Glassy, fresh pillow basalt flow at the NESCA site, northern half of Escanaba Trough.
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Glassy, fresh pillow basalt flow at the NESCA site, northern half of Escanaba Trough.
Older, oxidized sulfide deposit colonized by sponges at SESCA site, southern half of Escanaba Trough.
Older, oxidized sulfide deposit colonized by sponges at SESCA site, southern half of Escanaba Trough.
Sulfide mound and talus at NESCA site. Rectangular marker at center of photograph is 15 by 30 cm
linkSulfide mound and talus at NESCA site, northern half of Escanaba Trough. Rectangular marker at center of photograph is 15 by 30 cm.
Sulfide mound and talus at NESCA site. Rectangular marker at center of photograph is 15 by 30 cm
linkSulfide mound and talus at NESCA site, northern half of Escanaba Trough. Rectangular marker at center of photograph is 15 by 30 cm.
Photo shows the side of an actively venting massive sulfide chimney colonized by tube worms and palm worms.
Photo shows the side of an actively venting massive sulfide chimney colonized by tube worms and palm worms.
Tube worms and anemones colonize massive sulfide talus where diffuse hydrothermal venting is occurring
linkPhoto shows tube worms and anemones colonizing massive sulfide talus where diffuse hydrothermal venting is occurring.
Tube worms and anemones colonize massive sulfide talus where diffuse hydrothermal venting is occurring
linkPhoto shows tube worms and anemones colonizing massive sulfide talus where diffuse hydrothermal venting is occurring.
Photo shows side of sulfide mound showing cluster of tube worms, anemones, and bacterial mats.
Photo shows side of sulfide mound showing cluster of tube worms, anemones, and bacterial mats.
Hydrothermal deposits (primarily barite) adjacent to site of active venting. Shiny black material is possibly pyrobitumen.
Hydrothermal deposits (primarily barite) adjacent to site of active venting. Shiny black material is possibly pyrobitumen.
Dynaphot photomicrographs of foraminifers from Escanaba Trough. A-D, Rhabdammina sp.
Dynaphot photomicrographs of foraminifers from Escanaba Trough. A-D, Rhabdammina sp.
Sea Beam bathymetric map of Escanaba Trough from 1985. A, Northern half. B, Southern half. Contour interval is 50 m; each color change represents 100 m. Yellow indicates areas of no data.
Sea Beam bathymetric map of Escanaba Trough from 1985. A, Northern half. B, Southern half. Contour interval is 50 m; each color change represents 100 m. Yellow indicates areas of no data.
Topographic map of the Cape Flattery region (U.S. Geological Survey Cape Flattery Quadrangle, 15-min series).
Topographic map of the Cape Flattery region (U.S. Geological Survey Cape Flattery Quadrangle, 15-min series).
George Tate playfully brandishes a grappling hook in a boat in Cook Inlet, Alaska, 1978. The driver (not shown) and George are about to motor away from the research vessel Sea Sounder to drag for the large tripod dubbed the Geoprobe. The apparatus had not deployed its recovery float and line, so the scientists had to try to hook it up off the seafloor.
George Tate playfully brandishes a grappling hook in a boat in Cook Inlet, Alaska, 1978. The driver (not shown) and George are about to motor away from the research vessel Sea Sounder to drag for the large tripod dubbed the Geoprobe. The apparatus had not deployed its recovery float and line, so the scientists had to try to hook it up off the seafloor.
Three pioneers of USGS geological studies, in 1965, from left to right: Parke D. Snavely, Jr., Robert E. Wallace, and Thomas W. Dibblee, in front of a 1964 Cessna 182G Skylane.
Three pioneers of USGS geological studies, in 1965, from left to right: Parke D. Snavely, Jr., Robert E. Wallace, and Thomas W. Dibblee, in front of a 1964 Cessna 182G Skylane.
Photograph taken in 1964 of the main part of the Chenega village site in Alaska. Pilings in the ground mark the former locations of homes swept away by tsunami waves. The schoolhouse on high ground was undamaged.
Photograph taken in 1964 of the main part of the Chenega village site in Alaska. Pilings in the ground mark the former locations of homes swept away by tsunami waves. The schoolhouse on high ground was undamaged.
Aftermath of the 1960 Chilean tsunami in Hilo, Hawaii, where the tsunami caused 61 deaths.
Aftermath of the 1960 Chilean tsunami in Hilo, Hawaii, where the tsunami caused 61 deaths.
Front of the Wm. Wrigley Jr. Co. building in 1955, now home to the USGS Pacific Coastal and Marine Science Center.
Front of the Wm. Wrigley Jr. Co. building in 1955, now home to the USGS Pacific Coastal and Marine Science Center.
The Escanaba was built by Western Pipe and Steel Company in San Pedro, California, and began sailing in 1946. This 255-foot gunboat operated from its homeport in Alameda, California, until it was decommissioned in 1954.
The Escanaba was built by Western Pipe and Steel Company in San Pedro, California, and began sailing in 1946. This 255-foot gunboat operated from its homeport in Alameda, California, until it was decommissioned in 1954.
In 1932, the U.S. Coast Guard commissioned the construction of a 165-foot, 1,500-horsepower ship in Bay City, Michigan. This was the U.S. Coast Guard Cutter (USCGC) Escanaba.
In 1932, the U.S. Coast Guard commissioned the construction of a 165-foot, 1,500-horsepower ship in Bay City, Michigan. This was the U.S. Coast Guard Cutter (USCGC) Escanaba.
View of John Muir School on Pacific Avenue in Long Beach, California, showing damage from the March 10, 1933 Long Beach earthquake. Photo taken 8 days after the earthquake, on March 18, 1933. Photo by W.L. Huber, USGS.
View of John Muir School on Pacific Avenue in Long Beach, California, showing damage from the March 10, 1933 Long Beach earthquake. Photo taken 8 days after the earthquake, on March 18, 1933. Photo by W.L. Huber, USGS.
One of the most well-known photographs by George R. Lawrence, taken May 28, 1906, about 6 weeks after the Great San Francisco earthquake which occurred on April 18. The 160-degree panorama was taken from a camera suspended from a kite 2,000 feet in the air. The view looks up Market Street with the waterfront and Union Ferry Building in the foreground.
One of the most well-known photographs by George R. Lawrence, taken May 28, 1906, about 6 weeks after the Great San Francisco earthquake which occurred on April 18. The 160-degree panorama was taken from a camera suspended from a kite 2,000 feet in the air. The view looks up Market Street with the waterfront and Union Ferry Building in the foreground.
Under the Wave off Kanagawa (Kanagawa oki nami ura), also known as The Great Wave, from the series Thirty-six Views of Mount Fuji (Fugaku sanjūrokkei), by artist Katsushika Hokusai (Japanese, Tokyo (Edo) 1760–1849 Tokyo (Edo)). Dated sometime between 1829-1833.
Under the Wave off Kanagawa (Kanagawa oki nami ura), also known as The Great Wave, from the series Thirty-six Views of Mount Fuji (Fugaku sanjūrokkei), by artist Katsushika Hokusai (Japanese, Tokyo (Edo) 1760–1849 Tokyo (Edo)). Dated sometime between 1829-1833.