Statements (56)
| Predicate | Object |
|---|---|
| gptkbp:instance_of |
gptkb:volcano
|
| gptkbp:affects |
on agriculture in surrounding areas
|
| gptkbp:apparent_magnitude |
VEI 6
|
| gptkbp:ash_plume |
reached the stratosphere
|
| gptkbp:ashfall |
affected areas in Luzon
|
| gptkbp:ashfall_effects |
damaged infrastructure and agriculture
|
| gptkbp:ashfall_monitoring |
implemented during and after eruption
|
| gptkbp:ashfall_thickness |
up to 30 cm in some areas
|
| gptkbp:casualties |
around 800 deaths
|
| gptkbp:climate |
used to study eruption's effects on climate
|
| gptkbp:collaborations |
involved multiple international agencies
|
| gptkbp:colors |
up to 35 kilometers
|
| gptkbp:community_involvement |
tested by the eruption's aftermath
|
| gptkbp:cultural_significance |
important event in Philippine history
|
| gptkbp:date |
June 15, 1991
|
| gptkbp:displacement |
caused significant displacement of local communities
|
| gptkbp:emergency_exits |
approximately 200,000 people
established around the volcano |
| gptkbp:environmental_impact |
significant ash deposits in surrounding regions
|
| gptkbp:evacuation_success |
considered successful due to prior warnings
|
| gptkbp:followed_by |
lahars
|
| gptkbp:geological_features |
andesite
part of the Zambales Mountains |
| gptkbp:geological_formation |
conducted to assess damage
helped understand subduction zone volcanism |
| gptkbp:global_temperature_effect |
temporary cooling
|
| gptkbp:historical_context |
last major eruption before 1991 was in 1905
|
| https://www.w3.org/2000/01/rdf-schema#label |
Mount Pinatubo eruption
|
| gptkbp:impact |
climate change
|
| gptkbp:international_response |
aid provided by various countries
|
| gptkbp:lahar_formation |
triggered by heavy rains post-eruption
|
| gptkbp:last_eruption |
several days
sulfur dioxide conducted by USGS dispersed globally improved after the eruption monitored for years after eruption |
| gptkbp:location |
gptkb:Philippines
|
| gptkbp:pre-eruption_activity |
earthquakes
|
| gptkbp:publications |
numerous studies published post-eruption
|
| gptkbp:pyroclastic_flows |
generated during eruption
|
| gptkbp:research |
conducted on eruption's effects
|
| gptkbp:research_importance |
important for understanding volcanic eruptions
|
| gptkbp:significance |
one of the largest eruptions of the 20th century
|
| gptkbp:team |
ongoing for years after eruption
|
| gptkbp:tourism_impact |
affected local tourism industry
|
| gptkbp:type |
stratovolcano eruption
|
| gptkbp:volcanic_alert_level |
raised to level 5 before eruption
|
| gptkbp:volcanic_ash_composition |
rich in minerals
|
| gptkbp:volcanic_eruption_classification |
classified as a Plinian eruption
|
| gptkbp:volcanic_eruption_frequency |
historically eruptions occur every few hundred years.
|
| gptkbp:volcanic_history |
has been active for thousands of years
|
| gptkbp:volcanic_lightning |
observed during eruption
|
| gptkbp:bfsParent |
gptkb:Operation_Pinatubo
gptkb:Clark_Air_Base |
| gptkbp:bfsLayer |
6
|