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For details on the engineering and operation of the waterway, Soils are commonly reddish to brown and rich in clay.They vary in fertility, and in many areas crops can be grown continuously only if fertilizers are applied.The highlands and mountains are made up primarily of igneous (volcanic) rocks.The lowlands include the plains of Panamá and Chiriquí provinces, the plains and hills of Colón province, the Chepo and Chucunaque river basins in the east, and the narrow northeastern plains of the Caribbean region.
Our editors will review what you’ve submitted and determine whether to revise the article.The principal archipelagoes off the Caribbean coast are those of Bocas del Toro and San Blas. Rivers flowing to the Pacific include the Chiriquí Viejo, Santa María, Chepo, Chucunaque, and Tuira.During the rainy season the Tuira is navigable for some 40 miles (60 km) and the Chepo for 20 miles (30 km).Water in the Panama Canal does not flow from coast to coast; rather, it is released from the rain-fed Gatún and Alajuela (Madden) lakes in the central highlands.In effect, the water flows to both coasts simultaneously via the canal’s system of locks and dams.
The canal also secures Panama’s ongoing role in international affairs and world commerce.