The Huaynaputina volcano, southern Peru, was the site of the largest historical eruption (VEI 6) in the Andes in 1600 CE, which occurred during the historic transition between the Inca Empire and the Viceroyalty of Peru. This event had severe consequences in the Central Andes and a global climatic impact. Spanish chronicles reported that at least 15 villages or settlements existed around the volcano, of which seven of them were totally destroyed by the eruption. Multidisciplinary studies have allowed us to identify and analyze the characteristics of six settlements buried by the eruption. Tephra fallout and pyroclastic current deposits (PDCs) had different impacts according to the settlement distance from the crater, the location with respect to the emplacement of PDCs along valleys, the geomorphological characteristics of the site, and type of constructions. Thus, Calicanto, Cojraque, and San Juan de Dios, located beneath the main axis of tephra dispersal lobe due west and/or on valley edges, were buried under several meters of pyroclastic deposits, while the villages of Estagagache, Chimpapampa, and Moro Moro, located to the S and SE of the lobe, were partially mantled by tephra. The 1600 CE Huaynaputina eruption created an important geological and cultural heritage, which has scientific, educational, and touristic values. Geo-touristic attractions are proposed based on identification, characterization, and qualitative evaluation of four groups totaling 17 geosites: volcanic geosites, volcanic-cultural geomorphosites, and hot springs. Seven geological roads along with seven viewpoints are proposed, which allow to value the most relevant landscapes, deposits and geological structures.

秘鲁南部的瓦伊纳普蒂纳火山是公元 1600 年安第斯山脉历史上最大的火山喷发 (VEI 6) 的地点，发生在印加帝国和秘鲁总督之间的历史性过渡期间。这一事件对中安第斯山脉造成了严重后果，并对全球气候产生了影响。据西班牙编年史报道，火山周围至少有 15 个村庄或定居点，其中 7 个被火山喷发完全摧毁。多学科研究使我们能够识别和分析被火山喷发掩埋的六个定居点的特征。火山灰和火山碎屑流沉积物 (PDCs) 根据距火山口的沉降距离、PDCs 沿山谷的位置、场地的地貌特征、和建筑类型。因此，位于西部和/或山谷边缘的火山灰扩散叶主轴下方的卡利坎托、科伊拉克和圣胡安德迪奥斯被掩埋在几米厚的火山碎屑沉积物下，而埃斯塔加奇、奇姆帕帕帕和莫罗莫罗的村庄位于叶的 S 和 SE，部分被火山灰覆盖。公元 1600 年的 Huaynaputina 火山喷发创造了重要的地质和文化遗产，具有科学、教育和旅游价值。地质旅游景点是根据火山地质遗址、火山文化地貌遗址和温泉四组共 17 个地质遗址的识别、表征和定性评价提出的。提出了七个地质道路和七个视点，可以评估最相关的景观，