{"id":8399,"date":"2016-04-01T09:23:00","date_gmt":"2016-04-01T08:23:00","guid":{"rendered":"http:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/general\/de-malpas-a-erillcastell\/"},"modified":"2016-07-11T10:15:54","modified_gmt":"2016-07-11T09:15:54","slug":"de-malpas-a-erillcastell","status":"publish","type":"post","link":"https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/general\/de-malpas-a-erillcastell\/","title":{"rendered":"De Malp\u00e0s a Erillcastell"},"content":{"rendered":"<p style=\"text-align: left;\"><strong><span style=\"font-family: 'arial' , 'helvetica' , sans-serif;\">IES Lladonosa, Lleida<\/span><\/strong><\/p>\n<p style=\"text-align: center;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-8524 size-large aligncenter\" src=\"http:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/reillcastell-1024x768.jpg\" alt=\"reillcastell\" width=\"1024\" height=\"768\" srcset=\"https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/reillcastell-1024x768.jpg 1024w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/reillcastell-300x225.jpg 300w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/reillcastell-768x576.jpg 768w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/reillcastell-200x150.jpg 200w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/p>\n<p><b>Erillcastell<\/b> \u00e9s un poble de la comarca de l&#8217;<a title=\"Alta Ribagor\u00e7a\" href=\"https:\/\/www.blogger.com\/null\">Alta Ribagor\u00e7a<\/a>, i pertany al terme municipal del <a title=\"Pont de Suert\" href=\"https:\/\/www.blogger.com\/null\">Pont de Suert<\/a>. Antigament pertanyia al terme municipal de <a title=\"Malp\u00e0s (antic municipi)\" href=\"https:\/\/www.blogger.com\/null\">Malp\u00e0s<\/a>. Des de sempre, Erillcastell ha tingut un acc\u00e9s dif\u00edcil, que s&#8217;ha agreujat en quedar deshabitat.<\/p>\n<p>Erillcastell t\u00e9 una <b>identitat hist\u00f2rica<\/b> molt important, lligat amb l&#8217;antiguitat de la fam\u00edlia d&#8217;Erill. El castell est\u00e0 datat el 1024, i va ser donat als Erill el 1040. El primer membre conegut va ser Ramon I d&#8217;Erill, documentat el 1077. Els Erill eren s\u00fabdits dels comtes de Pallars, per\u00f2 no s&#8217;acontentaren amb l&#8217;actuaci\u00f3 a les seves terres, i passaren al servei directe dels reis d&#8217;Arag\u00f3 (fi del segle XI). Intervingueren en la conquesta de les terres lleidatanes (reberen Fraga, Almenar i altres llocs), i enlla\u00e7aren amb poderoses fam\u00edlies. Cal destacar que Berenguer d&#8217;Erill fou un destacat bisbe de Lleida (1205 &#8211; 1236) i conseller de Jaume I. La baronia d&#8217;Erill, amb centre inicial a Erillcastell, comprenia la vall de Bo\u00ed (on emprengueren la construcci\u00f3 de les esgl\u00e9sies rom\u00e0niques de la vall de Bo\u00ed), la vall de Viu, de Manyanet i la Vall Fosca, aix\u00ed com la ribera oriental de la Noguera Ribagor\u00e7ana entre el Pont de Suert i Espills.<\/p>\n<p>Amb els i les alumnes\u00a0 de segon de batxillerat de l&#8217;IES Lladonosa hem fet un magn\u00edfic itinerari per arribar al poble, on hi destaca l<b>&#8216;inter\u00e8s geol\u00f2gic<\/b> de l&#8217;indret.\u00a0 Aquesta \u00e9s una geozona de valor \u00fanic a nivell planetari: en destaca el conjunt d&#8217;afloraments de roques volc\u00e0niques calco-alcalines del Carbon\u00edfer Superior. La import\u00e0ncia geol\u00f2gica de la zona es remarca a Mart\u00ed (ignimbrites), on es d\u00f3na un breu informe sobre l\u2019inter\u00e8s de la contrada citant que:\u00a0<i>\u201cl\u2019observaci\u00f3 i estudi d\u2019aquesta geozona permet con\u00e8ixer la relaci\u00f3 entre el vulcanisme i el context estructural que condicion\u00e0 la creaci\u00f3 de les conques carbon\u00edferes al Pirineu, i tamb\u00e9 i de manera m\u00e9s general la din\u00e0mica de les grans erupcions volc\u00e0niques explosives\u201d.<\/i><\/p>\n<p>Durant l&#8217;itinerari, hem pogut observar materials com:<\/p>\n<div>\u2013 metasediments paleozoics (Devoni\u00e0)<\/div>\n<p>&nbsp;<\/p>\n<div>\u2013 dip\u00f2sits volc\u00e0nics i vulcano-sedimentaris carbon\u00edfers i permians (Estefani\u00e0 i Autuni\u00e0)<\/div>\n<p>&nbsp;<\/p>\n<div>\u2013 sediments i carbons carbon\u00edfers (Estefani\u00e0 inferior i superior)<\/div>\n<p>&nbsp;<\/p>\n<div>\u2013 sediments permians (Autuni\u00e0)<\/div>\n<p>&nbsp;<\/p>\n<div>\u2013 discordan\u00e7a angular (Tri\u00e0sic inferior)<\/div>\n<p>&nbsp;<\/p>\n<div>\u2013 sediments tri\u00e0sics (Tri\u00e0sic inferior)<\/div>\n<p>&nbsp;<\/p>\n<div>\u2013 roques subvolc\u00e0niques tri\u00e0siques (Tri\u00e0sic superior)<\/div>\n<div><\/div>\n<figure id=\"attachment_8521\" aria-describedby=\"caption-attachment-8521\" style=\"width: 768px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/IMG_20160401_232930-1.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-8521 size-large\" src=\"http:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/IMG_20160401_232930-1-768x1024.jpg\" alt=\"IMG_20160401_232930\" width=\"768\" height=\"1024\" srcset=\"https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/IMG_20160401_232930-1-768x1024.jpg 768w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/IMG_20160401_232930-1-225x300.jpg 225w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/IMG_20160401_232930-1.jpg 1920w\" sizes=\"auto, (max-width: 768px) 100vw, 768px\" \/><\/a><figcaption id=\"caption-attachment-8521\" class=\"wp-caption-text\">Empremtes de l&#8217;activitat volc\u00e0nica que es va produir en aquesta zona fa uns 300 milions d&#8217;anys: bombes i cendres volc\u00e0niques<\/figcaption><\/figure>\n<p>&nbsp;<\/p>\n<figure id=\"attachment_8526\" aria-describedby=\"caption-attachment-8526\" style=\"width: 1024px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/fossil.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-8526 size-large\" src=\"http:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/fossil-1024x768.jpg\" alt=\"fossil\" width=\"1024\" height=\"768\" srcset=\"https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/fossil-1024x768.jpg 1024w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/fossil-300x225.jpg 300w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/fossil-768x576.jpg 768w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/fossil-200x150.jpg 200w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption id=\"caption-attachment-8526\" class=\"wp-caption-text\">F\u00f2ssils de vegetaci\u00f3 entre sediments del Carbon\u00edfer<\/figcaption><\/figure>\n<p>&nbsp;<\/p>\n<figure id=\"attachment_8522\" aria-describedby=\"caption-attachment-8522\" style=\"width: 1024px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/IMG_20160401_141009-1.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-8522 size-large\" src=\"http:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/IMG_20160401_141009-1-1024x768.jpg\" alt=\"IMG_20160401_141009\" width=\"1024\" height=\"768\" srcset=\"https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/IMG_20160401_141009-1-1024x768.jpg 1024w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/IMG_20160401_141009-1-300x225.jpg 300w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/IMG_20160401_141009-1-768x576.jpg 768w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/IMG_20160401_141009-1-200x150.jpg 200w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption id=\"caption-attachment-8522\" class=\"wp-caption-text\">Erillcastell, i al fons, observem discordan\u00e7a angular (estrats del Carbon\u00edfer, foscos, a la part inferior, als quals se superposen els del Tri\u00e0sic, de to rogenc)<\/figcaption><\/figure>\n<figure id=\"attachment_8525\" aria-describedby=\"caption-attachment-8525\" style=\"width: 768px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/tussilago.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-8525 size-large\" src=\"http:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/tussilago-768x1024.jpg\" alt=\"tussilago\" width=\"768\" height=\"1024\" srcset=\"https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/tussilago-768x1024.jpg 768w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/tussilago-225x300.jpg 225w, https:\/\/serveiseducatius.xtec.cat\/cda-valldeboi\/wp-content\/uploads\/usu1369\/2016\/04\/tussilago.jpg 1920w\" sizes=\"auto, (max-width: 768px) 100vw, 768px\" \/><\/a><figcaption id=\"caption-attachment-8525\" class=\"wp-caption-text\">Flor de tartera: Tussilago farfara<\/figcaption><\/figure>\n<p><span style=\"font-family: 'arial' , 'helvetica' , sans-serif;\"><br \/>\n<\/span><\/p>\n<p style=\"text-align: justify;\">El Permi\u00e0 fou una \u00e8poca geol\u00f2gica de gran activitat tect\u00f2nica. En aquesta zona hi trobem un cas de vulcanisme; per\u00f2 tamb\u00e9 les granodiorites de la zona axial s\u00f3n del Permi\u00e0, tan antigues com les enormes erupcions siberianes que localment presenten colades de lava bas\u00e0ltica de fins a 4 km de gruix. Tot plegat va ser la manifestaci\u00f3 de la fragmentaci\u00f3 de Pangea i Gondwana, i principalment a partir d&#8217;aquest pic d&#8217;activitat volc\u00e0nica es va originar el canvi clim\u00e0tic global que va dur a l&#8217;extinci\u00f3 massiva del Permi\u00e0, amb la desaparici\u00f3 de formes vives m\u00e9s gran que s&#8217;ha conegut mai. La ra\u00f3 directa del desastre va ser una pres\u00e8ncia d&#8217;oxigen a l&#8217;atmosfera de nom\u00e9s 16-12%, un excessiu efecte hivernacle (CO2, CH4 i SO2) hi va ajudar, mitjan\u00e7ant un increment de l&#8217;absorci\u00f3 de la calor de la superf\u00edcie terrestre que va comportar la fosa de les grans glaceres de l&#8217;Ant\u00e0rtic i de Gondwana. El drama que es posa de manifest en aquesta secci\u00f3 va ser realment un esdeveniment de primer ordre a nivell planetari, perqu\u00e8 en va resultar l\u2019extinci\u00f3 d\u2019un 90% de les esp\u00e8cies del moment.<\/p>\n<p style=\"text-align: right;\">Font: ctfc.cat<\/p>\n","protected":false},"excerpt":{"rendered":"<p>IES Lladonosa, Lleida Erillcastell \u00e9s un poble de la comarca de l&#8217;Alta Ribagor\u00e7a, i pertany al terme municipal del Pont [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":8524,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"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 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