The Kilauea eruption in Hawaii has been making
headlines recently, with hundreds of residents displaced on the Big Island.
Let’s take a look at what’s happening there and why.
Volcanoes are vents into the center of the earth.
Liquid hot magma in the mantle is forced upward to the crust by pressure. Once
in a while, the pressure is great enough to force the magma out of the ground.
We call it a volcanic eruption, and change the magma’s name to lava. Not all
eruptions produce lava; in many cases gases and rocks are thrown from the
volcano. Such was the case at Mount St. Helens in 1980 and 2004. This
particular eruption isn’t even centered on the volcano’s summit crater. While
there have been steam, ash, and rocks erupting from the summit crater, there
hasn’t been a lava eruption there yet. Much of the lava is spewing from
fissures, cracks that have opened in the ground.
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Kilauea summit crater, May 9, 2018 (USGS) |
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Fissure eruption, Jan 3, 1983 (USGS) |
Most of the world’s active volcanoes are at the edges
of tectonic plates. To understand the concept of plates as they relate to
volcanic activity, imagine the crust is thin pieces of rocks fit together and
floating on top of the liquid magma mantle. The plates fit together but not
tightly enough to keep some of the magma from oozing to the surface. In some
areas, one plate is sliding underneath another. An example is the Juan de Fuca
plate sliding under the North American plate in the Pacific Northwest. This
action created the volcanoes of the Cascade Range. In other areas, the plates
are pulling away from each other, as in the Mid-Atlantic Rift. The Eurasian and
North American plates are separating, and the material coming forth from the
seafloor is what gave us Iceland.
Hawaii is in the
middle of the Pacific Ocean, thousands of miles from the edge of the Pacific
plate. Why the volcanic activity then? Hawaii sits on top of a hot spot. The
hot spot is a leak in the ocean crust. The Big Island is the newest in the
Hawaiian chain, and still growing as we can see. The hot spot has been leaking
magma into lava for millions of years. The spot remains in place, while the
plate slides along above it. That’s why Hawaii is a series of islands. The
plate is moving to the northwest, so the islands are oriented from northwest to
southeast. The current situation in Hawaii is even happening on the southeast
side of the island. As time goes by, activity at Kilauea will cease and a new
island will rise southeast of Hawaii.
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