Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3906
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dc.contributor.authorallLanza, R.; Dipartimento di Scienze della Terra, Università di Torino, Via Valperga Caluso 35, 10125 Torino, Italyen
dc.contributor.authorallMeloni, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallTema, E.; Dipartimento di Scienze della Terra, Università di Torino, Via Valperga Caluso 35, 10125 Torino, Italyen
dc.date.accessioned2008-06-23T09:10:47Zen
dc.date.available2008-06-23T09:10:47Zen
dc.date.issued2005en
dc.identifier.urihttp://hdl.handle.net/2122/3906en
dc.description.abstractDirect measurements of the Earth’s magnetic field in Italy since 1640 a.d. have been used to check the remanence directions derived from historically dated volcanic rocks of Etna and Vesuvius. Direct measurements consist of the records of L’Aquila and Pola geomagnetic observatories, the repeat stations of the Italian Magnetic Network and the data base of the Historical Italian Geomagnetic Data Catalogue. All have been relocated to the same reference site (Viterbo — lat. 42.45◦N, long. 12.03◦E) in order to draw a reference secular variation (SV) curve. The direction of the Earth’s field at Viterbo has also been calculated from the historical records (2000–1600) of ref. [Jackson, A., Jonkers, A.R.T., Walker, M.R., 2000. Four centuries of geomagnetic secular variation from historical records. Phil. Trans. R. Soc. London, Ser. A 358, 957–990] database. The remanence directions from Etna show a general agreement with the trend of the SV curve, although their inclination is usually lower than that from the direct measurement. The directions from Vesuvius are more scattered. Large discrepancies occur at both volcanoes and in some cases have been ascribed in the literature to poor geographic information, making it difficult to identify the flows actually emplaced during the eruptions reported in the chronicles. Closer examination shows that the great majority of the best-defined remanence directions (semi-angle of confidence α95 < 2.5◦) deviate significantly from the geomagnetic direction measured at the time of the emplacement, the angle between the two directions being larger than the α95 value. The value of 2.5–3.0◦ can thus be regarded as a conservative evaluation of the error when dealing with dating Etna and Vesuvius lava flows older than 17th century, even when the accuracy attained in remanence measurements is higher. In default of a SV curve for Italy derived from archaeological artefacts, a further error in dating is introduced when reference is made to SV curves of other countries, even if well-established, as these are from regions too far from Italy (>600 km) to confidently relocate magnetic directions.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofPhysics of the Earth and Planetary Interiorsen
dc.relation.ispartofseries1 / 148 (2005)en
dc.subjectSecular variationen
dc.subjectHistorical magnetic measurementsen
dc.subjectThermal remanent magnetizationen
dc.subjectVolcanic rocksen
dc.titleHistorical measurements of the Earth’s magnetic field compared with remanence directions from lava flows in Italy over the last four centuriesen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber97-107en
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.04. Magnetic and electrical methodsen
dc.subject.INGV04. Solid Earth::04.05. Geomagnetism::04.05.02. Geomagnetic field variations and reversalsen
dc.subject.INGV04. Solid Earth::04.05. Geomagnetism::04.05.06. Paleomagnetismen
dc.identifier.doi10.1016/j.pepi.2004.08.005en
dc.relation.referencesAlexandrescu, M., Courtillot, V., Le Mou¨el, J.-L., 1997. Highresolution secular variation of the geomagnetic field in western Europe over the last 4 centuries: comparison and integration of historical data from Paris and London. J. Geophys. Res. 102, 20245–20258. Angelino, A., Incoronato, A., 1996. Stratigrafia magnetica in aree vulcaniche; esperienze al Vesuvio e all’Etna. 15◦ Convegno GNGTS, CNR Roma, pp. 13–18. Baag, C., Helsley, C.E., Xu, S.Z., Lienert, B.R., 1995. Deflection of palaeomagnetic directions due to magnetisation of underlying terrain. J. Geophys. Res. 100, 10013–10027. Bucur, I., 1994. The direction of the terrestrial magnetic field in France during the last 21 centuries. Phys. Earth Planet. Int. 87, 95–109. Cafarella, L., De Santis, A., Meloni, A., 1992a. The Historical Italian Geomagnetic Data Catalogue. ING, Rome, p. 160. Cafarella, L., De Santis, A., Meloni, A., 1992b. Secular variation from historical geomagnetic field measurements. Phys. Earth Planet. Inter. 73, 206–221. Carracedo, J.C., Principe, C., Rosi, M., Soler,V., 1993. Time correlation by palaeomagnetism of the 1631 eruption of MountVesuvius Volcanological and volcanic hazard implications. J. Volcanol. Geotherm. Res. 58, 203–209. Chiari, G., Lanza, R., 1999. Remanent magnetization of mural paintings from the Bibliotheca Apostolica (Vatican Rome). J. Appl. Geophys. 41, 137–143. Cioni, R., Gurioli, L., Lanza, R., Zanella, E., 2004. Temperatures of the A.D. 79 pyroclastic density current deposits (Vesuvius Italy). J. Geophys. Res. 109, B02207, doi: 10.1029/2002JB.002251. Coticchia, A., De Santis, A., Di Ponzio, A., Dominici, G., Meloni, A., Pierozzi, M., Sperti, M., 2000. Italian Magnetic Network and Geomagnetic Field Maps of Italy at year 2000. Boll. Geod. Sci. Aff. LX/4, 262–291. De Santis, A., 1992. Conventional spherical harmonic analysis for regional modelling of the geomagnetic field. Geophys. Res. Lett. 19, 1065–1067. Hoye, G.S., 1981. Archaeomagnetic secular variation record of Mount Vesuvius. Nature 291, 216–218. Iliceto, V., Napoleone, G., Pinna, E., 1973. Geomagnetic changes during the cooling process of the Mount Etna 1971 lava flow: preliminary report. Boll. Assoc. Geof. Ital. 22, 89– 94. Incoronato, A., Angelino, A., Romano, R., Ferrante, A., Sauna, R., Vanacore, G., Vecchione, C., 2002. Retrieving geomagnetic secular variations from lava flows: evidence from Mounts Arso, Etna and Vesuvius (southern Italy). Geophys. J. Int. 149, 724– 730. INGV, 2003. Risultati delle osservazioni magnetiche, L’Aquila, 55 pp. Jackson, A., Jonkers, A.R.T., Walker, M.R., 2000. Four centuries of geomagnetic secular variation from historical records. Phil. Trans. R. Soc. London, Ser. A 358, 957–990. Knudsen, M.F., Jacobsen, B.H., Abrahamsen, N., 2003. Paleomagnetic distortion modelling and possible recovery by inversion. Phys. Earth Planet. Inter. 135, 55–73. Lanza, R., Zanella, E., 2003. Paleomagnetic secular variation at Vulcano (Aeolian Islands) during the last 135 kyr. Earth Planet. Sci. Lett. 213, 321–336. Noel, M., Batt, C.M., 1990. A method for correcting geographically separated remanence directions for the purpose of archeomagnetic dating. Geophys. J. Int. 102, 753–756. Principe, C., Tanguy, J.C., Arrighi, S., Paiotti, A., Le Goff, M., Zoppi, U., in press. Chronology of Vesuvius’ activity from A.D. 79 to 1631 based on archeomagnetism of lavas and historical sources. Bull. Volcanol. Rolph, T.C., 1997. An investigation of the magnetic variation within two recent lava flows. Geophys. J. Int. 130, 125–136. Rolph, T.C., Shaw, J., Guest, J.E., 1987. Geomagnetic field variations as a dating tool: application to Sicilian lavas. J. Archaeological Sci. 14, 215–225. Talamo, R., 1975. Le carte magnetiche d’ Italia delle isodinamiche dellaHe delle isogone dell’ Istituto Geografico Militare e loro aggiornamento al. 1973.0. Boll. Geod. Sci. Aff. XXXIV/1, 73–77. Tanguy, J.C., Le Goff, M., Principe, C., Arrighi, S., Chillemi, V., Paiotti, A., La Delfa, S., Patan`e, G., 2003. Archeomagnetic dating of Mediterranean volcanics of the last 2100 years: validity and limits. Earth Planet. Sci. Lett. 211, 111–124. Tanguy, J.C., Le Goff, M., 2004. Distortion of the geomagnetic field in volcanic terrains: an experimental study of the Mount Etna stratovolcano. Phys. Earth Planet. Inter. 141, 59–70. Tarling, D., 1988. Secular variation of the geomagnetic field — the archaeomagnetic record. In: Stephenson, F.R., Wolfendale, A.W. (Eds.), Secular Solar and Geomagnetic Variations in the Last 10,000 years, NATO ASI Series, vol. 236, pp. 349– 366. Thellier, E., 1981. Sur la direction du champ magnetique terrestre, en France, durant les deux derniers millenaires. Phys. Earth Planet. Inter. 13, 89–132. von Kesslitz, W., 1911. Ergebnisse aus den Erdmagnetischen Beobachtungen in Pola (1847–1909). HydrographischenAmtder Kaiserlichen und K¨oniglichen Kriegsmarine, Pola.en
dc.description.obiettivoSpecifico1.6. Osservazioni di geomagnetismoen
dc.description.obiettivoSpecifico2.6. TTC - Laboratorio di gravimetria, magnetismo ed elettromagnetismo in aree attiveen
dc.description.obiettivoSpecifico3.4. Geomagnetismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorLanza, R.en
dc.contributor.authorMeloni, A.en
dc.contributor.authorTema, E.en
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Torino, Via Valperga Caluso 35, 10125 Torino, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Torino, Via Valperga Caluso 35, 10125 Torino, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptALP — Alpine Laboratory of Paleomagnetism, Peveragno, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Torino-
crisitem.author.orcid0000-0003-1155-401X-
crisitem.author.orcid0000-0002-4362-2630-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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