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[[Image:Tumulus.jpg|thumb|300px|Tumulus about 30 m in diameter on the Hilina Pali road on the south flank of Kilauea Volcano, Hawai`i.]]The surfaces of [[pahoehoe]] flows on flat or gentle slopes often exhibit elliptical, domed structures called '''tumuli'''. A tumulus is created when the upward pressure of slow-moving molten [[lava]] within a flow swells or pushes the overlying crust upward. Since the solid crust is brittle, it usually breaks to accommodate the "inflating" core of the flow. Such fractures generally extend along the length of a tumulus, and are frequently accompanied by smaller irregular cracks down the sides. Lava commonly squeezes out through these fractures, and sometimes drains from the tumulus to leave a hollow shell.<ref>http://volcanoes.usgs.gov/Products/Pglossary/tumulus.html</ref>

[[Image:Tumulus.jpg|thumb|300px|Tumulus about 30 m in diameter on the Hilina Pali road on the south flank of Kilauea Volcano, Hawai`i.]]The surfaces of [[pahoehoe]] flows on flat or gentle slopes often exhibit elliptical, domed structures called '''tumuli'''. A tumulus is created when the upward pressure of slow-moving molten [[lava]] within a flow swells or pushes the overlying crust upward. Since the solid crust is brittle, it usually breaks to accommodate the "inflating" core of the flow. Such fractures generally extend along the length of a tumulus, and are frequently accompanied by smaller irregular cracks down the sides. Lava commonly squeezes out through these fractures, and sometimes drains from the tumulus to leave a hollow shell.<ref>http://volcanoes.usgs.gov/Products/Pglossary/tumulus.html</ref>