Excursion guide for field trip V2 : ‘Island of Terceira’

Bibliographic Details
Main Author: Self, Stephen
Publication Date: 1982
Format: Article
Language: eng
Source: Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
Download full: http://hdl.handle.net/10400.3/4884
Summary: The island of Terceira is 406 km2 in area and rises to 1021 metres above sea level. It consists of four strato-volcanoes grouped along a prominent fissure zone (Fig. 1). Two volcanoes, Pico Alto and Santa Barbara, are active and the other two, Guilherme Moniz and Cinquo Picos, are believed to be extinct. The fissure zone may be the sub-aerial expression of the Terceira Rift, regarded by Krause and Watkins (1970) as a secondary spreading centre. Terceira shows a great diversity of lavas and pyroclastics for an oceanic island and is noteworthy for voluminous production of peralkaline salic magma. Of the four volcanoes forming the island ; three are composed of both basic and salic rocks and one has only salic rocks exposed. Since the emergence of the island a compositionally bimodal population of rocks has been represented. The products of over 100 eruptions in the upper Terceira Group have been recognized. These include ignimbrites, pumice fall deposits, salic lava extrusions, strombolian scoria deposits, basaltic lava flows and littoral (surtseyan) basaltic tuffs. Basaltic activity is concentrated along the fissure zone which bisects the island diagonally from NW to SE. Volumetric studies give the rate of accumulation of new crust along this small spreading centre; 5.46 km3 of new material has been erupted on the island in the past 23,000 years, of which over 4 km3 is comendite pantellerite composition. The island's economy is dominated by agriculture and dairy farming. Much of the water for the maintown of Angra do Heroísmo (approximately 20,000 population) comes from underground springs or streams in the lava tubes of a 2000-year-ald basalt in Guilherme Moniz Caldera. The island has a good system of roads. Almost the entire papulation lives around a 5 km wide coastal strip (Fig. 2).
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spelling Excursion guide for field trip V2 : ‘Island of Terceira’VolcanismTerceira Island (Azores)Azores ArchipelagoThe island of Terceira is 406 km2 in area and rises to 1021 metres above sea level. It consists of four strato-volcanoes grouped along a prominent fissure zone (Fig. 1). Two volcanoes, Pico Alto and Santa Barbara, are active and the other two, Guilherme Moniz and Cinquo Picos, are believed to be extinct. The fissure zone may be the sub-aerial expression of the Terceira Rift, regarded by Krause and Watkins (1970) as a secondary spreading centre. Terceira shows a great diversity of lavas and pyroclastics for an oceanic island and is noteworthy for voluminous production of peralkaline salic magma. Of the four volcanoes forming the island ; three are composed of both basic and salic rocks and one has only salic rocks exposed. Since the emergence of the island a compositionally bimodal population of rocks has been represented. The products of over 100 eruptions in the upper Terceira Group have been recognized. These include ignimbrites, pumice fall deposits, salic lava extrusions, strombolian scoria deposits, basaltic lava flows and littoral (surtseyan) basaltic tuffs. Basaltic activity is concentrated along the fissure zone which bisects the island diagonally from NW to SE. Volumetric studies give the rate of accumulation of new crust along this small spreading centre; 5.46 km3 of new material has been erupted on the island in the past 23,000 years, of which over 4 km3 is comendite pantellerite composition. The island's economy is dominated by agriculture and dairy farming. Much of the water for the maintown of Angra do Heroísmo (approximately 20,000 population) comes from underground springs or streams in the lava tubes of a 2000-year-ald basalt in Guilherme Moniz Caldera. The island has a good system of roads. Almost the entire papulation lives around a 5 km wide coastal strip (Fig. 2).Universidade dos AçoresRepositório da Universidade dos AçoresSelf, Stephen2018-11-27T14:22:11Z1982-071982-07-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10400.3/4884enginfo:eu-repo/semantics/openAccessreponame:Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiainstacron:RCAAP2025-03-07T10:05:40Zoai:repositorio.uac.pt:10400.3/4884Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireinfo@rcaap.ptopendoar:https://opendoar.ac.uk/repository/71602025-05-29T00:36:03.831616Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) - FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiafalse
dc.title.none.fl_str_mv Excursion guide for field trip V2 : ‘Island of Terceira’
title Excursion guide for field trip V2 : ‘Island of Terceira’
spellingShingle Excursion guide for field trip V2 : ‘Island of Terceira’
Self, Stephen
Volcanism
Terceira Island (Azores)
Azores Archipelago
title_short Excursion guide for field trip V2 : ‘Island of Terceira’
title_full Excursion guide for field trip V2 : ‘Island of Terceira’
title_fullStr Excursion guide for field trip V2 : ‘Island of Terceira’
title_full_unstemmed Excursion guide for field trip V2 : ‘Island of Terceira’
title_sort Excursion guide for field trip V2 : ‘Island of Terceira’
author Self, Stephen
author_facet Self, Stephen
author_role author
dc.contributor.none.fl_str_mv Repositório da Universidade dos Açores
dc.contributor.author.fl_str_mv Self, Stephen
dc.subject.por.fl_str_mv Volcanism
Terceira Island (Azores)
Azores Archipelago
topic Volcanism
Terceira Island (Azores)
Azores Archipelago
description The island of Terceira is 406 km2 in area and rises to 1021 metres above sea level. It consists of four strato-volcanoes grouped along a prominent fissure zone (Fig. 1). Two volcanoes, Pico Alto and Santa Barbara, are active and the other two, Guilherme Moniz and Cinquo Picos, are believed to be extinct. The fissure zone may be the sub-aerial expression of the Terceira Rift, regarded by Krause and Watkins (1970) as a secondary spreading centre. Terceira shows a great diversity of lavas and pyroclastics for an oceanic island and is noteworthy for voluminous production of peralkaline salic magma. Of the four volcanoes forming the island ; three are composed of both basic and salic rocks and one has only salic rocks exposed. Since the emergence of the island a compositionally bimodal population of rocks has been represented. The products of over 100 eruptions in the upper Terceira Group have been recognized. These include ignimbrites, pumice fall deposits, salic lava extrusions, strombolian scoria deposits, basaltic lava flows and littoral (surtseyan) basaltic tuffs. Basaltic activity is concentrated along the fissure zone which bisects the island diagonally from NW to SE. Volumetric studies give the rate of accumulation of new crust along this small spreading centre; 5.46 km3 of new material has been erupted on the island in the past 23,000 years, of which over 4 km3 is comendite pantellerite composition. The island's economy is dominated by agriculture and dairy farming. Much of the water for the maintown of Angra do Heroísmo (approximately 20,000 population) comes from underground springs or streams in the lava tubes of a 2000-year-ald basalt in Guilherme Moniz Caldera. The island has a good system of roads. Almost the entire papulation lives around a 5 km wide coastal strip (Fig. 2).
publishDate 1982
dc.date.none.fl_str_mv 1982-07
1982-07-01T00:00:00Z
2018-11-27T14:22:11Z
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dc.identifier.uri.fl_str_mv http://hdl.handle.net/10400.3/4884
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dc.publisher.none.fl_str_mv Universidade dos Açores
publisher.none.fl_str_mv Universidade dos Açores
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instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologia
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