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Volcano Watch

Volcano Watch is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates. 

Filter Total Items: 1760
Volcano Watch — Deciphering explosive behavior at Mauna Loa

Volcano Watch — Deciphering explosive behavior at Mauna Loa

Mauna Loa is known for its effusive eruptions that produce spectacular lava flows. However, some of the volcanic products found on Mauna Loa are...

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Volcano Watch — HVO erupts with gratitude for University of Hawaiʻi partners

Volcano Watch — HVO erupts with gratitude for University of Hawaiʻi partners

Thanks to late Hawaii Senator Daniel Inouye, the University of Hawaiʻi at Hilo (UHH), and the Center for the Study of Active Volcanoes (CSAV), a...

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Volcano Watch — The legacy of Alexander Lancaster

Volcano Watch — The legacy of Alexander Lancaster

Known to many as “Pele’s Grandson,” Alexander (“Alex” or “Alec”) Lancaster guided both tourists and scientists to Hawai‘i’s volcanoes for over forty...

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Volcano Watch — Should old eruptions be forgot? Increase your volcano awareness this January

Volcano Watch — Should old eruptions be forgot? Increase your volcano awareness this January

We traditionally spend the New Year singing “Auld Lang Syne,” a song that reminisces about times long past. For the first month of the New Year, staff...

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Volcano Watch — Infrared (IR) measurements help HVO scientists unravel Kīlauea’s gas chemistry

Volcano Watch — Infrared (IR) measurements help HVO scientists unravel Kīlauea’s gas chemistry

Most people in Hawai‘i know about sulfur dioxide (SO2) gas, the major component of vog.  But, have you ever found yourself wanting to know the SO2/HCl...

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Volcano Watch — HVO’s ongoing recovery from the 2018 Kīlauea eruption

Volcano Watch — HVO’s ongoing recovery from the 2018 Kīlauea eruption

Communities on the Island of Hawai‘i continue to recover from Kīlauea’s 2018 lower East Rift Zone eruption and summit collapse as does the USGS...

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Volcano Watch — HVO innovation, 3D application

Volcano Watch — HVO innovation, 3D application

The electronics workshop at the USGS Hawaiian Volcano Observatory (HVO) buzzes with creative activity. 

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Volcano Watch — A cloud of ten thousand points: terrestrial laser scanning of Halemaʻumaʻu

Volcano Watch — A cloud of ten thousand points: terrestrial laser scanning of Halemaʻumaʻu

Scientists at the USGS Hawaiian Volcano Observatory (HVO) largely rely on aerial data collection for making maps of ongoing eruptions at Kīlauea. Most...

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Volcano Watch — The refilling of Halemaʻumaʻu crater

Volcano Watch — The refilling of Halemaʻumaʻu crater

Halemaʻumaʻu crater has undergone repeated changes during the past two centuries. Prior to 1924, the size and shape of the Halemaʻumaʻu lava lake...

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Volcano Watch — 30 years of Volcano Watch

Volcano Watch — 30 years of Volcano Watch

It’s hard to believe that the “Volcano Watch” weekly article and volcano activity update started 30 years ago. On November 3, 1991, the USGS Hawaiian...

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Volcano Watch — Tracking magma movement using olivine crystal “clocks”

Volcano Watch — Tracking magma movement using olivine crystal “clocks”

Olivine crystals—the beautiful green mineral common in Hawaiian lavas—record when and where magmas move inside Hawaiian volcanoes before they erupt...

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Volcano Watch — Pavlof: a volcano without typical signs of unrest?

Volcano Watch — Pavlof: a volcano without typical signs of unrest?

Volcanoes commonly give us clues that they are going to erupt. Before an eruption, gas, magma, and other fluids move below the surface of a volcano...

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Volcano Watch — How high is that lava fountain?

Volcano Watch — How high is that lava fountain?

The rapid onset of the current summit eruption sent USGS Hawaiian Volcano Observatory field crews running to grab their gear and head for the rim of...

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Volcano Watch — The Canary Islands “mega-tsunami” hypothesis, and why it doesn’t carry water

Volcano Watch — The Canary Islands “mega-tsunami” hypothesis, and why it doesn’t carry water

The recent eruption on La Palma, in the Canary Islands, has stimulated speculation that the volcano might collapse, creating a tsunami that would...

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Volcano Watch — Large Earthquake reminds us to “Drop, Cover, and Hold On”

Volcano Watch — Large Earthquake reminds us to “Drop, Cover, and Hold On”

The magnitude-6.2 earthquake that occurred on Sunday, October 10 at 11:49 a.m. HST, originated just south of the Island of Hawai‘i. The large...

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Volcano Watch — What’s that rising from the lava lake?

Volcano Watch — What’s that rising from the lava lake?

The past year has seen fluctuating lava lakes, ephemeral lava fountains, craggy spires, and drifting “islands” reminiscent of pre-1924 Halemaʻumaʻu...

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Volcano Watch — A new eruption in Halemaʻumaʻu

Volcano Watch — A new eruption in Halemaʻumaʻu

Kīlauea volcano is erupting again. Wednesday afternoon, lava returned to Kīlauea's summit within Hawaiʻi Volcanoes National Park after a 4-month...

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Volcano Watch — Observations and impacts of the 2017–2018 Ambae, Vanuatu eruption

Volcano Watch — Observations and impacts of the 2017–2018 Ambae, Vanuatu eruption

The Pacific is home to dozens of active volcanic systems including the massive Hawaiian shield volcanoes Kīlauea and Mauna Loa. Most basaltic shield...

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Volcano Watch — How does HVO determine which regions are most threatened by lava flows?

Volcano Watch — How does HVO determine which regions are most threatened by lava flows?

Most residents of the Island of Hawaiʻi live on one of four potentially active volcanoes and probably have wondered about the threat of lava flows at...

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Volcano Watch — The MILEAGE project - Mapping Kīlauea’s Gas Emissions

Volcano Watch — The MILEAGE project - Mapping Kīlauea’s Gas Emissions

Large quantities of volcanic gases, such as carbon dioxide (CO2), sulfur dioxide (SO2), and hydrogen sulfide (H2S), are released into the atmosphere...

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Volcano Watch — Eruption? Intrusion? What’s the difference?

Volcano Watch — Eruption? Intrusion? What’s the difference?

We know that when a volcano erupts, molten red rock makes it to the surface, while during an intrusion it doesn’t. The difference between the two...

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