![]() |
| The journey: From vent to the sea. |
At the start
of the video, standing waves in the lava channel can be seen near the vent
exit. The channel appears crust-free from vent to the bend around Kapoho
Crater. A surface crust forms over the channel as it spreads out during its
approach to the ocean. The overflight along the ocean entry is from north to
south along the coastline. The ocean entry is active along the whole length -
approximately 1 mile. Small litoral explosions are occurring and there are
several plumes of laze.
