F2-2 Felsic Lava
The 1980 explosive eruption of Mount St. Helens.

Felsic lava is lava that it is highly viscous; it is very “thick” and does not flow easily. Felsic lava also has a very high gas content. When pressure is released, the high gas content (typically water vapor and carbon dioxide) results in a violent explosion. This is what happened in the 1980 eruption of Mt. St. Helens in Washington state (see graphic to the right). This violent explosion resulting from a release of pressure is very similar to the foaming that can occur in a carbonated soft drink when the container is opened and the pressure is released. Felsic lava is common in continental crust, and is high in silica content. Lassen Peak in northern California is a typical example of a mountain formed by felsic lava. Granite is an example of a common rock formed by felsic lava.