The Moon has numerous named plains on its surface made of dark-appearing basaltic rocks. The plains are visibly prominent on the near side of the Moon because of their contrasting appearance from the surrounding lunar highlands, which are made up of anorthosite, an igneous rock containing significant concentrations of highly reflective plagioclase feldspar minerals. As with other topographical features on the Moon, the official nomenclature for lunar plains uses a Latin naming system. Due to their darker appearance, differing elevation from the highlands, and visual prominence, noted ancient Greek astronomers such as Plutarch believed the plains were water; subsequent astronomers such as Galileo Galilei and Michael van Langren built on this belief, using Latin words for water bodies in classifying them. The Latin classifications for lunar plains are oceanus (), mare (), lacus (), palus (), and sinus ().
The largest plain is Oceanus Procellarum (), covering much of the western half of the Moon's near side and the only plain to be classified as an oceanus. Most other prominent plains on the near side are the lunar maria, while the Moon's lacūs, sinūs, and paludes are generally smaller and less visually prominent.
The classification of and other designations for lunar geographic features are determined by the International Astronomical Union (IAU)—the official international organization for the standardization of astronomy.
Geology
In its early stages of formation, the Moon's surface was largely molten, with its deep ocean of magma persisting for roughly tens of millions to hundreds of millions of years. After the cooling of the magma at the end of this period, minerals began to crystallize and differentiate, with heavier minerals sinking into the Moon's inner layers while the lighter, highly-reflective mineral of plagioclase feldspar rose to the surface and fused with other light, mafic-type crystals to form anorthosite rocks. The anorthosite accumulated to become an early stage of the Moon's outer crust. This early outer crust later became heavily bombarded by immense numbers of meteoroids and other solar system debris around 4 billion years ago, with substantial parts of the surface being blasted out to create craters and large basins. Millions of years after these massive impact basins formed, lava from the interior flowed up to the surface through cracks in the crust and filled the basins. The lava cooled into the dark, volcanic rock basalt, creating the lunar plains of today.
Currently, basaltic rock, which is also fine-grained and rich in iron, magnesium, and plagioclase feldspar, makes up most of the lunar plains' composition. As with the distribution of the lunar plains, basalt is also not uniformly distributed over the surface of the Moon, with approximately 26% of the Moon's near side and only 2% of its far side composed of basalt.
Nomenclature
The modern system of Latin-based lunar nomenclature began in 1651, when Italian astronomer and Catholic priest Giovanni Battista Riccioli published Almagestum Novum, an encyclopedic work in which he and fellow Italian priest and scientist Francesco Maria Grimaldi created a detailed map of the lunar near side's surface. In the book, Riccioli introduced a system differentiating lunar topography into three categories, with dark plains comprising one category and given Latin labels for bodies of water together with poetic, abstract names. Riccioli's system was used significantly in Europe in the succeeding centuries and became the basis for the current global standard in 1935, when the IAU adopted much of Riccioli's names and conventions. Since the current IAU nomenclature rules were affirmed in 1973, new names for lunar plains have been restricted to Latin terms that describe weather and other abstract concepts. Currently, there are 5 lunar plains' names referring to sea features, 5 indicating sea attributes, and 5 expressing states of mind.
Of plains inscribed prior to 1973 by the IAU, there are four that carry non-abstract names: Mare Humboldtianum and Mare Smythii, named for German natural historian Alexander von Humboldt and British astronomer William Henry Smyth, respectively; Mare Moscoviense, named for Muscovy, a historical predecessor of Russia; and Sinus Lunicus, named for the Soviet space probe Luna 2 ( Lunik 2), which landed there in 1959. Because Mare Humboldtianum and Mare Smythii were established before the final nomenclature, they were maintained and not required to follow the name conventions. In the case of Mare Moscoviense, which was discovered by the Luna 3 and whose name was proposed by the Soviet Union, it was only accepted by the IAU with the justification that Moscow is a 'state of mind'.
List
+ Name(in Latin) Name(English translation) Diameter Year Quadrangles Lunar coordinates Mare Anguis Serpent Sea LAC-44 Mare Australe Southern Sea LAC-116 Mare Cognitum Sea that has become known LAC-76 Mare Crisium Sea of Crises LAC-44 Mare Fecunditatis Sea of Fecundity LAC-80 Mare Frigoris Sea of Cold LAC-12 Mare Humboldtianum Sea of Humboldt LAC-15 Mare Humorum Sea of Moisture LAC-93 Mare Imbrium Sea of Showers LAC-24 Mare Ingenii Sea of Cleverness LAC-119 Mare Insularum Sea of Islands LAC-57 Mare Marginis Sea of the Edge LAC-63 Mare Moscoviense Sea of Muscovy LAC-48 Mare Nectaris Sea of Nectar LAC-79 Mare Nubium Sea of Clouds LAC-94 Mare Orientale Eastern sea LAC-108 Mare Serenitatis Sea of Serenity LAC-42 Mare Smythii Sea of Smyth LAC-81 Mare Spumans Foaming Sea LAC-62 Mare Tranquillitatis Sea of Tranquility LAC-61 Mare Undarum Sea of Waves LAC-62 Mare Vaporum Sea of Vapors LAC-59 Oceanus Procellarum Ocean of Storms LAC-38 Lacus Aestatis Lake of Summer LAC-74 Lacus Autumni Lake of Autumn LAC-73 Lacus Bonitatis Lake of Goodness LAC-43 Lacus Doloris Lake of Sorrow LAC-41 Lacus Excellentiae Lake of Excellence LAC-110 Lacus Felicitatis Lake of Happiness LAC-41 Lacus Gaudii Lake of Joy LAC-42 Lacus Hiemalis Wintry Lake LAC-60 Lacus Lenitatis Lake of Softness LAC-60 Lacus Luxuriae Lake of Luxury LAC-50 Lacus Mortis Lake of Death LAC-26 Lacus Oblivionis Lake of Forgetfulness LAC-105 Lacus Odii Lake of Hatred LAC-41 Lacus Perseverantiae Lake of Perseverance LAC-62 Lacus Solitudinis Lake of Solitude LAC-100 Lacus Somniorum Lake of Dreams LAC-26 Lacus Spei Lake of Hope LAC-28 Lacus Temporis Lake of Time LAC-27 Lacus Tenebrarum Lake of Darkness LAC-144 Lacus Timoris Lake of Fear LAC-111 Lacus Veris Lake of Spring LAC-91 Palus Epidemiarum Marsh of Epidemics LAC-94 Palus Putredinis Marsh of Decay LAC-41 Palus Somni Marsh of Sleep LAC-61 Sinus Aestuum Seething Bay LAC-59 Sinus Amoris Bay of Love LAC-43 Sinus Asperitatis Bay of Roughness LAC-78 Sinus Concordiae Bay of Harmony LAC-61 Sinus Fidei Bay of Trust LAC-41 Sinus Honoris Bay of Honor LAC-60 Sinus Iridum Bay of Rainbows LAC-24 Sinus Lunicus Lunik Bay LAC-25 Sinus Medii Bay of the center LAC-59 Sinus Roris Bay of Dew LAC-10 Sinus Successus Bay of Success LAC-62 Sinus Viscositatis Bay of Stickiness LAC-23
Clickable map
See also
List of craters on the Moon List of features on the Moon List of mountains on the Moon List of valleys on the Moon Selenography
Notes
References
External links NASA Lunar Atlas Digital Lunar Orbiter Photographic Atlas of the Moon USGS: Moon Nomenclature USGS: Moon Nomenclature: Mare USGS: Moon Nomenclature: Oceanus USGS: Moon Nomenclature: Lacus USGS: Moon Nomenclature: Palus USGS: Moon Nomenclature: Sinus