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Astronaut Photography of Earth - Display RecordSTS099-735-46Low-resolution Browse Image(Most browse images are not color adjusted.)ImagesConditions for Use of Images >>Image Transformation Tutorial >> Saving, Color Adjusting, and Printing Images >> Images to View on Your Computer Now
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Download a Keyhole Markup Language (KML) file for use in Google Earth. Electronic Image DataCamera files only apply to electronic still cameras.No sound file available. IdentificationMission: STS099 Roll: 735 Frame: 46 Mission ID on the Film or image: STS99Country or Geographic Name: CHINA Features: HIMALAYA, MOUNT EVEREST Center Point Latitude: 28.0 Center Point Longitude: 87.0 (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: CameraCamera Tilt:Camera Focal Length: 250mm Camera: HB: Hasselblad Film: 5069 : Kodak Elite 100S, E6 Reversal, Replaces Lumiere, Warmer in tone vs. Lumiere. QualityFilm Exposure:Percentage of Cloud Cover: 25 (11-25) NadirDate: 200002__ (YYYYMMDD)GMT Time: (HHMMSS)Nadir Point Latitude: , Longitude: (Negative numbers indicate south for latitude and west for longitude) Nadir to Photo Center Direction: Sun Azimuth: (Clockwise angle in degrees from north to the sun measured at the nadir point) Spacecraft Altitude: nautical miles (0 km) Sun Elevation Angle: (Angle in degrees between the horizon and the sun, measured at the nadir point) Orbit Number: CaptionsMt. Everest, eastern Himalaya, Tibet Autonomous Region of ChinaMt. Everest (29,028 ft/8848 m; center of photo), also called Qomolangma Feng, is just north of the border between Nepal and China. The Himalayas and the Tibetan Plateau are products of the collision of the Indian and Eurasian tectonic plates. With the continuing northward march of India, the crust of the Earth has become thicker and the Tibetan Plateau has been uplifted to an average elevation of about 15,000 feet. At the summit of Mt. Everest are fossil-bearing limestones that were deposited beneath the sea around 510 million years ago (Cambrian to Ordovician time). Glaciers, moraines, and outwash plains are spectacularly displayed. Glacial meltwaters in this area feed the Arun River, eventually reaching the Ganges on the plains of India. Download Packaged File. This option downloads the following items, packaged into a single file, if they are available:
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