More from my deep read of Verne novels

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quentin skrabec

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Jan 26, 2024, 5:49:16 PMJan 26
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Verne Obscura et Trivia 5-

Journey to the Surface of the Earth- compass conundrums

By Quentin R. Skrabec Ph.D.

Island of Stromboli in the 19th century. by Unknown artist

 

            Most readers and movie makers focus on Verne’s descent to the earth's center, but it is the ascent to the surface that would augur geological research. Modern geology has settled on the molten core theory, but volcanic eruptions' exact nature and predictability remain an active research area.  Verne was a great collector of unusual scientific phenomena related to volcanos, which is still getting the attention of researchers. New research in seismographic detection is still dealing with some of Verne’s observations. For example, earthquakes and tremors that almost always precede eruptions, precise measurements of ground deformation that often accompany the rise of magma, changes in volcanic gas emissions, and changes in gravity and magnetic fields frozen in lava.

            Let us look at some phenomena in the ascent of Verne’s Journey to the Center of the Earth (1864). In chapter 42, Verne describes the following types of phenomena such as granite wall convulsions, earthquakes, jerky magma movement, periodic lulls, heat, boiling water, superheated steam, possible electromagnetic effects, compass spinning, sulfur, and finally, magnetic pole reversal. These volcanic observations were not well understood in 1863. Verne ends the novel with a research question: the mystery of pole reversal. However, the electromagnetic effects are currently the cutting edge of research for possible eruption prediction. Verne might not have had the answers, but he was asking the right questions.

            In 1863, there were several theories of the earth’s center and the nature of volcanos. Most widely held at the time was that of James Hutton (1726-1803) and Charles Lyell (1797 –1875)  of a  fiery core. The molten core geological theory was accepted by most after the 1830s. 1863 French science writer Louis Figuier (1819-1894) had popularized these theories. Verne certainly borrowed from Figuier on the natural history of the descent (see Breyer and Butcher), but the ascent focuses on volcanic theory and observations.

            Verne knew the latest geological theories well, but the molten center theory would not support a literary trip to the earth’s center. Verne used an earlier theory of Humprey Davy (1778- 1829), which allowed for a cool center and separate volcanic eruptions by a reaction of alkali minerals, water, and solid granite.  Verne placates his more astute readers by making Journey to the Center of the Earth a scientific and literary debate between the cool center theory (Davy) of Professor Lindenbrock and the fiery center theory (Lyell, etc.)) of his nephew Axel.

            The novel’s ascent combines questions, observations, and theory. Some of Verne’s descriptions fit the 1858 published observations of Sainte-Claire Deville of the volcanic eruptions of Stromboli (Verne’s location of the assent).  Verne’s literary observations of volcanic eruptions auger modern scientific observations and research efforts

            Electromagnetic observations of volcanic plumes have been described intermittently since at least the time of Pliny the Younger and the 79 AD eruption of Vesuvius. Although sometimes disregarded in the past as secondary effects, recent work suggests that the electrical properties of volcanic plumes reveal intrinsic and otherwise inaccessible parameters of explosive eruptions.                 

            The first scientific studies of electromagnetic effects, such as volcanic lightning and magnetic bursts, were also conducted at Mount Vesuvius by Professor Luigi Palmieri, who observed the eruptions of 1858, 1861, 1868, and 1872 from the Vesuvius Observatory. His daring (even reckless) observations of the1861 eruption were well-read throughout Europe. In the 1800s, many anecdotal observations of compass gyrations during volcanic activity led Palmieri to study them at his Vesuvius Observatory.

Palmieri used an adapted Peltier electrometer to help study magnetic and electrical fields before and during volcanic eruptions. Twenty years after Verne’s fictional journey, at Krakatoa in 1884, abnormal atmospheric and magnetic displays were observed, “compass needles rotated violently, and the barometer rose and fell many tenths of an inch in a minute.”

            Such anecdotal observations continue today.  Mt. St, Helena in 1982, a film crew was dropped by helicopter on St. Helens on May 23 (five days after its eruption) to document the destruction. Their compasses, however, spun in circles, and they quickly became lost.

            In the 1950s, on the Mihara volcano in Japan, a major scientific study on magnetic effects produced data on the inclination and declination of the magnetic fields. Although not diagnostic individually, these techniques, when used in combination at well-monitored volcanoes, have resulted in successful predictions. A successful forecast saved thousands of lives at Pinatubo volcano (Philippines) 1991.

            The USGS Volcano Hazards Program noted in 2023 that magnetic data can be used for low-cost volcano monitoring in various settings and environmental conditions.  ( see “Volcano Monitoring With Magnetic Measurements: A Simulation of Eruptions at Axial Seamount, Kilauea, Bardarbunga, and Mount Saint Helens” Joseph Biasi, Maurice Tivey, Bailey Fluegel, AGU, 2022). Scientists this decade hypothesize that it is caused by a natural geodynamo deep within the Earth. A boiling, molten metal mixture of iron and nickel constantly moves around a solid iron core, generating a magnetic field.

            Verne’s novel ending of finding the magnetic reversal of the compass has proved remarkably prophetic. In 1905, a French geologist discovered a lava field with iron within it that was magnetized in reverse. What should have been north was south. The geologist realized this could only be possible if Earth’s magnetic poles were reversed when the lava flowed. When it solidified, it preserved that reversed magnetic orientation. It took another 50 years for scientists to accept that Earth could change its polarity. In the 1970s, lava polarity was being used to help date ancient rock. Recent research has focused on using lava to predict and study the effects of the earth’s pole reversals. We are getting closer to fully understanding the reversed compass ending of Journey to the Center of the Earth.

 

 

 

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