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Martian canals

Erroneous idea of canals on Mars

  • 10 min read
  • 4 chapters

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Through Canal, Optical illusion and Opposition (astronomy)

They were first described by the Italian astronomer Giovanni Schiaparelli during the opposition of 1877, and attested to by later observers. The Irish astronomer Charles E. Burton made some of the earliest drawings of straight-line features on Mars, although his drawings did not match Schiaparelli's. Around the turn of the century there was even speculation that they were engineering works, irrigation canals constructed by a civilization of intelligent aliens indigenous to Mars.

By the early 20th century, improved astronomical observations revealed that, with the possible exception of the natural canyon Valles Marineris, the "canals" were likely an optical illusions, and modern high-resolution mapping of the Martian surface by spacecraft supports this interpretation.

Despite the existence of Martian canals was eventually disproven by improved astronomical observations, Schiaparelli's reports of linear features on Mars had a profound and lasting influence on science fiction. His observations, together with the popular interpretation that these features were artificial waterways, inspired writers to imagine Mars as a world inhabited by intelligent beings and advanced civilizations. This vision was further developed and popularized by Percival Lowell, whose theories of a dying Martian civilization sustaining itself through vast irrigation canals captured the public imagination. As a result, the concept of canal-covered Mars became one of the defining images of the planet in literature, shaping works by authors such as H. G. Wells, Edgar Rice Burroughs, C. S. Lewis, and Robert A. Heinlein.

Supposed "discoveries"

The Italian word canale (plural canali) can mean "canal", "channel", "duct" or "gully". The first person to use the word canale in connection with Mars was Angelo Secchi in 1858, although he did not see any straight lines and applied the term to large features—for example, he used the name "Canale Atlantico" for what later came to be called Syrtis Major Planum.

On 5 September 1877, a perihelic opposition to Mars occurred. The Italian astronomer Giovanni Schiaparelli used a 22-centimetre (8.7 in) telescope in Milan to help produce the first detailed map of Mars. These maps notably contained features he called canali, which, with the possible exception of the natural canyon Valles Marineris, were later shown to be an optical illusion. These canali were supposedly long, straight lines on the surface of Mars, after both real and legendary rivers of various places on Earth, or the mythological underworld. He estimated that these canali were 75 kilometres (47 mi) in width, the smallest 75 kilometres (47 mi) in length and the widest was 3,000 kilometres (1,900 mi). His term, which means "channels" or "grooves", was popularly mistranslated in English as "canals".

Influenced by the observations, the orientalist Percival Lowell founded an observatory which had 30- and 45-centimetre (12- and 18-in) telescopes. The observatory was used for the exploration of Mars during the last good opportunity in 1894, and the following less favorable oppositions. He published several books on Mars and life on the planet, which had a great influence on the public. The canali were independently observed by other astronomers, such as Henri Joseph Perrotin and Louis Thollon in Nice, using one of the largest telescopes of that time.

The seasonal changes (consisting of the diminishing of the polar caps and the dark areas formed during Martian summers) in combination with the canals led to speculation about life on Mars, and it was a long-held belief that Mars contained vast seas and vegetation. As bigger telescopes were used, fewer long, straight canali were observed.

At this time in the late 19th century, the resolution of telescopes reached a level sufficient for surface features to be identified. Astronomers had to stare for hours through their telescopes, waiting for a moment of still air when the image was clear, and then draw a picture of what they had seen. Astronomers believed at the time that Mars had a relatively substantial atmosphere. They knew that the rotation period of Mars (the length of its day) was almost the same as Earth's, and they knew that Mars's axial tilt was also almost the same as Earth's, which meant it had seasons in the astronomical and meteorological sense. They could also see Mars's polar ice caps shrinking and growing with these changing seasons. The similarities with Earth led them to interpret darker albedo features (for instance Syrtis Major) on the lighter surface as oceans. By the late 1920s, however, it was known that Mars is very dry and has a very low atmospheric pressure.

In 1889, American astronomer Charles A. Young reported that Schiaparelli's canal discovery of 1877 had been confirmed in 1881, though new canals had appeared where there had not been any before, prompting "very important and perplexing" questions as to their origin.

During the favourable opposition of 1892, W. H. Pickering observed numerous small circular black spots occurring at every intersection or starting-point of the "canals". Many of these had been seen by Schiaparelli as larger dark patches, and were termed seas or lakes; but Pickering's observatory was at Arequipa, Peru, about 2,400 metres (7,900 ft) above the sea, and with such atmospheric conditions as were, in his opinion, equal to a doubling of telescopic aperture. They were soon detected by other observers.

During the oppositions of 1892 and 1894, seasonal color changes were reported. This was first interpreted as the melting of polar snows, leading to overflowing of adjacent seas which spread out as far as the tropics, assuming a distinctly green colour. However, in 1894, doubts arose as to whether there were any seas at all. Under the best conditions, these supposed 'seas' were seen to lose all trace of uniformity, their appearance being that of a mountainous terrain, broken by ridges, rifts, and canyons.

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