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. Spook crater is approximately 340 m in diameter and over 20 m deep. Spook is about 550 m west of the landing site itself. The Lunar Portable Magnetometer (LPM) was used to obtain a reading of approximately 180 γ (gamma) at Spook. This was one of five locations at the landing site where the LPM was used.
*
*
| Attributes | Values |
|---|
| rdf:type
| |
| rdfs:label
| - Spook (cráter) (es)
- Spook (crater) (en)
|
| rdfs:comment
| - Spook es un pequeño cráter lunar situado en las Tierras Altas de Descartes, visitado por los astronautas del Apolo 16. El nombre del cráter fue adoptado formalmente por la Unión Astronómica Internacional en 1973. La Estación 2 de geología está adyacente a Spook, entre el propio cráter y un segundo cráter denominado Buster, más pequeño, más reciente y situado al norte de Spook. (es)
- 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. Spook crater is approximately 340 m in diameter and over 20 m deep. Spook is about 550 m west of the landing site itself. The Lunar Portable Magnetometer (LPM) was used to obtain a reading of approximately 180 γ (gamma) at Spook. This was one of five locations at the landing site where the LPM was used.
*
* (en)
|
| geo:lat
| |
| geo:long
| |
| foaf:depiction
| |
| location
| |
| dcterms:subject
| |
| Wikipage page ID
| |
| Wikipage revision ID
| |
| Link from a Wikipage to another Wikipage
| |
| Link from a Wikipage to an external page
| |
| sameAs
| |
| dbp:wikiPageUsesTemplate
| |
| thumbnail
| |
| caption
| - Apollo 16 image, with Flag left of center and Spook right of center. Buster is the small crater north of Spook. (en)
|
| diameter
| |
| image size
| |
| georss:point
| |
| has abstract
| - Spook es un pequeño cráter lunar situado en las Tierras Altas de Descartes, visitado por los astronautas del Apolo 16. El nombre del cráter fue adoptado formalmente por la Unión Astronómica Internacional en 1973. La Estación 2 de geología está adyacente a Spook, entre el propio cráter y un segundo cráter denominado Buster, más pequeño, más reciente y situado al norte de Spook. El módulo lunar Orion del Apolo 16 aterrizó entre los cráteres North Ray y South Ray el 21 de abril de 1972. Los astronautas John Young y Charles M. Duke exploraron el área entre los cráteres en el transcurso de tres EVAs utilizando un Lunar Roving Vehicle o rover. Se detuvieron en Spook durante EVA 1, en el camino de regreso al módulo lunar desde el cráter Flag. El cráter Spook tiene aproximadamente 340 metros de diámetro y más de 20 m de profundidad. Se halla a unos 550 metros al oeste del punto de aterrizaje. Fue uno de los puntos elegidos para utilizar el magnetómetro portátil Lunar (LPM), obteniéndose una lectura de aproximadamente 180 γ (gamma).. Esta fue una de las cinco ubicaciones la zona de aterrizaje donde se utilizó. Spook se inserta en la Formación Cayley del Período Ímbrico. (es)
- 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. On April 21, 1972, the Apollo 16 Lunar Module Orion landed about 500 m east of Spook, 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 stopped at Spook during EVA 1, on the way back to the LM from Flag crater. Spook crater is approximately 340 m in diameter and over 20 m deep. Spook is about 550 m west of the landing site itself. The Lunar Portable Magnetometer (LPM) was used to obtain a reading of approximately 180 γ (gamma) at Spook. This was one of five locations at the landing site where the LPM was used. Spook cuts into the Cayley Formation of Imbrian age.
* Mosaic showing Spook crater with Stone Mountain in the background
* The Lunar Portable Magnetometer (LPM) was used to take a magnetic field measurement at the north rim of Spook (en)
|
| eponym
| - Astronaut-named feature (en)
|
| gold:hypernym
| |
| schema:sameAs
| |
| prov:wasDerivedFrom
| |
| page length (characters) of wiki page
| |
| diameter (μ)
| |
| foaf:isPrimaryTopicOf
| |
| geo:geometry
| - POINT(15.479999542236 -8.9799995422363)
|
| is Link from a Wikipage to another Wikipage
of | |
| is Wikipage disambiguates
of | |
| is foaf:primaryTopic
of | |
![[RDF Data]](/fct/images/sw-rdf-blue.png)
![[cxml]](/fct/images/cxml_doc.png)
![[csv]](/fct/images/csv_doc.png)
![[text]](/fct/images/ntriples_doc.png)
![[turtle]](/fct/images/n3turtle_doc.png)
![[ld+json]](/fct/images/jsonld_doc.png)
![[rdf+json]](/fct/images/json_doc.png)
![[rdf+xml]](/fct/images/xml_doc.png)
![[atom+xml]](/fct/images/atom_doc.png)
![[html]](/fct/images/html_doc.png)
