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

Volcano World discussion of different types of volcanoes