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178:.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
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366:share alike
360:attribution
324:1.0 Generic
320:2.0 Generic
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136:Description
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80:image/jpeg
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682:Lava tube
667:MGA73bot2
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157:Lava tube
145:English:
737:लावा नहर
661:(1.8 MB)
349:to remix
343:to share
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195:09/10/07
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641:Comment
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176:volcano
173:Kīlauea
169:fissure
128:Summary
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163:. The
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270:GFDL
192:Date
184:link
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
