On 24 September 2023, the Origins, Spectral Interpretation, Resource Identification, and Security‐Regolith Explorer sample return capsule (SRC) entered Earth’s atmosphere after successfully collecting samples from an asteroid. The known trajectory and timing of this return provided a rare opportunity to strategically instrument sites to record geophysical signals produced by the capsule because it travelled at hypersonic speeds through the atmosphere. We deployed two distributed acoustic sensing (DAS) interrogators to sample over 12 km of surface‐draped fiber‐optic cables, as well as six collocated seismometer‐infrasound sensor pairs, spread across two sites near Eureka, Nevada. This campaign‐style rapid deployment is the first reported recording of an SRC re‐entry with any distributed fiber‐optic sensing technology. The DAS interrogators recorded an impulsive arrival with an extended coda which had features that were similar to recordings from both the seismometers and infrasound sensors. While the signal‐to‐noise ratio of the DAS data was lower than the seismic‐infrasound data, the extremely dense spacing of fiber‐optic sensors allowed for more phases to be clearly distinguished and the visualization of the continuous transformation of the wavefront as it impacted the ground. Unexpectedly, the DAS recordings contain less low‐frequency content than is present in both the seismic and infrasound data. The deployment conditions strongly affected the recorded DAS data; in particular, we observed that fiber selection and placement exert strong controls on data quality.

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