Categorized | Featured, Sci-Tech, Volcano

Volcano Watch: What is a volcano?

During a kona wind, fume from Pu‘u ‘Ō‘ō (foreground) and Halema‘uma‘u  Crater (background), both on Kīlauea, blows northward, with towering Mauna Loa and Mauna Kea on the horizon. USGS photo.

During a kona wind, fume from Pu‘u ‘Ō‘ō (foreground) and Halema‘uma‘u Crater (background), both on Kīlauea, blows northward, with towering Mauna Loa and Mauna Kea on the horizon. USGS photo.

(Volcano Watch is a weekly article written by scientists at the U.S. Geological Survey’s Hawaiian Volcano Observatory.)

Many readers know that the Island of Hawai‘i is made of five volcanoes—Kīlauea, Mauna Loa, Hualālai, Mauna Kea, and Kohala. Those same readers know that such obvious features as the cones that dot Mauna Kea, the Hāla‘i Hills and Kūlani Cone on Mauna Loa, and Kapoho Cone, Pu‘u ‘Ō‘ō, and Mauna Ulu on Kīlauea are places where eruptions took place. If that’s the case, then why aren’t they called volcanoes? Isn’t a volcano a place where lava reaches the surface of the earth? Why doesn’t the island have hundreds of volcanoes instead of only five?

In one dictionary definition, a volcano is a vent or opening in the earth’s crust through which rock or lava is ejected. In another, a volcano is a cone-shaped hill or mountain built around a vent. Most volcanologists disagree with both of these definitions.

To a volcanologist, a volcano is a structure containing a vent or cluster of vents fed by magma rising directly from great depth within the earth, generally more than 30 km (18 mi) and in Hawai‘i about 100 km (60 mi). Each of the five volcanoes on the Island of Hawai‘i has such a deeply rooted feeder conduit.

In contrast, all of the cones mentioned above, and most others on the island, are supplied by magma that branched off the main conduit at a shallow depth, probably less than 10 km (6 mi) deep and more likely, less than half that. These cones are analogous to limbs on a tree, and the deeply rooted volcano is equivalent to the trunk of the tree.

If we could plug the deep conduit to Kīlauea, the entire volcano, including Pu‘u ‘Ō‘ō, would die. In reality, however, Kīlauea will remain active long after Pu‘u ‘Ō‘ō stops erupting, because the main feeder conduit will still be intact.

Several terms are used to describe the vents that lack deep roots and get their magma from the main feeder conduit—flank vents, parasitic vents, and rift vents. Sometimes “cone” is substituted for “vent.” So, for example, on Mauna Loa, Kūlani Cone could be termed a flank vent and the Hāla‘i Hills parasitic cones. Pu‘u ‘Ō‘ō is an active flank or rift vent on Kīlauea.

Physical appearance cannot be used to make the distinction between a volcano and a subsidiary vent on that volcano. Lacking geophysical evidence, it would be nearly impossible to know, for example, that Pu‘u ‘Ō‘ō is fed from shallow, not great, depth. With that evidence, though, a clear distinction can be made.

The second dictionary definition of “volcano”—a cone-shaped hill or mountain built around a vent—does not account for volcanoes such as Kīlauea, whose shape is far from that of a cone. Another type of volcano lacking a cone shape is a large caldera, such as Long Valley in eastern California or Yellowstone in Wyoming. No one would guess, without doing some geologic sleuthing, that these wide shallow depressions are volcanoes.

Visitors to Hawai‘i Volcanoes National Park often remark that Kīlauea Crater (the official name of the summit caldera) “sure doesn’t look like a volcano.” Even visitors trained in geology make that comment, because the image of Mount Fuji in Japan or Mayon in the Philippines is strongly entrenched as the stereotype of a “real” volcano.

Had these visitors come to the summit of Kīlauea in 1400 CE, however, they would have seen a lava shield rather than a caldera. The caldera formed by collapse of the shield about 100 years later.

This illustrates another point about volcanoes—the shape can change drastically and quickly, and one year’s cone or shield can be next year’s caldera. So, shape is an unimportant and even misleading basis for defining a volcano.

Finally, the distinction between a caldera, such as Kīlauea’s, and a crater, such as Halema‘uma‘u, is both arbitrary and meaningful. A caldera is a depression more than 1.6 km (1 mi) in diameter, and a crater is smaller. Pretty arbitrary! A more important distinction is that a Hawaiian caldera forms by collapse of the volcano’s summit and has deep roots, whereas a crater, no matter where it forms, has shallow roots. In a perfect world, the term Kīlauea Crater on maps would be replaced by Kīlauea Caldera.

3 Responses to “Volcano Watch: What is a volcano?”

  1. Irma Dunne says:

    Correction… Mayon is in the Phillipines, not in Indonesia.

  2. Just note that Mayon is in the Philippines, not in Indonesia!

  3. Baron says:

    Mahalo sharp readers. Corrected!

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