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My Weigh T3 400 Triton T3 400 Gram x 0.01 Digital Pocket Scale Black

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Only 40% of Triton's surface has been observed and studied, but it may be entirely covered in such a thin sheet of nitrogen ice. Some maculae are simple dark spots with diffuse boundaries, and others comprise a dark central patch surrounded by a white halo with sharp boundaries. These observations indicated the presence of a denser atmosphere than was deduced from Voyager 2 data.

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During its 1989 flyby of Triton, Voyager 2 found surface temperatures of 38K (−235°C) and also discovered active geysers erupting sublimated nitrogen gas, contributing to a tenuous nitrogen atmosphere less than 1⁄ 70,000 the pressure of Earth's atmosphere at sea level. Impact craters [ edit ] Tuonela Planitia (left) and Ruach Planitia (center) are two of Triton's cryovolcanic "walled plains".Triton was discovered by British astronomer William Lassell on October 10, 1846, [17] just 17days after the discovery of Neptune. Triton's rotation is tidally locked to be synchronous with its orbit around Neptune: it keeps one face oriented toward the planet at all times. An early theory of how Triton may have been slowed was by collision with another object, either one that happened to be passing by Neptune (which is unlikely), or a moon or proto-moon in orbit around Neptune (which is more likely).

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All the geysers observed were located between 50° and 57°S, the part of Triton's surface close to the subsolar point.The Voyager 2 probe in 1989 observed a handful of geyser-like eruptions of nitrogen gas and entrained dust from beneath the surface of Triton in plumes up to 8km high.

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Surrounding this caldera is a volcanic dome that stretches for roughly 2,000km along its longest axis, indicating that Leviathan is the second largest volcano in the solar system by area, after Alba Mons. Because of its retrograde orbit and composition similar to Pluto, Triton is thought to have been a dwarf planet, captured from the Kuiper belt. The current understanding of moons in retrograde orbits means they cannot form in the same region of the solar nebula as the planets they orbit. Triton is the largest natural satellite of the planet Neptune, and was the first Neptunian moon to be discovered, on October 11, 1846, by English astronomer William Lassell. Capture [ edit ] The Kuiper belt (green), in the Solar System's outskirts, is where Triton is thought to have originated.All of them identified Triton as being a prime target and a separate Triton lander comparable to the Huygens probe for Titan was frequently included in those plans. Streaks on Triton's surface left by geyser plumes suggest that the troposphere is driven by seasonal winds capable of moving material over a micrometer in size. To be gravitationally captured by a planet, a passing body must lose sufficient energy to be slowed down to a speed less than that required to escape. Each eruption of a Triton geyser may last up to a year, driven by the sublimation of about 100millionm 3 (3.

My Weigh T3 400 Triton T3 400 Gram x 0.01 Digital Pocket

of nitrogen ice over this interval; dust entrained may be deposited up to 150km downwind in visible streaks, and perhaps much farther in more diffuse deposits. The best-observed examples are named Hili and Mahilani (after a Zulu water sprite and a Tongan sea spirit, respectively). The mostly darker region above it includes Triton's "cantaloupe terrain" and cryovolcanic and tectonic features. Tidal interactions also cause Triton's orbit, which is already closer to Neptune than the Moon is to Earth, to gradually decay further; predictions are that 3. Viscoelastic damping from tides alone is not thought to be capable of circularizing Triton's orbit in the time since the origin of the system, and gas drag from a prograde debris disc is likely to have played a substantial role.Between 1977 and the Voyager 2 flyby in 1989, Triton shifted from a reddish color, similar to Pluto, to a far paler hue, suggesting that lighter nitrogen frosts had covered older reddish material. These faults with parallel ridges expelled from the interior cross complex terrain with valleys in the equatorial region. Turbulence at Triton's surface creates a troposphere (a "weather region") rising to an altitude of 8km.

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