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GIS Data

USGS is a primary source of geographic information system (GIS) data. Our data and information is presented in spatial and geographic formats, including The National Map, Earth Explorer, GloVIS, LandsatLook, and much more. Explore GIS Data Maps. 

Filter Total Items: 9494

Geologic map of the Northport Quadrangle, Washington

No abstract available.

Geologic map of the Oppolzer A region of the Moon Lunar Orbiter Site II P-8, Sinus Medii including Apollo landing sites 3 and 3R

The map shows the regional geology of the Oppolzer A region of the moon, where potential Apollo landing sites 3 and 3R are located. Site 3R includes a prominent mare ridge and is of greater scientific interest (Trask, 1969). The Oppolzer A region is in Sinus Medii, near the center of the lunar earthside hemisphere; it is also important because surveyor VI successfully landed near the proposed Apol

Geologic map of the Orocovis Quadrangle, Puerto Rico

No abstract available.

Geologic map of the Owyhee Quadrangle, Nevada-Idaho

No abstract available.

Geologic map of the Rheita Quadrangle of the Moon

Photographs returned by unmanned Lunar Orbiters have contributed greatly to the current lunar geologic mapping program. This is particularly true for quadrangles near the limbs, such as Rheita in the southeast earthside quadrant. The new data and revised interpretations amend the geologic framework established by earlier workers (Shoemaker (1962) and Shoemaker and Hackman (1962) applied basic stra

Geologic map of the Rupes Altai Quadrangle of the Moon

The Rupes Altai quadrangle of the Moon is in the rugged, cratered terra of the southeastern earthside hemisphere. East-northeast of the quadrangle lies Mare Nectaris, approximately 350 km in diameter, and near the northeast corner is the crater Theophilus. Rupes Altai (the Altai scarp) divides the quadrangle into two markedly different morphologic provinces. To the west, complexly overlapping, fra

Geologic map of the Sabine EB region of the Moon

The Sabin EB region is a rolling plain which consists entirely of crater and mare materials. The areal density of craters, though variable within the region, is sufficiently high so that the craters are the dominant morphological feature. Crater morphology ranges from bright, sharp-rimmed craters to pan-shaped depressions. Superposition relations indicate that the bright-rimmed craters (unit br) a