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The universal geography : earth and its inhabitants

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6<br />

WEST AFRICA.<br />

expedition ill u purt of the Azorian Atlantic presenting great inequaUties of deptt,<br />

<strong>and</strong> where four soundings revealed 500, 95, 150, <strong>and</strong> 830 fathoms in rapid<br />

succession. J,'everthelcss, the same naturalists observed that tlie ^vatcr was of a<br />

sea-green colour between the Canaries <strong>and</strong> Cape Verd group, where, instead of<br />

meeting with comparatively shallow water, they determined a mean depth of uo<br />

to 3,300<br />

Feet.<br />

pi,r. 2. Deittus of the AzomAH Atlantic.<br />

Depths.<br />

3,300 to 1G,600<br />

feet.<br />

Scale 1 : 40,000,000.<br />

^'jp;! VltJ [sJos s<br />

*West or Gree^w'C^><br />

10,500 Feet <strong>and</strong><br />

upwards.<br />

. 600<br />

to 3,300<br />

Feet.<br />

Mfles.<br />

Heights.<br />

3,300 Feet <strong>and</strong><br />

upwards.<br />

less than 1,500 fathoms. In fact, this phenomenon of shifting colours in sea-<br />

wutor has been explained by physicists in the most diverse ways. While Toyubee<br />

asserts tliat a green tint prevails when the surface is cool <strong>and</strong> the atmosphere<br />

moist, the observations of the Gazelle would seem to show that the contrast<br />

between blue <strong>and</strong> greenish hues is due to the different degrees of salt held in<br />

solution, blue water being the most dense.

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