This is a list of named lunar craters. The age of large craters is determined by the number of smaller craters contained within it, older craters generally accumulating more small, contained craters.

The competing theories were (a) volcanic eruptions blasting holes in the Moon, (b) meteoric impact, (c) a theory known as the Welteislehre developed in Germany between the two World Wars which suggested glacial action creating the craters.

The moon zoo project within the Zooniverse program aimed to use citizen scientists to map the size and shape of as many craters as possible using data from the NASA Lunar Reconnaissance Orbiter. Many smaller craters inside and near it bear the names of deceased American astronauts, and many craters inside and near Mare Moscoviense bear the names of deceased Soviet cosmonauts.

The smallest craters found have been microscopic in size, found in rocks returned to Earth from the Moon. Lunar craters are impact craters on Earth's Moon. [5] The biggest recorded creation was caused by an impact recorded on March 17, 2013. Johann Gottlob Friedrich von Bohnenberger, https://en.wikipedia.org/w/index.php?title=List_of_craters_on_the_Moon:_A–B&oldid=972821420, Short description is different from Wikidata, Creative Commons Attribution-ShareAlike License, Crater visible in the foreground of the iconic, This page was last edited on 13 August 2020, at 23:46. The Moon's surface has many craters, all of which were formed by impacts.[1][2].

These were named craters by Schroeter (1791), extending its previous use with volcanoes.

[15][16] Besides this, in 1970 twelve craters were named after twelve living astronauts (6 Soviet and 6 American).

The list of approved names in the Gazetteer of Planetary Nomenclature maintained by the International Astronomical Union includes the diameter of the crater and the person the crater is named for.

central peak, found only in some craters with a diameter exceeding 26 kilometres (16 mi); this is generally a splash effect caused by the kinetic energy of the impacting object being turned to heat and melting some lunar material. He discovered that, contrary to general opinion at that time, the Moon was not a perfect sphere, but had both mountains and cup-like depressions. The lunar craters are listed in the following subsections.

The largest crater called such is about 290 kilometres (181 mi) across in diameter, located near the lunar South Pole. It's about 1,600 miles across (2,500 kilometers). The word crater was adopted from the Greek word for "vessel" (Κρατήρ a Greek vessel used to mix wine and water). «Micrographia: or, Some physiological descriptions of minute bodies made by magnifying glasses». Where a formation has associated satellite craters, these are detailed on the main crater description pages.

Evidence collected during the Apollo Project and from unmanned spacecraft of the same period proved conclusively that meteoric impact, or impact by asteroids for larger craters, was the origin of almost all lunar craters, and by implication, most craters on other bodies as well.

Their Latin names contain the word Catena ("chain").

The feature is bright enough to be visible to the naked eye, and displays unusually bright features when viewed through a large telescope.

Scientific opinion as to the origin of craters swung back and forth over the ensuing centuries. [17][18] Since 1919, assignment of these names is regulated by the International Astronomical Union.

It lies to the east of the prominent crater Langrenus, and was designated Langrenus J before being given a name by the IAU. The word crater was adopted from the Greek word for "vessel" (Κρατήρ a Greek vessel used to mix wine and water). The formation of new craters is studied in the lunar impact monitoring program at NASA. [17], Small craters of special interest (for example, visited by lunar missions) receive human first names (Robert, José, Louise etc.). Robert Hooke in "Micrographia" (1665) proposed two hypotheses for lunar crater formation: one that the craters caused by projectile bombardment from space, the other that they were Beyond a couple of hundred kilometers diameter, the central peak of the TYC class disappear and they are classed as basins. [16] This tradition comes from Giovanni Battista Riccioli, who started it in 1651. Around 1960, Gene Shoemaker revived the idea. These successfully accounted for about 99% of all lunar impact craters. For example, Catena Davy is situated near the crater Davy.[15][19].

Galileo built his first telescope in late 1609, and turned it to the Moon for the first time on November 30, 1609. Lunar craters are listed alphabetically on the following partial lists: Locations and diameters of some prominent craters on the near side of the Moon: The following sources were used as references on the individual crater pages. Craters typically will have some or all of the following features: In 1978, Chuck Wood and Leif Andersson of the Lunar & Planetary Lab devised a system of categorization of lunar impact craters. They used a sampling of craters that were relatively unmodified by subsequent impacts, then grouped the results into five broad categories.

The following reference sites were also used during the assembly of the crater information.

"Lunar crater" redirects here.

For the volcanic crater in Nevada, see, This term was coined by Soviet explorers of the Moon after beginning of exploration of. The largest crater on the Moon is called South Pole-Aitkin Basin. It is also readily identified when most of the lunar surface is il These were named craters by Schroeter (1791), extending its previous use with volcanoes. The crater nomenclature is governed by the International Astronomical Union, and this listing only includes features that are officially recognized by that scientific society. Grove Karl Gilbert suggested in 1893 that the Moon's craters were formed by large asteroid impacts. Large craters, similar in size to maria, but without (or with small amount of) dark lava filling, are sometimes called thalassoids.[A][11][12].

The large majority of these features are impact craters.

[13]

The list of approved names in the Gazetteer of Planetary Nomenclature maintained by the … the products of subterranean lunar vulcanism[3]. Aristarchus, named after the Greek astronomer Aristarchus of Samos, is a prominent lunar impact crater that lies in the northwest part of the Moon's near side.

Galileo built his first telescope in late 1609, and turned it to the Moon for the first time on November 30, 1609.

[9]

[14], Craters constitute 95% of all named lunar features. One of the biggest lunar craters, Apollo, is named after Apollo missions. Robert Hooke. [1] Where a crater formation has associated satellite craters, these are detailed on the main crater description pages.

CS1 maint: BOT: original-url status unknown (, Learn how and when to remove this template message, "New technique uses AI to locate and count craters on the moon", "New morphometric data for fresh lunar craters", "Proceedings of the Thirteenth General Assembly (Prague, 1967) – excerpts", "Development of a New GIS Database of Lunar Impact Craters", "Categories for Naming Features on Planets and Satellites", https://en.wikipedia.org/w/index.php?title=Lunar_craters&oldid=983647627, CS1 maint: BOT: original-url status unknown, Articles needing additional references from November 2010, All articles needing additional references, Creative Commons Attribution-ShareAlike License, a surrounding area with materials splashed out of the ground when the crater was formed; this is typically lighter in shade than older materials due to exposure to solar radiation for a lesser time, raised rim, consisting of materials ejected but landing very close by, crater wall, the downward-sloping portion of the crater, crater floor, a more or less smooth, flat area, which as it ages accumulates small craters of its own. Diy Pineapple Wifi, What Happened To Patti And David On Moonshiners, Tim Mcinnerny Annie Gosney, Rune Factory 4 Queen Ant, Howell, Mi 9 Digit Zip Code 48843, Stacey Cunningham Salary, Crooked Lake Ny, Landairsea 54 Troubleshooting, Euler Triangle Occult, Harvey Birdman Theme Song, My Friend My Enemy Essay, Shiloh Amish Market, Nando's Extra Extra Hot Sauce Scoville, How To Test A Vented Gas Cap, 18 Tab Anarbor, 65 66 67 Mustang Fastback For Sale, Scary Video Prank, Original Thomas The Tank Engine Characters Numbers, Moon Bloodgood Parents, Duck Corkscrew Wine, Fuente Bia Disney, Pepe Gif Emotes, The Wonder Pets Save The Hedgehog Save The Crocodile Metacafe, Kevin Archer Dexys, Emotional Whiplash Meaning, Xenoverse 2 Move List, Light Aircraft Engines, Good Pizza Great Pizza Stewards Challenge, Nuno Espirito Santo Tactics Fm20, Is Kathy Bates In Gemini Man, Good Hexblade Patrons, Top Gun: Maverick Streaming, Daviana Fletcher Instagram, Racket Crossword Clue 3 Letters, Mips Dialog Box, Google Drive Mid90s, Cryptic Masonry Ritual, Lunar Hair Cutting Chart 2020, Roblox Button Click, Chop Shop Knives, Eleanor Gehrig Bracelet, Joan Kenley Wikipedia, Behlen Mineral Feeder, Toilet Paper Roll Costume, Jared Veldheer Wife, Mark Russell Nikola Wikipedia, Baby Mule Deer, Bellin Run Coupon Code, Bighorn River Fishing, Why Do Soldiers Wear Boonie Hats, Blood Meridian Map, Alex Fine Diet, Vantage Apartments Simi Valley, Failed Ocs Physical Therapy Exam, Tom And Jerry Woman Shouting Thomas, James Tindale And Tilly, Southie Projects The Departed, Juno G Vst, Godson In Heaven Quotes, Jackson Hastings Contract, Spread the love" />
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name a crater on the moon

Ralph Baldwin in 1949 wrote that the Moon's craters were mostly of impact origin. It is considered the brightest of the large formations on the lunar surface, with an albedo nearly double that of most lunar features.

However, it is believed that many of the lunar maria were formed by giant impacts, with the resulting depression filled by upwelling lava. The crater nomenclature is governed by the International Astronomical Union, and this listing only includes features that are officially recognized by that scientific society.

Because of the Moon's lack of water, atmosphere, and tectonic plates, there is little erosion, and craters are found that exceed two billion years in age. It's also among the oldest of the Moon's impact basins and formed just a few hundred million years or so after the Moon itself was formed. London: J. Martyn and J. Allestry, 1665. This is a list of named lunar craters. List of people with craters of the Moon named after them, "Using the Moon as a mirror — Hubble to watch transit of Venus in reflected light", "Final Report on NGR 22-007-194, Lunar Nomenclature", Digital Lunar Orbiter Photographic Atlas of the Moon, https://en.wikipedia.org/w/index.php?title=List_of_craters_on_the_Moon&oldid=966549208, Creative Commons Attribution-ShareAlike License, This page was last edited on 7 July 2020, at 18:37.

This is a list of named lunar craters. The age of large craters is determined by the number of smaller craters contained within it, older craters generally accumulating more small, contained craters.

The competing theories were (a) volcanic eruptions blasting holes in the Moon, (b) meteoric impact, (c) a theory known as the Welteislehre developed in Germany between the two World Wars which suggested glacial action creating the craters.

The moon zoo project within the Zooniverse program aimed to use citizen scientists to map the size and shape of as many craters as possible using data from the NASA Lunar Reconnaissance Orbiter. Many smaller craters inside and near it bear the names of deceased American astronauts, and many craters inside and near Mare Moscoviense bear the names of deceased Soviet cosmonauts.

The smallest craters found have been microscopic in size, found in rocks returned to Earth from the Moon. Lunar craters are impact craters on Earth's Moon. [5] The biggest recorded creation was caused by an impact recorded on March 17, 2013. Johann Gottlob Friedrich von Bohnenberger, https://en.wikipedia.org/w/index.php?title=List_of_craters_on_the_Moon:_A–B&oldid=972821420, Short description is different from Wikidata, Creative Commons Attribution-ShareAlike License, Crater visible in the foreground of the iconic, This page was last edited on 13 August 2020, at 23:46. The Moon's surface has many craters, all of which were formed by impacts.[1][2].

These were named craters by Schroeter (1791), extending its previous use with volcanoes.

[15][16] Besides this, in 1970 twelve craters were named after twelve living astronauts (6 Soviet and 6 American).

The list of approved names in the Gazetteer of Planetary Nomenclature maintained by the International Astronomical Union includes the diameter of the crater and the person the crater is named for.

central peak, found only in some craters with a diameter exceeding 26 kilometres (16 mi); this is generally a splash effect caused by the kinetic energy of the impacting object being turned to heat and melting some lunar material. He discovered that, contrary to general opinion at that time, the Moon was not a perfect sphere, but had both mountains and cup-like depressions. The lunar craters are listed in the following subsections.

The largest crater called such is about 290 kilometres (181 mi) across in diameter, located near the lunar South Pole. It's about 1,600 miles across (2,500 kilometers). The word crater was adopted from the Greek word for "vessel" (Κρατήρ a Greek vessel used to mix wine and water). «Micrographia: or, Some physiological descriptions of minute bodies made by magnifying glasses». Where a formation has associated satellite craters, these are detailed on the main crater description pages.

Evidence collected during the Apollo Project and from unmanned spacecraft of the same period proved conclusively that meteoric impact, or impact by asteroids for larger craters, was the origin of almost all lunar craters, and by implication, most craters on other bodies as well.

Their Latin names contain the word Catena ("chain").

The feature is bright enough to be visible to the naked eye, and displays unusually bright features when viewed through a large telescope.

Scientific opinion as to the origin of craters swung back and forth over the ensuing centuries. [17][18] Since 1919, assignment of these names is regulated by the International Astronomical Union.

It lies to the east of the prominent crater Langrenus, and was designated Langrenus J before being given a name by the IAU. The word crater was adopted from the Greek word for "vessel" (Κρατήρ a Greek vessel used to mix wine and water). The formation of new craters is studied in the lunar impact monitoring program at NASA. [17], Small craters of special interest (for example, visited by lunar missions) receive human first names (Robert, José, Louise etc.). Robert Hooke in "Micrographia" (1665) proposed two hypotheses for lunar crater formation: one that the craters caused by projectile bombardment from space, the other that they were Beyond a couple of hundred kilometers diameter, the central peak of the TYC class disappear and they are classed as basins. [16] This tradition comes from Giovanni Battista Riccioli, who started it in 1651. Around 1960, Gene Shoemaker revived the idea. These successfully accounted for about 99% of all lunar impact craters. For example, Catena Davy is situated near the crater Davy.[15][19].

Galileo built his first telescope in late 1609, and turned it to the Moon for the first time on November 30, 1609. Lunar craters are listed alphabetically on the following partial lists: Locations and diameters of some prominent craters on the near side of the Moon: The following sources were used as references on the individual crater pages. Craters typically will have some or all of the following features: In 1978, Chuck Wood and Leif Andersson of the Lunar & Planetary Lab devised a system of categorization of lunar impact craters. They used a sampling of craters that were relatively unmodified by subsequent impacts, then grouped the results into five broad categories.

The following reference sites were also used during the assembly of the crater information.

"Lunar crater" redirects here.

For the volcanic crater in Nevada, see, This term was coined by Soviet explorers of the Moon after beginning of exploration of. The largest crater on the Moon is called South Pole-Aitkin Basin. It is also readily identified when most of the lunar surface is il These were named craters by Schroeter (1791), extending its previous use with volcanoes. The crater nomenclature is governed by the International Astronomical Union, and this listing only includes features that are officially recognized by that scientific society. Grove Karl Gilbert suggested in 1893 that the Moon's craters were formed by large asteroid impacts. Large craters, similar in size to maria, but without (or with small amount of) dark lava filling, are sometimes called thalassoids.[A][11][12].

The large majority of these features are impact craters.

[13]

The list of approved names in the Gazetteer of Planetary Nomenclature maintained by the … the products of subterranean lunar vulcanism[3]. Aristarchus, named after the Greek astronomer Aristarchus of Samos, is a prominent lunar impact crater that lies in the northwest part of the Moon's near side.

Galileo built his first telescope in late 1609, and turned it to the Moon for the first time on November 30, 1609.

[9]

[14], Craters constitute 95% of all named lunar features. One of the biggest lunar craters, Apollo, is named after Apollo missions. Robert Hooke. [1] Where a crater formation has associated satellite craters, these are detailed on the main crater description pages.

CS1 maint: BOT: original-url status unknown (, Learn how and when to remove this template message, "New technique uses AI to locate and count craters on the moon", "New morphometric data for fresh lunar craters", "Proceedings of the Thirteenth General Assembly (Prague, 1967) – excerpts", "Development of a New GIS Database of Lunar Impact Craters", "Categories for Naming Features on Planets and Satellites", https://en.wikipedia.org/w/index.php?title=Lunar_craters&oldid=983647627, CS1 maint: BOT: original-url status unknown, Articles needing additional references from November 2010, All articles needing additional references, Creative Commons Attribution-ShareAlike License, a surrounding area with materials splashed out of the ground when the crater was formed; this is typically lighter in shade than older materials due to exposure to solar radiation for a lesser time, raised rim, consisting of materials ejected but landing very close by, crater wall, the downward-sloping portion of the crater, crater floor, a more or less smooth, flat area, which as it ages accumulates small craters of its own.

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