'Basaltic Lava' images and/or videos results

P?hoehoe lava flow

UIG3524542

basalt structure Staffa

Graham Salter

SLR3829495

Fingal's cave,basalt structure

Graham Salter

SLR3829461

Fingal's cave,basalt structure

Graham Salter

SLR3829748

Extinct Volcanos of Central France (engraving)

English School, (19th century)

LIP1609511

Fingal's cave,basalt structure

Graham Salter

SLR3829746

Lava flow on the volcano Kilauea -Hawaii - Lava flow on Kilauea volcano -Hawaii - A flow of lava Pahoehoe, a type of fluid basaltic lava characteristic of the volcano Shield Kilauea a Hawaii. Pahoehoe (fluid and smooth basaltic lava) flow on the shield volcano Kilauea, in Hawaii

Martin Rietze

PIX4677307

Martin Rietze

PIX4677293

Lava flow on the volcano Kilauea -Hawaii - Lava flow on Kilauea volcano -Hawaii - Cooling of a lava flow Pahoehoe, a type of basaltic lava fluid characteristic of the volcano Shield Kilauea a Hawaii. Cooling Pahoehoe (fluid and smooth basaltic lava) flow on the shield volcano Kilauea, in Hawaii

Martin Rietze

PIX4677306

Volcano Erta-Ale In 3D, Ethiopia, True Colour Satellite Image

UIG601950

Lava entry into the OCEAN-kilauea -Hawaii - Lava sea Entry-kilauea -Hawaii - Lava flow into the Pacific Ocean. It is a type of fluid basaltic lava characteristic of the volcano shield Kilauea to Hawaii. Pahoehoe (fluid and smooth basaltic lava) sea entry from the shield volcano Kilauea, in Hawaii

Martin Rietze

PIX4677276

Lava entry into the OCEAN-kilauea -Hawaii - Lava sea Entry-kilauea -Hawaii - Entering a flow of Pahoehoe lava into the Pacific Ocean. It is a type of fluid basaltic lava characteristic of the volcano shield Kilauea to Hawaii. Pahoehoe (fluid and smooth basaltic lava) sea entry from the shield volcano Kilauea, in Hawaii

Martin Rietze

PIX4677290

Martin Rietze

PIX4677264

Lava flow on Kilauea volcano - Hawaii - Lava flow on Kilauea volcano - Hawaii - A flow of Pahoehoe lava ignites vegetation. It is a type of fluid basaltic lava characteristic of the volcano shield Kilauea to Hawaii. Pahoehoe (fluid and smooth basaltic lava) flow with burning ferns on the shield volcano Kilauea, in Hawaii

Martin Rietze

PIX4677295

Basaltic lava flows, Volcanic organs of Jaujac, Ardeche, France (photo)

Sebastien Beaucourt

SBE5917699

Basaltic lava flows, Volcanic organs of Jaujac, Ardeche, France (photo)

Sebastien Beaucourt

SBE5917700

Basaltic lava flows, Volcanic organs of Jaujac, Ardeche, France (photo)

Sebastien Beaucourt

SBE5917701

Basaltic lava flows, Volcanic organs of Jaujac, Ardeche, France (photo)

Sebastien Beaucourt

SBE5917702

NE of Lanzarote Island: “Jameos del Agua””, vast basaltic cave and swimming pool in lava: design Cesar Manrique in 1966

Herve Gyssels

GYS4718616

Sinus Iridum, c 2005-2006

UIS5106120

Ol Doinyo Lengai - Volcano Ol Doinyo Lengai - Ol Doinyo Lengai Volcano is an active volcano located in Tanzania in the Great Rift Valley. Ol Doinyo Lengai is the only volcano in the world to emit carbonatite. Image obtained from the EO-1 satellite on 12 September 2009. Volcano Ol Doinyo Lengai is an active volcano located in Tanzania in the great rift valley. It is the only known volcano producing carbonatite. The lava of Ol Doinyo Lengai is extremely cool (500 - 600* C, compared to 1,160* C for typical basaltic lava) and relatively fluid. Ol Doinyo Lengai alternates between eruptions of liquid lava that form lava lakes and fountains (called effusive eruptions) and explosive eruptions that build large cinder and ash cones. The new cone and crater are clearly visible in the center of the image acquired by satellite EO-1 on September 12, 2009. The dark spot in the crater may be fresh lava erupted from a new volcanic vent. Gray ash covers the volcano and much of the surrounding landscape

PIX4659350

March: Promethei Planum - Mars: Promethei Planum - Promethei Planum is a region located near the southern pole of Mars. This region is seasonally covered with a thick layer of ice up to 3500 metres thick. On this image obtained by the Mars Express probe on September 22, 2005, an impact crater about 100 km wide and 800 metres deep is visible to the right (north). It is partially covered with ice. In the center of the image, structures formed by lava flows; on the left of the image, ice, which is an extension of the southern polar cap. Promethei Planum, an area seasonally covered with layer of ice more than 3500 m thick layer of ice in the martian south polar region, was the subject of the High Resolution Stereo Camera's focus on 22 September 2005 as Mars Express was in orbit above the Red Planet. Promethei Planum lies at approximately 76* south and 105* east. An approximately 100 km - large and 800 m - deep impact crater is visible in the northern part of the image. The crater's interio

PIX4616118

Fingal's Cave, Staffa

Graham Salter

SLR3829340

Fingal's Cave from above

Graham Salter

SLR3829632

Fingal's Cave, Staffa

Graham Salter

SLR3829659

Fingal's Cave, Staffa

Graham Salter

SLR3829467

Fingal's Cave, Staffa

Graham Salter

SLR3829744

Fingal's Cave, Staffa

Graham Salter

SLR3829580

Fingal's Cave, Staffa

Graham Salter

SLR3829421

Fingal's Cave, Staffa

Graham Salter

SLR3829232

March: Promethei Planum - Mars: Promethei Planum - Promethei Planum is a region located near the southern pole of Mars. This region is seasonally covered with a thick layer of ice up to 3500 metres thick. On this perspective image obtained by the Mars Express probe on September 22, 2005, an impact crater about 100 km wide and 800 metres deep is visible at the bottom of the image. It is partially covered with ice. On top, structures formed by lava flows; at the top of the picture, ice, which is an extension of the southern polar cap. Promethei Planum, an area seasonally covered with layer of ice more than 3500 m thick layer of ice in the martian south polar region, was the subject of the High Resolution Stereo Camera's focus on 22 September 2005 as Mars Express was in orbit above the Red Planet. Promethei Planum lies at approximately 76* south and 105* east. An approximately 100 km - large and 800 m - deep impact crater is visible in the bottom of the image. The crater's interior is par

PIX4616138

Fingal's Cave from above

Graham Salter

SLR3829360

Fingal's Cave from abov

Graham Salter

SLR3829628

Fingal's Cave from above

Graham Salter

SLR3829445

Fingal's Cave from above

Graham Salter

SLR3829660

Fingal's Cave from above

Graham Salter

SLR3829665

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 fl

PIX4616176

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