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PIX4658526: Volcano Fogo - Cape Verde - Volcano Fogo - Cape Verde islands - Fogo Island with its highest volcano 2800 meters south of the Cape Verde archipelago. Image obtained from the EO-1 satellite on 10 June 2009. Fogo is one of the Cape Verde Islands located roughly 640 kilometers off the westernmost tip of Africa, Fogo received its name from English colonists around 1500 AD. 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 eastern half of the crater wall is gone, erased in a massive collapse deep in its ancient history. 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. The crater is inhabited. A straight road cuts between the crater wall and Pico, ending near the wind 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 / Bridgeman Images
PIX4649621: Decolving the shuttle Endeavour - May 2011 - Liftoff of Space Shuttle Endeavour. May 2011 - Launch of space shuttle Endeavour on 16 May 2011. Mission STS-134, last flight of shuttle Endeavour. Amid the tranquility of a wildlife refuge, space shuttle Endeavour rumbles off Launch Pad 39A at Nasa's Kennedy Space Center in Florida. Endeavour began its final flight, the STS - 134 mission, to the International Space Station on time at 8:56 a.m. EDT on May 16. Endeavour and its six - member crew are embarking on a mission to deliver the Alpha Magnetic Spectrometer - 2 (AMS), Express Logistics Carrier - 3, a high - pressure gas tank and additional spare parts for the Dextre robotic helper to the space station. Endeavour's first launch attempt on April 29 was scrubbed because of an issue associated with a faulty power distribution box called the aft load control assembly - 2 (ALCA - 2) / Bridgeman Images
TEC4649640: La Casa de Pilatos (1540), Quartier Santa Cruz in Seville (Spain). Finish in the first third of the 16th century, this palace, owned by the Duke of Medinaceli, combines in an astonishing way mudejar art, flamboyant Gothic and Renaissance art. According to popular belief, this palace is the reproduction of Pontius Pilate's palace in Jerusalem. Photography 10/03/97. / Bridgeman Images
PIX4594943: Apollo mission: astronaut training - Apollo desert survival training - Three astronauts participate in survival training in the desert (Washington State). From left to right, astronauts Charles M. Duke, Jr. and Thomas K. Mattingly, Colonel Bohart, and astronaut John L. Swigert. August 1967. Three astronauts participating in Apollo desert survival training in Washington state pose with Air Force Col. Chester Bohart (second from right). Standing from left to right are Charles M. Duke, Jr., Thomas K Mattingly, Col. Bohart, and John L. Swigert. Since the Mercury Program, astronauts have taken survival courses in case they are forced to land on a remote part of the Earth where they may need to do without human help for several weeks. August 1967 / Bridgeman Images
TEC4595021: Fouquet's avenue des Champs Elysees, Paris 8th round. It was Jean Baptiste (Jean-Baptiste) Colbert (1619-1683) who had Andre Le Notre (1613-1700) opened in 1667 an avenue starting from the Tuileries to reach a hill, today called L'Etoile. There's nothing left from that time. Only nineteenth century witnesses remain on the Champs Elysees. / Bridgeman Images
PIX4595105: Apollo 7/Saturn IV B - Saturn IVB stage from the Apollo 7 spacecraft - Saturn IV B photograph of the Apollo 7 module during mooring maneuvers. 1968. The expended Saturn IVB stage as photographed from the Apollo 7 spacecraft during transposition and docking maneuvers. 1968 / Bridgeman Images
PIX4595151: Apollo 9: Saturn V rocket - Apollo 9: Saturn V roll out - Saturn V rocket en route to its fire pad at the Kennedy space center. January 3, 1969. Aerial view of the Apollo 9 (Spacecraft 104/Lunar Module 3/Saturn 504) space vehicle on the way from the Vehicle Assembly Building to Pad A, Launch Complex 39, Kennedy Space Center. The Saturn V stack and its mobile launch tower are atop a huge crawler - transporter. (view looking toward Pad A) Jan 3, 1969 / Bridgeman Images
PIX4619956: Eagle Nebula (IC 4703) and M16 star cluster in the Snake - Eagle nebula in Serpens - The Eagle Nebula is a cluster of massive young stars (M16) surrounded by clouds of gas and dust. The three columns in the center of the image were sculpted by the intense radiation emitted by these massive stars. Stars will be born in these clouds if they survive the intense radiation that erodes these pillars. Messier 16 is a cluster of young stars which formed about 2 million years ago from the gas and dust which still surrounds them. Brilliant blue stars of this type are much hotter than the Sun and can be up to thirty times more massive. The dark intrusions visible across the face of the nebula are condensations of dusty material which might one day collapse into yet more stars, should they survive the radiation from the bright stars, which is gradually etching them away. Bright red regions of photo - ionised hydrogen such as M16 are usually found in the spiral arms of galaxies and are often associated recent star formation. This example is about 6000 - 7000 light years distant / Bridgeman Images
PIX4616083: Mars: crater in Myers Valles - Mars: crater in Myers Valles - Mamers Valles is a valley about 1000 km long located in the region of Deuteronilus Mensae, north of Arabia Terra. The image obtained by the Mars Express probe on 5 August 2006 shows a crater at the end of this valley. This circular formation measures about thirty kilometres in diameter and is 1400 metres deep. There are traces of flow of material probably composed of water ice, similar to the relief left by the passage of glaciers on Earth. The darker area could be caused by local erosion or wind-driven material. The High - Resolution Stereo Camera (HRSC) onboard the ESA spacecraft Mars Express obtained images focusing on a depression that displays a crater at the end of the long, winding valley, Mamers Valles. The data was obtained on 5 August 2006 with a ground resolution of approximately 14 m/per pixel. The image is centred at approximately 39* north and 17* east on the planet. The valley of Mamers Valles is approximately 1000 km long, running along the boundary between the northern lowlands and southern highlands in the region of Deuteronilus Mensae. This region shows numerous deep and wide labyrinth - like valleys and circular depressions which often show structures formed by flowing liquid on their even floors. The structures formed by the flows are thought to be ice - rich debris flows. They show some resemblance to block glaciers seen on Earth. The patches of rock at the centre of the depression are thought to be remnants of rock detached from the flanks of the depression and transported into its centre. The wrinkle ridges, are formed by compressive forces acting on the surface. The dark coloured material inside the crater could have formed in - situ or was transported by the wind. The depression is approximately 30 km wide and 1400 m deep / Bridgeman Images
PIX4616151: Mars: craters and channels in Hephaestus Fossae - Mars: craters and channels in Hephaestus Fossae - Impact crateres and channel system in Hephaestus Fossae, a region on Mars located on the western flank of Elysium Mons. The large impact crater at the top of the picture is 20 km in diameter. The image covering an area of about 150 square km was obtained by the Mars Express probe on 28 December 2007. This image of Hephaestus Fossae was obtained by Esa's Mars Express orbiter on 28 December 2007. The region is dotted with craters and channel systems and lies at about 21* North and 126* East on the Red Planet. Named after the Greek god of fire, Hephaestus Fossae extends for more than 600 km on the western flank of Elysium Mons in the Utopia Planitia region. The surface is mostly smooth, and is covered by several small impact craters measuring 800 to 2800 m in diameter. Smaller craters are scattered across the entire region. A larger impact crater measuring 20 km in diameter is a prominent feature. Covering an area of approximately 150 sq km, this crater could harbour cities such as Bonn or Kiel. In contrast to the smaller craters, it shows a blanket of ejecta with flow forms surrounding the rim. The large craters were formed when loose, soft material was ejected due to impact, and the smaller ones formed due to secondary impacts, when consolidated material was ejected in a ballistic path and impacted the original crater at varying distances. Most martian water exists in the form of subsurface ice. The presence of a blanket of ejecta and outflow channels around the crater suggest that the primary impact may have penetrated the surface enough to melt a buried frozen water reservoir / Bridgeman Images
PIX4616156: Mars: craters and channels in Hephaestus Fossae - Mars: craters and channels in Hephaestus Fossae - Impact crateres and channel system in Hephaestus Fossae, a region on Mars located on the western flank of Elysium Mons. The large impact crater on the left of the image measures 20 km in diameter. The image covering an area of about 150 square km was obtained by the Mars Express probe on 28 December 2007. This image of Hephaestus Fossae was obtained by Esa's Mars Express orbiter on 28 December 2007. The region is dotted with craters and channel systems and lies at about 21* North and 126* East on the Red Planet. Named after the Greek god of fire, Hephaestus Fossae extends for more than 600 km on the western flank of Elysium Mons in the Utopia Planitia region. The surface is mostly smooth, and is covered by several small impact craters measuring 800 to 2800 m in diameter. Smaller craters are scattered across the entire region. The left side of the image shows a large impact crater measuring 20 km in diameter. Covering an area of approximately 150 sq km, a crater of this size on Earth could harbour cities such as Bonn or Kiel. In contrast to the smaller craters, it shows a blanket of ejecta with flow forms surrounding the rim / Bridgeman Images
PIX4616176: March: chaotic terrain between Kasei Valles and Sacra Fossae - Mars: Chaotic terrain between Kasei Valles and Sacra Fossae - Region bordering Kasei Valles and Sacra Fossae. To the north, the large impact crater is 35 km in diameter. The image covering an area of 225 km by 95 km was obtained by the Mars Express probe. Mars Express flew over the boundary between Kasei Valles and Sacra Fossae and imaged the region, acquiring spectacular views of the chaotic terrain in the area. The images are centred at 12* N/285* E and have a ground resolution of about 21 m/pixel. They cover 225 x 95 km or 21.375 sq km, an area roughly half the size of the Netherlands. The image shows an old 35 km - diameter impact crater in the north. The crater's southwestern rim is eroded strongly, mostly by flowing water. The source of the water was located in Etus Chasma, which lies about 850 km to the southwest. The crater floor and the northwestern part are remarkably flat, formed by sediments and basaltic lava flows from the Tharsis volcanic region / Bridgeman Images
PIX4616213: March -View of the south pole - Mars South Pole: Image of the southern polar cap of Mars obtained by the Mars Express probe on December 17, 2012. The bright white region of this image shows the icy cap that covers Mars' south pole, composed of frozen water and carbon dioxide. The southern cap reaches some 3 km thick in places, and is around 350 km in diameter. This icy region is permanent; in the martian winter another, thinner ice cap forms over the top of it, stretching further out across the planet and disappearing again when the weather warms up. Mars Express imaged this area of March on 17 December 2012, in infrared, green and blue light, using its High Resolution Stereo Camera. / Bridgeman Images