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439  Articles
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Lava flow surface morphologies are like pages of a book. If we are able to read the writing of that book, we can understand its content, and learn, act, and react accordingly. In the same way, if we understand lava surface morphology, recognise how it for... see more

Lava flow surface morphologies are like pages of a book. If we are able to read the writing of that book, we can understand its content, and learn, act, and react accordingly. In the same way, if we understand lava surface morphology, recognise how it for... see more

Lava flow surface morphologies are like pages of a book. If we are able to read the writing of that book, we can understand its content, and learn, act, and react accordingly. In the same way, if we understand lava surface morphology, recognise how it for... see more

In the southern and south-eastern sectors of Somma-Vesuvius volcano (Campania region, southern Italy), archaeological sites covered by the deposits of A.D. 79 Vesuvius eruption, and dating back to Protohistoric and Roman periods are characterized by the p... see more

The 2014-2015 eruption at Holuhraun has produced more than 1.5 km3 of basaltic magma and can beconsidered one of the major effusive events of the last two centuries in the world. During this eruptionthe MIROVA system (a volcanic hot-spot detection system ... see more

During basaltic eruptions, the average rate at which lava is erupted (effusion rate) is one of the most important factor controlling the evolution, growth and extent of the flow field. This has implication both for forecasting purposes as input parameter ... see more

The 2014-2015 eruption at Holuhraun has produced more than 1.5 km3 of basaltic magma and can beconsidered one of the major effusive events of the last two centuries in the world. During this eruptionthe MIROVA system (a volcanic hot-spot detection system ... see more

During basaltic eruptions, the average rate at which lava is erupted (effusion rate) is one of the most important factor controlling the evolution, growth and extent of the flow field. This has implication both for forecasting purposes as input parameter ... see more

The 2014-2015 eruption at Holuhraun has produced more than 1.5 km3 of basaltic magma and can beconsidered one of the major effusive events of the last two centuries in the world. During this eruptionthe MIROVA system (a volcanic hot-spot detection system ... see more

1 of 45 pages  |  10  records  |  more records»