PIA12493: Southern Haiti Anaglyph
 Target Name:  Earth
 Is a satellite of:  Sol (our sun)
 Mission:  Shuttle Radar Topography Mission (SRTM)
 Spacecraft:  Space Shuttle Endeavour
 Instrument:  C-Band Radar
X-Band Radar 
 Product Size:  6001 x 1201 pixels (w x h)
 Produced By:  JPL
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 Full-Res TIFF:  PIA12493.tif (21.62 MB)
 Full-Res JPEG:  PIA12493.jpg (900.4 kB)

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Original Caption Released with Image:

A magnitude 7.0 earthquake occurred on January 12, 2010, at Port-au-Prince, Haiti, with major impact to the region and its citizens. This stereoscopic (anaglyph) view of the pre-quake topography of the area clearly shows the fault that is apparently responsible for the earthquake as a prominent linear landform immediately southwest of the city (image center) and as a series of fault traces that extend westward along the full length of Haiti's southern peninsula. This fault was already well known and is called the Enriquillo fault.

The Enriquillo fault generally moves left-laterally (horizontally, with features across the fault shifting to the left when the fault breaks in an earthquake), but vertical movements occur along the fault where irregularities in the fault line cause local compression or extension of the earth. Meanwhile, movements of the topography at the Earth's surface can falsely appear to be vertical where mountain slopes are cut and misaligned by horizontal shifts of the fault. Additionally, differing erosion rates on the two sides of the fault, due to the juxtapositioning of differing rock types by the fault, can give the appearance of vertical offsets of the current topographic surface. All of these real and apparent horizontal and vertical offsets of the topographic surface may (and likely do) occur here, making the fault easily observed in the topographic data. Notably, a horizontal stream offset along the fault (and adjacent to the city) is very distinct in this view, and displays a left-lateral offset of about 7 kilometers (4.3 miles).

Topographic shading plus stereoscopic projection were combined to create this anaglyph view. The shade image was derived by computing topographic slope in the north-south direction. Northern slopes appear bright and southern slopes appear dark. The stereoscopic effect was created by generating two differing perspectives, one for each eye. When viewed through special glasses, the result is a vertically exaggerated view of the Earth's surface in its full three dimensions. Anaglyph glasses cover the left eye with a red filter and cover the right eye with a blue filter.

The elevation data used in this image were produced by the Shuttle Radar Topography Mission (SRTM), flown aboard Space Shuttle Endeavour in February 2000. SRTM acquired elevation measurements for nearly all of Earth's landmass between 60 degrees North and 56 degrees South latitudes. For many areas of the world, SRTM data provide the first detailed three dimensional observation of landforms at regional scales. The mission was a cooperative project between the National Aeronautics and Space Administration (NASA), the National Geospatial-Intelligence Agency (NGA) of the U.S. Department of Defense (DOD), and the German and Italian space agencies. It was managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif., for NASA's Science Mission Directorate, Washington, D.C.

View Area: One degree latitude (111 kilometers, or 69 miles) by five degrees longitude (525 kilometers, or 325 miles)
Location: 18 to 19 degrees North latitude, 70 to 75 degrees West longitude
Orientation: North to the top
SRTM Data Acquired: February 2000

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