• Geophysics and Geophysical Exploration
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• v.9 no.1
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• pp.129-138
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• 2006

Helicopter-borne aeromagnetic surveys at two different times separated by three years were conducted to better understand the shallow subsurface structure of the Vulcano and Lipari volcanic complex, Aeolian Islands, southern Italy, and also to monitor the volcanic activity of the area. As there was no meaningful difference between the two magnetic datasets to imply an apparent change of the volcanic activity, the datasets were merged to produce an aeromagnetic map with wider coverage than was given by a single dataset. Apparent magnetisation intensity mapping was applied to terrain-corrected magnetic anomalies, and showed local magnetisation highs in and around Fossa Cone, suggesting heterogeneity of the cone. Magnetic modelling was conducted for three of those magnetisation highs. Each model implied the presence of concealed volcanic products overlain by pyroclastic rocks from the Fossa crater. The model for the Fossa crater area suggests a buried trachytic lava flow on the southern edge of the present crater. The magnetic model at Forgia Vecchia suggests that phreatic cones can be interpreted as resulting from a concealed eruptive centre, with thick latitic lavas that fill up Fossa Caldera. However, the distribution of lavas seems to be limited to a smaller area than was expected from drilling results. This can be explained partly by alteration of the lavas by intense hydrothermal activity, as seen at geothermal areas close to Porto Levante. The magnetic model at the north-eastern Fossa Cone implies that thick lavas accumulated as another eruption centre in the early stage of the activity of Fossa. Recent geoelectric surveys showed high-resistivity zones in the areas of the last two magnetic models.

• Korean Journal of Agricultural Science
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• v.5 no.2
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• pp.145-148
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• 1978

For the development of natural ornamental plants, an investigation was carried out about the vegetation of Soheuksan-do and Hong-do, islands located far in the southwestesn part of the Korean peninsular. The vegetation of Soheuksan-do was abundant. The dominant species were Machilus thunbergii, Buxus microphylla var. koreana, and Camellia japonica. Regarding the development of natural ornamental plants, 27 families and 54 species were reported in this investigation. Among these species there were 8 species including Calanthe discolor, Epipachs falcata, Dendrobium monniforme, Goodyera maximowiczii, and Lipari's krameri in Orchidaceae. The vegetation of Hong-do was similar to that of Soheuksan-do, but less abundant. Supplementary 10 species were reported in this investigation. Epipactis falcata and Dendrobium moniliforme were almost exterminated in these islands because of indiscriminating gathering. Therefore these species must be protected immediately.

• Journal of the Korean earth science society
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• v.39 no.6
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• pp.568-574
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• 2018

Microlite is crystallized under the supercooled condition of volcanic magma. This study reports the morphology and texture of microlites included in the obsidians from the Baekdusan (Mt. Baekdu), Kyushu (Japan), Hokkaido (Japan) and Lipari Island (Italy) by using a scanning electron microscope (SEM). Morphology and texture observed from the back scattered electron (BSE) image could give more detailed information on the microlite crystallization which cannot be acquired from the conventional optical microscope. Ten types of microlites are newly described according to the 14 morphological types of microlites by Clark (1961): Lath, Crenulite, Bacillite, Margarite, Belonites, Trichites, Arculites, Furculite, Scopulites, Scopulitic growth. Detailed description of the ten microlites can be used to interpret the crystallization and paragenetic relations of crystals during the cooling of acidic volcanic magma.