Kiladze Caldera: A Possible Cryovolcano on Pluto

Fuente: arXiv
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Autori principali: Emran, A., Cruikshank, D. P., Ahrens, C. J., Moore, J. M., White, O. L.
Natura: Preprint
Pubblicazione: 2023
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author Emran, A.
Cruikshank, D. P.
Ahrens, C. J.
Moore, J. M.
White, O. L.
author_facet Emran, A.
Cruikshank, D. P.
Ahrens, C. J.
Moore, J. M.
White, O. L.
contents In contrast with regional primarily methane composition, Kiladze and its surroundings exhibit a water-ice spectral signature that carries an ammoniated compound, similar to two other cryovolcanic sites on Pluto. The faulted structure of Kiladze, including shaping by numerous collapse pits and the distortion of the shape of the depression, are compatible with the surroundings in Hayabusa Terra, east of Sputnik Planitia. They are further compatible with an interpretation as a caldera formed during an era of an active cryovolcanic period that appears to be significantly more recent than the overall age of the planet's surface, possibly in the last several million years. In view of the size of the caldera and the large scale of the surrounding distribution of water ice, we suggest that Kiladze may have been a cryovolcano, in which one or more explosive events may have erupted $\sim$1000 km$_{3}$ of icy cryomagma onto the surface.
format Preprint
id arxiv_https___arxiv_org_abs_2310_10904
institution arXiv
publishDate 2023
record_format arxiv
spellingShingle Kiladze Caldera: A Possible Cryovolcano on Pluto
Emran, A.
Cruikshank, D. P.
Ahrens, C. J.
Moore, J. M.
White, O. L.
Earth and Planetary Astrophysics
In contrast with regional primarily methane composition, Kiladze and its surroundings exhibit a water-ice spectral signature that carries an ammoniated compound, similar to two other cryovolcanic sites on Pluto. The faulted structure of Kiladze, including shaping by numerous collapse pits and the distortion of the shape of the depression, are compatible with the surroundings in Hayabusa Terra, east of Sputnik Planitia. They are further compatible with an interpretation as a caldera formed during an era of an active cryovolcanic period that appears to be significantly more recent than the overall age of the planet's surface, possibly in the last several million years. In view of the size of the caldera and the large scale of the surrounding distribution of water ice, we suggest that Kiladze may have been a cryovolcano, in which one or more explosive events may have erupted $\sim$1000 km$_{3}$ of icy cryomagma onto the surface.
title Kiladze Caldera: A Possible Cryovolcano on Pluto
topic Earth and Planetary Astrophysics
url https://arxiv.org/abs/2310.10904