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.

Department(s)

Geosciences and Geological and Petroleum Engineering

Publication Status

Open Access

Comments

U.S. Geological Survey, Grant OISE-2153715

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

Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.

Publication Date

01 Dec 2026

Available for download on Tuesday, December 01, 2026

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