Destruction of emergent tuff cones in Faial Island, Azores: influence of tectonics and marine erosion

8th International MAAR CONFERENCE, Kamchatka, 24-30 August 2020 The island of Faial is the westernmost of the central islands of the Azores archipelago (North Atlantic Ocean), and is located east of the Mid-Atlantic Ridge. The Azores are in a unique geodynamic setting at the triple junction of the N...

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Main Authors: Pedrazzi, Dario, Zanon, V., Pimentel, A., Tempera, F.
Format: Conference Object
Language:unknown
Published: 2020
Subjects:
Online Access:http://hdl.handle.net/10261/232506
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author Pedrazzi, Dario
Zanon, V.
Pimentel, A.
Tempera, F.
author_facet Pedrazzi, Dario
Zanon, V.
Pimentel, A.
Tempera, F.
author_sort Pedrazzi, Dario
collection Digital.CSIC (Spanish National Research Council)
description 8th International MAAR CONFERENCE, Kamchatka, 24-30 August 2020 The island of Faial is the westernmost of the central islands of the Azores archipelago (North Atlantic Ocean), and is located east of the Mid-Atlantic Ridge. The Azores are in a unique geodynamic setting at the triple junction of the North-American, Eurasian and Nubia lithospheric plates (Searle, 1980; Madeira and Ribeiro, 1990; Vogt and Jung, 2004) (Fig. 1a) D.P. is grateful for his Juan de la Cierva (IJCI-2016-30482) contract.
format Conference Object
genre Kamchatka
North Atlantic
genre_facet Kamchatka
North Atlantic
geographic Cierva
Mid-Atlantic Ridge
Searle
geographic_facet Cierva
Mid-Atlantic Ridge
Searle
id ftcsic:oai:digital.csic.es:10261/232506
institution Open Polar
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long_lat ENVELOPE(-60.873,-60.873,-64.156,-64.156)
ENVELOPE(-67.237,-67.237,-67.813,-67.813)
op_collection_id ftcsic
op_relation Publisher's version
https://iavcei-cvl.org/2020/01/16/8th-international-maar-conference-kamchatka-24-30-august-2020/

http://hdl.handle.net/10261/232506
op_rights open
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spelling ftcsic:oai:digital.csic.es:10261/232506 2025-01-16T22:48:44+00:00 Destruction of emergent tuff cones in Faial Island, Azores: influence of tectonics and marine erosion Pedrazzi, Dario Zanon, V. Pimentel, A. Tempera, F. 2020-08-24 http://hdl.handle.net/10261/232506 unknown Publisher's version https://iavcei-cvl.org/2020/01/16/8th-international-maar-conference-kamchatka-24-30-august-2020/ Sí http://hdl.handle.net/10261/232506 open tuff cone hydrovolcanism marine geology basaltic magmatism comunicación de congreso http://purl.org/coar/resource_type/c_5794 2020 ftcsic 2024-01-16T11:03:59Z 8th International MAAR CONFERENCE, Kamchatka, 24-30 August 2020 The island of Faial is the westernmost of the central islands of the Azores archipelago (North Atlantic Ocean), and is located east of the Mid-Atlantic Ridge. The Azores are in a unique geodynamic setting at the triple junction of the North-American, Eurasian and Nubia lithospheric plates (Searle, 1980; Madeira and Ribeiro, 1990; Vogt and Jung, 2004) (Fig. 1a) D.P. is grateful for his Juan de la Cierva (IJCI-2016-30482) contract. Conference Object Kamchatka North Atlantic Digital.CSIC (Spanish National Research Council) Cierva ENVELOPE(-60.873,-60.873,-64.156,-64.156) Mid-Atlantic Ridge Searle ENVELOPE(-67.237,-67.237,-67.813,-67.813)
spellingShingle tuff cone
hydrovolcanism
marine geology
basaltic magmatism
Pedrazzi, Dario
Zanon, V.
Pimentel, A.
Tempera, F.
Destruction of emergent tuff cones in Faial Island, Azores: influence of tectonics and marine erosion
title Destruction of emergent tuff cones in Faial Island, Azores: influence of tectonics and marine erosion
title_full Destruction of emergent tuff cones in Faial Island, Azores: influence of tectonics and marine erosion
title_fullStr Destruction of emergent tuff cones in Faial Island, Azores: influence of tectonics and marine erosion
title_full_unstemmed Destruction of emergent tuff cones in Faial Island, Azores: influence of tectonics and marine erosion
title_short Destruction of emergent tuff cones in Faial Island, Azores: influence of tectonics and marine erosion
title_sort destruction of emergent tuff cones in faial island, azores: influence of tectonics and marine erosion
topic tuff cone
hydrovolcanism
marine geology
basaltic magmatism
topic_facet tuff cone
hydrovolcanism
marine geology
basaltic magmatism
url http://hdl.handle.net/10261/232506