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Bilder zu 'Volcanic Activity' gefunden, 200

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Polished stones from Mount Vesuvius, c 1770

Polished stones from Mount Vesuvius, c 1770

UIS5080773

Volcanoes on Io, one of the moons of Jupiter, 1979

Volcanoes on Io, one of the moons of Jupiter, 1979

UIS5070926

Pieces of lava from Mount Vesuvius, c 1770

Pieces of lava from Mount Vesuvius, c 1770

UIS5080731

Mount Vesuvius' crater, Kingdom of Naples, 1767

Mount Vesuvius' crater, Kingdom of Naples, 1767

UIS5080533

Mount Vesuvius' crater, Kingdom of Naples, 1767

Mount Vesuvius' crater, Kingdom of Naples, 1767

UIS5080520

Hot spring in the Solfaterra, near Naples, Kingdom of Naples, c 1760

Hot spring in the Solfaterra, near Naples, Kingdom of Naples, c 1760

UIS5080600

Rock fragments from Mount Vesuvius, c 1770

Rock fragments from Mount Vesuvius, c 1770

UIS5080763

Stones and crystals from Mount Vesuvius, c 1770

Stones and crystals from Mount Vesuvius, c 1770

UIS5080786

The outside of Solfaterra's cone, near Puzzoli, Kingdom of Naples, c 1760

The outside of Solfaterra's cone, near Puzzoli, Kingdom of Naples, c 1760

UIS5080609

Lava from Mount Vesuvius, c 1770

Lava from Mount Vesuvius, c 1770

UIS5080758

Rock fragments from Fossa Grande, Mount Vesuvius, c 1770

Rock fragments from Fossa Grande, Mount Vesuvius, c 1770

UIS5080760

Tufa from Mount Vesuvius, c 1770

Tufa from Mount Vesuvius, c 1770

UIS5080759

Earth - The geoid - Earth's geoid - The Earth's geoid, an image of the inegalites of the Earth's gravitation field. Image centered on the Atlantic Ocean. Image obtained by the GOCE satellite in 2011. ESA's GOCE mission has delivered the most accurate model of the 'geoid' ever produced, which will be used to further our understanding of how Earth works. A precise model of Earth's geoid is crucial for deriving accurate measurements of ocean circulation, sea - level change and terrestrial ice dynamics. The geoid is also used as a reference surface from which to map the topographical features on the planet. In addition, a better understanding of variations in the gravity field will lead to a deeper understanding of Earth's interior, such as the physics and dynamics associated with volcanic activity and earthquakes

Earth - The geoid - Earth's geoid - The Earth's geoid, an image of the inegalites of the Earth's gravitation field. Image centered on the Atlantic Ocean. Image obtained by the GOCE satellite in 2011. ESA's GOCE mission has delivered the most accurate model of the 'geoid' ever produced, which will be used to further our understanding of how Earth works. A precise model of Earth's geoid is crucial for deriving accurate measurements of ocean circulation, sea - level change and terrestrial ice dynamics. The geoid is also used as a reference surface from which to map the topographical features on the planet. In addition, a better understanding of variations in the gravity field will lead to a deeper understanding of Earth's interior, such as the physics and dynamics associated with volcanic activity and earthquakes

PIX4632044

Volcanoes: Piton de la Fournaise (Peak fo the Furnace) and Piton des Neiges, Reunion Island (photo)

Volcanoes: Piton de la Fournaise (Peak fo the Furnace) and Piton des Neiges, Reunion Island (photo)

Sergi Reboredo

SRB1202622

Auckland Region (New Zealand) satellite view - Auckland, New Zealand - Auckland Region, the largest urban area in New Zealand, in the North Island, viewed by Landsat satellite - 7 August 27, 2002. Auckland, New Zealand's largest city, is located on the country's North Island. Nearly a third of New Zealand's population lives in Auckland - - more than three million people. This natural - color (photo - like) image of Auckland was acquired on August 27, 2002, by Nasa's Landsat 7 satellite. The most densely developed areas appear white and gray, while suburban areas appear grayish green - - a mixture of houses, streets, and lawns. The city spreads out across various peninsulas surrounding Tamaki Strait and other bays and inlets. The city has been built up around the Auckland Volcanic Field; within a 20 - kilometer (12.4 - mile) radius of the heart of the city, there are 49 volcanoes, most of them small cones less than 150 meters (492 feet) high. Many of them have been protected as parks or

Auckland Region (New Zealand) satellite view - Auckland, New Zealand - Auckland Region, the largest urban area in New Zealand, in the North Island, viewed by Landsat satellite - 7 August 27, 2002. Auckland, New Zealand's largest city, is located on the country's North Island. Nearly a third of New Zealand's population lives in Auckland - - more than three million people. This natural - color (photo - like) image of Auckland was acquired on August 27, 2002, by Nasa's Landsat 7 satellite. The most densely developed areas appear white and gray, while suburban areas appear grayish green - - a mixture of houses, streets, and lawns. The city spreads out across various peninsulas surrounding Tamaki Strait and other bays and inlets. The city has been built up around the Auckland Volcanic Field; within a 20 - kilometer (12.4 - mile) radius of the heart of the city, there are 49 volcanoes, most of them small cones less than 150 meters (492 feet) high. Many of them have been protected as parks or

PIX4675653

Global view of the surface of Venus, 1982

Global view of the surface of Venus, 1982

UIS5072253

Noctis Labyrinthus landslides, Mars, c 2000

Noctis Labyrinthus landslides, Mars, c 2000

UIS5104169

Apollo 17: orange soil on the Moon - Apollo 17: the orange soil - View of orange soil, rich in zinc, probably of volcanic origin. Station 4, near the Shorty Crater. 12/12/1972. A view of the area at Station 4 (Shorty Crater) showing the now highly - publicized orange soil which the Apollo 17 crew members found on the moon during the second Apollo 17 extravehicular activity (EVA) at the Taurus - Littrow landing site. The tripod - like object is the gnomon and photometric chart assembly which is used as a photographic reference to establish local vertical sun angle, scale and lunar color. The gnomon is one of the Apollo lunar geology hand tools. While astronauts Eugene A. Cernan, commander, and Harrison H. Schmitt, lunar module pilot, descended in the Lunar Module (LM) “” Challenger”” to explore the Taurus - Littrow region of the moon, astronaut Ronald E. Evans, command module pilot, remained with the Command and Service Modules (CSM) “” America”” in lunar orbit. Schmitt was the crew man

Apollo 17: orange soil on the Moon - Apollo 17: the orange soil - View of orange soil, rich in zinc, probably of volcanic origin. Station 4, near the Shorty Crater. 12/12/1972. A view of the area at Station 4 (Shorty Crater) showing the now highly - publicized orange soil which the Apollo 17 crew members found on the moon during the second Apollo 17 extravehicular activity (EVA) at the Taurus - Littrow landing site. The tripod - like object is the gnomon and photometric chart assembly which is used as a photographic reference to establish local vertical sun angle, scale and lunar color. The gnomon is one of the Apollo lunar geology hand tools. While astronauts Eugene A. Cernan, commander, and Harrison H. Schmitt, lunar module pilot, descended in the Lunar Module (LM) “” Challenger”” to explore the Taurus - Littrow region of the moon, astronaut Ronald E. Evans, command module pilot, remained with the Command and Service Modules (CSM) “” America”” in lunar orbit. Schmitt was the crew man

PIX4598153

Leda Planitia is a plain located in the northern hemisphere of Venus. On this radar image obtained by the Magellan probe in 1991 appear in clear clear old terrain, fractures. The 40 km diameter Heloise impact crater is visible at the bottom of the picture - This false color Magellan image shows a portion of Leda Planitia (plains) in the northern hemisphere of Venus, centered at 41 degrees north latitude, 52 degrees east longitude. The area is 220 kilometers (135 miles) wide and 275 kilometers (170 miles) long. This image was produced from Magellan radar data collected in Cycle 2 of the mission. Cycle 2 was completed January 15, 1992. This image contains examples of several of the major geologic terrains on Venus and illustrates the basic stratigraphy or sequence of geologic events. The oldest terrains appear as bright, high-fractured or chaotic highlands rising out of the plains. This is seen in the upper left, or northwest, quadrant of the image. The chaotic highlands, sometimes calle

Leda Planitia is a plain located in the northern hemisphere of Venus. On this radar image obtained by the Magellan probe in 1991 appear in clear clear old terrain, fractures. The 40 km diameter Heloise impact crater is visible at the bottom of the picture - This false color Magellan image shows a portion of Leda Planitia (plains) in the northern hemisphere of Venus, centered at 41 degrees north latitude, 52 degrees east longitude. The area is 220 kilometers (135 miles) wide and 275 kilometers (170 miles) long. This image was produced from Magellan radar data collected in Cycle 2 of the mission. Cycle 2 was completed January 15, 1992. This image contains examples of several of the major geologic terrains on Venus and illustrates the basic stratigraphy or sequence of geologic events. The oldest terrains appear as bright, high-fractured or chaotic highlands rising out of the plains. This is seen in the upper left, or northwest, quadrant of the image. The chaotic highlands, sometimes calle

PIX4635230

Italy, Pozzuoli, Solfatara crater, ruin of former observatory in middle of steaming crater

Italy, Pozzuoli, Solfatara crater, ruin of former observatory in middle of steaming crater

UDK5432311

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