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north and south. They gradually feel the earth's rotation; but on their arrival at the tropics, being still inferior in velocity to the equatorial sea, they seem to roll backwards; in other words, they form a current from east to west. This current is farther impelled by the trade-winds.

      The progress of this great perpetual current includes almost every part of the ocean. In going westward, it necessarily rushes against the coast of America, where it divides into two vast branches, one running south with great force, and the other north-west. A succession of currents, all connected, obviously form a "moving power" to prevent the stagnation of the ocean, and, by their branches, visit every shore of the globe.

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      1

      Critical and Miscellaneous Essays, iii. 205, 206.

      2

      Critical and Historical Essays, iii. 446, 447.

      3

      Ibid., iii. 144-146.

      4

      Critical and Historical Essays, iii. 141, 142.

      5<

1

Critical and Miscellaneous Essays, iii. 205, 206.

2

Critical and Historical Essays, iii. 446, 447.

3

Ibid., iii. 144-146.

4

Critical and Historical Essays, iii. 141, 142.

5

History, i. 610, 611.

6

Vol. i. p. 127, 128.

7

The Physical Atlas: A series of Maps and Notes on the Geographical Distribution of Natural Phenomena. By Alexander Keith Johnston, Geographer in Ordinary to Her Majesty, &c. Folio.

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