FREE BOOKS

Author's List




PREV.   NEXT  
|<   545   546   547   548   549   550   551   552   553   554   555   556   557   558   559   560   561   562   563   564   565   566   567   568   569  
570   571   572   573   574   575   576   577   578   579   580   581   582   583   584   585   586   587   588   589   590   591   592   593   594   >>   >|  
, wrote descriptions of the earthquake; and the Royal Academy of Naples, not satisfied with these and other observations, sent a deputation from their own body into Calabria, before the shocks had ceased, who were accompanied by artists instructed to illustrate by drawings the physical changes of the district, and the state of ruined towns and edifices. Unfortunately these artists were not very successful in their representations of the condition of the country, particularly when they attempted to express, on a large scale, the extraordinary revolutions which many of the great and minor river-courses underwent. But many of the plates published by the Academy are valuable; and as they are little known, I shall frequently avail myself of them to illustrate the facts about to be described.[665] In addition to these Neapolitan sources of information, our countryman, Sir William Hamilton, surveyed the district, not without some personal risk, before the shocks had ceased; and his sketch, published in the Philosophical Transactions, supplies many facts that would otherwise have been lost. He has explained, in a rational manner, many events which, as related in the language of some eye-witnesses, appeared marvellous and incredible. Dolomieu also examined Calabria during the catastrophe, and wrote an account of the earthquake, correcting a mistake into which Hamilton had fallen, who supposed that a part of the tract shaken had consisted of volcanic tuff. It is, indeed, a circumstance which enhances the geological interest of the commotions which so often modify the surface of Calabria, that they are confined to a country where there are neither ancient nor modern rocks of volcanic or trappean origin; so that at some future time, when the era of disturbance shall have passed by, the cause of former revolutions will be as latent as in parts of Great Britain now occupied exclusively by ancient marine formations. _Extent of the area convulsed._--The convulsion of the earth, sea, and air extended over the whole of Calabria Ultra, the southeast part of Calabria Citra, and across the sea to Messina and its environs; a district lying between the 38th and 39th degrees of latitude. The concussion was perceptible over a great part of Sicily, and as far north as Naples; but the surface over which the shocks acted so forcibly as to excite intense alarm did not generally exceed 500 square miles in area. The soil of that part of Calabria
PREV.   NEXT  
|<   545   546   547   548   549   550   551   552   553   554   555   556   557   558   559   560   561   562   563   564   565   566   567   568   569  
570   571   572   573   574   575   576   577   578   579   580   581   582   583   584   585   586   587   588   589   590   591   592   593   594   >>   >|  



Top keywords:

Calabria

 

shocks

 

district

 

Naples

 

Academy

 

published

 
revolutions
 

surface

 
volcanic
 

ancient


Hamilton

 
earthquake
 
country
 
illustrate
 

artists

 
ceased
 

trappean

 
modern
 

passed

 

disturbance


future
 

origin

 

consisted

 

shaken

 

fallen

 

supposed

 

forcibly

 

circumstance

 
enhances
 

modify


excite

 

confined

 

geological

 

interest

 

commotions

 

southeast

 

Messina

 

perceptible

 
Sicily
 
exceed

generally
 

degrees

 
environs
 
concussion
 

mistake

 
extended
 

occupied

 

intense

 

exclusively

 
marine