{"id":22037,"date":"2026-05-16T00:41:23","date_gmt":"2026-05-16T00:41:23","guid":{"rendered":"https:\/\/stesa.com\/mapas\/?post_type=ficha&#038;p=22037"},"modified":"2026-05-16T00:41:23","modified_gmt":"2026-05-16T00:41:23","slug":"mapa-geologico-del-departamento-de-caazapa","status":"publish","type":"ficha","link":"https:\/\/stesa.com\/mapas\/doc\/mapa-geologico-del-departamento-de-caazapa\/","title":{"rendered":"Mapa geol\u00f3gico del departamento de Caazap\u00e1"},"content":{"rendered":"<p style=\"text-align: center;\"><label style=\"font-size: 15px;\">Mapa geol\u00f3gico del departamento de Caazap\u00e1.<\/label><\/p>\n<p><strong>Geolog\u00eda del departamento de Caazap\u00e1<\/strong><\/p>\n<p>La geolog\u00eda del departamento de Caazap\u00e1 est\u00e1 asociada principalmente a la cuenca del Paran\u00e1, una gran formaci\u00f3n geol\u00f3gica sudamericana compuesta por rocas volc\u00e1nicas y sedimentarias. Estas estructuras han originado suelos f\u00e9rtiles y paisajes ondulados caracter\u00edsticos del Paraguay oriental.<\/p>\n<p><strong>Caracter\u00edsticas geol\u00f3gicas principales<\/strong><\/p>\n<p><strong>1. Rocas bas\u00e1lticas<\/strong><\/p>\n<p>Gran parte del departamento est\u00e1 formada por basaltos originados durante intensas actividades volc\u00e1nicas del per\u00edodo Jur\u00e1sico\u2013Cret\u00e1cico.<\/p>\n<p>Caracter\u00edsticas:<\/p>\n<ul>\n<li>Rocas volc\u00e1nicas oscuras y resistentes.<\/li>\n<li>Formadas por antiguas coladas de lava.<\/li>\n<li>Relacionadas con la provincia bas\u00e1ltica de la Cuenca del Paran\u00e1.<\/li>\n<\/ul>\n<p>Los basaltos generan:<\/p>\n<ul>\n<li>Suelos rojos f\u00e9rtiles.<\/li>\n<li>Relieves ondulados.<\/li>\n<li>Colinas y lomadas suaves.<\/li>\n<\/ul>\n<p><strong>2. Rocas sedimentarias<\/strong><\/p>\n<p>En algunas zonas aparecen:<\/p>\n<ul>\n<li>Areniscas.<\/li>\n<li>Lutitas.<\/li>\n<li>Sedimentos antiguos.<\/li>\n<\/ul>\n<p>Las areniscas permiten:<\/p>\n<ul>\n<li>Mayor infiltraci\u00f3n de agua.<\/li>\n<li>Formaci\u00f3n de acu\u00edferos subterr\u00e1neos.<\/li>\n<li>Desarrollo de valles y pendientes suaves.<\/li>\n<\/ul>\n<p><strong>3. Relieve geol\u00f3gico<\/strong><\/p>\n<p>La interacci\u00f3n entre basaltos, areniscas y erosi\u00f3n natural ha producido:<\/p>\n<ul>\n<li>Colinas.<\/li>\n<li>Valles fluviales.<\/li>\n<li>Llanuras f\u00e9rtiles.<\/li>\n<li>Sectores boscosos elevados.<\/li>\n<\/ul>\n<p><strong>4. Suelos<\/strong><\/p>\n<p>Los suelos del departamento son:<\/p>\n<ul>\n<li>Profundos.<\/li>\n<li>Ricos en hierro y minerales.<\/li>\n<li>De color rojizo.<\/li>\n<\/ul>\n<p>Son aptos para:<\/p>\n<ul>\n<li>Agricultura intensiva.<\/li>\n<li>Ganader\u00eda.<\/li>\n<li>Actividades forestales.<\/li>\n<\/ul>\n<p><strong>5. Recursos h\u00eddricos subterr\u00e1neos<\/strong><\/p>\n<p>Caazap\u00e1 integra parte del sistema asociado al Acu\u00edfero Guaran\u00ed.<\/p>\n<p>Este acu\u00edfero:<\/p>\n<ul>\n<li>Contiene importantes reservas de agua subterr\u00e1nea.<\/li>\n<li>Se desarrolla principalmente en formaciones areniscas.<\/li>\n<li>Tiene relevancia para abastecimiento y producci\u00f3n agropecuaria.<\/li>\n<\/ul>\n<p><strong>Recursos minerales<\/strong><\/p>\n<p>Entre los recursos geol\u00f3gicos presentes se encuentran:<\/p>\n<ul>\n<li>Arcilla.<\/li>\n<li>Arena.<\/li>\n<li>Piedra bas\u00e1ltica.<\/li>\n<li>Materiales utilizados en construcci\u00f3n.<\/li>\n<\/ul>\n<p>La piedra bas\u00e1ltica se utiliza para:<\/p>\n<ul>\n<li>Pavimentaci\u00f3n.<\/li>\n<li>Obras viales.<\/li>\n<li>Construcci\u00f3n civil.<\/li>\n<\/ul>\n<p><strong>Influencia sobre la econom\u00eda<\/strong><\/p>\n<p>La geolog\u00eda favorece:<\/p>\n<ul>\n<li>Agricultura mecanizada.<\/li>\n<li>Producci\u00f3n forestal.<\/li>\n<li>Ganader\u00eda.<\/li>\n<li>Desarrollo de infraestructura vial y urbana.<\/li>\n<\/ul>\n<p><strong>Importancia geol\u00f3gica<\/strong><\/p>\n<p>La estructura geol\u00f3gica de Caazap\u00e1 es importante porque:<\/p>\n<ul>\n<li>Determina la fertilidad de los suelos.<\/li>\n<li>Influye en el relieve y la hidrograf\u00eda.<\/li>\n<li>Favorece la disponibilidad de agua subterr\u00e1nea.<\/li>\n<li>Sustenta actividades econ\u00f3micas fundamentales del departamento.<\/li>\n<\/ul>\n","protected":false},"excerpt":{"rendered":"<p>La geolog\u00eda del departamento de Caazap\u00e1 est\u00e1 asociada principalmente a la cuenca del Paran\u00e1, una gran formaci\u00f3n geol\u00f3gica sudamericana compuesta por rocas &#8230;<\/p>\n","protected":false},"author":1,"featured_media":22038,"template":"","categoria_ficha":[2233],"class_list":["post-22037","ficha","type-ficha","status-publish","has-post-thumbnail","hentry","categoria_ficha-mapas-del-departamento-de-caazapa"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.4 - 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