Planetary geology

[1][2] Although the geo- prefix typically indicates topics of or relating to Earth, planetary geology is named as such for historical and convenience reasons; due to the subject matter, it is closely linked with more traditional Earth-based geology.Despite their outermost layers being dominated by gases, the giant planets are also included in the field of planetary geology, especially when it comes to their interiors.Eugene Merle Shoemaker is credited with bringing geologic principles to planetary mapping and creating the branch of planetary science in the early 1960s, the Astrogeology Research Program, within the United States Geological Survey.[citation needed] Simulated interplanetary missions performed on Earth have studied procedures and tools for planetary geology.[11] The standard names are chosen to consciously avoid interpreting the underlying cause of the feature, but rather to describe only its appearance.
Planetary geologist and NASA astronaut Harrison "Jack" Schmitt collecting lunar samples during the Apollo 17 mission in early-December 1972
Surface of Mars in a false-color photograph by the Viking 2 lander, December 9, 1977
GeologyOutlineGlossaryHistoryTimelineMineralsIgneousSedimentaryMetamorphicSedimentPlate tectonicsStrataWeatheringErosionGeologic time scaleStratigraphic principlesPrinciple of original horizontalityLaw of superpositionPrinciple of lateral continuityPrinciple of cross-cutting relationshipsPrinciple of faunal successionPrinciple of inclusions and componentsWalther's lawGeochemistryMineralogySedimentologyPetrologyStructure of EarthGeomorphologyGlaciologyStructural GeologyVolcanologyGeological history of EarthGeologistGeological surveyEngineeringMiningForensicsMilitaryLists of geological features of the Solar SystemGeology of solar terrestrial planetsMercuryTritonCharonplanetary sciencecelestial bodiesplanetsasteroidscometsmeteoritesterrestrial planetssurfacevolcanismimpact cratersfluvialaeoliangiant planetsgeological sciencesgeophysicsHarrison "Jack" Schmittlunar samplesApollo 17Viking 2Eugene Merle ShoemakerAstrogeology Research ProgramUnited States Geological SurveyselenographyLunar and Planetary InstituteApplied Physics LaboratoryPlanetary Science InstituteJet Propulsion LaboratorySouthwest Research InstituteJohnson Space CenterMontana State UniversityBrown UniversityUniversity of ArizonaCalifornia Institute of TechnologyUniversity of ColoradoWestern Michigan UniversityMassachusetts Institute of TechnologyWashington University in St. Louisastronomyearth sciencesHubble Space TelescopePlanetary Data SystemPlanetary nomenclatureInternational Astronomical UnionGeological features of the Solar SystemGeology of MercuryGeology of VenusGeology of the MoonGeology of MarsGeology of CeresGeology of TritonGeology of PlutoGeology of CharonAstrobiologyExoplanetExoplanetologyPlanetary habitabilityCornell UniversityBibcodeJohn Wiley & SonsDwarf PlanetsGeology of IoGeology of TitanAstrochemistryAstrometryAstrophysicsCosmochemistryCosmologyExtragalactic astronomyGalactic astronomyOrbital mechanicsPhysical cosmologySolar astronomyOutline of geologyGlossary of geologyHistory of geologyIndex of geology articlesGeochronologyTimeline of geologyCrystallographyHistorical geologyStratigraphyPaleontologyPaleoclimatologyPalaeogeographyGeodynamicsHydrogeologyMarine geologyGeodesyCartographyEarth's orbitGeodetic astronomyGeomaticsGravity of EarthRemote sensingGeopositioningGeomagnetismGeophysical surveySeismologyTectonophysicsBiogeologyEconomic geologyEngineering geologyEnvironmental geologyGeobiologyGeologic modellingForensic geologyForensic geophysicsMeteoriticsMining geologyMineral physicsPetroleum geologistVolcanologist