MODELING AN ACTIVE (!!) EXPLOSIVE VOLCANO
Molly F. Miller and Thomas
Nashville, TN 37235
Level: Grades 3 - 6
Estimated time required: 30 minutes
Anticipated Learning Outcomes
This activity is an active simulation of an explosive volcanic eruption. The "volcano" (a plastic 35 mm film cannister) erupts (the lid blows off) when gas pressure generated by dissolving alka seltzer is sufficiently high. It is realistic in that the timing of the eruption is difficult to predict precisely and in that the eruption occurs when the pressure of the gas exceeds the confining pressure of the lid. The experiment can be modified to show that an eruption will not occur if there is not enough gas pressure generated (small piece of alka seltzer) or if gas is allowed to escape gradually through holes punched in lid of film cannister.
Not all volcanoes erupt explosively and unpredictably. The eruptive style (quiet streams of lava versus violent blasts of gases, ash, and debris) and eruption frequency and predictability are related to the viscosity (its resistance to flow) and amount of dissolved gas in the magma. (Magma = lava prior to eruption). Hot, runny magmas with little dissolved gas tend to flow smoothly out of vents and produce a volcano that is broad and not steep, such as the Hawaiian volcanoes.
On the other hand, slightly cooler magma with a higher dissolved gas content is much more viscous. Instead of running out smoothly, the magma may ooze out like toothpaste, clogging the vent. These volcanoes are steeper and have the typical "volcano shape" of famous volcanoes such as Mt. Fuji in Japan. Under this type of volcano, gases dissolved in magma can separate as the pressure decreases as the magma rises closer to the Earth's surface. If the gases separate rapidly and cannot escape immediately, they can build up pressure greater than that of the overlying rock. When this happens, they break the rock suddenly as a violent explosion occurs sending a plume of gas and ash upwards to heights as great as 20 miles. Commonly there is little if any lava extruded. The ejecta may consist primarily of ash, pumice (instantaneously cooled magma containing abundant trapped air), and debris blown off the volcano by the eruption. The force of the eruption can blast material tens of miles from the volcano, causing extensive loss of life and damage. It may take thousands of years for sufficient pressure to build to cause an eruption, and it is difficult to predict when a volcano that has long been dormant will become active. If the pressure were released gradually it would not build up to the point where it could cause an explosive eruption. Because they erupt infrequently, unpredictably, and violently, and because they occur in populated areas (e.g. Japan, Indonesia, Philippines, Pacific northwest of the United States, Central and South America), these explosive volcanoes pose the greatest danger to humans.
Results and Discussion
Repeat each experiment several times. Using a second hand on a clock, time how long it takes the lid to blow off with the half tablet. Measure the distance that the lid goes. Data from several groups can be pooled, tabulated, and histograms made.
Older students could research the eruptive history of a particular volcano, the effects it has had on humankind, and its potential for future destruction. Some famous volcanoes: Kilauea and Mauna Loa (both "nonviolent" volcanoes on the island of Hawaii), Mt. Vesuvius, Mt. Pinatubo (erupted 1991), Mt. Rainier, Mt. Lassen, Mt. St. Helens, Tambora, Krakatoa, El Chichon, Nevado del Ruiz (erupted 1985 causing 23,000 deaths in Columbia). Locate these volcanoes on a world map (geography) and have students discover some dramatic story or event for their assigned volcano.
Watch "Volcano!", 1988, National Geographic video (58 min.). It is sobering for students to learn that the volcanologists featured on the video, the Kraffts, a French husband and wife team, were killed in the 1991 eruption of Unzen in Japan.
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