Parry (crater)

Last updated
Parry
Parry crater 4120 h3.jpg
Coordinates 7°54′S15°48′W / 7.9°S 15.8°W / -7.9; -15.8 Coordinates: 7°54′S15°48′W / 7.9°S 15.8°W / -7.9; -15.8
Diameter 48 km
Depth 0.6 km
Colongitude 16° at sunrise
Eponym Sir William Parry

Parry is a lunar impact crater that is attached to the southeast rim of the walled plain Fra Mauro. It was named after British explorer William Parry. [1] Attached to the west and southwest rim of Parry is the crater Bonpland. Due south of Parry is the small crater Tolansky, and farther to the south-southwest is Guericke.

Contents

The rim of Parry is heavily worn and slightly distorted due to the co-joined formations. The wall is the most prominent along the northwest, and crossed along the southwest by the small Parry B. The floor has been flooded by lava, and is relatively flat. At the midpoint is a pair of small craters.

A rille system, called the Rimae Parry, crosses the region in a series of graben. One rille crosses the southeast rim of Parry in a northeast direction before crossing the east rim and continuing a short distance across the surrounding mare. Another extends from Tolansky crater across the west side of Parry and into Fra Mauro crater. One other crosses the north rim of Bonpland crater and into Fra Mauro where it intersects with another rille.

Parry crater AS16-M-1685.jpg
A16PSR Figure29-8 bottom Parry crater cross section.png
A patch of the Cayley Formation occupies the bottom of Parry crater, with its surface in the form of a subdued depression. [2]

Satellite craters

Parry (top center) from Apollo 16 AS16-M-1685.jpg
Parry (top center) from Apollo 16

By convention these features are identified on lunar maps by placing the letter on the side of the crater midpoint that is closest to Parry.

ParryLatitudeLongitudeDiameter
B8.9° S13.0° W1 km
C6.8° S12.7° W3 km
D7.9° S15.7° W3 km
E8.3° S16.3° W6 km
F7.6° S14.7° W4 km
L6.3° S14.7° W7 km
M8.9° S14.5° W26 km

The following craters have been renamed by the IAU.

Related Research Articles

<span class="mw-page-title-main">Fra Mauro (crater)</span> Crater on the Moon

Fra Mauro is the worn remnant of a walled lunar plain. It is part of the surrounding Fra Mauro formation, being located to the northeast of Mare Cognitum and southeast of Mare Insularum. Attached to the southern rim are the co-joined craters Bonpland and Parry, which intrude into the formation forming inward-bulging walls. The crater is named after Italian geographer Fra Mauro.

<span class="mw-page-title-main">Sirsalis (crater)</span> Crater on the Moon

Sirsalis is a relatively young lunar impact crater located near the western lunar limb, to the southwest of the Oceanus Procellarum. The crater lies across a ridge that runs in a north–south direction. It has a sharp edge and a low central peak. The crater overlaps the slightly larger and older Sirsalis A to the west-southwest, and the two form a distinctive feature.

<span class="mw-page-title-main">Triesnecker (crater)</span> Crater on the Moon

Triesnecker is a prominent lunar impact crater that is located in the Sinus Medii, near the central part of the Moon's near side. Its diameter is 25 km. It was named after Austrian astronomer Franz de Paula Triesnecker. It is located to the north-northwest of the crater Rhaeticus, and to the east-southeast of the flooded Murchison.

<span class="mw-page-title-main">Ariadaeus (crater)</span> Crater on the Moon

Ariadaeus is a small, bowl-shaped lunar impact crater on the western shores of Mare Tranquillitatis. It lies to the north of the crater Dionysius, and to the west-southwest of Arago. The crater is joined along the northeast rim by the slightly smaller Ariadaeus A, and the two form a double-crater. Its diameter is 10.4 km.

<span class="mw-page-title-main">Bonpland (crater)</span> Lunar impact crater

Bonpland is the remains of a lunar impact crater that is attached to the walled plain Fra Mauro to the north and Parry to the east. The intersection of their rims forms a three-pointed mountainous rise. To the southeast is the small crater Tolansky. Bonpland lies on the eastern edge of Mare Cognitum. It is named after Aimé Bonpland, a French explorer and botanist.

<span class="mw-page-title-main">Boscovich (crater)</span> Crater on the Moon

Boscovich is a lunar impact crater that has been almost completely eroded away by subsequent impacts. It is located west-northwest of the crater Julius Caesar, and south-southeast of the prominent Manilius. The crater floor has a low albedo, and the dark hue makes it relatively easy to recognize. The surface is crossed by the rille system designated Rimae Boscovich that extends for a diameter of 40 kilometres. The crater is named after Croatian physicist Roger Joseph Boscovich.

<span class="mw-page-title-main">Cavendish (crater)</span> Lunar impact crater

Cavendish is a lunar impact crater that is located in the southwest part of the Moon, to the southwest of the larger crater Mersenius. It lies between the smaller craters Henry to the west-northwest and de Gasparis to the east-southeast.

<span class="mw-page-title-main">Goclenius (crater)</span> Crater on the Moon

Goclenius is a lunar impact crater that is located near the west edge of Mare Fecunditatis. It lies to the southeast of the lava-flooded crater Gutenberg, and north of Magelhaens. To the northwest is a parallel rille system that follow a course toward the northwest, running for a length of up to 240 kilometers. This feature is named the Rimae Goclenius.

<span class="mw-page-title-main">Guericke (crater)</span> Crater on the Moon

Guericke is the remnant of a lunar impact crater at the north part of the Mare Nubium. It is named after German scientist Otto von Guericke. To the north-northwest lies the large Fra Mauro crater, along with the co-joined craters Parry and Bonpland. To the east are the craters Kundt and Davy.

<span class="mw-page-title-main">Hippalus (crater)</span> Crater on the Moon

Hippalus is the remnant of a lunar impact crater on the eastern edge of Mare Humorum. It was named after ancient Greek explorer Hippalus. To the southeast is the crater Campanus, and to the northwest is the small flooded crater Loewy.

<span class="mw-page-title-main">Sosigenes (crater)</span> Lunar impact crater

Sosigenes is a lunar impact crater on the west edge of Mare Tranquillitatis. Its diameter is 17 km. It was named after ancient Greek astronomer Sosigenes of Alexandria. It lies to the east of the large walled plain Julius Caesar. The crater rim has a high albedo, making it relatively bright. It has a small central rise at the midpoint of the floor.

<span class="mw-page-title-main">De Vico (crater)</span> Crater on the Moon

De Vico is a small lunar impact crater that is located in the southwest part of the Moon, to the south of the crater Sirsalis. To the west-northwest is Crüger. De Vico is a circular, bowl-shaped formation with a small, flat bottom at the midpoint. To the northwest is the lava-flooded remains of De Vico T. Beyond is a linear rille designated Rimae Sirsalis that follows a path to the northeast past the rim of Sirsalis.

<span class="mw-page-title-main">Tolansky (crater)</span> Crater on the Moon

Tolansky is a small, circular lunar impact crater that is located due south of the crater Parry on the Mare Cognitum. The formation is symmetric, with a light-hued outer rim and a darker interior floor. A rille belonging to the Rimae Parry almost connects with the north-northwestern rim of Tolansky.

<span class="mw-page-title-main">Krieger (crater)</span> Lunar impact crater

Krieger is a lunar impact crater on the eastern part of the Oceanus Procellarum. It is located to the north-northwest of the flooded crater Prinz, and north-northeast of the prominent ray crater Aristarchus. To the northwest lies the small Wollaston.

<span class="mw-page-title-main">Campanus (crater)</span> Lunar impact crater

Campanus is a lunar impact crater that is located on the southwestern edge of Mare Nubium. It was named after Italian astronomer Campanus of Novara. It forms a crater pair with Mercator just to the southeast. Along the southern rampart of Campanus is the small lunar mare named Palus Epidemiarum. To the southwest is the small crater Dunthorne.

<span class="mw-page-title-main">Damoiseau (crater)</span> Lunar impact crater

Damoiseau is a lunar impact crater that is located just to the west of the Oceanus Procellarum, in the western part of the Moon's near side. It lies due east of the prominent crater Grimaldi, a walled plain with a distinctive dark floor. Due south of Damoiseau is the crater Sirsalis.

<span class="mw-page-title-main">Maclear (crater)</span> Crater on the Moon

Maclear is a lava-flooded crater on the northwest part of the Mare Tranquillitatis, a lunar mare in the eastern half of the Moon. Its diameter is 20 km. The crater is located to the southwest of the slightly larger Ross. To the southwest of Maclear is Sosigenes, while farther to the south-southeast is Arago.

<span class="mw-page-title-main">Dunthorne (crater)</span> Lunar impact crater

Dunthorne is a small lunar impact crater that is located to the northwest of the small lunar mare called Palus Epidemiarum, in the southwest part of the Moon's near side. It was named after British astronomer Richard Dunthorne. It lies to the southwest of the crater Campanus, east of Vitello. Due south is Ramsden.

<span class="mw-page-title-main">Galvani (crater)</span> Crater on the Moon

Galvani is a lunar impact crater that lies close to the northwestern limb of the Moon, due south of the larger walled plain Volta. It partly overlies the southeast rim of the crater Langley, which occupies half the gap between Volta and Galvani. To the northeast is the large walled plain Repsold, and to the west-southwest, on the far side of the Moon, is the crater McLaughlin.

Fontana is a lunar impact crater that is located in the southwestern part of the Moon's near side, to the south of the Oceanus Procellarum. It lies to the west-northwest of the flooded crater Zupus. Midway between Fontana and Zupus is a rille system designated Rimae Zupus.

References

  1. "Parry (crater)". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
  2. Apollo 16 Preliminary Science Report, NASA Special Publication 315, 1972. Chapter 29, part B: Cayley Formation interpreted as basin ejecta.