THE HANNIBAL ENIGMA OF 218 BC: A FORENSIC EXERCISE OF
ment accrued in valleys by stream erosion and de-velopment of Holocene terraces but for the most part the landscape seen today is what Hannibal and his troops saw when they ventured forth across the Col de la Traversette The impediments to exfiltration faced by Hannibal are the very same as exist today
HANNIBAL’S TREK ACROSS THE ALPS: GEOMORPHOLOGICAL ANALYSIS OF
mentions the Col de la Traversette but makes no mention of de Beer (1967, 1969), Prevas (1998), amongst others, who argue for the southern route shown in Figure 1 And whilst the authors argue further that Hannibal might have easily moved through the Col de Montgenèvre, and assert he used local guides to surprise the
THE HANNIBAL ROUTE QUESTION OF 218 BC: A FORENSIC EXERCISE
fying the landscape in the area of the Col de la Traversette The impediments to exfiltration faced by Hannibal are the very same as exist today on both the French and Italian sides of the Western Alps It is within this matrix of bedrock and deposits that the search for environmental evidence related to the in-vasion began in 2002
Biostratigraphic Evidence Relating to the Age-Old Question of
of the army that Hannibal ordered its firing to allow the passage of the horses and elephants Ac-cording to this account, wood was brought to the site at 2600 m asl, then set alight, producing Figure 2 (a) Air-photographic coverage of the core/section sites relative to the Col de la Traversette, Hannibal’s proposed transit pass into Italia
Ancient horse poo sheds light on Hannibals march
that Hannibal is considered to have taken, it is thought the site at the Col de la Traversette could have been used for watering large numbers of animals Carbon isotope analysis dates the deposits to
THE HANNIBAL ROUTE CONTROVERSY AND FUTURE HISTORICAL
The major cols are listed from south to north with the Col de al Traversette (3000 m) called Hannibal’s col sin ce antiquity Tribes, e g Allobroges, are located in approximate cis-and trans
Notes on magnetic susceptibility in the Guil Valley alluvial
toward the Col de la Traversette Likewise, Polybius, who is the prime ancient authority, states definitely that Hannibal descended to the Po River Plains ra-ther than to the Dora Riparia approximately 50 km to the north After two millennia of investigations, correlation of ancient topographic names with moderns ones,
Cahn’s Quarterly 1/2017
route – from the River Rhône over the Col de la Traversette (2947 m asl) – which had already been favoured by Sir Gavin de Beer in the 1950s-1960s was in all likelihood the one taken by Hannibal Since 2016, the choice of this route has been substantiated by convincing stratigraphic, geochemical and microbiological evidence
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