Volcano structure

The basic parts are the magma supply system (which may or may not include a magma chamber), the plumbing system that gets magma from the magma chamber to the surface, the layers of lava and/or ash, and perhaps a summit crater or caldera.

This cross-section shows the parts of a volcano. A conduit feeds magma to the surface. Near the surface, the gas expands and fragments the lava into ash. Some magma passes through dikes to feed vents. Some magma intrudes parallel to layers to make sills.

Volcanoes are constructed mainly of two materials: lava and ash. Both of these volcanic products come in many different variations and different volcanoes have different proportions of them. For example, shield volcanoes (such as those in Hawai'i and the Galapagos) are probably >95% lava and only ~5% ash (in the form of cinder). Furthermore, the basaltic lava that makes up shield volcanoes is very fluid and cannot be piled up into steep mounds. This is why shield volcanoes have very gradual slopes.

Another kind of volcano is called either a stratovolcano or composite-volcano. Mt. St. Helens, Pinatubo, and Fuji are all stratovolcanoes. Stratovolcanoes have a higher proportion of ash, and perhaps are up to 50/50 lava and ash. Ash is loose and can be piled up to slopes up to 30 degrees. Additionally, these stratovolcanoes erupt much more viscous lava than basalt, and this highly viscous lava doesn't flow very well (the Mt. St. Helens lava dome is an example of this lava). Because of the combination of viscous lava and ash, stratovolcanoes are much steeper than shield volcanoes.

Volcanoes grow by intrusion and extrusion. An intrusion is magma that moves up into a volcano and then it stops, never erupting. This way the volcano grows on the inside. An extrusion is an eruption. It can add layers of lava or ash. This way the volcano grows on the outside.