Matthew Fontaine Maury, Lieutenant, U.S.N.

Summary

Matthew Fontaine Maury, Lieutenant, U.S.N. Physical Geography Of The Sea… (1855)

Instances of commotion in the sea at uncertain intervals — the making, as it were, of efforts by fits and starts to keep up to time in the performance of its manifold offices — are not unfrequent, nor are they inaptly likened to spasms. The sudden disruption of the ice which arctic voyagers tell of, the immense bergs which occasionally appear in groups near certain latitudes, the variable character of all the currents of the sea—now fast, now slow, now running this way, then that — may be taken as so many signs of the tremendous throes which occur in the bosom of the ocean.
Source: Wikisource

Matthew Fontaine Maury, Lieutenant, U.S.N. Physical Geography Of The Sea… (1855)

The volume of warm water in the North Atlantic is greater than the volume of cold water that meets and opposes it; consequently, the warm thrusts the cold aside, dividing and compelling it to go round. The same thing is repeated in the North Pacific, whereas the converse obtains in the South Atlantic. Here the great polar flow, after having been divided by the American Continent, enters the Atlantic, and filling up nearly the whole of the immense space between South America and Africa, seems to press the warm waters of the tropics aside, compelling them to drift along the coast on either hand.
Source: Wikisource

Matthew Fontaine Maury, Lieutenant, U.S.N. Physical Geography Of The Sea… (1855)

This sort of pulsation is heard also in the howlings of the storm and the whistling of the wind; the needle trembles unceasingly to it, and tells us of magnetic storms of great violence, which at times extend over large portions of the earth’s surface; and when we come to consult the records of those exquisitely sensitive anemometers, which the science and ingenuity of the age have placed at the service of philosophers, we find there that the pulse of the atmosphere is never still: in what appears to us the most perfect calm, the recording pens are moving to the pulses of the air.
Source: Wikisource

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