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Explore our planet through photography and imagery, including climate change and water all the way back to the 1800s when the USGS was surveying the country by horse and buggy.

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Image: Deadwood Formation in Deadwood, SD
Deadwood Formation in Deadwood, SD
Deadwood Formation in Deadwood, SD
Deadwood Formation in Deadwood, SD

Towering cliff of the Deadwood Formation in Deadwood, SD. The Deadwood Formation consists mostly of sandstone and shale.

Towering cliff of the Deadwood Formation in Deadwood, SD. The Deadwood Formation consists mostly of sandstone and shale.

Fish seining efforts on the Colorado River
Fish seining efforts on the Colorado River
Fish seining efforts on the Colorado River
Fish seining efforts on the Colorado River

Fish seining efforts on the Colorado River

Image: Grace Coolidge Creek, SD
Grace Coolidge Creek, SD
Grace Coolidge Creek, SD
Grace Coolidge Creek, SD

Grace Collidge Creek above loss zone in southern Black Hills of South Dakota.

Grace Collidge Creek above loss zone in southern Black Hills of South Dakota.

Image: Gypsum Layer in Spearfish Formation, SD
Gypsum Layer in Spearfish Formation, SD
Gypsum Layer in Spearfish Formation, SD
Gypsum Layer in Spearfish Formation, SD

Spearfish Formation near Spearfish, SD. The Spearfish Formation is a red, silty shale with interbedded red sandstone and siltstone. The formation contains massive gypsum deposits, which is the white layer in the photograph.

Spearfish Formation near Spearfish, SD. The Spearfish Formation is a red, silty shale with interbedded red sandstone and siltstone. The formation contains massive gypsum deposits, which is the white layer in the photograph.

Image: Iron Bog near Rochford, SD
Iron Bog near Rochford, SD
Iron Bog near Rochford, SD
Iron Bog near Rochford, SD

Naturally occuring bog-iron area near Rochford, SD, in the Black Hills of western South Dakota.

Naturally occuring bog-iron area near Rochford, SD, in the Black Hills of western South Dakota.

Image: Madison Limestone in Spearfish Canyon, SD
Madison Limestone in Spearfish Canyon, SD
Madison Limestone in Spearfish Canyon, SD
Madison Limestone in Spearfish Canyon, SD

Outcrop of the Madison Limestone in Spearfish Canyon in the northern Black Hills of South Dakota. The Madison Limestone is a massive, gray to buff limestone with some dolomite.

Outcrop of the Madison Limestone in Spearfish Canyon in the northern Black Hills of South Dakota. The Madison Limestone is a massive, gray to buff limestone with some dolomite.

Image: Minnelusa Formation at Ranch A near Beulah, WY
Minnelusa Formation at Ranch A near Beulah, WY
Minnelusa Formation at Ranch A near Beulah, WY
Minnelusa Formation at Ranch A near Beulah, WY

Outcrop of the Minneslua Formation at Ranch A near Beulah, Wyoming. The Minnelusa Formation consists mostly of yellow to red sandstone, limestone, dolomite, and shale.

Outcrop of the Minneslua Formation at Ranch A near Beulah, Wyoming. The Minnelusa Formation consists mostly of yellow to red sandstone, limestone, dolomite, and shale.

Image: Mt. Coolidge Area, Custer State Park, SD, 2001
Mt. Coolidge Area, Custer State Park, SD, 2001
Mt. Coolidge Area, Custer State Park, SD, 2001
Mt. Coolidge Area, Custer State Park, SD, 2001

Photograph taken in 2001 of Mt. Coolidge area in Black Hills of western South Dakota. The area was burned by the Galena Fire in 1988, which burned approximately 17,000 acres in Custer State Park.

Photograph taken in 2001 of Mt. Coolidge area in Black Hills of western South Dakota. The area was burned by the Galena Fire in 1988, which burned approximately 17,000 acres in Custer State Park.

Image: Precambrian Rocks in the Black Hills, SD
Precambrian Rocks in the Black Hills, SD
Precambrian Rocks in the Black Hills, SD
Precambrian Rocks in the Black Hills, SD

Precambrian rocks in the Black Hills of South Dakota. Precambrian rocks form the central crystalline core of the Black Hills. Fracturing and weathering in Precambrian rocks affect the availability of water in this unit.

Precambrian rocks in the Black Hills of South Dakota. Precambrian rocks form the central crystalline core of the Black Hills. Fracturing and weathering in Precambrian rocks affect the availability of water in this unit.

Image: Sand Creek at Ranch A near Beulah, WY
Sand Creek at Ranch A near Beulah, WY
Sand Creek at Ranch A near Beulah, WY
Sand Creek at Ranch A near Beulah, WY

Sand Creek at Ranch A near Beulah, Wyoming.

Image: Spearfish Creek, SD
Spearfish Creek, SD
Spearfish Creek, SD
Spearfish Creek, SD

Spearfish Creek in the northern Black Hills of South Dakota.

Spearfish Creek in the northern Black Hills of South Dakota.

Image: Spring above Rhoads Fork, SD
Spring above Rhoads Fork, SD
Spring above Rhoads Fork, SD
Spring above Rhoads Fork, SD

Headwater springflow is common in the Limestone Pateau area in the Black Hills of western South Dakota. Most headwater springs in the Black Hills, like this one contributing to Rhoads Fork, generally occur near the base of the Madison Limestone along the eastern edge of the Limestone Plateau area.

Headwater springflow is common in the Limestone Pateau area in the Black Hills of western South Dakota. Most headwater springs in the Black Hills, like this one contributing to Rhoads Fork, generally occur near the base of the Madison Limestone along the eastern edge of the Limestone Plateau area.

Plant foliage samples being placed in direct sunlight for water extraction by solar distillation
Plants Being Placed in Direct Sunlight for Water Extraction
Plants Being Placed in Direct Sunlight for Water Extraction
Plants Being Placed in Direct Sunlight for Water Extraction

Plant foliage samples being placed in direct sunlight for water extraction by solar distillation. Water vapor released from the foliage condenses as liquid on the inside surface of the sample bag.

Plant foliage samples being placed in direct sunlight for water extraction by solar distillation. Water vapor released from the foliage condenses as liquid on the inside surface of the sample bag.

Image: Landslide Sampling
Landslide Sampling
Landslide Sampling
Landslide Sampling

Scientist Jonathan Godt samples a landslide headscarp in Alameda County, CA.

Scientist Jonathan Godt samples a landslide headscarp in Alameda County, CA.

The South Branch Raritan River at High Bridge gage
High Bridge Gage House 1
High Bridge Gage House 1
High Bridge Gage House 1

Split brick and wood stilling well gage house on the bank of the South Branch Raritan River near High Bridge, New Jersey

Split brick and wood stilling well gage house on the bank of the South Branch Raritan River near High Bridge, New Jersey

Image: Ayers Rock (Uluru)
Ayers Rock (Uluru)
Ayers Rock (Uluru)
Ayers Rock (Uluru)

Ayers Rock (Uluru) and vegetation.

Ayers Rock (Uluru) and vegetation.

Image: Rocks and Vegetation
Rocks and Vegetation
Rocks and Vegetation
Rocks and Vegetation

An array of rocks with vegetation interspersed.

An array of rocks with vegetation interspersed.

National Aerial Photography Program (NAPP) - Little Rock, AR - CIR
National Aerial Photography Program (NAPP) - Little Rock, AR - CIR
National Aerial Photography Program (NAPP) - Little Rock, AR - CIR
National Aerial Photography Program (NAPP) - Little Rock, AR - CIR

National Aerial Photography Program (NAPP) - Little Rock, AR - Color Infrad - March 25, 2001

Mount Baker, aerial view to the northeast....
Mount Baker, aerial view to NE.
Mount Baker, aerial view to NE.
Mount Baker, aerial view to NE.

Mount Baker, aerial view to the northeast.

Sherman Crater, to the left of the true summit, at Mount Baker, Was...
Sherman Crater, to left of the true summit, at Mount Baker, WA
Sherman Crater, to left of the true summit, at Mount Baker, WA
Sherman Crater, to left of the true summit, at Mount Baker, WA

Sherman Crater, to the left of the true summit, at Mount Baker, Washington, aerial view to the northwest.

Sherman Crater, to the left of the true summit, at Mount Baker, Washington, aerial view to the northwest.

Image: Stream Bordered by Snow-Covered Trees and Low-Lying Vegetation
Stream Bordered by Snow-Covered Trees and Low-Lying Vegetation
Stream Bordered by Snow-Covered Trees and Low-Lying Vegetation
Stream Bordered by Snow-Covered Trees and Low-Lying Vegetation

Snow covers the coniferous trees and low-lying vegetation on either side of a calm stream.

Snow covers the coniferous trees and low-lying vegetation on either side of a calm stream.