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Castle Crags, located in Northern California, is characterized by its dramatic granite formations, which are part of the Sierra Nevada mountain range. The geology primarily consists of granodiorite, a type of intrusive igneous rock formed from magma that cooled slowly beneath the Earth's surface. The area exhibits features such as steep cliffs, spires, and glacially-carved valleys, showcasing the effects of both tectonic activity and erosion over millions of years. This unique geology contributes to the region's stunning landscapes and diverse ecosystems.

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