At Limon, Cahuita and Puerto Viejo, the hills, which are connected by spurs with the more elevated country of the interior, extend to the ocean coast. Between them, in plains extending from one to five miles inland, are forest-covered swamps, overflowed with not less than ten feet of water in the rainy season and only traversable in the dry.
Costa Rica claims sovereignty on the Atlantic side southeast as far as the Island of Escudo de Veragua, including the ancient Ducado de Veragua, whose frontier follows the coast of Chiriqui Viejo to the crest of the Cordillera, and crosses it to the head waters of the River Calobebora, then down this stream to the Escudo de Veragua.
Since their independence Colombia and Costa Rica have been in dispute in regard to their boundary line. Colombia has never ceased to claim jurisdiction over the entire Caribbean coast of Costa Rica, and even over that of Nicaragua as far north as Cape Gracias á Dios. In November, 1896, both governments signed a convention submitting their dispute to the arbitration of the President of the French Republic, or, in the event of his failure to act, to the President of Mexico or of the Swiss Confederation.
The principal lakes of Costa Rica are the Laguna Manatí, northwest from the Sarapiqui River; the Lagunas de Poas and de Barba, each on a volcano bearing its name; Lagunas de Sansan and Samay, towards the east and near the Sicsola River, in Talamanca; Laguna Tenoria, in Guanacaste; Laguna San Carlos, in the plains of San Carlos; Laguna de Arenal, between Las Cañas and San Carlos, and Laguna de Sierpe, in the south, northward from the Golfo Dulce.
Far away from Costa Rica, in the Pacific Ocean, lies the Cocos Island, about two hundred and sixty-six miles to the southwest of the Golfo Dulce, in N. latitude 5° 32′ 57″ and longitude 86° 58′ 25″ W. of Greenwich. Its highest point reaches 2250 feet, whence the descent is gradual to a bold, steep coast, which has many irregularities and rocks and a surf-beaten shore. Chatham Bay is its best harbor, having room for a dozen ships. The interior is broken into numerous fertile valleys, but there is probably not a square kilometer of level ground in the entire island. Other islands are Chira, Venado, San Lucas, Caño, etc.
Mineral Wealth.—In regard to the mineral wealth of Costa Rica, petroleum has been discovered near Uruchiko on the Talamanca coast, and coal in certain sandstone formations on both the Atlantic and Pacific sides of the Talamanca section.
In the province of Alajuela, a little to the north of the cart-road which runs from San José to Puentarenas, is Monte Aguacate, part of an old mountain range which extends far to the northwest, and not very distant from the Gulf of Nicoya. In general, it is of metamorphic formation, principally of diorite and porphyry.
Here, in a good climate, at 2000 feet elevation, are found auriferous veins of great richness. They are of quartz mixed with decomposed feldspathic rocks, and have yielded very lucrative bonanzas. The first mine was Guapinol, one bonanza of which produced $1,000,000. Several other mines were worked, from one of which (Los Castros) $2,000,000 were taken in a few years. It is estimated, from the best data obtainable, that about £1,000,000 have been taken from Monte Aguacate. Several of these veins are from six to seven feet wide, but that called the Quebrada Honda is sixteen feet wide. Most of the ore is of a high grade and of refractory character. It is probable that the whole southwestern slope of the Guatusos and Miravalles ranges of mountains is auriferous. The rocks in the northwestern extension of this district consist principally of feldspar, porphyry, basalt and dolorite.
The gold veins nearly all ran northeast and southwest, and are encased in feldspar, sometimes in porphyry, and occasionally in basalt. They consist, in great part, of crystalline quartz, and are from two to forty feet wide. Professor Pittier also found gold in the slopes of the Buena Vista mountain. Gold is further found in the Talamanca mountains, especially in the placer grounds of the Duedi River, and on the inferior hills between the Lari and Coen rivers.
Along the latter, and near Akbeta, also on the shore of Puerto Viejo, iron exists.