{"id":26914,"date":"2023-02-27T12:44:00","date_gmt":"2023-02-27T15:44:00","guid":{"rendered":"https:\/\/mindthegraph.com\/blog\/what-is-stargazing-copy\/"},"modified":"2023-02-28T18:06:09","modified_gmt":"2023-02-28T21:06:09","slug":"earthquake-magnitude","status":"publish","type":"post","link":"https:\/\/mindthegraph.com\/blog\/sk\/zemetrasenie-s-magnitudou\/","title":{"rendered":"Pochopenie magnit\u00fad zemetrasen\u00ed a ich vplyvu"},"content":{"rendered":"

Zemetrasenia s\u00fa roz\u0161\u00edren\u00fdm pr\u00edrodn\u00fdm javom, ktor\u00fd sa pravidelne vyskytuje na celom svete. Pod\u013ea Geologickej slu\u017eby Spojen\u00fdch \u0161t\u00e1tov americk\u00fdch (USGS) sa ka\u017ed\u00fd rok vyskytn\u00fa st\u00e1tis\u00edce zemetrasen\u00ed, z ktor\u00fdch v\u00e4\u010d\u0161ina je pr\u00edli\u0161 slab\u00e1 na to, aby si ich \u013eudia v\u0161imli. <\/p>\n\n\n\n

Frekvencia zemetrasen\u00ed sa v\u00fdrazne l\u00ed\u0161i v z\u00e1vislosti od miesta ich v\u00fdskytu. Vzh\u013eadom na umiestnenie na hraniciach akt\u00edvnych zemsk\u00fdch dosiek sa na niektor\u00fdch miestach, ako napr\u00edklad v Kalifornii a Japonsku, vyskytuj\u00fa zemetrasenia pravidelne, zatia\u013e \u010do na in\u00fdch miestach sa m\u00f4\u017eu vyskytova\u0165 len sporadick\u00e9 zemetrasenia.<\/p>\n\n\n\n

S\u00fdria a Turecko s\u00fa tie\u017e n\u00e1chyln\u00e9 na zemetrasenia. Turecko sa nach\u00e1dza na hranici africkej a euro\u00e1zijskej tektonickej dosky, zatia\u013e \u010do S\u00fdria le\u017e\u00ed na hranici africkej a arabskej tektonickej dosky. <\/p>\n\n\n\n

Preto ich 6. febru\u00e1ra 2023 postihlo stra\u0161n\u00e9 zemetrasenie, ktor\u00e9 zabilo viac ako 11 000 \u013eud\u00ed a desiatky tis\u00edc \u010fal\u0161\u00edch zranilo. Zemetrasenie dosiahlo magnit\u00fadu 7,8, \u010do sa pova\u017euje za ve\u013emi siln\u00e9 a potenci\u00e1lne ni\u010div\u00e9 zemetrasenie. <\/p>\n\n\n\n

\u010co je to magnit\u00fada zemetrasenia?<\/h2>\n\n\n\n

Magnit\u00fada zemetrasenia je miera jeho ve\u013ekosti alebo sily, ktor\u00e1 sa pou\u017e\u00edva na vyjadrenie mno\u017estva energie, ktor\u00fa zemetrasenie vyvolalo. Magnit\u00fada sa vypo\u010d\u00edta na z\u00e1klade ve\u013ekosti seizmick\u00fdch v\u013an a mno\u017estva pozorovan\u00fdch pohybov zeme. <\/p>\n\n\n\n

Richterova stupnica, ktor\u00fa v 30. rokoch 20. storo\u010dia vytvoril Charles Richter, bola dlh\u00e9 roky tradi\u010dn\u00fdm meradlom sily zemetrasenia, ale v s\u00fa\u010dasnosti ju v podstate nahradila Momentov\u00e1 stupnica. <\/p>\n\n\n\n

Ako mera\u0165 magnit\u00fadu zemetrasenia? <\/h2>\n\n\n\n

Existuje mnoho met\u00f3d na meranie magnit\u00fady zemetrasenia a ka\u017ed\u00e1 z nich poskytuje in\u00fd odhad ve\u013ekosti zemetrasenia. Nasleduj\u00face pr\u00edstupy s\u00fa najroz\u0161\u00edrenej\u0161ie:<\/p>\n\n\n\n

Richterova stupnica<\/h3>\n\n\n\n

Richterova stupnica je zalo\u017een\u00e1 na najv\u00e4\u010d\u0161ej seizmickej vlne zaznamenanej seizmometrom a pon\u00faka jedin\u00fa hodnotu, ktor\u00e1 opisuje celkov\u00fa silu zemetrasenia. <\/p>\n\n\n\n

Je logaritmick\u00fd, \u010do znamen\u00e1, \u017ee mal\u00fd n\u00e1rast magnit\u00fada m\u00e1 za n\u00e1sledok v\u00fdrazn\u00fd n\u00e1rast ve\u013ekosti zemetrasenia. Zemetrasenie s magnit\u00fadou 7,0 je napr\u00edklad desa\u0165kr\u00e1t v\u00e4\u010d\u0161ie ako zemetrasenie s magnit\u00fadou 6,0 a stokr\u00e1t v\u00e4\u010d\u0161ie ako zemetrasenie s magnit\u00fadou 5,0.<\/p>\n\n\n\n

Richterova stupnica m\u00e1 rozsah od 0 do 9, pri\u010dom \u010d\u00edsla men\u0161ie ako 2,0 \u013eudia zvy\u010dajne nepoc\u00edtia a \u010d\u00edsla v\u00e4\u010d\u0161ie ako 8,0 sa pova\u017euj\u00fa za ve\u013ek\u00e9 zemetrasenia, ktor\u00e9 m\u00f4\u017eu sp\u00f4sobi\u0165 rozsiahle \u0161kody a katastrofy. <\/p>\n\n\n\n

Momentov\u00e1 stupnica<\/h3>\n\n\n\n

Momentov\u00e1 stupnica bola zaveden\u00e1 ako alternat\u00edva k Richterovej stupnici na ur\u010denie magnit\u00fady zemetrasenia. Momentov\u00e1 stupnica na rozdiel od Richterovej stupnice odhaduje celkov\u00fa energiu vytvoren\u00fa zemetrasen\u00edm. <\/p>\n\n\n\n

Vych\u00e1dza z koncepcie seizmick\u00e9ho momentu, \u010do je ve\u013ekos\u0165 zemetrasenia zalo\u017een\u00e1 na ve\u013ekosti sklzu (pohybu) na poruche, ploche poruchy, ktor\u00e1 sa posunula, a tuhosti zemskej k\u00f4ry. Seizmick\u00fd moment sa vytv\u00e1ra na z\u00e1klade meran\u00ed seizmick\u00fdch v\u013an a pou\u017e\u00edva sa na pos\u00fadenie magnit\u00fady zemetrasenia.<\/p>\n\n\n\n

Momentov\u00e1 stupnica magnit\u00fad, podobne ako Richterova stupnica, je logaritmick\u00e1, \u010do znamen\u00e1, \u017ee mal\u00fd n\u00e1rast magnit\u00fada sa rovn\u00e1 obrovsk\u00e9mu n\u00e1rastu ve\u013ekosti zemetrasenia.<\/p>\n\n\n\n

Momentov\u00e1 stupnica m\u00e1 rozsah od -2,0 do 9,0 a je naj\u010dastej\u0161ie pou\u017e\u00edvanou stupnicou magnit\u00fad zemetrasen\u00ed, preto\u017ee meria ve\u013ekos\u0165 zemetrasenia presnej\u0161ie ako Richterova stupnica, najm\u00e4 v pr\u00edpade ve\u013ek\u00fdch zemetrasen\u00ed, ktor\u00e9 sa vyskytuj\u00fa v zna\u010dn\u00fdch h\u013abkach.<\/p>\n\n\n\n

<\/div>\n\n\n
\n
\"\"
Ilustr\u00e1cia je k dispoz\u00edcii v Mind the Graph<\/a><\/strong><\/em><\/figcaption><\/figure><\/div>\n\n\n
<\/div>\n\n\n\n

<\/a>Mercalliho stupnica<\/h3>\n\n\n\n

Mercalliho stupnica je stupnica z\u00e1va\u017enosti zemetrasenia, ktor\u00e1 zn\u00e1zor\u0148uje dopady zemetrasenia na zemsk\u00fa k\u00f4ru, ako aj na jednotlivcov, budovy a in\u00e9 stavby. Mercalliho stupnica sa \u010dasto pou\u017e\u00edva v kombin\u00e1cii s Richterovou alebo Momentovou stupnicou, ktor\u00e9 sa pou\u017e\u00edvaj\u00fa na ur\u010denie sily zemetrasenia.<\/p>\n\n\n\n

Stupnica je zalo\u017een\u00e1 na r\u00edmskom \u010d\u00edselnom syst\u00e9me od I po XII, pri\u010dom I znamen\u00e1 slab\u00e9 otrasy, ktor\u00e9 \u013eudia nepoc\u00edtia, a XII ozna\u010duje mimoriadne siln\u00e9 otrasy, ktor\u00e9 sp\u00f4sobuj\u00fa rozsiahle \u0161kody a ni\u010denie. Zoh\u013ead\u0148uje typ povrchu, na ktorom k zemetraseniu d\u00f4jde, typ zasiahnut\u00fdch \u0161trukt\u00far a rozsah sp\u00f4soben\u00fdch \u0161k\u00f4d.<\/p>\n\n\n\n

Mercalliho stupnica a Momentov\u00e1 stupnica alebo Richterova stupnica v kombin\u00e1cii umo\u017e\u0148uj\u00fa lep\u0161ie pochopi\u0165 zemetrasenie, zah\u0155\u0148aj\u00fac jeho silu aj dopad. <\/p>\n\n\n\n

Ak napr\u00edklad zemetrasenie s vy\u0161\u0161\u00edm momentov\u00fdm magnit\u00fadom nastane v menej os\u00eddlenej lokalite alebo ak je p\u00f4da menej n\u00e1chyln\u00e1 na po\u0161kodenie, nemus\u00ed sp\u00f4sobi\u0165 tak\u00e9 ve\u013ek\u00e9 \u0161kody ako zemetrasenie s ni\u017e\u0161\u00edm momentov\u00fdm magnit\u00fadom v husto os\u00eddlenej oblasti alebo ak je p\u00f4da ve\u013emi n\u00e1chyln\u00e1 na po\u0161kodenie, \u0161kody v tejto situ\u00e1cii m\u00f4\u017eu by\u0165 v\u00e4\u010d\u0161ie. <\/p>\n\n\n\n

Preto m\u00f4\u017ee by\u0165 najlep\u0161\u00edm pr\u00edstupom kombin\u00e1cia t\u00fdchto dvoch stupn\u00edc, preto\u017ee Mercalliho stupnica je zalo\u017een\u00e1 na pozorovaniach os\u00f4b, ktor\u00e9 za\u017eili zemetrasenie a nahl\u00e1sili n\u00e1sledky, ktor\u00e9 videli.<\/p>\n\n\n\n

Ako lokalizova\u0165 epicentrum zemetrasenia?<\/h2>\n\n\n\n

Seizmol\u00f3govia pou\u017e\u00edvaj\u00fa na ur\u010denie epicentra zemetrasenia techniku zn\u00e1mu ako triangul\u00e1cia. <\/p>\n\n\n\n

Z\u00e1kladn\u00e1 my\u0161lienka triangul\u00e1cie spo\u010d\u00edva v tom, \u017ee seizmick\u00e9 vlny zo zemetrasenia sa \u0161\u00edria r\u00f4znymi r\u00fdchlos\u0165ami cez r\u00f4zne materi\u00e1ly a prich\u00e1dzaj\u00fa v r\u00f4znom \u010dase na seizmografick\u00e9 stanice umiestnen\u00e9 v r\u00f4znych vzdialenostiach od epicentra. Seizmol\u00f3govia m\u00f4\u017eu odhadn\u00fa\u0165 polohu epicentra sk\u00faman\u00edm \u010dasu pr\u00edchodu seizmick\u00fdch v\u013an na nieko\u013ek\u00fdch seizmografick\u00fdch miestach.<\/p>\n\n\n\n

Intenzita zemetrasenia<\/h2>\n\n\n\n
Magnit\u00fada<\/th>Intenzita<\/th>Impact<\/th>Priemern\u00e1 frekvencia zemetrasen\u00ed<\/th><\/tr><\/thead>
2,0 alebo menej<\/strong><\/td>Mikro<\/td>Zriedkavo poci\u0165ovan\u00e9<\/td>Viac ako mili\u00f3ny ro\u010dne<\/td><\/tr>
2,0 a\u017e 2,9<\/strong><\/td>Men\u0161ie<\/td>Mierne c\u00edti\u0165<\/td>Viac ako jeden mili\u00f3n ro\u010dne<\/td><\/tr>
3,0 a\u017e 3,9<\/strong><\/td>Viac ako drobn\u00e9<\/td>\u010casto sa c\u00edtil<\/td>Viac ako sto tis\u00edc ro\u010dne<\/td><\/tr>
4,0 a\u017e 4,9<\/strong><\/td>Svetlo<\/td>Poci\u0165uje v\u00e4\u010d\u0161ina \u013eud\u00ed<\/td>Viac ako desa\u0165tis\u00edc ro\u010dne<\/td><\/tr>
5,0 a\u017e 5,9<\/strong><\/td>Mierne<\/td>M\u00f4\u017ee po\u0161kodi\u0165 slab\u00e9 \u0161trukt\u00fary<\/td>Viac ako tis\u00edc ro\u010dne<\/td><\/tr>
6,0 a\u017e 6,9<\/strong><\/td>Siln\u00fd<\/td>Sp\u00f4sobuje \u0161kody na stredne \u0165a\u017ek\u00fdch dobre postaven\u00fdch kon\u0161trukci\u00e1ch<\/td>Viac ako sto ro\u010dne<\/td><\/tr>
7,0 a\u017e 7,9<\/strong><\/td>Hlavn\u00e9 str\u00e1nky<\/td>Sp\u00f4sobuje \u0161kody na v\u00e4\u010d\u0161ine budov<\/td>Desa\u0165 a\u017e dvadsa\u0165 ro\u010dne<\/td><\/tr>
8,0 a\u017e 8,9<\/strong><\/td>Skvel\u00e9<\/td>Ve\u013ek\u00e9 \u0161kody na budov\u00e1ch<\/td>Jedenkr\u00e1t ro\u010dne<\/td><\/tr>
9,0 alebo viac<\/strong><\/td>Najv\u00e4\u010d\u0161\u00ed<\/td>M\u00f4\u017ee zr\u00fati\u0165 v\u0161etky budovy<\/td>Raz za desa\u0165 alebo viac rokov<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n

\u0160pecializujeme sa na grafick\u00e9 abstrakty, vedeck\u00e9 \u00fadaje, ktor\u00e9 s\u00fa kur\u00e1tormi vedcov<\/h2>\n\n\n\n

Grafick\u00e9 abstrakty m\u00f4\u017eu pom\u00f4c\u0165 vedcom pri sprostredkovan\u00ed zlo\u017eit\u00fdch konceptov, zd\u00f4razni\u0165 k\u013e\u00fa\u010dov\u00e9 zistenia, zv\u00fd\u0161i\u0165 objavnos\u0165 v\u00fdskumu a podpori\u0165 multidisciplin\u00e1rnu pr\u00e1cu. Vedci m\u00f4\u017eu spr\u00edstupni\u0165 svoje \u0161t\u00fadie a urobi\u0165 ich zrozumite\u013enej\u0161\u00edmi pomocou grafick\u00fdch abstraktov, \u010do m\u00f4\u017ee pom\u00f4c\u0165 pokroku v oblasti vedy vo v\u0161etk\u00fdch oblastiach. <\/p>\n\n\n\n

Ak potrebujete jednoduch\u00fd n\u00e1stroj na vytv\u00e1ranie grafick\u00fdch abstraktov, pou\u017eite n\u00e1stroj Mind The Graph, ktor\u00fd je pou\u017e\u00edvate\u013esky pr\u00edvetiv\u00fd a umo\u017e\u0148uje ka\u017ed\u00e9mu, dokonca aj t\u00fdm, ktor\u00ed maj\u00fa obmedzen\u00e9 n\u00e1vrh\u00e1rske schopnosti, vytv\u00e1ra\u0165 grafiku profesion\u00e1lnej kvality.<\/p>\n\n\n\n

<\/div>\n\n\n
\n
\"\"<\/a><\/figure><\/div>\n\n\n
<\/div>\n\n\n\n
<\/div>\n\n\n\n

<\/p>","protected":false},"excerpt":{"rendered":"

Je \u010das pochopi\u0165, \u010do je to magnit\u00fada zemetrasenia, ak\u00e9 stupnice sa naj\u010dastej\u0161ie pou\u017e\u00edvaj\u00fa a ako m\u00f4\u017eu predpoveda\u0165 z\u00e1va\u017enos\u0165 udalosti.<\/p>","protected":false},"author":28,"featured_media":26924,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":[],"categories":[959,28],"tags":[],"yoast_head":"\nUnderstanding Earthquake Magnitudes and Their Impact<\/title>\n<meta name=\"description\" content=\"It's time to understand the earthquake magnitude, the most often used scales, and how they might predict the severity of an event.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/mindthegraph.com\/blog\/sk\/wielkosc-trzesienia-ziemi\/\" \/>\n<meta property=\"og:locale\" content=\"sk_SK\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Understanding Earthquake Magnitudes and Their Impact\" \/>\n<meta property=\"og:description\" content=\"It's time to understand the earthquake magnitude, the most often used scales, and how they might predict the severity of an event.\" \/>\n<meta property=\"og:url\" content=\"https:\/\/mindthegraph.com\/blog\/sk\/wielkosc-trzesienia-ziemi\/\" \/>\n<meta property=\"og:site_name\" content=\"Mind the Graph Blog\" \/>\n<meta property=\"article:published_time\" content=\"2023-02-27T15:44:00+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2023-02-28T21:06:09+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/mindthegraph.com\/blog\/wp-content\/uploads\/2023\/02\/blog-earthquake.png\" \/>\n\t<meta property=\"og:image:width\" content=\"1124\" \/>\n\t<meta property=\"og:image:height\" content=\"613\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/png\" \/>\n<meta name=\"author\" content=\"Jessica Abbadia\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:title\" content=\"Understanding Earthquake Magnitudes and Their Impact\" \/>\n<meta name=\"twitter:description\" content=\"It's time to understand the earthquake magnitude, the most often used scales, and how they might predict the severity of an event.\" \/>\n<meta name=\"twitter:image\" content=\"https:\/\/mindthegraph.com\/blog\/wp-content\/uploads\/2023\/02\/blog-earthquake.png\" \/>\n<meta name=\"twitter:label1\" content=\"Written by\" \/>\n\t<meta name=\"twitter:data1\" content=\"Jessica Abbadia\" \/>\n\t<meta name=\"twitter:label2\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data2\" content=\"6 minutes\" \/>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Understanding Earthquake Magnitudes and Their Impact","description":"It's time to understand the earthquake magnitude, the most often used scales, and how they might predict the severity of an event.","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/mindthegraph.com\/blog\/sk\/wielkosc-trzesienia-ziemi\/","og_locale":"sk_SK","og_type":"article","og_title":"Understanding Earthquake Magnitudes and Their Impact","og_description":"It's time to understand the earthquake magnitude, the most often used scales, and how they might predict the severity of an event.","og_url":"https:\/\/mindthegraph.com\/blog\/sk\/wielkosc-trzesienia-ziemi\/","og_site_name":"Mind the Graph Blog","article_published_time":"2023-02-27T15:44:00+00:00","article_modified_time":"2023-02-28T21:06:09+00:00","og_image":[{"width":1124,"height":613,"url":"https:\/\/mindthegraph.com\/blog\/wp-content\/uploads\/2023\/02\/blog-earthquake.png","type":"image\/png"}],"author":"Jessica Abbadia","twitter_card":"summary_large_image","twitter_title":"Understanding Earthquake Magnitudes and Their Impact","twitter_description":"It's time to understand the earthquake magnitude, the most often used scales, and how they might predict the severity of an event.","twitter_image":"https:\/\/mindthegraph.com\/blog\/wp-content\/uploads\/2023\/02\/blog-earthquake.png","twitter_misc":{"Written by":"Jessica Abbadia","Est. reading time":"6 minutes"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"https:\/\/mindthegraph.com\/blog\/pl\/wielkosc-trzesienia-ziemi\/","url":"https:\/\/mindthegraph.com\/blog\/pl\/wielkosc-trzesienia-ziemi\/","name":"Understanding Earthquake Magnitudes and Their Impact","isPartOf":{"@id":"https:\/\/mindthegraph.com\/blog\/#website"},"datePublished":"2023-02-27T15:44:00+00:00","dateModified":"2023-02-28T21:06:09+00:00","author":{"@id":"https:\/\/mindthegraph.com\/blog\/#\/schema\/person\/96ecc2d785106e951f7773dc7c96d699"},"description":"It's time to understand the earthquake magnitude, the most often used scales, and how they might predict the severity of an event.","breadcrumb":{"@id":"https:\/\/mindthegraph.com\/blog\/pl\/wielkosc-trzesienia-ziemi\/#breadcrumb"},"inLanguage":"sk-SK","potentialAction":[{"@type":"ReadAction","target":["https:\/\/mindthegraph.com\/blog\/pl\/wielkosc-trzesienia-ziemi\/"]}]},{"@type":"BreadcrumbList","@id":"https:\/\/mindthegraph.com\/blog\/pl\/wielkosc-trzesienia-ziemi\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/mindthegraph.com\/blog\/"},{"@type":"ListItem","position":2,"name":"Understanding Earthquake Magnitudes and Their Impact"}]},{"@type":"WebSite","@id":"https:\/\/mindthegraph.com\/blog\/#website","url":"https:\/\/mindthegraph.com\/blog\/","name":"Mind the Graph Blog","description":"Your science can be beautiful!","potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/mindthegraph.com\/blog\/?s={search_term_string}"},"query-input":"required name=search_term_string"}],"inLanguage":"sk-SK"},{"@type":"Person","@id":"https:\/\/mindthegraph.com\/blog\/#\/schema\/person\/96ecc2d785106e951f7773dc7c96d699","name":"Jessica Abbadia","image":{"@type":"ImageObject","inLanguage":"sk-SK","@id":"https:\/\/mindthegraph.com\/blog\/#\/schema\/person\/image\/","url":"https:\/\/secure.gravatar.com\/avatar\/f477bd20199beb376b04b2fda9a2cec5?s=96&d=mm&r=g","contentUrl":"https:\/\/secure.gravatar.com\/avatar\/f477bd20199beb376b04b2fda9a2cec5?s=96&d=mm&r=g","caption":"Jessica Abbadia"},"description":"Jessica Abbadia is a lawyer that has been working in Digital Marketing since 2020, improving organic performance for apps and websites in various regions through ASO and SEO. Currently developing scientific and intellectual knowledge for the community's benefit. Jessica is an animal rights activist who enjoys reading and drinking strong coffee.","sameAs":["https:\/\/www.linkedin.com\/in\/jessica-abbadia-9b834a13b\/"],"url":"https:\/\/mindthegraph.com\/blog\/sk\/author\/jessica\/"}]}},"_links":{"self":[{"href":"https:\/\/mindthegraph.com\/blog\/sk\/wp-json\/wp\/v2\/posts\/26914"}],"collection":[{"href":"https:\/\/mindthegraph.com\/blog\/sk\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/mindthegraph.com\/blog\/sk\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/mindthegraph.com\/blog\/sk\/wp-json\/wp\/v2\/users\/28"}],"replies":[{"embeddable":true,"href":"https:\/\/mindthegraph.com\/blog\/sk\/wp-json\/wp\/v2\/comments?post=26914"}],"version-history":[{"count":4,"href":"https:\/\/mindthegraph.com\/blog\/sk\/wp-json\/wp\/v2\/posts\/26914\/revisions"}],"predecessor-version":[{"id":26931,"href":"https:\/\/mindthegraph.com\/blog\/sk\/wp-json\/wp\/v2\/posts\/26914\/revisions\/26931"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/mindthegraph.com\/blog\/sk\/wp-json\/wp\/v2\/media\/26924"}],"wp:attachment":[{"href":"https:\/\/mindthegraph.com\/blog\/sk\/wp-json\/wp\/v2\/media?parent=26914"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/mindthegraph.com\/blog\/sk\/wp-json\/wp\/v2\/categories?post=26914"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/mindthegraph.com\/blog\/sk\/wp-json\/wp\/v2\/tags?post=26914"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}