. The depths of the ocean : a general account of the modern science of oceanography based largely on the scientific researches of the Norwegian steamer Michael Sars in the North Atlantic. "Michael Sars" North Atlantic Deep-sea Expedition (1910); Oceanography; North Atlantic Ocean. 634 DEPTHS OF THE OCEAN chap. and the Faroe-Shetland channel. Johs. Schmidt first drew attention to this community. Salpa fusiforjuis, the larval actinia Arachnactis albida (the distribution of which is shown in Fig. 480), the barnacles Lepas pectmata and L. fasciathiris, young stages of the thread-like fis
. The depths of the ocean : a general account of the modern science of oceanography based largely on the scientific researches of the Norwegian steamer Michael Sars in the North Atlantic. "Michael Sars" North Atlantic Deep-sea Expedition (1910); Oceanography; North Atlantic Ocean. 634 DEPTHS OF THE OCEAN chap. and the Faroe-Shetland channel. Johs. Schmidt first drew attention to this community. Salpa fusiforjuis, the larval actinia Arachnactis albida (the distribution of which is shown in Fig. 480), the barnacles Lepas pectmata and L. fasciathiris, young stages of the thread-like fish Fierasfer, Nerophis cEquoreiis, larvae of the common eel and scopelidse iyMyctophum glaciale and M. pitnctatum) ozQMX here in great numbers. Excepting the salpse, the barnacles and the leptocephali, which also occur in the warm Atlantic, all these forms live in what may be. Fig. 480.—DiSTRTBUTION OF Arachx called a transitional area between the Atlantic and the Nor- wegian Sea. The conditions of temperature in this bathymetrical region are shown in Figs. 159, p. 227, and 160, p. 228 (surface temperature for February and August), and In Fig. 312, p. 445 (temperature at 100 metres). Comparing these charts with the current chart in Chapter X., we obtain a good impression of the currents of the North Atlantic. The warm Gulf Stream, originating in the Gulf of Mexico, follows the east coast of the United States towards the Banks of Newfoundland, where it divides into several branches. A northern branch appears to run towards Davis Strait, partly as an undercurrent. An eastern branch runs towards the Azores and, spreading out like a fan,. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Murray, John, Sir, 1841-1914; Hjort, Johan, 1869-; Appellöf, Jakob Johan Adolf, 1857-; Gran, H. H. (Haakon Hasberg), 1870?-; H
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