Meteorites & Asteroids

Orbit, Meteoroid Size, And Cosmic Ray Exposure History Of The Aguas Zarcas CM2 Breccia

By Keith Cowing
Status Report
astro-ph.EP
April 2, 2025
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Orbit, Meteoroid Size, And Cosmic Ray Exposure History Of The Aguas Zarcas CM2 Breccia
Example of alt-azimuth grid overlay on the Heredia dashboard camera video. Perspective lines on the road define the position of the horizon, and the orientation of a lamp post in different video frames (white lines left, slightly bend halfway up) and features on buildings (right) defines the rotation to normal. The flare elevation (assuming an altitude of 25.1 km) defines the scale. In this case, the camera’s central azimuth changed over time and the meteor path in the central frame shown was adjusted using the meteor wake as guidance. — astro-ph.EP

The Aguas Zarcas (Costa Rica) CM2 carbonaceous chondrite fell during night time in April 2019. Security and dashboard camera video of the meteor were analyzed to provide a trajectory, lightcurve, and orbit of the meteoroid.

The trajectory was near vertical, 81° steep, arriving from an ~109° (WNW) direction with apparent entry speed of 14.6 +/- 0.6 km/s. The meteoroid penetrated to ~25 km altitude (5 MPa dynamic pressure), where the surviving mass shattered, producing a flare that was detected by the Geostationary Lightning Mappers on GOES-16 and GOES-17.

The cosmogenic radionuclides were analyzed in three recovered meteorites by either gamma-ray spectroscopy or accelerator mass spectrometry (AMS), while noble gas concentrations and isotopic compositions were measured in the same fragment that was analyzed by AMS.

Aguas Zarcas meteorite. This 146.2 g stone shows irregular surface features from ablation
without the relatively flat surfaces that result from secondary fragmentation. — astro-ph.EP

From this, the pre-atmospheric size of the meteoroid and its cosmic-ray exposure age were determined. The studied samples came from a few cm up to 30 cm deep in an object with an original diameter of ~60 cm, that was ejected from its parent body 2.0 +/- 0.2 Ma ago. The ejected material had an argon retention age of 2.9 Ga.

The object was delivered most likely by the 3:1 or 5:2 mean motion resonances and, without subsequent fragmentation, approached Earth from a low i < 2.8° inclined orbit with perihelion distance q = 0.98 AU close to Earth orbit.

The steep entry trajectory and high strength resulted in deep penetration in the atmosphere and a relatively large fraction of surviving mass.

Peter Jenniskens, Gerardo J. Soto, Gabriel Goncalves Silva, Oscar Lücke, Pilar Madrigal, Tatiana Ballestero, Carolina Salas Matamoros, Paulo Ruiz Cubillo, Daniela Cardozo Mourao, Othon Cabo Winter, Rafael Sfair, Clemens E. Tillier, Jim Albers, Laurence A. J. Garvie, Karen Ziegler, Qing-zhu Yin, Matthew E. Sanborn, Henner Busemann, My E. I. Riebe, Kees C. Welten, Marc W. Caffee, Matthias Laubenstein, Darrel K. Robertson, And David Nesvorny

Comments: 26 pages, 13 figures
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:2504.00183 [astro-ph.EP](or arXiv:2504.00183v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2504.00183
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Journal reference: Meteoritics & Planetary Science 60 (2025)
Related DOI:
https://doi.org/10.1111/maps.14337
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Submission history
From: Peter Jenniskens
[v1] Mon, 31 Mar 2025 19:45:12 UTC (18,956 KB)
https://arxiv.org/abs/2504.00183
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