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

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Participating in Earth Day (https://www.earthday.org/take-action-now/) can be as simple as remembering to turn off the light when you leave a room or as involved as advocating for legislative change. Many people use Earth Day as an opportunity to educate themselves on their own personal carbon footprint (https://www3.epa.gov/carbon-footprint-calculator/). 

But have you ever thought about how natural events influence environmental change? 

For example, you probably won’t see any thriving vegetation immediately following a volcanic eruption. Depending on the scale of the eruption, the surrounding flora and fauna have probably been devastated by some combination of ash, volcanic gas, lava, or lahars.  

The resulting landscape seems inhospitable at first, but over time the volcanic deposits break down and release nutrients on which plants thrive. On the windward and wet east side of the Island of Hawai‘i, the substantial rainfall drives faster rates of plant growth, meaning the region can go from a barren and young lava flow to a thriving rainforest in under 150 years! 

Volcanic influence isn’t limited to the nearby ground surface. Ash plumes from large explosive eruptions can temporarily block out the sun, turning the clearest day into the darkest night. The darkness can last from hours to days, or until most of the ash particles make their way back down to Earth’s surface. However, the smallest particles remain suspended high in the atmosphere, carried by wind currents for thousands of kilometers or miles.  

You can think of these particles as trillions of tiny mirrors reflecting solar radiation back into space. Sulfur dioxide, a volcanic gas, combines with water droplets in the atmosphere and blocks solar radiation in the same way.  

Large volcanic eruptions can block so much solar radiation in this way that they briefly impact the climate. The 1883 eruption of Krakatoa in Indonesia, one of the largest eruptions in recent history, plunged the region into total darkness for two and a half days and lowered global temperature for five years. An even larger eruption from Mount Tambora in 1815 resulted in “the year without summer” across Europe and North America. 

However, global cooling brought on by volcanic eruptions is only temporary and isn’t a solution to the current climate change crisis our planet is currently experiencing. 

Volcanoes also regularly emit greenhouse gases into the atmosphere, but it is unlikely that we would notice any significant rise in global temperatures due to a single volcanic eruption. For that, we’d have to look back millions of years to volcanic events like those that created the Siberian Traps.  

These were large-scale eruptions that spanned millions of years and spewed enormous amounts of lava across Siberia. The resulting lava flows are known as flood basalts. They are made up of numerous and extensive lava flows stacked on one another. Flood basalt flows are very fluid and travelled very far from their source vents. The Siberian Traps eruption caused the largest identified mass extinction event on Earth. Emissions of volcanic gases were a major contribution to the extinction event, but the magma also ignited huge underground coal deposits that released vast amounts of carbon dioxide (CO2) and other greenhouse gases. Sound familiar? 

Today, human activities annually produce more than 100 times the greenhouse gas emissions than global volcanism (https://www.usgs.gov/programs/VHP/volcanoes-can-affect-climate). In other words, Mount St. Helens would have to erupt over 3,500 times a year to match human CO2 emissions. So, do volcanoes influence our local environment and global climate? Absolutely! But we shouldn't blame them for or rely on them to solve our current climate woes.  

This Earth Day, April 22, whether you are admiring the eruption glow from Halema‘uma‘u at the summit of Kīlauea or just remembering to turn off the light when you leave a room, we hope you take a moment to appreciate planet Earth. 

Volcano Activity Updates

Kīlauea volcano is erupting. Its USGS Volcano Alert level is at WATCH (https://www.usgs.gov/natural-hazards/volcano-hazards/about-alert-levels). Kīlauea updates are issued daily.    

Over the past week, lava has continued to erupt from the western vent within Halemaʻumaʻu crater. All lava is confined within Halemaʻumaʻu crater in Hawai‘i Volcanoes National Park. Sulfur dioxide emission rates remain elevated and were last measured at approximately 1,700 tonnes per day (t/d) on April 20, 2022. Seismicity is elevated but stable, with few earthquakes and ongoing volcanic tremor. Summit tiltmeters show one minor deflation and inflation trend over the past week. For more information on the current eruption of Kīlauea, see https://www.usgs.gov/volcanoes/kilauea/recent-eruption.

Mauna Loa is not erupting and remains at Volcano Alert Level ADVISORY. This alert level does not mean that an eruption is imminent or that progression to an eruption from the current level of unrest is certain. Mauna Loa updates are issued weekly.     

This past week, about 77 small-magnitude earthquakes were recorded below the summit and upper elevation flanks of Mauna Loa—the majority of these occurred at shallow depths less than 15 kilometers (9 miles) below sea level. Global Positioning System (GPS) measurements show low rates of ground deformation over the past week. Gas concentrations and fumarole temperatures at both the summit and at Sulphur Cone on the Southwest Rift Zone have remained stable over the past week. Webcams show no changes to the landscape. For more information on current monitoring of Mauna Loa, see: https://www.usgs.gov/volcanoes/mauna-loa/monitoring.  

Nine earthquakes were reported felt in the Hawaiian Islands during the past week: a M3.5 earthquake 25 km (15 mi) E of Honaunau-Napoopoo at 0 km (0 mi) depth on April 19 at 8:32 p.m. HST, a M3.1 earthquake 9 km (5 mi) NW of Kukuihaele at 30 km (19 mi) depth on April 18 at 3:17 p.m. HST, a M2.3 earthquake 1 km (0 mi) SW of Pāhala at 34 km (21 mi) depth on April 15 at 1:27 p.m. HST, a M2.6 earthquake 8 km (4 mi) E of Pāhala at 33 km (20 mi) depth on April 15 at 7:38 a.m. HST, a M2.0 earthquake 8 km (4 mi) E of Pāhala at 33 km (20 mi) depth on April 15 at 7:00 a.m. HST, a M2.1 earthquake 10 km (6 mi) E of Pāhala at 32 km (20 mi) depth on April 15 at 2:28 a.m. HST, a M3.0 earthquake 9 km (5 mi) ENE of Pāhala at 32 km (20 mi) depth on April 15 at 2:11 a.m. HST, a M4.6 earthquake 9 km (5 mi) E of Pāhala at 31 km (19 mi) depth on April 15 at 1:58 a.m. HST, a M4.3 earthquake 8 km (4 mi) ENE of Pāhala at 34 km (21 mi) depth on April 15 at 1:58 a.m. HST.

HVO continues to closely monitor Kīlauea’s ongoing eruption and Mauna Loa for any signs of increased activity.    

Please visit HVO’s website for past Volcano Watch articles, Kīlauea and Mauna Loa updates, volcano photos, maps, recent earthquake info, and more. Email questions to askHVO@usgs.gov.    

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