Papers by Antonio Jesús Talavera Montes
Las Islas Baleares en la Antigüedad Tardía (ss. III-X). Ed. M.A. Cau Ontiveros, 2024
Journal of Maritime Archaeology, 2023
Las Islas Baleares durante la Antigüedad Tardía (ss. III-X). Ed. M.A. Cau Ontiveros, 2024
V jornades d'Arqueologia de les Illes Balears: Palma, 28 a 30 de setembre, 2012, 2013, ISBN 978-84-154327-6-0, págs. 119-126, 2013
Study of amphorae from underwater survey work in the Roman port of Sanitja. The amphorae of Tunis... more Study of amphorae from underwater survey work in the Roman port of Sanitja. The amphorae of Tunisian origin and their pottery marks are studied in detail. CONTRERAS, F., TALAVERA, A., MASSÓ, P.: “Estudio de las ánforas de la Africa Bizacena localizadas en el fondo subacuático del puerto de Sanitja (Menorca)”, V Jornades d’arqueologia de les Illes Balears, Consell de Mallorca, Ed. Documenta Balear, 2013, pp. 119 – 126.
Living with Seismic Phenomena in the Mediterranean and Beyond between Antiquity and the Middle Ages Proceedings of Cascia (2019) and Le Mans (2021) Conferences, 2022
Riassunto
Il paesaggio dei Campi Flegrei nel Golfo di Pozzuoli da sempre è condizionato da una pa... more Riassunto
Il paesaggio dei Campi Flegrei nel Golfo di Pozzuoli da sempre è condizionato da una particolare attività vulcanica e sismica,
che rappresenta dunque una costante nella vita dei suoi abitanti. Questo contributo vuole approfondire in particolare quanto è
avvenuto tra il II secolo a.C. e il V secolo d.C., quando il bradisismo modificò profondamente la geografia di questo territorio. Il
bradisismo è il costante, silenzioso e lento movimento di parte della crosta terrestre, sia ascendente che discendente, provocato
dai livelli di pressione della attività vulcanica in profondità. Un’alta pressione può sollevare terreni duri e deformare suoli più
flessibili. La mancanza di pressione provoca invece il bradisismo discendente. Il suo movimento è sempre impercettibile e e può
variare da 1 a 60 cm all’anno.
Abstract
The landscape of the Phlegrean Fields in the Gulf of Pozzuoli has always been linked to a certain volcanic and seismic activity,
tectonic phenomena which constitute a constant in the life of their inhabitants. This contribution seeks to delve more deeply
into what happened between the 2nd century BC and the 5th century AD, when bradyseism profoundly changed the geography of
this territory. Bradyseism is the constant, silent and slow movement of part of the earth´s crust, both ascending and descending,
caused by the pressure levels of volcanic activity at great depths. High pressure can lift hard soils and deform more flexible soils.
Lack of pressure, on the other hand, causes descending bradyseism. Its movement is always imperceptible and we know, thanks
to the data collected in the past century, that it can vary from 1 to 60cm per year.
Convengo internazionale. Convivere con i fenomeni sismici nel Mediterraneo Antico. Cascia, Italia., 2019
Vivere con un sisma impercettibile: i Campi Flegrei tra periodo tardo-repubblicano ed età imperia... more Vivere con un sisma impercettibile: i Campi Flegrei tra periodo tardo-repubblicano ed età imperiale. 5 km N LAGO FUSARO LAGO AVERNO M. NUOVO 5 km N LAGO FUSARO LAGO AVERNO M. NUOVO ASTRONI GAURO NISIDA
Ambit 32, 2014
In the north of Menorca, very close to the Cap de Cavallería, is the ancient Roman city of Sanise... more In the north of Menorca, very close to the Cap de Cavallería, is the ancient Roman city of Sanisera located in the natural port of Sanitja that was abandoned in the early 9th century. In more modern times, this natural site was strategic at the military level and due to this, the remains of an English defense tower-martello tower-and defense parapets of the Spanish civil war are preserved. Also during more recent times, the port of Sanitja was a base for the fishing of tuna in a very short time lapse. As a testimony of this purpose, a small low-rise house is conserved, equipped with a cistern and various annexed structures, currently known as s'Almadrava. We can see it at the mouth of the port. It was built in 1787 and according to chronicles, it was the first fishing industry in Menorca. This publication aims to present a unique and surprising discovery in Menorca related to traditional coral fishing that is sufficiently documented in the most recent Balearic Islands. The piece was discovered in the course of underwater archaeological prospecting activities during 2011 and which are still in force today, led by the Sanitja archaeological association.
http://www.cime.es/WebEditor/Pagines/file/Ambit/Gener2014/8Sanitja.pdf
Resumen: A partir de un programa efectuado en varias campañas anuales consecutivas desde 2007 dir... more Resumen: A partir de un programa efectuado en varias campañas anuales consecutivas desde 2007 dirigido por la Asociación Sanitja sobre prospección subacuática, se presenta un estudio del conjunto de unos restos arqueológicos descubiertos en el fondo marino de la costa norteña de Menorca que colinda con el puerto de Sanitja y que pertenecen a dos embarcaciones púnicas hundidas en el siglo IV a.C. Para ello hemos analizado el repertorio anfórico con la intención de dar un paso más en el conocimiento que hace referencia a las rutas de navegación comerciales de estas embarcaciones durante el periodo postalayóico.
Abstract: From a program carried out in several consecutive annual campaigns since 2007 conduct by Sanitja Association about underwater exploration, we present a study of a group of archaeological remains discovered in the seabed of the northern coast of Menorca adjacent to the port of Sanitja and belonging to two Punic ships sunk in the fourth century B.C. So we've analyzed the amphorae repertoire with the intent to take another step in the knowledge that refers to the routes of commercial navigation of those vessels during the posttalayotic period.
El puerto de Sanitja y la pesca de coral en el siglo XVIII Talavera, A.J.; Contreras, F.; Massó, P.
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Papers by Antonio Jesús Talavera Montes
Il paesaggio dei Campi Flegrei nel Golfo di Pozzuoli da sempre è condizionato da una particolare attività vulcanica e sismica,
che rappresenta dunque una costante nella vita dei suoi abitanti. Questo contributo vuole approfondire in particolare quanto è
avvenuto tra il II secolo a.C. e il V secolo d.C., quando il bradisismo modificò profondamente la geografia di questo territorio. Il
bradisismo è il costante, silenzioso e lento movimento di parte della crosta terrestre, sia ascendente che discendente, provocato
dai livelli di pressione della attività vulcanica in profondità. Un’alta pressione può sollevare terreni duri e deformare suoli più
flessibili. La mancanza di pressione provoca invece il bradisismo discendente. Il suo movimento è sempre impercettibile e e può
variare da 1 a 60 cm all’anno.
Abstract
The landscape of the Phlegrean Fields in the Gulf of Pozzuoli has always been linked to a certain volcanic and seismic activity,
tectonic phenomena which constitute a constant in the life of their inhabitants. This contribution seeks to delve more deeply
into what happened between the 2nd century BC and the 5th century AD, when bradyseism profoundly changed the geography of
this territory. Bradyseism is the constant, silent and slow movement of part of the earth´s crust, both ascending and descending,
caused by the pressure levels of volcanic activity at great depths. High pressure can lift hard soils and deform more flexible soils.
Lack of pressure, on the other hand, causes descending bradyseism. Its movement is always imperceptible and we know, thanks
to the data collected in the past century, that it can vary from 1 to 60cm per year.
http://www.cime.es/WebEditor/Pagines/file/Ambit/Gener2014/8Sanitja.pdf
Abstract: From a program carried out in several consecutive annual campaigns since 2007 conduct by Sanitja Association about underwater exploration, we present a study of a group of archaeological remains discovered in the seabed of the northern coast of Menorca adjacent to the port of Sanitja and belonging to two Punic ships sunk in the fourth century B.C. So we've analyzed the amphorae repertoire with the intent to take another step in the knowledge that refers to the routes of commercial navigation of those vessels during the posttalayotic period.
Il paesaggio dei Campi Flegrei nel Golfo di Pozzuoli da sempre è condizionato da una particolare attività vulcanica e sismica,
che rappresenta dunque una costante nella vita dei suoi abitanti. Questo contributo vuole approfondire in particolare quanto è
avvenuto tra il II secolo a.C. e il V secolo d.C., quando il bradisismo modificò profondamente la geografia di questo territorio. Il
bradisismo è il costante, silenzioso e lento movimento di parte della crosta terrestre, sia ascendente che discendente, provocato
dai livelli di pressione della attività vulcanica in profondità. Un’alta pressione può sollevare terreni duri e deformare suoli più
flessibili. La mancanza di pressione provoca invece il bradisismo discendente. Il suo movimento è sempre impercettibile e e può
variare da 1 a 60 cm all’anno.
Abstract
The landscape of the Phlegrean Fields in the Gulf of Pozzuoli has always been linked to a certain volcanic and seismic activity,
tectonic phenomena which constitute a constant in the life of their inhabitants. This contribution seeks to delve more deeply
into what happened between the 2nd century BC and the 5th century AD, when bradyseism profoundly changed the geography of
this territory. Bradyseism is the constant, silent and slow movement of part of the earth´s crust, both ascending and descending,
caused by the pressure levels of volcanic activity at great depths. High pressure can lift hard soils and deform more flexible soils.
Lack of pressure, on the other hand, causes descending bradyseism. Its movement is always imperceptible and we know, thanks
to the data collected in the past century, that it can vary from 1 to 60cm per year.
http://www.cime.es/WebEditor/Pagines/file/Ambit/Gener2014/8Sanitja.pdf
Abstract: From a program carried out in several consecutive annual campaigns since 2007 conduct by Sanitja Association about underwater exploration, we present a study of a group of archaeological remains discovered in the seabed of the northern coast of Menorca adjacent to the port of Sanitja and belonging to two Punic ships sunk in the fourth century B.C. So we've analyzed the amphorae repertoire with the intent to take another step in the knowledge that refers to the routes of commercial navigation of those vessels during the posttalayotic period.