List of maria on the Moon

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This is a list of maria (large, dark, basaltic plains) on the Moon. It includes other basaltic plains, including the one oceanus as well as features known by the names lacus, palus and sinus. The modern system of lunar nomenclature was introduced in 1651 by Giovanni Battista Riccioli. [1] Riccioli's map of the Moon was drawn by Francesco Maria Grimaldi, who has a crater named after him.

Contents

Moon photo with maria and large impact craters labeled Topography of the Moon - Moon Craters and Seas.png
Moon photo with maria and large impact craters labeled
1882 chart of the moon with maria Astronomy for the use of schools and academies (1882) (14577550018).jpg
1882 chart of the moon with maria

Maria and Oceanus

Lunar Maria
Latin NameEnglish NameLat.Long.Diameter (km)
Mare Anguis Serpent Sea22.6° N67.7° E150
Mare Australe Southern Sea38.9° S93.0° E603
Mare Cognitum Sea of Knowledge10.0° S23.1° W376
Mare Crisium Sea of Crises17.0° N59.1° E418
Mare Fecunditatis Sea of Fecundity7.8° S51.3° E909
Mare Frigoris Sea of Cold56.0° N1.4° E1596
Mare Humboldtianum Sea of Alexander von Humboldt 56.8° N81.5° E273
Mare Humorum Sea of Moisture or Humors 24.4° S38.6° W389
Mare Imbrium [2] Sea of Showers32.8° N15.6° W1123
Mare Ingenii Sea of Cleverness33.7° S163.5° E318
Mare Insularum Sea of Islands7.5° N30.9° W513
Mare Marginis Sea of the Edge13.3° N86.1° E420
Mare Moscoviense Sea of Moscow 27.3° N147.9° E277
Mare Nectaris Sea of Nectar15.2° S35.5° E333
Mare Nubium Sea of Clouds21.3° S16.6° W715
Mare Orientale Eastern Sea19.4° S92.8° W327
Mare Serenitatis Sea of Serenity28.0° N17.5° E707
Mare Smythii Smyth's Sea1.3° N87.5° E373
Mare Spumans Foaming Sea1.1° N65.1° E139
Mare Tranquillitatis Sea of Tranquility8.5° N31.4° E873
Mare Undarum Sea of Waves6.8° N68.4° E243
Mare Vaporum Sea of Vapors13.3° N3.6° E245
Oceanus Procellarum Ocean of Storms18.4° N57.4° W2568

There was also a region on the Lunar farside that was briefly misidentified as a mare and named Mare Desiderii (Sea of Desire). It is no longer recognized. Other former maria include:

Lacus

A related set of features are the Lunar lacus /ˈlkəs/ (singular also lacus, Latin for "lake"), [lower-alpha 1] which are smaller basaltic plains of similar origin:

Lunar Lacus
Latin NameEnglish NameLat.Long.Diameter (km)
Lacus Aestatis Lake of Summer15.0° S69.0° W90
Lacus Autumni Lake of Autumn9.9° S83.9° W183
Lacus Bonitatis Lake of Goodness23.2° N43.7° E92
Lacus Doloris Lake of Sorrow17.1° N9.0° E110
Lacus Excellentiae Lake of Excellence35.4° S44.0° W184
Lacus Felicitatis Lake of Happiness19.0° N5.0° E90
Lacus Gaudii Lake of Joy16.2° N12.6° E113
Lacus Hiemalis Lake of Winter15.0° N14.0° E50
Lacus Lenitatis Lake of Softness14.0° N12.0° E80
Lacus Luxuriae Lake of Luxury19.0° N176.0° E50
Lacus Mortis Lake of Death45.0° N27.2° E151
Lacus Oblivionis Lake of Forgetfulness21.0° S168.0° W50
Lacus Odii Lake of Hatred19.0° N7.0° E70
Lacus Perseverantiae Lake of Perseverance8.0° N62.0° E70
Lacus Solitudinis Lake of Solitude27.8° S104.3° E139
Lacus Somniorum Lake of Dreams38.0° N29.2° E384
Lacus Spei Lake of Hope43.0° N65.0° E80
Lacus Temporis Lake of Time45.9° N58.4° E117
Lacus Timoris Lake of Fear38.8° S27.3° W117
Lacus Veris Lake of Spring16.5° S86.1° W396

Sinus and Paludes

A related set of features are the sinus /ˈsnəs/ (singular sinus, Latin for "bay") [lower-alpha 2] and paludes /pəˈldz/ (singular palus /ˈpləs/ , Latin palūs, palūdēs "marsh"):

Lunar Sinus and Paludes
Latin NameEnglish NameLat.Long.Diameter (km)
Palus Epidemiarum Marsh of Epidemics32.0° S28.2° W286
Palus Putredinis Marsh of Decay26.5° N0.4° E161
Palus Somni Marsh of Sleep14.1° N45.0° E143
Sinus Aestuum Seething Bay10.9° N8.8° W290
Sinus Amoris Bay of Love18.1° N39.1° E130
Sinus Asperitatis Bay of Roughness3.8° S27.4° E206
Sinus Concordiae Bay of Harmony10.8° N43.2° E142
Sinus Fidei Bay of Trust18.0° N2.0° E70
Sinus Honoris Bay of Honor11.7° N18.1° E109
Sinus Iridum Bay of Rainbows44.1° N31.5° W236
Sinus Lunicus Lunik Bay31.8° N1.4° W126
Sinus Medii Bay of the center2.4° N1.7° E335
Sinus Roris Bay of Dew54.0° N56.6° W202
Sinus Successus Bay of Success0.9° N59.0° E132

Some sources also list a Palus Nebularum (Latin palūs nebulārum /ˈpləsnɛbjʊˈlɛərəm/ "Marsh of Mists") at 38.0° N, 1.0° E. However the designation for this feature has not been officially recognized by the IAU.

See also

Notes

  1. In Latin, the singular is lacus ['lakʊs] and the plural is lacūs ['lakuːs] , but they are spelled and pronounced the same in English.
  2. As with 'lacus', Latin sg. sinus and plural sinūs are spelled and pronounced the same in English.

Related Research Articles

<span class="mw-page-title-main">Oceanus Procellarum</span> Vast lunar mare on the western edge of the near side of Earths Moon

Oceanus Procellarum is a vast lunar mare on the western edge of the near side of the Moon. It is the only one of the lunar maria to be called an "Oceanus" (ocean), due to its size: Oceanus Procellarum is the largest of the maria ("seas"), stretching more than 2,500 km (1,600 mi) across its north–south axis and covering roughly 4,000,000 km2 (1,500,000 sq mi), accounting for 10.5% of the total lunar surface area.

<span class="mw-page-title-main">Mare Imbrium</span> Vast lunar mare filling a basin on Earths Moon

Mare Imbrium is a vast lava plain within the Imbrium Basin on the Moon and is one of the larger craters in the Solar System. The Imbrium Basin formed from the collision of a proto-planet during the Late Heavy Bombardment. Basaltic lava later flooded the giant crater to form the flat volcanic plain seen today. The basin's age has been estimated using uranium–lead dating methods to approximately 3.9 billion years ago, and the diameter of the impactor has been estimated to be 250 ± 25 km. The Moon's maria have fewer features than other areas of the Moon because molten lava pooled in the craters and formed a relatively smooth surface. Mare Imbrium is not as flat as it was originally thought, because later events have altered its surface.

<span class="mw-page-title-main">Mare Tranquillitatis</span> Lunar mare

Mare Tranquillitatis is a lunar mare that sits within the Tranquillitatis basin on the Moon. It is the first location on another celestial body to be visited by humans.

<span class="mw-page-title-main">Mare Nubium</span> Lunar surface depression

Mare Nubium is a lunar mare in the Nubium basin on the Moon's near side. The mare is located just to the southeast of Oceanus Procellarum.

<span class="mw-page-title-main">Lunar mare</span> Large, dark, basaltic plains on Earths Moon

The lunar maria are large, dark, basaltic plains on Earth's Moon, formed by lava flowing into ancient impact basins. They were dubbed maria by early astronomers who mistook them for actual seas. They are less reflective than the "highlands" as a result of their iron-rich composition, and hence appear dark to the naked eye. The maria cover about 16% of the lunar surface, mostly on the side visible from Earth. The few maria on the far side are much smaller, residing mostly in very large craters. The traditional nomenclature for the Moon also includes one oceanus (ocean), as well as features with the names lacus ('lake'), palus ('marsh'), and sinus ('bay'). The last three are smaller than maria, but have the same nature and characteristics.

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

Archimedes is a large lunar impact crater on the eastern edges of the Mare Imbrium. Its diameter is 81 km.

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

Eddington is the lava-flooded remnant of a lunar impact crater, located on the western part of Oceanus Procellarum. The western rim is attached to the wall of the walled plain Struve. To the east-southeast is the smaller but prominent crater Seleucus. South of Eddington is Krafft.

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

Struve is the lava-flooded remains of a lunar impact crater. It is located near the western extreme of the Oceanus Procellarum, close to the western lunar limb. As a consequence, even though it is roughly circular in outline, it appears oval due to foreshortening.

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

Grimaldi is a large basin located near the western limb of the Moon. It lies to the southwest of the Oceanus Procellarum, and southeast of the crater Riccioli. Between Oceanus Procellarum is Damoiseau, and to the north is Lohrmann.

<span class="mw-page-title-main">Kepler (lunar crater)</span> Circular depression on the near side of Earths Moon

Kepler is a lunar impact crater that lies between the Oceanus Procellarum to the west and Mare Insularum in the east. To the southeast is the crater Encke. Kepler is named for the 17th century German astronomer and mathematician Johannes Kepler.

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

Democritus is a lunar impact crater that is located on the northern part of the Moon, just to the north of the Mare Frigoris. Just to the south of Democritus is the lava-flooded crater Gärtner, which forms a bay on the mare. Directly to the north is Arnold, another flooded formation.

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

Briggs is a lunar impact crater that is located in the western part of the Oceanus Procellarum, to the east of the large walled plain Struve. It lies to the northeast of the walled plain Eddington, and north-northwest of the crater Seleucus. The isolated position of this crater on the mare, near the northwestern limb of the Moon, makes it relatively easy for an Earth-bound observer to locate. The crater is named after the English mathematician Henry Briggs.

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

Lyell is a lunar impact crater that lies along the eastern edge of the Mare Tranquillitatis, at the northern arm of the bay designated Sinus Concordiae. It was named after Scottish geologist Charles Lyell. To the north along the edge of the lunar mare is the crater Franz. The region of terrain to the east of Lyell is named Palus Somni.

<span class="mw-page-title-main">Sinus Medii</span> Feature on the moon

Sinus Medii is a small lunar mare. It takes its name from its location at the intersection of the Moon's equator and prime meridian; as seen from the Earth, this feature is located in the central part of the Moon's near side, and it is the point closest to the Earth. From this spot, the Earth would always appear directly overhead, although the planet's position would vary slightly due to libration.

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

South is a large lunar impact crater that is located in the northwest part of the Moon. Most of the southern wall of this crater is joined to the Sinus Roris bay of the Oceanus Procellarum, with the southeast rim facing Mare Frigoris. Attached to the northwest of the formation is the larger walled plain Babbage. Just to the northeast is the crater Robinson, and farther to the northeast is another walled plain, J. Herschel.

<span class="mw-page-title-main">Louville</span> Crater on the Moon

Louville is a lunar impact crater that is located on the western edge of the Sinus Roris, a bay in the northern part of the Oceanus Procellarum. It lies to the northwest of the crater Mairan, on a triangular section of continental terrain to the west of Sinus Iridum and the Mare Imbrium.

<span class="mw-page-title-main">Lacus Somniorum</span> Feature on the moon

Lacus Somniorum is a basaltic plain located in the northeastern part of the Moon's near side. It is located at selenographic coordinates 37.56° N, 30.8° E, and has a diameter of 424.76 kilometers. The name is Latin for Lake of Dreams, a title given to this feature by Giovanni Riccioli. It is the largest of the lunar features designated Lacus.

<span class="mw-page-title-main">Sinus Roris</span> Moon feature

Sinus Roris is a dark, basaltic plain on the near side of the Moon that forms an extension of the northern edge of Oceanus Procellarum. The IAU-defined selenographic coordinates of this bay are 54.0° N, 56.6° W, and the diameter is 202 km.

<span class="mw-page-title-main">Selenography</span> Study of the surface and shape of the Moon

Selenography is the study of the surface and physical features of the Moon. Like geography and areography, selenography is a subdiscipline within the field of planetary science. Historically, the principal concern of selenographists was the mapping and naming of the lunar terrane identifying maria, craters, mountain ranges, and other various features. This task was largely finished when high resolution images of the near and far sides of the Moon were obtained by orbiting spacecraft during the early space era. Nevertheless, some regions of the Moon remain poorly imaged and the exact locations of many features are uncertain by several kilometers. Today, selenography is considered to be a subdiscipline of selenology, which itself is most often referred to as simply "lunar science." The word selenography is derived from the Greek word Σελήνη and γράφω graphō, meaning to write.

References

  1. Moore, Patrick (1983). The Guinness book of astronomy facts and feats. Enfield, Middlesex: Guinness Superlatives Ltd. p. 25. ISBN   0-85112-258-2.
  2. "Moon Mare/Maria". Gazetteer of Planetary Nomenclature. USGS Astrogeology. Retrieved 2010-08-20.
  3. 1 2 "Astronomica Langrenus" (in Italian). Archived from the original on 2006-10-12. Retrieved 2006-12-05.