207 Honoring the Late Professor Mohamed Abdelsalam: Outstanding Researcher, Generous Colleague, Legendary Mentor, and Ambassador for the Geosciences In Africa
To honor the late Professor Mohamed Abdelsalam, we invite abstracts on research in Africa by those who worked with him and those inspired by his outstanding work in structural geology, tectonics, geophysics, and remote sensing.
Tuesday, 21 October 2025
1:30 PM - 5:30 PM
HBGCC, 217D
Documenting Quaternary Fault Slip using High Resolution Structure-from-Motion (SfM) Photogrammetry Dataset: Insights from the Albertine Rift, East African Rift System
Paper number: 207-13
Program: Technical Sessions
Time: 4:45 PM – 5:00 PM
Authors
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Daniel MongovinThe University of Kansas, Lawrence, KS
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Asenath KwagalakweCalifornia State University Northridge, Northridge, CA
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Albert KabandaNorthwestern University, Evanston, IL
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Emmanuel NjinjuBaylor University, Waco, TX
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Isaac OluwasegunOklahoma State University, Stillwater, OK
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John KiberuMakerere University, Kampala
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Joan NakajigoMakerere University, Kampala
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Fred TugumeMinistry of Energy and Mineral Development, Entebbe
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Michael TaylorThe University of Kansas, LAWRENCE, KS
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D. Sarah StampsVirginia Tech, Blacksburg, VA
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Estella AtekwanaUC Davis, Davis, CA
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Suzan van der LeeNorthwestern University, Earth and Planetary Sciences Tech F379, Evanston, IL
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Rob EvansWoods Hole Oceanographic Institution, Falmouth, MA
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Andrew KatumweheOklahoma State University, Stillwater, OK
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Peter BarryWHOI, Woods Hole, MA
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Liang XueUniversity of California, Davis, Davis, CA
Abstract
The Albertine Rift is a seismically active rift basin of the Western Branch of the East African Rift System (EARS), characterized by moderate-magnitude earthquakes that influence fault slip on rift-bounding normal faults. While the widely available Shuttle Radar Topography Mission (SRTM) provides an invaluable resource for neotectonic studies, the dataset is imprecise for determining accurate offset magnitudes at the meter scale. We therefore utilize high-resolution topographic datasets generated from Structure from Motion (SfM) photogrammetry to document Quaternary fault slip at the Kibiro field site along the North Toro Bunyoro fault, a prominent rift bounding fault in the Albertine Rift. These drone-acquired images were processed to produce high-resolution (18 cm/pixel) topographic products, including a digital elevation model (DEM), hillshade, slope, and relief maps. These products are useful for quantifying accurate offset magnitudes from fault-truncated alluvial fan geomorphic markers. Vertical offset magnitudes of 6.86 ± 0.12 m and 3.92 ± 0.08 m were obtained for the upper and lower fan surfaces, respectively. The processed topographic products are invaluable for identifying piercing points and obtaining accurate offsets from geomorphic markers in regions where high-resolution data is often sparse or absent. Offset magnitudes will be integrated with 10Be depth-profile age constraints from the displaced fan surfaces to obtain a Quaternary fault slip rate. This study is the first SfM photogrammetry analysis along the EARS, providing key insights into Quaternary fault slip rates along the Albertine Rift and a framework for understanding the dynamics of continental breakup in regions with limited high-resolution geospatial data.
Geological Society of America Abstracts with Programs. Vol. 57, No. 6
doi: 10.1130/abs/2025AM-413445
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