2229
Author
Baillie, M.
Title Of Article Chaper
Hekla 3: how big was it?
Title Of Journal Book
Endeavour. New series
Volume
13
Pages
78-81
Collation
color plates, fig.
Reference Bibliography
refs.
ISSN
0160-9327
Language Of Text
English
Literature Type
Serial
Literature Level
Analytic
Abstract
The eruption of Hekla, Iceland, at about 1150 BC and consequent climatic worsening is detectable through Greenland ice-cores, the bristlecone pine sequence, and the Irish oak sequence. The construction of Haughey's Fort, Armagh, at about this time also supports evidence of scarce resources. Numerous catastrophic or violent events from the Caspian Sea to Norway also center on this period. Questions nonetheless remain: do the tree rings merely provide an anchor-date to which approximately dated events can be manipulated, and was Hekla 3 the sole cause of climatic worsening in mid-12th century? All the disciplines need to refine their dating.
Keywords
volcanic eruption;bristlecone pine;oak;dendrochronology; Iceland (Hekla); Greenland;ice cores;climate;dating
pub_id
2229