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(NASA Crew Earth Observations)

Photographing the Earth from the International Space Station

Astronaut Photography of Earth - Display Record


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File NameFile Size (bytes)WidthHeightAnnotatedCroppedPurposeComments
View ISS019-E-5286.JPG 70360640438 No No
View ISS019-E-5286.JPG 305599540649 Yes Yes NASA's Earth Observatory web site
View ISS019-E-5286.JPG 5531427061000 No Yes NASA's Earth Observatory web site
View ISS019-E-5286.JPG 96196942562913 No No

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Mission: ISS019 Roll: E Frame: 5286 Mission ID on the Film or image: ISS019
Country or Geographic Name: JAPAN
Features: MT. FUJI, LAND USE
Center Point: Latitude: 35.4 Longitude: 138.8 (Negative numbers indicate south for latitude and west for longitude)

Stereo: (Yes indicates there is an adjacent picture of the same area)


Camera Tilt: 47
Camera Focal Length: 800mm
Camera: N3: Nikon D3
Film: 4256E : 4256 x 2832 pixel CMOS sensor, 36.0mm x 23.9mm, total pixels: 12.87 million, Nikon FX format.


Film Exposure:
Percentage of Cloud Cover: 10 (0-10)


GMT Date: 20090408 (YYYYMMDD) GMT Time: 233914 (HHMMSS)
Nadir Point Latitude: 34.3, Longitude: 142.0 (Negative numbers indicate south for latitude and west for longitude)

Nadir to Photo Center Direction: West
Sun Azimuth: 113 (Clockwise angle in degrees from north to the sun measured at the nadir point)
Spacecraft Altitude: 191 nautical miles (354 km)
Sun Elevation Angle: 42 (Angle in degrees between the horizon and the sun, measured at the nadir point)
Orbit Number: 3506


Mount Fuji, Japan

The 3,776 meter high Mount Fuji volcano, located on the island of Honshu in Japan, is one of the world’s classic examples of a stratovolcano. The volcano’s steep, conical profile is the result of numerous interlayered lava flows and explosive eruption products – such as ash, cinders, and volcanic bombs – building up the volcano over time. The steep profile is possible because of the relatively high viscosity of the volcanic rocks typically associated with stratovolcanoes. This leads to thick sequences of lava flows near the eruptive vent that build the cone structure, rather than low viscosity flows that spread out over the landscape and build lower-profile shield volcanoes
Mount Fuji, or Fuji-san in Japan, is actually comprised of several overlapping volcanoes that began erupting in the Pleistocene Epoch (1.8 million to approximately 10,000 years ago). The currently active volcano, known as Younger Fuji, began forming approximately 11,000 to 8,000 years ago. The most recent explosive activity occurred in 1707, creating Hoei Crater on the southeastern flank of the volcano (image center). This eruption deposited ash on Edo (present-day Tokyo) located 95 km to the northeast. While there have been no further eruptions of Mount Fuji, steam was observed at the summit during 1780 – 1820, and the volcano is considered active.

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