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(LAC-40) Geologic map and section of the Timocharis region of the Moon (LAC-40) Geologic map and section of the Timocharis region of the Moon

Material exposed on the surface of the Moon is heterogeneous. The albedo and other physical characteristics that have been determined with the use of optical and radio telescopes vary from one part of the Moon to another, and the variations are particular correlated with differences in topography. Discontinuities in the areal variation permit the surface material to be divided into map...

(LAC-41) Geologic map of the Montes Apenninus region of the Moon (LAC-41) Geologic map of the Montes Apenninus region of the Moon

Material exposed on the surface of the Moon is heterogeneous. The albedo and other physical characteristics that have been determined with the use of optical and radio telescopes vary from one part of the Moon to another, and the variations are partially correlated with differences in topography. Discontinuities in the areal variation permit the surface material to be divided into map...

(LAC-42) Geologic map of the Mare Serenitatis region of the moon (LAC-42) Geologic map of the Mare Serenitatis region of the moon

The surface of the Moon is heterogeneous. Surface materials are classed on the basis of telescopic observations into map units, each having lateral continuity and a limited range of physiographic characteristics and optical properties (mainly polarization and albedo, the reflectivity under full moon illumination). Such units are analogous to the rock-stratigraphic formations of...

(LAC-58) Geologic map of the Copernicus quadrangle of the moon (LAC-58) Geologic map of the Copernicus quadrangle of the moon

The surface of the Moon is heterogeneous both on a regional and a fine scale. The geologic mapping of this surface is similar in principle to the geologic mapping of the Earth's surface and depends on the discrimination of similarities and differences between materials and features at different points on the surface. Differences from area to area in characteristic topographic forms and...

(LAC-60) Geologic map of the Julius Caesar quadrangle of the moon (LAC-60) Geologic map of the Julius Caesar quadrangle of the moon

The surface of the moon is heterogeneous. Surface materials are classed on the basis of telescopic observations into units each having a limited range of physical properties such as topography, visible under low-illumination and albedo, the reflectivity under full-Moon illumination. Such units are considered analogous to the rock-stratigraphic formations of terrestrial geology. By...

(LAC-75) Geologic map and sections of the Letronne region of the moon (LAC-75) Geologic map and sections of the Letronne region of the moon

Material exposed on the surface of the moon is heterogeneous. The albedo and other physical characteristics that have been determined with the use of optical and radio telescopes vary from one part of the moon to another, and the variations are patially correlated with differences in topography . Discontinuities in the areal variation permit the surfaces material to be divided into map...
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