Laze (geology)

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Laze plumes forming from pahoehoe lava flowing into the Pacific Ocean, Hawaii Pahoehoe lava meets Pacific.jpg
Laze plumes forming from pāhoehoe lava flowing into the Pacific Ocean, Hawaii

Laze is acid rain and air pollution arising from steam explosions and large plume clouds containing extremely acidic condensate (mainly hydrochloric acid), which occur when molten lava flows enter cold oceans. [1] [2] The term laze is a portmanteau of lava and haze.

Laze, created by the interaction of lava and cold seawater, differs from vog, which originates from volcanic vents. [3] [4]

The extremely high temperatures of lava flows 1,200 °C (2,200 °F) causes sea water to decompose into hydrogen and oxygen. The hydrogen combines with chloride ions dissolved in sea water, forming hydrogen chloride gas (hydrochloric acid). The rapidly rising plume of gas also carries with it fine particles of volcanic glass. [2] [5] The hydrochloric acid and other contaminants can precipitate out rapidly and the plume may become relatively safe a few hundred meters away, however, laze plumes have killed people who come in contact with them. [6] The USGS has reported that, in 2000, two people were killed by exposure to laze clouds. [7]

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Halemaʻumaʻu Pit crater located within the summit caldera of Kīlauea in Hawaii

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Lava Molten rock expelled by a volcano during an eruption

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Lava delta

Lava deltas, similar to river deltas, form wherever sufficient sub-aerial flows of lava enter standing bodies of water. The lava cools and breaks up as it encounters the water, with the resulting fragments filling in the adjacent seabed topography such that the flow can move further offshore sub-aerially. Lava deltas are generally associated with large-scale, effusive type basaltic volcanism.

Volcanic hazards

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The International Volcanic Health Hazard Network (IVHHN) is an organization that provides research and information on the health hazards and impacts of volcanic eruptions. IVHHN work covers a range of research areas including volcanology, toxicology, public health and exposure science, with the goal of determining the health impacts of volcanic emissions and how to protect exposed communities.

2018 lower Puna eruption

The 2018 lower Puna eruption was a volcanic event on the island of Hawaiʻi, on Kīlauea volcano's East Rift Zone that began on May 3, 2018. It is related to the larger eruption of Kīlauea that began on January 3, 1983, though some volcanologists and USGS scientists have discussed whether to classify it as a new eruption. Outbreaks of lava fountains up to 300 feet (90 m) high, lava flows, and volcanic gas in the Leilani Estates subdivision were preceded by earthquakes and ground deformation that created cracks in the roads.

References

  1. "Vog and Laze Seminar Abstracts" (PDF). Center for the Study of Active Volcanoes, University of Hawaii at Hilo. July 29, 1991. Archived from the original (PDF) on November 1, 2017.
  2. 1 2 Rice, Doyle (22 May 2018). "Lava, acid rain, vog, sulfur dioxide and now 'laze': New deadly threat emerges from Hawaii volcano". USA Today .
  3. Stokes, J.B. (July 29, 1991). "How Vog is made: A photographic perspective" (PDF). Vog and Laze Seminar. Center for the Study of Active Volcanoes, University of Hawaii at Hilo. Archived from the original (PDF) on November 1, 2017.
  4. "Fact Sheet, Volcanic Air Pollution--A Hazard in Hawai'i; Fact Sheet 169-97 Online Version 1.1". pubs.usgs.gov. USGS. June 2000.
  5. Lava entering ocean
  6. Hunter, Dana (22 May 2018). "The Lowdown on LAZE: Kilauea's Most Recent Hazard". Scientific American . Retrieved 24 May 2018.
  7. Kirkpatrick, Noel (May 22, 2018). "What is laze? This toxic volcanic mixture is nothing to be relaxed about". Mother Nature Network. Narrative Content Group. Retrieved May 22, 2018.