Dear Chuck, Steve, or Scott, I would like some information on volcanic activities for school.

rocky Noelle


Dear Noelle,

Here are few ideas. Explosive eruptions fragment the lava to make pyroclastic material (blocks, bombs, cinder, ash). This material tends to pile up close to the vent (some of it gets carried down wind). The slope of the flank of the volcano is related to the size of the volcanic material. Larger pieces have steeper slopes. Smaller pieces have gentler slopes. You might visit a local stone quarry and buy gravel and sand of different sizes. Ask you students to make piles of the different size materials and measure the angles of the slopes. Do they observe any correlation between particle size and slope angle? Do they think this would also be true for volcanoes? Repeat the experiment with any volcanic materials you can obtain (cinders or ash).

The shape of volcanoes that are made of lava flows is controlled (mostly) by the viscosity (stickiness) of the lava. Low viscosity (very fluid) lava travels far from the vent, making shield volcanoes like those in Hawaii. Higher viscosity (very sticky) lava cannot travel very far from the vent, making steep-sided volcanic domes like the one in inside Mount St.Helens.

Your students might experiment with fluids of different viscosity (perhaps cold molasses and cheap pancake syrup). Plan on them making a mess. Pour and equal volume on a gently sloping board and measure the distance they travel. Relate their observations back to types of volcanoes.

You might also look at the activities listed in The Teacher's Guide to the Geology of Hawaii Volcanoes National Park.

Steve Mattox, University of North Dakota


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