(2025) The Needles, Canyonlands, UT
My current research (advised by Dr. Eric Lindsey) focuses on understanding interseismic deformation using geodetic observations (e.g., InSAR and GNSS) and models. I'm also working to expand my research on the initiation and characterization of mass wasting (e.g., debris flows and landslides) primarily in the southwestern US, using models and remote and field observations.
For my master's research (advised by Dr. Eileen Evans), I worked on understanding the crustal deformation caused by plate motion in the Pacific Northwest using computational modeling called block models. For my undergraduate research, I analyzed the coseismic deformation of the 2018 Papua New Guinea earthquake using the sub-pixel offset method (advised by Dr. Mong-Han Huang).
My work led me to explore several geodetic and remote sensing techniques, such as block modeling, Interferometric Synthetic Aperture Radar (InSAR), and Synthetic Aperture Radar pixel tracking (sub-pixel offset). I'm also interested in applying techniques such as lidar, optical imagery analysis, and SfM photogrammetry to study localized geomorphological changes. I've worked on several regions, including the Pacific Northwest (US), Southern California, Southeast Asia (e.g., Borneo, Myanmar), and Papua New Guinea.
Additionally, I enjoy making 3D-printed topographic profiles and other geology-related models for educational purposes (introductory geology classes). These 3D models, along with illustrations, help students visualize topographic maps, cross-section profiles, and structural geology.
Feel free to contact me for more information or posters for the projects!
Advised by Eric Lindsey
Collaborators: Bar Oryan, Lin Shen, Michael Steckler
The Rakhine-Bangladesh megathrust is overlaid by km-deep sediments allowing us to characterize the shallow properties of the megathrust on land. Here, we processed the ALOS-2 InSAR time-series and identified regional scale structures that could affect the seismic potential in the region.
This research is funded by NASA FINESST 2022.
Published Paper
Chong, J.‐H., Oryan, B., Shen, L., Steckler,M. S., & Lindsey, E. O. (2025).Interseismic uplift of anticlines above the Rakhine‐Bangladesh megathrust from ALOS‐2 InSAR. Journal of Geophysical Research: Solid Earth, 130,e2024JB030003. https://doi.org/10.1029/2024JB030003
Advised by Eric Lindsey
This research is funded by NASA FINESST 2022.
In prep
Advised by Eric Lindsey
The dense GNSS network in the Pacific Northwest provides a unique opportunity to study the late interseismic phase of subduction since the 1700 earthquake. The GNSS observations show a broad regional subsidence along the Cascade volcanic arc even after correcting for non-tectonic processes, including hydrology and glacial isostatic adjustment. We construct a viscoelastic model of the subduction to understand the source of this broad subsidence better and examine the influence of geometry, plate thickness, deep slip on the megathrust, and a potential low-viscosity mantle wedge. Preliminary tests show that plate geometry has a greater influence on the surface displacement as compared to mantle viscosity.
This research is funded by NASA FINESST 2022.
In prep
Advised by Eileen L. Evans
The Cascadia subduction zone is an oblique subduction zone capable of producing megathrust earthquakes (e.g., the 1700 Cascadia earthquake). This study aims to better understand how oblique Juan de Fuca-North America convergence is partitioned between surface faults in the Pacific Northwest region and the subduction zone using block models.
In revision
Presentations
SSA 2021 presentation - (link)
Advised by Mong-Han Huang
The 2018 Mw7.5 earthquake was the largest earthquake recorded in the Papua New Guinea Highlands. We were able to resolve near-field deformation using the sub-pixel offset of Sentinel-1 SAR images. Our results show up to 2 meters of uplift and 4 meters of horizontal displacement as well as triggered landslides. We propose that the earthquake ruptured two separate faults of different geometries and it is possible that it involved a detachment fault.
This is a continuation of my undergraduate research on the same topic advised by Mong-Han Huang.
Published paper
Chong, J.-H., and M.-H. Huang (2020). Refining the 2018 Mw 7.5 Papua New Guinea Earthquake Fault-Slip Model Using Subpixel Offset, Bull. Seismol. Soc. Am. 111(2), 1032–1042, doi: 10.1785/0120200250
Advised by: Scott Hauswirth, Louis Scuderi, Eric Lindsey
Collaborators: Adit Ghosh, Brandon Page, Gregory Jesmok, Denise V. Berg, Marlene Lopez, Deepshika Upadhyay, David Stone,
We show in this research a post-fire debris flow analysis for the 2020 Lake Fire in Southern California, USA, over the span of four years. Specifically, we used high-resolution satellite imagery and field surveys (during the first and fourth years) to inform our simulations. Post-fire debris flow likelihood is still elevated in the fourth year, but can vary depending on the season. We found that hydraulic conductivity exerts the greatest control for debris flow initiation, whereby drier months significantly increase the hydraulic conductivity, reducing the likelihood of debris flows. This finding adds to the already very little literature on the influence of seasonality in the long-term analysis of post-fire debris flows.
I'm also interested in applying this method to fires affected by monsoons (e.g., Hermits Peak/Calf Canyon in New Mexico).
In review
Collaborators: Adit Ghosh and Scott Hauswirth
This project started as a hydrogeology class project inspired by the question "How can we estimate the river sediment discharge of a river with limited access for sample collection?". In this study, we propose a method to estimate the river properties along a river (water stage, velocity, discharge, sediment discharge, etc) with limited gauging stations by using only freely available Digital Elevation Models (DEM) and software.
Presentations
AEG 2020 poster presentation of this project (click here) & poster only (click here)
Analyzing seismic hazards of low strain rate faults:
Evaluating fault activity at the North-west Borneo Trough (and in Borneo)
Interseismic fault slip rates of Papua New Guinea & Rio Grande Rift using block models
Characterizing creeping landslides in the Santa Monica Mountains
Constraining multiyear post-fire debris flow initiation using remote observations
Normal faulting in the Basin and Range & Rio Grande Rift
Understanding low angle normal faults slip behavior