The European Space Agency released a satellite pair of earthquakes that rocked Venezuela last week.
The s, which are part of the European Copernicus program. These satellites do not take conventional photographs; instead, they use their radars to “illuminate” the Earth’s surface and record the time it takes for the signal to return to the sensor. By comparing two measurements of the same location taken on different dates, scientists can determine whether the ground has shifted, even when that shift is too small to be seen with the naked eye.
To create the map, scientists compared an observation taken on June 18—one week before the earthquakes—with another taken on June 25, the day after the pair of earthquakes that were mangitude 7.2 and 7.5 respectively. This comparison allowed them to construct what’s known as an interferogram revealing how much the ground deformed following the event.
The ESA explains that what stands out in the map are the repeating colored bands that form horizontal rows in the north. Each complete repetition of the sequence—blue, green, yellow, red, and blue again—represents a fixed increase in the change in distance between the satellite and the ground. The more complete cycles that appear between one area and another, the greater the cumulative ground displacement.
The pattern of bands observed in the northern part of the map corresponds to the region at the epicenter of the earthquakes, which is also where the main deformation occurred. The bands roughly follow the path of the San Sebastián fault system, one of the main tectonic structures in northern Venezuela. The ESA estimates that the displacement in the region was on the order of 30 centimeters (12 inches).
