{"id":890,"date":"2010-04-06T17:02:25","date_gmt":"2010-04-06T16:02:25","guid":{"rendered":"http:\/\/blocs.xtec.cat\/cdavallsdaneu\/?p=233"},"modified":"2010-04-06T17:02:25","modified_gmt":"2010-04-06T16:02:25","slug":"petits-moviments-sismics","status":"publish","type":"post","link":"https:\/\/serveiseducatius.xtec.cat\/cda-vallsdaneu\/general\/petits-moviments-sismics\/","title":{"rendered":"Petits moviments s\u00edsmics"},"content":{"rendered":"<p><a href=\"http:\/\/www.igc.cat\/web\/gcontent\/ca\/sismologia\/igc_sismologia_mapalocal30.html\"><img decoding=\"async\" class=\" wp-image-236 alignleft\" alt=\"Mapa s\u00edsmic dels \u00faltims 30 dies\" src=\"http:\/\/blocs.xtec.cat\/cdavallsdaneu_antic\/files\/2010\/04\/mapa-sismes-30-dies-278x300.jpg\" \/><\/a><\/p>\n<p>El passat 1 d&#8217;abril va tenir lloc al Pirineu franc\u00e8s un sisme de magnitud 4,2 a l&#8217;escala de Ritcher. Es va poder sentir incl\u00fas en alguns punts de les comarques pirinenques lleidatanes. Alg\u00fa de vosaltres el v\u00e0reu notar?<\/p>\n<p>I aquest no \u00e9s \u00fanicament un sisme a\u00efllat, guaiteu el mapa de sismes dels \u00faltims 30 dies en territori catal\u00e0. El Pirineu \u00e9s una zona d&#8217;activitat s\u00edsmica. Sort que la magnitud dels terratr\u00e8mols no sol ser molt elevada! Si cliqueu sobre la imatge anireu a parar a la web de l&#8217;Institut Geol\u00f2gic de Catalunya i obtindreu el mapa actualitzat.<\/p>\n<p>I per qu\u00e8 es produeixen terratr\u00e8mols?<\/p>\n<p><a href=\"http:\/\/blocs.xtec.cat\/cdavallsdaneu_antic\/files\/2010\/04\/plaques.jpg\"><img decoding=\"async\" class=\" wp-image-251 alignright\" alt=\"Plaques tect\u00f2niques m\u00e9s importants\" src=\"http:\/\/blocs.xtec.cat\/cdavallsdaneu_antic\/files\/2010\/04\/plaques-300x201.jpg\" \/><\/a><\/p>\n<p>L&#8217;escor\u00e7a terrestre est\u00e0 formada per 7 grans plaques i altres m\u00e9s petites. Aquestes plaques, conegudes com plaques tect\u00f2niques, no estan quietes, es van despla\u00e7ant a velocitats d&#8217;entre 1-7 cm\/any i a m\u00e9s a m\u00e9s no es mouen totes en el mateix sentit, sin\u00f3 que es poden moure en sentits oposats. Aquest moviment provoca tensions que poden superar la resist\u00e8ncia del material fins a trencar-lo. Al trencar-se, l&#8217;energia acumulada fins al moment s&#8217;allibera en forma d&#8217;ones que es propaguen en totes direccions i que produeixen una gran sacsejada del terreny, que \u00e9s el que coneixem com a sisme o terratr\u00e8mol. El trencament o discontinu\u00eftat que es produeix al material (roca) es coneix amb el nom de falla, i el punt on es produeix l&#8217;alliberament de l&#8217;energia \u00e9s l&#8217;hipocentre, i la seva projecci\u00f3 sobre la superf\u00edcie terrestre \u00e9s l&#8217;epicentre.<\/p>\n<p>Amb tot el que hem explicat, dedu\u00efm que les zones de la Terra amb m\u00e9s probabilitat de patir terratr\u00e8mols s\u00f3n precisament les zones situades en els l\u00edmits d&#8217;aquestes plaques tect\u00f2niques. Si observeu la imatge 2 us fareu una idea de les zones amb m\u00e9s risc s\u00edsmic.\u00a0 Hi reconeixeu els \u00faltims terratr\u00e8mols que han sacsejat la Terra? En el que portem del 2010 s&#8217;han enregistrat sis terratr\u00e8mols de m\u00e9s de 5 graus de magnitud a l&#8217;escala de Ritcher: Hait\u00ed (7.0), Xile (8.8 ), Turquia (5.9 ) o M\u00e8xic (7.2) en s\u00f3n algun dels exemples.<\/p>\n<p>I a casa nostra? Hi ha molts terratr\u00e8mols?<\/p>\n<p><a href=\"http:\/\/blocs.xtec.cat\/cdavallsdaneu_antic\/files\/2010\/04\/terratremols-mediterrania.gif\"><img decoding=\"async\" class=\" wp-image-241 alignleft\" alt=\"Mapa de sismicitat zona Mediterr\u00e0nia Occidental\" src=\"http:\/\/blocs.xtec.cat\/cdavallsdaneu_antic\/files\/2010\/04\/terratremols-mediterrania-300x166.gif\" \/><\/a><\/p>\n<p>La zona de la Mediterr\u00e0nia occidental est\u00e0 situada en una zona de col\u00b7lisi\u00f3 entre les plaques tect\u00f2niques d&#8217;Europa i \u00c0frica. La taxa de converg\u00e8ncia \u00e9s moderada i per aix\u00f2 la freq\u00fc\u00e8ncia en que es produeixen els terratr\u00e8mols no \u00e9s gaire elevada.<\/p>\n<p>I per \u00faltim fem una mica d&#8217;incid\u00e8ncia entre la difer\u00e8ncia entre la magnitud i la intensitat d&#8217;un terratr\u00e8mol. Malauradament hem comen\u00e7at l&#8217;any amb moltes not\u00edcies relacionades amb els sismes ocorreguts i no sempre els mitjans de comunicaci\u00f3 utilitzen b\u00e9 aquesta terminologia.<\/p>\n<p><a href=\"http:\/\/blocs.xtec.cat\/cdavallsdaneu_antic\/files\/2010\/04\/esquerda.jpg\"><img decoding=\"async\" class=\" wp-image-272 alignright\" alt=\"efectes terratr\u00e8mol\" src=\"http:\/\/blocs.xtec.cat\/cdavallsdaneu_antic\/files\/2010\/04\/esquerda-300x189.jpg\" \/><\/a><\/p>\n<p>La magnitud d&#8217;un terratr\u00e8mol indica l&#8217;energia que ha alliberat. L&#8217;escala de magnitud \u00e9s logar\u00edtmica i no t\u00e9 l\u00edmit superior, tot i que no es coneixen terratr\u00e8mols de grand\u00e0ria major que 9.5 a causa de la resist\u00e8ncia f\u00edsica de l&#8217;escor\u00e7a.<\/p>\n<p>La intensitat, per contra, mesura els efectes que produeix el terratr\u00e8mol sobre les persones, els objectes, les construccions i el terreny. La intensitat \u00e9s diferent a cada lloc ja que varia amb la dist\u00e0ncia a l&#8217;epicentre del terratr\u00e8mol. Aix\u00ed un terratr\u00e8mol tindr\u00e0 una magnitud \u00fanica (enregistrada en qualsevol sism\u00f2graf del m\u00f3n) i en canvi tindr\u00e0 diferents intensitats depenent de la dist\u00e0ncia de cada localitat a l&#8217;epicentre.<\/p>\n<p>Finalment afegim un llistat dels terratr\u00e8mols m\u00e9s grans des del 1900. Est\u00e0 extret del <a href=\"http:\/\/www.iea.ad\/crecit\/index2.html\">Centre de Recerca en Ci\u00e8ncies de la Terra (CRECIT)<\/a>, i est\u00e0 actualitzat fins a 2005 amb el sisme de Sumatra.<\/p>\n<table style=\"text-align: center;\" border=\"0\">\n<tbody>\n<tr>\n<td><strong>Magnitud<\/strong><\/td>\n<td><strong>Data<\/strong><\/td>\n<td><strong>Localitzaci\u00f3<\/strong><\/td>\n<\/tr>\n<tr>\n<td>9.5<\/td>\n<td>22\/05\/1960<\/td>\n<td>Xile<\/td>\n<\/tr>\n<tr>\n<td>9.4<\/td>\n<td>28\/03\/1964<\/td>\n<td>Prince Willian Sound, Alaska<\/td>\n<\/tr>\n<tr>\n<td>9.3<\/td>\n<td>26\/12\/2004<\/td>\n<td>Sumatra<\/td>\n<\/tr>\n<tr>\n<td>9.0<\/td>\n<td>04\/11\/1952<\/td>\n<td>Kamchatka<\/td>\n<\/tr>\n<tr>\n<td>8.8<\/td>\n<td>31\/01\/1906<\/td>\n<td>Costa d&#8217;Equador<\/td>\n<\/tr>\n<tr>\n<td>8.7<\/td>\n<td>28\/03\/2005<\/td>\n<td>Nord de Sumatra, Indon\u00e8sia<\/td>\n<\/tr>\n<tr>\n<td>8.7<\/td>\n<td>04\/02\/1965<\/td>\n<td>Illes Rat, Alaska<\/td>\n<\/tr>\n<tr>\n<td>8.6<\/td>\n<td>09\/03\/1957<\/td>\n<td>Illes Andreanof, Alaska<\/td>\n<\/tr>\n<tr>\n<td>8.6<\/td>\n<td>15\/08\/1950<\/td>\n<td>Assam-Tibet<\/td>\n<\/tr>\n<tr>\n<td>8.5<\/td>\n<td>13\/10\/1963<\/td>\n<td>Illes Kuril<\/td>\n<\/tr>\n<tr>\n<td>8.5<\/td>\n<td>01\/02\/1938<\/td>\n<td>Banda Sea, Indon\u00e8sia<\/td>\n<\/tr>\n<tr>\n<td>8.5<\/td>\n<td>11\/11\/1922<\/td>\n<td>Frontera Xile-Argentina<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p>Si voleu con\u00e8ixer els sismes que van esdevenint a Catalunya fins a dia d&#8217;avui podeu clicar el seg\u00fcent enlla\u00e7 de <a href=\"http:\/\/www1.igc.cat\/web\/gcontent\/ca\/sismologia\/igc_sismologia_comact_anys.php\">l&#8217;Institut Geol\u00f2gic de Catalunya<\/a>. Aqu\u00ed us deixem un petit resum dels sismes ocorreguts en el que portem d&#8217;abril:<\/p>\n<table style=\"text-align: center; width: 314px; height: 138px;\" border=\"0\">\n<tbody>\n<tr>\n<td><strong>Data<\/strong><\/td>\n<td><strong>Hora<\/strong><\/td>\n<td><strong>Magnitud<\/strong><\/td>\n<td><strong>Regi\u00f3 <\/strong><\/td>\n<\/tr>\n<tr>\n<td>01\/04\/2010<\/td>\n<td>01:36<\/td>\n<td>4.2<\/td>\n<td>Haytes Pyr\u00e9n\u00e9es<\/td>\n<\/tr>\n<tr>\n<td>01\/04\/2010<\/td>\n<td>12:27<\/td>\n<td>1.4<\/td>\n<td>Haytes Pyr\u00e9n\u00e9es<\/td>\n<\/tr>\n<tr>\n<td>02\/04\/2010<\/td>\n<td>00:03<\/td>\n<td>1.2<\/td>\n<td>Costa Garraf<\/td>\n<\/tr>\n<tr>\n<td>02\/04\/2010<\/td>\n<td>20:52<\/td>\n<td>0.3<\/td>\n<td>Cerdanya<\/td>\n<\/tr>\n<tr>\n<td>04\/04\/2010<\/td>\n<td>19:06<\/td>\n<td>1.5<\/td>\n<td>Selva<\/td>\n<\/tr>\n<tr>\n<td>06\/04\/2010<\/td>\n<td>19:42<\/td>\n<td>1.3<\/td>\n<td>Montsi\u00e0<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p>Doncs fins aqu\u00ed una mica d&#8217;informaci\u00f3 s\u00edsmica &#8230; i tot el que ens deixem per explicar!<\/p>\n<p>Equip del Camp d&#8217;Aprenentatge de les Valls d&#8217;\u00c0neu<\/p>\n","protected":false},"excerpt":{"rendered":"<p>El passat 1 d&#8217;abril va tenir lloc al Pirineu franc\u00e8s un sisme de magnitud 4,2 a l&#8217;escala de Ritcher. Es [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_bbp_topic_count":0,"_bbp_reply_count":0,"_bbp_total_topic_count":0,"_bbp_total_reply_count":0,"_bbp_voice_count":0,"_bbp_anonymous_reply_count":0,"_bbp_topic_count_hidden":0,"_bbp_reply_count_hidden":0,"_bbp_forum_subforum_count":0,"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"categories":[1],"tags":[],"class_list":["post-890","post","type-post","status-publish","format-standard","hentry","category-general"],"post_mailing_queue_ids":[],"_links":{"self":[{"href":"https:\/\/serveiseducatius.xtec.cat\/cda-vallsdaneu\/wp-json\/wp\/v2\/posts\/890","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/serveiseducatius.xtec.cat\/cda-vallsdaneu\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/serveiseducatius.xtec.cat\/cda-vallsdaneu\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/serveiseducatius.xtec.cat\/cda-vallsdaneu\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/serveiseducatius.xtec.cat\/cda-vallsdaneu\/wp-json\/wp\/v2\/comments?post=890"}],"version-history":[{"count":0,"href":"https:\/\/serveiseducatius.xtec.cat\/cda-vallsdaneu\/wp-json\/wp\/v2\/posts\/890\/revisions"}],"wp:attachment":[{"href":"https:\/\/serveiseducatius.xtec.cat\/cda-vallsdaneu\/wp-json\/wp\/v2\/media?parent=890"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/serveiseducatius.xtec.cat\/cda-vallsdaneu\/wp-json\/wp\/v2\/categories?post=890"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/serveiseducatius.xtec.cat\/cda-vallsdaneu\/wp-json\/wp\/v2\/tags?post=890"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}