event · evt_hekla_3
Hekla 3 Eruption
A VEI 5 eruption produced the H3 tephra around 1100 ±50 BCE.
What is the evidence?
observed evidence
- H3 tephra
- Calibrated radiocarbon dating
- Volcanic deposits
proposed causes
consequences
The eruption and broad date are established; Mediterranean climatic impact and tighter dating remain uncertain.
Inspect the sources →Review and provenance
Specialist reviewer: not recorded. Review date: not recorded.
Dataset workflow: reviewed for v0.1. This is separate from specialist review.
Recorded dataset maintenance date: 2026-08-11.
Confidence describes the stated assessment; it does not certify expert approval. How review works.
Chronology
Dating intervals may describe uncertainty or phases; their width alone does not establish event duration.
1150 BCE–1050 BCE
Precision: calibrated radiocarbon range
hightephrochronology and calibrated radiocarbon
- informs · establishes
Hekla: Eruptive History, H3 Tephra Entry — Smithsonian Institution Global Volcanism Program
Locator: H3 eruptive entry
Event context
Properties and assignments
A label’s definition and the evidence for assigning it here are separate.
Likely Unrelated to the Initial c.1200 BCE Crisis
Chronology or mechanism makes the event an unlikely initiator of the main collapse-period developments, though later effects may remain possible.
Why does this record have this property?
The currently preferred Hekla 3 date is too late to initiate most destructions and political failures clustered around the turn of the twelfth century BCE.
Evidence and sources
- informs · establishes
Hekla: Eruptive History, H3 Tephra Entry — Smithsonian Institution Global Volcanism ProgramSource relationship recorded for Hekla 3 Eruption.
Locator: H3 eruptive entry
Referenced records
- Iceland · entity
- Hekla · entity
- Smithsonian GVP Hekla 3 chronology · chronology model