Outlines of a mechanical theory of storms — Background and Themes

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Bassnett, Thomas, 1808- Project Gutenberg 2006
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Edition facts

Words: 78,793
Reading time: 343 min
Text sections: 9
This editorial note examines the structure and imagery in Bassnett's 1854 work, focusing on his mechanical theory of storms, lunar influence, and magnetic phenomena, using excerpts to trace his argumentative patterns and recurring motifs.
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Thomas Bassnett's Outlines of a Mechanical Theory of Storms (1854) opens with a bold claim: that storms obey a mechanical law tied to lunar influence, a proposition he defends by weaving together gravitation, ether, and magnetism. The book's structure is itself a kind of vortex, spiraling from first principles through specific storm records to magnetic anomalies. Bassnett repeatedly invokes the image of a "radial stream" striking a "circular current," a visual that recurs across sections to explain everything from wind shifts to compass declination. This note traces how the work's architecture and recurring figures—vortices, ethereal currents, and the moon's axis—shape its argument.

A System Built on Vortices

The book's opening section establishes a cosmological framework: the solar system began in a "primordial condition," and gravitation alone is insufficient—Bassnett posits an "ethereal medium" in motion that forms vortices. This is not a mere metaphor; he treats vortices as physical entities that displace the earth's axis under lunar influence. The structure here is deductive: first principles (the nature of ether, ponderosity of matter) lead to a "new principle developed," then to applications like Hutton's rain theory. Bassnett's prose moves from the abstract to the concrete, but the excerpts show he never fully defines the ether's properties—he asserts its motion and leaves details vague. The recurring phrase "medium of space" appears as a placeholder for an unobserved mechanism, a pattern that persists throughout.

Storm Narratives as Evidence

In the second section, Bassnett shifts to case studies: the "Milwaukie storm," "New York storm," "Ottawa storm," and "Liverpool storm." These are not described in narrative detail but are invoked as data points, each tied to a lunar position. The structure is list-like, almost tabular, with the storms named in a recurring order. Bassnett's method is to assert a correlation between moon phase and storm occurrence, but the excerpts offer no meteorological specifics—only the names and a reference to a "record of the weather." This pattern of naming without describing recurs, suggesting the storms function as rhetorical anchors rather than empirical proofs. The reader is left to infer the connection from the author's confidence alone.

Magnetic Deflection and the Cape Anomaly

The later excerpts turn to magnetism, where Bassnett's argument becomes most intricate. He claims the magnetic needle's daily variation—deflecting eastward in the morning in the northern hemisphere, westward in the southern—is "a positive demonstration" of his theory. The key image is the "radial stream" of solar heat striking the earth's circular currents, deflecting them. He then highlights Colonel Sabine's discovery of opposite deflections at the Cape of Good Hope during equinoxes, calling it "a still more capital feature." Bassnett explains this by the Cape's large magnetic declination (30° west) and the sun's changing declination. The structure here is layered: a general rule, then an exception that confirms the rule. His reasoning is geometric, relying on angles and latitudes, but the excerpts show he assumes the magnetic equator, not the geographical one, divides the hemispheres—a crucial and unproven premise.

Magnetic Storms and Unseen Forces

Bassnett introduces "magnetic storms" as irregular fluctuations caused by the moon's vortices passing over a location. He cites an example: on September 25, 1841, a magnetic storm was observed simultaneously in Toronto and at the Cape of Good Hope. Yet he immediately cautions that "the extent of these storms has been over estimated." This hedging reveals a tension in his structure: he needs large-scale phenomena to support his theory but also wants to limit their scope to fit his mechanical model. The recurring image of the vortex—a localized, rotating disturbance—serves both purposes. Bassnett's language here is tentative: the vortices' force "is proved to be of variable force," but whether due to "atmospheric conditions" or "increased activity of the ethereal medium" is "immaterial." This ambiguity is characteristic; he often asserts a mechanism without specifying its nature.

Bassnett's work is best approached as a system of analogies: vortices, currents, and streams are his building blocks, applied to weather, magnetism, and lunar motion alike. The excerpts reveal a writer who argues by assertion and geometric reasoning rather than by presenting raw data. Readers should attend to how he moves between scales—from the cosmic ether to a single storm—and note where he relies on unobserved entities. The book rewards those who trace its recurring images, but its claims remain speculative, grounded more in rhetorical structure than in empirical demonstration.

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