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CARTOLOGIUMThe living atlas
Survey desk + sources & coordinates
WGS 84

WAYS OF MAPPING / BEYOND EARTH

A Moon
made of
maps.

A familiar face becomes a landscape, a measured surface, a history. Change the map. Keep the world.

Compare the lunar surface
I / A WORLD, INTERPRETEDMOON · 2020
One world. Many ways of knowing.The near side, classified by geology and drawn over relief. NASA/GSFC/USGS, 2020.
NASA / GSFC / USGSSource & rights +

Orthographic projections of the Unified Geologic Map of the Moon. USGS Astrogeology Science Center.

The USGS media record explicitly marks this image Public Domain. Original credit: NASA/GSFC/USGS. The 2020 release illustration is distinct from the subsequently corrected version 2 GIS dataset.

Open source record ↗Open original source file ↗

The familiar face becomes a place.

The Moon is easy to recognize and harder to read. From a distance, its light and dark patches make a face. In a map, those patches become places that can be compared, measured and interpreted. The change begins with a question: what kind of evidence does this image offer?

The camera view below comes from a 2015 USGS map assembled from the Lunar Reconnaissance Orbiter’s Wide Angle Camera. Many observations become one continuous mosaic. Its companion sheet uses measurements from the Lunar Orbiter Laser Altimeter, or LOLA, to describe surface elevation. The same ground appears in two different visual languages.

II / SAME TERRAIN, DIFFERENT EVIDENCEUSGS · 2015
ELEVATION ← / → CAMERANORTH ↑
65°W → 65°E50°N → 50°S
READ THIS WINDOW

Central near side

Look for broad dark plains in the camera mosaic. Reveal elevation to compare their shapes with the surrounding higher terrain.

Two reading copies from USGS SIM 3316: LRO camera imagery and LOLA-derived elevation. Both use the published Mercator extent, with 0° at the central meridian. The divider reveals a change of representation, not a change through time. Source labels are omitted; this overview is not a pixel-precise terrain analysis.
Read the frame and source dates
Body / coordinates
Moon · mean Earth/polar axis (ME) · DE421-derived orientation · east-positive longitude · planetocentric latitude.
Projection / reference
Mercator; central meridian 0°, true scale at 0° latitude. Reference radius 1,737.4 km. Full panel: 180°W–180°E, 57°S–57°N.
Dates / scope
Published 2015. LOLA heights: July 2009–July 2013. Camera mosaic: many observations, not a single exposure or live view. Mercator stretches high latitudes and excludes the poles.
USGS / NASA / ASU · Hare and colleaguesSource & rights +

Lunar camera mosaic — SIM 3316, sheet 1. USGS Scientific Investigations Map 3316.

USGS-produced map, public domain in the United States under the USGS information policy. The inspected sheets carry no separate copyright notice. Credit retains NASA, ASU and the map authors. This reading copy does not imply endorsement.

Open source record ↗Open original source file ↗
USGS / NASA / ASU · Hare and colleaguesSource & rights +

Lunar elevation and shaded relief — SIM 3316, sheet 2. USGS Scientific Investigations Map 3316.

USGS-produced map, public domain in the United States under the USGS information policy. The inspected sheets carry no separate copyright notice. Credit retains NASA, ASU and the map authors. This reading copy does not imply endorsement.

Open source record ↗Open original source file ↗

Camera mosaic / elevation: Central near side

Start in the central near-side window. Follow a dark plain, then reveal the blue elevation map over it. Its outline may remain recognizable while its meaning changes. Darkness in a camera image is not a height measurement; blue in this map is a choice in an elevation key.

The broad dark maria are volcanic plains. Their name, inherited from the Latin for seas, preserves an earlier way of imagining the Moon. Here, the comparison helps separate the named landscape, its appearance and its topography. None is a substitute for the others.

There is a zero. It is not sea level.

An elevation map needs a reference. On this sheet, heights are measured above or below a sphere with a radius of 1,737.4 kilometres. Blue areas lie lower in that system. The color does not mean there is an ocean waiting at the bottom.

III / WHERE IS ZERO?ORIGINAL DIAGRAM
Below the referenceAbove the reference
The map’s zero is a sphere with a radius of 1,737.4 km. Elevation is the difference between the measured surface radius and that reference. This section explains the convention; it is not a terrain profile.
Original elevation legend, in metres relative to a 1,737.4 km reference sphere: approximately −9,130 to +10,780 metres

Source legend in metres. Blue indicates lower elevations; it does not indicate water. Approximate source range: −9.13 to +10.78 km.

Enlarge the original color key
Original elevation legend, in metres relative to a 1,737.4 km reference sphere: approximately −9,130 to +10,780 metres
USGS / NASA / ASU · Hare and colleaguesSource & rights +

Elevation legend — SIM 3316, sheet 2. USGS Scientific Investigations Map 3316.

USGS-produced map, public domain in the United States under the USGS information policy. The inspected sheets carry no separate copyright notice. Credit retains NASA, ASU and the map authors. This reading copy does not imply endorsement.

Open source record ↗Open original source file ↗

Relief adds another choice. The source’s shading uses an imagined light from the west, 45° above the horizontal, with no vertical exaggeration. It helps the eye read shape. It is not a record of sunlight at the moment you open this page. Color describes height; shading helps describe form.

Choose the Orientale window and follow its rings. Then choose Imbrium and compare the broad interior with its surrounding terrain. These are reading windows in a published map, not new surveys. The colored raster does not provide a trustworthy height for every pointer position, so this viewer offers no invented elevation readout.

Before asking “how high?”, ask “above what?”

The coordinate frame matters too. These sheets use the Moon’s mean Earth/polar axis frame, planetocentric latitude and east-positive longitude. Their Mercator panel stops at 57° north and south; the original publication supplies separate polar views. A familiar rectangular map shape does not make this Earth’s coordinate system.

A colored boundary makes a claim.

The geological Moon introduces a third kind of reading. A colored region represents a mapped unit; a line locates a contact or another mapped feature. The colors ask us to read a surface as a history, using the map’s unit descriptions and symbols.

IV / READ THE SURFACE AS HISTORY2020 RELEASE

Near side

Far side

The near and far sides of the Moon. Geological colors classify mapped units; the relief underneath comes from LOLA. 2020 release illustration. Read unit names and symbols in the full map and legend before assigning an age or material to a colored region.
NASA / GSFC / USGSSource & rights +

Orthographic projections of the Unified Geologic Map of the Moon. USGS Astrogeology Science Center.

The USGS media record explicitly marks this image Public Domain. Original credit: NASA/GSFC/USGS. The 2020 release illustration is distinct from the subsequently corrected version 2 GIS dataset.

Open source record ↗Open original source file ↗

The 2020 Unified Geologic Map brought six Apollo-era regional maps into a common scheme, alongside newer observations. Its authors describe reconciling units, joining regional boundaries and mapping surface features consistently. That work makes comparisons possible across regions that had previously been described in different ways.

Compare the two hemispheres above without assigning an age from color alone. Where do broad regions dominate? Where do circular forms interrupt them? Those observations can guide a closer look, but the legend supplies the unit meanings. A bright patch is not automatically a young crater, and a shared hue across unrelated maps need not mean the same thing.

A map also has its own history. The source record documents a later version 2 correction to polygon alignment and contact visibility. The illustration shown here is the 2020 release image, not a fresh rendering of that corrected GIS dataset. Readers who need the analytical data should follow the versioned record.

Read one place, three ways.

Return to Imbrium. Describe its appearance in the camera mosaic, then its form in the elevation view. Finally locate it toward the upper-left part of the near-side geological globe and open the full source legend. Keep three separate notes: what you can see, what the elevation map encodes, and what the geological map interprets.

Return to the comparison ↑

This is how the atlas can leave Earth without losing its method. Name the body, declare the frame, identify the evidence and keep the source within reach. A new world becomes readable through several maps held in conversation.

Sources and method.

The two comparison rasters are extracted from the equatorial Mercator panels of USGS Scientific Investigations Map 3316. They share the published extent, central meridian and latitude limits. A Mercator calculation places each reading window. Resampling creates lightweight display copies; source labels are omitted. This is an overview comparison, with no claim of pixel-level registration, local terrain analysis or landing suitability.

The elevation sheet incorporates LOLA measurements from July 2009 through July 2013 and uses interpolation between some tracks. Its publication date is 2015. The geological image is a separately sourced orthographic illustration from 2020. These dates identify different products and processes; switching maps does not show lunar change over time.

Every reproduced plate has a source and rights disclosure. The maps retain their original palettes in both themes. The datum section is an original explanation, and the social artwork is an original schematic. Neither supplies additional lunar measurements.

  1. Hare, T. M., Hayward, R. K., Blue, J. S., Archinal, B. A., Robinson, M. S., Speyerer, E. J., Wagner, R. V., Smith, D. E., Zuber, M. T., Neumann, G. A., & Mazarico, E. (2015). Image mosaic and topographic map of the Moon (Scientific Investigations Map 3316, 2 sheets). U.S. Geological Survey. https://doi.org/10.3133/sim3316

    Inspect the source
  2. Fortezzo, C. M., Spudis, P. D., & Harrel, S. L. (2020). Release of the digital unified global geologic map of the Moon at 1:5,000,000-scale [Abstract 2760]. 51st Lunar and Planetary Science Conference. https://www.hou.usra.edu/meetings/lpsc2020/pdf/2760.pdf

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  3. U.S. Geological Survey. (2020). Unified geologic map of the Moon (Version 2) [Geologic map and GIS dataset]. Astropedia. https://astrogeology.usgs.gov/search/map/Moon/Geology/Unified_Geologic_Map_of_the_Moon_GIS_v2

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  4. U.S. Geological Survey. (2015, October 15). Visit the Moon without leaving your desk. https://www.usgs.gov/news/featured-story/visit-moon-without-leaving-your-desk

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  5. NASA/GSFC/USGS. (2020). Orthographic projections of the Unified Geologic Map of the Moon [Geologic visualization]. U.S. Geological Survey. https://www.usgs.gov/media/images/orthographic-projections-unified-geologic-map-moon

    Inspect the image record

Editorial text and original diagrams © Cartologium. Source maps retain their public-domain status in the United States and their individual credits. Prepared 11 October 2026.