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The Panama plate is a small tectonic plate that exists between two actively spreading ridges and moves relatively independently of its surrounding plates. [1] The Panama plate is located between the Cocos plate and the Nazca plate to the south and the Caribbean plate to the north.
The Panama fracture zone is a major, active right lateral-moving transform fault and associated inactive fracture zone which forms part of the tectonic boundary between the Cocos plate and the Nazca plate, the Cocos–Nazca spreading centre.
The Cocos and Nazca plates formed in the Miocene.The Panama microplate is made of oceanic crust basalt, similar to the basalt plateau at the bottom of the Caribbean Sea.The isthmus of Panama formed due to convergent tectonics of the eastern Pacific subduction zone, which created a magmatic arc extending from southern North America.
The 13,000 km 2 Galápagos microplate lies at the western end of the GSC. It is bounded to the west by strands of the East Pacific Rise, to the southeast by the Dietz Volcanic Ridge and the Dietz Deep rift, and to the north by the GSC. [4] Another separate, smaller microplate has also been proposed , bounded to the north by an incipient rift ...
The geology of Costa Rica is part of the Panama Microplate, which is slowly moving north relative to the stable Caribbean Plate. [1] [2]In the late Cretaceous, an oceanic trench or backarc system formed in connection with a subduction zone, situated where the Isthmus of Panama is now located.
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The Panama block, a microplate, lies southeast of the country; its boundary with the Caribbean Plate, the Panama Thrust Bent, is a destructive plate boundary that stretches from Colombia to Limon, near the east coast of Costa Rica. In Costa Rica, the Panama Thrust Bent causes the Caribbean Plate to underthrust beneath the Cordillera de Talamanca.
Over 300,000 migrants crossed the Darien Gap into Panama in 2024, 42% fewer than the record number who made the perilous jungle crossing from South America a year earlier, Panama's migration ...