Zobrazeno 1 - 6
of 6
pro vyhledávání: '"S. P. Jakobsson"'
Autor:
Anna Garavelli, S. P. Jakobsson, Tonči Balić-Žunić, A. Katerinopoulou, M. J. Jacobsen, Donatella Mitolo
Publikováno v:
Mineralogical Magazine. 78:215-222
The new mineral oskarssonite (IMA2012-088), with ideal formula AlF3, was found in August 2009 at the surface of fumaroles on the Eldfell volcano, Heimaey Island, Iceland (GPS coordinates 63°25′58.9″N 20°14′50.3″W). It occurs as sub-micron-s
Autor:
S. P. Jakobsson, G. L. Johnson
Publikováno v:
Bulletin of Volcanology. 74:1141-1160
The Western Volcanic Zone in Iceland (64.19° to 65.22° N) has the morphological characteristics of a distinct Mid-Atlantic ridge segment. This volcanic zone was mapped at a scale of 1:36.000, and 258 intraglacial monogenetic volcanoes from the Late
Autor:
S. P. Jakobsson, Donatella Mitolo, Pasquale Acquafredda, Anna Garavelli, Tonči Balić-Žunić, E. Leonardsen
Publikováno v:
Mineralogical Magazine. 74:147-157
Heklaite, with the ideal formula KNaSiF6, was found among fumarolic encrustations collected in 1992 on the Hekla volcano, Iceland. Heklaite forms a fine-grained mass of micron- to sub-micron-sized crystals intimately associated with malladrite, hiera
Publikováno v:
Mineralogical Magazine. 73:51-57
A new mineral, eldfellite, was found among fumarolic encrustations collected in 1990 on the Eldfell volcano, Heimaey Island, Iceland. Associated minerals are ralstonite, anhydrite, gypsum, bassanite, hematite, opal and tamarugite, as well as a presum
Publikováno v:
Nature. 243:213-214
THE Vestmannaeyjar archipelago has been the site of two recent volcanic eruptions (Fig. 1). The first was the Surtsey eruption from November 1963 to June 1967 and the second is the Heimaey eruption which began on January 23, 1973, and is still contin
Autor:
G. L. Johnson, S. P. Jakobsson
Publikováno v:
Journal of Geophysical Research. 90:10073
Geophysical and petrologic data are presented on the northern extent of the Reykjanes Ridge. As it nears Iceland the crest of the Reykjanes Ridge is a small belt of rough topography superimposed on an elevated plateau. The rough topography consists o