ATLAS SELENOGRAPHICUSSURFACE / RECORDS / EARTH

The lunar atlas.

Explore named terrain, illustrated geophysical layers, landing sites, and the Moon’s connection to Earth. Start with a layer; follow a feature.

01 / Lunar surface

Explore the surface

NASA surface imagery and selected lunar features. Other layers are conceptual illustrations.

SOURCED IMAGERY
01 / Optical atlasLROC · Study light
CopernicusTychoPlatoHypatiaTheophilusMare ImbriumMare TranquillitatisMontes ApenninusRima HyginusAristarchusGassendiArchimedesCleomedesTranquility Base (Statio Tranquillitatis)N
CopernicusSelected surface feature

North-up sphere · fixed study lighting, not today’s lunar phase. Marker sizes are symbolic; no terrain relief.

NASA / LROC · Image source
NASA SVS · LROC WAC color mosaic ↗

Ernie Wright / NASA’s Scientific Visualization Studio · 2025 · Public Domain

NASA LROC color mosaic adapted for visualization on a spherical surface. Manual inspection view, not computed libration or a view from a terrestrial location. Feature coordinates come from the site’s selected nomenclature catalogue. Markers are symbolic, not feature outlines. No elevation, temperature, or gravity raster is displayed in this optical view.

✦GRAVITAS LUNARIS
OBSERVED

GRAIL Bouguer Gravity Mascons

Mare Imbrium Mascon+340 mGal
Diameter: 1145 km · Crust Thickness: 6.2 km · Age: 3.85 Ga

The most prominent mass concentration on the near side. Dense mantle plug uplifted following giant impact, subsequently superloaded with 3–5 km of dense iron-rich flood basalt.

Mare Serenitatis Mascon+310 mGal
Diameter: 920 km · Crust Thickness: 8.5 km · Age: 3.87 Ga

Strong positive gravitational anomaly causing significant orbital perturbations for low-altitude spacecraft (discovered during Apollo 8 navigation).

Mare Crisium Mascon+280 mGal
Diameter: 740 km · Crust Thickness: 5.1 km · Age: 3.92 Ga

Isolated circular multi-ring basin surrounded by an intense negative gravity annular moat, indicative of unrelaxed flexural crustal stress.

✦RADIOMETRIA THERMALIS
OBSERVED

LRO Diviner Surface Radiometry

Equatorial Sub-Solar Noon395 K (122°C)
Direct zenith sunlight (Alpha_Sun = 90°)

Direct solar irradiance (~1361 W/m²) absorbed by low-albedo regolith; lack of atmosphere prevents convective cooling.

Equatorial Terminator Dawn/Dusk220 K (-53°C)
Grazing sunlight (Alpha_Sun = 0° to 5°)

Rapid radiative equilibrium drop as solar incident flux vector approaches tangent to surface.

Equatorial Midnight100 K (-173°C)
Deep lunar night (14 Earth days in darkness)

Unimpeded blackbody radiation to deep space (3K background); upper centimeters of porous dust insulate heat from depth.

02 / Landing records

Footprints on the Moon.

Chronological cartography of lunar landings, EVAs, coordinates, and sample return sites.

OBSERVED
Crewed (Human Footprints)Landed: 1969-07-20

Apollo 11

Tranquility Base (Statio Tranquillitatis)

Buzz Aldrin on the lunar surface, with the photographer reflected in his visor.
AS11-40-5903 / 1969

Buzz Aldrin at Tranquility Base, photographed by Neil Armstrong during the first lunar EVA.

Neil Armstrong / NASA · NASA Image and Video Library
0.674° Lat, 23.473° Long (Nearside)
Crew / Vehicle: Neil Armstrong, Buzz Aldrin
Historical Milestone

First human footprints on another celestial body; proved operational capability of crewed lunar landing and return.

Humanity's first extraterrestrial landing. LM Eagle landed with 25 seconds of fuel remaining in southwestern Mare Tranquillitatis.

Surface Instrumentation Package
EASEPLaser Ranging RetroreflectorSolar Wind Composition ExperimentPassive Seismic Experiment
Surface Duration: 21.6 Hours
Sample Mass: 21.55 kg returned
03 / Earth horizons
Earth / Lunar horizon

The Moon from here.

One Moon. A different horizon at every longitude.

Computed snapshot · UTC
North up · Equirectangular180° W — 180° E
Sub-lunar pointSelected stationAbove horizon
Directly beneath the Moon Geocentric, spherical-Earth reference—
Map source & calculation notes
Natural Earth land, 1:110 million ↗

Natural Earth contributors; Tom Patterson and Nathaniel Vaughn Kelso. Public Domain. Natural Earth 4.1.0 geography redistributed by world-atlas. Equirectangular projection with antimeridian clipping; generalized coastlines, not navigation-grade.

Coordinates: Astronomy Engine, apparent equator of date. Station altitudes use observer-specific parallax and standard refraction at sea level. Snapshot refreshes each minute while this page is visible.

Natural Earth usage terms ↗
04 / Sample archive

Fragments of another world.

Petrology, radiometric isochron ages, and thin sections for curated lunar rock specimens brought to Earth.

OBSERVED
Cataloged Specimens
NASA #15415Ferroan Anorthosite
Collected: 1971-08-01

Genesis Rock

Apollo 15

Lunar sample 15415, the pale Genesis Rock, photographed in the Lunar Receiving Laboratory.
S71-42955 / 1971

Sample 15415 in the Lunar Receiving Laboratory after its return aboard Apollo 15.

NASA · NASA Image and Video Library
Hadley-Apennine (Spur Crater, Station 7) (26.132° N, 3.634° E)
Collected by: David Scott, James Irwin · Mass: 269.4 grams
Geological Breakthrough

The definitive physical evidence for the Lunar Magma Ocean hypothesis—a relic of the primordial crust that floated to the top of a molten Moon 4.5 billion years ago.

Primary Mineral Assemblage
Plagioclase Feldspar (Anorthite 98%)Pyroxene (1.5%)Olivine (0.5%)
Petrographic Thin-Section Analysis

Granulitic anorthosite composed almost entirely of calcic plagioclase with complex deformation twinning and shock fractures.

Radiometric Age: 4.46 Billion Years (Sm-Nd internal isochron (Norman et al. 2003))
NASA Astromaterials File
✦CORPUS SCIENTIAE LUNARIS • KNOWLEDGE GRAPH

Inquiry Knowledge Graph & AEO Questions

Hierarchical recursive search tree with atomic passages and peer-reviewed academic research citations.

Exploratory Research

Market Observatory & Evidence Limits

Modeled / Tradition

Corporate Chart Candidates & Interpretation

Chronobiology

Chronobiology & Lunar Biological Rhythms

Almanac Science

Biodynamic Lunar Gardening & Sap Dynamics

Astrometry

Astrometric Coordinates: Tropical vs. Sidereal & Constellations