TYPE OF VOLCANIC FEATURE |
TYPE OF ERUPTION |
TYPE OF MAGMA |
PLATE-TECTONIC SETTING |
Shield volcano, e.g. Mauna Loa, Kilauea |
non-explosive, flowing lava, may have lava
fountains |
Basaltic; pahoehoe or aa lava |
Hot spot, ocean floor |
Flood basalt or plateau basalt, e.g. Iceland, Columbia
Plateau |
fissure eruptions on land, lava flowing over
broad areas |
Basaltic |
Hot spot (early stage of development) |
Cinder cone, e.g. Paricutin, Mexico; Sunset
Crater, Arizona; Cerro Negro, Nicaragua |
pyroclastic but not necessarily explosive;
often occur in groups or "swarms"; may be associated with larger volcanoes but
cinder cones are smaller than other volcanoes |
Basaltic to andesitic; even if basaltic, magma
is cooler and more viscous than examples listed above |
Generally on land, various settings; may be
associated with areas of incipient continental rifting and uplift, or with last phase of
activity in a region of basaltic flows |
Pillow basalt |
underwater eruption |
Basaltic |
mid-ocean ridge or hot spot |
Stratovolcano or composite volcano, e.g. Pinatubo,
Mt. St. Helens,
Krakatoa, Katmai |
explosive, with large amounts of ash,
pyroclastic flows, some lava flows |
Andesitic |
convergent boundary, created by partial melting
of oceanic lithosphere in subduction zone |
Caldera, e.g. Taal, Crater Lake,
Kilauea and Mauna Loa summit calderas |
varies, but generally occurs by collapse of
surface above depleted magma chamber |
Basaltic, andesitic or rhyolitic; the largest
ones are associated with rhyolitic magmas |
various |
Large rhyolite caldera complexes, e.g. Yellowstone
(click here
for more); Long
Valley Caldera, California (click here
for more) |
highly explosive, huge volumes of pyroclastic
debris - world's larges eruptions (none in recorded human history, luckily for us!) |
Rhyolite or dacite, forming ignimbrites
and welded tuffs |
Continental location above hot spot, rift zone
or subduction zone, caused by partial melting of continental crust in contact with
basaltic or andesitic magma rising from the mantle |