{"id":136269,"date":"2021-02-28T09:00:43","date_gmt":"2021-02-28T19:00:43","guid":{"rendered":"https:\/\/www.hawaii.edu\/news\/?p=136269"},"modified":"2021-02-26T15:50:46","modified_gmt":"2021-02-27T01:50:46","slug":"lava-zones-attract-development","status":"publish","type":"post","link":"https:\/\/www.hawaii.edu\/news\/2021\/02\/28\/lava-zones-attract-development\/","title":{"rendered":"High-risk lava zones with infrequent eruptions attract development"},"content":{"rendered":"Reading time: <\/span> 2<\/span> minutes<\/span><\/span>
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Fissure 8 erupts in lava hazard zone 1, May 5, 2018. (Photo credit: Bruce Houghton)<\/figcaption><\/figure>\n

The unprecedented cost of the 2018 Kiīlauea eruption in Hawaiʻi<\/span> reflects the intersection of distinct physical and social phenomena: infrequent, highly destructive eruptions and atypically high population growth, according to a new study published in Nature Communications<\/em><\/a> and led by University of Hawaiʻi<\/span> at Mānoa researchers.<\/p>\n

It has long been recognized that areas in Puna, Hawaiʻi,<\/span> are at high risk from lava flows. In fact, Puna lies within the three highest-risk lava hazard zones (1, 2 and 3). This ensured that land values were lower, which actively promoted rapid population growth.<\/p>\n