<p>Within the next decade or so, Venus will be visited by a fleet of spacecraft. This grand tour of the second planet, the likes of which hasn’t been seen since the Cold War, is being driven by the quest to solve a profound planetary puzzle. Earth and Venus are the same size, are right next to each other and are made of the same star stuff. But Earth became an oasis while Venus became an acid-flecked inferno. Why?</p>.<p>To derive an answer, every aspect of Venus requires examination. That includes the way its face has metamorphosed over time. Earth has plate tectonics, the gradual migration of continent-size geologic jigsaw pieces on its surface — a game-changing sculptor that crafts an exuberance of diverse volcanoes, giant mountain ranges and vast ocean basins.</p>.<p>Venus doesn’t have plate tectonics. But according to a study published Monday in the Proceedings of the National Academy of Sciences, it may possess a quirky variation of that process: Parts of its surface seem to be made up of blocks that have shifted and twisted about, contorting their surroundings as they went.</p>.<p>These boogying blocks, thin and flat slices of rock referred to as campi (Latin for “fields”), can be as small as Ireland or as expansive as Alaska. They were found using data from NASA’s Magellan orbiter mission, the agency’s last foray to Venus. In the early 1990s, it used radar to peer through the planet’s obfuscating atmosphere and map the entire surface. Taking another look at these maps, scientists found 58 campi scattered throughout the planet’s lava-covered lowlands.</p>.<p>These campi are bordered by lines of small mountain ranges and grooves, features that have also been warped and scarred over time. What made them? According to Paul Byrne, a planetary scientist at North Carolina State University and the study’s lead author, there is only one reasonable explanation: Essentially dragged around by the flowing mantle below, the campi “have been shimmying around the place, just like pack ice.”</p>.<p>Is this dance still happening today?</p>.<p>NASA’s VERITAS and Europe’s EnVision missions will find out. Equipped with their own advanced radar systems, these orbiters will examine these campi in high-resolution, allowing scientists to ascertain if any have shimmied about since the days of Magellan. If they have, then it will further evidence a long-harbored notion: Venus is tectonically active, if not as hyperactive or as dynamic as Earth.</p>
<p>Within the next decade or so, Venus will be visited by a fleet of spacecraft. This grand tour of the second planet, the likes of which hasn’t been seen since the Cold War, is being driven by the quest to solve a profound planetary puzzle. Earth and Venus are the same size, are right next to each other and are made of the same star stuff. But Earth became an oasis while Venus became an acid-flecked inferno. Why?</p>.<p>To derive an answer, every aspect of Venus requires examination. That includes the way its face has metamorphosed over time. Earth has plate tectonics, the gradual migration of continent-size geologic jigsaw pieces on its surface — a game-changing sculptor that crafts an exuberance of diverse volcanoes, giant mountain ranges and vast ocean basins.</p>.<p>Venus doesn’t have plate tectonics. But according to a study published Monday in the Proceedings of the National Academy of Sciences, it may possess a quirky variation of that process: Parts of its surface seem to be made up of blocks that have shifted and twisted about, contorting their surroundings as they went.</p>.<p>These boogying blocks, thin and flat slices of rock referred to as campi (Latin for “fields”), can be as small as Ireland or as expansive as Alaska. They were found using data from NASA’s Magellan orbiter mission, the agency’s last foray to Venus. In the early 1990s, it used radar to peer through the planet’s obfuscating atmosphere and map the entire surface. Taking another look at these maps, scientists found 58 campi scattered throughout the planet’s lava-covered lowlands.</p>.<p>These campi are bordered by lines of small mountain ranges and grooves, features that have also been warped and scarred over time. What made them? According to Paul Byrne, a planetary scientist at North Carolina State University and the study’s lead author, there is only one reasonable explanation: Essentially dragged around by the flowing mantle below, the campi “have been shimmying around the place, just like pack ice.”</p>.<p>Is this dance still happening today?</p>.<p>NASA’s VERITAS and Europe’s EnVision missions will find out. Equipped with their own advanced radar systems, these orbiters will examine these campi in high-resolution, allowing scientists to ascertain if any have shimmied about since the days of Magellan. If they have, then it will further evidence a long-harbored notion: Venus is tectonically active, if not as hyperactive or as dynamic as Earth.</p>