Mount Etna, the anatomy of a volcano
著者
書誌事項
Mount Etna, the anatomy of a volcano
Chapman and Hall, 1985
大学図書館所蔵 全17件
  青森
  岩手
  宮城
  秋田
  山形
  福島
  茨城
  栃木
  群馬
  埼玉
  千葉
  東京
  神奈川
  新潟
  富山
  石川
  福井
  山梨
  長野
  岐阜
  静岡
  愛知
  三重
  滋賀
  京都
  大阪
  兵庫
  奈良
  和歌山
  鳥取
  島根
  岡山
  広島
  山口
  徳島
  香川
  愛媛
  高知
  福岡
  佐賀
  長崎
  熊本
  大分
  宮崎
  鹿児島
  沖縄
  韓国
  中国
  タイ
  イギリス
  ドイツ
  スイス
  フランス
  ベルギー
  オランダ
  スウェーデン
  ノルウェー
  アメリカ
注記
Bibliography: p. [367]-388
Includes index
内容説明・目次
内容説明
Since the Second World War interest in the active by Italian geophysicists; studies of ground deform volcano Mount Etna, in Sicily, has been steadily ation by British and Italian groups; measurements increasing. This interest has not been restricted of microgravity changes particularly by a British to Italy, and scientists from Belgium, France, group; endeavours to improve analytical tech Germany, the United States and the United King niques for gases and sublimates by French and also dom have played a part in volcanological studies. Italian and British workers; pioneering work on In 1972 much of this work was drawn together at a rheology of lavas and growth of lava fields by discussion meeting convened by the Royal Society British scientists; and greatly improved surveil of London and attended by representatives of most lance of activity, notably that occurring in the summit region. of the projects that were being conducted on Etna. The meeting served to draw together current It is a principal aim of this book to synthesize the knowledge of Etna, especially information derived results of these many different studies into a more during the 1971 flank eruption, and also to point complete understanding of the volcano. Inevitably out deficiencies in knowledge and methods of the coverage is somewhat uneven; some fields of approach to investigating the volcano. In his study have been researched more thoroughly than opening statement to the meeting Professor A. others.
目次
1 The forge of Vulcan.- 1.1 The summit cone.- 1.2 Flank activity.- 1.3 Other activity.- 1.4 From myth to science.- 2 Etna and the Etna region.- 2.1 The physical environment.- 2.2 The human response.- 2.3 Concluding remarks.- 3 Geological setting and volcanic history.- 3.1 Volcanism and tectonics in the central Mediterranean.- 3.2 Geological setting of Mount Etna.- 3.3 Nomenclature of the lavas of Mount Etna.- 3.4 Stratigraphy.- 4 Volcanic processes and products.- 4.1 Explosive volcanism.- 4.2 Effusive activity.- 4.3 Collapse structures.- 5 The rheological behaviour of basaltic lavas.- 5.1 Rheological concepts and definitions.- 5.2 The rheological characteristics of suspensions.- 5.3 The rheological properties of basaltic fluids.- 5.4 Concluding comments.- 6 Petrology and magmatic processes.- 6.1 Isotope geochemistry.- 6.2 Basal tholeiitic volcanics.- 6.3 Paterno alkali olivine basalt.- 6.4 The alkalic series.- 6.5 Petrological variations in historic times.- 6.6 Volcanic gases.- 7 Internal plumbing.- 7.1 Conduits and magma chambers.- 7.2 Ground deformation.- 7.3 Seismic studies.- 7.4 Gravimetric measurements.- 7.5 Magma budget and ascent rate.- 7.6 Summary and discussion.- 8 Volcanic hazard on Etna.- 8.1 The sources of hazard on Mount Etna.- 8.2 Specific prediction and hazard assessment.- 8.3 The empirical determination of the relative vulnerabilities of Etnean districts.- 8.4 The manipulation of lava flows.- 9 Volcanic hazards: human response and adjustment.- 9.1 The conceptual framework.- 9.2 Mount Etna: hazard response and adjustment.- 9.3 Conclusion: prospects for the future.- References.- Note.- % (v/v) is equivalent to vol. %.- % (w/w) is equivalent to wt %.
「Nielsen BookData」 より