Item talk:Q319569
From geokb
{
"DOI": {
"doi": "10.5066/p9scu4re",
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{
"name": "Matthew R Patrick",
"nameType": "Personal",
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"United States Geological Survey"
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{
"name": "Kevan P Kamibayashi",
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{
"name": "R. Lopaka Lee",
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"United States Geological Survey"
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"titles": [
{
"title": "Timelapse camera and webcam images of the fissure 8 lava flow during the 2018 lower East Rift Zone eruption of K\u012blauea volcano, Island of Hawai\u02bbi"
}
],
"publisher": "U.S. Geological Survey",
"container": {},
"publicationYear": 2024,
"subjects": [
{
"subject": "volcanology"
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"description": "\nThe 2018 lower East Rift Zone eruption of K\u012blauea volcano, Island of Hawai\u02bbi, was one of the most destructive effusive eruptions worldwide in the past century, destroying over 700 structures (Neal and others, 2019; Meredith and others, 2022).\u00a0 Between May and September\u00a02018, a total of 24 fissures opened, producing a lava flow field with an area of 36 km2.\u00a0 By the end of May, the eruption had focused at fissure 8, which produced the dominant lava flow of the eruption.\u00a0 This lava flow extended north from its vent in Leilani Estates and entered the ocean in Kapoho, reaching a total subaerial length of 13 km.\u00a0 This flow was active for about two months, from May 28 to August 4, followed by several weeks of weak vent activity at the fissure.\u00a0\n\u00a0\nWhile monitoring the fissure 8 flow and its hazards, staff from the U.S. Geological Survey\u2019s Hawaiian Volcano Observatory placed several small timelapse cameras near the flow margin to better track and understand the flow changes.\u00a0 This data release includes images collected by five timelapse cameras, consisting of two deployment locations.\u00a0 One deployment location was close to the vent, and imaged the proximal portion (also called the \u201cspillway\u201d) of the fissure 8 flow.\u00a0 The second deployment location was 10 km downflow, on high ground in an active quarry on the cinder cone from the 1960 eruption.\u00a0\n\u00a0\nThese cameras were all small trail cameras designed for hunters to track game animals, and were used due to their inexpensive cost and ease of deployment.\u00a0 However, the cameras would switch into a near-infrared mode at night that, due to the intense infrared radiation emitted by the lava flow, produced oversaturated images that had little use.\u00a0 We have included all of the images collected by the camera for completeness, while recognizing that the majority of nighttime images will not be useful.\u00a0 More recent deployments of timelapse cameras have remedied this problem and now use different models of timelapse cameras (such as the Reconyx Hyperfire 2 white flash camera) that do not go into infrared mode and have produced much better nighttime images.\u00a0\n\nWe also include images from a continuously operating webcam (PGcam) near the eruption site, which had images transmitted in real time every 5 minutes.\u00a0\n\u00a0\nThis data release accompanies DeSmither and Patrick (2024), which includes images from a timelapse camera pointed at the fissure 8 cone and lava fountain.\u00a0 It also accompanies Patrick and Anderson (2024), which includes images from timelapse cameras stationed at the summit of K\u012blauea during the 2018 collapse sequences that occurred while the lower East Rift Zone eruption ensued.\u00a0 Some of the data in the current data release were used in Patrick and others (2019a), with some of the data released previously in Patrick and others (2019b).\n\n\nReferences\n\nDeSmither L, Patrick M. 2024. Lava fountain heights and associated timelapse images during the 2018 lower East Rift Zone eruption of K\u012blauea volcano, Island of Hawai\u02bbi. U.S. Geological Survey data release, https://doi.org/10.5066/P9DSIP05.\n\u00a0\nMeredith ES, Jenkins SF, Hayes JL, Deligne NI, Lallamant D, Patrick M, Neal C. 2022. Damage assessment for the 2018 Lower East Rift Zone lava flows of K\u012blauea volcano, Hawai\u02bbi. Bulletin of Volcanology 84, 65. https://doi.org/10.1007/s00445-022-01568-2.\n\u00a0\nNeal CA, Brantley SR, Antolik L, Babb J, Burgess M, Calles K, Cappos M, Chang JC, Conway S, DeSmither L, Dotray P, Elias T, Fukunaga P, Fuke S, Johanson IA, Kamibayashi K, Kauahikaua J, Lee RL, Pekalib S, Miklius A, Million W, Moniz CJ, Nadeau PA, Okubo P, Parcheta C, Patrick MR, Shiro B, Swanson DA, Tollett W, Trusdell F, Younger EF, Zoeller MH, Montgomery-Brown EK, Anderson KR, Poland MP, Ball J, Bard J, Coombs M, Dietterich HR, Kern C, Thelen WA, Cervelli PF, Orr T, Houghton BF, Gansecki C, Hazlett R, Lundgren P, Diefenbach AK, Lerner AH, Waite G, Kelly P, Clor L, Werner C, Mulliken K, Fisher G. 2019. The 2018 rift eruption and summit collapse of K\u012blauea Volcano. Science, eaav7046. https://doi.org/10.1126/science.aav7046\u00a0\n\u00a0\nPatrick MR, Anderson KR. 2024. Timelapse camera images of caldera floor subsidence during the 2018 eruption of K\u012blauea Volcano, Island of Hawai`i. U.S. Geological Survey data release, https://doi.org/10.5066/P90263TJ.\n\u00a0\nPatrick MR, Dietterich HR, Lyons JJ, Diefenbach AK, Parcheta C, Anderson KR, Namiki A, Sumita I, Shiro B, Kauahikaua JP. 2019a. Cyclic lava effusion during the 2018 eruption of K\u012blauea Volcano. Science, https://doi.org/10.1126/science.aay9070\n\u00a0\nPatrick MR, Dietterich H, Lyons J, Diefenbach A, Parcheta C, Anderson K, Namiki A, Sumita I., Shiro B, Kauahikaua J. 2019b. Cyclic lava effusion during the 2018 eruption of K\u012blauea Volcano: data release: U.S. Geological Survey data release, https://doi.org/10.5066/P9PJZ17R.\n\n",
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"created": "2024-02-14T02:39:58Z",
"registered": "2024-02-14T02:39:58Z",
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"updated": "2024-02-14T02:40:11Z"
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