The history of Mars observation is about the recorded history of observation of the planet Mars. Some of the early records of Mars' observation date back to the era of the ancient Egyptian astronomers in the 2nd millennium BCE. Chinese records about the motions of Mars appeared before the founding of the Zhou dynasty (1045 BCE). Detailed observations of the position of Mars were made by Babylonian astronomers who developed arithmetic techniques to predict the future position of the planet. The ancient Greek philosophers and Hellenistic astronomers developed a geocentric model to explain the planet's motions. Measurements of Mars' angular diameter can be found in ancient Greek and Indian texts. In the 16th century, Nicolaus Copernicus proposed a heliocentric model for the Solar System in which the planets follow circular orbits about the Sun. This was revised by Johannes Kepler, yielding an elliptic orbit for Mars that more accurately fitted the observational data.
The first telescopic observation of Mars was by Galileo Galilei in 1610. Within a century, astronomers discovered distinct albedo features on the planet, including the dark patch Syrtis Major Planum and polar ice caps. They were able to determine the planet's rotation period and axial tilt. These observations were primarily made during the time intervals when the planet was located in opposition to the Sun, at which points Mars made its closest approaches to the Earth.
Better telescopes developed early in the 19th century allowed permanent Martian albedo features to be mapped in detail. The first crude map of Mars was published in 1840, followed by more refined maps from 1877 onward. When astronomers mistakenly thought they had detected the spectroscopic signature of water in the Martian atmosphere, the idea of life on Mars became popularized among the public. Percival Lowell believed he could see a network of artificial canals on Mars.[1] These linear features later proved to be an optical illusion, and the atmosphere was found to be too thin to support an Earth-like environment.
Yellow clouds on Mars have been observed since the 1870s, which Eugène M. Antoniadi suggested were windblown sand or dust. During the 1920s, the range of Martian surface temperature was measured; it ranged from −85 to 7 °C (−121 to 45 °F). The planetary atmosphere was found to be arid with only trace amounts of oxygen and water. In 1947, Gerard Kuiper showed that the thin Martian atmosphere contained extensive carbon dioxide; roughly double the quantity found in Earth's atmosphere. The first standard nomenclature for Mars albedo features was adopted in 1960 by the International Astronomical Union. Since the 1960s, multiple robotic spacecraft have been sent to explore Mars from orbit and the surface. The planet has remained under observation by ground and space-based instruments across a broad range of the electromagnetic spectrum.The discovery of meteorites on Earth that originated on Mars has allowed laboratory examination of the chemical conditions on the planet.
^Dunlap, David W. (October 1, 2015). "Life on Mars? You Read It Here First". New York Times. Retrieved October 1, 2015.
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The HistoryofMars may be HistoryofMarsobservation Geological historyofMars This disambiguation page lists articles associated with the title History...
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cratered terrain in southern highlands – this terrain observation is known as the Martian dichotomy. Mars hosts many enormous extinct volcanoes (the tallest...
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1997). "Appendix 1: Oppositions ofMars, 1901–2035". The Planet Mars: A HistoryofObservation and Discovery. University of Arizona Press. Archived from...
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الصفراء) HistoryofMarsobservation F.; Martin, Leonard J. (1971). "The developing stages of the Martian yellow storm of 1971". Bulletin of the Lowell...
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geology ofMars is the scientific study of the surface, crust, and interior of the planet Mars. It emphasizes the composition, structure, history, and physical...
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observed the comet travel by Mercury, Mars, and the sun as well. After this discovery, Tycho Brahe created a new model of the Universe – a hybrid between the...
The atmosphere ofMars is the layer of gases surrounding Mars. It is primarily composed of carbon dioxide (95%), molecular nitrogen (2.85%), and argon...