Agglutinate in North Jan Mayen
By: Hawkins, T.R.W
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Contributor(s): Roberts, B.
Material type: 
ArticleDescription: 156-163pp ; Illustration.Subject(s): Agglutinate deposit - Jan Mayen - Norway | Beerenberg volcano - Jan Mayen - North Atlantic ocean
In:
Geological magazine : Vol. 100 Iss. 1-6 Year. 1963Summary: Abstract
In North Jan Mayen agglutinate is recognized as an important and widespread pyroclastic deposit of recent parasitic activity associated with the Beerenberg volcano. Lips of agglutinate along fissures, areas up to one square kilometre composed entirely of agglutinate, and other smaller morphological features are described. It is proposed to term the more widespread areas of agglutinate, “agglutinate fields,”, owing to their superficial resemblance to aa lava fields. Two varieties of agglutinate, one composed mainly of pancakes and bombs and the other of driblets of ankaramitic basaltic material are described, and conclusions given on their significance and formation.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode |
|---|---|---|---|---|---|---|
Article
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Library and Information Centre Periodical Section | Bound Journal Collection | Not for loan | 002548_19 | ||
Serials/Scientific Journal
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Library and Information Centre Periodical Section | Bound Journal Collection | 550 GEO (Browse shelf) | Available | 002548 |
Abstract
In North Jan Mayen agglutinate is recognized as an important and widespread pyroclastic deposit of recent parasitic activity associated with the Beerenberg volcano. Lips of agglutinate along fissures, areas up to one square kilometre composed entirely of agglutinate, and other smaller morphological features are described. It is proposed to term the more widespread areas of agglutinate, “agglutinate fields,”, owing to their superficial resemblance to aa lava fields. Two varieties of agglutinate, one composed mainly of pancakes and bombs and the other of driblets of ankaramitic basaltic material are described, and conclusions given on their significance and formation.
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