Matches in DBpedia 2016-04 for { ?s ?p "Carrizalillo is a caldera in Chile. It is located in the Central Volcanic Zone and is part of the Paleocene-Eocene volcanic belt. The caldera is located 50 kilometres (31 mi) southwest of Copiapo. It is heavily eroded. Active during the Cretaceous, it is a large caldera. Postcollapse activity generated subsidiary calderas inside the older main caldera."@en }
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- Carrizalillo_(caldera) abstract "Carrizalillo is a caldera in Chile. It is located in the Central Volcanic Zone and is part of the Paleocene-Eocene volcanic belt. The caldera is located 50 kilometres (31 mi) southwest of Copiapo. It is heavily eroded. Active during the Cretaceous, it is a large caldera. Postcollapse activity generated subsidiary calderas inside the older main caldera.".
- Q21044353 abstract "Carrizalillo is a caldera in Chile. It is located in the Central Volcanic Zone and is part of the Paleocene-Eocene volcanic belt. The caldera is located 50 kilometres (31 mi) southwest of Copiapo. It is heavily eroded. Active during the Cretaceous, it is a large caldera. Postcollapse activity generated subsidiary calderas inside the older main caldera.".
- Carrizalillo_(caldera) comment "Carrizalillo is a caldera in Chile. It is located in the Central Volcanic Zone and is part of the Paleocene-Eocene volcanic belt. The caldera is located 50 kilometres (31 mi) southwest of Copiapo. It is heavily eroded. Active during the Cretaceous, it is a large caldera. Postcollapse activity generated subsidiary calderas inside the older main caldera.".
- Q21044353 comment "Carrizalillo is a caldera in Chile. It is located in the Central Volcanic Zone and is part of the Paleocene-Eocene volcanic belt. The caldera is located 50 kilometres (31 mi) southwest of Copiapo. It is heavily eroded. Active during the Cretaceous, it is a large caldera. Postcollapse activity generated subsidiary calderas inside the older main caldera.".