{"id":9887,"date":"2018-06-07T10:16:49","date_gmt":"2018-06-07T08:16:49","guid":{"rendered":"http:\/\/agora.xtec.cat\/iesm-jmzafra\/?p=9887"},"modified":"2018-06-07T10:16:49","modified_gmt":"2018-06-07T08:16:49","slug":"creta","status":"publish","type":"post","link":"https:\/\/agora.xtec.cat\/inscaterinaalbert\/blogs\/museu-de-geologia\/creta\/","title":{"rendered":"CRETA"},"content":{"rendered":"<p><strong>Nom:<\/strong><br \/>\nCatal\u00e0: <strong>Creta<\/strong><br \/>\nCastell\u00e0: Creta<br \/>\nAngles: Chalk<br \/>\nFranc\u00e8s: Craie<br \/>\n<strong>Imatges:<\/strong><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"http:\/\/4.bp.blogspot.com\/-lt62bRu_U0I\/U55V9KY0ucI\/AAAAAAAAeT8\/re1nA4bvcak\/s1600\/creta.jpg\" alt=\"Resultat d'imatges de Creta roca\" width=\"270\" height=\"210\" \/><\/p>\n<p><strong>Quin tipus i subtipus de roca i\/o mineral \u00e9s?<\/strong><\/p>\n<p>Es una roca sedimentaria i calc\u00e0ria<\/p>\n<p><strong>Formaci\u00f3 de la roca i\/o mineral<\/strong><br \/>\nEs forma sota condicions marines profundes per l&#8217;acumulaci\u00f3 gradual de petites plaques de calcita (cocc\u00f2lits), posades per microorganismes anomenats coccolitoforal<\/p>\n<p><strong>Composici\u00f3 qu\u00edmica:<\/strong><br \/>\nEst\u00e0 compost per carbonat de calci o CaCO3 .<\/p>\n<p><strong>Breu descripci\u00f3 (color, textura&#8230;)<\/strong><br \/>\nLa roca Creta es blanca , amb pols i tova. T\u00e9 una forma calc\u00e0ria .Resisteix m\u00e9s la meteoritzaci\u00f3 que l&#8217;argila amb la qual normalment est\u00e0 associada, format aix\u00ed penya-segats als litorals. La creta, per la seva porositat, olla acumular molta aigua i alliberar-la en els estacions seques.<\/p>\n<p><strong>Usos i\/o aplicacions<\/strong><br \/>\nLa creta s&#8217;utilitza per fer el guix per escriure o dibuixar en superf\u00edcies rugoses. En agricultura s&#8217;utilitza per elevar el pH dels s\u00f2ls \u00e0cids. En esports com el tennis s&#8217;utilitza per marcar els l\u00edmits del terreny de joc per\u00f2 actualment s&#8217;utilitza m\u00e9s el di\u00f2xid de titani. En gimn\u00e0stica tradicionalment s&#8217;utilitzava la creta per a les mans, actualment s&#8217;utilitza per\u00f2, el carbonat de magnesi. La creta pot ser un ingredient de la pasta dent\u00edfrica, tamb\u00e9 en el polit de metalls.<\/p>\n<p><strong>Lloc d&#8217;origen (Jaciments m\u00e9s importants)<\/strong><br \/>\n\u00c9s una roca que s\u2019ha format en ambient aqu\u00e0tic, per acumulaci\u00f3 en el fons del mar de caparrons<br \/>\nPenya-segats de Dover ( Regne Unit), \u00abel penya-segat, que arriba fins a 106 metres d&#8217;altura, deu el seu cridanera fa\u00e7ana a la seva composici\u00f3 de creta\u00bb.<\/p>\n<p><strong>Refer\u00e8ncia bibliogr\u00e0fica<\/strong><br \/>\nhttps:\/\/ca.wikipedia.org\/wiki\/Creta_(geologia)<br \/>\nhttps:\/\/ca.wikipedia.org\/wiki\/Llista_de_roques_sediment%C3%A0ries<br \/>\nhttps:\/\/www.ecured.cu\/index.php?search=+roca+creta&#038;button=<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Nom: Catal\u00e0: Creta Castell\u00e0: Creta Angles: Chalk Franc\u00e8s: Craie Imatges: Quin tipus i subtipus de roca i\/o mineral \u00e9s? Es una roca sedimentaria i calc\u00e0ria Formaci\u00f3 de la roca i\/o mineral Es forma sota condicions marines profundes per l&#8217;acumulaci\u00f3 gradual de petites plaques de calcita (cocc\u00f2lits), posades per microorganismes anomenats coccolitoforal Composici\u00f3 qu\u00edmica: Est\u00e0 compost [&hellip;]<\/p>\n","protected":false},"author":185,"featured_media":0,"comment_status":"closed","ping_status":"closed","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":[321],"tags":[],"class_list":["post-9887","post","type-post","status-publish","format-standard","hentry","category-museu-de-geologia"],"post_mailing_queue_ids":[],"_links":{"self":[{"href":"https:\/\/agora.xtec.cat\/inscaterinaalbert\/wp-json\/wp\/v2\/posts\/9887","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/agora.xtec.cat\/inscaterinaalbert\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/agora.xtec.cat\/inscaterinaalbert\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/agora.xtec.cat\/inscaterinaalbert\/wp-json\/wp\/v2\/users\/185"}],"replies":[{"embeddable":true,"href":"https:\/\/agora.xtec.cat\/inscaterinaalbert\/wp-json\/wp\/v2\/comments?post=9887"}],"version-history":[{"count":4,"href":"https:\/\/agora.xtec.cat\/inscaterinaalbert\/wp-json\/wp\/v2\/posts\/9887\/revisions"}],"predecessor-version":[{"id":9912,"href":"https:\/\/agora.xtec.cat\/inscaterinaalbert\/wp-json\/wp\/v2\/posts\/9887\/revisions\/9912"}],"wp:attachment":[{"href":"https:\/\/agora.xtec.cat\/inscaterinaalbert\/wp-json\/wp\/v2\/media?parent=9887"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/agora.xtec.cat\/inscaterinaalbert\/wp-json\/wp\/v2\/categories?post=9887"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/agora.xtec.cat\/inscaterinaalbert\/wp-json\/wp\/v2\/tags?post=9887"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}