| 
      |  | 
      Terrestrial and extraterrestrial 
      volcanism:   |  | 
  
    | 
      |  | Large Igneous Provinces |  | 
  
    | 
      
    
    or LIPs are voluminous emplacements of predominantly mafic 
    extrusive and intrusive rock whose origins lie in processes other than 'normal' seafloor 
    spreading. LIPs include continental flood basalts and associated 
      intrusive rocks, volcanic passive margins, oceanic plateaus, 
    submarine ridges, seamount groups, and ocean basin flood basalts. Click on 
    this map of LIPs, shown below, to read about the research on LIPs.
 | 
  
    | 
      |  | 
      Notable LIPs on Land
 The 
    most notable of continental flood basalts and flood basalt provinces are:
   
        |  | 
    Columbia 
    River Basalts (~15 Ma), |  |  | 
    Ethiopian 
        Traps (~38 Na), |  |  | 
    Deccan Traps 
        (~65 Ma), |  |  | 
    Parana/Serra Geral 
        lavas (~135 Ma), |  |  | 
    Karoo/Stromberg, Patagonian 
        and Ferrar lavas (~180 Ma), |  |  | 
    Siberian 
        Traps (~250 Ma), and   |  |  | 
    Keweenawan Lavas 
        (~1,250 Ma).
 |  |  | 
    
     | 
  
    |    
    Explore Volcano World at the URL:
    
    http://volcano.und.nodak.edu/vw.html. Also available on-line,at
    
    http://adsbit.harvard.edu/books/bvtp/toc.html is 
    the treatise: Basaltic Volcanism on the 
    Terrestrial Planets. For extra-terrestrial volcanism, try the URL:
    
    
    
    http://pubs.usgs.gov/gip/volc/extraterrestrial.html | 
      |  | Other Kinds of Volcanism:
 
        |  | 
        
        Spreading Submarine Ridges:
 
    
        Spreading submarine ridges and rises (e.g., Reykjanes/ Mid-Atlantic Ridge, 
    East Pacific Rise, hydrothermal vents) and associated volcanic islands 
    (e.g., Iceland).
 |  |  | 
    
    Volcanism at the Subduction Zones 
    
    
    Convergent plate margins  have volcanism towards the edge of the plate 
    that is being subducted (e.g., Cascade Ranges and the Pacific “Ring of 
    Fire”)..
 
      |  |  | 
    'Hot 
    Spots' and Aseismic Ridges: 
      
    
    Intra-plate or “hot-spot” volcanism (e.g., Hawaii-Emperor Seamounts, 
    Yellowstone-Snake River volcanics) |  |  | 
  
    |  |  |  | 
  
    |  | The sketch alongside, taken from the URL: 
    
    
    http://vulcan.wr.usgs.gov/Glossary/Plate Tectonics/Maps/map_juan_de_fuca_subduction.html explains the entire 
    cycle of volcanism from Juan de Fuca Ridge to Juan de Fuca subduction (i.e., 
    the Filled Trench) and 
    the Cascades.
 | 
  
    |  |  |  | 
  
    |   
      |  | 
    Volcanic 
    materials/products and rock classification:
 
        |  | 
    
    Volcanic 
    Rocks: 
 Increasing 
    order of silica (SiO2) content,
 from silica-rich rhyolite at one end and the more common basalt at the 
    other, with the compositionally intermediate andesite 
    denoting crustal contamination of the
 magma on its passage through the 
    crust.
 |  |  
      
    
    
    Why 
    andesites on Mars, then? |  |  | 
  
    |  |  |  | 
  
    | 
      |  | 
    
    Other 
    products : 
      
        |  | 
    
    Cinder cones/ Pyroclastics (Ash, Cinders, Blocks/Bombs, Lahars) |  |  | 
    
    Gases and Gas Clouds: Nuees Ardentes, Toxics, Climate Change |  |  | 
    
    Other materials: Pyroclasts, Volcanic Breccia |  |  
      |  | 
      |  | Textures of Volcanic Rocks: 
 
        |  | Glassy (Obsidian), |  |  | Vesicular (Scoria, Pumice), |  |  | Aphanitic (Andesite, Basalt, 
    Rhyolite), |  |  | Porphyritic (Andesite Porphyry, Basalt Porphyry, and Rhyolite Porphyry). |  |  | 
  
    | 
    Visit the USGS volcanoe sites, starting 
    with
    
    http://volcanoes.usgs.gov/  
    and its links 
    Also try the site:
    
    http://interactive2.usgs.gov/learningweb/explorer/topic_rocks_igneous.htm | 
  
    |  | 
  
    |  |  |  | 
  
    | 
      |  | Volcanic Precursors and/or 
      Predictors? 
 
        |  | Seismicity 
    (Harmonic Tremors?) |  |  | Bulging or 
    Uptilting? |  |  | Exotic 
    Gas Emanations? |  |  | Volcanism and Climate 
    Try
    
    http://www.etl.noaa.gov/about/review/aq/post 
    for a comparison of the 
    climate effects of Mt. Pinatubo and El Chichon events. | 
  
    |   
      |  | 
    Is 
    Volcanism Predictable?
    
 |  
      | American Geophysical 
    Union has an interesting discussion of terrestrial degassing at the URL: 
    
    
    http://www.agu.org/sci_soc/eosvarekamp.html.
 Also try the URL:
    
    
    http://unr.edu/homepage/fbiondi/BiondiFessenden1999E.pdf | 
  
    |   
      
        | 
          |  | Try the following links for interesting presentations on the rock 
    cycle shown alongside: 
 |  |  |  |