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.
Latin Name | English Name | Lat. | Long. | Diameter (km) |
---|---|---|---|---|
Mare Anguis | Serpent Sea | 22.6° N | 67.7° E | 150 |
Mare Australe | Southern Sea | 38.9° S | 93.0° E | 603 |
Mare Cognitum | Sea of Knowledge | 10.0° S | 23.1° W | 376 |
Mare Crisium | Sea of Crises | 17.0° N | 59.1° E | 418 |
Mare Fecunditatis | Sea of Fecundity | 7.8° S | 51.3° E | 909 |
Mare Frigoris | Sea of Cold | 56.0° N | 1.4° E | 1596 |
Mare Humboldtianum | Sea of Alexander von Humboldt | 56.8° N | 81.5° E | 273 |
Mare Humorum | Sea of Moisture or Humors | 24.4° S | 38.6° W | 389 |
Mare Imbrium [2] | Sea of Showers | 32.8° N | 15.6° W | 1123 |
Mare Ingenii | Sea of Cleverness | 33.7° S | 163.5° E | 318 |
Mare Insularum | Sea of Islands | 7.5° N | 30.9° W | 513 |
Mare Marginis | Sea of the Edge | 13.3° N | 86.1° E | 420 |
Mare Moscoviense | Sea of Moscow | 27.3° N | 147.9° E | 277 |
Mare Nectaris | Sea of Nectar | 15.2° S | 35.5° E | 333 |
Mare Nubium | Sea of Clouds | 21.3° S | 16.6° W | 715 |
Mare Orientale | Eastern Sea | 19.4° S | 92.8° W | 327 |
Mare Serenitatis | Sea of Serenity | 28.0° N | 17.5° E | 707 |
Mare Smythii | Smyth's Sea | 1.3° N | 87.5° E | 373 |
Mare Spumans | Foaming Sea | 1.1° N | 65.1° E | 139 |
Mare Tranquillitatis | Sea of Tranquility | 8.5° N | 31.4° E | 873 |
Mare Undarum | Sea of Waves | 6.8° N | 68.4° E | 243 |
Mare Vaporum | Sea of Vapors | 13.3° N | 3.6° E | 245 |
Oceanus Procellarum | Ocean of Storms | 18.4° N | 57.4° W | 2568 |
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:
A related set of features are the Lunar lacus /ˈleɪkəs/ (singular also lacus, Latin for "lake"), [lower-alpha 1] which are smaller basaltic plains of similar origin:
Latin Name | English Name | Lat. | Long. | Diameter (km) |
---|---|---|---|---|
Lacus Aestatis | Lake of Summer | 15.0° S | 69.0° W | 90 |
Lacus Autumni | Lake of Autumn | 9.9° S | 83.9° W | 183 |
Lacus Bonitatis | Lake of Goodness | 23.2° N | 43.7° E | 92 |
Lacus Doloris | Lake of Sorrow | 17.1° N | 9.0° E | 110 |
Lacus Excellentiae | Lake of Excellence | 35.4° S | 44.0° W | 184 |
Lacus Felicitatis | Lake of Happiness | 19.0° N | 5.0° E | 90 |
Lacus Gaudii | Lake of Joy | 16.2° N | 12.6° E | 113 |
Lacus Hiemalis | Lake of Winter | 15.0° N | 14.0° E | 50 |
Lacus Lenitatis | Lake of Softness | 14.0° N | 12.0° E | 80 |
Lacus Luxuriae | Lake of Luxury | 19.0° N | 176.0° E | 50 |
Lacus Mortis | Lake of Death | 45.0° N | 27.2° E | 151 |
Lacus Oblivionis | Lake of Forgetfulness | 21.0° S | 168.0° W | 50 |
Lacus Odii | Lake of Hatred | 19.0° N | 7.0° E | 70 |
Lacus Perseverantiae | Lake of Perseverance | 8.0° N | 62.0° E | 70 |
Lacus Solitudinis | Lake of Solitude | 27.8° S | 104.3° E | 139 |
Lacus Somniorum | Lake of Dreams | 38.0° N | 29.2° E | 384 |
Lacus Spei | Lake of Hope | 43.0° N | 65.0° E | 80 |
Lacus Temporis | Lake of Time | 45.9° N | 58.4° E | 117 |
Lacus Timoris | Lake of Fear | 38.8° S | 27.3° W | 117 |
Lacus Veris | Lake of Spring | 16.5° S | 86.1° W | 396 |
A related set of features are the sinus /ˈsaɪnəs/ (singular sinus, Latin for "bay") [lower-alpha 2] and paludes /pəˈluːdiːz/ (singular palus /ˈpeɪləs/ , Latin palūs, palūdēs "marsh"):
Latin Name | English Name | Lat. | Long. | Diameter (km) |
---|---|---|---|---|
Palus Epidemiarum | Marsh of Epidemics | 32.0° S | 28.2° W | 286 |
Palus Putredinis | Marsh of Decay | 26.5° N | 0.4° E | 161 |
Palus Somni | Marsh of Sleep | 14.1° N | 45.0° E | 143 |
Sinus Aestuum | Seething Bay | 10.9° N | 8.8° W | 290 |
Sinus Amoris | Bay of Love | 18.1° N | 39.1° E | 130 |
Sinus Asperitatis | Bay of Roughness | 3.8° S | 27.4° E | 206 |
Sinus Concordiae | Bay of Harmony | 10.8° N | 43.2° E | 142 |
Sinus Fidei | Bay of Trust | 18.0° N | 2.0° E | 70 |
Sinus Honoris | Bay of Honor | 11.7° N | 18.1° E | 109 |
Sinus Iridum | Bay of Rainbows | 44.1° N | 31.5° W | 236 |
Sinus Lunicus | Lunik Bay | 31.8° N | 1.4° W | 126 |
Sinus Medii | Bay of the center | 2.4° N | 1.7° E | 335 |
Sinus Roris | Bay of Dew | 54.0° N | 56.6° W | 202 |
Sinus Successus | Bay of Success | 0.9° N | 59.0° E | 132 |
Some sources also list a Palus Nebularum (Latin palūs nebulārum /ˈpeɪləsnɛbjʊˈlɛərəm/ "Marsh of Mists") at 38.0° N, 1.0° E. However the designation for this feature has not been officially recognized by the IAU.
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.
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 would have originally been when it first formed as a result of later events that have altered its surface.
Mare Tranquillitatis is a lunar mare that sits within the Tranquillitatis basin on the Moon. It contains Tranquility Base, the first location on another celestial body to be visited by humans.
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.
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.
Archimedes is a large lunar impact crater on the eastern edges of the Mare Imbrium. Its diameter is 81 km.
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.
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.
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.
Flamsteed is a small lunar impact crater located on the Oceanus Procellarum, which is named after British astronomer John Flamsteed. It lies almost due east of the dark-hued Grimaldi, and north-northwest of the flooded Letronne bay on the south edge of the mare.
Bowditch is a lunar impact crater that lies on the far side of the Moon, just beyond the eastern limb. It is located on a region of the lunar surface that is brought into view due to libration, but at such times the area is viewed from the edge and so not much detail can be observed. It lies just to the north of the small Lacus Solitudinis lunar mare, between the craters Titius to the southwest and Perel'man to the east-northeast.
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.
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.
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.
Hall is a lunar impact crater in the southeast part of the Lacus Somniorum, a lunar mare in the northeast part of the Moon. It was named after American astronomer Asaph Hall. This feature can be found to the east of the prominent walled plain Posidonius. Just to the south, and nearly attached to the southern rim of Hall is the smaller crater G. Bond.
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.
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.
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.
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.