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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. 

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Map of distal flow field

This large-scale map uses a satellite image acquired in March 2014 (provided by Digital Globe) as a base to show the area around the front of Kīlauea’s active East Rift Zone lava flow.

By
Volcano Hazards Program, Hawaiian Volcano Observatory, Kīlauea

Small-scale map of flow field

This small-scale map shows Kīlauea’s active East Rift Zone lava flow in relation to lower Puna. 

By
Volcano Hazards Program, Hawaiian Volcano Observatory, Kīlauea

Large-scale map of flow field

This large-scale map shows the distal part of Kīlauea’s active East Rift Zone lava flow in relation to nearby Puna communities.

By
Volcano Hazards Program, Hawaiian Volcano Observatory, Kīlauea

Thermal overlay of distal part of flow field

This map overlays a georegistered mosaic of thermal images collected during a helicopter overflight of the distal part of Kīlauea’s active East Rift Zone lava flow on February 19 at about 10:30 AM. 

By
Volcano Hazards Program, Hawaiian Volcano Observatory, Kīlauea

Map of distal part of flow field

This large-scale map uses a satellite image acquired in March 2014 (provided by Digital Globe) as a base to show the area around the front of Kīlauea’s active East Rift Zone lava flow. 

By
Volcano Hazards Program, Hawaiian Volcano Observatory, Kīlauea

Potentiometric surface, 2013, and water-level differences, 1991-2013, of the Carrizo-Wilcox aquifer in northwest Louisiana

The Carrizo-Wilcox aquifer is the primary source of fresh groundwater for public supply as well as industrial, agricultural, and domestic uses in several parishes in northwestern Louisiana, including Bienville, Bossier, Caddo, De Soto, Natchitoches, Red River, Sabine, and Webster. In 2010, about 19 million gallons per day (Mgal/d) were withdrawn from the Carrizo-Wilcox aquifer in Louisiana. This i
By
Water Resources Mission Area, Lower Mississippi-Gulf Water Science Center

Satellite image of area around front of Kīlauea’s East Rift Zone lava flow

This satellite image was captured on Saturday, February 14, by the Advanced Land Imager instrument onboard NASA's Earth Observing 1 satellite.

By
Volcano Hazards Program, Hawaiian Volcano Observatory, Kīlauea

Thermal overlay of distal part of flow field

This map overlays a georegistered mosaic of thermal images collected during a helicopter overflight of the distal part of Kīlauea’s active East Rift Zone lav£a flow on February 10 at about 12:30 PM. 

By
Volcano Hazards Program, Hawaiian Volcano Observatory, Kīlauea

Small-scale map of Kīlauea’s East Rift Zone lava flow

This small-scale map shows Kīlauea’s active East Rift Zone lava£ flow in relation to lower Puna. 

By
Volcano Hazards Program, Hawaiian Volcano Observatory, Kīlauea

Large-scale map of Kīlauea’s East Rift Zone lava flow

This large-scale map shows the distal part of Kīlauea’s active East Rift Zone lava flow in relation to nearby Puna communities.

By
Volcano Hazards Program, Hawaiian Volcano Observatory, Kīlauea

Satellite image of area around front of Kīlauea’s East Rift Zone lava flow

This large-scale map uses a satellite image acquired in March 2014 (provided by Digital Globe) as a base to show the area around the front of Kīlauea’s active East Rift Zone lava flow. 

By
Volcano Hazards Program, Hawaiian Volcano Observatory, Kīlauea

Bedrock geologic map of the Spring Valley, West Plains, and parts of the Piedmont and Poplar Bluff 30'x60' quadrangles, Missouri, including the upper Current River and Eleven Point River drainage basins

This map covers the drainage basins of the upper Current River and the Eleven Point River in the Ozark Plateaus physiographic province of southeastern Missouri. The two surface drainage basins are contiguous in their headwaters regions, but are separated in their lower reaches by the lower Black River basin in the southeast corner of the map area. Numerous dye-trace studies demonstrate that in the
By
Florence Bascom Geoscience Center