{"id":22129,"date":"2026-05-17T00:46:14","date_gmt":"2026-05-17T00:46:14","guid":{"rendered":"https:\/\/stesa.com\/mapas\/?post_type=ficha&#038;p=22129"},"modified":"2026-05-17T00:46:14","modified_gmt":"2026-05-17T00:46:14","slug":"mapa-geologico-del-departamento-central-paraguay","status":"publish","type":"ficha","link":"https:\/\/stesa.com\/mapas\/doc\/mapa-geologico-del-departamento-central-paraguay\/","title":{"rendered":"Mapa geol\u00f3gico del departamento Central (Paraguay)"},"content":{"rendered":"<p style=\"text-align: center;\"><label style=\"font-size: 15px;\">Mapa geol\u00f3gico del departamento Central.<\/label><\/p>\n<p><strong>Geolog\u00eda del departamento Central<\/strong><\/p>\n<p>La geolog\u00eda del departamento Central est\u00e1 formada principalmente por rocas sedimentarias, dep\u00f3sitos aluviales y materiales de origen volc\u00e1nico antiguo vinculados a la cuenca del r\u00edo Paraguay y a la evoluci\u00f3n geol\u00f3gica de la Regi\u00f3n Oriental del Paraguay.<\/p>\n<p><strong>Caracter\u00edsticas geol\u00f3gicas generales<\/strong><\/p>\n<p>El departamento se ubica en una zona de transici\u00f3n entre \u00e1reas sedimentarias y antiguas formaciones volc\u00e1nicas.<\/p>\n<p>El subsuelo est\u00e1 compuesto por:<\/p>\n<ul>\n<li>areniscas,<\/li>\n<li>arcillas,<\/li>\n<li>limos,<\/li>\n<li>conglomerados,<\/li>\n<li>y dep\u00f3sitos aluviales recientes.<\/li>\n<\/ul>\n<p>Estas formaciones fueron originadas por procesos fluviales y sedimentarios desarrollados durante millones de a\u00f1os.<\/p>\n<p><strong>Rocas sedimentarias<\/strong><\/p>\n<p>Predominan las rocas sedimentarias pertenecientes a formaciones geol\u00f3gicas de la cuenca del Paran\u00e1.<\/p>\n<p>Las principales rocas incluyen:<\/p>\n<ul>\n<li>areniscas rojizas,<\/li>\n<li>lutitas,<\/li>\n<li>limolitas,<\/li>\n<li>y arcillas sedimentarias.<\/li>\n<\/ul>\n<p>Estas rocas afloran en varias zonas del departamento y sirven de base para los suelos agr\u00edcolas y urbanos.<\/p>\n<p><strong>Dep\u00f3sitos aluviales<\/strong><\/p>\n<p>A lo largo del R\u00edo Paraguay y de numerosos arroyos existen dep\u00f3sitos aluviales modernos formados por:<\/p>\n<ul>\n<li>arena,<\/li>\n<li>limo,<\/li>\n<li>arcilla,<\/li>\n<li>y sedimentos fluviales.<\/li>\n<\/ul>\n<p>Estos materiales generan:<\/p>\n<ul>\n<li>llanuras inundables,<\/li>\n<li>humedales,<\/li>\n<li>y terrenos bajos cercanos al r\u00edo.<\/li>\n<\/ul>\n<p><strong>Influencia volc\u00e1nica antigua<\/strong><\/p>\n<p>En algunas \u00e1reas aparecen materiales relacionados con antiguos eventos volc\u00e1nicos de la cuenca del Paran\u00e1, aunque menos extensos que en el este del Paraguay.<\/p>\n<p>Estos materiales contribuyen a la fertilidad de ciertos suelos del departamento.<\/p>\n<p><strong>Suelos<\/strong><\/p>\n<p>Los suelos predominantes son:<\/p>\n<ul>\n<li>franco-arcillosos,<\/li>\n<li>arcillosos,<\/li>\n<li>y aluviales.<\/li>\n<\/ul>\n<p>Son adecuados para:<\/p>\n<ul>\n<li>horticultura,<\/li>\n<li>agricultura intensiva,<\/li>\n<li>fruticultura,<\/li>\n<li>y urbanizaci\u00f3n.<\/li>\n<\/ul>\n<p><strong>Relaci\u00f3n entre geolog\u00eda y relieve<\/strong><\/p>\n<p>La geolog\u00eda explica el relieve suavemente ondulado del departamento:<\/p>\n<ul>\n<li>las areniscas forman lomadas bajas,<\/li>\n<li>los dep\u00f3sitos fluviales originan planicies,<\/li>\n<li>y los sedimentos recientes generan zonas pantanosas e inundables.<\/li>\n<\/ul>\n<p><strong>Recursos naturales<\/strong><\/p>\n<p>Entre los principales recursos geol\u00f3gicos se encuentran:<\/p>\n<ul>\n<li>arena para construcci\u00f3n,<\/li>\n<li>arcilla utilizada en ladriller\u00edas,<\/li>\n<li>agua subterr\u00e1nea,<\/li>\n<li>y suelos f\u00e9rtiles.<\/li>\n<\/ul>\n<p><strong>Problemas ambientales relacionados<\/strong><\/p>\n<p>La intensa urbanizaci\u00f3n del departamento ha provocado:<\/p>\n<ul>\n<li>erosi\u00f3n del suelo,<\/li>\n<li>sedimentaci\u00f3n de arroyos,<\/li>\n<li>contaminaci\u00f3n de aguas,<\/li>\n<li>y extracci\u00f3n excesiva de materiales de construcci\u00f3n en algunas zonas.<\/li>\n<\/ul>\n<p>Estos problemas afectan especialmente a la cuenca del Lago Ypacara\u00ed y a los arroyos metropolitanos.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>La geolog\u00eda del departamento Central est\u00e1 formada principalmente por rocas sedimentarias, dep\u00f3sitos aluviales y materiales de origen volc\u00e1nico antiguo &#8230;<\/p>\n","protected":false},"author":1,"featured_media":22130,"template":"","categoria_ficha":[2238],"class_list":["post-22129","ficha","type-ficha","status-publish","has-post-thumbnail","hentry","categoria_ficha-mapas-del-departamento-central"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.4 - 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