{"id":7350,"date":"2018-05-04T23:06:36","date_gmt":"2018-05-05T07:06:36","guid":{"rendered":"http:\/\/earthjay.com\/?p=7350"},"modified":"2024-05-04T22:14:00","modified_gmt":"2024-05-04T22:14:00","slug":"earthquake-volcanic-eruption-report-hawaii","status":"publish","type":"post","link":"https:\/\/earthjay.com\/?p=7350","title":{"rendered":"Earthquake-Volcanic Eruption Report: Hawai&#8217;i"},"content":{"rendered":"<p>My USGS Earthquake Notification Service email inbox has been going on overtime.<\/p>\n<p>There has been a swarm of earthquakes on the southeastern part of the big island, with USGS volcanologists hypothesizing about magma movement and suggesting that an eruption may be imminent. Here is a great place to <a href=\"https:\/\/volcanoes.usgs.gov\/volcanoes\/kilauea\/multimedia_maps.html\" rel=\"noopener\" target=\"_blank\">find official USGS updates on the volcanism in Hawaii<\/a> (including maps). I had been following this on social media.<\/p>\n<p>Here is a <a href=\"http:\/\/temblor.net\/earthquake-insights\/pele-the-hawaii-goddess-of-fire-lightening-wind-and-volcanoes-7004\/\" rel=\"noopener\" target=\"_blank\">temblor blogpost that I wrote<\/a>. Here is a <a href=\"http:\/\/temblor.net\/earthquake-insights\/pele-la-diosa-hawaiana-del-fuego-los-relampagos-el-viento-y-los-volcanes-de-hawai-7021\/\" rel=\"noopener\" target=\"_blank\">Spanish version<\/a>.<\/p>\n<p>Hawaii is an active volcanic island formed by hotspot volcanism. The Hawaii-Emperor Seamount Chain is a series of active and inactive volcanoes formed by this process and are in a line because the Pacific plate has been moving over the hotspot for many millions of years.<\/p>\n<p>As these volcanoes grow with time, the flanks of the volcanoes become covered in new volcanic rock. The flanks become unstable and collapse as landslides. There is evidence that some of these landslides trigger some of the largest tsunami ever found.<\/p>\n<p>The seismicity started in the central part of the &#8220;East Rift Zone&#8221; (ERZ), a region of extension probably caused by flank collapse. This extension lowers pressure in the magma chamber, leading to eruptions. Magma migrates around for various reasons, including changes in pressure in the magma chamber. These motions of magma and fluids can cause earthquakes.<\/p>\n<p>This part of Hawaii is the locus of the most recent volcanism, with the newest volcanic center formed to the southeast of the island.<\/p>\n<p>Southeast of the main Kilauea vent, the Pu\u2018u \u2018\u00d6\u2018\u00f6 crater saw an elevation of lava into the crater, leading to overtopping of the crater (on 4\/30\/2018). Seismicity migrated eastward along the ERZ. This morning, there was a M 5.0 earthquake in the region of the Hilina fault zone (HFZ). I was getting ready to write something up, but I had other work that I needed to complete. Then, this evening, there was a M 6.9 earthquake between the ERZ and the HFZ.<\/p>\n<p>There have been earthquakes this large in this region in the past (e.g. the 1975.1.29 M 7.1 earthquake along the HFZ). This earthquake was also most likely related to magma injection (Ando, 1979). The 1975 M 7.1 earthquake generated a small tsunami (Ando, 1979). These earthquakes are generally compressional in nature (including the earthquakes from today).<\/p>\n<p>Today&#8217;s earthquake also generated a tsunami as recorded on tide gages throughout Hawaii. There is probably no chance that a tsunami will travel across the Pacific to have a significant impact elsewhere.<\/p>\n<p>So. This M 6.9 may be the largest earthquake. There may be a larger one in store (the USGS suggests that these fault systems could produce a M 8 earthquake). The eruptions may be done for now. There may be more.<\/p>\n<h2><font color=\"orange\">Below is my interpretive poster for this earthquake<\/font><\/h2>\n<p>I plot the seismicity from the past month, with color representing depth and diameter representing magnitude (see legend). I include earthquake epicenters from 1918-2018 with magnitudes M \u2265 4.5 in a second poster (and down to M \u2265 3.5 in a third poster).<br \/>\nI plot the USGS fault plane solutions (moment tensors in blue and focal mechanisms in orange) for the M 6.9 earthquake, in addition to some relevant historic earthquakes.<br \/>\nI placed green circles in the locations of the (a) 4\/30 lava lake filling event and (b) 5\/3-4 fissure eruption.<\/p>\n<ul>\n<li>I placed a moment tensor \/ focal mechanism legend on the poster. There is more material from the USGS web sites about <a href=\"http:\/\/earthquake.usgs.gov\/learn\/glossary\/?term=moment%20tensor\" target=\"_blank\" rel=\"noopener\">moment tensors<\/a> and <a href=\"http:\/\/earthquake.usgs.gov\/learn\/topics\/beachball.php\" target=\"_blank\" rel=\"noopener\">focal mechanisms<\/a> (the beach ball symbols). Both moment tensors and focal mechanisms are solutions to seismologic data that reveal two possible interpretations for fault orientation and sense of motion. One must use other information, like the regional tectonics, to interpret which of the two possibilities is more likely. <\/li>\n<\/ul>\n<ul>\n<li>\n<h3><strong>I include some inset figures.<\/strong><\/h3>\n<\/li>\n<li>In the upper right corner is a geologic map with color representing the relative age of volcanic deposits (Sherrod et al., 2007). (red = youngest, orange next youngest) I placed a blue circle in the location of the vents that erupted on 5\/3-4.<\/li>\n<li>In the upper left corner is a map that shows the rift zones (active extensional volcanism) and the region is divided by the major sources for the volcanic rocks (e.g. Mauna Kea, Mauna Loa, and Kilauea; Tilling et al., 2010). I placed a blue circle in the location of the vents that erupted on 5\/3-4.<\/li>\n<li>In the lower left corner is a visualization showing the magma reservoir hypothesized to be the source of lava along the Southwest and East Rift zones, as well as for Kilauea (Tilling et al., 2010).<\/li>\n<li>In the lower right corner is a map that shows the relative severity of volcanic hazard for the island of Hawaii (Tilling, et al., 2010).<\/li>\n<li>To the left of the hazard map is a geological cross section showing the subsurface structures in the region (USGS).<\/li>\n<\/ul>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180504_hawaii_interpretation.pdf\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180504_hawaii_interpretation.jpg\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<ul>\n<li>This version includes earthquakes M \u2265 4.5<\/li>\n<\/ul>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180504_hawaii_interpretation_M45.pdf\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180504_hawaii_interpretation_M45.jpg\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<ul>\n<li>This version includes earthquakes M \u2265 3.5 (note the seismicity offshore to the south, this is where the youngest Hawaii volcano is).<\/li>\n<\/ul>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180504_hawaii_interpretation_M35.pdf\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180504_hawaii_interpretation_M35.jpg\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<ul>\n<li>Here is a photo of the seismic wave record on the <a href=\"https:\/\/www.facebook.com\/humboldtgeology\/photos\/a.655139441163496.1073741828.182630635081048\/1899427763401318\/?type=3&#038;theater\" rel=\"noopener\" target=\"_blank\">Humboldt State University, Department of Geology<\/a>, baby benioff seismograph.<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180504_hawaii_69_HSU_benioff.jpg\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180504_hawaii_69_HSU_benioff.jpg\" width=\"100%\" alt=\"\" \/><\/a>\n<\/ul>\n<h2><strong><font color=\"orange\">USGS Earthquake Pages<\/font><\/strong><\/h2>\n<ul>\n<h3><strong>These are from this current sequence<\/strong><\/h3>\n<li>2018.05.04 <a href=\"https:\/\/earthquake.usgs.gov\/earthquakes\/eventpage\/us1000dxhr#executive\" rel=\"noopener\" target=\"_blank\">M 5.0 Hawaii<\/a><\/li>\n<li>2018.05.04 <a href=\"https:\/\/earthquake.usgs.gov\/earthquakes\/eventpage\/us1000dyad#executive\" rel=\"noopener\" target=\"_blank\">M 6.9 Hawaii<\/a><\/li>\n<li>2018.05.04 <a href=\"https:\/\/earthquake.usgs.gov\/earthquakes\/eventpage\/us1000dy8n#executive\" rel=\"noopener\" target=\"_blank\">M 5.4 Hawaii<\/a><\/li>\n<\/ul>\n<ul>\n<li>I put together a short video that shows seismicity from the past month. This reveals how the magma may have moved throughout the region between 4\/27 and 5\/4. Here is a <a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180427_20180504_hawaii.mp4\" rel=\"noopener\" target=\"_blank\">link to download the ~8 MB mp4 video file<\/a>.<\/li>\n<p><div style=\"width: 640px;\" class=\"wp-video\"><!--[if lt IE 9]><script>document.createElement('video');<\/script><![endif]-->\n<video class=\"wp-video-shortcode\" id=\"video-7350-1\" width=\"640\" height=\"360\" preload=\"metadata\" controls=\"controls\"><source type=\"video\/mp4\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180427_20180504_hawaii.mp4?_=1\" \/><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180427_20180504_hawaii.mp4\">http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/20180427_20180504_hawaii.mp4<\/a><\/video><\/div>\n<\/ul>\n<h2><strong><font color=\"orange\">Some Relevant Discussion and Figures<\/font><\/strong><\/h2>\n<ul>\n<li>Here is the map showing the rifts (Tilling et al., 2010)<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/tilling_etal_2010_eruptions_hawaii_volcanoes_map_kilauea.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/tilling_etal_2010_eruptions_hawaii_volcanoes_map_kilauea.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>\nShaded relief map of the southeastern part of the Island of Hawai\u2018i, showing the principal features and localities of Mauna Loa, K\u00eflauea, and L\u00f6\u2018ihi Volcanoes discussed in the text.\n<\/p><\/blockquote>\n<li>This is the figure that shows an hypothetical configuration of the magma reservoir beneath Kilauea (Tilling et al., 2010).<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/tilling_etal_2010_eruptions_hawaii_volcanoes_plumbing_cut_away.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/tilling_etal_2010_eruptions_hawaii_volcanoes_plumbing_cut_away.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>\nCut-away view looking deep beneath K\u00eflauea Volcano, showing the shallow magma reservoir and the principal magma passageways. Areas in yellow are the most favorable zones for magma movement (arrows show direction) and storage. Though greatly generalized, this depiction of K\u00eflauea\u2019s \u201cplumbing system\u201d is compatible with all known scientific information. (Simplified from technical illustration of Michael P. Ryan, USGS.)\n<\/p><\/blockquote>\n<\/ul>\n<ul>\n<li>Below are a series of plots from tide gages installed at several sites in the Hawaii Island Chain. These data are all <a href=\"https:\/\/tidesandcurrents.noaa.gov\/map\/index.shtml?type=PreliminaryData&#038;region=Hawaii\" rel=\"noopener\" target=\"_blank\">posted online here<\/a> and <a href=\"http:\/\/www.ioc-sealevelmonitoring.org\/news.php?p=show&#038;id=5370\" rel=\"noopener\" target=\"_blank\">here<\/a>.<\/li>\n<li>Hilo, Hawaii<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/hilo_getchart.php_20180504_2340.png\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/hilo_getchart.php_20180504_2340.png\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<li>Kawaihae, Hawaii<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/kawaihae_getchart.php_20180504_2340.png\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/kawaihae_getchart.php_20180504_2340.png\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<li>Here is a plot showing the tsunami from the 1975 M 7.1 earthquake (Ando, 1979). On the left are modeled tsunami wave height based on two different fault models (each with fault dips of 20 degrees, but widths of 20km and 30km).<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/19751129_hawaii\/ando_1979_magma_injection_low_dip_angle_earthquake_19751129_kilauea_71_fig_11_B.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/19751129_hawaii\/ando_1979_magma_injection_low_dip_angle_earthquake_19751129_kilauea_71_fig_11_B.JPG\" width=\"100%\" alt=\"\" \/><\/a>\n<\/ul>\n<ul>\n<li>This is a timeline of historic volcanism on Hawaii (Tilling et al., 2010).<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/tilling_etal_2010_eruptions_hawaii_volcanoes_eruptions_historic_kilauea.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/tilling_etal_2010_eruptions_hawaii_volcanoes_eruptions_historic_kilauea.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>\nGraph summarizing the eruptions of Mauna Loa and K\u00eflauea Volcanoes during the past 200 years. The Pu\u2018u \u2018\u00d6\u2018\u00f6- Kupaianaha eruption has continued into the 21st century. Information is sketchy for eruptions before 1823, when the first missionaries arrived on the Island of Hawai\u2018i. The total duration of eruptive activity in a given year, shown by the length of the vertical bar, may be for a single eruption or a combination of several separate eruptions.\n<\/p><\/blockquote>\n<\/ul>\n<ul>\n<li>Here is the volcanic hazard severity map from Tilling et al. (2010).<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/tilling_etal_2010_eruptions_hawaii_volcanoes_hazard_hawaii.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/tilling_etal_2010_eruptions_hawaii_volcanoes_hazard_hawaii.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>\nMap of Island of Hawai\u2018i showing the volcanic hazards from lava flows. Severity of the hazard increases from zone 9 to zone 1. Shaded areas show land covered by flows erupted in the past two centuries from three of Hawai\u2018i\u2019s five volcanoes (Hual\u00e4lai, Mauna Loa, and K\u00eflauea).\n<\/p><\/blockquote>\n<\/ul>\n<ul>\n<li>Below is a series of maps that shows the recent volcanism in the region (Orr et al., 2012).<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/orr_etal_2012_info_packet_puuoo_eruption_30_yrs_map_1983_1986.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/orr_etal_2012_info_packet_puuoo_eruption_30_yrs_map_1983_1986.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>The first 3\u00bd years of the Pu\u2018u \u2018\u00d6\u00ff\u00f6 eruption of K\u00eflauea Volcano (January 1983\u2013June 1986) were dominated by episodic lava fountains that constructed the Pu\u2018u \u2018\u00d6\u00ff\u00f6 cone and fed \u2018a\u2018\u00e4 flows (the less fluid of the two types of Hawaiian lava flows) (USGS photo by J.D. Griggs, June 1984). The map shows lava flows erupted from K\u00eflauea Volcano in the 19th and 20th centuries (gray). These flows originated from the summit caldera, the East Rift Zone, or the Southwest Rift Zone (not shown). Flows erupted during the first 3\u00bd years of the Pu\u2018u \u2018\u00d6\u00ff\u00f6 eruption are shown in red. The Island of Hawai\u2018i (see inset map) is composed of five volcanoes\u2014Kohala, Mauna Kea, Hual\u00e4lai, Mauna Loa, and K\u00eflauea\n<\/p><\/blockquote>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/orr_etal_2012_info_packet_puuoo_eruption_30_yrs_map_1986_1992.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/orr_etal_2012_info_packet_puuoo_eruption_30_yrs_map_1986_1992.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>\nIn 1986, the Pu\u2018u \u2018\u00d6\u00ff\u00f6 eruption shifted to the Kupaianaha vent. This photo shows lava flows erupted from Kupaianaha entering the community of Kalapana on the Island of Hawai\u2018i\u2019s southeast coast in May 1990 (USGS photo by J.D. Griggs). Over the following months, Kalapana was almost completely destroyed, and lava filled beautiful nearby Kaim\u00fc Bay. The map shows lava flows erupted from Kupaianaha and nearby fissures during 1986\u20131992 in red. Older flows from the Pu\u2018u \u2018\u00d6\u00ff\u00f6 eruption are shown in orange.\n<\/p><\/blockquote>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/orr_etal_2012_info_packet_puuoo_eruption_30_yrs_map_1992_2007.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/orr_etal_2012_info_packet_puuoo_eruption_30_yrs_map_1992_2007.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>Lava flows erupt from new vents on the south flank of the Pu\u2018u \u2018\u00d6\u00ff\u00f6 cone (right side of photo) that opened after Pu\u2018u \u2018\u00d6\u00ff\u00f6 Crater filled to overflowing in early 2004 (USGS photo by Richard Hoblitt, January 2004). Collapse of the southwest side of the cone formed a scallop-shaped scar, revealing red layers of welded spatter (deposited as clots of molten lava) that under-lie loose tan-colored pyroclastic deposits (hot debris ejected during an eruption). The map shows flows erupted from Pu\u2018u \u2018\u00d6\u00ff\u00f6 and from fissures in N\u00e4pau Crater during 1992\u20132007 in red. Older flows from the Pu\u2018u \u2018\u00d6\u00ff\u00f6 eruption are shown in orange.\n<\/p><\/blockquote>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/orr_etal_2012_info_packet_puuoo_eruption_30_yrs_map_2007_2011.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/orr_etal_2012_info_packet_puuoo_eruption_30_yrs_map_2007_2011.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>\nA lava channel, elevated as much as 150 feet (45 meters) above the adjacent terrain, transports lava away from the Fissure D vent, which opened in July 2007 (USGS photo by James Kauahikaua, October 2007). The \u201cperched\u201d (elevated) lava channel was the main path for lava until November 2007, when lava was diverted from the vent to the southeast. Pu\u2018u \u2018\u00d6\u00ff\u00f6 is at upper right. The map shows lava flows erupted in Pu\u2018u \u2018\u00d6\u00ff\u00f6 and from the Fissure D vent between Pu\u2018u \u2018\u00d6\u00ff\u00f6 and Kupaianaha during 2007\u20132011 in red. Older flows from the Pu\u2018u \u2018\u00d6\u00ff\u00f6 eruption are shown in orange.\n<\/p><\/blockquote>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/orr_etal_2012_info_packet_puuoo_eruption_30_yrs_map_2011_2012.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/orr_etal_2012_info_packet_puuoo_eruption_30_yrs_map_2011_2012.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>\nIn March 2011, lava broke to the surface between Pu\u2018u \u2018\u00d6\u00ff\u00f6 and N\u00e4pau Crater marking the start of the Kamoamoa fissure eruption. In this photo lava erupts from the fissure shortly after the beginning of the eruption and pours into a deep, older crack (USGS photo by Tim Orr). The map shows flows erupted during the Kamoamoa eruption and from Pu\u2018u \u2018\u00d6\u00ff\u00f6 during 2011\u20132012 in red. The Kamoamoa flows are to the left, flows from the August 2011 Pu\u2018u \u2018\u00d6\u00ff\u00f6 flank breakout are at center, flows from a fissure high on Pu\u2018u \u2018\u00d6\u00ff\u00f6\u2019s northeast flank are to the right. Older flows from the Pu\u2018u \u2018\u00d6\u00ff\u00f6 eruption are shown in orange.\n<\/p><\/blockquote>\n<\/ul>\n<ul>\n<li>This map highlights the seismicity associated with volcanism related to the youngest volcano in the Hawaii Islands (Tilling et al., 2010).<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/tilling_etal_2010_eruptions_hawaii_volcanoes_loihi_volcano_newest.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/tilling_etal_2010_eruptions_hawaii_volcanoes_loihi_volcano_newest.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>\nMap showing the locations of earthquakes that occurred during the 1970s and in the July\u2013August 1996 period in the vicinity of L\u00f6\u2018ihi. These earthquake swarms, plus similar occurrences in 1984\u201385 and the early 1990s, provide seismic evidence that L\u00f6\u2018ihi is an active submarine volcano.\n<\/p><\/blockquote>\n<\/ul>\n<ul>\n<li>The ERZ and HFZ are also actively deforming between earthquakes. Below are two maps that show (a) regional vertical land motion and (b) results from block modeling to resolve the differential motion across this area (Shirzaei et al., 2013).<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/shirzaei_etal_2013_aseismic_deformation_hilina_fault_fig_01_A.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/shirzaei_etal_2013_aseismic_deformation_hilina_fault_fig_01_A.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>\nThe linear velocity field in the line of sight of the descending-orbit Envisat satellite (track 200) over the Kilauea south flank from 2003 till 2010. Area of the study, Hilina Fault System (HFS), is outlined by dashed box. Location of GPS stations used is marked by their names next to filled squares colored by the mean rate of motion in the LOS direction. Station PGF1 is the reference for both GPS and InSAR datasets. WHP = western Hilina Pali, HP = Holei Pali.\n<\/p><\/blockquote>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/shirzaei_etal_2013_aseismic_deformation_hilina_fault_fig_06_A.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/shirzaei_etal_2013_aseismic_deformation_hilina_fault_fig_06_A.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>\nColored panels represent relatively coherently moving blocks based on the InSAR deformation over the HFS according to Figs. 2\u20134 and traces of mapped faults, which are used to compare with GPS data. Each block is labeled by its average LOS velocity.\n<\/p><\/blockquote>\n<\/ul>\n<h2><strong><font color=\"orange\">Geologic Fundamentals<\/font><\/strong><\/h2>\n<ul>\n<li>This is an image from the USGS that shows how, when an oceanic plate moves over a hotspot, the volcanoes formed over the hotspot form a series of volcanoes that increase in age in the direction of plate motion. The presumption is that the hotspot is stable and stays in one location. Torsvik et al. (2017) use various methods to evaluate why this is a false presumption for the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Hawaii_hotspot\" rel=\"noopener\" target=\"_blank\">Hawaii Hotspot<\/a>.<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/USGS_Hawaii_hotspot_cross_sectional_diagram.jpg\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/USGS_Hawaii_hotspot_cross_sectional_diagram.jpg\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>A cutaway view along the Hawaiian island chain showing the inferred mantle plume that has fed the Hawaiian hot spot on the overriding Pacific Plate. The geologic ages of the oldest volcano on each island (Ma = millions of years ago) are progressively older to the northwest, consistent with the hot spot model for the origin of the Hawaiian Ridge-Emperor Seamount Chain. (Modified from image of Joel E. Robinson, USGS, in \u201cThis Dynamic Planet\u201d map of Simkin and others, 2006.)\n<\/p><\/blockquote>\n<li>Here is a map from Torsvik et al. (2017) that shows the age of volcanic rocks at different locations along the Hawaii-Emperor Seamount Chain.<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/torsvik_etal_2017_pacific_plate_motion_fig_01.JPG\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/torsvik_etal_2017_pacific_plate_motion_fig_01.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<blockquote><p>\nHawaiian-Emperor Chain. White dots are the locations of radiometrically dated seamounts, atolls and islands, based on compilations of Doubrovine et al. and O\u2019Connor et al. Features encircled with larger white circles are discussed in the text and Fig. 2. Marine gravity anomaly map is from Sandwell and Smith.\n<\/p><\/blockquote>\n<\/ul>\n<ul>\n<li>Here is a great educational video from the USGS that discusses eruptions in 2011, which were similar in type and style of eruptions as the current phase of eruption. Here is a <a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/A_007_hawaiiOriginOfEarthquakes.mp4\" rel=\"noopener\" target=\"_blank\">link to the 4 MB mp4 video file<\/a>.<\/li>\n<p><div style=\"width: 640px;\" class=\"wp-video\"><video class=\"wp-video-shortcode\" id=\"video-7350-2\" width=\"640\" height=\"360\" preload=\"metadata\" controls=\"controls\"><source type=\"video\/mp4\" src=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/K%c4%ablauea_Summit_Eruption_Halemaumau_USGS_2017.mp4?_=2\" \/><a href=\"http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/K%c4%ablauea_Summit_Eruption_Halemaumau_USGS_2017.mp4\">http:\/\/earthjay.com\/earthquakes\/20180504_hawaii\/K%c4%ablauea_Summit_Eruption_Halemaumau_USGS_2017.mp4<\/a><\/video><\/div>\n<\/ul>\n<ul>\n<li>For more on the graphical representation of moment tensors and focal mechanisms, check this <a href=\"http:\/\/www.iris.edu\/hq\/programs\/education_and_outreach\/animations\/25\" target=\"_blank\" rel=\"noopener\">IRIS<\/a> video out:<\/li>\n<p><iframe loading=\"lazy\" width=\"420\" height=\"315\" src=\"https:\/\/www.youtube.com\/embed\/MomVOkyDdLo\" frameborder=\"0\" allowfullscreen><\/iframe>\n<\/ul>\n<ul>\n<li>Here is a fantastic infographic from Frisch et al. (2011). This figure shows some examples of earthquakes in different plate tectonic settings, and what their fault plane solutions are. There is a cross section showing these focal mechanisms for a thrust or reverse earthquake. The upper right corner includes my favorite figure of all time. This shows the first motion (up or down) for each of the four quadrants. This figure also shows how the amplitude of the seismic waves are greatest (generally) in the middle of the quadrant and decrease to zero at the nodal planes (the boundary of each quadrant).<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/Plate_Tectonics_2011_page_23_fault_plane_solutions.pdf\" rel=\"noopener\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/Plate_Tectonics_2011_page_23_fault_plane_solutions.jpg\" width=\"100%\" width=\"100%\" alt=\"\" \/><\/a>\n<\/ul>\n<ul>\n<li>There are three types of earthquakes, strike-slip, compressional (reverse or thrust, depending upon the dip of the fault), and extensional (normal). Here is are some animations of these three types of earthquake faults. The following three animations are from <a href=\"http:\/\/www.iris.edu\/hq\/programs\/education_and_outreach\/animations\/2\" target=\"_blank\" rel=\"noopener\">IRIS<\/a>.<\/li>\n<p>Strike Slip:<br \/>\n<iframe loading=\"lazy\" width=\"420\" height=\"315\" src=\"https:\/\/www.youtube.com\/embed\/MrrLJ4vXHCs\" frameborder=\"0\" allowfullscreen><\/iframe><br \/>\nCompressional:<br \/>\n<iframe loading=\"lazy\" width=\"420\" height=\"315\" src=\"https:\/\/www.youtube.com\/embed\/4b81nXSVA34\" frameborder=\"0\" allowfullscreen><\/iframe><br \/>\nExtensional:<br \/>\n<iframe loading=\"lazy\" width=\"420\" height=\"315\" src=\"https:\/\/www.youtube.com\/embed\/tJDnfT1pqhQ\" frameborder=\"0\" allowfullscreen><\/iframe>\n<\/ul>\n<h2><strong><font color=\"orange\">Social Media<\/font><\/strong><\/h2>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Earthquakes in <a href=\"https:\/\/twitter.com\/hashtag\/Hawaii?src=hash&amp;ref_src=twsrc%5Etfw\">#Hawaii<\/a> &#8211; what you need to know. From the <a href=\"https:\/\/twitter.com\/USGS?ref_src=twsrc%5Etfw\">@USGS<\/a> <a href=\"https:\/\/t.co\/G3zjXwUBFZ\">https:\/\/t.co\/G3zjXwUBFZ<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/earthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#earthquake<\/a> <a href=\"https:\/\/t.co\/UOqbXeycUi\">pic.twitter.com\/UOqbXeycUi<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/992574912597577729?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Volcano talk! Kilauea is the world&#39;s most active volcano. It&#39;s been erupting since the early 1980s. Hawai&#39;i volcanoes are shield volcanoes, meaning they don&#39;t look or erupt like their stratovolcano (cone-shaped) cousins. Here&#39;s a pic of Kilauea&#39;s summit eruption last April. 1\/ <a href=\"https:\/\/t.co\/u6rhjiDM0N\">pic.twitter.com\/u6rhjiDM0N<\/a><\/p>\n<p>&mdash; Jess Phoenix (@jessphoenix2018) <a href=\"https:\/\/twitter.com\/jessphoenix2018\/status\/992494416731361280?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\"><a href=\"https:\/\/t.co\/IO9VJ8yYVL\">https:\/\/t.co\/IO9VJ8yYVL<\/a> An eruption has begun in the Puna District of the Big Island of Hawai&#39;i. Eruptions in this area are rarer, but more people live there as well. Here&#39;s a bit of perspective on why this eruption isn&#39;t &quot;run of the mill&quot;. <a href=\"https:\/\/t.co\/SQmaOJR7oN\">pic.twitter.com\/SQmaOJR7oN<\/a><\/p>\n<p>&mdash; Garry Hayes (@geotripper) <a href=\"https:\/\/twitter.com\/geotripper\/status\/992304188892708864?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\"><a href=\"https:\/\/twitter.com\/hashtag\/earthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#earthquake<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/hawaii?src=hash&amp;ref_src=twsrc%5Etfw\">#hawaii<\/a> video my boyfriend took in our house in Papaikou during the 6.9 earthquake &#x1f633; <a href=\"https:\/\/t.co\/xAAjeN1zFO\">pic.twitter.com\/xAAjeN1zFO<\/a><\/p>\n<p>&mdash; Allison (@Allieb1792) <a href=\"https:\/\/twitter.com\/Allieb1792\/status\/992560580241211393?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Earthquakes migrate east of Pu\u2018u \u2018\u014c\u2018\u014d, signaling an intrusion of magma along the middle and lower East Rift Zone. Orange dashed line marks the approximate area within which most of the earthquakes are located. <a href=\"https:\/\/t.co\/vJRUw2HRvh\">https:\/\/t.co\/vJRUw2HRvh<\/a> <a href=\"https:\/\/t.co\/nhMbMH20yW\">pic.twitter.com\/nhMbMH20yW<\/a><\/p>\n<p>&mdash; USGS Volcanoes&#x1f30b; (@USGSVolcanoes) <a href=\"https:\/\/twitter.com\/USGSVolcanoes\/status\/992067345140015105?ref_src=twsrc%5Etfw\">May 3, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">VIDEO &#8211; What is a volcanic hotspot?<a href=\"https:\/\/t.co\/HjaDofrKJU\">https:\/\/t.co\/HjaDofrKJU<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/earthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#earthquake<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/Hawaii?src=hash&amp;ref_src=twsrc%5Etfw\">#Hawaii<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/volcano?src=hash&amp;ref_src=twsrc%5Etfw\">#volcano<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/hawaiivolcano?src=hash&amp;ref_src=twsrc%5Etfw\">#hawaiivolcano<\/a> <a href=\"https:\/\/t.co\/Esu4rYA03v\">pic.twitter.com\/Esu4rYA03v<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/992579753621192704?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Phwoooarrrr, look at those gorgeous fringes. <a href=\"https:\/\/t.co\/JgyJwtxlIW\">https:\/\/t.co\/JgyJwtxlIW<\/a><\/p>\n<p>&mdash; Stephen Hicks (@seismo_steve) <a href=\"https:\/\/twitter.com\/seismo_steve\/status\/991937487034568704?ref_src=twsrc%5Etfw\">May 3, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Kilauea has been an active volcano for a very long time. To learn more about the recent history, go here: <a href=\"https:\/\/t.co\/5EPtjQ2lR3\">https:\/\/t.co\/5EPtjQ2lR3<\/a> <a href=\"https:\/\/t.co\/zdRpnHHjEU\">pic.twitter.com\/zdRpnHHjEU<\/a><\/p>\n<p>&mdash; Dr Janine Krippner (@janinekrippner) <a href=\"https:\/\/twitter.com\/janinekrippner\/status\/992413750991912960?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Mw=6.8, HAWAII (Depth: 32 km), 2018\/05\/04 22:32:55 UTC &#8211; Full details here: <a href=\"https:\/\/t.co\/Ii2DCFI3ga\">https:\/\/t.co\/Ii2DCFI3ga<\/a> <a href=\"https:\/\/t.co\/WNlRcGFNmP\">pic.twitter.com\/WNlRcGFNmP<\/a><\/p>\n<p>&mdash; Earthquakes (@geoscope_ipgp) <a href=\"https:\/\/twitter.com\/geoscope_ipgp\/status\/992545491404689408?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">NASA-JPL ARIA automatic wrapped interferogram Copernicus Sentinel-1 (2.8 cm contours) with USGS preliminary epicenter for Mw6.9 earthquake (red star). My early interpretation is earthquake likely on detachment beneath East Rift Zone. <a href=\"https:\/\/t.co\/ZocsY4AuTO\">pic.twitter.com\/ZocsY4AuTO<\/a><\/p>\n<p>&mdash; Eric Fielding (@EricFielding) <a href=\"https:\/\/twitter.com\/EricFielding\/status\/992545159857430528?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">And for seismology fans, some jargon: the double couple % of 66 for this moment tensor suggests this M5.4 may not be simple motion on a fault plane, or it could just be due to this being a small quake in a complex velocity structure <a href=\"https:\/\/t.co\/ghwUiIUxJP\">https:\/\/t.co\/ghwUiIUxJP<\/a> <a href=\"https:\/\/t.co\/sAK0Ay95dK\">pic.twitter.com\/sAK0Ay95dK<\/a><\/p>\n<p>&mdash; Jascha Polet (@CPPGeophysics) <a href=\"https:\/\/twitter.com\/CPPGeophysics\/status\/992528776897560576?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">How the erupting Hawaiian <a href=\"https:\/\/twitter.com\/hashtag\/volcano?src=hash&amp;ref_src=twsrc%5Etfw\">#volcano<\/a> caused today\u2019s magnitude 6.9 quake on Hawaii Island \u2014 and was felt as far as Honolulu <a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> <a href=\"https:\/\/t.co\/jSKTuFhJ3m\">https:\/\/t.co\/jSKTuFhJ3m<\/a> <a href=\"https:\/\/t.co\/spL90lBtDJ\">pic.twitter.com\/spL90lBtDJ<\/a><\/p>\n<p>&mdash; Ron Lin (@ronlin) <a href=\"https:\/\/twitter.com\/ronlin\/status\/992612499693428736?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Mechanism for M5.6 from <a href=\"https:\/\/twitter.com\/geoscope_ipgp?ref_src=twsrc%5Etfw\">@geoscope_ipgp<\/a> similar to that of other large shallow earthquakes on the Big Island, such as the 1975 Kalapana M7.5+ quake <a href=\"https:\/\/t.co\/gfGfu4MFxn\">https:\/\/t.co\/gfGfu4MFxn<\/a> <a href=\"https:\/\/t.co\/eAvk6HaUmJ\">pic.twitter.com\/eAvk6HaUmJ<\/a><\/p>\n<p>&mdash; Jascha Polet (@CPPGeophysics) <a href=\"https:\/\/twitter.com\/CPPGeophysics\/status\/992533557724631041?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\"><a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> update: <a href=\"https:\/\/twitter.com\/hashtag\/PuuOo?src=hash&amp;ref_src=twsrc%5Etfw\">#PuuOo<\/a> erupted red ash when crater collapsed (webcam is coated).<br \/>+ 61G flow sluggish, but active.<br \/>+ 1km-long <a href=\"https:\/\/twitter.com\/hashtag\/groundcrack?src=hash&amp;ref_src=twsrc%5Etfw\">#groundcrack<\/a> uprift of PuuOo<br \/>+ Summit unaffected by ERZ activity<br \/>Update: <a href=\"https:\/\/t.co\/sfajMPjR8Z\">https:\/\/t.co\/sfajMPjR8Z<\/a><br \/>Images: <a href=\"https:\/\/t.co\/gU4wYZM10M\">https:\/\/t.co\/gU4wYZM10M<\/a><a href=\"https:\/\/twitter.com\/hashtag\/Hawaii?src=hash&amp;ref_src=twsrc%5Etfw\">#Hawaii<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/volcano?src=hash&amp;ref_src=twsrc%5Etfw\">#volcano<\/a> <a href=\"https:\/\/t.co\/FyzlrSWb8w\">pic.twitter.com\/FyzlrSWb8w<\/a><\/p>\n<p>&mdash; USGS Volcanoes&#x1f30b; (@USGSVolcanoes) <a href=\"https:\/\/twitter.com\/USGSVolcanoes\/status\/991729200036904960?ref_src=twsrc%5Etfw\">May 2, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Own processing of a Sentinel-1 interferogram showing deformation (from 19th March to 1st May 2018) before the current Kilauea eruption.<\/p>\n<p>Note: Same interferogram (and essentially same information) as already provided by HVO USGS, differences due to refined InSAR processing. <a href=\"https:\/\/t.co\/3ARmvbkDTS\">pic.twitter.com\/3ARmvbkDTS<\/a><\/p>\n<p>&mdash; Pablo J. Gonz\u00e1lez (@pabloj_gonzalez) <a href=\"https:\/\/twitter.com\/pabloj_gonzalez\/status\/992462731088408576?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Get <a href=\"https:\/\/twitter.com\/ESA_EO?ref_src=twsrc%5Etfw\">@ESA_EO<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/Sentinel1?src=hash&amp;ref_src=twsrc%5Etfw\">#Sentinel1<\/a> ifgrms for Kilauea, Hawaii from <a href=\"https:\/\/twitter.com\/UAFGI?ref_src=twsrc%5Etfw\">@UAFGI<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/SARVIEWS?src=hash&amp;ref_src=twsrc%5Etfw\">#SARVIEWS<\/a> portal. All <a href=\"https:\/\/twitter.com\/hashtag\/InSAR?src=hash&amp;ref_src=twsrc%5Etfw\">#InSAR<\/a> data &amp; geocoded images can be freely downloaded @ <a href=\"https:\/\/t.co\/chhgAEwy4q\">https:\/\/t.co\/chhgAEwy4q<\/a>. Go &amp; get your research on &#x1f6f0;&#xfe0f;! <\/p>\n<p>More data also from <a href=\"https:\/\/twitter.com\/NERC_COMET?ref_src=twsrc%5Etfw\">@NERC_COMET<\/a> &amp; <a href=\"https:\/\/twitter.com\/NASAJPL?ref_src=twsrc%5Etfw\">@NASAJPL<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/ARIA?src=hash&amp;ref_src=twsrc%5Etfw\">#ARIA<\/a> <a href=\"https:\/\/twitter.com\/InSARinfo?ref_src=twsrc%5Etfw\">@InSARinfo<\/a> <a href=\"https:\/\/twitter.com\/Ak_Satellite?ref_src=twsrc%5Etfw\">@Ak_Satellite<\/a> <a href=\"https:\/\/t.co\/baZqxsabwT\">pic.twitter.com\/baZqxsabwT<\/a><\/p>\n<p>&mdash; Franz J Meyer (@SARevangelist) <a href=\"https:\/\/twitter.com\/SARevangelist\/status\/992563881078804480?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Scientists predicted that the current <a href=\"https:\/\/twitter.com\/hashtag\/KilaueaVolcano?src=hash&amp;ref_src=twsrc%5Etfw\">#KilaueaVolcano<\/a>  <a href=\"https:\/\/twitter.com\/hashtag\/eruption?src=hash&amp;ref_src=twsrc%5Etfw\">#eruption<\/a> was going to happen! Since collapse of the Pu&#39;u O&#39;o vent (4\/30), there have been tons of earthquakes under the East Rift Zone- signaling magma injection that way<br \/>I made this map showing Mag 2+ EQs in last week <a href=\"https:\/\/t.co\/DVOdqIQtIg\">pic.twitter.com\/DVOdqIQtIg<\/a><\/p>\n<p>&mdash; Dr. Brad Pitcher (@TieDyeSciGuy) <a href=\"https:\/\/twitter.com\/TieDyeSciGuy\/status\/992440770627014656?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"es\" dir=\"ltr\"><a href=\"https:\/\/twitter.com\/hashtag\/Ahora?src=hash&amp;ref_src=twsrc%5Etfw\">#Ahora<\/a> &#8211; se registra una erupci\u00f3n fisural en Leilani Estates al sureste de la Isla Grande, Haw\u00e1i. Al fondo se observa lava brotando de la fractura en la superficie.<\/p>\n<p>Cr\u00e9ditos: <a href=\"https:\/\/twitter.com\/JenMyersFox4?ref_src=twsrc%5Etfw\">@JenMyersFox4<\/a> &amp; Jeff Wise<\/p>\n<p> <a href=\"https:\/\/t.co\/hloCkViSGn\">pic.twitter.com\/hloCkViSGn<\/a><\/p>\n<p>&mdash; SkyAlert (@SkyAlertMx) <a href=\"https:\/\/twitter.com\/SkyAlertMx\/status\/992242733677981696?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Drone video from above the lava outbreak in Leilani Estates on Hawaii Island shows roads, homes near the path of destruction. MORE: <a href=\"https:\/\/t.co\/ji6WuCmylO\">https:\/\/t.co\/ji6WuCmylO<\/a> <a href=\"https:\/\/t.co\/q41ZyD8hix\">pic.twitter.com\/q41ZyD8hix<\/a><\/p>\n<p>&mdash; Hawaii News Now (@HawaiiNewsNow) <a href=\"https:\/\/twitter.com\/HawaiiNewsNow\/status\/992249742389166080?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">New map of locations of first three eruptive fissures in Leilani Estates Subdivision (Hawaii) as of this morning (May 4). Fissures are jetting sulfur dioxide gas and lava spatter. Updated maps will be posted on the USGS-Hawaiian Volcano Observatory page at <a href=\"https:\/\/t.co\/TD5y5GV1Xk\">https:\/\/t.co\/TD5y5GV1Xk<\/a> <a href=\"https:\/\/t.co\/ACS76UibXv\">pic.twitter.com\/ACS76UibXv<\/a><\/p>\n<p>&mdash; USGS Volcanoes&#x1f30b; (@USGSVolcanoes) <a href=\"https:\/\/twitter.com\/USGSVolcanoes\/status\/992514410638860288?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">VIDEO &#8211; What do earthquakes tell us about a volcano? <a href=\"https:\/\/t.co\/4sLpdlKeY7\">https:\/\/t.co\/4sLpdlKeY7<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/Earthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#Earthquake<\/a> activity beneath a <a href=\"https:\/\/twitter.com\/hashtag\/volcano?src=hash&amp;ref_src=twsrc%5Etfw\">#volcano<\/a> usually increases before an eruption bc magma &amp; gases must force their way up through underground fractures &amp; passageways causing rocks to break &amp; vibrate. <a href=\"https:\/\/t.co\/oahBGnlU7l\">pic.twitter.com\/oahBGnlU7l<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/992596526785617922?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Kilauea Volcano Erupts: information from USGS, with more information links:<a href=\"https:\/\/t.co\/9L65xWK6O6\">https:\/\/t.co\/9L65xWK6O6<\/a> <a href=\"https:\/\/t.co\/SFWXWMCAlL\">pic.twitter.com\/SFWXWMCAlL<\/a><\/p>\n<p>&mdash; Dr Janine Krippner (@janinekrippner) <a href=\"https:\/\/twitter.com\/janinekrippner\/status\/992453140690751490?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">I\u2019ve updated today\u2019s post on the <a href=\"https:\/\/twitter.com\/hashtag\/LeilaniEstates?src=hash&amp;ref_src=twsrc%5Etfw\">#LeilaniEstates<\/a> eruption with news of the M6.9 earthquake on the East Rift zone and continuing fissure eruptions: <a href=\"https:\/\/t.co\/1apjbUJIir\">https:\/\/t.co\/1apjbUJIir<\/a> <a href=\"https:\/\/t.co\/FRnBRaYs14\">pic.twitter.com\/FRnBRaYs14<\/a><\/p>\n<p>&mdash; Erik Klemetti (@eruptionsblog) <a href=\"https:\/\/twitter.com\/eruptionsblog\/status\/992581104849780741?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><br \/>\n<iframe loading=\"lazy\" width=\"520\" height=\"315\" src=\"https:\/\/www.youtube.com\/embed\/rM9wjM-ucEs\" frameborder=\"0\" allow=\"autoplay; encrypted-media\" allowfullscreen><\/iframe><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">There have been more than 428 M2+ <a href=\"https:\/\/twitter.com\/hashtag\/earthquakes?src=hash&amp;ref_src=twsrc%5Etfw\">#earthquakes<\/a> along the south flank of <a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> in the last month. The recent M6.9 is the largest in this series. <a href=\"https:\/\/twitter.com\/hashtag\/Hawaiiearthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#Hawaiiearthquake<\/a> <a href=\"https:\/\/t.co\/Jb3K65hzDR\">https:\/\/t.co\/Jb3K65hzDR<\/a> <a href=\"https:\/\/t.co\/DvjyRxUEB6\">pic.twitter.com\/DvjyRxUEB6<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/992588892493766656?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"ca\" dir=\"ltr\">WEBINAR &#8211; Several flavors of seismogenic magma movement under Kilauea Volcano <a href=\"https:\/\/t.co\/LodCt1afLQ\">https:\/\/t.co\/LodCt1afLQ<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/KilaueaVolcano?src=hash&amp;ref_src=twsrc%5Etfw\">#KilaueaVolcano<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/hawaiivolcano?src=hash&amp;ref_src=twsrc%5Etfw\">#hawaiivolcano<\/a> <a href=\"https:\/\/t.co\/SQfFLRaaPd\">pic.twitter.com\/SQfFLRaaPd<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/992596970484191232?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Seismic waves from the M6.9 Hawaii earthquake rolled through greater Vancouver about 30 minutes ago. Not felt in <a href=\"https:\/\/twitter.com\/hashtag\/Canada?src=hash&amp;ref_src=twsrc%5Etfw\">#Canada<\/a>, but easily recorded by our seismometers.<br \/>Details on the earthquake and impacts in Hawaii from the USGS:<a href=\"https:\/\/t.co\/1z5aYWuzcn\">https:\/\/t.co\/1z5aYWuzcn<\/a> <a href=\"https:\/\/t.co\/SbD8a3zJVW\">pic.twitter.com\/SbD8a3zJVW<\/a><\/p>\n<p>&mdash; John Cassidy (@earthquakeguy) <a href=\"https:\/\/twitter.com\/earthquakeguy\/status\/992550138911617025?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<h2>UPDATE 5\/5<\/h2>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">The IRIS special events page for the <a href=\"https:\/\/twitter.com\/hashtag\/Hawaiiearthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#Hawaiiearthquake<\/a> is now live. We welcome any additional contributions that might be of interest to the seismology research community.<a href=\"https:\/\/t.co\/0c9crR3lSr\">https:\/\/t.co\/0c9crR3lSr<\/a> <a href=\"https:\/\/t.co\/4xjcPs4VAx\">pic.twitter.com\/4xjcPs4VAx<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/992746672487849985?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\"><a href=\"https:\/\/t.co\/IO9VJ8yYVL\">https:\/\/t.co\/IO9VJ8yYVL<\/a> An eruption has begun in the Puna District of the Big Island of Hawai&#39;i. Eruptions in this area are rarer, but more people live there as well. Here&#39;s a bit of perspective on why this eruption isn&#39;t &quot;run of the mill&quot;. <a href=\"https:\/\/t.co\/SQmaOJR7oN\">pic.twitter.com\/SQmaOJR7oN<\/a><\/p>\n<p>&mdash; Garry Hayes (@geotripper) <a href=\"https:\/\/twitter.com\/geotripper\/status\/992304188892708864?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Watch the waves from the recent <a href=\"https:\/\/twitter.com\/hashtag\/hawaiiearthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#hawaiiearthquake<\/a> travel across the USArray seismic network (<a href=\"https:\/\/t.co\/RIcNz4bgWq\">https:\/\/t.co\/RIcNz4bgWq<\/a>) in Alaska! <a href=\"https:\/\/t.co\/t6zCZT4y3R\">https:\/\/t.co\/t6zCZT4y3R<\/a> <a href=\"https:\/\/t.co\/sKaV1bPHPI\">pic.twitter.com\/sKaV1bPHPI<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/992717355305271296?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><br \/>\n<iframe loading=\"lazy\" width=\"520\" height=\"315\" src=\"https:\/\/www.youtube.com\/embed\/cY5-nJ1tpdo\" frameborder=\"0\" allow=\"autoplay; encrypted-media\" allowfullscreen><\/iframe><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\"><a href=\"https:\/\/twitter.com\/hashtag\/GPS?src=hash&amp;ref_src=twsrc%5Etfw\">#GPS<\/a> data show up to 0.5 m of motion due to Friday&#39;s M6.9 <a href=\"https:\/\/twitter.com\/hashtag\/earthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#earthquake<\/a> at <a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a>. A computer simulation indicates up to 2.5 m of motion on the <a href=\"https:\/\/twitter.com\/hashtag\/fault?src=hash&amp;ref_src=twsrc%5Etfw\">#fault<\/a> beneath Kilauea, 7-9 km beneath the volcano&#39;s south flank. <a href=\"https:\/\/t.co\/hhZHif6ysS\">pic.twitter.com\/hhZHif6ysS<\/a><\/p>\n<p>&mdash; USGS Volcanoes&#x1f30b; (@USGSVolcanoes) <a href=\"https:\/\/twitter.com\/USGSVolcanoes\/status\/992858669711699968?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">7 am Eruption Update: Fissure Activity Continues In Leilani.<br \/>\u201cActive volcanic vents are located on Makamae, Kaupili and Mohala Streets,\u201d <br \/>Recording: <a href=\"https:\/\/t.co\/nBTjpFJiTc\">https:\/\/t.co\/nBTjpFJiTc<\/a> <a href=\"https:\/\/t.co\/fFOXqsJXQs\">pic.twitter.com\/fFOXqsJXQs<\/a><\/p>\n<p>&mdash; Dr Janine Krippner (@janinekrippner) <a href=\"https:\/\/twitter.com\/janinekrippner\/status\/992828729868144640?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\"><a href=\"https:\/\/twitter.com\/hashtag\/Sentinel1?src=hash&amp;ref_src=twsrc%5Etfw\">#Sentinel1<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/InSAR?src=hash&amp;ref_src=twsrc%5Etfw\">#InSAR<\/a> result for Apr 19-May 1 (6 pm local) from <a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> shows deformation due to ongoing magmatic intrusion. Magma withdrawn from middle East Rift Zone and intruded beneath lower East Rift Zone. No coincident deflation of summit. Update: <a href=\"https:\/\/t.co\/sfajMPjR8Z\">https:\/\/t.co\/sfajMPjR8Z<\/a> <a href=\"https:\/\/t.co\/szjuyk2b5D\">pic.twitter.com\/szjuyk2b5D<\/a><\/p>\n<p>&mdash; USGS Volcanoes&#x1f30b; (@USGSVolcanoes) <a href=\"https:\/\/twitter.com\/USGSVolcanoes\/status\/991769893665034240?ref_src=twsrc%5Etfw\">May 2, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\"><a href=\"https:\/\/twitter.com\/hashtag\/NOAA20?src=hash&amp;ref_src=twsrc%5Etfw\">#NOAA20<\/a> saw the <a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/volcano?src=hash&amp;ref_src=twsrc%5Etfw\">#volcano<\/a> eruption on <a href=\"https:\/\/twitter.com\/hashtag\/Hawaii?src=hash&amp;ref_src=twsrc%5Etfw\">#Hawaii<\/a>&#39;s Big Island last night. The bright spots at Pu&#39;u O&#39;o crater show the site of yesterday&#39;s earthquake and lava flows. Learn more: <a href=\"https:\/\/t.co\/aA2Tw1ZbIm\">https:\/\/t.co\/aA2Tw1ZbIm<\/a> <a href=\"https:\/\/t.co\/z8fN5feV9D\">pic.twitter.com\/z8fN5feV9D<\/a><\/p>\n<p>&mdash; NOAA Satellites (@NOAASatellites) <a href=\"https:\/\/twitter.com\/NOAASatellites\/status\/992491373432639489?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\"><a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/eruption?src=hash&amp;ref_src=twsrc%5Etfw\">#eruption<\/a> in <a href=\"https:\/\/twitter.com\/hashtag\/LeilaniEstates?src=hash&amp;ref_src=twsrc%5Etfw\">#LeilaniEstates<\/a> ended ~6:30PM last night. <a href=\"https:\/\/twitter.com\/hashtag\/Lava?src=hash&amp;ref_src=twsrc%5Etfw\">#Lava<\/a> spatter &amp; <a href=\"https:\/\/twitter.com\/hashtag\/gas?src=hash&amp;ref_src=twsrc%5Etfw\">#gas<\/a> bursts erupted from <a href=\"https:\/\/twitter.com\/hashtag\/fissure?src=hash&amp;ref_src=twsrc%5Etfw\">#fissure<\/a> for ~2 hours. Lava spread ~10m (33ft). See Descriptions &amp; updates on <a href=\"https:\/\/twitter.com\/hashtag\/HVO?src=hash&amp;ref_src=twsrc%5Etfw\">#HVO<\/a> website. Scientists monitored overnight &#8211; more updates this AM. <a href=\"https:\/\/t.co\/fXSpF9YxwX\">https:\/\/t.co\/fXSpF9YxwX<\/a> <a href=\"https:\/\/t.co\/1a6KK0cSCn\">pic.twitter.com\/1a6KK0cSCn<\/a><\/p>\n<p>&mdash; USGS Volcanoes&#x1f30b; (@USGSVolcanoes) <a href=\"https:\/\/twitter.com\/USGSVolcanoes\/status\/992411586974203904?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Here\u2019s footage of some of the lava activity inside Leilani Estates from CB photographer <a href=\"https:\/\/twitter.com\/corylumphoto?ref_src=twsrc%5Etfw\">@corylumphoto<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/bigisland?src=hash&amp;ref_src=twsrc%5Etfw\">#bigisland<\/a> <a href=\"https:\/\/t.co\/OkZz9xw6aJ\">pic.twitter.com\/OkZz9xw6aJ<\/a><\/p>\n<p>&mdash; Honolulu Civil Beat (@CivilBeat) <a href=\"https:\/\/twitter.com\/CivilBeat\/status\/992593640626180098?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">WATCH: This fissure from the <a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/Volcano?src=hash&amp;ref_src=twsrc%5Etfw\">#Volcano<\/a> eruption is spewing <a href=\"https:\/\/twitter.com\/hashtag\/lava?src=hash&amp;ref_src=twsrc%5Etfw\">#lava<\/a> and molten rock. The sound was unexpectedly thunderous. One of the most amazing things I\u2019ve ever experienced. <a href=\"https:\/\/t.co\/G27LXE2Vvq\">pic.twitter.com\/G27LXE2Vvq<\/a><\/p>\n<p>&mdash; Stephanie Elam (@StephanieElam) <a href=\"https:\/\/twitter.com\/StephanieElam\/status\/992634109406068736?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Mount <a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> on the Big Island in Hawaii erupted straight through a subdivision on Thursday. Mandatory evacuations were issued as magma gushed from the new vent, cracking roads and splitting the earth through the volcano&#39;s East Rift Zone. [THREAD] <a href=\"https:\/\/t.co\/mBG68fEe5E\">pic.twitter.com\/mBG68fEe5E<\/a><\/p>\n<p>&mdash; Capital Weather Gang (@capitalweather) <a href=\"https:\/\/twitter.com\/capitalweather\/status\/992486504479019008?ref_src=twsrc%5Etfw\">May 4, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><br \/>\n<iframe loading=\"lazy\" src=\"https:\/\/www.facebook.com\/plugins\/post.php?href=https%3A%2F%2Fwww.facebook.com%2FUSGSVolcanoes%2Fposts%2F2020876274607590&#038;width=500\" width=\"500\" height=\"388\" style=\"border:none;overflow:hidden\" scrolling=\"no\" frameborder=\"0\" allowTransparency=\"true\" allow=\"encrypted-media\"><\/iframe><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Latest <a href=\"https:\/\/twitter.com\/USGSVolcanoes?ref_src=twsrc%5Etfw\">@USGSVolcanoes<\/a> map of the 8 fissures that have formed during the current <a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> eruption: <a href=\"https:\/\/t.co\/8Y4gPq7VSY\">https:\/\/t.co\/8Y4gPq7VSY<\/a> <a href=\"https:\/\/t.co\/kqLmuIkXnP\">pic.twitter.com\/kqLmuIkXnP<\/a><\/p>\n<p>&mdash; Dr Janine Krippner (@janinekrippner) <a href=\"https:\/\/twitter.com\/janinekrippner\/status\/992894648640262144?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">The change in the Halema\u02bbuma\u02bbu Overlook Vent from yesterday (4 May) to today: <a href=\"https:\/\/t.co\/lXKYFjcyJK\">https:\/\/t.co\/lXKYFjcyJK<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> <a href=\"https:\/\/t.co\/Mmt87rS3hs\">pic.twitter.com\/Mmt87rS3hs<\/a><\/p>\n<p>&mdash; Dr Janine Krippner (@janinekrippner) <a href=\"https:\/\/twitter.com\/janinekrippner\/status\/992895859745533954?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Better NASA-JPL ARIA automatic interferogram from Copernicus Sentinel-1 acquired 23 April and 5 May 2018. Wrapped interferogram with 2.8 cm color contours. This includes both magma movement in rift and M6.9 earthquake signals making complex pattern of fringes. <a href=\"https:\/\/t.co\/m47tOLlsy1\">pic.twitter.com\/m47tOLlsy1<\/a><\/p>\n<p>&mdash; Eric Fielding (@EricFielding) <a href=\"https:\/\/twitter.com\/EricFielding\/status\/992906033403084800?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">So, why is <a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> so active?? The plumbing beneath Kilauea by <a href=\"https:\/\/twitter.com\/TheEarthStory?ref_src=twsrc%5Etfw\">@TheEarthStory<\/a> here: <a href=\"https:\/\/t.co\/WFKPHBbbpo\">https:\/\/t.co\/WFKPHBbbpo<\/a> <a href=\"https:\/\/t.co\/pT1kAY8dD8\">pic.twitter.com\/pT1kAY8dD8<\/a><\/p>\n<p>&mdash; Dr Janine Krippner (@janinekrippner) <a href=\"https:\/\/twitter.com\/janinekrippner\/status\/992900451518550016?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><br \/>\n<iframe loading=\"lazy\" src=\"https:\/\/www.facebook.com\/plugins\/video.php?href=https%3A%2F%2Fwww.facebook.com%2Flavaocean%2Fvideos%2F10216082532964071%2F&#038;show_text=0&#038;width=560\" width=\"560\" height=\"315\" style=\"border:none;overflow:hidden\" scrolling=\"no\" frameborder=\"0\" allowTransparency=\"true\" allowFullScreen=\"true\"><\/iframe><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Field photos just in: at 07:45 a.m. HST, today (May 5), lava from fissure 7 slowly advanced to the northeast on Hookapu Street. <a href=\"https:\/\/t.co\/5w1RIQyCCC\">https:\/\/t.co\/5w1RIQyCCC<\/a> <a href=\"https:\/\/t.co\/ZuG3uH5oiv\">pic.twitter.com\/ZuG3uH5oiv<\/a><\/p>\n<p>&mdash; USGS Volcanoes&#x1f30b; (@USGSVolcanoes) <a href=\"https:\/\/twitter.com\/USGSVolcanoes\/status\/992929271810211841?ref_src=twsrc%5Etfw\">May 6, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Fissure 7 from the intersection of Leilani and Makamae Streets in the Leilani Estates subdivision on K\u012blauea Volcano&#39;s lower East Rift Zone. <a href=\"https:\/\/t.co\/trIyZtTgSc\">https:\/\/t.co\/trIyZtTgSc<\/a> <a href=\"https:\/\/t.co\/3GUbAkMhTy\">pic.twitter.com\/3GUbAkMhTy<\/a><\/p>\n<p>&mdash; USGS Volcanoes&#x1f30b; (@USGSVolcanoes) <a href=\"https:\/\/twitter.com\/USGSVolcanoes\/status\/992929864947675136?ref_src=twsrc%5Etfw\">May 6, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Impressive decrease (~20cm) in change in distance between 2 GPS station near Pu\u2018u \u2018\u014c\u2018\u014d crater <a href=\"https:\/\/twitter.com\/hashtag\/KilaueaVolcano?src=hash&amp;ref_src=twsrc%5Etfw\">#KilaueaVolcano<\/a>. One station located on the north rim of the crater, the other on the south flank. Can be interpreted as deflation of the summit magma reservoir <a href=\"https:\/\/t.co\/Jgefhoizzk\">https:\/\/t.co\/Jgefhoizzk<\/a> <a href=\"https:\/\/t.co\/vIL3YlKcMm\">pic.twitter.com\/vIL3YlKcMm<\/a><\/p>\n<p>&mdash; Lucile Bruhat (@seismolucy) <a href=\"https:\/\/twitter.com\/seismolucy\/status\/992606880395546624?ref_src=twsrc%5Etfw\">May 5, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\"><a href=\"https:\/\/twitter.com\/hashtag\/Kilauea?src=hash&amp;ref_src=twsrc%5Etfw\">#Kilauea<\/a> eruption update by <a href=\"https:\/\/twitter.com\/USGSVolcanoes?ref_src=twsrc%5Etfw\">@USGSVolcanoes<\/a> <a href=\"https:\/\/t.co\/p9ZRiWGxcp\">https:\/\/t.co\/p9ZRiWGxcp<\/a><br \/>Civil defense updates and instructions: <a href=\"https:\/\/t.co\/0RBhz98iGv\">https:\/\/t.co\/0RBhz98iGv<\/a> <a href=\"https:\/\/t.co\/ISsejP6e6z\">pic.twitter.com\/ISsejP6e6z<\/a><\/p>\n<p>&mdash; Dr Janine Krippner (@janinekrippner) <a href=\"https:\/\/twitter.com\/janinekrippner\/status\/992928741532815362?ref_src=twsrc%5Etfw\">May 6, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">What is an interferogram? Learn more on the <a href=\"https:\/\/twitter.com\/IRIS_EPO?ref_src=twsrc%5Etfw\">@IRIS_EPO<\/a> website here: <a href=\"https:\/\/t.co\/pf3I4H4vYl\">https:\/\/t.co\/pf3I4H4vYl<\/a> <a href=\"https:\/\/t.co\/C5d5T119Ps\">https:\/\/t.co\/C5d5T119Ps<\/a><\/p>\n<p>&mdash; Dr Janine Krippner (@janinekrippner) <a href=\"https:\/\/twitter.com\/janinekrippner\/status\/992936879925465088?ref_src=twsrc%5Etfw\">May 6, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Want to know more on how the earthquakes can be linked to surface volcanic activity? I\u2019ve written a short piece that gives some more details: <a href=\"https:\/\/t.co\/OG222axTJY\">https:\/\/t.co\/OG222axTJY<\/a> <a href=\"https:\/\/t.co\/KoASw1xzdM\">https:\/\/t.co\/KoASw1xzdM<\/a><\/p>\n<p>&mdash; Chris Rowan (@Allochthonous) <a href=\"https:\/\/twitter.com\/Allochthonous\/status\/992962952599949312?ref_src=twsrc%5Etfw\">May 6, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<ul>\n<h2><strong><font color=\"orange\">References:<\/font><\/strong><\/h2>\n<li>Ando, M., 1979. The Hawaii Earthquake of November 29, 1975: Low Dip Angle Faulting Due to Forceful Injection of Magma in JGR, v. 84, no. B13<\/li>\n<li>Orr, T.R., et a., 2012. <a href=\"https:\/\/pubs.usgs.gov\/fs\/2012\/3127\/fs2012-3127.pdf\" rel=\"noopener\" target=\"_blank\">The Ongoing Pu\u2018u \u2018\u00d6\u2018\u00f6 Eruption of K\u00eflauea Volcano, Hawai\u2018i\u201430 Years of Eruptive Activity<\/a> in USGS Fact Sheet 2012-3127, 2013.<\/li>\n<li>Sherrod, D.R., Sinton, J.M., Watkins, S.E., and Brunt, K.M., 2007, Geologic Map of the State of Hawaii: U.S. Geological Survey Open-File Report 2007-1089, 83 p., 8 plates, scales 1:100,000 and 1:250,000, with GIS database<\/li>\n<li>Tilling, R.I., Keliker, C., and Swanson, D.A., 2010. Eruptions of Hawaiian Volcanoes\u2014Past, Present, and Future, U.S. Geological Survey, General Information Product 117, 72 pp.<\/li>\n<li>Torsvik, T.H., et al., 2017. <a href=\"https:\/\/www.nature.com\/articles\/ncomms15660\" rel=\"noopener\" target=\"_blank\">Pacific plate motion change caused the Hawaiian-Emperor Bend<\/a> in Nature Communications, DOI: 10.1038\/ncomms15660<\/li>\n<\/ul>\n","protected":false},"excerpt":{"rendered":"<div class=\"entry-summary\">\nMy USGS Earthquake Notification Service email inbox has been going on overtime. There has been a swarm of earthquakes on the southeastern part of the big island, with USGS volcanologists hypothesizing about magma movement and suggesting that an eruption may&hellip;\n<\/div>\n<div class=\"link-more\"><a href=\"https:\/\/earthjay.com\/?p=7350\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &ldquo;Earthquake-Volcanic Eruption Report: Hawai&#8217;i&rdquo;<\/span>&hellip;<\/a><\/div>\n","protected":false},"author":3,"featured_media":7380,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0},"categories":[5,6,7,26,27,39],"tags":[],"aioseo_notices":[],"jetpack_featured_media_url":"https:\/\/earthjay.com\/wp-content\/uploads\/2018\/05\/20180504_hawaii_interpretation_M35-1-scaled.jpg","_links":{"self":[{"href":"https:\/\/earthjay.com\/index.php?rest_route=\/wp\/v2\/posts\/7350"}],"collection":[{"href":"https:\/\/earthjay.com\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/earthjay.com\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/earthjay.com\/index.php?rest_route=\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/earthjay.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=7350"}],"version-history":[{"count":2,"href":"https:\/\/earthjay.com\/index.php?rest_route=\/wp\/v2\/posts\/7350\/revisions"}],"predecessor-version":[{"id":11931,"href":"https:\/\/earthjay.com\/index.php?rest_route=\/wp\/v2\/posts\/7350\/revisions\/11931"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/earthjay.com\/index.php?rest_route=\/wp\/v2\/media\/7380"}],"wp:attachment":[{"href":"https:\/\/earthjay.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=7350"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/earthjay.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=7350"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/earthjay.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=7350"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}