Iranian Earthquake Leaves Hundreds Dead

TECTONICS

This image shows elevation data acquired by NASA's Shuttle Radar Topography Mission on the Space Shuttle Endeavour, launched on February 11, 2000. The red dot shows the epicenter of the earthquake, near Zarand, Iran. Green represents landscape at 1000 metres elevation, yellow at 2250 metres, and white at 3500 metres, or higher elevation. See larger image.

Greenbelt MD (SPX) Feb 23, 2005
For eleven seconds on Tuesday morning February 22, 2005, the ground shook in southern Iran as a 6.4-magnitude earthquake rattled the mountainous area near the town of Zarand. According to news reports, more than 500 people have been killed, and tens of thousands of people have been affected in dozens of scattered villages, many of which were almost completely destroyed.

This image shows the topography around the town of Zarand, in the Kerman region to the west of the Lut Desert. Two lines of mountains run southeastward through the scene, separated by a broad valley, through which the Shur Ab river flows.

The approximate location of the earthquake's epicenter is marked with a red dot near image center. The highest elevations in the scene (white) are found on the summit of Kuhpayeh Mountain, near the right center edge.

Iran is very seismically active. The land there is being compressed by the coming together of the Arabian tectonic plate to the west and the Eurasian plate to the east-northeast.

Much of the compressional forces of the two plates pushing together is released by mountain-building and rock-folding processes in the Zagros Mountains, which overlook the Persian Gulf, to the west of this scene.

However, in the central-east portion of Iran, the pressure is released at numerous "strike-slip" faults, places where the plates grind past each other in a sideways motion, rather than over or under each other. The town of Zarand is located along one of several northwest-southeast slip faults in the region north of the town of Kerman.

This image shows elevation data acquired by NASA's Shuttle Radar Topography Mission (SRTM) on the Space Shuttle Endeavour, launched on February 11, 2000. SRTM used the same radar instrument that comprised the Spaceborne Imaging Radar-C/X-Band Synthetic Aperture Radar (SIR-C/X-SAR) that flew twice on the Space Shuttle Endeavour in 1994.

For SRTM, engineers refined the technology of previous missions by adding a 60-meter (approximately 200-foot) mast, installing additional C-band and X-band antennas, and improving tracking and navigation devices. These refinements allowed SRTM to collect the 3-dimensional observations of Earth's surface.

The mission is a cooperative project between NASA, the National Geospatial-Intelligence Agency (NGA) of the U.S. Department of Defense and the German and Italian space agencies. It is managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif., for NASA's Earth Science Enterprise, Washington, D.C.

NASA image created by Jesse Allen, Earth Observatory, using SRTM data obtained from the University of Maryland's Global Land Cover Facility.

TECTONICS

Seismic Rocker Aims To Cut The Noise

Vancouver BC (SPX) Feb 22, 2005
A Canadian seismologist is arguing that our understanding of the structure of the Earth's interior is based on the equivalent of fuzzy ultrasound images that leave room for improvement.

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