Mount Burney

E1037395

Mount Burney is a remote stratovolcano in southern Chilean Patagonia, notable for its explosive eruptions and extensive tephra deposits that have influenced regional climate and ecosystems.

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Statements (47)

Predicate Object
instanceOf stratovolcano
volcano
accessibility difficult to access
climateZone cold oceanic climate
continent South America
country Chile
dominantRockType andesite
dacite
elevation 1758 m
about 5770 ft
eruptionStyle explosive
firstScientificStudies 20th century GENERATED
geologicalAge Quaternary
glaciation glacier-covered flanks
hasCrater summit crater lake
hasSignificantEruption Holocene explosive eruptions
hasSummitFeature ice-filled crater
hasTephraLayersIdentifiedIn Patagonian lakes
Patagonian peat bogs
hazard ash fall
lahars
pyroclastic density currents
impact distal ash layers in Antarctic ice cores
influences regional climate
regional ecosystems
isRemote true
lastEruptionPeriod Holocene
locatedIn Chilean Patagonia NERFINISHED
Magallanes Region NERFINISHED
locatedOn Taitao Peninsula NERFINISHED
monitoredBy Chilean geological and volcanological authorities
mountainRange Andes
namedAfter Burney NERFINISHED
nearbyFeature Patagonian icefields NERFINISHED
fjords of southern Chile
partOf Andean volcanic arc NERFINISHED
produces ash fall deposits
pyroclastic flows
tephra
region southern Chile NERFINISHED
relatedTo subduction of Nazca Plate beneath South American Plate
tectonicSetting Andean Southern Volcanic Zone margin NERFINISHED
tephraDispersal Argentine Patagonia NERFINISHED
southern Chile NERFINISHED
southern Patagonia
usedFor tephrochronology in southern South America
volcanoType stratovolcano

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.