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Figure 3. Air photo of Naples showing the extent of the city walls. The red line shows the approximate extent of Naples during the fifth century B.C.; the blue line
encloses the enlargement of the city during the fourth century A.D.; the green line shows the wall added during the Angevin period; the violet line shows the
extension of the wall during the Aragonese period; the orange line shows the extent of the wall during the Viceroy period (modified from Amato et al., 2009).
GSA TODAY | MAY 2015 sloped terrain frequently wreaked havoc throughout the city. In Bersani, P., and Bencivenga, M., 2001, Le piene del Tevere a Roma dal V secolo
spite of these problems, Naples was always an important port city, a.C. all’anno 2000: Presidenza del Consiglio dei Ministri, Servizio
well connected with Greece and Greek culture. On one hand, this Idrografico e Mareografico Nazionale, 114 p.
was a fortunate situation, but on the other, it caused rapid over-
crowding of a city without the necessary local resources. Urban Butler, R.W.H., Mazzoli, S., Corrado, S., de Donatis, M., Scorcca, D., Di Bucci,
overgrowth and substantial increases in the population were D., Gabini, R., Naso, G., Nicolai, C., Shiner, P., and Zucconi, V., 2004,
always followed by economic crises and the rapid development of Applying thick-skinned tectonic models to the Apennine thrust belt of
epidemics that resulted in decimation of the population at various Italy: Limitations and implications, in McClay, K.R., ed., Thrust Tectonics
points in its history. and Hydrocarbon Systems: AAPG Memoir 82, p. 647–667.
Geological knowledge is therefore essential for the sustainable Calcaterra, D., and Guarino, P.M., 1999, Morphodynamics and recent
development of a city. The fortune of Rome until Republican landslides in the Neapolitan slopes (western sector): Geologia Tecnica ed
times was sourced in the abundance of local resources and in the Ambientale, no. 2/99, p. 11–17.
practical management of the land that ensured reduction of
natural risks. With more geological hazards and limited resources, Cardone, V., 1990, Il tufo nudo nell’architettura napoletana: Napoli, Ed.
Naples was less fortunate in comparison. Cuen, 225 p.
ACKNOWLEDGMENTS D’Agostino, N., D’Anastasio, E., Gervasi, A., Guerra, I., Nedimovic, M.R.,
Seeber, L., and Steckler, M., 2011, Forearc extension and slow rollback of
This work benefited from a three month senior fellowship from the Rachel the Calabrian Arc from GPS measurements: Geophysical Research Letters,
Carson Center of Munich (2012) to D. de Rita. Particular thanks are due to v. 38, L17304, doi: 10.1029/2011GL048270.
Prof. Don Dingwell. A warm thank-you goes to our colleague Neil Thomas
Ellwood for the careful review of the final version of the English text. Finally, de’ Gennaro, M., Calcaterra, D., Cappelletti, P., Langella, A., and Morra, V.,
we are grateful to the two anonymous reviewers whose suggestions and criti- 2000, Building stone and related weathering in the architecture of the
cisms have helped to improve the text. ancient city of Naples: Journal of Cultural Heritage, v. 1, p. 399–414,
doi: 10.1016/S1296-2074(00)01096-7.
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