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.
Public-domain text, read in full here on John Shaqi.
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