Paricutin is a volcano located in the state of Michoacán, Mexico. It famously erupted in 1943, emerging from a cornfield and quickly growing to a height of over 400 meters. The eruption lasted for about nine years, creating a significant amount of lava and ash that affected the surrounding area. The volcano is known for its unique formation and is a popular site for scientific study. It is part of the Trans-Mexican Volcanic Belt and is considered a classic example of a cinder cone volcano. Today, Paricutin is a UNESCO World Heritage site, attracting visitors interested in geology and natural history.