In the race to put humans on the Moon, NASA faced countless unprecedented challenges. Yet among the most critical was one deceptively simple question: where exactly should astronauts land? This decision—balancing safety, scientific value, and operational constraints—required years of meticulous planning, cutting-edge technology, and pioneering methodologies that continue to influence space exploration today.
Before Neil Armstrong took his historic first steps on lunar soil, NASA engineers and scientists engaged in a years-long process to identify locations that would maximize both crew safety and scientific discovery. This methodical approach was especially remarkable considering the limited knowledge of the lunar surface available in the 1960s.
Interactive: NASA’s Apollo Landing Sites Selection
Explore the methodology behind one of space exploration’s greatest achievements
The Five Primary Apollo Landing Sites
Click on each landing site to learn more about why it was selected and its significance.
Site One: Sea of Tranquility (Mare Tranquilitatis)
Coordinates: 34° East, 2°40″ North
Characteristics: This site offered a relatively smooth mare surface, making it a safer option for landing. Located in the Sea of Tranquility, this region featured fewer craters and a relatively flat terrain that would allow the Lunar Module to make a controlled descent.
Site Two: Tranquility Base (Apollo 11 Landing Site)
Coordinates: 23°37″ East, 0°45″ North
Characteristics: Also in the Sea of Tranquility, this site became famous as Tranquility Base, where Apollo 11 successfully landed on July 20, 1969. It was selected primarily for its relative safety, with flat mare terrain and few obstacles. This conservative choice prioritized mission success for humanity’s first lunar landing.
Historical Note: Neil Armstrong actually landed about 4 miles downrange from the intended spot after manually navigating away from a boulder-strewn area.
Site Three: Central Bay (Sinus Medii)
Coordinates: 1°20″ West, 0°25″ North
Characteristics: Located almost directly on the lunar equator and at the center of the Moon’s visible face, this site in Sinus Medii provided excellent visibility from Earth and offered optimal communications capability. Its central location made it favorable for mission planning and tracking.
Site Four: Ocean of Storms (Oceanus Procellarum)
Coordinates: 36°25″ West, 3°30″ South
Characteristics: This site in Oceanus Procellarum offered different geological characteristics from the eastern mare regions. It represented a chance to explore the western regions of the visible Moon, expanding the geographic diversity of potential sample collection.
Site Five: Western Ocean of Storms
Coordinates: 41°40″ West, 1°40″ North
Characteristics: Also in the Ocean of Storms, this westernmost site further expanded the geographic diversity of potential landing locations. By including sites across the lunar nearside, NASA ensured they had options that could accommodate different mission parameters and scientific objectives.
Key Selection Criteria
NASA evaluated potential landing sites based on multiple safety and scientific factors. Click each criterion to learn more.
Surface Smoothness
Sites needed relatively few craters or boulders that could damage the Lunar Module or impede astronaut movement. The ideal landing zone would have a generally flat, smooth surface with minimal obstacles within a radius of several hundred feet to ensure the LM could land safely and astronauts could conduct EVAs without excessive hazards.
Approach Paths
Areas with large hills, tall cliffs, or deep craters were avoided as these could cause incorrect altitude readings on the LM’s landing radar. The approach corridor needed to be free of significant obstacles that might interfere with the LM’s descent trajectory or radar readings, which were critical for a controlled landing.
Propellant Efficiency
Sites were selected to allow for the least amount of propellant expenditure, maximizing safety margins. The location needed to be reachable with enough propellant reserve to accommodate contingencies, such as having to hover longer than expected or abort to orbit if necessary.
Recycling Capability
The locations needed to accommodate potential countdown delays, allowing mission controllers to “recycle” the launch timeline if necessary. This meant sites had to remain accessible even if the mission launched later than originally planned, ensuring flexibility in mission scheduling.
Free-Return Trajectory
All sites had to be reachable via a free-return trajectory, meaning the spacecraft could loop around the Moon and return to Earth without engine firings in case of an emergency. This was a critical safety feature that ensured astronauts could return home even if major systems failed.
Scientific Value
Beyond safety considerations, sites were evaluated for their scientific value, particularly the variety of geological features they offered for sample collection. Geologists like Farouk El-Baz helped categorize potential landing zones based on their scientific merits, looking for locations that would maximize the knowledge gained from each mission.
Precursor Missions: Building Knowledge Step by Step
NASA’s methodical approach relied on data from earlier missions. Click on each mission series to learn how they contributed.
First close-up images of the lunar surface
The Ranger program consisted of nine missions designed to capture close-up images of the lunar surface before impacting it. Rangers 7, 8, and 9 successfully returned thousands of increasingly detailed photographs as they approached the Moon, providing the first high-resolution views of potential landing areas.
These kamikaze-style missions transmitted images until the moment of impact, giving scientists ever-closer views of the lunar terrain. The Ranger images revealed a cratered but generally navigable surface, giving hope that safe landing zones could be identified.
First soft landings to test surface conditions
Following Ranger, five Surveyor spacecraft successfully soft-landed on the Moon, providing crucial ground-truth data about surface conditions. These robotic missions tested the bearing strength of the lunar soil, investigated the surface composition, and transmitted panoramic images of their surroundings.
Surveyor data proved invaluable in confirming that the lunar surface could support the weight of the Apollo LM and that astronauts could safely walk on the regolith. Before Surveyor, some scientists worried the lunar dust might be many feet deep, potentially swallowing a landing spacecraft. Surveyor disproved this concern.
Comprehensive mapping of potential landing zones
Perhaps most critical to the landing site selection process were the five Lunar Orbiter missions, which systematically photographed nearly the entire lunar surface, including the far side. These spacecraft captured high-resolution images of potential landing zones, allowing engineers to create detailed maps and identify hazards not visible from Earth-based observations.
The data processing methods used for these images were groundbreaking. NASA employed novel photogrammetric techniques that differed significantly from standard procedures of that era. Monoscopic photography was computationally processed using high-speed digital computers to extract topographic information, which was then statistically analyzed to determine landing suitability.
The Evolution of Landing Site Selection
See how NASA’s approach evolved from Apollo 11 to Apollo 17. Click on each mission to learn more.
First lunar landing at Tranquility Base
NASA selected Site 2 in the Sea of Tranquility as the primary landing location. This choice reflected a conservative approach prioritizing safety for the first landing attempt. The relatively flat mare terrain offered fewer hazards, and previous Surveyor missions had demonstrated the surface could support a landed spacecraft.
During the actual landing, Neil Armstrong had to manually navigate away from a crater with boulders, demonstrating the importance of having skilled pilots for the missions.
Precision landing near Surveyor 3
Apollo 12 targeted a precise landing near Surveyor 3 in Oceanus Procellarum (Site 7), demonstrating pinpoint landing capability. This mission showed NASA’s growing confidence in their ability to target specific locations, as the LM landed within walking distance of the Surveyor 3 probe that had been on the lunar surface for over two years.
Fra Mauro formation exploration
Apollo 14 visited the Fra Mauro formation, a hilly region of geological interest. This site was initially planned for Apollo 13 before that mission’s abort. The Fra Mauro formation was believed to contain material ejected from the Imbrium Basin, offering insights into the Moon’s early history and formation.
Hadley Rille and Apennine Mountains
Apollo 15 landed at Hadley Rille, adjacent to the Apennine Mountains, requiring a more challenging approach but offering access to both highland and mare materials. This mission represented a significant shift toward prioritizing scientific discovery, featuring the first lunar rover to expand the exploration range.
Descartes Highlands exploration
Apollo 16 explored the Descartes Highlands, a dramatically different terrain from the mare regions of earlier landings. This mission focused on highland geology, providing important comparative data to the mare samples collected on earlier missions and expanding our understanding of lunar diversity.
Taurus-Littrow valley with geologist crew member
Apollo 17, the final mission, landed in the Taurus-Littrow valley, a location selected to maximize the scientific return with a geologist (Harrison Schmitt) on the crew. This mission represented the culmination of NASA’s site selection evolution, choosing a complex geological setting that offered access to both highland material and younger volcanic deposits.
The Initial Challenge: Navigating the Unknown
Prior to the Apollo missions, NASA's understanding of the Moon's surface was extremely limited. The agency had only pixelated images from early probes and telescopic observations from Earth. This presented an extraordinary challenge: how could they safely land astronauts on a surface potentially riddled with hazards?
The lunar landscape was known to contain impact craters deeper than the Marianas Trench and mountains taller than Mount Everest. Placing the three-legged Lunar Module (LM) safely required extreme precision and careful planning.
The stakes couldn't have been higher. A poor landing site selection might lead to disaster—the LM tipping over, becoming stuck in soft regolith, or placing astronauts in terrain too dangerous to navigate. NASA needed a comprehensive, scientific approach to narrow down the vast lunar surface to specific landing zones that maximized safety while still achieving mission objectives.
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Establishing the Apollo Zone of Interest
To begin narrowing the search, NASA established what became known as the "Apollo Zone of Interest". This zone represented a region along the visible side of the Moon, between 45 degrees East and West longitude, and between 5 degrees North and South of the lunar equator.
This equatorial band was chosen for several practical reasons:
- Landing sites along the equator maximized communication capabilities with Earth, a critical safety consideration
- The equatorial region presented better opportunities for continuous sunlight, essential for visibility during landing and surface operations
- These areas allowed for more flexible launch windows from Earth, as the Moon's position relative to Kennedy Space Center favored equatorial approaches
By establishing this zone, NASA engineers were able to focus their analysis on the most promising regions of the lunar surface, making the enormously complex problem somewhat more manageable.
The Role of Precursor Missions
NASA's approach to landing site selection was methodical and progressive, building upon knowledge gained from each previous mission. Three key mission series provided the essential data needed to select suitable landing sites.
Ranger Missions (1961-1965)
The Ranger program consisted of nine missions designed to capture close-up images of the lunar surface before impacting it. Rangers 7, 8, and 9 successfully returned thousands of increasingly detailed photographs as they approached the Moon, providing the first high-resolution views of potential landing areas.
These images revealed a cratered but generally navigable surface, giving hope that safe landing zones could be identified. The Ranger missions provided crucial first looks at the detailed texture of the lunar landscape, helping engineers understand what astronauts might encounter.
Surveyor Missions (1966-1968)
Following Ranger, five Surveyor spacecraft successfully soft-landed on the Moon, providing crucial ground-truth data about surface conditions. These robotic missions tested the bearing strength of the lunar soil, investigated the surface composition, and transmitted panoramic images of their surroundings.
Surveyor data proved invaluable in confirming that the lunar surface could support the weight of the Apollo LM and that astronauts could safely walk on the regolith. This hands-on information was essential to validate assumptions made from orbital imagery.
Lunar Orbiter Missions (1966-1967)
Perhaps most critical to the landing site selection process were the five Lunar Orbiter missions, which systematically photographed nearly the entire lunar surface, including the far side. These spacecraft captured high-resolution images of potential landing zones, allowing engineers to create detailed maps and identify hazards not visible from Earth-based observations.
The data processing methods used for these images were groundbreaking. NASA employed novel photogrammetric techniques that differed significantly from standard procedures of that era. Monoscopic photography was computationally processed using high-speed digital computers to extract topographic information, which was then statistically analyzed to determine landing suitability.
This combination of missions—impactors, landers, and orbiters—provided a comprehensive dataset that allowed NASA to gradually build confidence in its understanding of the lunar surface, moving from general knowledge to the detailed information needed for human landing sites.
The Apollo Site Selection Board
In 1966, NASA established the Apollo Site Selection Board to formally evaluate and recommend potential landing sites. Composed of engineers, scientists, and mission planners, this board methodically assessed the growing body of lunar data.
The Board's process was iterative and thorough. Originally considering 30 candidate sites, they gradually narrowed the options based on increasingly stringent criteria. Their deliberations lasted two years, culminating in the announcement of five potential landing sites for the first human lunar landing on February 8, 1968.
Selection Criteria: Safety First
Throughout the selection process, astronaut safety remained the paramount concern. The Board evaluated potential sites based on several key criteria:
Safety Criteria | Description |
Surface smoothness | Sites needed relatively few craters or boulders that could damage the LM or impede astronaut movement |
Approach paths | Areas with large hills, tall cliffs, or deep craters were avoided as these could cause incorrect altitude readings on the LM's landing radar |
Propellant efficiency | Sites were selected to allow for the least amount of propellant expenditure, maximizing safety margins |
Recycling capability | The locations needed to accommodate potential countdown delays, allowing mission controllers to "recycle" the launch timeline if necessary |
Free-return trajectory | All sites had to be reachable via a free-return trajectory, meaning the spacecraft could loop around the Moon and return to Earth without engine firings in case of an emergency |
Beyond these safety considerations, sites were also evaluated for their scientific value, particularly the variety of geological features they offered for sample collection. Farouk El-Baz, a geologist working for NASA, played a crucial role in categorizing potential landing zones based on their scientific merits.
The Five Primary Landing Sites
After extensive analysis, the Apollo Site Selection Board identified five primary landing sites for the first lunar landing, each with specific coordinates and characteristics:
Site | Location | Description |
Site One | 34° East, 2°40" North in the Sea of Tranquility (Mare Tranquilitatis) | Offered a relatively smooth mare surface |
Site Two | 23°37" East, 0°45" North, also in the Sea of Tranquility | Would eventually become Tranquility Base, where Apollo 11 landed |
Site Three | 1°20" West, 0°25" North in the Central Bay (Sinus Medii) | Almost directly on the lunar equator and at the center of the Moon's visible face |
Site Four | 36°25" West, 3°30" South in the Ocean of Storms (Oceanus Procellarum) | Offered different geological characteristics from the eastern mare regions |
Site Five | 41°40" West, 1°40" North, also in the Ocean of Storms | Westernmost site that expanded the geographic diversity of potential landing locations |
These sites were not just backup options for one another—they represented a strategic approach to exploring different regions of the lunar surface should Apollo accomplish multiple landings. Each location offered unique scientific opportunities while meeting the stringent safety requirements.
From Planning to Reality: Apollo 11

For the historic Apollo 11 mission, NASA selected Site 2 in the Sea of Tranquility as the primary landing location. This choice reflected a conservative approach prioritizing safety for the first landing attempt. The relatively flat mare terrain offered fewer hazards, and previous Surveyor missions had demonstrated the surface could support a landed spacecraft.
However, even with years of planning, the actual landing did not proceed exactly as intended. When the Eagle lunar module approached the designated landing area, Commander Neil Armstrong observed that they were heading toward a boulder-strewn area near a crater. Using his piloting skills, Armstrong manually flew the LM to a smoother area about four miles downrange from the planned landing point.
This illustrates an important reality of the Apollo program: despite meticulous planning, real-time human judgment remained essential to mission success. Armstrong's quick decision-making demonstrated why having experienced test pilots as astronauts was a crucial component of NASA's approach to lunar exploration.
Evolution of Site Selection: Later Apollo Missions

After the successful Apollo 11 landing validated NASA's approach, subsequent missions gradually targeted more challenging and scientifically interesting locations. The conservative, safety-first approach of early missions evolved into a more balanced consideration of scientific value.
The site selection for later missions reflected specific scientific objectives:
- Apollo 12 targeted a precise landing near Surveyor 3 in Oceanus Procellarum (Site 7), demonstrating pinpoint landing capability
- Apollo 14 visited the Fra Mauro formation, a hilly region of geological interest
- Apollo 15 landed at Hadley Rille, adjacent to the Apennine Mountains, requiring a more challenging approach but offering access to both highland and mare materials
- Apollo 16 explored the Descartes Highlands, a dramatically different terrain from the mare regions of earlier landings
- Apollo 17, the final mission, landed in the Taurus-Littrow valley, a location selected to maximize the scientific return with a geologist (Harrison Schmitt) on the crew
This progression demonstrates how NASA's confidence grew with experience, allowing for increasingly ambitious landing sites that prioritized scientific discovery while maintaining necessary safety margins. Each mission built upon the knowledge and techniques developed for previous landings, enabling exploration of more diverse and geologically interesting regions of the lunar surface.
The Site Selection Process: A Technical Achievement
The methodology NASA developed for lunar landing site selection represented a significant technical achievement in its own right. The process combined emerging computer technology, novel data analysis techniques, and interdisciplinary collaboration between engineers, geologists, and mission planners.
The Site Selection Board employed a matrix approach to evaluate candidate sites against multiple criteria. This systematic methodology allowed for quantitative comparison of qualitative factors and helped ensure that both technical and scientific considerations were properly weighted.
For photo analysis, NASA pioneered digital techniques that went beyond conventional photogrammetry. Lunar Orbiter images were processed through high-speed computers to create topographic maps and perform statistical analysis of surface roughness. These techniques laid the groundwork for modern remote sensing and GIS applications in planetary exploration.
The Human Element: Geologists and Astronauts
While technical criteria drove much of the site selection process, human expertise played a crucial role. Geologists like Farouk El-Baz brought a scientific perspective to the engineering-dominated process. El-Baz and his colleagues studied Lunar Orbiter photographs, categorizing them according to geological features and potential scientific value.
As El-Baz would later explain in interviews and documentation, the geologists worked to balance pure scientific interest with the practical requirements of mission safety.
The astronauts themselves also contributed to the site selection process through intensive training and simulation. They became familiar with the expected terrain features at candidate landing sites, prepared to make real-time judgments during descent, and offered feedback on operational considerations.
This combination of cutting-edge technology and human expertise allowed NASA to solve a problem of unprecedented complexity: selecting safe landing sites on another world with limited prior knowledge.
Legacy and Lessons for Future Exploration
NASA's Apollo landing site selection methodology established principles that continue to influence lunar and planetary mission planning today. The balance between safety, scientific return, and operational constraints remains fundamental to mission design.
Modern lunar missions like NASA's Artemis program build upon Apollo's foundation while incorporating new technologies. Today's planners benefit from vastly improved data resolution, sophisticated computational techniques, and decades of additional scientific understanding about the Moon.
However, the fundamental approach remains similar: identify mission objectives, establish selection criteria, gather precursor data, analyze systematically, and make informed choices that balance competing priorities. The meticulous, evidence-based approach developed for Apollo stands as a model for methodical exploration of challenging environments.
New research continues to build on these foundations, with recent studies examining how modern computational techniques can enhance our understanding of historical Apollo landing sites and inform future lunar exploration.
Conclusion: A Blueprint for Exploring Other Worlds
NASA's selection of the Apollo landing sites represented an extraordinary exercise in methodical problem-solving under conditions of significant uncertainty. Starting with limited knowledge of the lunar surface, NASA leveraged precursor missions, developed novel analytical techniques, and established a rigorous selection process to identify landing sites that balanced safety and science.
The success of this approach is evident in the perfect safety record of lunar landing attempts during Apollo and the wealth of scientific knowledge gained from the diverse landing sites. From Neil Armstrong's first step at Tranquility Base to the complex geological explorations of Apollo 17, each mission built upon the foundation of careful site selection that maximized both crew safety and scientific return.
As humanity prepares to return to the Moon through the Artemis program and other international efforts, the lessons learned from Apollo site selection remain relevant. The meticulous process that enabled humans to first set foot on another world continues to inform how we plan exploration of the Moon, Mars, and beyond.
The story of how NASA selected the Apollo landing sites is more than just a historical curiosity—it's a masterclass in problem-solving, risk management, and the integration of scientific and engineering considerations. As we look toward establishing a permanent human presence on the Moon and eventually journeying to Mars, the methodical approach pioneered during Apollo will continue to guide our path to the stars.
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