Matches in DBpedia 2016-04 for { ?s ?p "Fueguino, also known as Cook, is a cluster of lava domes and pyroclastic cones located on Cook Island, Tierra del Fuego, Chile. This volcanic group lies south of the Magallanes–Fagnano Fault, on the Scotia Plate. This volcanic system has erupted relatively silicic hornblende andesites and dacites with SiO2 contents of 59-66% and it is not considered to be a source of Holocene tephra in Tierra del Fuego unlike other volcanoes such as Mount Hudson and Monte Burney."@en }
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- Fueguino abstract "Fueguino, also known as Cook, is a cluster of lava domes and pyroclastic cones located on Cook Island, Tierra del Fuego, Chile. This volcanic group lies south of the Magallanes–Fagnano Fault, on the Scotia Plate. This volcanic system has erupted relatively silicic hornblende andesites and dacites with SiO2 contents of 59-66% and it is not considered to be a source of Holocene tephra in Tierra del Fuego unlike other volcanoes such as Mount Hudson and Monte Burney.".
- Q3090546 abstract "Fueguino, also known as Cook, is a cluster of lava domes and pyroclastic cones located on Cook Island, Tierra del Fuego, Chile. This volcanic group lies south of the Magallanes–Fagnano Fault, on the Scotia Plate. This volcanic system has erupted relatively silicic hornblende andesites and dacites with SiO2 contents of 59-66% and it is not considered to be a source of Holocene tephra in Tierra del Fuego unlike other volcanoes such as Mount Hudson and Monte Burney.".
- Fueguino comment "Fueguino, also known as Cook, is a cluster of lava domes and pyroclastic cones located on Cook Island, Tierra del Fuego, Chile. This volcanic group lies south of the Magallanes–Fagnano Fault, on the Scotia Plate. This volcanic system has erupted relatively silicic hornblende andesites and dacites with SiO2 contents of 59-66% and it is not considered to be a source of Holocene tephra in Tierra del Fuego unlike other volcanoes such as Mount Hudson and Monte Burney.".
- Q3090546 comment "Fueguino, also known as Cook, is a cluster of lava domes and pyroclastic cones located on Cook Island, Tierra del Fuego, Chile. This volcanic group lies south of the Magallanes–Fagnano Fault, on the Scotia Plate. This volcanic system has erupted relatively silicic hornblende andesites and dacites with SiO2 contents of 59-66% and it is not considered to be a source of Holocene tephra in Tierra del Fuego unlike other volcanoes such as Mount Hudson and Monte Burney.".