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- Lava flow (9578 bytes)
11: ...erao]] of the eruption of [[Vesuvius]] which took place between [[May 14]] and [[June 4]] [[1737]]. I...
23: ...front advancing over pāhoehoe on the coastal plain of [[Kilauea|Kīlauea]] in [[Hawaii|Hawai...
29: ... texture of pāhoehoe flows varies widely, displaying all kinds of bizarre shapes often referred t...
44: ...iscosity increases as it cools. Hence, on a level plain, and at some distance from its source, the lav...
46: ...se, almost amounting to a shriek. The trees then plunge into the - Lava (9992 bytes)
11: ...erao]] of the eruption of [[Vesuvius]] which took place between [[May 14]] and [[June 4]] [[1737]]. I...
23: ...front advancing over pāhoehoe on the coastal plain of [[Kilauea|Kīlauea]] in [[Hawaii|Hawai...
29: ... texture of pāhoehoe flows varies widely, displaying all kinds of bizarre shapes often referred t...
44: ...iscosity increases as it cools. Hence, on a level plain, and at some distance from its source, the lav...
46: ...se, almost amounting to a shriek. The trees then plunge into the
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