Craterra

LUNAR ATLAS · VOLCANIC BASIN

Mare Cognitum: The Known Sea

Enclosed by Montes Riphaeus and the Fra Mauro formation, this 350-kilometer mare was named following the 1964 Ranger 7 mission and explored on foot by Apollo 12.

Feature Profile & Selenographic Data

Feature type
mare
Coordinates
10.0° S · 23.1° W
Diameter
350 km
IAU approval
1964/01/01 00:00:00
LAC quadrangle
LAC-76 · Montes Riphaeus
Geological Period
Upper Imbrian (Basalt) / Pre-Nectarian (Basin)

Geological Chronicle

Mare Cognitum, translated from Latin as 'The Sea That Has Become Known', is a circular lunar mare located in the southern near side of the Moon within the second structural ring of Oceanus Procellarum. Centered at 10.0° S and 23.1° W, the dark basaltic expanse spans 350 kilometers across. The underlying impact basin formed during the Pre-Nectarian epoch, while subsequent eruptions of basaltic lava flooded the structure during the Upper Imbrian epoch. The mare is bounded to the northwest by Montes Riphaeus, an arcuate ridge representing the rim of the degraded basin, and bordered to the east by the hummocky terrain of the Fra Mauro formation.

The region received its modern name in 1964 when the International Astronomical Union designated the formerly unnamed basaltic plain following the success of the Ranger 7 spacecraft. On July 31, 1964, Ranger 7 transmitted 4,308 high-resolution photographs during its final minutes of flight before impacting the mare floor. The images provided the first close-range views of lunar craters and surface texture, demonstrating that the lunar maria were structurally solid enough to support future robotic and crewed landings.

Exploration of Mare Cognitum expanded through NASA surface missions. On November 19, 1969, Apollo 12 astronauts Pete Conrad and Alan Bean landed their Lunar Module Intrepid at Statio Cognitum on the northern perimeter of the mare, touching down within walking distance of the robotic probe Surveyor 3, which had arrived in 1967. The astronauts gathered basalt samples with lower titanium concentrations than those from Apollo 11, giving the local terrain a slightly redder spectral hue. Laboratory dating showed the Apollo 12 basalts formed roughly 500 million years later than basalts from Tranquility Base, confirming that lunar mare volcanism occurred in distinct stages. Apollo 12 also recovered light-colored soil identified as ray ejecta from Copernicus crater, located hundreds of kilometers to the north.

In February 1971, lunar surface exploration returned to the eastern border of Mare Cognitum with the Apollo 14 mission. Astronauts Alan Shepard and Edgar Mitchell landed in the adjacent Fra Mauro formation to sample materials excavated by the impact that formed Mare Imbrium. The field data and returned samples collected around Mare Cognitum and the neighboring Fra Mauro ridges established foundational reference points for dating volcanic and impact sequences across the Moon.

Chronology & Exploration

  1. > 3.9 Ga Pre-Nectarian Basin Formation

    An ancient impact excavates a 350-kilometer structural depression in the crust of the southern near side.

  2. 3.8 to 3.2 Ga Upper Imbrian Basalt Flooding

    Effusive volcanism fills the depression with low-titanium basalt lava flows, creating the smooth mare plain.

  3. 1964 Ranger 7 Impact and IAU Naming

    NASA probe Ranger 7 transmits 4,308 close-range photos before impact, prompting the IAU to name the region Mare Cognitum.

  4. 1969 Apollo 12 at Statio Cognitum

    Pete Conrad and Alan Bean land near Surveyor 3, collecting 34.35 kilograms of basalts and Copernicus ray ejecta.

  5. 1971 Apollo 14 Explores Mare Border

    Alan Shepard and Edgar Mitchell sample the adjacent Fra Mauro formation along the eastern margin of the mare.

Scientific Sources & References

Name Origin

"Sea that has become known." Ranger VII impact site.

Interactive Lunar Surface

Explore Mare Cognitum in 3D

Inspect lunar elevation data and the official selenographic position.