acquired June 2, 2012
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acquired June 2, 2012
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acquired June 2, 2012
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Impact craters can be tough to detect
from the ground, especially if they are situated in remote locations
and covered by vegetation. Both factors hampered understanding of the
Luizi Structure, located in southeastern Congo. The crater is covered by
grasses up to a meter (3 feet) high, and tucked away in central Africa.
The Advanced Land Imager (ALI) on NASA’s Earth Observing-1 (EO-1) satellite captured this natural-color image of Luizi on June 2, 2012. It is not perfectly round, but instead fills a semicircular basin where vegetation carpets the complicated topography.
A mention of Luizi made it into a geological report in 1919, but the feature remained unexplored for decades. Satellite imagery of the structure from the 1990s inspired an international team of geologists to look more closely. In 2011, they announced their findings.
Satellite imagery suggested that Luizi might be an impact crater, but volcanoes and even salt domes can form structures that look like impact craters, so the researchers had to go into the field. They found shatter cones, and microscopic analysis of rock samples collected from the site revealed shocked quartz grains. Both shatter cones and shocked quartz are considered strong evidence of meteorite impacts.
Impact craters can be simple or complex. While simple craters have uncomplicated bowl shapes, complex craters sport features that can be counterintuitive, such as inner rings and central peaks. Geologists have linked both crater types to the action of high-velocity impacts.
The researchers studying Luizi reported that the crater spans about 17 kilometers (11 miles) in diameter, with an intermittent ring about 5.2 kilometers (3.2 miles) across, and a smaller, center ring about 2 kilometers (1.2 miles) across. Around the perimeter of the crater, a rim rises approximately 300 to 350 meters (980 to 1,150 feet) above the interior. In short, Luizi is a well-preserved, moderately sized, complex crater.
Exactly when Luizi formed is hard to answer. The researchers estimate that nearby rocks are 575 million years old—more than 300 million years older than the first dinosaurs. But besides knowing that the impact can’t be older than the rock layers it disrupted, the geologists can’t yet say when the impact occurred. Whenever the meteorite arrived, it may have been moving as fast as 72,000 kilometers (45,000 miles) per hour.
The Advanced Land Imager (ALI) on NASA’s Earth Observing-1 (EO-1) satellite captured this natural-color image of Luizi on June 2, 2012. It is not perfectly round, but instead fills a semicircular basin where vegetation carpets the complicated topography.
A mention of Luizi made it into a geological report in 1919, but the feature remained unexplored for decades. Satellite imagery of the structure from the 1990s inspired an international team of geologists to look more closely. In 2011, they announced their findings.
Satellite imagery suggested that Luizi might be an impact crater, but volcanoes and even salt domes can form structures that look like impact craters, so the researchers had to go into the field. They found shatter cones, and microscopic analysis of rock samples collected from the site revealed shocked quartz grains. Both shatter cones and shocked quartz are considered strong evidence of meteorite impacts.
Impact craters can be simple or complex. While simple craters have uncomplicated bowl shapes, complex craters sport features that can be counterintuitive, such as inner rings and central peaks. Geologists have linked both crater types to the action of high-velocity impacts.
The researchers studying Luizi reported that the crater spans about 17 kilometers (11 miles) in diameter, with an intermittent ring about 5.2 kilometers (3.2 miles) across, and a smaller, center ring about 2 kilometers (1.2 miles) across. Around the perimeter of the crater, a rim rises approximately 300 to 350 meters (980 to 1,150 feet) above the interior. In short, Luizi is a well-preserved, moderately sized, complex crater.
Exactly when Luizi formed is hard to answer. The researchers estimate that nearby rocks are 575 million years old—more than 300 million years older than the first dinosaurs. But besides knowing that the impact can’t be older than the rock layers it disrupted, the geologists can’t yet say when the impact occurred. Whenever the meteorite arrived, it may have been moving as fast as 72,000 kilometers (45,000 miles) per hour.
Related Resources
- Department of Earth Science and Engineering. (2012) The formation of complex craters. Imperial College, London. Accessed June 8, 2012.
- Ferrière, L., Lubala, F.R.T., Osinski, G.R., Kaseti, P.K. (2011) The Luizi Structure (Democratic Republic of Congo) — First confirmed meteorite impact crater in Central Africa. 42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas.
- Ferrière, L., Osinski, G.R. (2011) The new Luizi Impact Structure (Democratic Republic of Congo) and implications for central peak and peak ring formation. 42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas.
- Jaggard, V. (2011, March 8) Huge impact crater found in remote Congo. Accessed June 8, 2012.
NASA Earth Observatory image by Jesse Allen and Robert Simmon, using Advanced Land Imager data from the NASA EO-1 team. Caption by Michon Scott.
- Instrument:
- EO-1 - ALI
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