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Tsingy Bemaraha, located in Madagascar, is formed primarily through a combination of limestone erosion and geological processes. Over millions of years, acidic rainwater has dissolved the limestone, creating deep fissures and sharp, needle-like rock formations known as "tsingy." This unique karst landscape is characterized by its rugged pinnacles and is often surrounded by dense forest, resulting from the interplay of erosion, tectonic activity, and climatic conditions. The area is also notable for its rich biodiversity, making it a significant natural site.

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