Maritime impacts of volcanic eruptions

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Satellite view of a pumice raft from an undersea eruption in Tonga Pumice-raft.jpg
Satellite view of a pumice raft from an undersea eruption in Tonga

Volcanic eruptions can have various impacts on maritime transportation. When a volcano erupts, large amounts of noxious gases, steam, rock, and ash are released into the atmosphere; fine ash can be transported thousands of miles from the volcano, while high concentrations of coarse particles fall out of the air near the volcano. [1] The high concentrations of hazardous toxic gases are localized in the immediate vicinity of the volcano.

Contents

Until more recently public focus has mainly been on effects on aviation effectsash, which can be undetectable, can cause an aircraft's engine to cut out with catastrophic potential. However, the July 2008 eruption of Okmok Volcano in Alaska triggered attention to the maritime effects. Employees at the National Weather Service Ocean Prediction Center's Ocean Applications Branch examined this event and partnered with the Alaska Volcano Observatory to compile information on the topic.

Ash can affect marine transportation in many ways:

  1. Volcanic ash can clog air intake filters in a matter of minutes, crippling airflow to vital machinery. Ash particles are very abrasive and, if they get into an engine's moving parts, can cause severe damage very quickly. [2]
  2. Water is the main component in volcanic eruptions; it is what makes them so explosive. Through chemical reactions, toxic gases that are released in eruptions can bond or adsorb to ashfall particles. As the particles land on skin, metal, or other exposed shipboard equipment, they can begin to corrode.
  3. Certain types of volcanic ash do not dissolve easily in water. Instead, they clump on the surface of the ocean in pumice rafts. These rafts can clog salt water intake strainers very quickly, which can result in overheating of shipboard machinery dependent on sea water service cooling.
  4. Heavy amounts of volcanic ash reduce visibility to less than ½ mi, which is a hazard to navigation. This, combined with the above three other main impacts make sailing in the vicinity of volcanic ash very dangerous for mariners. [3]

National Weather Service Ashfall Advisories

National Weather Service Instruction 10-311 will includes a new text guidance for the offshore and high seas text weather forecasts issued by the Ocean Prediction Center and Tropical Prediction Center's Tropical Analysis and Forecast Branch (TAFB).

Reported incidents

A few cases of ash impact on ships that have been documented are:

The 2008 Eruption of Chaitén Volcano in Chile prompted mass evacuations, in which the Chilean Navy participated. There are reports [4] that the Chilean Navy encountered pumice rafts which were sucked into the salt water service system of the ship's propulsion system. This clogged sea strainers and overheated the engines, almost making the ships unable to escape.

The NOAA Ship Miller Freeman reported light accumulations of volcanic ash during the 2008 Okmok eruption in Dutch Harbor, Alaska. Due to volcanic-ash clogged ventilation systems, the ship remained in port until the event subsided. [5]

In 1891 the Australian steam ship Catterthun reported steaming "for miles through masses of volcanic debris" after an eruption on the island of Sagir in the Indonesian archipelago. It was rumoured that all of the island's 12,000 inhabitants had perished in the eruption.

Related Research Articles

<span class="mw-page-title-main">Volcano</span> Rupture in a planets crust where material escapes

A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.

<span class="mw-page-title-main">Mount St. Helens</span> Volcano in Washington, U.S.

Mount St. Helens is an active stratovolcano located in Skamania County, Washington, in the Pacific Northwest region of the United States. It lies 52 miles (83 km) northeast of Portland, Oregon, and 98 miles (158 km) south of Seattle. Mount St. Helens takes its English name from that of the British diplomat Alleyne Fitzherbert, 1st Baron St Helens, a friend of explorer George Vancouver who surveyed the area in the late 18th century. The volcano is part of the Cascade Volcanic Arc, a segment of the Pacific Ring of Fire.

<span class="mw-page-title-main">Rhyolite</span> Igneous, volcanic rock, of felsic (silica-rich) composition

Rhyolite is the most silica-rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained groundmass. The mineral assemblage is predominantly quartz, sanidine, and plagioclase. It is the extrusive equivalent of granite.

<span class="mw-page-title-main">Ring of Fire</span> Region around the rim of the Pacific Ocean where many volcanic eruptions and earthquakes occur

The Ring of Fire is a tectonic belt of volcanoes and earthquakes.

<span class="mw-page-title-main">Pumice</span> Light colored highly vesicular volcanic rock

Pumice, called pumicite in its powdered or dust form, is a volcanic rock that consists of highly vesicular rough-textured volcanic glass, which may or may not contain crystals. It is typically light-colored. Scoria is another vesicular volcanic rock that differs from pumice in having larger vesicles, thicker vesicle walls, and being dark colored and denser.

<span class="mw-page-title-main">Valley of Ten Thousand Smokes</span> Valley within Katmai National Park and Preserve, Alaska, United States

The Valley of Ten Thousand Smokes is a valley within Katmai National Park and Preserve in Alaska which is filled with ash flow from the eruption of Novarupta on June 6–8, 1912. Following the eruption, thousands of fumaroles vented steam from the ash. Robert F. Griggs, who explored the volcano's aftermath for the National Geographic Society in 1916, gave the valley its name, saying that "the whole valley as far as the eye could reach was full of hundreds, no thousands—literally, tens of thousands—of smokes curling up from its fissured floor."

<span class="mw-page-title-main">Tephra</span> Fragmental material produced by a volcanic eruption

Tephra is fragmental material produced by a volcanic eruption regardless of composition, fragment size, or emplacement mechanism.

<span class="mw-page-title-main">Mount Redoubt</span> Volcanic cone in the United States

Redoubt Volcano, or Mount Redoubt, is an active stratovolcano in the largely volcanic Aleutian Range of the U.S. state of Alaska. Located at the head of the Chigmit Mountains subrange in Lake Clark National Park and Preserve, the mountain is just west of Cook Inlet, in the Kenai Peninsula Borough about 110 miles (180 km) southwest of Anchorage. At 10,197 feet (3,108 m), in just over 5 miles (8.0 km) Mount Redoubt attains 9,150 feet (2,790 m) of prominence over its surrounding terrain. It is the highest summit in the Aleutian Range. In 1976, Redoubt Volcano was designated as a National Natural Landmark by the National Park Service.

<span class="mw-page-title-main">Augustine Volcano</span> Stratovolcano in Alaska

Augustine Volcano is a stratovolcano in Alaska consisting of a central complex of summit lava domes and flows surrounded by an apron of pyroclastic, lahar, avalanche, and ash deposits. The volcano is frequently active, with major eruptions recorded in 1883, 1935, 1963–64, 1976, 1986, and 2006. Minor eruptive events were reported in 1812, 1885, 1908, 1944, and 1971. The large eruptions are characterized by an explosive onset followed by the quieter effusion of lava. It forms Augustine Island in southwestern Cook Inlet in the Kenai Peninsula Borough of southcentral coastal Alaska, 174 miles (280 km) southwest of Anchorage. Augustine Island has a land area of 32.4 square miles (83.9 km2), while West Island, just off Augustine's western shores, has 2 sq mi (5.2 km2). The irregular coastline of Augustine Island is due to the repeated catastrophic collapse of the summit dome, forming debris avalanches down the flanks and into Cook Inlet.

<span class="mw-page-title-main">Alaska Volcano Observatory</span> Research center in Alaska, United States

The Alaska Volcano Observatory (AVO) is a joint program of the United States Geological Survey (USGS), the Geophysical Institute of the University of Alaska Fairbanks (UAFGI), and the State of Alaska Division of Geological and Geophysical Surveys (ADGGS). AVO was formed in 1988, and uses federal, state, and university resources to monitor and study Alaska's volcanology, hazardous volcanoes, to predict and record eruptive activity, and to mitigate volcanic hazards to life and property. The Observatory website allows users to monitor active volcanoes, with seismographs and webcameras that update regularly. AVO now monitors more than 20 volcanoes in Cook Inlet, which is close to Alaskan population centers, and the Aleutian Arc due to the hazard that plumes of ash pose to aviation.

<span class="mw-page-title-main">Pumice raft</span> Floating mass of pumice in the ocean

A pumice raft is a floating raft of pumice created by some eruptions of submarine volcanoes or coastal subaerial volcanoes.

<span class="mw-page-title-main">Home Reef</span> Ephemeral island in the South Pacific

Home Reef is a volcanic island atop a submarine volcano in Tonga. It is located southwest of Vava'u, between the islands of Kao and Late along the Tofua volcanic arc. The island is ephemeral, and has been repeatedly built and eroded by successive eruptions in 1852, 1857, 1984, 2006, 2022, and 2023.

<span class="mw-page-title-main">Types of volcanic eruptions</span> Overview of different types of volcanic eruptions

Several types of volcanic eruptions—during which lava, tephra, and assorted gases are expelled from a volcanic vent or fissure—have been distinguished by volcanologists. These are often named after famous volcanoes where that type of behavior has been observed. Some volcanoes may exhibit only one characteristic type of eruption during a period of activity, while others may display an entire sequence of types all in one eruptive series.

<span class="mw-page-title-main">Chaitén</span> Town and Commune in Los Lagos, Chile

Chaitén is a Chilean town, commune and former capital of the Palena Province in Los Lagos Region. The town is north of the mouth of Yelcho River, on the east coast of the Gulf of Corcovado. The town is strategically close to the northern end of the Carretera Austral, where the highway goes inland. The Desertores Islands are part of the commune.

<span class="mw-page-title-main">Chaitén (volcano)</span> Active volcano in Palena Province, Los Lagos Region, Chile

Chaitén is a volcanic caldera 3 kilometres (2 mi) in diameter, 17 kilometres (11 mi) west of the elongated ice-capped Michinmahuida volcano and 10 kilometres (6 mi) northeast of the town of Chaitén, near the Gulf of Corcovado in southern Chile. The most recent eruptive phase of the volcano erupted on 2008. Originally, radiocarbon dating of older tephra from the volcano suggested that its last previous eruption was in 7420 BC ± 75 years. However, recent studies have found that the volcano is more active than thought. According to the Global Volcanism Program, its last eruption was in 2011.

<span class="mw-page-title-main">1883 eruption of Krakatoa</span> Catastrophic volcanic eruption

The 1883 eruption of Krakatoa in the Sunda Strait occurred from 20 May until 21 October 1883, peaking in the late morning hours of 27 August when over 70% of the island of Krakatoa and its surrounding archipelago were destroyed as it collapsed into a caldera.

<span class="mw-page-title-main">Mount Gareloi</span> Stratovolcano in the Aleutian Islands of Alaska, U.S.

Mount Gareloi, or Gareloi Volcano, is a stratovolcano in the Aleutian Islands of Alaska, United States, about 1,259 miles (2,026 km) from Anchorage. Gareloi is located on Gareloi Island, and comprises most of its land mass. The island also has two small glaciers which protrude to the northwest and southeast.

<span class="mw-page-title-main">Volcanic ash and aviation safety</span>

Plumes of volcanic ash near active volcanoes are a flight safety hazard, especially for night flights. Volcanic ash is hard and abrasive, and can quickly cause significant wear to propellers and turbocompressor blades, and scratch cockpit windows, impairing visibility. The ash contaminates fuel and water systems, can jam gears, and make engines flame out. Its particles have low melting points, so they melt in the engines' combustion chamber then the ceramic mass sticks to turbine blades, fuel nozzles, and combustors—which can lead to total engine failure. Ash can also contaminate the cabin and damage avionics.

<span class="mw-page-title-main">Volcanic ash</span> Natural material created during volcanic eruptions

Volcanic ash consists of fragments of rock, mineral crystals, and volcanic glass, produced during volcanic eruptions and measuring less than 2 mm (0.079 inches) in diameter. The term volcanic ash is also often loosely used to refer to all explosive eruption products, including particles larger than 2 mm. Volcanic ash is formed during explosive volcanic eruptions when dissolved gases in magma expand and escape violently into the atmosphere. The force of the gases shatters the magma and propels it into the atmosphere where it solidifies into fragments of volcanic rock and glass. Ash is also produced when magma comes into contact with water during phreatomagmatic eruptions, causing the water to explosively flash to steam leading to shattering of magma. Once in the air, ash is transported by wind up to thousands of kilometres away.

<span class="mw-page-title-main">Mount Okmok</span>

Mount Okmok is a volcano on eastern Umnak Island, in the central-eastern Aleutian Islands of Alaska. Part of the Aleutian Volcanic Arc, it was formed by the subduction of the oceanic Pacific Plate under the North American Plate. Okmok is a large shield volcano capped by a 10 kilometers (6.2 mi) wide caldera. The caldera contains numerous cinder cones, their lava flows, and a few lakes. Okmok erupts mainly basaltic lava, mostly from the cones within the caldera.

References

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  2. Church, John A.; White, Neil J.; Arblaster, Julie M. (November 2005). "Significant decadal-scale impact of volcanic eruptions on sea level and ocean heat content". Nature. 438 (7064): 74–77. Bibcode:2005Natur.438...74C. doi:10.1038/nature04237. ISSN   0028-0836. PMID   16267551. S2CID   4384262.
  3. "Ocean Prediction Center - Maritime Impacts of Volcanic Eruptions". Archived from the original on 2009-11-13. Retrieved 2009-10-27.
  4. Lara, Luis E. (January 2009). "The 2008 eruption of the Chaitén Volcano, Chile: a preliminary report". Andean Geology. 36 (1): 125–129. doi: 10.4067/S0718-71062009000100009 . ISSN   0718-7106.
  5. Durant, Adam J.; Villarosa, Gustavo; Rose, William I.; Delmelle, Pierre; Prata, Alfred J.; Viramonte, José G. (January 2012). "Long-range volcanic ash transport and fallout during the 2008 eruption of Chaitén volcano, Chile". Physics and Chemistry of the Earth, Parts A/B/C. 45–46: 50–64. Bibcode:2012PCE....45...50D. doi:10.1016/j.pce.2011.09.004. hdl: 11336/76260 .