Astrophysicists believe it might have originated in the Kuiper belt, [13] a ring of small icy objects extending from just inside the orbit of Neptune to about 50 AU from the Sun. To help get you started with the tritone scale, here's a fun little lick I came up with using the C tritone scale over the C7 chord in this ii-V-I-vi chord progression in F major. Although commonly termed "cryovolcanic", this nitrogen plume activity is distinct from Triton's larger-scale cryovolcanic eruptions, as well as volcanic processes on other worlds, which are powered by internal heat.

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At present, Triton's rotational axis is about 40° from Neptune's orbital plane, and hence as Neptune orbits the Sun, Triton's polar regions take turns facing the Sun, resulting in seasonal changes as one pole, then the other moves into the sunlight. The surface shows deposits of tholins, organic chemical compounds that may be precursors to the origin of life.

Lassell did not name his discovery; he later successfully suggested the name Hyperion, previously chosen by John Herschel, for the eighth moon of Saturn when he discovered it. Triton has a tenuous nitrogen atmosphere, with trace amounts of carbon monoxide and small amounts of methane near its surface. 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. These observations indicated Triton was approaching an unusually warm southern hemisphere summer season that happens only once every few hundred years.

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Triton's revolution around Neptune has become a nearly perfect circle with an eccentricity of almost zero. Triton is the seventh-largest moon and sixteenth-largest object in the Solar System and is modestly larger than the dwarf planets Pluto and Eris.As the probe was only able to study about 40% of the moon's surface, future missions (dubbed "Trident") have been proposed to NASA via their Discovery Program to revisit the Neptune system with a focus on Triton; and its subsurface ocean. Some maculae are simple dark spots with diffuse boundaries, and others comprise a dark central patch surrounded by a white halo with sharp boundaries. Check out these fingerings, one off of the sixth string and one from the fifth-string root, and see how they lay under your fingers and if they sit comfortably for you as well.

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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. Triton is unique among all large moons in the Solar System for its retrograde orbit around its planet (i. Triton is thus, along with Earth, Io, Europa and Enceladus, one of the few bodies in the Solar System on which active eruptions of some sort have been observed. 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).Fifty-five percent of Triton's surface is covered with frozen nitrogen, with water ice comprising 15–35% and frozen CO 2 forming the remaining 10–20%. Most of the outer irregular moons of Jupiter and Saturn also have retrograde orbits, as do some of Uranus's outer moons. Triton's initially eccentric orbit would have intersected the orbits of irregular moons and disrupted those of smaller regular moons, dispersing them through gravitational interactions. Triton's western hemisphere consists of a strange series of fissures and depressions known as "cantaloupe terrain" because it resembles the skin of a cantaloupe melon.

Triton Inference Server | NVIDIA Developer Triton Inference Server | NVIDIA Developer

The 40% of Triton's surface imaged by Voyager 2 revealed blocky outcrops, ridges, troughs, furrows, hollows, plateaus, icy plains and a few craters. All the geysers observed were located between 50° and 57°S, the part of Triton's surface close to the subsolar point.The eruption of volatiles from Triton's equator and their deposition at the poles may redistribute enough mass over 10,000 years to cause polar wander. Water, the most abundant volatile in the Solar System, comprises Triton's mantle, enveloping a core of rock and metal. The depressions ( cavi) are probably not impact craters because they are all of the similar size and have smooth curves. In the 1990s, various observations from Earth were made of the limb of Triton using the occultation of nearby stars, which indicated the presence of an atmosphere and an exotic surface.