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Record #171390:

Rof Surtseyjar. Maelingar 1967-2002 og framtídharspá / Sveinn P. Jakobsson, Gudhmundur Gudhmundsson.

Title: Rof Surtseyjar. Maelingar 1967-2002 og framtídharspá / Sveinn P. Jakobsson, Gudhmundur Gudhmundsson.
Translated title: Erosion in Surtsey. Measurements 1967-2002 and prediction for future.
Author(s): Jakobsson, Sveinn P.
Gudhmundsson, Gudhmundur.
Date: 2003.
Language: Icelandic.
In: Náttúrufraedingurinn. (2003.), Vol. 71(3-4) (2003)
Abstract: Eruption was from November 1963 to May 1965. Tephra fell from air, making two craters. Basalt lava then flowed, building up shield 100 m thick. More lava erupted in 1966-7. Storms produce wave action and rapid sea cliff recession, especially of tephra, but also of lava. Hydrothermal activity in craters has created palagonite tuff, very resistant to erosion. Island size has halved since 1967, and will go rapidly until tuff core is reached. Simple conical model gave fair results.
Notes:

Náttúrufraedingurinn. Vol. 71(3-4) :138-144 (2003).

English summary p.143, English captions.

Keywords: 519.673 -- Modelling.
551.21 -- Volcanoes.
551.217 -- Volcanic products.
551.3.053 -- Geological erosion, corrosion and disintegration.
551.466 -- Waves and tides, marine.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*35) -- Iceland.
SPRI record no.: 171390

MARCXML

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100 1# ‡aJakobsson, Sveinn P.
242 10 ‡aErosion in Surtsey. Measurements 1967-2002 and prediction for future.‡yeng
245 10 ‡aRof Surtseyjar. Maelingar 1967-2002 og framtídharspá /‡cSveinn P. Jakobsson, Gudhmundur Gudhmundsson.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2003.
300 ## ‡ap. 138-144 :‡bill., diags., maps.
500 ## ‡aNáttúrufraedingurinn. Vol. 71(3-4) :138-144 (2003).
500 ## ‡aEnglish summary p.143, English captions.
520 3# ‡aEruption was from November 1963 to May 1965. Tephra fell from air, making two craters. Basalt lava then flowed, building up shield 100 m thick. More lava erupted in 1966-7. Storms produce wave action and rapid sea cliff recession, especially of tephra, but also of lava. Hydrothermal activity in craters has created palagonite tuff, very resistant to erosion. Island size has halved since 1967, and will go rapidly until tuff core is reached. Simple conical model gave fair results.
546 ## ‡aIn Icelandic.
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a551.21 -- Volcanoes.‡2udc
650 07 ‡a551.217 -- Volcanic products.‡2udc
650 07 ‡a551.3.053 -- Geological erosion, corrosion and disintegration.‡2udc
650 07 ‡a551.466 -- Waves and tides, marine.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*35) -- Iceland.‡2udc
700 1# ‡aGudhmundsson, Gudhmundur.
773 0# ‡7nnas ‡tNáttúrufraedingurinn. ‡gVol. 71(3-4) (2003) ‡wSPRI-14577
916 ## ‡a2005/10/18 -- JP
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221003 ‡bJP