Question: Paricutin is what natural phenomenon that resulted in covering the town of San Juan Parangaricutiro?

full_context: Document 1: San Pedro Cholula: San Pedro Cholula is a municipality in the Mexican state of Puebla and one of two municipalities which made up the city of Cholula. The city has been divided into two sections since the pre Hispanic era, when revolting Toltec-Chichimecas pushed the formerly dominant Olmec-Xicallanca to the eastern side of the city in the 13th century. The new lords called themselves Cholutecas and built a new temple to Quetzalcoatl on the San Pedro side, which eventually eclipsed the formerly prominent Great Pyramid of Cholula, now on the San Andrés side. When the Spanish arrived in the 16th century, the city of Cholula was an important religious and economic center, but the center of power was on the San Pedro side, centered on what is now the main city plaza and the San Gabriel monastery. The division of the city persisted and San Pedro remained the more dominant, with Spanish families moving onto that side and the rest of the population quickly becoming mestizo. Today, San Pedro is still more commercial and less residential than neighboring San Andrés with most of its population employed in industry, commerce and services rather than agriculture. Although Cholula's main tourist attraction, the Pyramid, is in San Andrés, San Pedro has more tourism infrastructure such as hotels, restaurants and bars.
Document 2: San Miguel (volcano): San Miguel (also known as Volcán Chaparrastique) is a stratovolcano in central-eastern El Salvador, approximately 15 km southwest of the city of San Miguel. On January 16, 2002, a minor eruption of steam, gas, and ash occurred from the summit crater, lasting 3 hours but causing no real damage to life or property. Carbon dioxide emissions had been monitored since November 2001, and their steady increase continued to build up until the eruption.
Document 3: San Juan volcanic field: The San Juan volcanic field is part of the San Juan Mountains in southwestern Colorado. It consist mainly of volcanic rocks that form the largest remnant of a major composite volcanic field that covered most of the southern Rocky Mountains in the Middle Tertiary geologic time. Within the region lie an abundance of caldera volcanoes, which comprise the San Juan Volcanic Fields. There are approximately 15 calderas known in the San Juan Volcanic Fields; however, it is possible that there are 2, or even 3 more in the region.
Document 4: Pico de Orizaba: Pico de Orizaba, also known as Citlaltépetl (from Nahuatl "citlal(in)" = star, and "tepētl" = mountain), is a stratovolcano, the highest mountain in Mexico and the third highest in North America, after Denali (formerly known as Mount McKinley) of the United States and Mount Logan of Canada. It rises 5636 m above sea level in the eastern end of the Trans-Mexican Volcanic Belt, on the border between the states of Veracruz and Puebla. The volcano is currently dormant but not extinct, with the last eruption taking place during the 19th century. It is the second most prominent volcanic peak in the world after Africa's Mount Kilimanjaro.
Document 5: Pico Viejo: Pico Viejo is a volcano located on the island of Tenerife (Canary Islands, Spain). It is the second highest peak of Tenerife and the Canary Islands (after the Teide) with a height of 3,135 m above sea level, a huge crater approximately of 720 metres in diameter.
Document 6: Neo Chorio, Crete: Neo Chorio is located 25km (15.5 miles) southeast of Chania in the center of the Apokoronas province. It was named Neo ("new") Chorio because it was a new village, but it was built on the ruins of an old village which was destroyed during the raids in Crete. It is built on a stone hill on a plain that is crossed by the river Mantamas. Smaller rivers include: the Anavreti, the Koliakoudes, etc. According to tradition, the small town was originally settled in the Late Minoan era, on a site located in the northernmost part of the village where it still stands today. According to the census of 1881, the village had only 451 inhabitants. At the village square, there is a plane tree which is many centuries old. Under this tree, there is a famous well. The plane tree and the well have been there since the Venetian domination. In the past, water was supplied by the rivers Koliakoude and Mantama. Later, when the village was destroyed, the inhabitants moved south and people collected water from the Koliakoude river. Even today, there are still many wells and cisterns within the village, the most important of which is the well of Anavreti. Agios Thomas’s church is located in the village’s square and is a royal rhythm church. In the Turkish domination this church was used as a cemetery and a school. The Agios Gerasimos is a graphic little church which was built on a rock at the edge of the village going towards to Bryses. The Agios Therapontas church is Byzantine rhythm and was built in 1971. Today, the cemetery is located on a hill 100 meters high, located near the church of Koimisi tis Theotokou. During the Turkish domination, priests and nuns took on the role of teachers and secretly taught the Greek language to the children of the village. The only school in the village was built in 1900. The fort of Koule was built by the Turks to control the passage from Apokoronas to Keramia.
Document 7: Puʻu ʻŌʻō: Puʻ u ʻ Ōʻ ō (often written Puu Oo, ] ) is a volcanic cone in the eastern rift zone of the Kīlauea volcano of the Hawaiian Islands. Puʻ u ʻ Ōʻ ō has been erupting continuously since January 3, 1983, making it the longest-lived rift-zone eruption of the last two centuries.
Document 8: Tecuamburro: Tecuamburro is a stratovolcano in southern Guatemala, roughly 50 kilometres south east of Guatemala City. The Tecuamburro is an andesitic stratovolcano which formed approximately 38,000 years ago inside a horseshoe-shaped caldera formed by a structural failure in a second, 100,000-year-old stratovolcano, known as Miraflores. At the top of the Tecuamburro is an acidic crater lake around which many hot springs, fumaroles, and boiling mudpots are found.
Document 9: Nuevo San Juan Parangaricutiro: Nuevo San Juan Parangaricutiro, in the Mexican state of Michoacán, is a small village near the Parícutin volcano. The city is called "Nuevo" (Spanish for "New") because the original San Juan Parangaricutiro was destroyed during the formation of the Parícutin volcano in 1943. Along with the village of Parícutin, San Juan Parangaricutiro was buried beneath ash and lava. The tops of cathedrals in old San Juan Parangaricutiro still protrude from the volcanic deposits.
Document 10: Piton de la Fournaise: Piton de la Fournaise (French): "Peak of the Furnace" is a shield volcano on the eastern side of Réunion island (a French department) in the Indian Ocean. It is currently one of the most active volcanoes in the world, along with Kīlauea in the Hawaiian Islands (Pacific Ocean), Stromboli, Etna (Italy) and Mount Erebus in Antarctica. A previous eruption began in August 2006 and ended in January 2007. The volcano erupted again in February 2007, on 21 September 2008, on 9 December 2010, which lasted for two days. and on 1 August 2015. The most recent eruption began on 14 July 2017. The volcano is located within Réunion National Park, a World Heritage site.
Document 11: San Patricio, Jalisco: San Patricio - Melaque in the Mexican state of Jalisco is a busy community located 4+ kilometers northwest of Barra de Navidad on Bahia de Navidad. The area comprises two beachfront villages: San Patricio - Melaque and Villa Obregon all generally referred to as "Melaque." The small village of Melaque has been a vacation retreat for Mexicans for generations. San Patricio - Melaque, a kilometer long strip on the west end of the bay, is named after the Ejido San Patricio and before that a small Rancho named San Patricio. Downtown Melaque contains a colorful town square, many retail shops, two banks, many restaurants and a few hardware stores. Villa Obregon, to the east, is much more residential. The two areas of San Patricio - Melaque and Villa Obregon form the largest community along the coast between Puerto Vallarta and Cihuatlan. Playa Melaque is the main beach in the area and good for swimming, bodyboarding, and skimboarding. The west end of Melaque beach is protected from the large swells found elsewhere on the beach, allowing for swimming for children and the less adventurous.
Document 12: Mount Vesuvius: Mount Vesuvius ( ; Italian: "Monte Vesuvio" ] ; Neapolitan: "Vesuvio" ; Latin: "Mons Vesuvius" ] ; also "Vesevus " or "Vesaevus " in some Roman sources) is a somma-stratovolcano located on the Gulf of Naples in Campania, Italy, about 9 km east of Naples and a short distance from the shore. It is one of several volcanoes which form the Campanian volcanic arc. Vesuvius consists of a large cone partially encircled by the steep rim of a summit caldera caused by the collapse of an earlier and originally much higher structure.
Document 13: Villa de Guadalupe, Mexico City: Colonia Villa de Guadalupe (also known as La Villa de Guadalupe Hidalgo) is a former separate town, now a neighborhood in northern Mexico City which in 1531 was the site of the apparition of Our Lady of Guadalupe, the most renowned Marian apparition in the Americas. She can be venerated in the Our Lady of Guadalupe Shrine, located in the "villa" (town).
Document 14: Cotopaxi National Park: Cotopaxi National Park (Spanish: "Parque Nacional Cotopaxi" ) is a protected area in Ecuador situated in the Cotopaxi Province, Napo Province and Pichincha Province, roughly 50 km south of Quito. The Cotopaxi volcano (supposedly meaning smooth neck of the moon) that lends its name to the park is located within its boundaries, together with two others: the dormant Rumiñawi volcano to its north-west and the historical Sincholagua volcano (last major eruption: 1877) to the south east. Cotopaxi is among the highest active volcanoes in the world; its last significant eruption took place in 1904.
Document 15: Parícutin: Parícutin (or Volcán de Parícutin, also accented Paricutín) is a cinder cone volcano located in the Mexican state of Michoacán, near the city of Uruapan and about 322 km west of Mexico City. The volcano surged suddenly from the cornfield of local farmer Dionisio Pulido in 1943, attracting both popular and scientific attention.
ground_truth: a cinder cone volcano