{"id":4626,"date":"2025-07-02T00:18:38","date_gmt":"2025-07-02T00:18:38","guid":{"rendered":"https:\/\/www.andex-rhp.org\/?p=4626"},"modified":"2025-07-02T00:18:39","modified_gmt":"2025-07-02T00:18:39","slug":"son-propensos-los-glaciares-de-chile-central-a-desencadenar-movimientos-en-masa","status":"publish","type":"post","link":"https:\/\/www.andex-rhp.org\/?p=4626","title":{"rendered":"\u00bfSon propensos los glaciares de Chile central a desencadenar movimientos en masa?"},"content":{"rendered":"\n

Por Felipe Ugalde Peralta*\/<\/strong><\/p>\n\n\n\n

Los Andes centrales de Chile son conocidos por ser una de las zonas m\u00e1s pobladas del pa\u00eds, incluyendo la ciudad de Santiago de Chile con m\u00e1s de 8 millones de habitantes. Al mismo tiempo, esta porci\u00f3n de la cordillera abarca una amplia variedad de glaciares, entre los que se incluyen las masas de hielo m\u00e1s grandes al norte de la Patagonia. Es el caso de la cuenca del r\u00edo Volc\u00e1n (33,82\u00b0S\/70,00\u00b0W), ubicada 40 km al este de Santiago (Figura 1). Esta cuenca se caracteriza por la coexistencia de volcanismo activo, en el Complejo Volc\u00e1nico San Jos\u00e9, junto con 195 glaciares identificados a lo largo de su extensi\u00f3n (Figura 2).<\/p>\n\n\n\n

\n

En este contexto, este estudio presenta una evaluaci\u00f3n de susceptibilidad de movimientos en masa de origen glaciar en la cuenca del r\u00edo Volc\u00e1n. Se entiende por susceptibilidad la posibilidad de que ocurra, o no, una remoci\u00f3n o movimiento en masa en un \u00e1rea determinada y en funci\u00f3n de condiciones locales del terreno (tambi\u00e9n conocidas como factores condicionantes). <\/p>\n<\/blockquote>\n\n\n\n

As\u00ed, se analiza la susceptibilidad de cinco tipos de movimientos en masa a partir de un an\u00e1lisis jer\u00e1rquico de procesos mediante la determinaci\u00f3n de un \u00edndice de susceptibilidad (IS). Los fen\u00f3menos abordados incluyen avalanchas de hielo, surges (o avances s\u00fabitos de glaciares), deslizamientos catastr\u00f3ficos de glaciares de baja pendiente, vaciamiento de lagos de origen glaciar (o GLOFs por sus siglas en ingl\u00e9s, Glacial Lake Outburst Floods<\/em>) y lahares primarios (derivados de la interacci\u00f3n glaciovolc\u00e1nica). El an\u00e1lisis se aplica a 70 glaciares, correspondientes a todos los glaciares no rocosos identificados en el \u00e1rea de estudio (Figura 1 y Figura 2).<\/p>\n\n\n\n

Nuestros resultados dan cuenta que en el \u00e1rea de estudio existen glaciares altamente susceptibles ante todos los fen\u00f3menos evaluados. En particular, 10 glaciares poseen susceptibilidad alta por avalanchas de hielo, siete ante GLOFs, tres a lahares primarios, dos a deslizamientos catastr\u00f3ficos y solo uno ante surges<\/em>. Estos hallazgos son discutidos respecto a la evaluaci\u00f3n del peligro y riesgo que representan, a su vez que son comparados con estudios previamente publicados en la literatura cient\u00edfica. La propuesta metodol\u00f3gica es una primera etapa respecto a la gesti\u00f3n del riesgo de origen glaciar en la regi\u00f3n y cuenta con el potencial de ser ampliamente replicada en otras regiones andinas.<\/p>\n\n\n\n

\"Figura
Figura 1. Glaciares del \u00e1rea de estudio y principales asentamientos en la cuenca del r\u00edo Volc\u00e1n. Letras rojas indican los glaciares presentados en la Figura 2: A) Glaciar El Morado, B) Glaciar Mu\u00f1iri, C) Glaciar San Francisco, D) Glaciar Nieves Negras, E) Glaciar Loma Larga y F) Glaciar Cortaderas<\/figcaption><\/figure>\n\n\n\n
\"Figura
Figura 2. Glaciares de la cuenca del r\u00edo Volc\u00e1n. A) Glaciar y lago proglaciar El Morado. B) Cerro San Francisco y glaciar, y cerro, El Morado. C) Glaciar Nieves Negras en la cara sur del volc\u00e1n San Jos\u00e9. D) Glaciar Mu\u00f1iri y glaciares cubiertos Loma Larga y Cortaderas con el cerro Loma Larga de fondo.<\/figcaption><\/figure>\n\n\n\n
\n\n\n\n

*Departamento de Geolog\u00eda, Facultad de Ciencias F\u00edsicas y Matem\u00e1ticas, Universidad de Chile<\/p>\n\n\n\n

\n\n\n\n

Ugalde, F., and Sep\u00falveda, S. A. (2025). Susceptibility assessment for glacier hazards in the Volc\u00e1n catchment (33.82\u00b0 S\/70.00\u00b0 W), Central Andes of Chile. Journal of South American Earth Sciences, 105581. https:\/\/doi.org\/10.1016\/j.jsames.2025.105581<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

Por Felipe Ugalde Peralta*\/ Los Andes centrales de Chile son conocidos por ser una de las zonas m\u00e1s pobladas del pa\u00eds, incluyendo la ciudad de Santiago de Chile con m\u00e1s de 8 millones de habitantes. Al mismo tiempo, esta porci\u00f3n de la cordillera abarca una amplia variedad de glaciares, entre los que se incluyen las […]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"ocean_post_layout":"","ocean_both_sidebars_style":"","ocean_both_sidebars_content_width":0,"ocean_both_sidebars_sidebars_width":0,"ocean_sidebar":"","ocean_second_sidebar":"","ocean_disable_margins":"enable","ocean_add_body_class":"","ocean_shortcode_before_top_bar":"","ocean_shortcode_after_top_bar":"","ocean_shortcode_before_header":"","ocean_shortcode_after_header":"","ocean_has_shortcode":"","ocean_shortcode_after_title":"","ocean_shortcode_before_footer_widgets":"","ocean_shortcode_after_footer_widgets":"","ocean_shortcode_before_footer_bottom":"","ocean_shortcode_after_footer_bottom":"","ocean_display_top_bar":"default","ocean_display_header":"default","ocean_header_style":"","ocean_center_header_left_menu":"","ocean_custom_header_template":"","ocean_custom_logo":0,"ocean_custom_retina_logo":0,"ocean_custom_logo_max_width":0,"ocean_custom_logo_tablet_max_width":0,"ocean_custom_logo_mobile_max_width":0,"ocean_custom_logo_max_height":0,"ocean_custom_logo_tablet_max_height":0,"ocean_custom_logo_mobile_max_height":0,"ocean_header_custom_menu":"","ocean_menu_typo_font_family":"","ocean_menu_typo_font_subset":"","ocean_menu_typo_font_size":0,"ocean_menu_typo_font_size_tablet":0,"ocean_menu_typo_font_size_mobile":0,"ocean_menu_typo_font_size_unit":"px","ocean_menu_typo_font_weight":"","ocean_menu_typo_font_weight_tablet":"","ocean_menu_typo_font_weight_mobile":"","ocean_menu_typo_transform":"","ocean_menu_typo_transform_tablet":"","ocean_menu_typo_transform_mobile":"","ocean_menu_typo_line_height":0,"ocean_menu_typo_line_height_tablet":0,"ocean_menu_typo_line_height_mobile":0,"ocean_menu_typo_line_height_unit":"","ocean_menu_typo_spacing":0,"ocean_menu_typo_spacing_tablet":0,"ocean_menu_typo_spacing_mobile":0,"ocean_menu_typo_spacing_unit":"","ocean_menu_link_color":"","ocean_menu_link_color_hover":"","ocean_menu_link_color_active":"","ocean_menu_link_background":"","ocean_menu_link_hover_background":"","ocean_menu_link_active_background":"","ocean_menu_social_links_bg":"","ocean_menu_social_hover_links_bg":"","ocean_menu_social_links_color":"","ocean_menu_social_hover_links_color":"","ocean_disable_title":"default","ocean_disable_heading":"default","ocean_post_title":"","ocean_post_subheading":"","ocean_post_title_style":"","ocean_post_title_background_color":"","ocean_post_title_background":0,"ocean_post_title_bg_image_position":"","ocean_post_title_bg_image_attachment":"","ocean_post_title_bg_image_repeat":"","ocean_post_title_bg_image_size":"","ocean_post_title_height":0,"ocean_post_title_bg_overlay":0.5,"ocean_post_title_bg_overlay_color":"","ocean_disable_breadcrumbs":"default","ocean_breadcrumbs_color":"","ocean_breadcrumbs_separator_color":"","ocean_breadcrumbs_links_color":"","ocean_breadcrumbs_links_hover_color":"","ocean_display_footer_widgets":"default","ocean_display_footer_bottom":"default","ocean_custom_footer_template":"","ocean_post_oembed":"","ocean_post_self_hosted_media":"","ocean_post_video_embed":"","ocean_link_format":"","ocean_link_format_target":"self","ocean_quote_format":"","ocean_quote_format_link":"post","ocean_gallery_link_images":"on","ocean_gallery_id":[],"footnotes":""},"categories":[16],"tags":[37,154,41,153],"class_list":["post-4626","post","type-post","status-publish","format-standard","hentry","category-lecturas","tag-chile","tag-gestion-de-riesgos","tag-glaciares","tag-susceptibilidad","entry"],"yoast_head":"\n\u00bfSon propensos los glaciares de Chile central a desencadenar movimientos en masa? - Programa Hidroclim\u00e1tico Regional para los Andes<\/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:\/\/www.andex-rhp.org\/?p=4626\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"\u00bfSon propensos los glaciares de Chile central a desencadenar movimientos en masa? - Programa Hidroclim\u00e1tico Regional para los Andes\" \/>\n<meta property=\"og:description\" content=\"Por Felipe Ugalde Peralta*\/ Los Andes centrales de Chile son conocidos por ser una de las zonas m\u00e1s pobladas del pa\u00eds, incluyendo la ciudad de Santiago de Chile con m\u00e1s de 8 millones de habitantes. 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Letras rojas indican los glaciares presentados en la Figura 2: A) Glaciar El Morado, B) Glaciar Mu\u00f1iri, C) Glaciar San Francisco, D) Glaciar Nieves Negras, E) Glaciar Loma Larga y F) Glaciar Cortaderas"},{"@type":"BreadcrumbList","@id":"https:\/\/www.andex-rhp.org\/?p=4626#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/www.andex-rhp.org\/"},{"@type":"ListItem","position":2,"name":"\u00bfSon propensos los glaciares de Chile central a desencadenar movimientos en masa?"}]},{"@type":"WebSite","@id":"https:\/\/www.andex-rhp.org\/#website","url":"https:\/\/www.andex-rhp.org\/","name":"Programa Hidroclim\u00e1tico Regional para los Andes","description":"ANDEX","publisher":{"@id":"https:\/\/www.andex-rhp.org\/#organization"},"potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/www.andex-rhp.org\/?s={search_term_string}"},"query-input":{"@type":"PropertyValueSpecification","valueRequired":true,"valueName":"search_term_string"}}],"inLanguage":"en-US"},{"@type":"Organization","@id":"https:\/\/www.andex-rhp.org\/#organization","name":"Programa Hidroclim\u00e1tico Regional para los Andes","url":"https:\/\/www.andex-rhp.org\/","logo":{"@type":"ImageObject","inLanguage":"en-US","@id":"https:\/\/www.andex-rhp.org\/#\/schema\/logo\/image\/","url":"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2024\/04\/cropped-cropped-logo_ANDEX_color_trans1.png","contentUrl":"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2024\/04\/cropped-cropped-logo_ANDEX_color_trans1.png","width":555,"height":444,"caption":"Programa Hidroclim\u00e1tico Regional para los Andes"},"image":{"@id":"https:\/\/www.andex-rhp.org\/#\/schema\/logo\/image\/"}},{"@type":"Person","@id":"https:\/\/www.andex-rhp.org\/#\/schema\/person\/502e4f38fe30f00d8b101cd988a956fb","name":"andex","image":{"@type":"ImageObject","inLanguage":"en-US","@id":"https:\/\/www.andex-rhp.org\/#\/schema\/person\/image\/","url":"https:\/\/secure.gravatar.com\/avatar\/23494ed4720f39176481de38bcdec2a13011e1321adeb3faa91d0e623a2a8587?s=96&d=mm&r=g","contentUrl":"https:\/\/secure.gravatar.com\/avatar\/23494ed4720f39176481de38bcdec2a13011e1321adeb3faa91d0e623a2a8587?s=96&d=mm&r=g","caption":"andex"},"url":"https:\/\/www.andex-rhp.org\/?author=2"}]}},"_links":{"self":[{"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/posts\/4626","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=4626"}],"version-history":[{"count":2,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/posts\/4626\/revisions"}],"predecessor-version":[{"id":4630,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/posts\/4626\/revisions\/4630"}],"wp:attachment":[{"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=4626"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=4626"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=4626"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}