Earth Observations taken by the Expedition 18 Crew

ISS018-E-006051 (29 Oct. 2008) --- Deriba Caldera in Sudan is featured in this image photographed by an Expedition 18 crewmember on the International Space Station. Deriba Caldera is a geologically young volcanic structure located at the top of the Marra Mountains of western Sudan. The Marra Mountains are part of a large geologic feature known as the Darfur Dome -- this structure is thought to be the result of a mantle plume heating the crust from below, leading to uplift of the crust and providing a magma source for the extensive volcanism observed in the region. According to scientists, the five-kilometers-wide Deriba Caldera was formed by explosive eruption of the Jebel Marra volcano approximately 3,500 years ago. The volcano is considered dormant, as hot springs and fumaroles (gas and steam vents) are still present. The caldera presents a classic crater morphology, formed as overlying rock and soil collapsed into the magma chamber after it was emptied by powerful eruptions -- shadows in this image throw the steep southern wall of the outer crater into sharp relief. Following the formation of the main outer crater a second inner crater (center) formed, most likely due to later uplift and eruption of fresh magma moving towards the surface. This inner crater is filled with water -- however, as its outer walls are higher than the adjacent caldera floor, precipitation flowing inwards from the outer crater walls do not enter the inner crater lake. White stream bed sediments (center) show the water pathway around the inner crater to a second lake located along the northeast wall of the outer crater. While Jebel Marra is high enough (3,042 meters) to have a temperate climate and high precipitation, these lakes may also be fed by hot springs. The inner crater lake has a mottled appearance caused by sunglint.