Page:Proceedings of the Royal Society of London Vol 2.djvu/50

Rh who found a current at the rate of one mile per hour, setting nearly along shore on the north coast of Spain.

With respect to the progress of the current which thus evidently sets along the southern side of the Bay of Biscay, the author has not been able to procure any further evidence directly showing its continuance round the Bay; but he observes that the soundings evidently show that the mud of the Garonne, Charante, Loire, &c., on the west coast of France, is all carried to the northward; and that the openings of these rivers evidently point in that direction in consequence of the current that sets across their mouths.

With regard to the further progress of the same current to the northward along the coast of France, direct evidence is again obtained in the instance of H.M.S. Russel, which was carried seventy miles to the N.W. by an unexpected current in that direction.

In addition to these facts, which are of comparatively recent occurrence, the author finds that the generally observed and well-known flow of the tides on the west of Scilly, cannot well be accounted for but by the supposition of a current setting in from the southward, which causes the flood tide to run nine hours northward, while the ebb in the opposite direction lasts only three hours.

Major Rennell has also recourse for evidence to two publications which have but recently come to his knowledge, though printed so long since as 1733 and 1757. In Joshua Kelly's Treatise on Navigation, of the former date, an instance is related of a West Indiaman drifted, during two days of dead calm, forty-six miles northward, across the mouth of the British Channel.

Captain Mead also, in relating the case of the ship Hope of Liverpool, in 1735, mentions her having been drifted forty-eight miles to the northward of her expected course, by the same current which he represents as an indraught into St. George's Channel; and says it was well known to the Bristol men in making for their Channel, and that accordingly they made allowance in their bearing of 4° or 5° for that indraught.

The author takes this occasion to notice another current, setting to the north-eastward across St. George's Channel into Cardigan Bay, which sometimes endangers the safety of vessels in their passage from the Land's End to Dublin.

This may partly arise from the tail of the Scilly current having an easterly set, in consequence of meeting the S.E. coast of Ireland; but in the author's estimation is more likely to originate from a cause similar to that of the Scilly current itself, in consequence of the south-westerly winds carrying a heavy sea along that coast from Cape Clear to Carnsore Point. 