<div class="css-17ih8de interactive-body"><!-- birdkit: do not modify this file --> <!-- birdkit: html header automatically hoisted to the head --> <div class="birdkit-body g-bk-Ut5xAR62M0mAOw g-dark-mode-incompatible" data-birdkit-hydrate="f2556b591844455b" data-preview-slug="bk-Ut5xAR62M0mAOw" id="g-bk-Ut5xAR62M0mAOw"> <!--[--><!--[0--><!--[--><!--[--><!--[--><!--[0--><!--[--><div class="g-header-wrapper g-align- svelte-10ngljz"><div class="g-header-container g-theme-news g-align-center g-style-extrabold svelte-l86h6b" style="--g-header-text-wrap:balance"><header class="g-header svelte-l86h6b" style="max-width: 700px;"><!--[-1--><!--]--> <!--[-1--><!--]--> <div class="g-heading-wrapper svelte-l86h6b"><h1 class="g-heading svelte-1ya5ar5"><!-- -->Map: 3.7-Magnitude Earthquake Shakes the San Francisco Bay Area<!-- --></h1><!-- --></div> <!--[-1--><!--]--> <!--[-1--><!--]--> <!--[0--><div class="g-byline-wrapper svelte-l86h6b"><p class="g-byline svelte-1lajuuz"><!--[0--><span class="g-byline-prefix">By</span><!--]--> <!--[1--><!--[--><!--[-1--><!--]--><span class="svelte-1lajuuz" itemprop="name"><!--[-1--><!--[1--><a class="svelte-1gilwwa" href="https://www.nytimes.com/by/william-b-davis"><!-- -->William B. Davis<!-- --></a><!--]--><!--]--><!--[0-->, <!--]--></span><!--[-1--><!--]--><span class="svelte-1lajuuz" itemprop="name"><!--[-1--><!--[1--><a class="svelte-1gilwwa" href="https://www.nytimes.com/by/madison-dong"><!-- -->Madison Dong<!-- --></a><!--]--><!--]--><!--[0-->, <!--]--></span><!--[-1--><!--]--><span class="svelte-1lajuuz" itemprop="name"><!--[-1--><!--[1--><a class="svelte-1gilwwa" href="https://www.nytimes.com/by/judson-jones"><!-- -->Judson Jones<!-- --></a><!--]--><!--]--><!--[0-->, <!--]--></span><!--[-1--><!--]--><span class="svelte-1lajuuz" itemprop="name"><!--[-1--><!--[1--><a class="svelte-1gilwwa" href="https://www.nytimes.com/by/john-keefe"><!-- -->John Keefe<!-- --></a><!--]--><!--]--><!--[0-->, <!--]--></span><!--[-1--><!--]--><span class="svelte-1lajuuz" itemprop="name"><!--[-1--><!--[1--><a class="svelte-1gilwwa" href="https://www.nytimes.com/by/joey-k-lee"><!-- -->Joey K. Lee<!-- --></a><!--]--><!--]--><!--[-1--><!--]--></span><!--[0--> and <!--]--><span class="svelte-1lajuuz g-last-byline" itemprop="name"><!--[-1--><!--[1--><a class="svelte-1gilwwa" href="https://www.nytimes.com/by/bea-malsky"><!-- -->Bea Malsky<!-- --></a><!--]--><!--]--><!--[-1--><!--]--></span><!--]--><!--]--> <!--[-1--><!--]--></p><!-- --> <span class="g-timestamp-wrapper"><time class="g-interactive-timestamp svelte-cm3h0f g-interactive-timestamp-updated g-interactive-timestamp-last-updated" datetime="2026-06-02T13:41:15-04:00"><!--[0-->Updated June 2, 2026 at 1:41 p.m. E.T.<!--]--></time><!-- --></span></div><!--]--> <!--[-1--><!--]--> <!--[-1--><!--]--> <!--[0--><div class="g-sharetools svelte-l86h6b"><div class="g-sharetools-wrapper svelte-1llcq6u g-align-center"><span class="svelte-1llcq6u" data-disable="" data-place-component="sharetools" data-render-hash="h--b031da0" data-theme="light-filled"><div class="css-1sm67ns"><div aria-label="Social Media Share buttons, Save button, 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fill-rule="evenodd"></path></svg><span class="css-1k9w9vl">0</span></div></button></li></ul></div></div></div></span></div><!-- --></div><!--]--></header></div><!-- --></div><!--]--><!--]--><!--[0--><!--[--><!--[1--><!-- --><figure class="g-wrapper svelte-nnmo52 g-needs-margin-block" style="--g-wrapper_hed-text-wrap:balance"><!--[-1--><!--]--> <!--[-1--><!--]--> <div class="g-block g-block-margin svelte-ki8lyz"><div class="g-block-width g-max-width-wide svelte-ki8lyz"><!--[--><!--[-1--><!--]--> <div class="g-wrapper_main-content svelte-nnmo52 g-overflow-visible"><!--[-1--><!--]--> <div class="g-wrapper_main_content_slot svelte-nnmo52"><!--[--><!--[--><!--[-1--><!--[--><!-- --><figure class="g-wrapper svelte-nnmo52 g-needs-margin-block" style="--g-wrapper_hed-text-wrap:balance"><!--[-1--><!--]--> <!--[-1--><!--]--> <div class="g-block g-block-margin svelte-ki8lyz"><div class="g-block-width g-max-width-wide svelte-ki8lyz"><!--[--><!--[-1--><!--]--> <div class="g-wrapper_main-content svelte-nnmo52 g-overflow-visible"><!--[-1--><!--]--> <div class="g-wrapper_main_content_slot svelte-nnmo52"><!--[--><!--[--><!--[-1--><!--]--> <div class="g-map-wrap svelte-1n8h63m"><div class="g-map-wrap-column svelte-1n8h63m"><!--[-1--><!--]--> <div class="g-map g-map9 svelte-1jmkkc6" id="g-map9" style="height:NaNpx;max-height:800px"><!--[0--><div class="loader-wrap svelte-1jmkkc6"></div><!--]--> <!--[-1--><!--]--> <!--[--><!--]--></div><!-- --></div> <!--[-1--><!--]--></div> <div class="g-perimeter-map-note"><div class="g-note-wrapper svelte-1nmzn36"><!--[0--><span class="g-source-note svelte-1nmzn36">Note: Map shows the area with a shake intensity of 3 or greater, which U.S.G.S. defines as “weak,” though the earthquake may be felt outside the areas shown.</span><!--]--> <!--[-1--><!--]--> <!--[-1--><!--]--> <!--[1--><span class="g-source-note g-note-outage g-outages-timestamp svelte-1nmzn36"> All times on the map are Pacific time.</span><!--]--> <!--[0--><span class="g-credit-note svelte-1nmzn36">The New York Times</span><!--]--></div><!-- --></div><!--]--><!--]--></div></div> <!--[-1--><!--]--><!--]--></div></div><!-- --> <!--[-1--><!--]--><!-- --></figure><!-- --><!--]--><!--]--><!--]--><!--]--></div></div> <!--[-1--><!--]--><!--]--></div></div><!-- --> <!--[-1--><!--]--><!-- --></figure><!-- --><!--]--><!--]--><!--]--><!--[0--><!--[--><!--[--><!--[-1--><!-- --><p class="g-text g-body-text svelte-kxgec5 g-text_last"><!--[0--><!-- -->A minor, 3.7-magnitude earthquake struck in the San Francisco Bay Area on Tuesday, according to the United States Geological Survey.<!-- --><!--]--><!-- --></p><!-- --><!--]--><!--]--><!--]--><!--]--><!--[0--><!--[--><!--[--><!--[-1--><!-- --><p class="g-text g-body-text svelte-kxgec5 g-text_last"><!--[0--><!-- -->The temblor happened at 9:44 a.m. Pacific time about 4 miles southeast of Cloverdale, Calif., data from the agency shows.<!-- --><!--]--><!-- --></p><!-- --><!--]--><!--]--><!--]--><!--]--><!--[0--><!--[--><!--[--><!--[-1--><!-- --><p class="g-text g-body-text svelte-kxgec5 g-text_last"><!--[0--><!-- -->U.S.G.S. data earlier reported that the magnitude was 3.6.<!-- --><!--]--><!-- --></p><!-- --><!--]--><!--]--><!--]--><!--]--><!--[0--><!--[--><!--[--><!--[-1--><!-- --><p class="g-text g-body-text svelte-kxgec5 g-text_last"><!--[0--><!-- -->As seismologists review available data, they may revise the earthquake’s reported magnitude. Additional information collected about the earthquake may also prompt U.S.G.S. scientists to update the shake-severity map.<!-- --><!--]--><!-- --></p><!-- --><!--]--><!--]--><!--]--><!--]--><!--[0--><!--[--><!--[1--><!-- --><figure class="g-wrapper svelte-nnmo52 g-needs-margin-block" style="--g-wrapper_hed-text-wrap:balance"><!--[-1--><!--]--> <!--[-1--><!--]--> <div class="g-block g-block-margin svelte-ki8lyz"><div class="g-block-width g-max-width-600 svelte-ki8lyz" style="max-width: 600px;"><!--[--><!--[-1--><!--]--> <div class="g-wrapper_main-content svelte-nnmo52 g-overflow-visible"><!--[-1--><!--]--> <div class="g-wrapper_main_content_slot svelte-nnmo52"><!--[--><!--[--><!--[-1--><!--[--><!--[0--><!-- --><figure class="g-wrapper svelte-nnmo52 g-needs-margin-block" style="--g-wrapper_hed-text-wrap:balance"><!--[-1--><!--]--> <!--[-1--><!--]--> <div class="g-block g-block-margin svelte-ki8lyz"><div class="g-block-width g-max-width-600 svelte-ki8lyz" style="max-width: 600px;"><!--[--><!--[-1--><!--]--> <div class="g-wrapper_main-content svelte-nnmo52 g-overflow-visible"><!--[-1--><!--]--> <div class="g-wrapper_main_content_slot svelte-nnmo52"><!--[--><!--[--><!--[0--><h2 class="g-subhed theme- svelte-1c31w29"><!-- -->Aftershocks detected<!-- --></h2><!-- --> <!--[--><!--[0--><p class="g-text svelte-1rn1e1l"><!-- -->Subsequent quakes have been reported in the same area. Such temblors are typically aftershocks caused by minor adjustments along the portion of a fault that slipped at the time of the initial earthquake.<!-- --></p><!--]--><!--]--><!-- --><!--]--> <div class="g-aftershocks-map-legend svelte-jm3clf"><h2 class="svelte-jm3clf">Quakes and aftershocks within 100 miles</h2> <svg class="svelte-jm3clf" viewbox="0 0 20 20" xmlns="http://www.w3.org/2000/svg"><circle cx="10" cy="10" r="9" style="fill: none; stroke: hsl(4, 69%, 66%); stroke-width:2; stroke-linecap: round; stroke-line join: round;"></circle></svg></div> <div class="g-map g-map10 svelte-1jmkkc6" id="g-map10" style="height:NaNpx;max-height:600px"><!--[0--><div class="loader-wrap svelte-1jmkkc6"></div><!--]--> <!--[-1--><!--]--> <!--[--><!--]--></div><!-- --> <div class="g-perimeter-map-note"><div class="g-note-wrapper svelte-1nmzn36"><!--[-1--><!--]--> <!--[-1--><!--]--> <!--[-1--><!--]--> <!--[-1--><!--]--> <!--[0--><span class="g-credit-note svelte-1nmzn36">The New York Times</span><!--]--></div><!-- --></div><!--]--><!--]--></div></div> <!--[-1--><!--]--><!--]--></div></div><!-- --> <!--[-1--><!--]--><!-- --></figure><!-- --><!--]--><!--]--><!--]--><!--]--><!--]--></div></div> <!--[-1--><!--]--><!--]--></div></div><!-- --> <!--[-1--><!--]--><!-- --></figure><!-- --><!--]--><!--]--><!--]--><!--[0--><!--[--><!--[-1--><!--[--><!--[0--><!--[0--><!--[--><!--[0--><p class="g-text svelte-1rn1e1l"><!-- -->Aftershocks can occur days, weeks or even years after the first earthquake. These events can be of equal or larger magnitude to the initial earthquake, and they can continue to affect already damaged locations.<!-- --></p><!--]--><!--]--><!--]--> <!-- --><figure class="g-wrapper svelte-nnmo52 g-needs-margin-block" style="--g-wrapper_hed-text-wrap:balance"><!--[-1--><!--]--> <!--[-1--><!--]--> <div class="g-block g-block-margin svelte-ki8lyz g-margin-inline"><div class="g-block-width g-max-width-1080 svelte-ki8lyz" style="max-width: 1080px;"><!--[--><!--[-1--><!--]--> <div class="g-wrapper_main-content svelte-nnmo52 g-overflow-visible"><!--[-1--><!--]--> <div class="g-wrapper_main_content_slot svelte-nnmo52"><!--[--><!--[--><div class="g-earthquake-map-legend svelte-1knsz5k"><h2 class="svelte-1knsz5k">When quakes and aftershocks occurred</h2></div> <div class="chart-container svelte-1knsz5k"><!--[-1--><!--]--><!-- --></div> <div class="g-earthquake-map-note svelte-1knsz5k"><div class="g-note-wrapper svelte-1nmzn36 margin"><!--[-1--><!--]--> <!--[-1--><!--]--> <!--[-1--><!--]--> <!--[1--><span class="g-source-note g-note-outage g-outages-timestamp svelte-1nmzn36"> All times are Pacific time.</span><!--]--> <!--[0--><span class="g-credit-note svelte-1nmzn36">The New York Times</span><!--]--></div><!-- --></div><!--]--><!--]--></div></div> <!--[-1--><!--]--><!--]--></div></div><!-- --> <!--[-1--><!--]--><!-- --></figure><!-- --><!-- --><!--]--><!--]--><!--]--><!--]--><!--]--><!--[0--><!--[--><!-- --><figure class="g-wrapper svelte-nnmo52" style="--g-wrapper_hed-text-wrap:balance"><!--[-1--><!--]--> <!--[-1--><!--]--> <div class="g-block g-block-margin svelte-ki8lyz g-margin-inline"><div class="g-block-width g-max-width-body svelte-ki8lyz"><!--[--><!--[-1--><!--]--> <div class="g-wrapper_main-content svelte-nnmo52 g-overflow-visible"><!--[-1--><!--]--> <div class="g-wrapper_main_content_slot svelte-nnmo52"><!--[--><div class="g-methodology svelte-1fho0c5"><!--[-1--><!--]--> <!--[0--><!--[--><!--[-1--><!-- --><p class="g-text svelte-kxgec5 g-text_last"><!--[0--><!-- -->Sources: United States Geological Survey (epicenter, aftershocks, shake intensity); LandScan via Oak Ridge National Laboratory (population density) | Notes: Shaking categories are based on the <a href="https://www.usgs.gov/programs/earthquake-hazards/modified-mercalli-intensity-scale">Modified Mercalli Intensity</a> scale. When aftershock data is available, the corresponding maps and charts include earthquakes within 100 miles and seven days of the initial quake. All times above are Pacific time. Shake data is as of Tuesday, June 2 at 12:59 p.m. Eastern. Aftershocks data is as of Tuesday, June 2 at 1:15 p.m. Eastern.<!-- --><!--]--><!-- --></p><!-- --><!--]--><!--]--><!--]--></div><!--]--></div></div> <!--[-1--><!--]--><!--]--></div></div><!-- --> <!--[-1--><!--]--><!-- --></figure><!-- --><!--]--><!--]--><!--]--><!--]--><!-- --><!--]--><!--]--> <!--[-1--><!--]--><!--]--> <cript> { __sveltekit_dv0n5h = { base: new URL(".", location).pathname.slice(0, -1) }; const element = document.currentScript.parentElement.dataset.birdkitHydrate ? document.currentScript.parentElement : document.querySelector('[data-birdkit-hydrate="f2556b591844455b"]'); Promise.all([ import("https://static01.nytimes.com/newsgraphics/Ut5xAR62M0mAOw/_app.YGe96tfDUdOw562nGVVPiriMbd_N2lP79QZ-Ym6rzcw/immutable/entry/start.ClLZmv7X.js"), import("https://static01.nytimes.com/newsgraphics/Ut5xAR62M0mAOw/_app.YGe96tfDUdOw562nGVVPiriMbd_N2lP79QZ-Ym6rzcw/immutable/entry/app.B_pfLZfu.js") ]).then(([kit, app]) => { kit.start(app, element, { node_ids: [0, 2], data: [null,{type:"data",data:{body:[{type:"header",value:{sharetools:{show:true,theme:"light-filled"},style:"extrabold",maxWidth:"700",lastUpdated:{show:true,time:true},headline:"Map: 3.7-Magnitude Earthquake Shakes the San Francisco Bay Area",leadin:"",bylines:[{creatorSnapshots:[{bioUrl:"https://www.nytimes.com/by/william-b-davis",displayName:"William B. 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Additional information collected about the earthquake may also prompt U.S.G.S. scientists to update the shake-severity map."},{type:"svelte",value:{component:"AftershocksMap",wrapper:true,hed:void 0,dependent:[{subhed:"Aftershocks detected",paragraph:"Subsequent quakes have been reported in the same area. Such temblors are typically aftershocks caused by minor adjustments along the portion of a fault that slipped at the time of the initial earthquake."}],noteOverride:"Map shows earthquakes within 100 miles and up to seven days of the initial quake.",sources:void 0,alt:"Map of the region affected with a thick circle in the center showing the initial earthquake and thinner circles nearby showing subsequent quakes.",creditOverride:"The New York Times",textAlign:"left",maxWidth:"600",marginInline:false,marginBlock:true,zoom:"6.5",showInsetMap:true,mapInsetType:"state",mapInsetShape:"CA",insetPosition:"left",insetMaxWidth:"120",insetMaxWidthMobile:"100",showInsetLabel:true,insetlabel:[{name:"Calif.",left:"48",top:"50"}],epiLabelBoldLine:"Epicenter",epiLabelLine2:"Magnitude 3.7 earthquake",epiLabelLine3:"timestamp",mainLabelPosition:"left",hideBbox:true,showCustomLabel:false,customlabels:[{name:"Mexico",category:"country",center:[-105.183,28.177]}],showWeakZone:false,subheds:[{subhed:"Initial quake"},{subhed:"Smaller aftershock"}]}},{type:"svelte",value:{component:"AftershockChart",dependent:[{paragraph:"Aftershocks can occur days, weeks or even years after the first earthquake. These events can be of equal or larger magnitude to the initial earthquake, and they can continue to affect already damaged locations."}],wrapper:false,hed:void 0,creditOverride:"The New York Times",textAlign:"left",maxWidth:"1080",marginInline:true,marginBlock:true,altText:"A graphic showing aftershocks represented by circles on a timeline, with the size of the circles indicating each aftershock’s magnitude."}},{type:"methodology",value:{hed:"",text:[{type:"text",value:"Sources: United States Geological Survey (epicenter, aftershocks, shake intensity); LandScan via Oak Ridge National Laboratory (population density) | Notes: Shaking categories are based on the \u003Ca href=\"https://www.usgs.gov/programs/earthquake-hazards/modified-mercalli-intensity-scale\">Modified Mercalli Intensity\u003C/a> scale. When aftershock data is available, the corresponding maps and charts include earthquakes within 100 miles and seven days of the initial quake. All times above are Pacific time. 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