Puerto Rico | History, Geography, & Points Of Interest - Britannica

Relief

Puerto Rico is largely composed of mountainous and hilly terrain, with nearly one-fourth of the island covered by steep slopes. The mountains are the easternmost extension of a tightly folded and faulted ridge that extends from the Central American mainland across the northern Caribbean to the Lesser Antilles. Although Puerto Rican relief is relatively low by continental standards, the island sits less than 100 miles (160 km) south of a precipitous depression in Earth’s crust: an extensive submarine feature of the Atlantic known as the Puerto Rico Trench, which descends to more than 5 miles (8 km) below sea level—the Atlantic’s deepest point—at a site northeast of the Dominican Republic. Powerful tectonic forces that over millions of years have created these features still occasionally cause earthquakes in Puerto Rico.

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The island’s highest mountain range, the Cordillera Central, trends east-west and exceeds 3,000 feet (900 meters) in many areas; its slopes are somewhat gentle in the north but rise sharply from the south coast to the loftier peaks, topped at about 4,390 feet (1,338 meters) by Cerro de Punta, the highest point on the island. Near the island’s eastern tip, the partly isolated Sierra de Luquillo rises to 3,494 feet (1,065 meters) at El Yunque Peak.

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The northwestern foothills and lowlands are characterized by karst features, including sinkholes (sumideros), caverns, and eroded mogotes, or haystack hills (pepinos). There is a continuous but narrow lowland along the north coast, where most people live, and smaller bands along the south and west coasts that also include densely populated areas. The Caguas Basin, in the Grande de Loíza River valley south of San Juan, is the largest of several basins in the mountains that provide level land for settlements and agriculture. The islands of Mona, Vieques, and Culebra are generally hilly but ringed by narrow coastal plains; Vieques rises to 988 feet (301 meters) at Mount Pirata.