Consequences of the Deluge.

of

burning at the same time with thatVesuvius in Campania , viz. in the Y e3 f1633. So that not only Vesuvius commun 1 'cates with Ætna by lubterraneous Vault 5 ’but also (a; he rationally infers) Ætna Witthe Mountains of Syria , the Tunnels rufl'ning under the depths of the Mediterrant^Sea, and thole with the Arabian , and last*;the Arabian with Mount Semo in Æ^ lt '

pia

That an inflamed Damp or fubterraneo 0 *Fire is the cause of all Earthquakes in geO 6 'ral, and not only such as precede the erup'tions of Vulcano’s, may be proved by an e ’minent instance of an Earthquake happ el Ting May iz. i68z.which Ihook the greatspart of France and Switzerland , and read 1as far as Collen in Germany : an AccO 1111whereof we have in th c Journal des Seasot forth June 1. i68z. inserted in the ’ly Memorials printed for Mr. Faithos'

Numb. 2.3. In which they write, That

was perceived in Lionnois , (which wasto pass for a place exempt from suchdents) in Dauphiny and Beaujolou , thous?very little, and without any ill conlequ’’ 11 ^Tsoit at Met sin Lor rain the Watch-pJ ace f 6a Bulwark was thrown down intoDitch, with the Soldier that stood Sentn 1

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