Fogo—fire—is an apt name for this imposing volcanic island. One of the Cape Verde Islands located roughly 640 kilometers off the westernmost tip of Africa, Fogo received its name from Portuguese colonists around 1500 AD. The volcano was almost continuously active from that time until about 1760, said the Smithsonian Global Volcanism Program.
The Advanced Land Imager on NASA’s EO-1 satellite captured this detailed image of the volcano on June 10, 2009. The volcano’s most distinctive feature, its nine-kilometer wide caldera, Cha Caldera, is shown in this image. The crater wall in the west towers one kilometer above the crater floor. The eastern half of the crater wall is gone, erased in a massive collapse deep in its ancient history.
Evidence of the volcano’s more recent eruptive history is written on the surface of the crater as well. In the center of the crater, a steep cone named Pico rises about 100 meters above the crater rim (more than a kilometer from the crater floor). The young peak reaches 2,829 meters (9,281 feet) above sea level, making it the island’s highest point.
Dark trails of hardened lava from the volcano’s most recent eruptions stream out of the crater east into the Atlantic Ocean. The volcano last erupted in 1995. The sepia stream of lava from that eruption is pooled near the crater rim west of Pico.
Remarkably, the crater is inhabited. A straight road cuts between the crater wall and Pico, ending near the vent that erupted in 1995. Bright white dots on the north side of the crater are villages. Residents of the Cha Caldera evacuated during the eruption.
NASA image created by Jesse Allen, using EO-1 ALI data provided courtesy of the NASA EO-1 Team. Caption by Holli Riebeek.
The volcano was almost continuously active from the 1500s until 1760.
Germany’s Ries Crater (or Nördlinger Ries) is not easily discerned in space-based images. The crater’s existence was probably just as subtle to the medieval Europeans who established a settlement inside it and unknowingly matched their 1-kilometer- (0.6-mile-) wide city to the likely diameter of the meteorite that formed the crater.
Wolfe Creek Crater is the second largest crater in the world from which meteorite fragments have been collected. Because of its excellent preservation, the crater clearly shows the classic features that result from a large meteorite striking the Earth.
India’s Lonar Crater began causing confusion soon after it was identified. Lonar Crater sits inside the Deccan Plateau—a massive plain of volcanic basalt rock leftover from eruptions some 65 million years ago. Its location in this basalt field suggested to some geologists that it was a volcanic crater. Today, however, Lonar Crater is understood to result from a meteorite impact that occurred between 35,000 and 50,000 years ago.