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Summary

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Description

Pāhoehoe Lava flows in the open lava channel (not in a Lava tube) with overflows at both sides. The image was taken at The Big Island of Hawaii. The lava flow is due to July 21, 2007 fissure eruption at Kīlauea volcano.The channel is crusting over with a v-shaped opening pointing upstream. The crusting-over process usually starts at the upstream end, the crust grows downstream for a considerable distance, then the crust founders and sinks opening the channel to crusting over again. The main channel and overflows show perched nature of this kind of lava channels. The picture was taken from a helicopter. The link to the map of the flow by USGS.

Source

self-made

Date

09/10/07

Author

Mila Zinkova edited by -- mikaul talk 23:10, 7 November 2007 (UTC)

Permission
( Reusing this file)
I, the copyright holder of this work, hereby publish it under the following licenses:
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File history

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Date/TimeThumbnailDimensionsUserComment
current 23:10, 7 November 2007 Thumbnail for version as of 23:10, 7 November 20071,600 × 1,067 (2.07 MB) MIckStephenson ( talk | contribs)== Summary == {{Information |Description=[http://en.wikipedia.org/wiki/Lava#P.C4.81hoehoe Pāhoehoe Lava] flows in the open lava channel (not in a Lava tube) with overflows at both sides. The image was taken at [http://en.wikipedia.org/wiki/Hawaii
No pages on the English Wikipedia use this file (pages on other projects are not listed).

Metadata

From Wikipedia, the free encyclopedia

Original file(1,600 × 1,067 pixels, file size: 2.07 MB, MIME type: image/jpeg)

Summary

File information
Description

Pāhoehoe Lava flows in the open lava channel (not in a Lava tube) with overflows at both sides. The image was taken at The Big Island of Hawaii. The lava flow is due to July 21, 2007 fissure eruption at Kīlauea volcano.The channel is crusting over with a v-shaped opening pointing upstream. The crusting-over process usually starts at the upstream end, the crust grows downstream for a considerable distance, then the crust founders and sinks opening the channel to crusting over again. The main channel and overflows show perched nature of this kind of lava channels. The picture was taken from a helicopter. The link to the map of the flow by USGS.

Source

self-made

Date

09/10/07

Author

Mila Zinkova edited by -- mikaul talk 23:10, 7 November 2007 (UTC)

Permission
( Reusing this file)
I, the copyright holder of this work, hereby publish it under the following licenses:
You may select the license of your choice.


Licensing

I, the copyright holder of this work, hereby publish it under the following licenses:
You may select the license of your choice.

File history

Click on a date/time to view the file as it appeared at that time.

Date/TimeThumbnailDimensionsUserComment
current 23:10, 7 November 2007 Thumbnail for version as of 23:10, 7 November 20071,600 × 1,067 (2.07 MB) MIckStephenson ( talk | contribs)== Summary == {{Information |Description=[http://en.wikipedia.org/wiki/Lava#P.C4.81hoehoe Pāhoehoe Lava] flows in the open lava channel (not in a Lava tube) with overflows at both sides. The image was taken at [http://en.wikipedia.org/wiki/Hawaii
No pages on the English Wikipedia use this file (pages on other projects are not listed).

Metadata


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