On Kilauea’s east rift zone, breakouts from the Peace Day tube remain active on the pali and on the coastal plain.
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Posted on 2:45 am, Friday, May 10, 2013.
On Kilauea’s east rift zone, breakouts from the Peace Day tube remain active on the pali and on the coastal plain.
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Posted on 12:27 am, Monday, May 6, 2013.
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Posted on 7:46 pm, Sunday, May 5, 2013.
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Posted on 11:47 pm, Thursday, April 25, 2013.
A lava lake within the Halema`uma`u Overlook vent produced nighttime glow that was visible from the Jaggar Museum overlook and via HVO’s Webcam during the past week.
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Posted on 10:30 pm, Monday, April 22, 2013.
ometimes a geologic study resembles a crime scene investigation (CSI), as seen on TV. You piece together information from eyewitnesses and compare it with your own detailed observations to arrive at an interpretation of what happened.
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Posted on 9:11 am, Monday, April 22, 2013.
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Posted on 7:55 pm, Thursday, April 11, 2013.
On Kilauea’s east rift zone, breakouts from the Peace Day tube remain active above the pali and on the coastal plain. Small ocean entries are active on both sides of the Hawai`i Volcanoes National Park boundary.
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Posted on 11:11 pm, Friday, April 5, 2013.
Petrology, the study of the origin, or genesis, of rocks, is an important aspect of our multi-faceted approach to monitoring the current eruptions of Kilauea Volcano.
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Posted on 10:53 pm, Friday, April 5, 2013.
A lava lake within the Halema`uma`u Overlook vent produced nighttime glow that was visible from the Jaggar Museum overlook and via HVO’s Webcam during the past week.
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Posted on 3:29 am, Friday, March 29, 2013.
On Kilauea’s east rift zone, breakouts from the Peace Day tube remain active above and at the base of the pali and on the coastal plain.
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Posted on 3:19 am, Friday, March 29, 2013.
Over the past six months, the pace of Kilauea’s 30-year-long ongoing eruption has quickened. This follows the quietest period—spanning most of 2012—of the eruption yet recorded.
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Posted on 11:58 pm, Thursday, March 21, 2013.
Kahaualeʻa Cone, shown here, has long been a small oasis in the midst of Puʻu ʻŌʻō lava. New lava from the active Kahaualeʻa flow has now surrounded the cone, which has also partly burned.
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