Few organic remains have been found near Brighton. Dr. Mantell mentions but a fragment of a bone resembling the femur, and a grinder of a large size, decidedly the latter that of an Asiatic elephant, in the brick-loam at Hove; the jaw of a whale in the shingle bed; the antlers and bones of the red deer in a bed of loam, in sinking a well near the cavalry barracks; the remains of a deer in the diluvium at Copperas Gap, by the Rev. H. Hoper; and similar remains in digging a well near the Western Road. With respect to climate, medical men, who have made it their study, have divided the town into three districts. In 1845, Dr. Wigan, then in medical practice in the town, published an elaborate treatise, “Brighton and its Three Climates,” and in 1859, Dr. Kebbell, Physician to the Sussex County Hospital, produced his valuable book, “The Climate of Brighton.” The former considers the north-west part of the town the most salubrious, as it is exempt from the keen easterly winds, and is generally free from the fogs and smoke of the central district. It is free, too, of the marine exhalations to which that district is subject. The air of the east division is bracing, and likewise exempt from the saline particles which impregnate the atmosphere of the lower part of the town, a district which differs but little from any inland town in a low situation, and possesses none of the quality called bracing. Fogs, night and morning, frequently hang about the middle district, which may be termed the business quarter of the town. Dr. Kebbell says:—