{"id":22281,"date":"2026-05-17T23:28:48","date_gmt":"2026-05-17T23:28:48","guid":{"rendered":"https:\/\/stesa.com\/mapas\/?post_type=ficha&#038;p=22281"},"modified":"2026-05-17T23:28:48","modified_gmt":"2026-05-17T23:28:48","slug":"mapa-geologico-del-departamento-de-itapua","status":"publish","type":"ficha","link":"https:\/\/stesa.com\/mapas\/doc\/mapa-geologico-del-departamento-de-itapua\/","title":{"rendered":"Mapa geol\u00f3gico del departamento de Itap\u00faa"},"content":{"rendered":"<p style=\"text-align: center;\"><label style=\"font-size: 15px;\">Mapa geol\u00f3gico del departamento de Itap\u00faa.<\/label><\/p>\n<p><strong>Geolog\u00eda del departamento de Itap\u00faa<\/strong><\/p>\n<p>La geolog\u00eda del departamento de Itap\u00faa est\u00e1 dominada por formaciones sedimentarias y volc\u00e1nicas asociadas a la cuenca del Paran\u00e1. El territorio presenta rocas bas\u00e1lticas, areniscas y dep\u00f3sitos aluviales que han dado origen a algunos de los suelos m\u00e1s f\u00e9rtiles de Paraguay.<\/p>\n<p><strong>Caracter\u00edsticas geol\u00f3gicas generales<\/strong><\/p>\n<p>Itap\u00faa forma parte de la gran cuenca geol\u00f3gica del Paran\u00e1, una de las estructuras geol\u00f3gicas m\u00e1s extensas de Sudam\u00e9rica.<\/p>\n<p>La evoluci\u00f3n del relieve estuvo influida por:<\/p>\n<ul>\n<li>actividad volc\u00e1nica antigua;<\/li>\n<li>sedimentaci\u00f3n;<\/li>\n<li>erosi\u00f3n fluvial;<\/li>\n<li>movimientos tect\u00f3nicos muy antiguos.<\/li>\n<\/ul>\n<p><strong>Rocas bas\u00e1lticas<\/strong><\/p>\n<p>Las rocas m\u00e1s representativas del departamento son los basaltos originados por enormes derrames volc\u00e1nicos ocurridos durante el per\u00edodo Mesozoico.<\/p>\n<p>Estas rocas:<\/p>\n<ul>\n<li>poseen color oscuro;<\/li>\n<li>son resistentes a la erosi\u00f3n;<\/li>\n<li>generan suelos muy f\u00e9rtiles.<\/li>\n<\/ul>\n<p>Gran parte del paisaje agr\u00edcola del departamento se desarrolla sobre estas formaciones bas\u00e1lticas.<\/p>\n<p><strong>Areniscas<\/strong><\/p>\n<p>Tambi\u00e9n existen capas de areniscas rojizas asociadas a antiguos ambientes sedimentarios.<\/p>\n<p>Estas formaciones aparecen en:<\/p>\n<ul>\n<li>colinas;<\/li>\n<li>zonas erosionadas;<\/li>\n<li>valles fluviales.<\/li>\n<\/ul>\n<p><strong>Dep\u00f3sitos aluviales<\/strong><\/p>\n<p>En las \u00e1reas cercanas al R\u00edo Paran\u00e1 y otros cursos de agua predominan dep\u00f3sitos recientes de:<\/p>\n<ul>\n<li>arena;<\/li>\n<li>limo;<\/li>\n<li>arcilla;<\/li>\n<li>grava.<\/li>\n<\/ul>\n<p>Estos sedimentos fueron transportados por r\u00edos y arroyos a lo largo de miles de a\u00f1os.<\/p>\n<p><strong>Relaci\u00f3n con los suelos<\/strong><\/p>\n<p>La descomposici\u00f3n de basaltos origin\u00f3 los famosos suelos rojizos f\u00e9rtiles de Itap\u00faa.<\/p>\n<p>Estos suelos son ideales para:<\/p>\n<ul>\n<li>agricultura mecanizada;<\/li>\n<li>soja;<\/li>\n<li>trigo;<\/li>\n<li>ma\u00edz;<\/li>\n<li>yerba mate;<\/li>\n<li>forestaci\u00f3n.<\/li>\n<\/ul>\n<p><strong>Recursos minerales<\/strong><\/p>\n<p>El departamento posee principalmente minerales no met\u00e1licos utilizados en:<\/p>\n<ul>\n<li>construcci\u00f3n;<\/li>\n<li>extracci\u00f3n de piedra;<\/li>\n<li>fabricaci\u00f3n de ladrillos y cer\u00e1mica.<\/li>\n<\/ul>\n<p>En algunas zonas existen canteras de roca bas\u00e1ltica.<\/p>\n<p><strong>Hidrogeolog\u00eda<\/strong><\/p>\n<p>Las capas volc\u00e1nicas fracturadas y las areniscas permiten el almacenamiento de aguas subterr\u00e1neas.<\/p>\n<p>Parte del territorio est\u00e1 relacionado con el Acu\u00edfero Guaran\u00ed, una de las mayores reservas de agua dulce subterr\u00e1nea del mundo.<\/p>\n<p><strong>Influencia del r\u00edo Paran\u00e1<\/strong><\/p>\n<p>El R\u00edo Paran\u00e1 ha desempe\u00f1ado un papel fundamental en:<\/p>\n<ul>\n<li>la erosi\u00f3n del relieve;<\/li>\n<li>la formaci\u00f3n de terrazas fluviales;<\/li>\n<li>la acumulaci\u00f3n de sedimentos;<\/li>\n<li>y la configuraci\u00f3n del paisaje actual.<\/li>\n<\/ul>\n<p><strong>Paisaje geol\u00f3gico<\/strong><\/p>\n<p>La combinaci\u00f3n de:<\/p>\n<ul>\n<li>mesetas bas\u00e1lticas;<\/li>\n<li>valles fluviales;<\/li>\n<li>colinas onduladas;<\/li>\n<li>y \u00e1reas agr\u00edcolas<\/li>\n<\/ul>\n<p>ha creado uno de los paisajes geol\u00f3gicos y productivos m\u00e1s importantes del Paraguay.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>La geolog\u00eda del departamento de Itap\u00faa est\u00e1 dominada por formaciones sedimentarias y volc\u00e1nicas asociadas a la cuenca del Paran\u00e1. El territorio presenta rocas <\/p>\n","protected":false},"author":1,"featured_media":22283,"template":"","categoria_ficha":[2234],"class_list":["post-22281","ficha","type-ficha","status-publish","has-post-thumbnail","hentry","categoria_ficha-mapas-del-departamento-de-itapua"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.4 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Mapa geol\u00f3gico del departamento de Itap\u00faa - Galer\u00eda de mapas<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/stesa.com\/mapas\/doc\/mapa-geologico-del-departamento-de-itapua\/\" \/>\n<meta property=\"og:locale\" content=\"es_ES\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Mapa geol\u00f3gico del departamento de Itap\u00faa - Galer\u00eda de mapas\" \/>\n<meta property=\"og:description\" content=\"La geolog\u00eda del departamento de Itap\u00faa est\u00e1 dominada por formaciones sedimentarias y volc\u00e1nicas asociadas a la cuenca del Paran\u00e1. 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