The San Andreas fault is nearly vertical
Is it true that the San Andreas fault is nearly vertical?
Yes. Geophysical studies including seismic imaging, magnetotelluric sounding, and gravity modeling demonstrate that segments of the San Andreas Fault are indeed nearly vertical or steeply dipping in the upper crust.
Verdict: SUPPORTED · 4 sources for, 0 against · Last checked
The retrieved literature consistently supports the claim that the San Andreas fault is nearly vertical or steeply dipping. Papers [0], [3], [9], and [11] all explicitly report geophysical evidence (such as seismic tomography, geodetic and seismic inversions, magnetotelluric imaging, and gravity models) showing that the fault or key sections of it (like the southern San Andreas fault) are vertical to steeply dipping (e.g., 60-80 degrees) in the upper crust. No papers refute the claim, so the verdict is SUPPORTED.
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Barak, S., Klemperer, S., & Lawrence, J. (2015). San Andreas Fault dip, Peninsular Ranges mafic lower crust and partial melt in the Salton Trough, Southern California, from ambient‐noise tomography. doi.org. https://doi.org/10.1002/2015GC005970
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Vavra, E. J., Qiu, H., Chi, B., Share, P., Allam, A., Morzfeld, M., Vernon, F., Ben‐Zion, Y., & Fialko, Y. (2023). Active Dipping Interface of the Southern San Andreas Fault Revealed by Space Geodetic and Seismic Imaging. doi.org. https://doi.org/10.1029/2023JB026811
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Share, P., Peacock, J., Constable, S., Vernon, F., & Wang, S. (2022). Structural properties of the Southern San Andreas fault zone in northern Coachella Valley from magnetotelluric imaging. doi.org. https://doi.org/10.1093/gji/ggac356
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Langenheim, V. & Fuis, G. (2022). Insights into the geometry and evolution of the southern San Andreas fault from geophysical data, southern California. doi.org. https://doi.org/10.1130/ges02378.1
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