Puerto Rico
Geology
Puerto Rico is composed of Cretaceous to Eocene volcanic and plutonic rocks, which are overlain by younger Oligocene to recent carbonates and other sedimentary rocks. Most of the caverns and karst topography on the island occurs in the northern Oligocene to recent carbonates. The oldest rocks are approximately 190 million years old (Jurassic) and are located at Sierra Bermeja in the southwest part of the island. These rocks may represent part of the oceanic crust and are believed to come from the Pacific Ocean realm. Puerto Rico lies at the boundary between the Caribbean and North America plates. This means that it is currently being deformed by the tectonic stresses caused by the interaction of these plates. These stresses may cause earthquakes and tsunamis. These seismic events, along with landslides, represent some of the most dangerous geologic hazards in the island and in the northeastern Caribbean.
Related Topics:
Cretaceous - Eocene - Volcanic - Plutonic - Oligocene - Carbonate - Sedimentary rock - Cavern - Karst - Jurassic - Sierra Bermeja - Oceanic crust - Pacific Ocean - Plate - Tectonic - Earthquakes - Tsunami - Seismic - Landslide - Geologic hazards
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~ Table of Content ~
| ► | Introduction |
| ► | History |
| ► | Geography |
| ► | Geology |
| ► | Politics |
| ► | Economy |
| ► | Demographics |
| ► | Culture |
| ► | Municipalities |
| ► | See also |
| ► | Related Topics |
| ► | External links |
| ► | References |
| ► | Notes |
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