. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology; Zoology. BIGELOW: COAST WATER EXPLORATION OF 1913. 211 cially interesting because while it runs almost horizontal at about fifty fathoms from Station 10090 to and across Jeffrey's Bank, it must then dip to bottom in about seventy fathoms, the bottom salinity at Station 10102 being only , suggesting a shoreward movement of salt bottom water across the Bank. The next profile (Fig. 51) is parallel to the last, some 30 miles further east (Station 10099, 10100, 10092). Here the slope ofjthe bottom is. Fig. 52.— Sali
. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology; Zoology. BIGELOW: COAST WATER EXPLORATION OF 1913. 211 cially interesting because while it runs almost horizontal at about fifty fathoms from Station 10090 to and across Jeffrey's Bank, it must then dip to bottom in about seventy fathoms, the bottom salinity at Station 10102 being only , suggesting a shoreward movement of salt bottom water across the Bank. The next profile (Fig. 51) is parallel to the last, some 30 miles further east (Station 10099, 10100, 10092). Here the slope ofjthe bottom is. Fig. 52.— Salinity profile lengthwise of the northeastern part of the Gulf of Maine from south to north (Stations 10092, 10097, 10098). m even one, consequently the salinity curves do not show the anoma- ies noted for the profiles further west; but they agree with the latter n dipping shoreward between the surface and thirty fathoms. The water close to the surface was slightly Salter at Station 10100 han at Station 10092, though the former is the nearer shore; but this. 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 Harvard University. Museum of Comparative Zoology. Cambridge, Mass. : The Museum
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