Nawish (crater)

Last updated
Nawish
PIA19065-Ceres-DwarfPlanet-Dawn-OpNav9-image1-20150523.jpg
Ezinu (top) and Nawish (bottom)
Location Ceres
Coordinates 18°17′N193°47′E / 18.28°N 193.79°E / 18.28; 193.79 Coordinates: 18°17′N193°47′E / 18.28°N 193.79°E / 18.28; 193.79 [1]
Diameter77 kilometres (48 mi)
Peak1 kilometre (0.62 mi) [2]
Naming Acoma guardian of the field

Nawish is a crater on Ceres. It is named after the Acoma guardian of the field. [1]

Ezinu and Nawish craters in context Ezinu and Nawish craters in context.jpg
Ezinu and Nawish craters in context

Related Research Articles

<span class="mw-page-title-main">Asteroid</span> Natural objects within Jupiters orbit

An asteroid is a minor planet of the inner Solar System. Sizes and shapes of asteroids vary significantly, ranging from 1-meter rocks to a dwarf planet almost 1000 km in diameter; they are rocky, metallic or icy bodies with no atmosphere.

<span class="mw-page-title-main">4 Vesta</span> Second largest asteroid of the main asteroid belt

Vesta is one of the largest objects in the asteroid belt, with a mean diameter of 525 kilometres (326 mi). It was discovered by the German astronomer Heinrich Wilhelm Matthias Olbers on 29 March 1807 and is named after Vesta, the virgin goddess of home and hearth from Roman mythology.

<span class="mw-page-title-main">2 Pallas</span> Large asteroid of the main asteroid belt; 2nd largest known asteroid

Pallas is the second asteroid to have been discovered, after Ceres. It is believed to have a mineral composition similar to carbonaceous chondrite meteorites, like Ceres, though significantly less hydrated than Ceres. It is the third-largest asteroid in the Solar System by both volume and mass, and is a likely remnant protoplanet. It is 79% the mass of Vesta and 22% the mass of Ceres, constituting an estimated 7% of the mass of the asteroid belt. Its estimated volume is equivalent to a sphere 507 to 515 kilometers in diameter, 90–95% the volume of Vesta.

<i>Dawn</i> (spacecraft) NASA mission to study main-belt asteroids via a robotic probe (2007-18)

Dawn is a retired space probe that was launched by NASA in September 2007 with the mission of studying two of the three known protoplanets of the asteroid belt: Vesta and Ceres. In the fulfillment of that mission—the ninth in NASA's Discovery Program—Dawn entered orbit around Vesta on July 16, 2011, and completed a 14-month survey mission before leaving for Ceres in late 2012. It entered orbit around Ceres on March 6, 2015. In 2017, NASA announced that the planned nine-year mission would be extended until the probe's hydrazine fuel supply was depleted. On November 1, 2018, NASA announced that Dawn had depleted its hydrazine, and the mission was ended. The spacecraft is currently in a derelict, but stable, orbit around Ceres.

<span class="mw-page-title-main">Stickney (crater)</span> Largest crater on Phobos

Stickney is the largest crater on Phobos, which is a satellite of Mars. It is 9 km (5.6 mi) in diameter, taking up a substantial proportion of the moon's surface.

<span class="mw-page-title-main">Cryovolcano</span> Type of volcano that erupts volatiles such as water, ammonia or methane, instead of molten rock

A cryovolcano is a type of volcano that erupts volatiles such as water, ammonia or methane into an extremely cold environment that is at or below their freezing point. The process of formation is known as cryovolcanism. Collectively referred to as cryomagma, cryolava or ice-volcanic melt, these substances are usually liquids and can form plumes, but can also be in vapour form. After the eruption, cryomagma is expected to condense to a solid form when exposed to the very low surrounding temperature. Cryovolcanoes may potentially form on icy moons and other objects with abundant water past the Solar System's snow line. A number of features have been identified as possible cryovolcanoes on Pluto, Titan and Ceres, and a subset of domes on Europa may have cryovolcanic origins. In addition, although they are not known to form volcanoes, ice geysers have been observed on Enceladus and potentially Triton.

<span class="mw-page-title-main">Crater chain</span> Line of craters along the surface of an astronomical body

A crater chain is a line of craters along the surface of an astronomical body. The descriptor term for crater chains is catena, plural catenae, as specified by the International Astronomical Union's rules on planetary nomenclature.

<span class="mw-page-title-main">Ceres (dwarf planet)</span> Dwarf planet in the asteroid belt

Ceres is a dwarf planet in the asteroid belt between the orbits of Mars and Jupiter. It was the first asteroid discovered, on 1 January 1801, by Giuseppe Piazzi at Palermo Astronomical Observatory in Sicily and announced as a new planet. Ceres was later classified as an asteroid and then a dwarf planet – the only one always inside Neptune's orbit.

<span class="mw-page-title-main">Dwarf planet</span> Small planetary-mass object

A dwarf planet is a small planetary-mass object that is in direct orbit of the Sun, smaller than any of the eight classical planets but still a world in its own right. The prototypical dwarf planet is Pluto. The interest of dwarf planets to planetary geologists is that they may be geologically active bodies, an expectation that was borne out in 2015 by the Dawn mission to Ceres and the New Horizons mission to Pluto.

<span class="mw-page-title-main">Permanently shadowed crater</span> Permanently shadowed region of a body in the Solar System

A permanently shadowed crater is a depression on a body in the Solar System within which lies a point that is always in darkness.

<span class="mw-page-title-main">Bright spots on Ceres</span> Surface features discovered 2015

Several bright surface features were discovered on the dwarf planet Ceres by the Dawn spacecraft in 2015.

<span class="mw-page-title-main">Occator (crater)</span>

Occator is an impact crater located on Ceres, the largest object in the main asteroid belt that lies between the orbits of Mars and Jupiter, that contains "Spot 5", the brightest of the bright spots observed by the Dawn spacecraft. It was known as "Region A" in ground-based images taken by the W. M. Keck Observatory on Mauna Kea.

<span class="mw-page-title-main">Kerwan (crater)</span>

Kerwan is the largest confirmed crater and one of the largest geological features on Ceres. It was discovered on February 19, 2015 from Dawn images as it approached Ceres. The crater is distinctly shallow for its size, and lacks a central peak. A central peak might have been destroyed by a 15-kilometer-wide crater at the center of Kerwan. The crater is likely to be young relative to the rest of Ceres's surface, as Kerwan has largely obliterated the cratering in the southern part of Vendimia Planitia.

<span class="mw-page-title-main">Haulani (crater)</span>

Haulani is an impact crater located on Ceres that contains "Spot 1", one of the bright spots observed by the Dawn spacecraft. The crater was named after Haulani, the Hawaiian goddess of plants. In July 2018, NASA released a comparison of physical features, including Haulani crater, found on Ceres with similar ones present on Earth.

<span class="mw-page-title-main">Dantu (crater)</span>

Dantu is a large crater on Ceres, located within the Vendimia Planitia. It is rimmed by a number of minor faculae, which together form Bright Spot 2.

<span class="mw-page-title-main">Geology of Ceres</span>

The geology of Ceres consists of the characteristics of the surface, the crust and the interior of the dwarf planet Ceres. The surface of Ceres is comparable to the surfaces of Saturn's moons Rhea and Tethys, and Uranus's moons Umbriel and Oberon.

<span class="mw-page-title-main">Achita (crater)</span>

Achita is a large crater on Ceres.

<span class="mw-page-title-main">Oxo (crater)</span>

Oxo is a small impact crater on the dwarf planet Ceres, located in Ceres' northern hemisphere. It is the second-brightest feature on Ceres. The crater was named after the Candomblé god of agriculture.

References

  1. 1 2 "Planetary Names: Crater, craters: Nawish on Ceres". USGS . Gazeteer of Planetary Nomenclature. 3 July 2015. Retrieved 25 August 2015.
  2. Frigeri, Alessandro; et al. (December 2018). "The geology of the Nawish quadrangle of Ceres: The rim of an ancient basin". Icarus . Elsevier. 316: 114–127. doi:10.1016/j.icarus.2018.08.015. S2CID   135182579 . Retrieved 10 October 2022.