1(58

Consequences of the Deluge.

and Nea between Lemnos and the Hellefpont-Alone between Leledos and 7 m,and arnonf?the Cyclades , Th er a and Therafiafilymp.

An. 4. [which last, or one of the fame naifl e 'Seneca faith was raised, himself beholding lt)nohs spellantilus enata Among theafter r 30 years Hiera , and two Furlongdistant in his own time,when Junius Sylla^and L.Balhus were Consuls, Thia. Butmost considerable and remarkable mutatisthat have been made in the Earth haveon the Sea-coasts, either by carrying on ^Land into the Sea, and attcrrating the b o 1 'torn of the Sea ; or by drowning the Lafl^near the Sea, by Irruptions and Inundati^ 5thereof, or undermining or washing avvfl/the shores.

Of the first fort of Change by Atterrat!^'or making the Sea dry Land, we have ^eminent Instance in the Dutch Net her lanwwhich, I easily consent with Verftegan, ^far as they are even and plain withoutHills, have undoubtedly heretofore in ti^long past, been Sea; as appears 1. From 1 ' 1Jowmess of their situation, some of the n^>Maritime Parts of them , as Zealand flslHolland , and part of Flanders, being so l 0 ^’that by breach or cutting of the Sand B an hor Downs, which the Sea by little andhath cast up, and the labour of Man