Radiocarbon Dating Recent Volcanic Activity on Faial Island (Azores)
Issue Date
1995-01-01Keywords
Caldeira FormationFaial Island
Azores
Atlantic Ocean Islands
lithostratigraphy
tephrochronology
geologic hazards
volcanology
Holocene
volcanoes
igneous rocks
pyroclastics
volcanic rocks
volcanism
chronology
soils
organic compounds
organic materials
peat
organic residues
sediments
Cenozoic
Quaternary
wood
C 14
carbon
dates
isotopes
radioactive isotopes
absolute age
Metadata
Show full item recordCitation
Madeira, J., Monge Soares, A. M., Brum da Silveira, A., & Serralheiro, A. (1995). Radiocarbon dating recent volcanic activity on Faial Island (Azores). Radiocarbon, 37(2), 139-147.Journal
RadiocarbonAdditional Links
http://radiocarbon.webhost.uits.arizona.edu/Abstract
Recent fieldwork on the island of Faial (Azores) led to the establishment of a detailed volcanic stratigraphic sequence, which is composed of five main geological formations. One of them, the Caldeira Formation, comprising mainly pumice fall and flow deposits, was judged to be Holocene in age. Organic materials were found preserved in or below some of the pyroclastic deposits from this formation. Wood, charcoal, peat and soil samples were radiocarbon dated, permitting correlation of deposits from different sequences and the establishment of a chronological framework for the Caldeira volcanic activity. These materials yielded ages from ca. 10-1 ka BP. The average dormant interval in the Caldeira pyroclastic activity from 4-1 ka ago is ca. 400 yr, with eruptions approximately every 200-800 yr. This frequency of activity indicates that the Caldeira volcano is an active, dangerous structure that should be closely monitored.Type
Articletext
Language
enISSN
0033-8222ae974a485f413a2113503eed53cd6c53
10.1017/S0033822200030575
