Show A Tlde feea sea I 1 for practical purposes the mediterranean may be accepted as being what it is 1 l I 1 popularly supposed to bea be a deless tl sea I 1 ot 1 betit but it Is not coln so in reality Inmany in many places v there is a distinct rise and fall though this is more frequently due to winds and il c cu rients than to lunar attraction pk at venice there Is a rise of from one to d two feet in spring tides according to the I 1 1 1 I 1 prevalence of winds up or down the tile aarl abic in many straits and narrow arms of t 11 the sea there is a periodical lux flux and re 1 flux but the only place where the tidal in 9 r fluence properly property BO so called is unmistakably r I 1 observed Is in the gulf of cabos cabes where tho A tide runs at the rate of two or three knots 01 1 an hour and the rise and tall fall varies from three to elahi feet philadelphia ledger |