Claire Horwell

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Claire Judith Horwell
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Alma mater University of Bristol (PhD)
Victoria University of Wellington (Dip. App. Sci. Volcanol.)
University of East Anglia (BSc Hons.)
Known forGeohealth
Volcanology
Health protection
Crystalline silica toxicity
Air pollution
Disaster risk reduction
Scientific career
Institutions Durham University
University of Cambridge (NERC Fellow)
University of Bristol (Leverhulme Trust Researcher)
Doctoral advisor Robert Stephen John Sparks
Website https://www.durham.ac.uk/staff/claire-horwell/

Claire Judith Horwell is a professor of Geohealth in the Department of Earth Sciences and Institute of Hazard, Risk and Resilience at Durham University and the founding Director of the International Volcanic Health Hazard Network (IVHHN). She studies the health hazards of natural and industrial mineral dusts and community protection.

Contents

Early life and education

Horwell became interested in volcanoes as a child [1] when she visited Mount Batur in Bali at the age of seven. Her undergraduate degree was in Environmental Science at the University of East Anglia, UK, where she studied environmental, earth and public health sciences. [1] She moved to Victoria University of Wellington for her master's degree (Diploma in Applied Science), and studied volcanology. [1] Her research at Victoria University was based in Rotorua, an urban area where 60,000 people are exposed to geothermal emissions. [1] Horwell designed passive samplers to simultaneously measure gas emissions around the town, collecting information on hydrogen sulphide exposures and providing advice to public health experts. [1] She earned her doctorate at the University of Bristol, where she worked with Robert Stephen John Sparks supported by the Natural Environment Research Council. [2] Her PhD research focused on the characteristics of crystalline silica in volcanic ash which control its toxicity. [3] [4]

Research and career

In 2003, Horwell founded the International Volcanic Health Hazard Network through a Leverhulme Trust network grant. IVHHN provides information on the health hazards and impacts of volcanic emissions to the general public and civil protection agencies, and helps governments prepare for the health response to volcanic eruptions. [5] [6] She has remained the director of the IVHHN, and has since co-created the Hawaii Interagency Vog dashboard to provide information about volcanic smog to the general public. [1] [7] In 2005, Horwell joined the University of Cambridge as a NERC postdoctoral fellow. [8] She moved to Durham University in 2007 as a Research Councils UK research fellow where she is now Professor. [8] [9]

Horwell has served as an advisor to the World Health Organization, UK Cabinet Office and Public Health England. [10] She was appointed to the Government of the United Kingdom Scientific Advisory Group for Emergencies for volcanic eruptions in 2015. [11] She was President (and, formerly, President-elect) and founding leader of the American Geophysical Union's GeoHealth Section and served on AGU's Council (2017-2020). She has held an honorary position at the UK Health Security Agency (formerly Public Health England/Health Protection Agency) since 2014.

Horwell studies the health hazards of mineral dusts, and ways to support communities to protect themselves from inhaling particulate air pollution. She uses physicochemical analysis to establish whether or not, and how, mineral particles are harmful, as well as toxicological assessments to determine the respiratory hazards. These help her to understand the structure-toxicity relationships of minerals. She has studied how crystalline silica forms in volcanic systems such as lava domes using petrological techniques. [1] Crystalline silica can be a pathogen, and can result in silicosis and lung cancer. Horwell is trying to establish whether the silica in volcanic ash has the potential to cause these diseases. [1] [12] Horwell worked with authorities in Hawaii to help local communities respond to the Kīlauea vog (volcanic smog) emissions. The Interagency Vog Dashboard website was accessed over 50,000/week during the 2018 lower Puna eruption. [13] [14]

She has worked with the Pan American Health Organization to introduce new epidemiological protocols for use in volcanic crises and has supported many governmental agencies and non-governmental organizations in Indonesia, New Zealand, Singapore, Japan, St Vincent and Mexico in preparing for, and responding to, community exposures to volcanic emissions.

She created the Health Interventions in Volcanic Eruptions (HIVE) Consortium project (funded by ELRHA) to collect evidence on respiratory protection for communities. [15] She investigated the effectiveness of facemasks distributed by agencies during volcanic eruptions, looking to identify whether or not they could adequately filter fine-grained particles, as well as to understand the behavioural reasons why some communities may or may not wear masks, through collaborations with a range of social scientists. During this program Horwell co-developed train-the-trainer courses with the International Society for Respiratory Protection to teach people in Indonesia how to better protect themselves. Her research, with the Institute of Occupational Medicine, confirmed that N95 industry certified masks are most effective at protecting communities from inhaling volcanic ash, and that the more commonly used surgical masks offered less protection. [16] A summary of the project was published as a Supplement of the Pan American Health Organization's Disasters bulletin [17] which is distributed globally to more than 25,000 people.

During the COVID-19 pandemic, Horwell has published media articles on the ethics and use of respiratory protection by the public. [18] [19]

Awards and honours

Her recent awards and honours include;

Selected publications

Horwell has published more than 60 papers and several book chapters across disciplines including volcanology, petrology, behavioural science, social anthropology, toxicology, exposure science, public health and epidemiology, law and ethics. A full list of publications can be found at: https://www.durham.ac.uk/staff/claire-horwell/. Her publications include:

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">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">Popocatépetl</span> Stratovolcano in Puebla, Mexico

Popocatépetl is an active stratovolcano located in the states of Puebla, Morelos, and Mexico in central Mexico. It lies in the eastern half of the Trans-Mexican volcanic belt. At 5,393 m (17,694 ft) it is the second highest peak in Mexico, after Citlaltépetl at 5,636 m (18,491 ft).

<span class="mw-page-title-main">Stratovolcano</span> Type of conical volcano composed of layers of lava and tephra

A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high to intermediate levels of silica, with lesser amounts of less viscous mafic magma. Extensive felsic lava flows are uncommon, but have traveled as far as 15 km (9 mi).

<span class="mw-page-title-main">Volcanologist</span> Scientist who studies volcanoes

A volcanologist, or volcano scientist, is a geologist who focuses on understanding the formation and eruptive activity of volcanoes. Volcanologists frequently visit volcanoes, sometimes active ones, to observe and monitor volcanic eruptions, collect eruptive products including tephra, rock and lava samples. One major focus of inquiry in recent times is the prediction of eruptions to alleviate the impact on surrounding populations and monitor natural hazards associated with volcanic activity. Geologists who research volcanic materials that make up the solid Earth are referred to as igneous petrologists.

Pneumono­ultra­micro­scopic­silico­volcano­coniosis is a 45-letter made-up word coined in 1935 by the then president of the National Puzzlers' League, Everett M. Smith. It has sometimes been used as a synonym for the occupational disease known as silicosis, but it should not be as most silicosis is not related to mining of volcanic dusts. It is the longest word in the English language published in a popular dictionary, Oxford Dictionaries, which defines it as "an artificial long word said to mean a lung disease caused by inhaling very fine ash and sand dust".

<span class="mw-page-title-main">Vog</span> Air pollution resulting from volcanic gases reacting with the atmosphere

Vog is a form of air pollution that results when sulfur dioxide and other gases and particles emitted by an erupting volcano react with oxygen and moisture in the presence of sunlight. The word is a portmanteau of the words "volcanic" and "smog". The term is in common use in the Hawaiian islands, where the Kīlauea volcano, on the Island of Hawaiʻi (the "Big Island"), erupted continuously between 1983 and 2018. Based on June 2008 measurements, Kīlauea emits 2,000–4,000 tons of sulfur dioxide (SO2) every day.

<span class="mw-page-title-main">Mayor Island / Tūhua</span> New Zealand shield volcano

Mayor Island / Tūhua is a dormant shield volcano located off the Bay of Plenty coast of New Zealand's North Island. It lies 35 kilometres (22 mi) north of Tauranga and covers 13 km2 (5 sq mi).

<span class="mw-page-title-main">Anak Krakatoa</span> Volcanic island in the Sunda Strait

Anak Krakatoa is a volcanic island in Indonesia. On 29 December 1927, Anak Krakatoa first emerged from the caldera formed in 1883 by the explosive volcanic eruption that destroyed the island of Krakatoa. There has been sporadic eruptive activity at the site since the late 20th century, culminating with a large underwater collapse of the volcano that caused a deadly tsunami in December 2018. There has been subsequent activity since. Due to its young age, the island is one of several in the area that are of interest to, and the subject of extensive study by, volcanologists.

<span class="mw-page-title-main">La Garita Caldera</span> Large caldera in the state of Colorado, U.S.

La Garita Caldera is a large caldera in the San Juan volcanic field in the San Juan Mountains around the town of Creede in southwestern Colorado, United States. It is west of La Garita, Colorado. The eruption that created the La Garita Caldera is among the largest known volcanic eruptions in Earth's history, as well as being one of the most powerful known supervolcanic events.

<span class="mw-page-title-main">Mount Meager massif</span> Group of volcanoes in British Columbia, Canada

The Mount Meager massif is a group of volcanic peaks in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. Part of the Cascade Volcanic Arc of western North America, it is located 150 km (93 mi) north of Vancouver at the northern end of the Pemberton Valley and reaches a maximum elevation of 2,680 m (8,790 ft). The massif is capped by several eroded volcanic edifices, including lava domes, volcanic plugs and overlapping piles of lava flows; these form at least six major summits including Mount Meager which is the second highest of the massif.

<span class="mw-page-title-main">Silverthrone Caldera</span> Caldera in British Columbia, Canada

The Silverthrone Caldera is a potentially active caldera complex in southwestern British Columbia, Canada, located over 350 kilometres (220 mi) northwest of the city of Vancouver and about 50 kilometres (31 mi) west of Mount Waddington in the Pacific Ranges of the Coast Mountains. The caldera is one of the largest of the few calderas in western Canada, measuring about 30 kilometres (19 mi) long (north-south) and 20 kilometres (12 mi) wide (east-west). Mount Silverthrone, an eroded lava dome on the caldera's northern flank that is 2,864 metres (9,396 ft) high, may be the highest volcano in Canada.

<span class="mw-page-title-main">Lava</span> Molten rock expelled by a volcano during an eruption

Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from 800 to 1,200 °C. The volcanic rock resulting from subsequent cooling is also often called lava.

<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 hazards</span>

A volcanic hazard is the probability a volcanic eruption or related geophysical event will occur in a given geographic area and within a specified window of time. The risk that can be associated with a volcanic hazard depends on the proximity and vulnerability of an asset or a population of people near to where a volcanic event might occur.

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.

<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">Sabancaya</span> Active stratovolcano in Southern Peru

Sabancaya is an active 5,976-metre-high (19,606 ft) stratovolcano in the Andes of southern Peru, about 70 kilometres (43 mi) northwest of Arequipa. It is considered part of the Central Volcanic Zone of the Andes, one of the three distinct volcanic belts of the Andes. The Central Volcanic Zone includes a number of volcanoes, some of which like Huaynaputina have had large eruptions and others such as Sabancaya and Ubinas have been active in historical time. Sabancaya forms a volcanic complex together with Hualca Hualca to the north and Ampato to the south and has erupted andesite and dacite. It is covered by a small ice cap which leads to a risk of lahars during eruptions.

Jenni Barclay is a professor of volcanology at the University of East Anglia. She works on ways to mitigate volcanic risks, the interactions between rainfall and volcanic activity and the communication of volcanic hazards in the Caribbean. Barclay leads the NERC-ESRC funded Strengthening Resilience to Volcanic Hazards (STREVA) research project as well as a Leverhulme Trust programme looking at the volcanic history of the Ascension Islands.

Susan Loughlin MBE is a British volcanologist. She was Director of the Montserrat Volcano Observatory from 2004-2006, and has been Head of Volcanology for the British Geological Survey since 2008.

References

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  2. "Dr. Claire Horwell". Earth Observatory of Singapore. Retrieved 2019-09-15.
  3. Bristol, University of. "2002: The hidden hazards of volcanoes | News | University of Bristol". www.bristol.ac.uk. Retrieved 2019-09-16.
  4. Editor, Our Health (2002-12-28). "Volcanic dust 'link to cancer'". The Times. ISSN   0140-0460 . Retrieved 2019-09-15.{{cite news}}: |last= has generic name (help)
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  12. Science, American Association for the Advancement of (2003-03-28). "News this Week". Science. 299 (5615): 251. ISSN   0036-8075.
  13. "Claire Horwell Wins Faculty of Science Inaugural Impact and Engagement Award - Durham University". www.dur.ac.uk. Retrieved 2019-09-15.
  14. Siegel, Ethan. "The USGS Hawaiian Volcano Observatory Is A Trusted Source For The Kilauea Eruption". Forbes. Retrieved 2020-05-13.
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  16. "Protecting Against Volcanic Ash". www.enn.com. Archived from the original on 2018-09-11. Retrieved 2019-09-15.
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  18. Horwell, Claire J.; McDonald, Fiona. "Coronavirus: why you need to wear a face mask in France, but not in the UK". The Conversation. Retrieved 2022-01-14.
  19. "Ministers know which masks provide the best Covid protection – why not tell the UK public? | Claire Horwell". The Guardian. 2021-12-30. Retrieved 2022-01-14.
  20. "EGU announces 2020 awards and medals". egu.eu. European Geosciences Union. October 22, 2019. Retrieved January 1, 2020.
  21. "Dr Claire Horwell appointed President-elect of new AGU GeoHealth Section - Durham University". www.dur.ac.uk. Retrieved 2019-09-15.