520 



APPENDIX. 



oce^n to the east of it ; while the still greater cold of the sea-water 

 on its western side, between the Gulf Stream and the continental 

 shore, is explained by the great Arctic current, pouring down from 

 Baffin s Bay, and skirting the shore of North America as far as the 

 Coast of Florida, until it is lost in that latitude under the Gulf 

 Stream. The object of Dr. Bache s investigation was to trace the 

 mutual relations of these two great currents of warm and cold 

 water, flowing side by side in opposite directions, and to discover 

 the conditions which regulate their movements and keep them 

 within definite limits. 



The investigation is even now by no means complete, though it has 

 been going on for many years. It has, however, been ascertained 

 that, while the ocean-bed deepens more or less rapidly as we recede 

 from the shore, forming a trough in which the Gulf Stream flows, 

 this trough is limited on its eastern side by a range of hills trend 

 ing in the direction of the current, outside of which is another de 

 pression or valley. Indeed, the sea-bottom exhibits parallel ridges 

 and depressions, running like the shore of the continent itself, in a 

 northeasterly direction. The water presents differences of tem 

 perature, not only on the surface, but at various depths below. 

 These inequalities have been determined by a succession of 

 thermometric observations along several lines, crossing the Gulf 

 Stream from the shore to the ocean water on its eastern side, at 

 intervals of about a hundred miles. The observations have been 

 made first at the surface, and then at successively greater depths, 

 varying from ten to twenty, thirty, one hundred, two hundred, and 

 even three and four hundred fathoms. This survey has shown 

 that, while the Gulf Stream has a temperature higher than that 

 of the waters on either side, it is also alternately warmer and 

 colder within itself, being made up as it were of distinct streaks 

 of water of different temperature. These alternations continue to 

 as great a depth as the observations have been carried, and are 

 found to extend even to the very bottom of the sea, where this has 

 been reached. The most surprising part of this result is the 



