Flag (crater)

Last updated
Flag
Flag crater Spook crater AS16-P-4618 ASU.jpg
Apollo 16 image, with Flag left of center and Spook right of center. Plum is the tiny crater on the southeast rim of Flag.
Coordinates 8°58′S15°27′E / 8.97°S 15.45°E / -8.97; 15.45
Diameter 240 m [1]
Eponym Astronaut-named feature

Flag crater is a small crater in the Descartes Highlands of the Moon visited by the astronauts of Apollo 16. The name of the crater was formally adopted by the IAU in 1973. [1] Geology Station 1 is adjacent to Flag, at the much smaller Plum crater.

Contents

On April 21, 1972, the Apollo 16 Apollo Lunar Module (LM) Orion landed about 1.5 km east of Flag, which is between the prominent North Ray and South Ray craters. The astronauts John Young and Charles Duke explored the area over the course of three EVAs using a Lunar Roving Vehicle, or rover. They drove to Flag on EVA 1.

Panorama of Flag crater taken by Charlie Duke, facing northwest at center Flag crater AS16-109-17776-78-80-82.jpg
Panorama of Flag crater taken by Charlie Duke, facing northwest at center
Panorama of Plum crater, to the left of the panorama above, facing southwest. Mission Commander John Young at left. The astronauts sampled soil in the foreground, and a boulder on the distal crater rim. Sample 61016, called Big Muley, is just above the right end of Young's shadow. Plum crater AS16-109-17789-90-91-92.jpg
Panorama of Plum crater, to the left of the panorama above, facing southwest. Mission Commander John Young at left. The astronauts sampled soil in the foreground, and a boulder on the distal crater rim. Sample 61016, called Big Muley, is just above the right end of Young's shadow.
Planimetric map of Station 1 from the Apollo 16 Preliminary Science Report. X indicates sample locations, 5-digit numbers are LRL sample numbers, rectangle is lunar rover (dot indicates TV camera), black spots are large rocks, dashed lines are crater rims or other topographic features, and triangles are panorama stations. Apollo 16 PSR Figure 6-21 Planimetric map of Station 1.jpg
Planimetric map of Station 1 from the Apollo 16 Preliminary Science Report. X indicates sample locations, 5-digit numbers are LRL sample numbers, rectangle is lunar rover (dot indicates TV camera), black spots are large rocks, dashed lines are crater rims or other topographic features, and triangles are panorama stations.

Flag crater is approximately 240 m in diameter and over 20 m deep. [2] The adjacent crater Plum is only about 30 m in diameter. [3] The slightly larger crater Spook, also visited by the astronauts, lies less than 1 km to the east.

Flag cuts into the Cayley Formation of Imbrian age. [4]

Samples

The following samples were collected from the vicinity of Plum and Flag crater (Station 1), as listed in Table 6-II of the Apollo 16 Preliminary Science Report, [5] which does not include samples smaller than 25 g weight (of which there were many). Sample type, lithology, and descriptions are from the Lunar Sample Atlas of the Lunar and Planetary Institute. [6]

SampleSample TypeLithologyPhotoDescription
61015rockbreccia Lunar sample 61015 S72-37756.jpg coated with black glass on one side and is thought to be ejecta from

South Ray crater

61016rockimpact melt breccia Lunar Sample 61016 - Big Muley.jpg known as Big Muley ; named after Bill Muehlberger,

the leader of the Apollo 16 field geology team

61135rockregolith breccia Lunar sample 61135 S72-38312.jpg an ancient regolith breccia that became a closed system

about 3.9 b.y. ago; and has a few zap pits

61155rakebreccia Lunar sample 61155 S72-38376.jpg clast-rich "glassy impact melt"; has abundant white clasts,

thin glass veins and glassy mesostasis

61156rockimpact melt breccia Lunar sample 61156 S72-38391.jpg Tough, medium gray, poikilitic impact melt

that has been thermally metamorphosed

61175rockfragmental breccia Lunar sample 61175 S72-40965.jpg Contains a high percentage of glass, with some agglutinate.

It also contains a small, but significant, mare component

61195rockbreccia Lunar sample 61195 S72-37972.jpg coherent, medium grey breccia with a glassy matrix and abundant clasts;

zap pits are surrounded with wide spall zones

61295rockbreccia Lunar sample 61295 S72-38964.jpg friable light matrix breccia with both light and dark clasts;

rounded and has many zap pits

61536rakebreccia Lunar sample 61536 S72-43398.jpg contains a large white clast held within a glass matrix,

and has a thin glass coating on surface

61546rakebreccia Lunar sample 61546 S72-43422.jpg vesicular chunk of glass with numerous small white clasts

and micrometeorite craters on one side only

Related Research Articles

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

Shorty is a feature on Earth's Moon, an impact crater in the Taurus–Littrow valley. Astronauts Eugene Cernan and Harrison Schmitt visited it in 1972, on the Apollo 17 mission. It is the location of the famous "orange soil", which geologists believe to be small bits of rapidly-cooled molten rock ejected in a fire fountain. It is about 110 meters in diameter and up to 14 m (15 yd) deep.

Shorty Crater is about 14 m deep. Based on our investigations at the site and later examination of photographs, the impact that formed it penetrated, in order, regolith on the avalanche deposit, the avalanche deposit, regolith on a basalt flow, a basalt flow overlying and protecting the orange and black glass layers, the orange and black glass layers, regolith on a second basalt flow, and, finally, the upper portion of that second flow. Orange and black glass clods and basalt boulders are spread throughout the ejecta blanket surrounding Shorty.

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

North Ray crater is a small crater in the Descartes Highlands of the Moon visited by the astronauts of Apollo 16. The name of the crater was formally adopted by the IAU in 1973. It is the largest crater sampled by astronauts during the Apollo program.

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

South Ray crater is a small crater in the Descartes Highlands of the Moon photographed from the lunar surface by the astronauts of Apollo 16. The name of the crater was formally adopted by the IAU in 1973.

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

Palmetto crater is a small crater in the Descartes Highlands of the Moon visited by the astronauts of Apollo 16. The name of the crater was formally adopted by the IAU in 1973.

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

Camelot is a feature on Earth's Moon, a crater in Taurus-Littrow valley. Astronauts Eugene Cernan and Harrison Schmitt visited it in 1972, on the Apollo 17 mission, during EVA 2. Geology Station 5 was along the south rim of Camelot.

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

Victory is a feature on Earth's Moon, a crater in Taurus–Littrow valley. Astronauts Eugene Cernan and Harrison Schmitt visited it in 1972, on the Apollo 17 mission, during EVA 2. The astronauts stopped at the south rim of Victory on their way back to the Lunar Module from Shorty crater.

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

Van Serg is a feature on Earth's Moon, a crater in Taurus–Littrow valley. Astronauts Eugene Cernan and Harrison Schmitt visited it in 1972, on the Apollo 17 mission, during EVA 3. Van Serg was designated Geology Station 9.

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

Sherlock is a feature on Earth's Moon, a crater in Taurus–Littrow valley. Astronauts Eugene Cernan and Harrison Schmitt drove their rover to the north of it in 1972, on the Apollo 17 mission. They photographed the rim, as shown below.

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

Nansen-Apollo is a feature on Earth's Moon, a crater in Taurus-Littrow valley, at the base of the South Massif. Astronauts Eugene Cernan and Harrison Schmitt visited it in 1972, on the Apollo 17 mission. The astronauts referred to it simply as Nansen during the mission. Geology Station 2 of the mission was located at Nansen. Nansen is located in the 'light mantle' which is almost certainly an avalanche deposit from the South Massif.

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

Lara is a feature on Earth's Moon, a crater in Taurus-Littrow valley. Astronauts Eugene Cernan and Harrison Schmitt visited it in 1972, on the Apollo 17 mission, during EVA 2. Geology Station 3 of the mission is located on the northeast rim of Lara.

<span class="mw-page-title-main">Cochise (crater)</span> Lunar impact crater in the Taurus–Littrow valley

Cochise is a feature on Earth's Moon, a crater in Taurus-Littrow valley. Astronauts Eugene Cernan and Harrison Schmitt landed southwest of it in 1972, on the Apollo 17 mission. They drove along its rim in the rover during EVA 3, but did not stop.

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

Trident is a feature on Earth's Moon, a crater in Taurus-Littrow valley. Astronauts Eugene Cernan and Harrison Schmitt landed about 300 m north of its rim in 1972, on the Apollo 17 mission. They drove along the east rim of Trident during EVA 1 of the mission, in their rover.

<span class="mw-page-title-main">Spur (lunar crater)</span> Surface depression on the Moon

Spur is a feature on Earth's Moon, a crater in the Hadley–Apennine region. Astronauts David Scott and James Irwin visited it in 1971, on the Apollo 15 mission, during EVA 2. Spur was designated Geology Station 7.

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

Dune is a feature on Earth's Moon, a crater in the Hadley–Apennine region. Astronauts David Scott and James Irwin visited the south rim of it in 1971, on the Apollo 15 mission, during EVA 2. The south rim of Dune was designated Geology Station 4 of the mission.

<span class="mw-page-title-main">Spook (crater)</span> Lunar crater explored on Apollo 16

Spook crater is a small crater in the Descartes Highlands of the Moon visited by the astronauts of Apollo 16. The name of the crater was formally adopted by the IAU in 1973. Geology Station 2 is adjacent to Spook, between it and the smaller, younger crater called Buster to the north of it.

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

Elbow is a feature on Earth's Moon, a crater in the Hadley–Apennine region. Astronauts David Scott and James Irwin visited the east rim of it in 1971, on the Apollo 15 mission, during EVA 1. The east rim of Elbow was designated Geology Station 1 of the mission. Geology Station 2 was to the southwest of the crater, up the slope of Mons Hadley Delta.

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

St. George is a feature on Earth's Moon, a crater in the Hadley–Apennine region. Astronauts David Scott and James Irwin drove their rover onto what was suspected to be its ejecta blanket in 1971, on the Apollo 15 mission, during EVA 1. They collected samples to the northeast of the crater, at Geology Station 2 of the mission.

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

Cinco is a small crater in the Descartes Highlands of the Moon visited by the astronauts of Apollo 16. The crater is one of a group of five (hence the name, Spanish for five) craters that were collectively called the Cinco craters during the Apollo 16 mission. The craters were designated a, b, c, d, and e, and the largest (a) was officially named Cinco after the mission in 1973 by the IAU.

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

Bench crater is a small crater in Oceanus Procellarum on the Moon. The name of the crater was formally adopted by the IAU in 1973.

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

Cone crater is a small crater in the Fra Mauro highlands, north of Fra Mauro crater, on the Moon. The name of the crater was formally adopted by the IAU in 1973.

References

  1. 1 2 Flag, Gazetteer of Planetary Nomenclature, International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN)
  2. Apollo 16 Landing Area, 78D2S1(50), NASA Lunar Topophotomap. Published by The Defense Mapping Agency, November 1974. Available from Lunar and Planetary Institute.
  3. Plum, Gazetteer of Planetary Nomenclature, International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN)
  4. Geologic Map of the Apollo 16 (Descartes) Landing Area Archived 2019-07-21 at the Wayback Machine by Apollo Field Geology Investigation Team (D. P. Elston, E. L. Boudette, J. P. Schafer), United States Geological Survey, April 1972
  5. Apollo 16 Preliminary Science Report (NASA SP-315), 1972
  6. Lunar Sample Atlas, Lunar and Planetary Institute