shield volcanoes are found at divergent boundaries
they are low with gentle sloping sides
they are formed by eruptions of thin, runny lava
eruptions tend to be frequent but relatively gentle
composite volcanoes formed of sticky (viscous) acidic lava, ash and cinders
found at convergent boundaries
e.g. Mt St Helens in the USA
composite volcanoes may have several cones rather than just a single cone
supervolcanoes erupts 1000km³ of material
forms depression called caldera
has a ridge of higher land around it
erupts rarely, eruptions hundreds of thousands years apart