Magnetic and seismic reflection study of Lake Cheko, a possible impact crater for the 1908 Tunguska Event

A major explosion occurred on 30 June 1908 in the Tunguska region of Siberia, causing the destruction of over 2,000 square km of taiga; pressure and seismic waves detected as far as 1,000 km away; bright luminescence in the night skies of Northern Europe and Central Asia; and other unusual phenomena...

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Published in:Geochemistry Geophysics Geosystems
Main Authors: Gasperini, L., Cocchi, L., Stanghellini, C., Stanghellini, G., Del Bianco, F., Serrazanetti, M., Carmisciano, C.
Other Authors: Gasperini, L.; CNR-Ismar Bologna, Cocchi, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Stanghellini, C.; INAF-Bologna, Stanghellini, G.; CNR-Ismar Bologna, Del Bianco, F.; CNR-Ismar Bologna, Serrazanetti, M.; CNR-Ismar Bologna, Carmisciano, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, CNR-Ismar Bologna, Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, INAF-Bologna
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2012
Subjects:
Online Access:http://hdl.handle.net/2122/8039
https://doi.org/10.1029/2012GC004054
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spelling ftingv:oai:www.earth-prints.org:2122/8039 2023-05-15T18:30:56+02:00 Magnetic and seismic reflection study of Lake Cheko, a possible impact crater for the 1908 Tunguska Event Gasperini, L. Cocchi, L. Stanghellini, C. Stanghellini, G. Del Bianco, F. Serrazanetti, M. Carmisciano, C. Gasperini, L.; CNR-Ismar Bologna Cocchi, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Stanghellini, C.; INAF-Bologna Stanghellini, G.; CNR-Ismar Bologna Del Bianco, F.; CNR-Ismar Bologna Serrazanetti, M.; CNR-Ismar Bologna Carmisciano, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia CNR-Ismar Bologna Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia INAF-Bologna 2012-05-12 http://hdl.handle.net/2122/8039 https://doi.org/10.1029/2012GC004054 en eng American Geophysical Union Geochemistry Geophysics Geosystem 5/13 (2012) 1525-2027 http://hdl.handle.net/2122/8039 doi:10.1029/2012GC004054 restricted Tunguska Lake Cheko Central Siberia Impact cratering magnetometry seismic reflection 04. Solid Earth::04.02. Exploration geophysics::04.02.06. Seismic methods 04. Solid Earth::04.04. Geology::04.04.04. Marine geology 04. Solid Earth::04.05. Geomagnetism::04.05.04. Magnetic anomalies article 2012 ftingv https://doi.org/10.1029/2012GC004054 2022-07-29T06:06:19Z A major explosion occurred on 30 June 1908 in the Tunguska region of Siberia, causing the destruction of over 2,000 square km of taiga; pressure and seismic waves detected as far as 1,000 km away; bright luminescence in the night skies of Northern Europe and Central Asia; and other unusual phenomena. This “Tunguska Event” is probably related to the impact with the Earth of a cosmic body that exploded about 5-10 km above ground, releasing in the atmosphere 10-15 Mton of energy. Fragments of the impacting body have never been found, and its nature (comet or asteroid) is still a matter of debate. We report here results from a magnetic and seismic-reflection study of a small (~500 m diameter) lake, Lake Cheko, located about 8 km NW of the inferred explosion epicenter, that was proposed to be an impact crater left by a fragment of the Tunguska Cosmic Body. Seismic-reflection and magnetic data revealed a P-wave velocity/magnetic anomaly close to the lake center, about 10 m below the lake floor; this anomaly is compatible with the presence of a buried stony object and supports the impact crater origin for Lake Cheko. Published Q05008 3.4. Geomagnetismo JCR Journal restricted Article in Journal/Newspaper taiga Siberia Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Tunguska ENVELOPE(144.784,144.784,59.388,59.388) Geochemistry Geophysics Geosystems 13
institution Open Polar
collection Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia)
op_collection_id ftingv
language English
topic Tunguska
Lake Cheko
Central Siberia
Impact cratering
magnetometry
seismic reflection
04. Solid Earth::04.02. Exploration geophysics::04.02.06. Seismic methods
04. Solid Earth::04.04. Geology::04.04.04. Marine geology
04. Solid Earth::04.05. Geomagnetism::04.05.04. Magnetic anomalies
spellingShingle Tunguska
Lake Cheko
Central Siberia
Impact cratering
magnetometry
seismic reflection
04. Solid Earth::04.02. Exploration geophysics::04.02.06. Seismic methods
04. Solid Earth::04.04. Geology::04.04.04. Marine geology
04. Solid Earth::04.05. Geomagnetism::04.05.04. Magnetic anomalies
Gasperini, L.
Cocchi, L.
Stanghellini, C.
Stanghellini, G.
Del Bianco, F.
Serrazanetti, M.
Carmisciano, C.
Magnetic and seismic reflection study of Lake Cheko, a possible impact crater for the 1908 Tunguska Event
topic_facet Tunguska
Lake Cheko
Central Siberia
Impact cratering
magnetometry
seismic reflection
04. Solid Earth::04.02. Exploration geophysics::04.02.06. Seismic methods
04. Solid Earth::04.04. Geology::04.04.04. Marine geology
04. Solid Earth::04.05. Geomagnetism::04.05.04. Magnetic anomalies
description A major explosion occurred on 30 June 1908 in the Tunguska region of Siberia, causing the destruction of over 2,000 square km of taiga; pressure and seismic waves detected as far as 1,000 km away; bright luminescence in the night skies of Northern Europe and Central Asia; and other unusual phenomena. This “Tunguska Event” is probably related to the impact with the Earth of a cosmic body that exploded about 5-10 km above ground, releasing in the atmosphere 10-15 Mton of energy. Fragments of the impacting body have never been found, and its nature (comet or asteroid) is still a matter of debate. We report here results from a magnetic and seismic-reflection study of a small (~500 m diameter) lake, Lake Cheko, located about 8 km NW of the inferred explosion epicenter, that was proposed to be an impact crater left by a fragment of the Tunguska Cosmic Body. Seismic-reflection and magnetic data revealed a P-wave velocity/magnetic anomaly close to the lake center, about 10 m below the lake floor; this anomaly is compatible with the presence of a buried stony object and supports the impact crater origin for Lake Cheko. Published Q05008 3.4. Geomagnetismo JCR Journal restricted
author2 Gasperini, L.; CNR-Ismar Bologna
Cocchi, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
Stanghellini, C.; INAF-Bologna
Stanghellini, G.; CNR-Ismar Bologna
Del Bianco, F.; CNR-Ismar Bologna
Serrazanetti, M.; CNR-Ismar Bologna
Carmisciano, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
CNR-Ismar Bologna
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
INAF-Bologna
format Article in Journal/Newspaper
author Gasperini, L.
Cocchi, L.
Stanghellini, C.
Stanghellini, G.
Del Bianco, F.
Serrazanetti, M.
Carmisciano, C.
author_facet Gasperini, L.
Cocchi, L.
Stanghellini, C.
Stanghellini, G.
Del Bianco, F.
Serrazanetti, M.
Carmisciano, C.
author_sort Gasperini, L.
title Magnetic and seismic reflection study of Lake Cheko, a possible impact crater for the 1908 Tunguska Event
title_short Magnetic and seismic reflection study of Lake Cheko, a possible impact crater for the 1908 Tunguska Event
title_full Magnetic and seismic reflection study of Lake Cheko, a possible impact crater for the 1908 Tunguska Event
title_fullStr Magnetic and seismic reflection study of Lake Cheko, a possible impact crater for the 1908 Tunguska Event
title_full_unstemmed Magnetic and seismic reflection study of Lake Cheko, a possible impact crater for the 1908 Tunguska Event
title_sort magnetic and seismic reflection study of lake cheko, a possible impact crater for the 1908 tunguska event
publisher American Geophysical Union
publishDate 2012
url http://hdl.handle.net/2122/8039
https://doi.org/10.1029/2012GC004054
long_lat ENVELOPE(144.784,144.784,59.388,59.388)
geographic Tunguska
geographic_facet Tunguska
genre taiga
Siberia
genre_facet taiga
Siberia
op_relation Geochemistry Geophysics Geosystem
5/13 (2012)
1525-2027
http://hdl.handle.net/2122/8039
doi:10.1029/2012GC004054
op_rights restricted
op_doi https://doi.org/10.1029/2012GC004054
container_title Geochemistry Geophysics Geosystems
container_volume 13
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