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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
On December 26, 2004, tsunamis swept across the Indian ocean, spawned by a magnitude 9.0 earthquake off the coast of Sumatra. Aside from Indonesia, the island nation of Sri Lanka likely suffered the most casualties, with the death toll reported at 21,715 on December 29th.DigitalGlobe?s [ http://www.digitalglobe.com/ ] Quickbird satellite captured an image of the devestation around Kalutara, Sri Lanka (top), on December 26, 2004, at 10:20 a.m. local time?about an hour after the first in the series of waves hit. [A Quickbird image taken on January 1, 2004 (lower), shows the normal ocean conditions.] Water is flowing out of the inundated area and back into the sea, creating turbulence offshore. Some near-shore streets and yards are covered with muddy water. It is possible that the image was acquired in a ?trough? between wave crests. Imagery of nearby beaches shows that the edge of the ocean had receded about 150 meters from the shoreline.More images [ http://www.digitalglobe.com/tsunami_gallery.html ] are available on the DigitalGlobe web site. Images Copyright DigitalGlobe [ http://www.digitalglobe.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
On December 26, 2004, tsunamis swept across the Indian ocean, spawned by a magnitude 9.0 earthquake off the coast of Sumatra. Aside from Indonesia, the island nation of Sri Lanka likely suffered the most casualties, with the death toll reported at 21,715 on December 29th.DigitalGlobe?s [ http://www.digitalglobe.com/ ] Quickbird satellite captured an image of the devestation around Kalutara, Sri Lanka (top), on December 26, 2004, at 10:20 a.m. local time?about an hour after the first in the series of waves hit. [A Quickbird image taken on January 1, 2004 (lower), shows the normal ocean conditions.] Water is flowing out of the inundated area and back into the sea, creating turbulence offshore. Some near-shore streets and yards are covered with muddy water. It is possible that the image was acquired in a ?trough? between wave crests. Imagery of nearby beaches shows that the edge of the ocean had receded about 150 meters from the shoreline.More images [ http://www.digitalglobe.com/tsunami_gallery.html ] are available on the DigitalGlobe web site. Images Copyright DigitalGlobe [ http://www.digitalglobe.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
On December 26, 2004, tsunamis swept across the Indian ocean, spawned by a magnitude 9.0 earthquake off the coast of Sumatra. Aside from Indonesia, the island nation of Sri Lanka likely suffered the most casualties, with the death toll reported at 21,715 on December 29th.DigitalGlobe?s [ http://www.digitalglobe.com/ ] Quickbird satellite captured an image of the devestation around Kalutara, Sri Lanka (top), on December 26, 2004, at 10:20 a.m. local time?about an hour after the first in the series of waves hit. [A Quickbird image taken on January 1, 2004 (lower), shows the normal ocean conditions.] Water is flowing out of the inundated area and back into the sea, creating turbulence offshore. Some near-shore streets and yards are covered with muddy water. It is possible that the image was acquired in a ?trough? between wave crests. Imagery of nearby beaches shows that the edge of the ocean had receded about 150 meters from the shoreline.More images [ http://www.digitalglobe.com/tsunami_gallery.html ] are available on the DigitalGlobe web site. Images Copyright DigitalGlobe [ http://www.digitalglobe.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
On December 26, 2004, tsunamis swept across the Indian ocean, spawned by a magnitude 9.0 earthquake off the coast of Sumatra. Aside from Indonesia, the island nation of Sri Lanka likely suffered the most casualties, with the death toll reported at 21,715 on December 29th.DigitalGlobe?s [ http://www.digitalglobe.com/ ] Quickbird satellite captured an image of the devestation around Kalutara, Sri Lanka (top), on December 26, 2004, at 10:20 a.m. local time?about an hour after the first in the series of waves hit. [A Quickbird image taken on January 1, 2004 (lower), shows the normal ocean conditions.] Water is flowing out of the inundated area and back into the sea, creating turbulence offshore. Some near-shore streets and yards are covered with muddy water. It is possible that the image was acquired in a ?trough? between wave crests. Imagery of nearby beaches shows that the edge of the ocean had receded about 150 meters from the shoreline.More images [ http://www.digitalglobe.com/tsunami_gallery.html ] are available on the DigitalGlobe web site. Images Copyright DigitalGlobe [ http://www.digitalglobe.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
On December 26, 2004, tsunamis swept across the Indian ocean, spawned by a magnitude 9.0 earthquake off the coast of Sumatra. Aside from Indonesia, the island nation of Sri Lanka likely suffered the most casualties, with the death toll reported at 21,715 on December 29th.DigitalGlobe?s [ http://www.digitalglobe.com/ ] Quickbird satellite captured an image of the devestation around Kalutara, Sri Lanka (top), on December 26, 2004, at 10:20 a.m. local time?about an hour after the first in the series of waves hit. [A Quickbird image taken on January 1, 2004 (lower), shows the normal ocean conditions.] Water is flowing out of the inundated area and back into the sea, creating turbulence offshore. Some near-shore streets and yards are covered with muddy water. It is possible that the image was acquired in a ?trough? between wave crests. Imagery of nearby beaches shows that the edge of the ocean had receded about 150 meters from the shoreline.More images [ http://www.digitalglobe.com/tsunami_gallery.html ] are available on the DigitalGlobe web site. Images Copyright DigitalGlobe [ http://www.digitalglobe.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
On December 26, 2004, tsunamis swept across the Indian ocean, spawned by a magnitude 9.0 earthquake off the coast of Sumatra. Aside from Indonesia, the island nation of Sri Lanka likely suffered the most casualties, with the death toll reported at 21,715 on December 29th.DigitalGlobe?s [ http://www.digitalglobe.com/ ] Quickbird satellite captured an image of the devestation around Kalutara, Sri Lanka (top), on December 26, 2004, at 10:20 a.m. local time?about an hour after the first in the series of waves hit. [A Quickbird image taken on January 1, 2004 (lower), shows the normal ocean conditions.] Water is flowing out of the inundated area and back into the sea, creating turbulence offshore. Some near-shore streets and yards are covered with muddy water. It is possible that the image was acquired in a ?trough? between wave crests. Imagery of nearby beaches shows that the edge of the ocean had receded about 150 meters from the shoreline.More images [ http://www.digitalglobe.com/tsunami_gallery.html ] are available on the DigitalGlobe web site. Images Copyright DigitalGlobe [ http://www.digitalglobe.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
The Indonesian province of Aceh was hit hardest by the earthquake and tsunamis of December 26, 2004. Aceh is located on the northern tip of the island of Sumatra. Early Western media attention was focused on Sri Lanka and Thailand, even though the earthquake epicenter was closer to Aceh, and the largest waves struck the northwestern coast of Sumatra. On Decemebr 29, estimates of the death toll in Indonesia were over 80,000more than half the global total. The town of Lhoknga, on the west coast of Sumatra near the capital of Aceh, Banda Aceh, was completely destroyed by the tsunami, with the exception of the mosque in the city's center. These high-resolution satellite images, acquired by Space Imaging's [ http://www.spaceimaging.com/ ] Ikonos satellite, show Lhoknga before (lower) and after (top) the earthquake and Tsunami. Almost all the trees, vegetation, and buildings in the area were washed away. Behind the town, low-lying agricultural areas remained covered with water 4 days after the disaster, and sand on the nearby beaches was completely removed. The wave height [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12645 ] might have exceeded 15 meters (50 feet) when it struck the shore. Equivalent devestation extends 225 km southeast along the Sumatran Coast, in a band up to 3 km (1.9 miles) deep. Imagery from the Moderate Resolution Imaging Spectroradiometer [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12644 ] (above) shows the affected area as a thin strip of brown along the coast. Ikonos images copyright Centre for Remote Imaging, Sensing and Processing, [ http://www.crisp.nus.edu.sg/ ] National University of Singapore and Space Imaging. [ http://www.spaceimaging.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
The Indonesian province of Aceh was hit hardest by the earthquake and tsunamis of December 26, 2004. Aceh is located on the northern tip of the island of Sumatra. Early Western media attention was focused on Sri Lanka and Thailand, even though the earthquake epicenter was closer to Aceh, and the largest waves struck the northwestern coast of Sumatra. On Decemebr 29, estimates of the death toll in Indonesia were over 80,000more than half the global total. The town of Lhoknga, on the west coast of Sumatra near the capital of Aceh, Banda Aceh, was completely destroyed by the tsunami, with the exception of the mosque in the city's center. These high-resolution satellite images, acquired by Space Imaging's [ http://www.spaceimaging.com/ ] Ikonos satellite, show Lhoknga before (lower) and after (top) the earthquake and Tsunami. Almost all the trees, vegetation, and buildings in the area were washed away. Behind the town, low-lying agricultural areas remained covered with water 4 days after the disaster, and sand on the nearby beaches was completely removed. The wave height [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12645 ] might have exceeded 15 meters (50 feet) when it struck the shore. Equivalent devestation extends 225 km southeast along the Sumatran Coast, in a band up to 3 km (1.9 miles) deep. Imagery from the Moderate Resolution Imaging Spectroradiometer [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12644 ] (above) shows the affected area as a thin strip of brown along the coast. Ikonos images copyright Centre for Remote Imaging, Sensing and Processing, [ http://www.crisp.nus.edu.sg/ ] National University of Singapore and Space Imaging. [ http://www.spaceimaging.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
The Indonesian province of Aceh was hit hardest by the earthquake and tsunamis of December 26, 2004. Aceh is located on the northern tip of the island of Sumatra. Early Western media attention was focused on Sri Lanka and Thailand, even though the earthquake epicenter was closer to Aceh, and the largest waves struck the northwestern coast of Sumatra. On Decemebr 29, estimates of the death toll in Indonesia were over 80,000more than half the global total. The town of Lhoknga, on the west coast of Sumatra near the capital of Aceh, Banda Aceh, was completely destroyed by the tsunami, with the exception of the mosque in the city's center. These high-resolution satellite images, acquired by Space Imaging's [ http://www.spaceimaging.com/ ] Ikonos satellite, show Lhoknga before (lower) and after (top) the earthquake and Tsunami. Almost all the trees, vegetation, and buildings in the area were washed away. Behind the town, low-lying agricultural areas remained covered with water 4 days after the disaster, and sand on the nearby beaches was completely removed. The wave height [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12645 ] might have exceeded 15 meters (50 feet) when it struck the shore. Equivalent devestation extends 225 km southeast along the Sumatran Coast, in a band up to 3 km (1.9 miles) deep. Imagery from the Moderate Resolution Imaging Spectroradiometer [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12644 ] (above) shows the affected area as a thin strip of brown along the coast. Ikonos images copyright Centre for Remote Imaging, Sensing and Processing, [ http://www.crisp.nus.edu.sg/ ] National University of Singapore and Space Imaging. [ http://www.spaceimaging.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
The Indonesian province of Aceh was hit hardest by the earthquake and tsunamis of December 26, 2004. Aceh is located on the northern tip of the island of Sumatra. Early Western media attention was focused on Sri Lanka and Thailand, even though the earthquake epicenter was closer to Aceh, and the largest waves struck the northwestern coast of Sumatra. On Decemebr 29, estimates of the death toll in Indonesia were over 80,000more than half the global total. The town of Lhoknga, on the west coast of Sumatra near the capital of Aceh, Banda Aceh, was completely destroyed by the tsunami, with the exception of the mosque in the city's center. These high-resolution satellite images, acquired by Space Imaging's [ http://www.spaceimaging.com/ ] Ikonos satellite, show Lhoknga before (lower) and after (top) the earthquake and Tsunami. Almost all the trees, vegetation, and buildings in the area were washed away. Behind the town, low-lying agricultural areas remained covered with water 4 days after the disaster, and sand on the nearby beaches was completely removed. The wave height [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12645 ] might have exceeded 15 meters (50 feet) when it struck the shore. Equivalent devestation extends 225 km southeast along the Sumatran Coast, in a band up to 3 km (1.9 miles) deep. Imagery from the Moderate Resolution Imaging Spectroradiometer [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12644 ] (above) shows the affected area as a thin strip of brown along the coast. Ikonos images copyright Centre for Remote Imaging, Sensing and Processing, [ http://www.crisp.nus.edu.sg/ ] National University of Singapore and Space Imaging. [ http://www.spaceimaging.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
The Indonesian province of Aceh was hit hardest by the earthquake and tsunamis of December 26, 2004. Aceh is located on the northern tip of the island of Sumatra. Early Western media attention was focused on Sri Lanka and Thailand, even though the earthquake epicenter was closer to Aceh, and the largest waves struck the northwestern coast of Sumatra. On Decemebr 29, estimates of the death toll in Indonesia were over 80,000more than half the global total. The town of Lhoknga, on the west coast of Sumatra near the capital of Aceh, Banda Aceh, was completely destroyed by the tsunami, with the exception of the mosque in the city's center. These high-resolution satellite images, acquired by Space Imaging's [ http://www.spaceimaging.com/ ] Ikonos satellite, show Lhoknga before (lower) and after (top) the earthquake and Tsunami. Almost all the trees, vegetation, and buildings in the area were washed away. Behind the town, low-lying agricultural areas remained covered with water 4 days after the disaster, and sand on the nearby beaches was completely removed. The wave height [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12645 ] might have exceeded 15 meters (50 feet) when it struck the shore. Equivalent devestation extends 225 km southeast along the Sumatran Coast, in a band up to 3 km (1.9 miles) deep. Imagery from the Moderate Resolution Imaging Spectroradiometer [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12644 ] (above) shows the affected area as a thin strip of brown along the coast. Ikonos images copyright Centre for Remote Imaging, Sensing and Processing, [ http://www.crisp.nus.edu.sg/ ] National University of Singapore and Space Imaging. [ http://www.spaceimaging.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
The Indonesian province of Aceh was hit hardest by the earthquake and tsunamis of December 26, 2004. Aceh is located on the northern tip of the island of Sumatra. Early Western media attention was focused on Sri Lanka and Thailand, even though the earthquake epicenter was closer to Aceh, and the largest waves struck the northwestern coast of Sumatra. On Decemebr 29, estimates of the death toll in Indonesia were over 80,000more than half the global total. The town of Lhoknga, on the west coast of Sumatra near the capital of Aceh, Banda Aceh, was completely destroyed by the tsunami, with the exception of the mosque in the city's center. These high-resolution satellite images, acquired by Space Imaging's [ http://www.spaceimaging.com/ ] Ikonos satellite, show Lhoknga before (lower) and after (top) the earthquake and Tsunami. Almost all the trees, vegetation, and buildings in the area were washed away. Behind the town, low-lying agricultural areas remained covered with water 4 days after the disaster, and sand on the nearby beaches was completely removed. The wave height [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12645 ] might have exceeded 15 meters (50 feet) when it struck the shore. Equivalent devestation extends 225 km southeast along the Sumatran Coast, in a band up to 3 km (1.9 miles) deep. Imagery from the Moderate Resolution Imaging Spectroradiometer [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12644 ] (above) shows the affected area as a thin strip of brown along the coast. Ikonos images copyright Centre for Remote Imaging, Sensing and Processing, [ http://www.crisp.nus.edu.sg/ ] National University of Singapore and Space Imaging. [ http://www.spaceimaging.com/ ] |
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Earthquake Spawns Tsunamis
| Title |
Earthquake Spawns Tsunamis |
| Description |
The Earth?s solid surface floats on a layer of softer rock as a collection of interlocking, movable puzzle pieces called tectonic plates. At 7:58 a.m. (local time), on December 26, 2004, beneath the Indian Ocean west of Sumatra, Indonesia, pent-up energy from the compressional forces of one tectonic plate grinding under another found a weak spot in the overlying rock. The rock was thrust upward, and the Earth shook as a 9.0 magnitude earthquake sent its vibrations out into the ocean. Tsunamis spread out in all directions, the massive waves washed over islands and crashed against coastlines in Sri Lanka, Southern India, and even the east coast of Africa. Tens of thousands of people were killed, millions are homeless. The image above shows how the tectonic puzzle pieces fit together around Indonesia. The epicenter of the recent quake is marked with a red star in the image. It is located just to the east of the Sunda Trench, where the India Plate begins to get subducted beneath (forced under) the Burma Plate. The blue arrows along the plate boundary show the direction of subduction. As the India Plate slides beneath the Burma Plate, it meets pockets of resistance, which causes compressional forces to build up. Weakened overlying rock gets forced upward. Based on the location of aftershocks (red shaded circles on the image), the United States Geological Survey reports that approximately 1,200 kilometers of the plate boundary probably slipped as a result of the quake. The initial rupture was likely more than 100 kilometers wide, and probably produced an average vertical displacement along the fault plane (the slope along which the two plates meet) of 15 meters. When the bottom of the ocean is deformed by this type of ?megathrust? quake, the upward force acts like a fist rising up from underwater. Water rolls down off the sides of the ?fist,? creating massive waves that can travel as fast as an airplane. The waves can move across the ocean and barely disturb the surface, but when they reach shallow coastal water, the earthquake?s energy thrusts them tens of meters into the air. The tsunami created by this earthquake reached India and Sri Lanka in about four hours. The wave eventually reached Africa, the Pacific Ocean, Hawaii, and the west coast of North and South America. For more information about this earthquake and plate tectonics, visit the Website of the USGS. [ http://earthquake.usgs.gov/eqinthenews/2004/usslav/ ] Image courtesy United States Geological Survey [ http://www.usgs.gov/ ] |
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North Reef Island, Andaman S
…
| Title |
North Reef Island, Andaman Sea |
| Description |
On December 26, 2004, one of the largest earthquakes in recorded history struck offshore of the island of Sumatra, Indonesia. The ocean floor heaved in some places and sank in others, creating catastrophic tsunamis that raced across the Indian Ocean. Hundreds of thousands of people died as the waves struck coastlines from Thailand to Sri Lanka to Somalia. In addition to tsunami damage, satellite images of reefs, islands, and coastlines identified signs of permanent elevation changesinking or upliftalong the fault between the Indo-Australia and Burma plates. [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12640 ] In places such as North Reef Island, shown in this pair of images from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) [ http://asterweb.jpl.nasa.gov ] on NASA's Terra [ http://terra.nasa.gov ] satellite, the quake lifted the reefs permanently out of the water. The images use visible and infrared light detected by ASTER to make different land surfaces stand out clearly from one another: water is blue, vegetation is red, coral or bare sand appears white. In the "before" image, from December 2, 2004, the submerged reef creates a bright blue glow around the island. In the "after" image, from February 4, 2005, the white coral stands completely up out of the water. It is even tinged with red, which suggests the exposed coral had died, and algae had colonized it. In the weeks and months after the earthquake, satellite images provided broad coverage of an area where ground-based observations were initially very limited. A team of scientists led by Caltech Ph.D. geology student Aron Meltzner discovered changes in elevation along nearly 1,600 kilometers (994 miles) of the tectonic plate boundary. The images revealed that the earthquake rupture extended 100 kilometers (62 miles) farther north than estimates based on seismic and Global Positioning System (GPS) data suggested. The feature article Rise and Fall: Satellites Reveal Full Length of Tsunami-Generating Earthquake [ http://earthobservatory.nasa.gov/Study/Aceh/aceh.html ] describes how scientists used satellite images to map the length of the earthquake rupture zone. The article includes additional satellite and ground-based images of elevation changes resulting from the 2004 Aceh-Andaman earthquake. NASA images created by Jesse Allen, Earth Observatory, using data provided courtesy of the NASA/GSFC/MITI/ERSDAC/JAROS, and U.S./Japan ASTER Science Team. [ http://asterweb.jpl.nasa.gov/ ] |
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North Reef Island, Andaman S
…
| Title |
North Reef Island, Andaman Sea |
| Description |
On December 26, 2004, one of the largest earthquakes in recorded history struck offshore of the island of Sumatra, Indonesia. The ocean floor heaved in some places and sank in others, creating catastrophic tsunamis that raced across the Indian Ocean. Hundreds of thousands of people died as the waves struck coastlines from Thailand to Sri Lanka to Somalia. In addition to tsunami damage, satellite images of reefs, islands, and coastlines identified signs of permanent elevation changesinking or upliftalong the fault between the Indo-Australia and Burma plates. [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=12640 ] In places such as North Reef Island, shown in this pair of images from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) [ http://asterweb.jpl.nasa.gov ] on NASA's Terra [ http://terra.nasa.gov ] satellite, the quake lifted the reefs permanently out of the water. The images use visible and infrared light detected by ASTER to make different land surfaces stand out clearly from one another: water is blue, vegetation is red, coral or bare sand appears white. In the "before" image, from December 2, 2004, the submerged reef creates a bright blue glow around the island. In the "after" image, from February 4, 2005, the white coral stands completely up out of the water. It is even tinged with red, which suggests the exposed coral had died, and algae had colonized it. In the weeks and months after the earthquake, satellite images provided broad coverage of an area where ground-based observations were initially very limited. A team of scientists led by Caltech Ph.D. geology student Aron Meltzner discovered changes in elevation along nearly 1,600 kilometers (994 miles) of the tectonic plate boundary. The images revealed that the earthquake rupture extended 100 kilometers (62 miles) farther north than estimates based on seismic and Global Positioning System (GPS) data suggested. The feature article Rise and Fall: Satellites Reveal Full Length of Tsunami-Generating Earthquake [ http://earthobservatory.nasa.gov/Study/Aceh/aceh.html ] describes how scientists used satellite images to map the length of the earthquake rupture zone. The article includes additional satellite and ground-based images of elevation changes resulting from the 2004 Aceh-Andaman earthquake. NASA images created by Jesse Allen, Earth Observatory, using data provided courtesy of the NASA/GSFC/MITI/ERSDAC/JAROS, and U.S./Japan ASTER Science Team. [ http://asterweb.jpl.nasa.gov/ ] |
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Tsunami Destroys Lhoknga, In
…
nasa, nasaimageofthedaygalle
…
* eoimages.gsfc.nasa.gov/ima
…
lhoknga_iko_2004364
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2004-12-29 |
| creator |
NASA -- Ikonos images copyright www.crisp.nus.edu.sg/ Centre for Remote Imaging, Sensing and Processing, National University of Singapore and www.spaceimaging.com/ Space Imaging. |
| identifier |
lhoknga_iko_2004364 |
|
Deep Ocean Tsunami Waves off
…
nasa, nasaimageofthedaygalle
…
The initial tsunami waves re
…
PIA04373
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2004-12-26 |
| creator |
NASA -- Image courtesy NASA/GSFC/LaRC/JPL, MISR Team. Text by Clare Averill (Raytheon ITSS/JPL), Michael Garay and David J. Diner (JPL, California Institute of Technology), and Vasily Titov (NOAA/Pacific Marine Environmental Laboratory and University of Washington/Joint Institute for the Study of the Atmosphere and Oceans). |
| identifier |
PIA04373 |
|
Breaking Tsunami Waves along
…
nasa, nasaimageofthedaygalle
…
At 00:58:53 UTC (Coordinated
…
PIA04372
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2004-12-26 |
| creator |
NASA -- NASA image courtesy NASA/GSFC/LaRC/JPL, www-misr.jpl.nasa.gov/ MISR Team. Text by Michael Garay and David J. Diner (JPL, California Institute of Technology), Clare Averill (Raytheon ITSS/ JPL), Vasily Titov (NOAA Pacific Marine Environmental Laboratory) |
| identifier |
PIA04372 |
|
Tsunami Strikes Sri Lanka: I
…
nasa, nasaimageofthedaygalle
…
* eoimages.gsfc.nasa.gov/ima
…
srilanka_qbd_2004361
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2004-12-26 |
| creator |
NASA -- Images Copyright www.digitalglobe.com/ DigitalGlobe |
| identifier |
srilanka_qbd_2004361 |
|
Breaking Tsunami Waves along
…
PIA04372
Sol (our sun)
Multi-angle Imaging SpectroR
…
| Title |
Breaking Tsunami Waves along India's Eastern Coast |
| Original Caption Released with Image |
(3.8 MB) shows a region further south, at the northern end of India's Coromandel Coast, and covers an area of 43 kilometers x 58 kilometers. Cloud "motion" in these animations results from apparent displacements due to parallax associated with their height above the surface. The tsunami waves, on the other hand, are at sea level and show actual motion. When the waves arrive in the shallower water near the shore, they grow and, if they become large enough, they will break in a manner similar to typical oceanic waves, but on a much larger scale. The leading edge of the breaking waves is likely what is visible in the imagery. Additionally, if the tsunami waves impact the coast at an angle, they can produce what are known as "edge waves" which propagate parallel to the coast. There is clear evidence of edge wave generation in these images. Upon discovering the unique content of this imagery, MISR scientists contacted Dr. Vasily Titov at the National Oceanic and Atmospheric Administration's Pacific Marine Environmental Laboratory in Seattle, WA. Dr. Titov is an expert in the propagation of tsunamis, and has generated a model animation of the tsunami's progression from its origin near Sumatra (see http://www.pmel.noaa.gov/tsunami/indo_1204.html [ http://www.pmel.noaa.gov/tsunami/indo_1204.html ]). The MISR imagery provides measurements of the location and timing of the breaking waves, their angle relative to the shoreline, and their speed of propagation, which is estimated from these data to be around 30 kilometers/hour. In conjunction with bathymetric measurements of ocean depth, this information can be used to refine and calibrate tsunami propagation models. According to Dr. Titov, improving these models has two primary benefits. First, a detailed understanding of wave interactions with coastal areas is necessary for developing damage mitigation approaches. Second, a better predictive capability of the models will make possible more accurate near-real-time forecasts of tsunami arrival times and effects. The Multi-angle Imaging SpectroRadiometer observes the daylit Earth continuously and every 9 days views the entire globe between 82° north and 82° south latitude. These data products were generated from a portion of the imagery acquired during Terra orbit 26720 and utilize data from within blocks 77 and 78 within World Reference System-2 path 142. MISR was built and is managed by NASA's Jet Propulsion Laboratory, Pasadena, CA, for NASA's Office of Earth Science, Washington, DC. The Terra satellite is managed by NASA's Goddard Space Flight Center, Greenbelt, MD. JPL is a division of the California Institute of Technology., At 00:58:53 UTC (Coordinated Universal Time) on 26 December 2004, a magnitude 9.0 earthquake occurred off the west coast of Sumatra, Indonesia. This was the fourth largest earthquake in the world since 1900 and the largest in over 40 years. It was caused by the release of stresses in the Earth that are built up as the Indian tectonic plate descends into the mantle beneath the Burma plate. It is estimated that the sea floor was displaced several meters due to the quake, resulting in large ocean waves, called "tsunamis" from the Japanese for "harbor waves." The tsunami moved rapidly across the deep ocean, with speeds estimated around 640 km/hr. When the waves reach shallow water near land, they slow considerably, but their size increases dramatically and they strike with catastrophic force. With human casualities exceeding 150,000, this event is one of the deadliest natural disasters in modern history, causing devastation along the shores of Indonesia, Sri Lanka, India, Thailand, and other countries. The initial tsunami waves reached the eastern Indian coast around 3:35 UTC, based on tide gauge measurements made at the port city of Vishakapatnam. The Multi-angle Imaging SpectroRadiometer (MISR) aboard NASA's Terra satellite passed over the eastern Indian coast between 5:10 to 5:20 UTC, when the tide gauge indicated the arrival of another series of waves. Because MISR's nine cameras imaged the coast over a time span of about 7 minutes, and because the the waves are unusually large, MISR was able to capture unique time-lapse imagery of the breaking waves. The still image shows four frames from the instrument's backward-viewing cameras spanning a period of about 2.5 minutes. This scene is located along the shores of Andhra Pradesh, near the mouth of the Godavari River, and covers an area of 42 kilometers x 37 kilometers. The arrows show the progression of the southwestern edges of the breakers. A series of frames spanning nearly 6 minutes has been made into a small animated GIF (below). An animated GIF (5.8 MB) covering a somewhat larger area of 86 kilometers x 49 kilometers is also available. A second animated GIF |
|
Breaking Tsunami Waves along
…
PIA04372
Sol (our sun)
Multi-angle Imaging SpectroR
…
| Title |
Breaking Tsunami Waves along India's Eastern Coast |
| Original Caption Released with Image |
(3.8 MB) shows a region further south, at the northern end of India's Coromandel Coast, and covers an area of 43 kilometers x 58 kilometers. Cloud "motion" in these animations results from apparent displacements due to parallax associated with their height above the surface. The tsunami waves, on the other hand, are at sea level and show actual motion. When the waves arrive in the shallower water near the shore, they grow and, if they become large enough, they will break in a manner similar to typical oceanic waves, but on a much larger scale. The leading edge of the breaking waves is likely what is visible in the imagery. Additionally, if the tsunami waves impact the coast at an angle, they can produce what are known as "edge waves" which propagate parallel to the coast. There is clear evidence of edge wave generation in these images. Upon discovering the unique content of this imagery, MISR scientists contacted Dr. Vasily Titov at the National Oceanic and Atmospheric Administration's Pacific Marine Environmental Laboratory in Seattle, WA. Dr. Titov is an expert in the propagation of tsunamis, and has generated a model animation of the tsunami's progression from its origin near Sumatra (see http://www.pmel.noaa.gov/tsunami/indo_1204.html [ http://www.pmel.noaa.gov/tsunami/indo_1204.html ]). The MISR imagery provides measurements of the location and timing of the breaking waves, their angle relative to the shoreline, and their speed of propagation, which is estimated from these data to be around 30 kilometers/hour. In conjunction with bathymetric measurements of ocean depth, this information can be used to refine and calibrate tsunami propagation models. According to Dr. Titov, improving these models has two primary benefits. First, a detailed understanding of wave interactions with coastal areas is necessary for developing damage mitigation approaches. Second, a better predictive capability of the models will make possible more accurate near-real-time forecasts of tsunami arrival times and effects. The Multi-angle Imaging SpectroRadiometer observes the daylit Earth continuously and every 9 days views the entire globe between 82° north and 82° south latitude. These data products were generated from a portion of the imagery acquired during Terra orbit 26720 and utilize data from within blocks 77 and 78 within World Reference System-2 path 142. MISR was built and is managed by NASA's Jet Propulsion Laboratory, Pasadena, CA, for NASA's Office of Earth Science, Washington, DC. The Terra satellite is managed by NASA's Goddard Space Flight Center, Greenbelt, MD. JPL is a division of the California Institute of Technology., At 00:58:53 UTC (Coordinated Universal Time) on 26 December 2004, a magnitude 9.0 earthquake occurred off the west coast of Sumatra, Indonesia. This was the fourth largest earthquake in the world since 1900 and the largest in over 40 years. It was caused by the release of stresses in the Earth that are built up as the Indian tectonic plate descends into the mantle beneath the Burma plate. It is estimated that the sea floor was displaced several meters due to the quake, resulting in large ocean waves, called "tsunamis" from the Japanese for "harbor waves." The tsunami moved rapidly across the deep ocean, with speeds estimated around 640 km/hr. When the waves reach shallow water near land, they slow considerably, but their size increases dramatically and they strike with catastrophic force. With human casualities exceeding 150,000, this event is one of the deadliest natural disasters in modern history, causing devastation along the shores of Indonesia, Sri Lanka, India, Thailand, and other countries. The initial tsunami waves reached the eastern Indian coast around 3:35 UTC, based on tide gauge measurements made at the port city of Vishakapatnam. The Multi-angle Imaging SpectroRadiometer (MISR) aboard NASA's Terra satellite passed over the eastern Indian coast between 5:10 to 5:20 UTC, when the tide gauge indicated the arrival of another series of waves. Because MISR's nine cameras imaged the coast over a time span of about 7 minutes, and because the the waves are unusually large, MISR was able to capture unique time-lapse imagery of the breaking waves. The still image shows four frames from the instrument's backward-viewing cameras spanning a period of about 2.5 minutes. This scene is located along the shores of Andhra Pradesh, near the mouth of the Godavari River, and covers an area of 42 kilometers x 37 kilometers. The arrows show the progression of the southwestern edges of the breakers. A series of frames spanning nearly 6 minutes has been made into a small animated GIF (below). An animated GIF (5.8 MB) covering a somewhat larger area of 86 kilometers x 49 kilometers is also available. A second animated GIF |
|
Breaking Tsunami Waves along
…
PIA04372
Sol (our sun)
Multi-angle Imaging SpectroR
…
| Title |
Breaking Tsunami Waves along India's Eastern Coast |
| Original Caption Released with Image |
(3.8 MB) shows a region further south, at the northern end of India's Coromandel Coast, and covers an area of 43 kilometers x 58 kilometers. Cloud "motion" in these animations results from apparent displacements due to parallax associated with their height above the surface. The tsunami waves, on the other hand, are at sea level and show actual motion. When the waves arrive in the shallower water near the shore, they grow and, if they become large enough, they will break in a manner similar to typical oceanic waves, but on a much larger scale. The leading edge of the breaking waves is likely what is visible in the imagery. Additionally, if the tsunami waves impact the coast at an angle, they can produce what are known as "edge waves" which propagate parallel to the coast. There is clear evidence of edge wave generation in these images. Upon discovering the unique content of this imagery, MISR scientists contacted Dr. Vasily Titov at the National Oceanic and Atmospheric Administration's Pacific Marine Environmental Laboratory in Seattle, WA. Dr. Titov is an expert in the propagation of tsunamis, and has generated a model animation of the tsunami's progression from its origin near Sumatra (see http://www.pmel.noaa.gov/tsunami/indo_1204.html [ http://www.pmel.noaa.gov/tsunami/indo_1204.html ]). The MISR imagery provides measurements of the location and timing of the breaking waves, their angle relative to the shoreline, and their speed of propagation, which is estimated from these data to be around 30 kilometers/hour. In conjunction with bathymetric measurements of ocean depth, this information can be used to refine and calibrate tsunami propagation models. According to Dr. Titov, improving these models has two primary benefits. First, a detailed understanding of wave interactions with coastal areas is necessary for developing damage mitigation approaches. Second, a better predictive capability of the models will make possible more accurate near-real-time forecasts of tsunami arrival times and effects. The Multi-angle Imaging SpectroRadiometer observes the daylit Earth continuously and every 9 days views the entire globe between 82° north and 82° south latitude. These data products were generated from a portion of the imagery acquired during Terra orbit 26720 and utilize data from within blocks 77 and 78 within World Reference System-2 path 142. MISR was built and is managed by NASA's Jet Propulsion Laboratory, Pasadena, CA, for NASA's Office of Earth Science, Washington, DC. The Terra satellite is managed by NASA's Goddard Space Flight Center, Greenbelt, MD. JPL is a division of the California Institute of Technology., At 00:58:53 UTC (Coordinated Universal Time) on 26 December 2004, a magnitude 9.0 earthquake occurred off the west coast of Sumatra, Indonesia. This was the fourth largest earthquake in the world since 1900 and the largest in over 40 years. It was caused by the release of stresses in the Earth that are built up as the Indian tectonic plate descends into the mantle beneath the Burma plate. It is estimated that the sea floor was displaced several meters due to the quake, resulting in large ocean waves, called "tsunamis" from the Japanese for "harbor waves." The tsunami moved rapidly across the deep ocean, with speeds estimated around 640 km/hr. When the waves reach shallow water near land, they slow considerably, but their size increases dramatically and they strike with catastrophic force. With human casualities exceeding 150,000, this event is one of the deadliest natural disasters in modern history, causing devastation along the shores of Indonesia, Sri Lanka, India, Thailand, and other countries. The initial tsunami waves reached the eastern Indian coast around 3:35 UTC, based on tide gauge measurements made at the port city of Vishakapatnam. The Multi-angle Imaging SpectroRadiometer (MISR) aboard NASA's Terra satellite passed over the eastern Indian coast between 5:10 to 5:20 UTC, when the tide gauge indicated the arrival of another series of waves. Because MISR's nine cameras imaged the coast over a time span of about 7 minutes, and because the the waves are unusually large, MISR was able to capture unique time-lapse imagery of the breaking waves. The still image shows four frames from the instrument's backward-viewing cameras spanning a period of about 2.5 minutes. This scene is located along the shores of Andhra Pradesh, near the mouth of the Godavari River, and covers an area of 42 kilometers x 37 kilometers. The arrows show the progression of the southwestern edges of the breakers. A series of frames spanning nearly 6 minutes has been made into a small animated GIF (below). An animated GIF (5.8 MB) covering a somewhat larger area of 86 kilometers x 49 kilometers is also available. A second animated GIF |
|
Breaking Tsunami Waves along
…
PIA04372
Sol (our sun)
Multi-angle Imaging SpectroR
…
| Title |
Breaking Tsunami Waves along India's Eastern Coast |
| Original Caption Released with Image |
(3.8 MB) shows a region further south, at the northern end of India's Coromandel Coast, and covers an area of 43 kilometers x 58 kilometers. Cloud "motion" in these animations results from apparent displacements due to parallax associated with their height above the surface. The tsunami waves, on the other hand, are at sea level and show actual motion. When the waves arrive in the shallower water near the shore, they grow and, if they become large enough, they will break in a manner similar to typical oceanic waves, but on a much larger scale. The leading edge of the breaking waves is likely what is visible in the imagery. Additionally, if the tsunami waves impact the coast at an angle, they can produce what are known as "edge waves" which propagate parallel to the coast. There is clear evidence of edge wave generation in these images. Upon discovering the unique content of this imagery, MISR scientists contacted Dr. Vasily Titov at the National Oceanic and Atmospheric Administration's Pacific Marine Environmental Laboratory in Seattle, WA. Dr. Titov is an expert in the propagation of tsunamis, and has generated a model animation of the tsunami's progression from its origin near Sumatra (see http://www.pmel.noaa.gov/tsunami/indo_1204.html [ http://www.pmel.noaa.gov/tsunami/indo_1204.html ]). The MISR imagery provides measurements of the location and timing of the breaking waves, their angle relative to the shoreline, and their speed of propagation, which is estimated from these data to be around 30 kilometers/hour. In conjunction with bathymetric measurements of ocean depth, this information can be used to refine and calibrate tsunami propagation models. According to Dr. Titov, improving these models has two primary benefits. First, a detailed understanding of wave interactions with coastal areas is necessary for developing damage mitigation approaches. Second, a better predictive capability of the models will make possible more accurate near-real-time forecasts of tsunami arrival times and effects. The Multi-angle Imaging SpectroRadiometer observes the daylit Earth continuously and every 9 days views the entire globe between 82° north and 82° south latitude. These data products were generated from a portion of the imagery acquired during Terra orbit 26720 and utilize data from within blocks 77 and 78 within World Reference System-2 path 142. MISR was built and is managed by NASA's Jet Propulsion Laboratory, Pasadena, CA, for NASA's Office of Earth Science, Washington, DC. The Terra satellite is managed by NASA's Goddard Space Flight Center, Greenbelt, MD. JPL is a division of the California Institute of Technology., At 00:58:53 UTC (Coordinated Universal Time) on 26 December 2004, a magnitude 9.0 earthquake occurred off the west coast of Sumatra, Indonesia. This was the fourth largest earthquake in the world since 1900 and the largest in over 40 years. It was caused by the release of stresses in the Earth that are built up as the Indian tectonic plate descends into the mantle beneath the Burma plate. It is estimated that the sea floor was displaced several meters due to the quake, resulting in large ocean waves, called "tsunamis" from the Japanese for "harbor waves." The tsunami moved rapidly across the deep ocean, with speeds estimated around 640 km/hr. When the waves reach shallow water near land, they slow considerably, but their size increases dramatically and they strike with catastrophic force. With human casualities exceeding 150,000, this event is one of the deadliest natural disasters in modern history, causing devastation along the shores of Indonesia, Sri Lanka, India, Thailand, and other countries. The initial tsunami waves reached the eastern Indian coast around 3:35 UTC, based on tide gauge measurements made at the port city of Vishakapatnam. The Multi-angle Imaging SpectroRadiometer (MISR) aboard NASA's Terra satellite passed over the eastern Indian coast between 5:10 to 5:20 UTC, when the tide gauge indicated the arrival of another series of waves. Because MISR's nine cameras imaged the coast over a time span of about 7 minutes, and because the the waves are unusually large, MISR was able to capture unique time-lapse imagery of the breaking waves. The still image shows four frames from the instrument's backward-viewing cameras spanning a period of about 2.5 minutes. This scene is located along the shores of Andhra Pradesh, near the mouth of the Godavari River, and covers an area of 42 kilometers x 37 kilometers. The arrows show the progression of the southwestern edges of the breakers. A series of frames spanning nearly 6 minutes has been made into a small animated GIF (below). An animated GIF (5.8 MB) covering a somewhat larger area of 86 kilometers x 49 kilometers is also available. A second animated GIF |
|
Deep Ocean Tsunami Waves off
…
PIA04373
Sol (our sun)
Multi-angle Imaging SpectroR
…
| Title |
Deep Ocean Tsunami Waves off the Sri Lankan Coast |
| Original Caption Released with Image |
The initial tsunami waves resulting from the undersea earthquake that occurred at 00:58:53 UTC (Coordinated Universal Time) on 26 December 2004 off the island of Sumatra, Indonesia, took a little over 2 hours to reach the teardrop-shaped island of Sri Lanka. Additional waves continued to arrive for many hours afterward. At approximately 05:15 UTC, as NASA's Terra satellite passed overhead, the Multi-angle Imaging SpectroRadiometer (MISR) captured this image of deep ocean tsunami waves about 30-40 kilometers from Sri Lanka's southwestern coast. The waves are made visible due to the effects of changes in sea-surface slope on the reflected sunglint pattern, shown here in MISR's 46° forward-pointing camera. Sunglint occurs when sunlight reflects off a water surface in much the same way light reflects off a mirror, and the position of the Sun, angle of observation, and orientation of the sea surface determines how bright each part of the ocean appears in the image. These large wave features were invisible to MISR's nadir (vertical-viewing) camera. The image covers an area of 208 kilometers x 207 kilometers. Since the greatest impact of the tsunami was generally in an east-west direction, the havoc caused by the tsunami along the southwestern shores of Sri Lanka was not as severe as along the eastern coast, though there was still substantial damage in this region--as evidenced by the brownish debris in the water--because tsunami waves can diffract around land masses. The ripple-like wave pattern evident in this MISR image roughly correlates with the undersea boundary of the continental shelf. This surface manifestation is likely to be caused by interaction of deep waves with the ocean floor, rather than by the more usually-observed surface waves driven by winds. It is possible that this semi-concentric pattern represents wave reflection from the continental land mass, however, a combination of wave modeling and detailed bathymetric data is required to fully understand the dynamics. Examination of other MISR images of this area, taken under similar illumination conditions, has not uncovered any surface patterns resembling those seen here. This image is an example of how MISR's multiangular capability provides unique information for understanding how tsunamis propagate. Another application of MISR data enabled measuring the motion of breaking tsunami waves [ http://www-misr.jpl.nasa.gov/gallery/galhistory/2005_jan_12.html ], along the eastern shores of Andhra Pradesh, India. The Multi-angle Imaging SpectroRadiometer observes the daylit Earth continuously and every 9 days views the entire globe between 82° north and 82° south latitude. These data products were generated from a portion of the imagery acquired during Terra orbit 26720 and utilize data from within blocks 85 to 86 within World Reference System-2 path 142. MISR was built and is managed by NASA's Jet Propulsion Laboratory, Pasadena, CA, for NASA's Office of Earth Science, Washington, DC. The Terra satellite is managed by NASA's Goddard Space Flight Center, Greenbelt, MD. JPL is a division of the California Institute of Technology. |
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