A NASA handout photo taken on April 8, 2009 shows the 3,776-meter-high Mount Fuji Volcano on the island of Honshu in Japan, It is one of the world�s classic examples of a stratovolcano. The volcano�s steep, conical profile is the result of numerous layers of lava and debris from explosive eruptions, including ash, cinders, and volcanic bombs, that built up over time. The steep profile is possible because of the relatively high viscosity (stickiness) of the lava typically associated with stratovolcanoes. The high viscosity leads to thick sequences of lava flows near the eruptive vent that build the cone structure.