Bandelier Tuff

Summary

Bandelier Tuff is a geological formation^[1]. It ranks in the top 8% of geological_formation entities by monthly Wikipedia readership (4 views/month).^[2]

Key Facts

• Bandelier Tuff is located in New Mexico^[3].
• Bandelier Tuff is in the country of United States^[4].
• Bandelier Tuff's image is recorded as Bandelier Formation.jpg^[5].
• Bandelier Tuff's instance of is recorded as geological formation^[6].
• Bandelier National Monument is named after Bandelier Tuff^[7].
• Bandelier Tuff's made from material is recorded as ignimbrite^[8].
• Bandelier Tuff's coordinate location is recorded as {'globe': 'http://www.wikidata.org/entity/Q2', 'altitude': None, 'latitude': 35.763888888888886, 'longitude': -106.32194444444444, 'precision': 0.0002777777777777778}^[9].
• Bandelier Tuff's has cause is recorded as Valles Caldera^[10].
• Bandelier Tuff's elevation above sea level is recorded as {'unit': 'http://www.wikidata.org/entity/Q11573', 'amount': '+2030'}^[11].
• Bandelier Tuff's Google Knowledge Graph ID is recorded as /g/11j66cd535^[12].
• Bandelier Tuff's named by is recorded as Harold Smith^[13].
• Bandelier Tuff's model item is recorded as Kwage Mesa^[14].

Why It Matters

Bandelier Tuff ranks in the top 8% of geological_formation entities by monthly Wikipedia readership (4 views/month).^[2]