The Introduction. 
tica River, Negro River, Little River, Rio Para Matartiboron River, 
Cameron’s River, Rio Bueno Still River, Bear-Garden River, Lang- 
land's River, 
Rivers on the Noorthfide are, 
‘YT. Aie’s Great River, Ochorios or Rivers WhiteRiver, Stone- Bridge 
River, Rio Nuevo River, Rio Sambre Tiabo River, Oro Cabeca 
River, Six Mile River, Plantain Walk River, Negro River, Puerto 
Maria River, (rawle River, Water's River, Stony River, Agua alta, 
Anotto River, Flinty Rivee Trunnel's River, Orange River, Ugly Ri- 
ver, Ginge’s River, Little Tom's River, Fox’s River, Sandy River, 
Plantain Walk River, Church River or Pencarne River, Iterboreale 
River, Dry River, Flaycock River, White River, Buffe Bay River, 
Spanifh River, Devils River, Swift River, Great Devil's River, 
Back River, Loufie River, Daniel's River, Rio Grande White River, 
Fox’s River, Sandy River, Sc. Antonio River, Cameron River, Back 
River, Annotto River, Guava River, Savanna River, Snaky River, 
Negro River, Stony River, Annotto River, Porto Antonio River, Turtle 
Crawle Rivers, Prieft Man’s River, © Mulato River, Manchinil River, 
Crawle River, Driver's River, White River, Heéfor’s River, Horfe- 
Savanna River, Savage River, Plantain-Garden River, Muddy River, 
Sulphur River, Clark’s-Rivers»Coquar-Tree River; Cove River. 
The whole Ifland has one continu’d ridge of Hills running Eaft 
and Weft through its. middle, which. are called generally the blue 
Mountains, from their appearing of that colour, which comes from 
the Eyes going through a vaft quanticy of ther, or Air, as looking | 
to the Heavens in a clear day. The tops of fome are higher than 
others, one of the higheft is called Mount Diablo. . Ocher Hills there 
are on each fide of this Ridge of Mountains, which are lower.< 
Although this place be ficuated in the Torrid Zone, yet’the Air 
of it may very well be affirm’d temperate, in that the heatof the 
days is qualified by the length of the nights, which here ‘is. about 
twelve hours long all the year round ; fo that the Sun has hor'that 
length of timeto heat the Atmofphere, as where the days are longer, 
and the nights fhorter, or noneat all, *Tis.on the fame account 
that the evenings are much hotter than the mornings, although the 
Sun be equally diftant, and. the Rays fall the fame way, the heat 
becoming then extraordinary, becaufe it has been watm’d from morn- 
ing to that time, by the beams of the Sun, a great many of which 
continue to act with thofe coming frefh from theSun. The Breezes 
blowing all the year between from North-Eaft to South-Eaft, and 
rifing 
