volcano on the planet Mars, the highest point on the planet and the largest known volcano in the solar system. Centred at 19° N, 133° W, Olympus Mons consists of a central edifice 22 km (14 miles) high and 700 km (435 miles) across. Around its perimeter an outward-facing cliff ascends as high as 10 km (6 miles) above the surrounding area. At the summit is an 85-km- (53-mile-) diameter crater, or caldera, comprising several mutually intersecting craters. For comparison, the largest volcano on Earth, Mauna Loa, Hawaii, measures 120 km (75 miles) across at its widest extent and rises 9 km (5.6 miles) above the ocean floor. Broad, gradually sloping flanks and the presence of numerous long flows and lava channels identify Olympus Mons as a shield volcano and suggest that it was built up from eruptions largely of fairly fluid basaltic lava. Its tremendous size has been attributed to the stability of the Martian crust and to a long accumulation time, possibly more than a billion years.
Olympus Mars Volcano
Olympus Mons (Latin for Mount Olympus) is a large volcanic mountain on the planet Mars. By one measure it has a height of nearly 22 km (14 mi);[3] the tallest known mountain in the Solar System, almost three times as tall as Mount Everest.
Wednesday, May 16, 2012
Introductions and Information about Olympus Mars Volcano
Olympus Mons,
volcano on the planet Mars, the highest point on the planet and the largest known volcano in the solar system. Centred at 19° N, 133° W, Olympus Mons consists of a central edifice 22 km (14 miles) high and 700 km (435 miles) across. Around its perimeter an outward-facing cliff ascends as high as 10 km (6 miles) above the surrounding area. At the summit is an 85-km- (53-mile-) diameter crater, or caldera, comprising several mutually intersecting craters. For comparison, the largest volcano on Earth, Mauna Loa, Hawaii, measures 120 km (75 miles) across at its widest extent and rises 9 km (5.6 miles) above the ocean floor. Broad, gradually sloping flanks and the presence of numerous long flows and lava channels identify Olympus Mons as a shield volcano and suggest that it was built up from eruptions largely of fairly fluid basaltic lava. Its tremendous size has been attributed to the stability of the Martian crust and to a long accumulation time, possibly more than a billion years.
volcano on the planet Mars, the highest point on the planet and the largest known volcano in the solar system. Centred at 19° N, 133° W, Olympus Mons consists of a central edifice 22 km (14 miles) high and 700 km (435 miles) across. Around its perimeter an outward-facing cliff ascends as high as 10 km (6 miles) above the surrounding area. At the summit is an 85-km- (53-mile-) diameter crater, or caldera, comprising several mutually intersecting craters. For comparison, the largest volcano on Earth, Mauna Loa, Hawaii, measures 120 km (75 miles) across at its widest extent and rises 9 km (5.6 miles) above the ocean floor. Broad, gradually sloping flanks and the presence of numerous long flows and lava channels identify Olympus Mons as a shield volcano and suggest that it was built up from eruptions largely of fairly fluid basaltic lava. Its tremendous size has been attributed to the stability of the Martian crust and to a long accumulation time, possibly more than a billion years.
Subscribe to:
Comments (Atom)




