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The Active Volcanoes of Kamchatka as Suitable Terrestrial Analogs Within the AVENGERS Initiative: An Opportunity for In-Situ Operational Tests for Future Landing Venus MissionsThe next decade will see the return to Venus thanks to a number of missions which have been recently selected and proposed for launch. The Roscosmos Venera-D mission, along with the NASA DAVINCI, NASA VERITAS, ESA EnVision, the ISRO Shukrayaan-1, and the CNSA VOICE missions will open a new era for the exploration of the Earth’s hellish twin planet.

The next missions to Venus should be able to shed new light on the science questions such as: a) whether the volcanic activity on this planet is locally constrained, or volcanism acts on a global scale, b) the rate of the present-day
volcanic activity, and c) the style of volcanism on Venus, whether it is predominantly effusive, or the occurrence of local episodes of pyroclastic volcanism is also possible. In preparation for the future missions to Venus, the Analogs for VENus’ Geologically Recent Surfaces (AVENGERS) initiative will select and analyze a number of active terrestrial volcanoes as suitable analogs for the identification and analysis of active volcanism on Venus.

Among the future missions to Venus, the Roscosmos Venera-D is the only one to be equipped with a lander which will analyze the elemental and mineralogical composition of the surface. As the young topographic rises (areas characterized by recent volcano-tectonic activity) on Venus are being proposed as one of the possible terrain types for the Venera-D landing, it is crucial to look for volcanic areas on Earth where to perform operational tests such as surface drilling and in-situ elemental composition analysis. To this regard, we propose here the analysis of the active volcanoes of the Kamchatka Peninsula in Russia as a very suitable analog for the Venera-D mission, as well as for the analysis of surface change detection due to ongoing eruptions. The Kamchatka Peninsula is located on the eastern margin of the Eurasia plate, in proximity of the Kuril-Kamchatka subduction zone. The volcanoes of the Kamchatka Peninsula are among the most active volcanoes of the world, making them a suitable terrestrial analog in the search for active volcanism on Venus. Moreover, the volcanoes of Kamchatka are characterized by pyroclastic activity. Since the previous Soviet Venera and Vega missions landed over areas which elemental composition was most likely consistent with that of tholeiitic basalts, performing operational tests over areas characterized by pyroclastic activity also offers the unique opportunity to provide us the tools to potentially interpret the diverse output given by landing over portions of the surface of Venus possibly characterized by explosive volcanic products.
Finally, the frequent eruptions characterizing the volcanoes of the Kamchatka Peninsula make them also a suitable terrestrial analog for the possible detection of ongoing eruptions on Venus by future missions, which can be achieved by comparing two (or more) radar images of the same volcano (and its surroundings) in two (or more) different moments of time.
Document ID
20240010947
Acquisition Source
Johnson Space Center
Document Type
Abstract
Authors
P D'Incecco ORCID
(Collurania Teramo Observatory Teramo, Italy)
J Filiberto ORCID
(Johnson Space Center Houston, United States)
J B Garvin ORCID
(Goddard Space Flight Center Greenbelt, United States)
G N Arney ORCID
(Goddard Space Flight Center Greenbelt, United States)
S A Getty ORCID
(Goddard Space Flight Center Greenbelt, United States)
E Kohler ORCID
(Goddard Space Flight Center Greenbelt, United States)
L M Zelenyi
(Space Research Institute Moscow, Russia)
L V Zasova
(Space Research Institute Moscow, Russia)
O Korablev
(Space Research Institute Moscow, Russia)
M A Ivanov ORCID
(V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry Moscow, Russia)
J W Head ORCID
(Brown University Providence, Rhode Island, United States)
D A Gorinov ORCID
(Space Research Institute Moscow, Russia)
S Bhattacharya
(Indian Space Research Organisation Bengaluru, India)
S S Bhiravarasu
(Indian Space Research Organisation Bengaluru, India)
D Putrevu
(Indian Space Research Organisation Bengaluru, India)
I López ORCID
(King Juan Carlos University Madrid, Spain)
R Ghail ORCID
(Royal Holloway University of London Egham, United Kingdom)
P Mason
(Imperial College London London, United Kingdom)
J Brossier
(Institute for Space Astrophysics and Planetology Rome, Italy)
C Monaco ORCID
(University of Catania Catania, Italy)
S Branca
(INGV Osservatorio Etneo Catania, Italy)
R A Corsaro
(INGV Osservatorio Etneo Catania, Italy)
D Trang ORCID
(University of Hawaiʻi at Mānoa Honolulu, United States)
J R Crandall ORCID
(Eastern Illinois University Charleston, Illinois, United States)
N Mari ORCID
(University of Pavia Pavia, Italy)
M Blackett ORCID
(Coventry University Coventry, United Kingdom)
G Komatsu ORCID
(Università degli Studi "Gabriele d'Annunzio" Pescara, Italy)
A Kosenkova
(Bauman Moscow State Technical University Moscow, Russia)
I Flynn
(University of Pittsburgh Pittsburgh, United States)
S Aveni ORCID
(Sapienza University of Rome Rome, Lazio, Italy)
N Lang
(National Aeronautics and Space Administration Washington, United States)
B Thomson ORCID
(University of Tennessee at Knoxville Knoxville, United States)
I Pagano ORCID
(Osservatorio Astrofisico di Catania Catania, Italy)
S Cassisi
(Collurania Teramo Observatory Teramo, Italy)
G Eggers ORCID
(Wesleyan University Middletown, Connecticut, United States)
R E Ernst ORCID
(Carleton University Ottawa, Ontario, Canada)
H El Bilali
(Carleton University Ottawa, Ontario, Canada)
T Kremic
(Glenn Research Center Cleveland, United States)
J Lustig-Yaeger ORCID
(Johns Hopkins University Applied Physics Laboratory North Laurel, United States)
N Izenberg ORCID
(Johns Hopkins University Applied Physics Laboratory North Laurel, United States)
L Bruzzone
(University of Trento Trento, Italy)
M El Yazidi ORCID
(Università Cattolica del Sacro Cuore Milan, Italy)
E Ferroni
(Collurania Teramo Observatory Teramo, Italy)
D Coero Borga
(National Institute for Astrophysics Rome, Italy)
C Badia
(Collurania Teramo Observatory Teramo, Italy)
S Parisini
(Istituto di Radioastronomia di Bologna Bologna, Italy)
G Fiasconaro
(Istituto di Astrofisica Spaziale e Fisica cosmica di Palermo Palermo, Italy)
S Cussini
(Osservatorio di Astrofisica e Scienza dello Spazio Bologna, Italy)
E Brocato
(Collurania Teramo Observatory Teramo, Italy)
G Di Achille ORCID
(Collurania Teramo Observatory Teramo, Italy)
Date Acquired
August 23, 2024
Publication Date
October 21, 2024
Publication Information
Publisher: Space Research Institute
Subject Category
Lunar and Planetary Science and Exploration
Meeting Information
Meeting: 15th Moscow Solar System Symposium (15M-S3)
Location: Moscow
Country: RU
Start Date: October 21, 2024
End Date: October 25, 2024
Sponsors: Space Research Institute
Funding Number(s)
WBS: 811073
WBS: 748208.04.02.05
Distribution Limits
Public
Copyright
Portions of document may include copyright protected material.
Keywords
Planetary Geology
Venus
Volcanism
Terrestrial Analogs
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