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- Eruption_column abstract "An eruption column consists of hot volcanic ash emitted during an explosive volcanic eruption. The ash forms a column rising many kilometres into the air above the peak of the volcano. In the most explosive eruptions, the eruption column may rise over 40 km, penetrating the stratosphere. Stratospheric injection of aerosols by volcanoes is a major cause of short-term climate change.A common occurrence in explosive eruptions is for column collapse to occur. In this case, the eruption column is too dense to be lifted high into the air by air convection, and instead falls down the flanks of the volcano to form a pyroclastic flow or surge. On some occasions, if ash weren't dense enough to fall, they may create pyrocumulonimbus.".
- Eruption_column thumbnail Pinatubo_ash_plume_910612.jpg?width=300.
- Eruption_column wikiPageExternalLink 30410914-052_caption.html.
- Eruption_column wikiPageExternalLink contents.html.
- Eruption_column wikiPageExternalLink framework.html.
- Eruption_column wikiPageExternalLink nature07866.pdf.
- Eruption_column wikiPageID "1533051".
- Eruption_column wikiPageRevisionID "581773608".
- Eruption_column hasPhotoCollection Eruption_column.
- Eruption_column subject Category:Volcanoes.
- Eruption_column type Abstraction100002137.
- Eruption_column type AmorphousShape113867492.
- Eruption_column type Attribute100024264.
- Eruption_column type Crack109258715.
- Eruption_column type Location100027167.
- Eruption_column type Object100002684.
- Eruption_column type Opening109379111.
- Eruption_column type PhysicalEntity100001930.
- Eruption_column type Shape100027807.
- Eruption_column type Space113910384.
- Eruption_column type Vent109470550.
- Eruption_column type Volcanoes.
- Eruption_column type YagoGeoEntity.
- Eruption_column type YagoLegalActorGeo.
- Eruption_column type YagoPermanentlyLocatedEntity.
- Eruption_column comment "An eruption column consists of hot volcanic ash emitted during an explosive volcanic eruption. The ash forms a column rising many kilometres into the air above the peak of the volcano. In the most explosive eruptions, the eruption column may rise over 40 km, penetrating the stratosphere. Stratospheric injection of aerosols by volcanoes is a major cause of short-term climate change.A common occurrence in explosive eruptions is for column collapse to occur.".
- Eruption_column label "Colonna eruttiva".
- Eruption_column label "Columna eruptiva".
- Eruption_column label "Eruption column".
- Eruption_column label "Eruptionssäule".
- Eruption_column label "Panache volcanique".
- Eruption_column label "Pluma vulcânica".
- Eruption_column label "Uitbarstingskolom".
- Eruption_column sameAs Eruptionssäule.
- Eruption_column sameAs Columna_eruptiva.
- Eruption_column sameAs Panache_volcanique.
- Eruption_column sameAs Colonna_eruttiva.
- Eruption_column sameAs Uitbarstingskolom.
- Eruption_column sameAs Pluma_vulcânica.
- Eruption_column sameAs m.058n4c.
- Eruption_column sameAs Q1362572.
- Eruption_column sameAs Q1362572.
- Eruption_column sameAs Eruption_column.
- Eruption_column wasDerivedFrom Eruption_column?oldid=581773608.
- Eruption_column depiction Pinatubo_ash_plume_910612.jpg.
- Eruption_column isPrimaryTopicOf Eruption_column.
