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Astronaut Photography of Earth - Display Record

STS101-718-27

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File NameFile Size (bytes)WidthHeightAnnotatedCroppedPurposeComments
View STS101-718-27.JPG 31943517512 No No From ISD PhotoCDs
View STS101-718-27.JPG 28203399400 No Photographic Highlights

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Request STS101-718-27.JPG 10041410341024 No No From ISD PhotoCDs
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Electronic Image Data

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Identification

Mission: STS101 Roll: 718 Frame: 27 Mission ID on the Film or image: STS101
Country or Geographic Name: IRAN
Features: PAN-STR. OF HORMUZ, DUST
Center Point Latitude: 27.5 Center Point Longitude: 54.0 (Negative numbers indicate south for latitude and west for longitude)
Stereo: (Yes indicates there is an adjacent picture of the same area)
ONC Map ID: JNC Map ID:

Camera

Camera Tilt: High Oblique
Camera Focal Length: 40mm
Camera: HB: Hasselblad
Film: 5069 : Kodak Elite 100S, E6 Reversal, Replaces Lumiere, Warmer in tone vs. Lumiere.

Quality

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

Nadir

Date: 20000527 (YYYYMMDD)GMT Time: 070541 (HHMMSS)
Nadir Point Latitude: 29.8, Longitude: 46.6 (Negative numbers indicate south for latitude and west for longitude)
Nadir to Photo Center Direction: East
Sun Azimuth: 103 (Clockwise angle in degrees from north to the sun measured at the nadir point)
Spacecraft Altitude: 203 nautical miles (376 km)
Sun Elevation Angle: 65 (Angle in degrees between the horizon and the sun, measured at the nadir point)
Orbit Number: 124

Captions

N. and S. Zagros Ranges & Persian Gulf
The lobate Qatar peninsula and Bahrain, on the southwestern shore of the
Persian Gulf, lie beyond the orbiter stabilizer in this southeastward
view. Along the northern Gulf coast are the folded mountain ranges of
Iran, where the contrasting structural styles in the Northern and
Southern Zagros ranges are clearly visible. Folds of the Northern
Zagros, at left just above the orbiter, are long and tight, whereas
those of the Southern Zagros are broader and less continuous. The
differing styles reflect the responses of different rock types to the
collision of the Arabian and Eurasian tectonic plates.
Arabia is moving northward and is descending beneath the Eurasian plate
margin, resulting in the crumpling of strata along the margin. The dark
rocks in the crescent along the Oman Peninsula (distant center) are
remnants of oceanic crust that were uplifted about 70 million years ago,
early in the collision of the two plates.


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