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Mairan (crater)

Mairan is a lunar impact crater that is located on a highland peninsula between Oceanus Procellarum to the west and Mare Imbrium to the east. To the north-northeast is the comparably sized crater Sharp. Northwest of Mairan is the heavily eroded Louville.

Mairan
Coordinates41°36′N 43°24′W / 41.6°N 43.4°W / 41.6; -43.4
Diameter40 km
Depth3.4 km
Colongitude44° at sunrise
EponymJean J. d'Ortous
de Mairan
Oblique view from Apollo 15

The outer rim of Mairan has not been significantly eroded or impacted, and retains a sharp edge. The surface around Mairan is rough and irregular, with a multitude of many tiny craters, particularly to the south and west. The inner walls display some terracing, and flow down to a relatively flat interior floor.

Mairan is a crater of Upper (Late) Imbrian age.[1]

Mairan domes edit

The volcanic complex, known as Mairan Hills or Mairan Domes, is composed of Mairan T together with three satellite domes (Mairan Northwest, Mairan Middle, and Mairan South). It was formed by two volcanic episodes 3.75±0.1 and 3.35±0.2 billion years ago, extruding a viscous silicic lava simultaneously with basalt eruptions in nearby mare. Most of volcanic complex, except for dome summits, is now buried under mare surface.[2]

In the mare, due west of Mairan, is a small lunar dome designated Mairan T with 3.8 km wide depression at the summit (in official IAU nomenclature "Mairan T" name refers only to the depression), believed to be a caldera[3] The width of hill is about 7 km, and height is about 800 m.[4] It is one of four unusually steep (with slopes reaching 22-27 degrees) and bright domes in area which are thought to be formed by very viscous, high-Si lava.[5]

The composition of domes is changing from the north to south, with Mairan Northwest composed of pyroxenes with 30% quartz admixture, while Mairan South dome composed of nearly pure quartz, with extremely high thorium concentration of 83±19 ppm.[6]

Rima Mairan edit

There is a sinuous rille along the southwest edge of the highland peninsula containing Mairan. It is designated Rima Mairan, and follows a north–south course for a length of about 100 kilometers.

 
Oblique view of part of Rima Mairan, from Apollo 15

Satellite craters edit

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

Mairan Latitude Longitude Diameter
A 38.6° N 38.8° W 16 km
C 38.6° N 46.0° W 7 km
D 40.9° N 45.4° W 10 km
E 37.8° N 37.2° W 6 km
F 40.3° N 45.1° W 9 km
G 40.9° N 50.8° W 6 km
H 39.3° N 40.0° W 5 km
K 40.8° N 41.0° W 6 km
L 39.0° N 43.2° W 6 km
N 39.2° N 45.5° W 6 km
T 41.7° N 48.3° W 3 km
Y 42.7° N 44.0° W 7 km

References edit

  1. ^ The geologic history of the Moon. USGS Professional Paper 1348. By Don E. Wilhelms, John F. McCauley, and Newell J. Trask. U.S. Government Printing Office, Washington: 1987. Table 11.2.
  2. ^ Geology of Mairan middle dome: Its implication to silicic volcanism on the Moon
  3. ^ "Mairan". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
  4. ^ Tran, T.; Robinson, M. S.; Lawrence, S. J.; Braden, S. E.; Plescia, J.; Hawke, B. R.; et al. (March 2011). "Morphometry of Lunar Volcanic Domes from LROC" (PDF). 42nd Lunar and Planetary Science Conference, Held March 7–11, 2011 at the Woodlands, Texas. LPI Contribution (1608 p.2228): 2228. Bibcode:2011LPI....42.2228T.
  5. ^ Lena R.; Wöhler C.; Phillips J.; Chiocchetta M. T. (2013). Lunar Domes: Properties and Formation Processes. Springer Science & Business Media. pp. vii, 5–13, 35, 42. Bibcode:2013ldpf.book.....L. doi:10.1007/978-88-470-2637-7. ISBN 9788847026377.
  6. ^ The Mairan domes: Silicic volcanic constructs on the Moon

mairan, crater, mairan, lunar, impact, crater, that, located, highland, peninsula, between, oceanus, procellarum, west, mare, imbrium, east, north, northeast, comparably, sized, crater, sharp, northwest, mairan, heavily, eroded, louville, mairanlunar, orbiter,. Mairan is a lunar impact crater that is located on a highland peninsula between Oceanus Procellarum to the west and Mare Imbrium to the east To the north northeast is the comparably sized crater Sharp Northwest of Mairan is the heavily eroded Louville MairanLunar Orbiter 4 imageCoordinates41 36 N 43 24 W 41 6 N 43 4 W 41 6 43 4Diameter40 kmDepth3 4 kmColongitude44 at sunriseEponymJean J d Ortousde MairanOblique view from Apollo 15The outer rim of Mairan has not been significantly eroded or impacted and retains a sharp edge The surface around Mairan is rough and irregular with a multitude of many tiny craters particularly to the south and west The inner walls display some terracing and flow down to a relatively flat interior floor Mairan is a crater of Upper Late Imbrian age 1 Contents 1 Mairan domes 2 Rima Mairan 3 Satellite craters 4 ReferencesMairan domes editThe volcanic complex known as Mairan Hills or Mairan Domes is composed of Mairan T together with three satellite domes Mairan Northwest Mairan Middle and Mairan South It was formed by two volcanic episodes 3 75 0 1 and 3 35 0 2 billion years ago extruding a viscous silicic lava simultaneously with basalt eruptions in nearby mare Most of volcanic complex except for dome summits is now buried under mare surface 2 In the mare due west of Mairan is a small lunar dome designated Mairan T with 3 8 km wide depression at the summit in official IAU nomenclature Mairan T name refers only to the depression believed to be a caldera 3 The width of hill is about 7 km and height is about 800 m 4 It is one of four unusually steep with slopes reaching 22 27 degrees and bright domes in area which are thought to be formed by very viscous high Si lava 5 The composition of domes is changing from the north to south with Mairan Northwest composed of pyroxenes with 30 quartz admixture while Mairan South dome composed of nearly pure quartz with extremely high thorium concentration of 83 19 ppm 6 Rima Mairan editThere is a sinuous rille along the southwest edge of the highland peninsula containing Mairan It is designated Rima Mairan and follows a north south course for a length of about 100 kilometers nbsp Oblique view of part of Rima Mairan from Apollo 15Satellite craters editBy convention these features are identified on lunar maps by placing the letter on the side of the crater midpoint that is closest to Mairan Mairan Latitude Longitude DiameterA 38 6 N 38 8 W 16 kmC 38 6 N 46 0 W 7 kmD 40 9 N 45 4 W 10 kmE 37 8 N 37 2 W 6 kmF 40 3 N 45 1 W 9 kmG 40 9 N 50 8 W 6 kmH 39 3 N 40 0 W 5 kmK 40 8 N 41 0 W 6 kmL 39 0 N 43 2 W 6 kmN 39 2 N 45 5 W 6 kmT 41 7 N 48 3 W 3 kmY 42 7 N 44 0 W 7 km nbsp Lunar dome Mairan T nbsp Mairan T from Apollo 15References edit The geologic history of the Moon USGS Professional Paper 1348 By Don E Wilhelms John F McCauley and Newell J Trask U S Government Printing Office Washington 1987 Table 11 2 Geology of Mairan middle dome Its implication to silicic volcanism on the Moon Mairan Gazetteer of Planetary Nomenclature USGS Astrogeology Research Program Tran T Robinson M S Lawrence S J Braden S E Plescia J Hawke B R et al March 2011 Morphometry of Lunar Volcanic Domes from LROC PDF 42nd Lunar and Planetary Science Conference Held March 7 11 2011 at the Woodlands Texas LPI Contribution 1608 p 2228 2228 Bibcode 2011LPI 42 2228T Lena R Wohler C Phillips J Chiocchetta M T 2013 Lunar Domes Properties and Formation Processes Springer Science amp Business Media pp vii 5 13 35 42 Bibcode 2013ldpf book L doi 10 1007 978 88 470 2637 7 ISBN 9788847026377 The Mairan domes Silicic volcanic constructs on the Moon Andersson L E Whitaker E A 1982 NASA Catalogue of Lunar Nomenclature PDF NASA RP 1097 Archived from the original on 2014 10 06 a href Template Cite book html title Template Cite book cite book a CS1 maint bot original URL status unknown link Blue Jennifer July 25 2007 Gazetteer of Planetary Nomenclature USGS Retrieved 2015 12 31 Bussey B Spudis P 2004 The Clementine Atlas of the Moon New York Cambridge University Press ISBN 978 0 521 81528 4 Cocks Elijah E Cocks Josiah C 1995 Who s Who on the Moon A Biographical Dictionary of Lunar Nomenclature Tudor Publishers ISBN 978 0 936389 27 1 McDowell Jonathan July 15 2007 Lunar Nomenclature Jonathan s Space Report Retrieved 2007 10 24 Menzel D H Minnaert M Levin B Dollfus A Bell B 1971 Report on Lunar Nomenclature by the Working Group of Commission 17 of the IAU Space Science Reviews 12 2 136 186 Bibcode 1971SSRv 12 136M doi 10 1007 BF00171763 S2CID 122125855 Moore Patrick 2001 On the Moon Sterling Publishing Co ISBN 978 0 304 35469 6 Price Fred W 1988 The Moon Observer s Handbook Cambridge University Press ISBN 978 0 521 33500 3 Rukl Antonin 1990 Atlas of the Moon Kalmbach Books ISBN 978 0 913135 17 4 Webb Rev T W 1962 Celestial Objects for Common Telescopes 6th revised ed Dover ISBN 978 0 486 20917 3 Whitaker Ewen A 2003 Mapping and Naming the Moon Cambridge University Press ISBN 978 0 521 54414 6 Wlasuk Peter T 2000 Observing the Moon Springer Science amp Business Media ISBN 978 1 852 33193 1 Retrieved from https en wikipedia org w index php title Mairan crater amp oldid 1199122587, wikipedia, wiki, book, books, library,

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