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See also:ADIGE (Ger. Etsch, anc. Athesis) , a considerable See also:river in See also:North See also:Italy . The true source of the See also:Adige is in some small lakes on the See also:summit of the Reschen Scheideck Pass (4902 ft.), and it is swollen by several other streams, near Glurns, where the roads over the Ofen and the Stelvio Passes fall in . It thence flows See also:east to See also:Meran, and then See also:south-east to See also:Botzen, where it receives the Fisak (6 ft.), and becomes navigable . It then turns south-See also:west, and, after receiving the Noce (right) and the Avisio (See also:left), leaves See also:Tirol, and enters See also:Lombardy, 13 M. south of See also:Rovereto . After traversing North Italy, in a direction first southerly and theneasterly, it falls into the Adriatic at See also:Porto Fossone, a few See also:miles north of the mouth of the Po . The most considerable towns on its See also:banks (south of Botzen) are See also:Trent and Rovereto, in Tirol, and See also:Verona and See also:Legnago, in Italy . It is a very rapid river; and subject to sudden swellings and overflowings, which cause See also:great damage to the surrounding See also:country . It is navigable from the See also:heart of Tirol to the See also:sea . In Lombardy it has a breadth of 200 yds., and a See also:depth of to to 16 ft., but the strength of the current renders its See also:navigation very difficult, and lessens its value as a means of transit between See also:Germany and Italy . The Adige has a course of about 220 m., and, after the Po, is the most important river in Italy . In See also:Roman times it flowed, in its See also:lower course, much farther north than at See also:present, along the See also:base of the Euganean hills, and entered the sea at Brondolo . In A.D . 587 the river See also:broke its banks, and the See also:main stream took its present course, but new streams opened repeatedly to the south, until now the Adige and the Po See also:form conjointly one See also:delta . (W . A . B . |
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