{"id":6990,"date":"2018-01-23T11:41:18","date_gmt":"2018-01-23T19:41:18","guid":{"rendered":"http:\/\/earthjay.com\/?p=6990"},"modified":"2023-01-23T18:21:21","modified_gmt":"2023-01-23T18:21:21","slug":"earthquake-report-gulf-of-alaska","status":"publish","type":"post","link":"https:\/\/earthjay.com\/?p=6990","title":{"rendered":"Earthquake Report: Gulf of Alaska!"},"content":{"rendered":"<p>I was asleep in bed, trying to catch up to prevent myself from getting ill, when there was a large earthquake in the Gulf of Alaska (GA), offshore of Kodiak, Alaska. When I wakened, I noticed a fb message from my friend Scott Willits notifying me of an M 8.2 earthquake in Alaska, posted at 2:20 AM local time. I immediately got up to check on this and was surprised that there was not a tsunami evacuation going on. I live in the small town of Manila (population ~700), on the North Spit (a sand spit west of Arcata and Eureka, CA). I live above 10 m in elevation and do not consider myself exposed to tsunami risks, local or distant (especially given that (1) the CSZ locked zone is mostly under land here and (2) that the part of the locked zone that is not under land is in shallow water; so our local tsunami will probably be much smaller than further north, like Crescent City or Brookings). I have been involved in tsunami education and outreach for over 15 years and prepared the first tsunami hazard map for northern CA (working with Dr. Lori Dengler and the Redwood Coast Tsunami Work Group). Needless to say, I am cogent and aware about the tsunami risk here in norcal.<\/p>\n<p><a href=\"https:\/\/earthquake.usgs.gov\/earthquakes\/eventpage\/us2000cmy3\/executive\" rel=\"noopener\" target=\"_blank\">https:\/\/earthquake.usgs.gov\/earthquakes\/eventpage\/us2000cmy3\/executive<\/a><\/p>\n<p>SO. I soon discovered that the GA earthquake happened in the Pacific plate, far from the subduction zone and that the earthquake was a strike-slip earthquake. Both of these facts explained why the sheriff had not been at my door earlier this morning. In addition, the magnitude had been adjusted to M 7.9 (no longer a Great earthquake, just a Large earthquake; <a href=\"http:\/\/www.geo.mtu.edu\/UPSeis\/magnitude.html\" rel=\"noopener noreferrer\" target=\"_blank\">earthquake classes are defined here<\/a>). However, there were some small tsunami waves observed (see below) as reported by the National Tsunami Warning Center (see social media below).<br \/>\nThis earthquake appears to be located along a reactivated fracture zone in the GA. There have only been a couple earthquakes in this region in the past century, one an M 6.0 to the east (though this M 6.0 was a thrust earthquake). The Gulf of Alaska shear zone is even further to the east and has a more active historic fault history (a pair of earthquakes in 1987-1988). The magnetic anomalies (formed when the Earth&#8217;s magnetic polarity flips) reflect a ~north-south oriented spreading ridge (the anomalies are oriented north-south in the region of today&#8217;s earthquake). There is a right-lateral offset of these magnetic anomalies located near the M 7.9 epicenter. Interesting that this right-lateral strike-slip fault (?) is also located at the intersection of the Gulf of Alaska shear zone and the 1988 M 7.8 earthquake (probably just a coincidence?). However, the 1988 M 7.8 earthquake fault plane solution can be interpreted for both fault planes (it is probably on the GA shear zone, but I don&#8217;t think that we can really tell).<br \/>\nThis is strange because the USGS fault plane is oriented east-west, leading us to interpret the fault plane solution (moment tensor or focal mechanism) as a left-lateral strike-slip earthquake. So, maybe this earthquake is a little more complicated than first presumed. The USGS fault model is constrained by seismic waves, so this is probably the correct fault (east-west).<br \/>\nI prepared an <a href=\"http:\/\/earthjay.com\/?p=3833\" rel=\"noopener noreferrer\" target=\"_blank\">Earthquake Report for the 1964 Good Friday Earthquake here<\/a>.<br \/>\n<strong><font color=\"orange\">UPDATES<\/font><\/strong> Below is a list of all the reports associated with this earthquake sequence.<\/p>\n<ul>\n<li><a href=\"http:\/\/earthjay.com\/?p=6990\">Original Report<\/a><\/li>\n<li><a href=\"http:\/\/earthjay.com\/?p=7019\">Report Update #1<\/a><\/li>\n<li><a href=\"http:\/\/earthjay.com\/?p=7038\">Report Update #2<\/a><\/li>\n<\/ul>\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 6.5. More about the plate boundary can be found in <a href=\"http:\/\/earthjay.com\/?p=3833\" rel=\"noopener noreferrer\" target=\"_blank\">that report<\/a>.<br \/>\nI plot the USGS fault plane solutions (moment tensors in blue and focal mechanisms in orange) for the M 7.9 earthquake, in addition to some relevant historic earthquakes.<\/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 noreferrer\">moment tensors<\/a> and <a href=\"http:\/\/earthquake.usgs.gov\/learn\/topics\/beachball.php\" target=\"_blank\" rel=\"noopener noreferrer\">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<li>I also include the shaking intensity contours on the map. These use the Modified Mercalli Intensity Scale (MMI; see the legend on the map). This is based upon a computer model estimate of ground motions, different from the &#8220;Did You Feel It?&#8221; estimate of ground motions that is actually based on real observations. The MMI is a qualitative measure of shaking intensity. More on the MMI scale can be found <a href=\"http:\/\/earthquake.usgs.gov\/learn\/topics\/mercalli.php\" target=\"_blank\" rel=\"noopener noreferrer\">here<\/a> and <a href=\"https:\/\/en.wikipedia.org\/wiki\/Mercalli_intensity_scale\" target=\"_blank\" rel=\"noopener noreferrer\">here<\/a>. This is based upon a computer model estimate of ground motions, different from the &#8220;Did You Feel It?&#8221; estimate of ground motions that is actually based on real observations.<\/li>\n<li>I include the slab contours plotted (<a href=\"http:\/\/www.agu.org\/pubs\/crossref\/2012\/2011JB008524.shtml\" target=\"_blank\" rel=\"noopener noreferrer\">Hayes et al., 2012<\/a>), which are contours that represent the depth to the subduction zone fault. These are mostly based upon seismicity. The depths of the earthquakes have considerable error and do not all occur along the subduction zone faults, so these slab contours are simply the best estimate for the location of the fault. Slab 2.0 is due out later this year!<\/li>\n<\/ul>\n<ul>\n<li>\n<h3><strong>I include some inset figures.<\/strong><\/h3>\n<\/li>\n<li>In the upper left corner, I place a map created by <a href=\"http:\/\/alaska.usgs.gov\/staff\/staffbio.php?employeeid=25\" target=\"_blank\" rel=\"noopener noreferrer\">Dr. Peter Haeussler, USGS<\/a>, which shows the historic earthquakes along the Alaska and Aleutian subduction zones. I place the epicenter from today&#8217;s earthquake as a cyan star.<\/li>\n<li>To the right of this map, I include first the USGS map that shows their interpretation of where the fault is (the red line) and then I include the USGS fault slip model (color = slip in meters).<\/li>\n<li>In the upper right corner is a map from IRIS that shows seismicity with color representing depth.<\/li>\n<li>In the lower right corner, I include a low angle oblique view of the subduction zone, showing how the Pacific plate is subducting beneath the North America plate.<\/li>\n<li>In the lower left corner, I include a map that shows the magnetic anomalies in the GA region. I include USGS seismicity from 1918-2018 for earthquakes M \u2265 5.5.<\/li>\n<\/ul>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180123_alaska\/20180123_alaska_interpretation.pdf\" rel=\"noopener noreferrer\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180123_alaska\/20180123_alaska_interpretation.jpg\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<ul>\n<li><font color=\"orange\"><strong>UPDATE<\/strong> 12:45 my local time<\/font><\/li>\n<li>The USGS updated their MMI contours to reflect their fault model. Below is my updated poster. I also added green dashed lines for the fracture zones related to today&#8217;s M 7.9 earthquake (on the magnetic anomaly inset map).<\/li>\n<\/ul>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180123_alaska\/20180123_alaska_interpretation_update_01.pdf\" rel=\"noopener noreferrer\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180123_alaska\/20180123_alaska_interpretation_update_01.jpg\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<ul>\n<li>These are the observations as reported by the NTWC this morning (at 4:15 AM my local time).<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180123_alaska\/20180123_alaska_79_nwtc_tsunami_observations_20180123_0415.JPG\" rel=\"noopener noreferrer\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180123_alaska\/20180123_alaska_79_nwtc_tsunami_observations_20180123_0415.JPG\" width=\"100%\" alt=\"\" \/><\/a>\n<\/ul>\n<ul>\n<li>Here is the map showing magnetic anomalies in the region of the M 7.9 earthquake. These <a href=\"https:\/\/www.ngdc.noaa.gov\/geomag\/emag2.html\" rel=\"noopener noreferrer\" target=\"_blank\">magnetic anomalies have been compiled in a global dataset here<\/a>, more about their methods can be found on their page.<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20180123_alaska\/20180123_alaska_79_local_slab_cont_19182018_EQGTE_55_mag.jpg\" rel=\"noopener noreferrer\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20180123_alaska\/20180123_alaska_79_local_slab_cont_19182018_EQGTE_55_mag.jpg\" width=\"100%\" alt=\"\" \/><\/a>\n<\/ul>\n<ul>\n<li>Here is an educational video from IRIS about the tectonics in Alaska.<\/li>\n<\/ul>\n<p><iframe loading=\"lazy\" width=\"520\" height=\"315\" src=\"https:\/\/www.youtube.com\/embed\/hEW0jMW1vbY\" frameborder=\"0\" allow=\"autoplay; encrypted-media\" allowfullscreen><\/iframe><\/p>\n<h2><strong><font color=\"orange\">Some Relevant Discussion and Figures<\/font><\/strong><\/h2>\n<ul>\n<li>Here is a map from Michael West at the Alaska Earthquake Center. This shows today&#8217;s earthquake in reference to the <a href=\"http:\/\/www.dggs.alaska.gov\/pubs\/id\/23944\" target=\"_blank\" rel=\"noopener noreferrer\">Quaternary faults and folds in Alaska: A digital database<\/a> (Koehler et al., 2012). Dr. Rick Koehler is currently at the <a href=\"http:\/\/www.nbmg.unr.edu\/Staff\/Koehler.html\" target=\"_blank\" rel=\"noopener noreferrer\">University of Nevada Reno and The Nevada Bureau of Mines and Geology<\/a>. This is the map poster from Koehler et al. (2012). The link is to a 63 MB pdf file.<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20160402_alaska\/mp141_sh001.pdf\" target=\"_blank\" rel=\"noopener noreferrer\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20160402_alaska\/mp141_sh001_thumb_small.jpg\" width=\"100%\" alt=\"\" \/><\/a>\n<\/ul>\n<ul>\n<li>Here is a map for the earthquakes of magnitude greater than or equal to M 7.0 between 1900 and 2016. This is the <a href=\"http:\/\/tinyurl.com\/gq78uz4\" target=\"_blank\" rel=\"noopener noreferrer\">USGS query that I used to make this map<\/a>. One may locate the USGS web pages for all the earthquakes on this map by following that link.<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20160124_alaska\/1900_2016_alaska_interpretation.pdf\" target=\"_blank\" rel=\"noopener noreferrer\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20160124_alaska\/1900_2016_alaska_interpretation.jpg\" width=\"100%\" alt=\"\" \/><\/a>\n<\/ul>\n<ul>\n<li>This is a map from <a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/haeussler_1964_geophysical_advances_1964_alaska.pdf\" target=\"_blank\" rel=\"noopener noreferrer\">Haeussler et al. (2014)<\/a>. The region in red shows the area that subsided and the area in blue shows the region that uplifted during the earthquake. These regions were originally measured in the field by George Plafker and published in several documents, including this <a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/plafker_1969_tectonics_1964_alaska_earthquake.pdf\" target=\"_blank\" rel=\"noopener noreferrer\">USGS Professional Paper<\/a> (Plafker, 1969). I present <a href=\"http:\/\/earthjay.com\/?p=3833\" target=\"_blank\" rel=\"noopener noreferrer\">more information about the 1964 Good Friday Earthquake here<\/a>.<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/1964_red_blue_up_down.jpg\" target=\"_blank\" rel=\"noopener noreferrer\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/1964_red_blue_up_down.jpg\" width=\"100%\" alt=\"\" \/><\/a>\n<\/ul>\n<ul>\n<li>Here is a cross section showing the differences of vertical deformation between the coseismic (during the earthquake) and interseismic (between earthquakes).<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/plafker_eq_cycle.jpg\" target=\"_blank\" rel=\"noopener noreferrer\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/plafker_eq_cycle.jpg\" width=\"100%\" alt=\"\" \/><\/a>\n<\/ul>\n<ul>\n<li>Here is a figure recently published in the 5th International Conference of IGCP 588 by the <a href=\"http:\/\/www.dggs.alaska.gov\" target=\"_blank\" rel=\"noopener noreferrer\">Division of Geological and Geophysical Surveys<\/a>, Dept. of Natural Resources, State of Alaska (State of Alaska, 2015). This is derived from a figure published originally by Plafker (1969). There is a cross section included that shows how the slip was distributed along upper plate faults (e.g. the Patton Bay and Middleton Island faults).<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/igcp_2015_seismic_nonseismic_influences_coastal_change_alaska_page_96_fig_421.pdf\" target=\"_blank\" rel=\"noopener noreferrer\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/igcp_2015_seismic_nonseismic_influences_coastal_change_alaska_page_96_fig_421.jpg\" width=\"100%\" alt=\"\" \/><\/a>\n<\/ul>\n<ul>\n<li>Here is an animation that shows earthquakes of magnitude > 6.5 for the period from 1900-2016. Above is a map showing the region and below is the animation. This is the <a href=\"http:\/\/tinyurl.com\/hyuabdr\" target=\"_blank\" rel=\"noopener noreferrer\">URL for the USGS query<\/a> that I used to make this animation in Google Earth.<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/1900_2016_alaska_EQ_GTE_M_65_GE_map.JPG\" target=\"_blank\" rel=\"noopener noreferrer\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/1900_2016_alaska_EQ_GTE_M_65_GE_map.JPG\" width=\"100%\" alt=\"\" \/><\/a><\/p>\n<li>Here is a <a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/1900_2016_alaska_EQ_GTE_65.mp4\" target=\"_blank\" rel=\"noopener noreferrer\">link to the file<\/a> for the embedded video below (5 MB mp4)<\/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-6990-1\" width=\"640\" height=\"360\" preload=\"metadata\" controls=\"controls\"><source type=\"video\/mp4\" src=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/1900_2016_alaska_EQ_GTE_65.mp4?_=1\" \/><a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/1900_2016_alaska_EQ_GTE_65.mp4\">http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/1900_2016_alaska_EQ_GTE_65.mp4<\/a><\/video><\/div>\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. Many of the earthquakes people are familiar with in the Mendocino triple junction region are either compressional or strike slip. The following three animations are from <a href=\"http:\/\/www.iris.edu\/hq\/programs\/education_and_outreach\/animations\/2\" target=\"_blank\" rel=\"noopener noreferrer\">IRIS<\/a>.<\/li>\n<li>Strike Slip:<\/li>\n<p><iframe loading=\"lazy\" width=\"420\" height=\"315\" src=\"https:\/\/www.youtube.com\/embed\/MrrLJ4vXHCs\" frameborder=\"0\" allowfullscreen><\/iframe><\/p>\n<li>Compressional:<\/li>\n<p><iframe loading=\"lazy\" width=\"420\" height=\"315\" src=\"https:\/\/www.youtube.com\/embed\/4b81nXSVA34\" frameborder=\"0\" allowfullscreen><\/iframe><\/p>\n<li>Extensional:<\/li>\n<p><iframe loading=\"lazy\" width=\"420\" height=\"315\" src=\"https:\/\/www.youtube.com\/embed\/tJDnfT1pqhQ\" frameborder=\"0\" allowfullscreen><\/iframe>\n<\/ul>\n<ul>\n<li>This figure shows what a transform plate boundary fault is. Looking down from outer space, the crust on either side of the fault moves side-by-side. When one is standing on the ground, on one side of the fault, looking across the fault as it moves&#8230; If the crust on the other side of the fault moves to the right, the fault is a &#8220;right lateral&#8221; strike slip fault. The Mendocino and San Andreas faults are right-lateral (dextral) strike-slip faults. I believe this is from <a href=\"https:\/\/www.pearsonhighered.com\/lutgens-12e-info\/sample-chapter\/echapter\/files\/assets\/basic-html\/page18.html\" target=\"_blank\" rel=\"noopener noreferrer\">Pearson Higher Ed<\/a>.<\/li>\n<p><a href=\"http:\/\/earthjay.com\/earthquakes\/20150128_ferndale\/transform_faults_MAR.JPG\" target=\"_blank\" rel=\"noopener noreferrer\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/20150128_ferndale\/transform_faults_MAR.JPG\" width=\"100%\" alt=\"\" \/><\/a>\n<\/ul>\n<ul>\n<li>For more on the graphical representation of moment tensors and focal mechnisms, check this <a href=\"http:\/\/www.iris.edu\/hq\/programs\/education_and_outreach\/animations\/25\" target=\"_blank\" rel=\"noopener noreferrer\">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 noreferrer\" target=\"_blank\"><br \/>\n<img decoding=\"async\" src=\"http:\/\/earthjay.com\/earthquakes\/Plate_Tectonics_2011_page_23_fault_plane_solutions.jpg\" width=\"100%\" alt=\"\" \/><\/a>\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\">[Top Story] Magnitude 7.9 Earthquake Gulf of Alaska. <a href=\"https:\/\/t.co\/SbsoXcGHU9\">https:\/\/t.co\/SbsoXcGHU9<\/a> <a href=\"https:\/\/t.co\/VkTNhiwx7l\">pic.twitter.com\/VkTNhiwx7l<\/a><\/p>\n<p>&mdash; USGS (@USGS) <a href=\"https:\/\/twitter.com\/USGS\/status\/955858166444683264?ref_src=twsrc%5Etfw\">January 23, 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\">M=7.9 Alaska earthquake strikes off the coast of Kodiak Island, triggering a tsunami and questions | <a href=\"https:\/\/t.co\/6d516uWWTP\">https:\/\/t.co\/6d516uWWTP<\/a> <a href=\"https:\/\/t.co\/n3JIhSFClU\">https:\/\/t.co\/n3JIhSFClU<\/a><\/p>\n<p>&mdash; Ross S Stein (@rstein357) <a href=\"https:\/\/twitter.com\/rstein357\/status\/955866897332842496?ref_src=twsrc%5Etfw\">January 23, 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\">Glad this earthquake was on a strike-slip fault, about 90 km from the  subduction trench where the tsunamigenic megathrust earthquakes occur.  Oceanic strike-slip faults are shallow (~50km) so this must have ruptured along a very long fault of ~200 km or multiple faults segments. <a href=\"https:\/\/t.co\/q8iOKGxGW9\">pic.twitter.com\/q8iOKGxGW9<\/a><\/p>\n<p>&mdash; Kasey Aderhold (@kaseyaderhold) <a href=\"https:\/\/twitter.com\/kaseyaderhold\/status\/955817413634793472?ref_src=twsrc%5Etfw\">January 23, 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\">.Map of sea-floor geophysical features in Gulf of Alaska from a paper in 1973 shows a number of east-west trending fracture zones in Pacific plate. Possible that today&#39;s M7.9 earthquake occurred along one of these &#8211; reasonably consistent with faulting mechanism from seismic data <a href=\"https:\/\/t.co\/jV8t0bhUkw\">pic.twitter.com\/jV8t0bhUkw<\/a><\/p>\n<p>&mdash; Stephen Hicks (@seismo_steve) <a href=\"https:\/\/twitter.com\/seismo_steve\/status\/955752011542224897?ref_src=twsrc%5Etfw\">January 23, 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\">Excellent story from <a href=\"https:\/\/twitter.com\/nytimes?ref_src=twsrc%5Etfw\">@nytimes<\/a> of last night\u2019s earthquake offshore Alaska and small, resultant tsunami. <a href=\"https:\/\/t.co\/DoQcPGr1XZ\">https:\/\/t.co\/DoQcPGr1XZ<\/a><\/p>\n<p>&mdash; The TsunamiZone (@thetsunamizone) <a href=\"https:\/\/twitter.com\/thetsunamizone\/status\/955884136010416128?ref_src=twsrc%5Etfw\">January 23, 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\">This mornings Alaska M7.9 earthquake felt in Costa Rica with my <a href=\"https:\/\/twitter.com\/raspishake?ref_src=twsrc%5Etfw\">@raspishake<\/a>. <a href=\"https:\/\/t.co\/z0qUOMgIJV\">pic.twitter.com\/z0qUOMgIJV<\/a><\/p>\n<p>&mdash; Benjamin Martin (@ben7230) <a href=\"https:\/\/twitter.com\/ben7230\/status\/955798650013306881?ref_src=twsrc%5Etfw\">January 23, 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\">It took nearly 7 hours for our Middle School M7.9 <a href=\"https:\/\/twitter.com\/hashtag\/Alaska?src=hash&amp;ref_src=twsrc%5Etfw\">#Alaska<\/a> seismogram to scroll enough to show full amplitude of these large <a href=\"https:\/\/twitter.com\/hashtag\/Earthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#Earthquake<\/a> traces! Another <a href=\"https:\/\/twitter.com\/hashtag\/STEM?src=hash&amp;ref_src=twsrc%5Etfw\">#STEM<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/TeachableMoment?src=hash&amp;ref_src=twsrc%5Etfw\">#TeachableMoment<\/a> thanks to funding from <a href=\"https:\/\/twitter.com\/IRIS_EPO?ref_src=twsrc%5Etfw\">@IRIS_EPO<\/a> &amp; <a href=\"https:\/\/twitter.com\/IRIS_quakes?ref_src=twsrc%5Etfw\">@IRIS_quakes<\/a> It&#39;s why <a href=\"https:\/\/twitter.com\/hashtag\/WhyEarthScienceIsTheBestSubject?src=hash&amp;ref_src=twsrc%5Etfw\">#WhyEarthScienceIsTheBestSubject<\/a> <a href=\"https:\/\/t.co\/67AnOT6mmr\">pic.twitter.com\/67AnOT6mmr<\/a><\/p>\n<p>&mdash; Dave Curry (@CarlSaganRox) <a href=\"https:\/\/twitter.com\/CarlSaganRox\/status\/955838225674797056?ref_src=twsrc%5Etfw\">January 23, 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=8.0, GULF OF ALASKA (Depth: 17 km), 2018\/01\/23 09:31:40 UTC &#8211; Full details here: <a href=\"https:\/\/t.co\/lJnOdzjhs5\">https:\/\/t.co\/lJnOdzjhs5<\/a> <a href=\"https:\/\/t.co\/S9p9wHXrZo\">pic.twitter.com\/S9p9wHXrZo<\/a><\/p>\n<p>&mdash; Earthquakes (@geoscope_ipgp) <a href=\"https:\/\/twitter.com\/geoscope_ipgp\/status\/955746923197161473?ref_src=twsrc%5Etfw\">January 23, 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\">Tue Jan 23 11:18:49 UTC 2018  event picture <a href=\"https:\/\/t.co\/ZpFFEWbkvf\">pic.twitter.com\/ZpFFEWbkvf<\/a><\/p>\n<p>&mdash; NWS Tsunami Alerts (@NWS_NTWC) <a href=\"https:\/\/twitter.com\/NWS_NTWC\/status\/955761737223016449?ref_src=twsrc%5Etfw\">January 23, 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\">Possible strike-slip FirstMoMech: Mw7.6 <a href=\"https:\/\/twitter.com\/hashtag\/earthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#earthquake<\/a> Gulf of Alaska <a href=\"https:\/\/t.co\/kCIw9Vypa6\">https:\/\/t.co\/kCIw9Vypa6<\/a>  <a href=\"https:\/\/twitter.com\/ALomaxNet?ref_src=twsrc%5Etfw\">@ALomaxNet<\/a> <a href=\"https:\/\/t.co\/dllZXOwBj8\">pic.twitter.com\/dllZXOwBj8<\/a><\/p>\n<p>&mdash; Anthony Lomax &#x1f30d; (@ALomaxNet) <a href=\"https:\/\/twitter.com\/ALomaxNet\/status\/955737952524566528?ref_src=twsrc%5Etfw\">January 23, 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\">GFZ Mww gives M7.8 and seems to confirm strike-slip faulting <a href=\"https:\/\/t.co\/hN2Fju5BCW\">https:\/\/t.co\/hN2Fju5BCW<\/a> <a href=\"https:\/\/t.co\/RsOpLVa5Lj\">pic.twitter.com\/RsOpLVa5Lj<\/a><\/p>\n<p>&mdash; Anthony Lomax &#x1f30d; (@ALomaxNet) <a href=\"https:\/\/twitter.com\/ALomaxNet\/status\/955740937241669633?ref_src=twsrc%5Etfw\">January 23, 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\">M=7.9 Alaska earthquake strikes off the coast of Kodiak Island, triggering a tsunami and questions | <a href=\"https:\/\/twitter.com\/temblor?ref_src=twsrc%5Etfw\">@temblor<\/a> | <a href=\"https:\/\/t.co\/LumawcrkQL\">https:\/\/t.co\/LumawcrkQL<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/AlaskaEarthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#AlaskaEarthquake<\/a> <a href=\"https:\/\/t.co\/BTZ3bpw7Cl\">pic.twitter.com\/BTZ3bpw7Cl<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/955871421074427904?ref_src=twsrc%5Etfw\">January 23, 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\">Tsunami waves from M7.9 outer-rise earthquake detected at Kodiak tide station <a href=\"https:\/\/t.co\/CmjuLqGQ6A\">pic.twitter.com\/CmjuLqGQ6A<\/a><\/p>\n<p>&mdash; Rob Witter (@WitterBanter) <a href=\"https:\/\/twitter.com\/WitterBanter\/status\/955784539028074502?ref_src=twsrc%5Etfw\">January 23, 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\">Current location estimate of magnitude~8 offshore Alaska earthquake 10 mins ago seems to indicate that it occurred within the oceanic Pacific plate before it subducts at the trench. Possibly a normal faulting event? Significant tsunami risk. <a href=\"https:\/\/t.co\/G5BL1HwLi3\">pic.twitter.com\/G5BL1HwLi3<\/a><\/p>\n<p>&mdash; Stephen Hicks (@seismo_steve) <a href=\"https:\/\/twitter.com\/seismo_steve\/status\/955737316525568000?ref_src=twsrc%5Etfw\">January 23, 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\">Powerful earthquake jolts Alaska awake with middle-of-the-night tsunami warning, which was canceled after a few intense hours. <a href=\"https:\/\/t.co\/1EOVhSUa40\">https:\/\/t.co\/1EOVhSUa40<\/a><\/p>\n<p>&mdash; AP West Region (@APWestRegion) <a href=\"https:\/\/twitter.com\/APWestRegion\/status\/955855913608515584?ref_src=twsrc%5Etfw\">January 23, 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 explore the seismicity of <a href=\"https:\/\/twitter.com\/hashtag\/Alaska?src=hash&amp;ref_src=twsrc%5Etfw\">#Alaska<\/a>? View past and current <a href=\"https:\/\/twitter.com\/hashtag\/earthquakes?src=hash&amp;ref_src=twsrc%5Etfw\">#earthquakes<\/a> using our free Interactive Earthquake Browser. You can even look at earthquake locations in 3D! <a href=\"https:\/\/t.co\/s1XIzHPEQY\">https:\/\/t.co\/s1XIzHPEQY<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/AlaskaQuake?src=hash&amp;ref_src=twsrc%5Etfw\">#AlaskaQuake<\/a> <a href=\"https:\/\/t.co\/rjHiywdcKi\">pic.twitter.com\/rjHiywdcKi<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/955765208781336576?ref_src=twsrc%5Etfw\">January 23, 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\">.Yup, a preliminary movie of the <a href=\"https:\/\/twitter.com\/hashtag\/Alaska?src=hash&amp;ref_src=twsrc%5Etfw\">#Alaska<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/earthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#earthquake<\/a> rupture (&quot;back projection&quot;) indicates that the rupture propagates to the east and west of its starting point (epicentre). Agrees with faulting mechanism and plate fabric (fracture zones). Via <a href=\"https:\/\/twitter.com\/IRIS_EPO?ref_src=twsrc%5Etfw\">@IRIS_EPO<\/a> <a href=\"https:\/\/twitter.com\/alexanderhutko?ref_src=twsrc%5Etfw\">@alexanderhutko<\/a> <a href=\"https:\/\/t.co\/TmDdzwHb36\">pic.twitter.com\/TmDdzwHb36<\/a><\/p>\n<p>&mdash; Stephen Hicks (@seismo_steve) <a href=\"https:\/\/twitter.com\/seismo_steve\/status\/955771740331958272?ref_src=twsrc%5Etfw\">January 23, 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\">Alaska <a href=\"https:\/\/twitter.com\/hashtag\/tsunami?src=hash&amp;ref_src=twsrc%5Etfw\">#tsunami<\/a> just passed <a href=\"https:\/\/twitter.com\/Ocean_Networks?ref_src=twsrc%5Etfw\">@Ocean_Networks<\/a> bottom pressure station at Clayoquot Slope: 3-cm sea level drop; not big but there.<a href=\"https:\/\/t.co\/b27CdUo3as\">https:\/\/t.co\/b27CdUo3as<\/a> <a href=\"https:\/\/t.co\/T6A8FT2SdT\">pic.twitter.com\/T6A8FT2SdT<\/a><\/p>\n<p>&mdash; Martin Scherwath (@mscherwath) <a href=\"https:\/\/twitter.com\/mscherwath\/status\/955779841223249920?ref_src=twsrc%5Etfw\">January 23, 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\/PointArena?src=hash&amp;ref_src=twsrc%5Etfw\">#PointArena<\/a> tide gauge @ Arena Cove showing a small <a href=\"https:\/\/twitter.com\/hashtag\/tsunami?src=hash&amp;ref_src=twsrc%5Etfw\">#tsunami<\/a> this morning. This small tsunami is working its way down the coast.<a href=\"https:\/\/twitter.com\/hashtag\/cawx?src=hash&amp;ref_src=twsrc%5Etfw\">#cawx<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/earthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#earthquake<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/alaska?src=hash&amp;ref_src=twsrc%5Etfw\">#alaska<\/a> <a href=\"https:\/\/t.co\/bizkraSBxs\">pic.twitter.com\/bizkraSBxs<\/a><\/p>\n<p>&mdash; NWS Bay Area (@NWSBayArea) <a href=\"https:\/\/twitter.com\/NWSBayArea\/status\/955819319954468865?ref_src=twsrc%5Etfw\">January 23, 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\">Updating some earlier tide-gauge screenshots by <a href=\"https:\/\/twitter.com\/theearthquakes?ref_src=twsrc%5Etfw\">@theearthquakes<\/a> and <a href=\"https:\/\/twitter.com\/TTremblingEarth?ref_src=twsrc%5Etfw\">@TTremblingEarth<\/a>: can see tsunami arriving on Kodiak Island as up to 20cm fluctuations superimposed on rising tide. <a href=\"https:\/\/t.co\/k8110ewlcV\">https:\/\/t.co\/k8110ewlcV<\/a> <a href=\"https:\/\/t.co\/mJHaszKGE9\">pic.twitter.com\/mJHaszKGE9<\/a><\/p>\n<p>&mdash; Chris Rowan (@Allochthonous) <a href=\"https:\/\/twitter.com\/Allochthonous\/status\/955784770398629888?ref_src=twsrc%5Etfw\">January 23, 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\">Check out the surface waves from the 8.2 (!!) in Alaska going through Lincoln Nebraska right now live (9:50UTC) <a href=\"https:\/\/t.co\/LSGCcIbF1j\">https:\/\/t.co\/LSGCcIbF1j<\/a><\/p>\n<p>&mdash; Austin Elliott (@TTremblingEarth) <a href=\"https:\/\/twitter.com\/TTremblingEarth\/status\/955739547895201792?ref_src=twsrc%5Etfw\">January 23, 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\">Regarding aftershocks: The largest is ~M5 as of 2 hours into the sequence. It looks like the aftershocks extend North-South, suggesting the fault ruptured along along a North-South oriented fault.<\/p>\n<p>&mdash; AK Earthquake Center (@AKearthquake) <a href=\"https:\/\/twitter.com\/AKearthquake\/status\/955768339187490816?ref_src=twsrc%5Etfw\">January 23, 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 Are 4 Levels of Tsunami Messaging? Warning &gt; Advisory &gt; Watch &gt; Info Statement. Find Out What they Mean. Learn What a Tsunami Is and Be Prepared Before any Potential <a href=\"https:\/\/twitter.com\/hashtag\/tsunami?src=hash&amp;ref_src=twsrc%5Etfw\">#tsunami<\/a> Strikes. <a href=\"https:\/\/twitter.com\/NWS_NTWC?ref_src=twsrc%5Etfw\">@NWS_NTWC<\/a> Click here <a href=\"https:\/\/t.co\/F6Z7MhIvRv\">https:\/\/t.co\/F6Z7MhIvRv<\/a>\u2026 <a href=\"https:\/\/t.co\/TaUycap87b\">pic.twitter.com\/TaUycap87b<\/a><\/p>\n<p>&mdash; Cal OES (@Cal_OES) <a href=\"https:\/\/twitter.com\/Cal_OES\/status\/955768735926665216?ref_src=twsrc%5Etfw\">January 23, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-video\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Watch the earthquake waves from the M7.9 Alaska earthquake cross the USArray (<a href=\"https:\/\/t.co\/lfcuOauaVB\">https:\/\/t.co\/lfcuOauaVB<\/a>)!  <a href=\"https:\/\/twitter.com\/hashtag\/AlaskaEarthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#AlaskaEarthquake<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/earthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#earthquake<\/a> <a href=\"https:\/\/t.co\/SoZMmJHvCU\">https:\/\/t.co\/SoZMmJHvCU<\/a> <a href=\"https:\/\/t.co\/jrcGL5xvg9\">pic.twitter.com\/jrcGL5xvg9<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/955901175848755201?ref_src=twsrc%5Etfw\">January 23, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-video\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Watch the earthquake waves from the M7.9 Alaska earthquake cross the USArray (<a href=\"https:\/\/t.co\/lfcuOauaVB\">https:\/\/t.co\/lfcuOauaVB<\/a>)!  <a href=\"https:\/\/twitter.com\/hashtag\/AlaskaEarthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#AlaskaEarthquake<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/earthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#earthquake<\/a> <a href=\"https:\/\/t.co\/SoZMmJHvCU\">https:\/\/t.co\/SoZMmJHvCU<\/a> <a href=\"https:\/\/t.co\/jrcGL5xvg9\">pic.twitter.com\/jrcGL5xvg9<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/955901175848755201?ref_src=twsrc%5Etfw\">January 23, 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\">IRIS Special Event page for the M7.9 <a href=\"https:\/\/twitter.com\/hashtag\/AlaskaEarthquake?src=hash&amp;ref_src=twsrc%5Etfw\">#AlaskaEarthquake<\/a> <a href=\"https:\/\/t.co\/7XDDdb0IBb\">https:\/\/t.co\/7XDDdb0IBb<\/a> (Figure from the <a href=\"https:\/\/twitter.com\/USGS?ref_src=twsrc%5Etfw\">@USGS<\/a>) <a href=\"https:\/\/t.co\/NJKaN3EM7H\">pic.twitter.com\/NJKaN3EM7H<\/a><\/p>\n<p>&mdash; IRIS Earthquake Sci (@IRIS_EPO) <a href=\"https:\/\/twitter.com\/IRIS_EPO\/status\/955901597380378624?ref_src=twsrc%5Etfw\">January 23, 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\">Many seismic stations in Alaska operate multiple types of instruments to fully record the seismic wavefield. Here are records from the <a href=\"https:\/\/twitter.com\/IRIS_EPO?ref_src=twsrc%5Etfw\">@IRIS_EPO<\/a> Global Seismographic Network station on Kodiak Island, 280 km from the source. <a href=\"https:\/\/t.co\/JJAlhUKYSe\">pic.twitter.com\/JJAlhUKYSe<\/a><\/p>\n<p>&mdash; Andy Frassetto (@drrocks1982) <a href=\"https:\/\/twitter.com\/drrocks1982\/status\/955891613548544000?ref_src=twsrc%5Etfw\">January 23, 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\">This morning&#39;s  7.9 earthquake occurred along a strike-slip fault. The horizontal movement of the two plates in a strike-slip fault, typically limits the threat of tsunami&#39;s <a href=\"https:\/\/t.co\/o7kgwNHqxS\">pic.twitter.com\/o7kgwNHqxS<\/a><\/p>\n<p>&mdash; Greg Diamond (@gdimeweather) <a href=\"https:\/\/twitter.com\/gdimeweather\/status\/955787925563887616?ref_src=twsrc%5Etfw\">January 23, 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\">If you missed my posts from earlier: <a href=\"https:\/\/twitter.com\/hashtag\/Kusatsu?src=hash&amp;ref_src=twsrc%5Etfw\">#Kusatsu<\/a> in Japan erupts, killing one &#8211; <a href=\"https:\/\/t.co\/guwE7VM9DL\">https:\/\/t.co\/guwE7VM9DL<\/a> and a M7.9 earthquakes strikes off Alaska, but luckily doesn\u2019t generate a tsunami: <a href=\"https:\/\/t.co\/ff8dpsGHsh\">https:\/\/t.co\/ff8dpsGHsh<\/a><\/p>\n<p>&mdash; Erik Klemetti (@eruptionsblog) <a href=\"https:\/\/twitter.com\/eruptionsblog\/status\/955915618632589313?ref_src=twsrc%5Etfw\">January 23, 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>Alaska | Kamchatka | Kurile<\/font><\/strong><\/h2>\n<h3>General Overview<\/h3>\n<li><a href=\"http:\/\/earthjay.com\/?p=5190\">Summary of the 1964 Earthquake<\/a><\/li>\n<h3>Earthquake Reports<\/h3>\n<ul>\n<li>2018.01.23 <a href=\"http:\/\/earthjay.com\/?p=6990\">M 7.9 Gulf of Alaska<\/a><\/li>\n<li>2018.01.23 <a href=\"http:\/\/earthjay.com\/?p=7019\">M 7.9 Gulf of Alaska<\/a> UPDATE #1<\/li>\n<li>2018.01.23 <a href=\"http:\/\/earthjay.com\/?p=7038\">M 7.9 Gulf of Alaska<\/a> UPDATE #2<\/li>\n<\/ul>\n<ul>\n<li>2017.07.17 <a href=\"http:\/\/earthjay.com\/?p=5607\">M 7.7 Aleutians<\/a><\/li>\n<li>2017.07.17 <a href=\"http:\/\/earthjay.com\/?p=5625\">M 7.7 Aleutians<\/a> UPDATE #1<\/li>\n<li>2017.06.02 <a href=\"http:\/\/earthjay.com\/?p=5540\">M 6.8 Aleutians<\/a><\/li>\n<\/ul>\n<ul>\n<li>2017.05.08 <a href=\"http:\/\/earthjay.com\/?p=5366\">M 6.2 Aleutians<\/a><\/li>\n<li>2017.05.01 <a href=\"http:\/\/earthjay.com\/?p=5345\">M 6.3 British Columbia<\/a><\/li>\n<li>2017.03.29 <a href=\"http:\/\/earthjay.com\/?p=5200\">M 6.6 Kamchatka<\/a><\/li>\n<li>2017.03.02 <a href=\"http:\/\/earthjay.com\/?p=5127\">M 5.5 Alaska<\/a><\/li>\n<\/ul>\n<ul>\n<li>2016.09.05 <a href=\"http:\/\/earthjay.com\/?p=4303\">M 6.3 Bering Kresla<\/a> (west of Aleutians)<\/li>\n<li>2016.04.13 <a href=\"http:\/\/earthjay.com\/?p=3938\" target=\"_blank\" rel=\"noopener noreferrer\">M 5.7 &#038; 6.4 Kamchatka<\/a><\/li>\n<li>2016.04.02 <a href=\"http:\/\/earthjay.com\/?p=3880\">M 6.2 Alaska Peninsula<\/a><\/li>\n<li>2016.03.27 <a href=\"http:\/\/earthjay.com\/?p=3839\">M 5.7 Aleutians<\/a><\/li>\n<li>2016.03.12 <a href=\"http:\/\/earthjay.com\/?p=3777\">M 6.3 Aleutians<\/a><\/li>\n<li>2016.01.29 <a href=\"http:\/\/earthjay.com\/?p=3678\">M 7.2 Kamchatka<\/a><\/li>\n<li>2016.01.24 <a href=\"http:\/\/earthjay.com\/?p=3589\">M 7.1 Alaska<\/a><\/li>\n<\/ul>\n<ul>\n<li>2015.11.09 <a href=\"http:\/\/earthjay.com\/?p=3195\">M 6.2 Aleutians<\/a><\/li>\n<li>2015.11.02 <a href=\"http:\/\/earthjay.com\/?p=3143\">M 5.9 Aleutians<\/a><\/li>\n<li>2015.11.02 <a href=\"http:\/\/earthjay.com\/?p=3147\">M 5.9 Aleutians (update)<\/a><\/li>\n<li>2015.07.27 <a href=\"http:\/\/earthjay.com\/?p=2737\">M 6.9 Aleutians<\/a><\/li>\n<li>2015.05.29 <a href=\"http:\/\/earthjay.com\/?p=2551\">M 6.7 Alaska Peninsula<\/a><\/li>\n<li>2015.05.29 <a href=\"http:\/\/earthjay.com\/?p=2559\">M 6.7 Alaska Peninsula (animations)<\/a><\/li>\n<\/ul>\n<ul>\n<li>1964.03.27 <a href=\"http:\/\/earthjay.com\/?p=3833\">M 9.2 Good Friday<\/a><\/li>\n<\/ul>\n<\/ul>\n<ul>\n<h2><strong><font color=\"orange\">References:<\/font><\/strong><\/h2>\n<li>Atwater, B.F., Yamaguchi, D.K., Bondevik, S., Barnhardt, W.A., Amidon, L.J., Benson, B.E., Skjerdal, G., Shulene, J.A., and Nanalyama ,F., 2001. <a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/atwater_etal_2001_resettling_1964.pdf\" target=\"_blank\" rel=\"noopener noreferrer\">Rapid resetting of an estuarine recorder of the 1964 Alaska earthquake<\/a> in Geology, v. 113, no. 9, p. 1193-1204.<\/li>\n<li>Benz, H.M., Tarr, A.C., Hayes, G.P., Villase\u00f1or, Antonio, Hayes, G.P., Furlong, K.P., Dart, R.L., and Rhea, Susan, 2011. <a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/OF10_1083_B.pdf\" target=\"_blank\" rel=\"noopener noreferrer\">Seismicity of the Earth 1900\u20132010 Aleutian arc and vicinity<\/a>: U.S. Geological Survey Open-File Report 2010\u20131083-B, scale 1:5,000,000.<\/li>\n<li>Frisch, W., Meschede, M., Blakey, R., 2011. Plate Tectonics, Springer-Verlag, London, 213 pp.<\/li>\n<li>Hayes, G.P., Wald, D.J., and Johnson, R.L., 2012. <a href=\"http:\/\/www.agu.org\/pubs\/crossref\/2012\/2011JB008524.shtml\" target=\"_blank\" rel=\"noopener noreferrer\">Slab1.0: A three-dimensional model of global subduction zone geometries<\/a> in, J. Geophys. Res., 117, B01302, doi:10.1029\/2011JB008524<\/li>\n<li>Haeussler, P., Leith, W., Wald, D., Filson, J., Wolfe, C., and Applegate, D., 2014. <a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/haeussler_1964_geophysical_advances_1964_alaska.pdf\" target=\"_blank\" rel=\"noopener noreferrer\">Geophysical Advances Triggered by the 1964 Great Alaska Earthquake<\/a> in EOS, Transactions, American Geophysical Union, v. 95, no. 17, p. 141-142.<\/li>\n<li>Koehler, R.D., Farrell, Rebecca-Ellen, Burns, P.A.C., and Combellick, R.A., 2012. <a href=\"http:\/\/www.dggs.alaska.gov\/pubs\/id\/23944\" target=\"_blank\" rel=\"noopener noreferrer\">Quaternary faults and folds in Alaska: A digital database<\/a>, in Koehler, R.D., <a href=\"http:\/\/www.dggs.alaska.gov\/pubs\/id\/24956\" target=\"_blank\" rel=\"noopener noreferrer\">Quaternary Faults and Folds (QFF): Alaska Division of Geological &#038; Geophysical Surveys Miscellaneous Publication 141<\/a>, 31 p., 1 sheet, scale 1:3,700,000. doi:10.14509\/23944<\/li>\n<li>Plafker, G., 1969. <a href=\"http:\/\/earthjay.com\/earthquakes\/19640327_alaska\/plafker_1969_tectonics_1964_alaska_earthquake.pdf\" target=\"_blank\" rel=\"noopener noreferrer\">Tectonics of the March 27, 1964 Alaska earthquake<\/a>: U.S. Geological Survey Professional Paper 543\u2013I, 74 p., 2 sheets, scales 1:2,000,000 and 1:500,000, http:\/\/pubs.usgs.gov\/pp\/0543i\/.<\/li>\n<li>Plafker, G., 1972. <a href=\"http:\/\/onlinelibrary.wiley.com\/doi\/10.1029\/JB077i005p00901\/full\" target=\"_blank\" rel=\"noopener noreferrer\">Alaskan earthquake of 1964 and Chilean earthquake of 1960: Implications for arc tectonics<\/a> in Journal of Geophysical Research, v. 77, p. 901-925.<\/li>\n<li>Saltus, R.W., and Barnett, A., 2000. <a href=\"http:\/\/pubs.usgs.gov\/of\/2000\/ofr-00-0365\/report.htm\" target=\"_blank\" rel=\"noopener noreferrer\">Eastern Aleutian Volcanic Arc Digital Model<\/a> &#8211; Version 1.0: U.S. Geological Survey Open-File Report 00<\/li>\n<\/ul>\n","protected":false},"excerpt":{"rendered":"<div class=\"entry-summary\">\nI was asleep in bed, trying to catch up to prevent myself from getting ill, when there was a large earthquake in the Gulf of Alaska (GA), offshore of Kodiak, Alaska. When I wakened, I noticed a fb message from&hellip;\n<\/div>\n<div class=\"link-more\"><a href=\"https:\/\/earthjay.com\/?p=6990\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &ldquo;Earthquake Report: Gulf of Alaska!&rdquo;<\/span>&hellip;<\/a><\/div>\n","protected":false},"author":3,"featured_media":6991,"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":[42,5,6,7,26,27,33,34,37],"tags":[],"aioseo_notices":[],"jetpack_featured_media_url":"https:\/\/earthjay.com\/wp-content\/uploads\/2018\/01\/20180123_alaska_interpretation-scaled.jpg","_links":{"self":[{"href":"https:\/\/earthjay.com\/index.php?rest_route=\/wp\/v2\/posts\/6990"}],"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=6990"}],"version-history":[{"count":1,"href":"https:\/\/earthjay.com\/index.php?rest_route=\/wp\/v2\/posts\/6990\/revisions"}],"predecessor-version":[{"id":10760,"href":"https:\/\/earthjay.com\/index.php?rest_route=\/wp\/v2\/posts\/6990\/revisions\/10760"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/earthjay.com\/index.php?rest_route=\/wp\/v2\/media\/6991"}],"wp:attachment":[{"href":"https:\/\/earthjay.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=6990"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/earthjay.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=6990"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/earthjay.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=6990"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}