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Krishna Ramanujan Goddard Space Flight Center, Greenbelt, Md. (Phone: 301/286-3026)

To get daily reports from the expedition and more information about ICE 2002 check out the expedition web site at: ICE2002 website

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Caption for Images 1-5: REMOTE AND WILD: SCIENCE IN THE BOLIVIAN JUNGLE

The Iturralde structure's remoteness has been one of the more frustrating factors facing scientists working to verify the origin of the structure. The Iturralde Structure is located approximately 180 miles (288 km) from the nearest civilized town of Riberalta, Bolivia. These still images from the 1998 Iturralde Crater Expedition show the remote working conditions the ICE 2002 team will encounter during their expedition through the jungle. The ICE 2002 team will reach the crater impact site after traveling by jet airliner, small airplane, motor boat, dugout canoe, and finally by walking a 15 km long trail, cut by the 1998 expedition, through the forest. Credit: Peter Wasilewski, NASA GSFC

 

 

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September 04, 2002 - (date of web publication)

NASA SCIENTISTS DETERMINED TO UNEARTH ORIGIN OF THE ITURRALDE CRATER

These still images from the 1998 Iturralde Crater Expedition show the remote working conditions the ICE 2002 team will encounter during their expedition through the jungle.

 

Image 1

 

NASA scientists will venture into an isolated part of the Bolivian Amazon to try and uncover the origin of a 5 mile (8 kilometer) diameter crater there known as the Iturralde Crater. Traveling to this inhospitable forest setting, the Iturralde Crater Expedition 2002 will seek to determine if the unusual circular crater was created by a meteor or comet.

Organized by Dr. Peter Wasilewski of NASA's Goddard Space Flight Center, Greenbelt, Md., the Iturralde Crater Expedition 2002 will be led by Dr. Tim Killeen of Conservation International, which is based in Bolivia. Killeen will be assisted by Dr. Compton Tucker of Goddard.

These still images from the 1998 Iturralde Crater Expedition show the remote working conditions the ICE 2002 team will encounter during their expedition through the jungle.

 

Image 2

 

The team intends to collect and analyze rocks and soil, look for glass particles that develop from meteor impacts and study magnetic properties in the area to determine if the Iturralde site, discovered in the mid-1980s with satellite imagery, was indeed created by a meteor.

If a meteorite is responsible for the impression, rocks in the area will have shock features that do not develop under normal geological circumstances. The team will also look for glass particles, which develop from the high temperatures of impact.

These still images from the 1998 Iturralde Crater Expedition show the remote working conditions the ICE 2002 team will encounter during their expedition through the jungle.

 

Image 3

 

The Iturralde Crater Expedition 2002 team will extensively analyze soil in the impact zone for confirmation of an impact. One unique aspect of the Iturralde site is the 4-5 km deep surface sediment above the bedrock. Thus the impact was more of a gigantic "splat" rather than a collision into bedrock.

The large crater is only 1 meter lower in elevation than the surrounding area. Water collects within the depression, but not on the rim of the crater, which is slightly higher than both the surrounding landscape and the interior of the crater. These subtle differences in drainage are reflected in the forest and grassland habitats that developed on the landscape. It is precisely these differences in the vegetation structure that can be observed from space and which led to the identification of the Iturralde Crater in the 1970s when Landsat Images first became available for Bolivia.

These still images from the 1998 Iturralde Crater Expedition show the remote working conditions the ICE 2002 team will encounter during their expedition through the jungle.

 

Image 4

 

Impact craters can also be confirmed through the magnetic study of the impact zone. Dr. Wasilewski's team will conduct ground magnetometer surveys and will examine the area through an unmanned aerial vehicle plane fitted with a magnetometer, an instrument for measuring the magnitude and direction of magnetic field. The resulting data will be analyzed by associating the magnetic readings with geographical coordinates, to map magnetic properties of the area. The magnetometer data could provide conclusive evidence as to whether or not the Iturralde feature is an impact crater.

These still images from the 1998 Iturralde Crater Expedition show the remote working conditions the ICE 2002 team will encounter during their expedition through the jungle.

 

Image 5

 

The Iturralde Crater Expedition 2002 expedition also contains an education component. Teachers from around the world who are involved with the teacher professional development program, called Teacher as Scientist, have helped to design the expedition. One teacher will actually be on-site assisting with data collection.

University students from Bolivia will also be involved in the expedition. The educational element of the expedition is just as important as the science results," said Goddard engineer Patrick Coronado. "This is one of those experiments that stirs the imagination, where science and technology come head-to-head with nature in an attempt to unlock its secrets."



This Landsat image shows the 8 km circular Iturralde Structure that resembles a meteor impact on the eastern Bolivian landscape.

 

Image 6

 

Caption for Image 6 / animation: ITURRALDE STRUCTURE VISUALIZATION

This Landsat image shows the 8 km circular Iturralde Structure that resembles a meteor impact on the eastern Bolivian landscape. The Iturralde Structure is located in perhaps the most remote and wildest part of the Bolivian lowlands. The crater is situated on the boarder of the Amazon forest and the vast open savannas of eastern Bolivia.

The MAGPLANE is a one-third scale, remote controlled model of a 1930 Piper Cub airplane.

 

Image 7

 

Caption for Image 7 / animation:

Image 7: MAGPLANE IMAGE The MAGPLANE is a one-third scale, remote controlled model of a 1930 Piper Cub airplane. It is outfitted with a magnetometer, auto-pilot, GPS, onboard computer and a satellite communication system and will be used to remotely collect data of the magnetic signature in and around the Iturralde Structure. Click here for an enlargement of this image.

Animation: MAGPLANE FLIGHT PATH VISUALIZATION

The MAGPLANE will take off from a dirt runway at Porta Araona, within the Bolivian jungle under the remote control of an operator. After an in-flight checkout, the remote system will be turned off and the onboard autopilot will fly the plane through the preprogrammed flight path at an altitude of about 200ft. The plane's instruments will record the magnetometer data and simultaneously transmit the data via satellite for researchers in Bolivia and the United States. After completing its flight plan, the MAGPLANE will return to the launch site, where the operator will reclaim remote control and land the plane. It may take several days to complete the planned magnetic survey flight plan shown in this visualization.

This visualization shows the distribution of verified impact structures across the globe.

 

Image 8

 

Caption for Image 8 / animation: GLOBAL DISPERSION OF VERIFIED IMPACT CRATERS

Approximately 150 geological structures have been verified as meteor impact craters on the Earth. It is estimated that several hundred more remain to be identified. This visualization shows the distribution of verified impact structures across the globe. The small dots represent impact crater diameters of .02 - 20km in diameter. The medium size dots represent impact crater diameters of 20 - 100 km in diameter. The largest dots represent impact craters of 100 - 300 km in diameter.

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