Cosiguina Volcano, Nicaragua
Three Central American countriesâ€”El Salvador, Honduras, and Nicaraguaâ€”have coastline along the Gulf of Fonseca, which opens into the Pacific Ocean. The southern boundary of the Gulf is a peninsula formed by the Cosigueina Volcano. Cosigueina is a stratovolcano, which is a cone-shaped volcano formed by alternating layers of solidified lava and volcanic rocks produced by explosive eruptions. The summit crater is filled with a lake (Laguna Cosigueina). The volcano last erupted in 1859, but its most famous activity occurred in 1835, when it produced the largest historical eruption in Nicaragua. Ash from the 1835 eruption has been found in Mexico, Costa Rica, and Jamaica.
The volcano has been quiet since 1859, only an instant in terms of geological time. An earthquake swarm was measured near Cosigueina in 2002, indicating that tectonic forces are still active in the region although the volcano is somewhat isolated from the line of more recently active Central American volcanoes to the northwest and southeast. The only indicators of hydrothermal activity at the volcano are intermittently observed gas bubbles in Laguna Cosigueina and a hot spring along the eastern flank of the volcano. The fairly uniform vegetation cover (green) on the volcano's sides also attest to a general lack of gas emissions or â€œhot spotsâ€ on the 872-meter-high cone.
The featured astronaut photograph, ISS016-E-10894, was acquired November 17, 2007, with a Kodak 760C digital camera using an 180 mm lens, and is provided by the ISS Crew Earth Observations experiment and the Image Science & Analysis Laboratory, Johnson Space Center.