REGGIO EMILIA in northern Italy

1999 ◽  
Vol 1 (1) ◽  
pp. 16-18
Author(s):  
Professor Helen Penn
Keyword(s):  
2019 ◽  
pp. 23-50
Author(s):  
John Henderson

This chapter discusses the origins and spread of plague in northern Italy. Plague arrived in Italy in 1629 with French and German troops. It is no accident that the initial cases of plague identified in October of 1629 were first in Piedmont in the Val di Susa, west of Turin and near the border with France, and secondly in the Valtellina in Lombardy, subsequently travelling to Lake Como to the north of Milan. Other cities in northern Italy soon became infected and on May 6, 1630, the authorities as far south as Bologna announced the official outbreak of plague. Judging by the rapidity with which plague spread between these northern urban centres, one would have expected the epidemic to have arrived in Tuscany by early May, given that Bologna is only 65 miles north of Florence, but it was delayed by both natural and man-made factors. Tuscany is separated from Reggio-Emilia by the Apennine mountain range, which provided a physical barrier and facilitated the control of traffic coming from the north. The chapter then traces the preventive measures adopted by the health board as the plague approached Tuscany, including cordons sanitaires along frontiers, the removal of the sick to quarantine centres, and the rapid burial of the dead.


1999 ◽  
Vol 42 (5) ◽  
Author(s):  
R. Di Giovambattista ◽  
Y. Tyupki

We present the results of studies of seismicity in the Reggio Emilia area (Northern Italy). The Istituto Nazionale di Geofisica instrumental earthquake catalogue (1975-1996) reported about three moderate-size earthquakes with M ³ 4.5 that occurred in this area (November 1983, May 1987, October 1996). The RTL prognostic parameter proposed by Sobolev and Tyupkin (1996a) was used for analysis. This parameter is designed in such a way that a seismic quiescence produces negative anomaly of the RTL parameter in comparison to its perennial background level and an activation of seismicity initiates the growth of its value. The RTL prognostic parameter indicates that all three earthquakes are preceded by activation of the seismicity. The interval between the commencement of the activation identified by RTL parameter and the event itself was about one year for the 1987 and 1996 earthquakes, and about three months for the 1983 earthquake.


2007 ◽  
Vol 57 (1) ◽  
pp. 171-178 ◽  
Author(s):  
Carlo Salvarani ◽  
Nicolò Pipitone ◽  
Maria Grazia Catanoso ◽  
Luca Cimino ◽  
Bruno Tumiati ◽  
...  

2020 ◽  
Vol 11 ◽  
Author(s):  
Fiorello Ghiretti ◽  
Gabriela Gildoni ◽  
Gaddo Maria Grassi ◽  
Laura Torricelli ◽  
Elena Benassi ◽  
...  

2013 ◽  
Vol 93 (14) ◽  
pp. 3502-3511 ◽  
Author(s):  
Giuseppe Vasile Simone ◽  
Giuseppe Montevecchi ◽  
Francesca Masino ◽  
Valentina Matrella ◽  
Serena Anna Imazio ◽  
...  

Aerobiologia ◽  
1991 ◽  
Vol 7 (2) ◽  
pp. 160-163 ◽  
Author(s):  
Alberto Malanca ◽  
Rosella Orlandini ◽  
Valerio Pessina ◽  
Giuseppe Dallara
Keyword(s):  

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