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California Water Science Center Images

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a green Anza Valley with mountains in the background
Anza Valley, CA
Anza Valley, CA
Anza Valley, CA

Groundwater is the sole source for water use to the rural community and two Native American tribes in the Cahuilla Valley and Terwilliger Valley groundwater basins, which are located approximately 35 miles southwest of Palm Springs, California.

Groundwater is the sole source for water use to the rural community and two Native American tribes in the Cahuilla Valley and Terwilliger Valley groundwater basins, which are located approximately 35 miles southwest of Palm Springs, California.

Illustration of the aquifer compaction process.
Aquifer Compaction
Aquifer Compaction
Aquifer Compaction

Fine-grained sediments (clays and silts) within an aquifer system are the main culprits in land subsidence due to groundwater pumping. Fine-grained sediments are special because they are composed of platy grains. When fine-grained sediments are originally deposited, they tend to be deposited in random orientations.

Fine-grained sediments (clays and silts) within an aquifer system are the main culprits in land subsidence due to groundwater pumping. Fine-grained sediments are special because they are composed of platy grains. When fine-grained sediments are originally deposited, they tend to be deposited in random orientations.

Image: Land Subsidence in the San Joaquin Valley
Land Subsidence in the San Joaquin Valley
Land Subsidence in the San Joaquin Valley
Land Subsidence in the San Joaquin Valley

Approximate point of maximum subsidence in the San Joaquin Valley, California. Land surface subsided ~9 m from 1925 to 1977 due to aquifer-system compaction. Signs on the telephone pole indicate the former elevations of the land surface in 1925 and 1955.

Photograph by Richard Ireland, U.S. Geological Survey

Approximate point of maximum subsidence in the San Joaquin Valley, California. Land surface subsided ~9 m from 1925 to 1977 due to aquifer-system compaction. Signs on the telephone pole indicate the former elevations of the land surface in 1925 and 1955.

Photograph by Richard Ireland, U.S. Geological Survey

black doors with windows that have writing on them
Hooe Building
Hooe Building
Hooe Building

The Hooe Building

Location

  • Address: 16th Street NW, Washington, D.C., at the corner of 16th and H Streets NW.
  • Current Reference: The site is now known as the Hooe Building (Historical).

Historical Background

The Hooe Building

Location

  • Address: 16th Street NW, Washington, D.C., at the corner of 16th and H Streets NW.
  • Current Reference: The site is now known as the Hooe Building (Historical).

Historical Background

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