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Updated: June 3, 2025


Point Martin Garcia where the western side of Ocoa Bay is regarded as terminating also marks the beginning of another large bay, Neiba Bay, which has the form of a cul-de-sac, with a length of eighteen miles and an average breadth of seven miles. It is open to the southeast, but in all other directions is well protected by high mountains.

The Neiba Valley, situated in the southwestern portion of the Republic between the Neiba and the Baboruco Mountains is more regular. It is part of the valley which stretches from Neiba Bay, in Santo Domingo, to Port-au-Prince in Haiti. The Dominican portion is 65 miles long by 12 miles wide, and over one-half of its area is covered by the waters of Lake Enriquillo.

Among them special reference may be made to the Sierra Zamba, which runs parallel to the Yaque del Norte River, the Sierra de San Jose de las Matas, the Santiago Range, the Jarabacoa Range and the Cotui Range. The fourth principal mountain range of the Republic, the Neiba Range, is sometimes classed as a part of the Cordillera Central.

The water is of ample depth and there are several good anchorages, the best being the port of the small city of Barahona. From Neiba Bay to Cape Beata the coast waters are shallow and are only visited by small vessels which come to take away lumber or coffee from the neighboring heights.

The only lakes of any size are two which lie in the Neiba Valley, the larger one, Lake Enriquillo, being comprised entirely within Dominican territory, while of the smaller one, variously called Etang Saumatre, or Lake Azuei, or Laguna del Fondo, through which the frontier line passes, less than one-fourth is under Dominican jurisdiction.

The modern lands are the coast plains and the small terraces on the south of the central range and on the south of the Baboruco mountains, the Maguana, Azua and Neiba valleys, small areas on the north coast at the foot of the mountains, and the marshes and Yuna River delta at the head of Samana Bay.

Rock salt is found near Neiba in inexhaustible quantities, there being several hills of native salt covered with a thin layer of soil. The fact that the waters of Lake Enriquillo are saltier than the sea is attributed by some to a deposit of this kind. The salt is so pure that it does not attract moisture and deliquesce.

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