Abstract
In 1976, the Motagua Fault along the North American-Caribbean plate boundary ruptured in a devastating M 7.5 earthquake. Despite its considerable scientific importance and its potential for catastrophic societal impact, very little is known about the seismic history of this major fault. Here, we show direct on-fault paleo seismic evidence for five ground-rupturing earthquakes on the Motagua Fault in the last 1,300 years that led to cultural and architectural adaptations. Radiocarbon ages of fault scarp-derived colluvial wedges, along with damage and repair at Maya and Colonial sites, provide constraints for three earthquakes during the 8th–13th centuries and two during the 18th-20th centuries, separated by a six-century interval of seismic quiescence. The research presented here provides new insight into the seismic character of the Motagua Fault and illustrates that earthquake recurrence on the fault is variable, allowing for improved estimation of current and future seismic risk in Guatemala.
Recommended Citation
T. M. Niemi and C. Grützner and O. Flores Beltetón and L. Alberto Romero and F. Gomez and J. Maurer and T. McEnaney and R. Daniels and A. Dollens and H. Ebell and C. Pérez Arias and A. H. Graettinger and J. Obrist-Farner, "Five Major Earthquakes Since the Late Classic Maya Period on the Motagua Fault in Guatemala," Communications Earth and Environment, vol. 7, no. 1, article no. 277, Nature Research, Dec 2026.
The definitive version is available at https://doi.org/10.1038/s43247-026-03271-y
Department(s)
Geosciences and Geological and Petroleum Engineering
Publication Status
Open Access
International Standard Serial Number (ISSN)
2662-4435
Document Type
Article - Journal
Document Version
Final Version
File Type
text
Language(s)
English
Rights
© 2026 The Authors, All rights reserved.
Creative Commons Licensing

This work is licensed under a Creative Commons Attribution 4.0 License.
Publication Date
01 Dec 2026

Comments
U.S. Geological Survey, Grant OISE-2153715