{"id":21882,"date":"2026-05-14T14:27:32","date_gmt":"2026-05-14T14:27:32","guid":{"rendered":"https:\/\/stesa.com\/mapas\/?post_type=ficha&#038;p=21882"},"modified":"2026-05-14T14:27:32","modified_gmt":"2026-05-14T14:27:32","slug":"mapa-geologico-del-departamento-de-alto-parana","status":"publish","type":"ficha","link":"https:\/\/stesa.com\/mapas\/doc\/mapa-geologico-del-departamento-de-alto-parana\/","title":{"rendered":"Mapa geol\u00f3gico del departamento de Alto Paran\u00e1"},"content":{"rendered":"<p style=\"text-align: center;\"><label style=\"font-size: 15px;\">Mapa geol\u00f3gico del departamento de Alto Paran\u00e1.<\/label><\/p>\n<p><strong>Geolog\u00eda del departamento de Alto Paran\u00e1<\/strong><\/p>\n<p>La geolog\u00eda del departamento de Alto Paran\u00e1 est\u00e1 dominada por formaciones bas\u00e1lticas, rocas sedimentarias y suelos rojos muy f\u00e9rtiles, caracter\u00edsticos de la Regi\u00f3n Oriental de Paraguay. El departamento forma parte de la gran cuenca geol\u00f3gica del Paran\u00e1, una de las m\u00e1s extensas de Am\u00e9rica del Sur.<\/p>\n<p><strong>Estructura geol\u00f3gica<\/strong><\/p>\n<p>El territorio pertenece principalmente a la:<\/p>\n<ul>\n<li>Cuenca del Paran\u00e1;<\/li>\n<li>meseta bas\u00e1ltica oriental paraguaya.<\/li>\n<\/ul>\n<p>Estas estructuras se originaron por intensos procesos volc\u00e1nicos y sedimentarios ocurridos durante la era mesozoica.<\/p>\n<p><strong>Rocas predominantes<\/strong><\/p>\n<p><strong>Basaltos<\/strong><\/p>\n<p>Las rocas m\u00e1s abundantes son los basaltos, originados por grandes derrames de lava volc\u00e1nica relacionados con la Formaci\u00f3n Serra Geral.<\/p>\n<p>Caracter\u00edsticas:<\/p>\n<ul>\n<li>color oscuro;<\/li>\n<li>gran dureza;<\/li>\n<li>alta riqueza mineral;<\/li>\n<li>origen \u00edgneo volc\u00e1nico.<\/li>\n<\/ul>\n<p>Estas rocas cubren gran parte del este paraguayo y son responsables de los famosos suelos rojos f\u00e9rtiles.<\/p>\n<p><strong>Rocas sedimentarias<\/strong><\/p>\n<p>Tambi\u00e9n existen:<\/p>\n<ul>\n<li>areniscas;<\/li>\n<li>limolitas;<\/li>\n<li>sedimentos fluviales recientes.<\/li>\n<\/ul>\n<p>Las areniscas pertenecen principalmente a antiguas formaciones depositadas antes de los eventos volc\u00e1nicos.<\/p>\n<p><strong>Suelos<\/strong><\/p>\n<p>Los suelos predominantes son:<\/p>\n<ul>\n<li>later\u00edticos;<\/li>\n<li>rojos;<\/li>\n<li>profundos;<\/li>\n<li>ricos en hierro y aluminio.<\/li>\n<\/ul>\n<p>Estos suelos derivan de la meteorizaci\u00f3n del basalto y favorecen el desarrollo agr\u00edcola intensivo.<\/p>\n<p><strong>Relaci\u00f3n con el relieve<\/strong><\/p>\n<p>La geolog\u00eda influye directamente en:<\/p>\n<ul>\n<li>las colinas onduladas;<\/li>\n<li>los valles fluviales;<\/li>\n<li>las cascadas y saltos de agua.<\/li>\n<\/ul>\n<p>Los Saltos del Monday y otros saltos se formaron por la erosi\u00f3n diferencial de las capas bas\u00e1lticas.<\/p>\n<p><strong>Recursos minerales<\/strong><\/p>\n<p>Aunque Alto Paran\u00e1 no es una gran regi\u00f3n minera, posee:<\/p>\n<ul>\n<li>materiales de construcci\u00f3n;<\/li>\n<li>piedra bas\u00e1ltica;<\/li>\n<li>arcillas;<\/li>\n<li>arena y grava fluvial.<\/li>\n<\/ul>\n<p>El basalto es utilizado en:<\/p>\n<ul>\n<li>carreteras;<\/li>\n<li>pavimentaci\u00f3n;<\/li>\n<li>obras civiles.<\/li>\n<\/ul>\n<p><strong>Hidrogeolog\u00eda<\/strong><\/p>\n<p>El departamento se encuentra sobre \u00e1reas vinculadas al:<\/p>\n<ul>\n<li>Sistema Acu\u00edfero Guaran\u00ed.<\/li>\n<\/ul>\n<p>Este acu\u00edfero es una de las reservas subterr\u00e1neas de agua dulce m\u00e1s grandes del mundo.<\/p>\n<p><strong>Importancia geol\u00f3gica y econ\u00f3mica<\/strong><\/p>\n<p>La geolog\u00eda de Alto Paran\u00e1 favorece:<\/p>\n<ul>\n<li>agricultura altamente productiva;<\/li>\n<li>abundancia h\u00eddrica;<\/li>\n<li>generaci\u00f3n hidroel\u00e9ctrica;<\/li>\n<li>disponibilidad de materiales para infraestructura.<\/li>\n<\/ul>\n<p>Adem\u00e1s, las formaciones bas\u00e1lticas contribuyen al gran potencial hidroel\u00e9ctrico del R\u00edo Paran\u00e1, aprovechado por la Represa de Itaip\u00fa.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>La geolog\u00eda del departamento de Alto Paran\u00e1 est\u00e1 dominada por formaciones bas\u00e1lticas, rocas sedimentarias y suelos rojos muy f\u00e9rtiles, caracter\u00edsticos de la &#8230;<\/p>\n","protected":false},"author":1,"featured_media":21883,"template":"","categoria_ficha":[2237],"class_list":["post-21882","ficha","type-ficha","status-publish","has-post-thumbnail","hentry","categoria_ficha-mapas-del-departamento-de-alto-parana"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.4 - 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