflections and meet objectives.

Session 4: Planning for the future of creep monitoring
Develop a community strategy for maintaining the alignment array network, including criteria for prioritizing measurement sites and identifying sites for retirement or replacement. Consider the spatial and temporal sampling needed to address future research priorities, and evaluate opportunities to integrate or transition to complementary monitoring methods. Develop recommendations for post-earthquake creep monitoring and operational approaches for observing and forecasting afterslip.

15:40 - 15:55
  • Community Geodetic Model (PDF)
Mike Floyd & Katia Tymofyeyeva
15:55 - 16:10
  • Migrating USGS fault creep measurements and processing workflows to the cloud (PDF)
Curtis Baden
16:10 - 16:25
  • Fault creep information and dynamic rupture simulations (PDF)
Ruth Harris
16:25 - 16:40Break
16:40 - 17:10

Breakout 3

  • What additional observations or monitoring technologies contribute to understanding fault creep through time and across fault systems?
  • What opportunities exist to complement or, where appropriate, replace alignment arrays with other observational datasets or monitoring methods?
  • What efficiencies can be achieved in maintaining and operating the long-term monitoring network?
  • What are the optimal spatial scales for future fault creep observations?
  • Where should monitoring be enhanced (e.g., by increasing station density near creeping fault strands or targeting key fault connections such as the Hayward–Calaveras system)?
  • What observations and capabilities are needed to support effective post-earthquake creep investigations?
  • What data, monitoring, and operational capabilities are needed to improve observation and forecasting of afterslip?
17:10 - 17:40Reconvene in larger group to share reflections and meet objectives.
17:40End

March 6, 2026

TimeDescription
08:30 - 12:00

Session 5: Workplan writing
Develop a draft report summarizing the current state of the art in fault creep monitoring methods and their applications to earthquake science and seismic hazard. Define community goals for maintaining long-term data continuity in space and time, including recommendations for sustaining alignment array measurements and integrating or transitioning to more efficient or higher-precision monitoring technologies.

08:30 - 09:00
  • Introduction to community synthesis on critical topics for planning the future of the alignment arrays (AA)
09:00 - 09:30
  • Topic 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 - 10:00
  • Topic 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 - 11:00
  • Topic 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 - 11:40
  • Topic 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 - 12:00
  • Wrap-up and conclude

Participants

The workshop brought together 58 scientists from universities, federal and state agencies, national laboratories, and industry representing a broad range of expertise in fault creep observations, geodesy, remote sensing, laboratory rock mechanics, earthquake physics, seismic hazard, and numerical modeling. Participants included researchers working with long-term alignment arrays, creepmeters, GNSS, InSAR, lidar, photogrammetry, coda wave interferometry, and other emerging techniques for monitoring active fault deformation. The workshop also welcomed graduate students, postdoctoral researchers, early-career scientists, and established investigators, fostering collaboration across career stages and scientific disciplines.

* Remote Participant

Last NameFirst NameOrganization
AgbayaniEvanUniversity of California Berkeley
AlongiTravisUSGS Earthquake Science Center
AntoineSoleneCaltech
BadenCurtisUSGS
* BarbourAndrewUSGS Earthquake Science Center
BilhamRogerUniversity of Colorado
BlisniukKimberlySJSU
BotellBrittanyUniversity of Memphis
BrodskyEmilyUCSC
BurgmannRolandUC Berkeley
CardiffDylan
CastanedaKarenSan Jose State University
ContrerasNormaUniversity of California, Riverside
CrumeHeatherMoody's
DeLongStephenUSGS
ElbannaAhmedUSC/SCEC
* ElliottAustinU.S. Geological Survey
EricksenToddUSGS
FieldingEricJet Propulsion Laboratory, Caltech
FloydMichaelMassachusetts Institute of Technology
FunningGarethUniversity of California, Riverside
GivlerRobertLettis Consultants International, Inc.
GunsKatherineUSGS
HanaganCatherine (Cassie)USGS Earthquake Science Center
HarrisRuthUSGS
* HoughSusanU.S. Geological Survey
HearnLizUSGS
* JohnsonKajIndiana University
JiangJunleThe University of Oklahoma
* LindsayDanielleGNS Science
* LozosJulianCalifornia State University, Northridge
JonesAngelikaSan José State University
LeeJaeseokBrown University
LuckieThomasSandia National Labs
MaddenBetsySan José State University
MadugoChristopherPG&E
MadugoDanielleCalifornia Geological Survey (CGS)
MartinHannahNevada Seismological Laboratory, UNR
* MaternaKathyrnUC Boulder
MendozaMattU.S. Bureau of Reclamation
MilaniRezageneUSGS & San Jose State University
* MillinerChrisCaltech
* MinsonSarahUSGS
MurrayJessicaUSGS Earthquake Science Center
NevittJosieUSGS
PhilibosianBelleUSGS Earthquake Science Center
PollitzFredUSGS
PrushVeronicaNew Mexico Institute of Mining and Technology
RosaCarlaCalifornia Geological Survey (CGS)
RoweChristieNevada Seismological Laboratory
SavageHeatherUCSC
ScottChelseaArizona State University
SloatCateSan Jose State University
SoneHirokiUniversity of Wisconsin-Madison
TairaTaka'akiUniversity of California, Berkeley
VermeerJessieUSGS
WalshAshleySan Jose State University
* YoonClaraUSGS

Registration and Travel Support

Workshop participation was limited to approximately 50 participants to foster active discussion and collaboration among researchers representing academia, government, and industry with expertise in fault creep observations, monitoring technologies, geodesy, earthquake physics, and seismic hazard.

The workshop registration fee was $150, which covered meals during the workshop and transportation and meals for the included March 4 field trip. Participants were responsible for transportation to and from San José, parking, and meals not included in the workshop program.

Travel support was available to help offset registration, lodging, and travel expenses associated with attending the workshop. Lodging was arranged for supported out-of-town participants at the Signia Hotel adjacent to San José State University. Students, early-career researchers, and participants without institutional funding were especially encouraged to request support as part of the application process. SCEC provided travel support to 28 workshop participants.

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The Statewide California Earthquake Center (SCEC) fosters a diverse and inclusive community where everyone feels safe, productive, and welcome. We expect all participants in SCEC-supported events to uphold this commitment by adhering to the SCEC Activities Code of Conduct.

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