Scottish geographical magazine . Nov. 1 Dec. for 1 Year. Edinburgh, 1-81 1-01 1-55 1-36 i 1-68 2-38 2-68 2-70 2-33 2-30 2-07 1-94 24-61 London, . 1-80 1-57 1-50 1-65 2-12 1-90 2-56 2-29 2-36 2-73 2-23 1-90 24-66 Paris, 1-47 1-42 1-21 1-25 1-44 1-93 1-90 2-02 1-79 1-94 1-79 1 1-72 19-89 Nice, 3-12 2-13 2-49 2-92 1-70 1-14 1-10 0 95 3-98 3-51 4-65 1 3-47 31-16 A^jaccio, . 2-39 1-69 1-94 2-07 1-55 0-72 0-15 1-07 1-01 2-81 4-96 1 2-40 22-76 Algiers, . 3 0 2-64 3-04 1-93 0-99 0-67 0-04 0-32 1-02 2-84 3-63 1 4-38 24-50 REFERENCE NOTE. FORESTS COLOURED GREEN trettipForest of TettI f B. Beech. I C. Co
Scottish geographical magazine . Nov. 1 Dec. for 1 Year. Edinburgh, 1-81 1-01 1-55 1-36 i 1-68 2-38 2-68 2-70 2-33 2-30 2-07 1-94 24-61 London, . 1-80 1-57 1-50 1-65 2-12 1-90 2-56 2-29 2-36 2-73 2-23 1-90 24-66 Paris, 1-47 1-42 1-21 1-25 1-44 1-93 1-90 2-02 1-79 1-94 1-79 1 1-72 19-89 Nice, 3-12 2-13 2-49 2-92 1-70 1-14 1-10 0 95 3-98 3-51 4-65 1 3-47 31-16 A^jaccio, . 2-39 1-69 1-94 2-07 1-55 0-72 0-15 1-07 1-01 2-81 4-96 1 2-40 22-76 Algiers, . 3 0 2-64 3-04 1-93 0-99 0-67 0-04 0-32 1-02 2-84 3-63 1 4-38 24-50 REFERENCE NOTE. FORESTS COLOURED GREEN trettipForest of TettI f B. Beech. I C. Cork Trees -| e. Evergreen C I M. Maritime F ^ P. Corsican PiMINERALS SHOWN THUSCopper Mines • CardoAntimony „ Luri Castlll Iron „ X OIjTieta Lead „ • Prato Silver Lead „ <Calenzano Anthracite „ • OsanI Lignite „ Saliceto Chef-lieu of arrondissement of same name thus ?CALVI Boundaries of 5 arrondissemerTowns of 1500 inhabitantsand upwards ns91V a REFERENCE NOTE. FORESTS COLOUREDtmtl^ForMt of Tett. SCOTTISH GEOGRAPHICAL MAGAZINE. 525 A REVIEW OF SWEDISH HYDROGRAPHIC RESEARCH IN THEBALTIC AND THE NORTH SEAS. By Otto Tie Waters in the Swedish fiords and in the submarine ponds and channels of thecoast—Changes in the Coast-Water at the close of the winter season, and theireffect upon the Herring Fishery. The depth of the water on the Swedish coast-bank ^ does not generallyexceed .30 metres. Through this coast-bank some deeper channels stretchobliquely in a direction from SW. to NE. Each channel may beregarded as a submarine continuation of one of the fiords of BohuslJin, adeep furrow ploughed by the glaciers during the Glacial Period in therocky ground of our continent. The Scandinavian fiords, as a rule, are?deeper in their inner parts, where the bottom forms a deep basin, which,at the entrance to the fiord, is shut off from communication, below acertain depth, with the waters of the open sea. It depends upon thedepth of this submarine
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Keywords: ., bookcentury1800, bookdecade1880, booksubjectgeography, bookyear18
