{"id":719,"date":"2025-04-09T09:11:07","date_gmt":"2025-04-09T09:11:07","guid":{"rendered":"https:\/\/www.craag.dz\/constantine2025\/?page_id=719"},"modified":"2025-07-01T20:47:54","modified_gmt":"2025-07-01T20:47:54","slug":"field-trip-2","status":"publish","type":"page","link":"https:\/\/www.craag.dz\/suremed2025\/index.php\/field-trip-2\/","title":{"rendered":"Field Trip"},"content":{"rendered":"\t\t<div data-elementor-type=\"wp-page\" data-elementor-id=\"719\" class=\"elementor elementor-719\">\n\t\t\t\t<div class=\"elementor-element elementor-element-2f14e6e e-con-full e-flex e-con e-parent\" data-id=\"2f14e6e\" data-element_type=\"container\" 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class=\"elementor-shape elementor-shape-bottom\" data-negative=\"true\">\n\t\t\t<svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" viewBox=\"0 0 1000 100\" preserveAspectRatio=\"none\">\n\t<path class=\"elementor-shape-fill\" d=\"M500.2,94.7L0,0v100h1000V0L500.2,94.7z\"\/>\n<\/svg>\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-e8c52ea elementor-widget elementor-widget-spacer\" data-id=\"e8c52ea\" data-element_type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-205249c elementor-widget elementor-widget-heading\" data-id=\"205249c\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">Field Trip<\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-f952ab7 e-flex e-con-boxed e-con e-parent\" data-id=\"f952ab7\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-41916d5 elementor-widget elementor-widget-heading\" data-id=\"41916d5\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\"><h1 style=\"text-align: center\"><strong> Exploring Active Faults in the Constantine Basin<\/strong><span style=\"font-size: 1.875rem;font-style: inherit;text-align: start\"><\/span><\/h1><\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-69c263c e-flex e-con-boxed e-con e-parent\" data-id=\"69c263c\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-f211ed6 elementor-widget__width-auto elementor-widget elementor-widget-heading\" data-id=\"f211ed6\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">Overview<\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-df2e921 e-con-full e-flex e-con e-parent\" data-id=\"df2e921\" data-element_type=\"container\">\n\t\t<div class=\"elementor-element elementor-element-3192243 e-con-full e-flex e-con e-child\" data-id=\"3192243\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-6385532 elementor-widget elementor-widget-text-editor\" data-id=\"6385532\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p>Join us for a one-day field trip on <strong>October 29, 2025<\/strong>, as part of the <em>International Symposium on Seismic Risk, Urbanization, and Resilience in the Western Mediterranean (SURE-MED)<\/em>, marking the 40th anniversary of the 1985 Ms6.0 Constantine earthquake. This excursion explores active fault systems and associated geohazards in the Constantine Basin, northeastern Algeria. Designed for students, researchers, and professionals, the trip offers hands-on insights into seismic hazards, regional tectonics, and their implications for urban resilience. Participants will also visit the ancient Roman city of Tiddis, bridging modern geoscience with historical adaptations to the region\u2019s dynamic geology.<\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-66178b1 e-con-full e-flex e-con e-child\" data-id=\"66178b1\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-69f8eaf elementor-widget elementor-widget-image\" data-id=\"69f8eaf\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t<img fetchpriority=\"high\" decoding=\"async\" width=\"530\" height=\"430\" src=\"https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/half-img-field-trips-1.png\" class=\"attachment-large size-large wp-image-1502\" alt=\"\" srcset=\"https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/half-img-field-trips-1.png 530w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/half-img-field-trips-1-300x243.png 300w\" sizes=\"(max-width: 530px) 100vw, 530px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-ee0abfc e-flex e-con-boxed e-con e-parent\" data-id=\"ee0abfc\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-68305a1 elementor-widget-divider--view-line elementor-widget elementor-widget-divider\" data-id=\"68305a1\" data-element_type=\"widget\" data-widget_type=\"divider.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-divider\">\n\t\t\t<span class=\"elementor-divider-separator\">\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-abcae85 e-flex e-con-boxed e-con e-parent\" data-id=\"abcae85\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-96d8b30 elementor-widget__width-auto elementor-widget elementor-widget-heading\" data-id=\"96d8b30\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">Geological Context<\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-40e568e e-grid e-con-full e-con e-parent\" data-id=\"40e568e\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-cb5df4e elementor-widget elementor-widget-image\" data-id=\"cb5df4e\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"803\" height=\"549\" src=\"https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/fieldtrip2-e1748425428766.png\" class=\"attachment-large size-large wp-image-1198\" alt=\"\" srcset=\"https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/fieldtrip2-e1748425428766.png 803w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/fieldtrip2-e1748425428766-300x205.png 300w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/fieldtrip2-e1748425428766-768x525.png 768w\" sizes=\"(max-width: 803px) 100vw, 803px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-4b913e9 elementor-widget elementor-widget-text-editor\" data-id=\"4b913e9\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p><span style=\"font-style: inherit; font-weight: inherit; white-space-collapse: preserve;\">The Constantine Basin, a Neogene east-west intramontane basin, is located on the southern margin of the Lesser Kabylia block within the Tell Atlas thrust belt of northeastern Algeria. Formed after the main Tell thrusting event in the Lower Miocene, it evolved in a continental setting with lagoonal and lacustrine phases since the Middle Miocene, accumulating reddish conglomerates, grey gypsum marls, and lacustrine limestones. Its complex neotectonic history, driven by successive episodes of transtension and transpression, has shaped a morphotectonic framework ideal for active tectonic studies. The basin experiences frequent moderate seismic activity, concentrated primarily along its borders, which are defined by active faults exhibiting a predominantly strike-slip regime, as evidenced by geological records (slickenlines), seismotectonic data (focal mechanisms), and geodetic measurements.<\/span>&nbsp;<\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-c4151e3 e-flex e-con-boxed e-con e-parent\" data-id=\"c4151e3\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-53760a5 elementor-widget-divider--view-line elementor-widget elementor-widget-divider\" data-id=\"53760a5\" data-element_type=\"widget\" data-widget_type=\"divider.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-divider\">\n\t\t\t<span class=\"elementor-divider-separator\">\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-98b2907 e-flex e-con-boxed e-con e-parent\" data-id=\"98b2907\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-633db50 elementor-widget__width-auto elementor-widget elementor-widget-heading\" data-id=\"633db50\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">Northern Boundary: North Constantine Fault<\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-d40120e e-grid e-con-full e-con e-parent\" data-id=\"d40120e\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-bc9af1c elementor-widget elementor-widget-text-editor\" data-id=\"bc9af1c\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p dir=\"auto\" style=\"white-space-collapse: preserve;\">The northern boundary of the Constantine Basin is defined by one of the most prominent strike-slip faults in North Africa, the North Constantine Fault (also known as the Mcid Aicha Debbagh Fault). This over 100-km-long east-west fault zone, part of the 300-km-long Ghardimaou\u2014North Constantine (GNC) fault system, delineates the northern margin of the Constantine and Guelma pull-apart basins, separating them from the Numidian Chain. The fault system accommodates approximately 2.4 mm\/yr of convergence between the African and Eurasian plates and generates frequent moderate seismicity (M&lt;5), including the 2017 Mw 4.7 sequence along its central segment. Although no major historical earthquakes are directly linked to this fault, geological and morphotectonic evidence suggests significant seismic potential. The fault\u2019s intersection with the Beni Haroun Dam, Algeria\u2019s largest, highlights its societal and economic importance. Segmented by NE-SW and NW-SE transverse faults, the system has produced moderate events, such as the 2020 Mw 4.8 Mila sequence.<\/p>\n<p><\/p>\n<p><\/p>\n<p><\/p>\n<p><\/p>\n<p><\/p>\n<p><\/p>\n<p><\/p>\n<p><\/p>\n<p><\/p>\n<p><\/p>\n<p><\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-e2415e3 elementor-widget elementor-widget-image\" data-id=\"e2415e3\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"1024\" height=\"423\" src=\"https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Mohammedi-et-al.-2023-2-1024x423.png\" class=\"attachment-large size-large wp-image-1295\" alt=\"\" srcset=\"https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Mohammedi-et-al.-2023-2-1024x423.png 1024w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Mohammedi-et-al.-2023-2-300x124.png 300w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Mohammedi-et-al.-2023-2-768x318.png 768w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Mohammedi-et-al.-2023-2-1536x635.png 1536w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Mohammedi-et-al.-2023-2-2048x847.png 2048w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-d98fdcd e-flex e-con-boxed e-con e-parent\" data-id=\"d98fdcd\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-b253a11 elementor-widget-divider--view-line elementor-widget elementor-widget-divider\" data-id=\"b253a11\" data-element_type=\"widget\" data-widget_type=\"divider.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-divider\">\n\t\t\t<span class=\"elementor-divider-separator\">\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-20c2227 e-flex e-con-boxed e-con e-parent\" data-id=\"20c2227\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-608078c elementor-widget__width-auto elementor-widget elementor-widget-heading\" data-id=\"608078c\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">Southern Boundary: El Aria and Ain Smara Faults<\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-4ffd6c8 e-con-full e-flex e-con e-parent\" data-id=\"4ffd6c8\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-75d6c8e elementor-widget elementor-widget-text-editor\" data-id=\"75d6c8e\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p dir=\"auto\" style=\"white-space-collapse: preserve;\">The southern boundary of the Constantine Basin, unlike the northern boundary, is not defined by a single major fault but by a system of neotectonic NE-SW-oriented faults, including the El Aria Fault and the Ain Smara Fault system. The El Aria Fault was responsible for the 1985 Ms 6.0 Constantine earthquake. Although these faults are less prominent in seismotectonic records, they are critical to the region\u2019s seismotectonic framework. The Ain Smara Fault, a 20-km-long western segment of the El Aria system, borders the Djebel Felten-Sekkoum-Sellem massif. While inactive during the 1985 earthquake, its fault scarps and deformed Quaternary deposits indicate recent activity, suggesting a significant seismic risk to the Constantine region.<\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-8c3d8d6 e-flex e-con-boxed e-con e-parent\" data-id=\"8c3d8d6\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t<div class=\"elementor-element elementor-element-06b842a e-con-full e-flex e-con e-child\" data-id=\"06b842a\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-502a391 elementor-widget-divider--view-line elementor-widget elementor-widget-divider\" data-id=\"502a391\" data-element_type=\"widget\" data-widget_type=\"divider.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-divider\">\n\t\t\t<span class=\"elementor-divider-separator\">\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-918e5f8 e-flex e-con-boxed e-con e-parent\" data-id=\"918e5f8\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-49b6873 elementor-widget__width-auto elementor-widget elementor-widget-heading\" data-id=\"49b6873\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">Additional Hazards: Landslides<\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-b66aaa6 e-grid e-con-full e-con e-parent\" data-id=\"b66aaa6\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-e4440a4 elementor-widget elementor-widget-text-editor\" data-id=\"e4440a4\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p dir=\"auto\" style=\"white-space-collapse: preserve;\">The Constantine Basin\u2019s steep topography, combined with climatic and lithologic factors, makes it highly susceptible to landslides, which are often triggered by seismic activity or anthropogenic activities. These hazards are among the most challenging in the region, as their contributing factors interact across regional scales. The 2020 Mw 5.0 Mila earthquake triggered catastrophic landslides, highlighting secondary geohazards that pose significant challenges to urban development<\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\n<p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-883df4b elementor-widget elementor-widget-image\" data-id=\"883df4b\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t<img loading=\"lazy\" decoding=\"async\" width=\"768\" height=\"577\" src=\"https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/IMG_20200809_152742-768x577.jpg\" class=\"attachment-medium_large size-medium_large wp-image-1503\" alt=\"\" srcset=\"https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/IMG_20200809_152742-768x577.jpg 768w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/IMG_20200809_152742-300x225.jpg 300w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/IMG_20200809_152742-1024x769.jpg 1024w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/IMG_20200809_152742-1536x1153.jpg 1536w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/IMG_20200809_152742-2048x1538.jpg 2048w\" sizes=\"(max-width: 768px) 100vw, 768px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-bd07af7 e-con-full e-flex e-con e-parent\" data-id=\"bd07af7\" data-element_type=\"container\">\n\t\t<div class=\"elementor-element elementor-element-b286034 e-flex e-con-boxed e-con e-child\" data-id=\"b286034\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-cb42d2b elementor-widget-divider--view-line elementor-widget elementor-widget-divider\" data-id=\"cb42d2b\" data-element_type=\"widget\" data-widget_type=\"divider.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-divider\">\n\t\t\t<span class=\"elementor-divider-separator\">\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-f0408b1 e-flex e-con-boxed e-con e-parent\" data-id=\"f0408b1\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-983c45f elementor-widget__width-auto elementor-widget elementor-widget-heading\" data-id=\"983c45f\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">Field Trip Highlights<\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-a4e79ea e-con-full e-flex e-con e-parent\" data-id=\"a4e79ea\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-64a2925 elementor-widget elementor-widget-text-editor\" data-id=\"64a2925\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p>This field trip provides a hands-on exploration of the Constantine Basin\u2019s tectonics and geohazards, with four key stops:<\/p><ol><li><strong>Stop 1: Ain Smara Fault (4 km from symposium venue)<\/strong>: Observe a N40E-striking fault scarp, visible in satellite imagery and field, and examine geomorphic evidences underscoring the fault\u2019s activity.<\/li><li><strong>Stop 2: El Kharba Landslide (Mila)<\/strong>: Panoramic view on the 2020 coseismic landslide site to analyze the interplay of tectonics, topography, and lithology in triggering mass movements, a critical factor for urban planning (Hallal et al., 2024) (<strong>Figs. 1 and 5<\/strong>).<\/li><li><strong>Stop 3: Mcid Aicha Debbagh Fault<\/strong>: Study morphological evidence of active faulting and discuss its role in regional convergence, its proximity to the Beni Haroun Dam, and implications for seismic risk (Bendjama et al., 2021) (<strong>Figs. 1 and 6<\/strong>).<\/li><li><strong>Stop 4<\/strong>: <strong>2020 (Mw 4.8) Hamala Mainshock:<\/strong> Panoramic view of Mount M\u2019cid A\u00efcha, a Cretaceous limestone massif (<strong>Figs. 1 and 5<\/strong>)<\/li><li><p><strong>Stop 5: Tiddis Archaeological Site<\/strong>: Explore the Roman-Berber city of Tiddis, offering a panoramic view of the basin and insights into historical adaptations to its dynamic geology, connecting geoscience with cultural heritage (<strong>Figs. 1 and 7<\/strong>).<\/p><\/li><\/ol><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-c5e0588 e-con-full e-flex e-con e-parent\" data-id=\"c5e0588\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-ba7b612 elementor-widget elementor-widget-image\" data-id=\"ba7b612\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t<img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"875\" src=\"https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Field_Trip_Stop-1024x875.jpg\" class=\"attachment-large size-large wp-image-1458\" alt=\"\" srcset=\"https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Field_Trip_Stop-1024x875.jpg 1024w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Field_Trip_Stop-300x256.jpg 300w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Field_Trip_Stop-768x656.jpg 768w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Field_Trip_Stop-1536x1313.jpg 1536w, https:\/\/www.craag.dz\/suremed2025\/wp-content\/uploads\/2025\/05\/Field_Trip_Stop-2048x1750.jpg 2048w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-7d02ed7 e-con-full e-flex e-con e-parent\" data-id=\"7d02ed7\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-cc71da6 elementor-widget elementor-widget-text-editor\" data-id=\"cc71da6\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<h2><strong>Field Trip Details:<\/strong><\/h2><ul><li><strong>Date<\/strong>: October 29, 2025<\/li><li><strong>Duration<\/strong>: Approximately 8 hours<\/li><li><strong>Prerequisites<\/strong>: Background in geoscience or related fields recommended. participants).<\/li><li><strong>Equipment<\/strong>: Comfortable clothing, sturdy footwear, notebook, and optional camera.<\/li><li><strong>Capacity<\/strong>: Limited to 50 participants (registration required).<\/li><li><strong>Logistics<\/strong>: Transportation and meals provided.<\/li><\/ul><div>\u00a0<\/div><div>\u00a0<\/div><h3><strong>References<\/strong><\/h3><p><em>Note<\/em>: The following references are a selection of key studies relevant to the Constantine Basin\u2019s geology, seismotectonics, and geohazards. This list is not exhaustive, as the region has been extensively studied in additional works not cited here.<\/p><ul><li><p>Aris, Y., Coiffait, P. E., &amp; Guiraud, M. (1998). Characterisation of Mesozoic\u2013Cenozoic deformations and palaeostress fields in the Central Constantinois, northeast Algeria. <em>Tectonophysics<\/em>, 290(1\u20132), 59\u201385. https:\/\/doi.org\/10.1016\/S0040-1951(98)00012-2<\/p><\/li><li><p>Bendjama, H., Yelles-Chaouche, A., Boulahia, O., Abacha, I., Mohammedi, Y., Beldjoudi, H., Rahmani, S. T.-E., &amp; Belheouane, O. (2021). The March 2017 earthquake sequence along the E-W-trending Mcid A\u00efcha-Debbagh Fault, northeast Algeria. <em>Geosciences Journal<\/em>, 25(5), 697\u2013713. <a href=\"https:\/\/doi.org\/10.1007\/s12303-020-0059-y\">https:\/\/doi.org\/10.1007\/s12303-020-0059-y<\/a>.<\/p><\/li><li><p>Bougrine, A., Yelles-Chaouche, A. K., &amp; Calais, E. (2019). Active deformation in Algeria from continuous GPS measurements. Geophysical Journal International, 217, 572\u2013588.<\/p><\/li><li><p>Bounif, A., Haessler, H., &amp; Meghraoui, M. (1987). The Constantine (northeast Algeria) earthquake of October 27, 1985: Surface ruptures and aftershock study. <em>Earth and Planetary Science Letters<\/em>, 85(4), 451\u2013460. https:\/\/doi.org\/10.1016\/0012-821X(87)90140-3<\/p><\/li><li><p>Hallal, N., Hamidatou, M., Hamai, L., Aguemoune, S., &amp; Lamali, A. (2024). Landslides triggered by the August 2020 Mw 5.0 Mila, Algeria, earthquake: Spatial distribution and susceptibility mapping. <em>Euro-Mediterranean Journal for Environmental Integration<\/em>, 9(3), 1063\u20131085. https:\/\/doi.org\/10.1007\/s41207-024-00471-w<\/p><\/li><li><p>Harbi, A., Maouche, S., &amp; Ayadi, A. (1999). Neotectonics and associate seismicity in the Eastern Tellian Atlas of Algeria. <em>Journal of Seismology<\/em>, 3(1), 95\u2013104. https:\/\/doi.org\/10.1023\/A:1009743404491<\/p><\/li><li><p>Maouche, S., Abtout, A., Merabet, N.-E., A\u00effa, T., Lamali, A., Bouyahiaoui, B., Bougchiche, S., &amp; Ayache, M. (2013). Tectonic and hydrothermal activities in Debagh, Guelma Basin (Algeria). <em>Journal of Geological Research<\/em>, 2013, 1\u201313. https:\/\/doi.org\/10.1155\/2013\/409475<\/p><\/li><li><p>Marmi, R., &amp; Guiraud, R. (2006). End Cretaceous to recent polyphased compressive tectonics along the \u201cM\u00f4le Constantinois\u201d and foreland (NE Algeria). <em>Journal of African Earth Sciences<\/em>, 45(1), 123\u2013136. https:\/\/doi.org\/10.1016\/j.jafrearsci.2006.01.009<\/p><\/li><li><p>Meghraoui, M. (1988). <em>G\u00e9ologie des zones sismiques du Nord de l\u2019Alg\u00e9rie: Pal\u00e9osismologie, tectonique active et synth\u00e8se sismotectonique<\/em> [Doctoral dissertation]. Universit\u00e9 de Paris-Sud, Centre d\u2019Orsay.<\/p><\/li><li><p>Mohammedi, Y., Djellit, H., Yelles-Chaouche, A., Hamidatou, M., &amp; Hallal, N. (2019). New evidence of active faulting along the Ain Smara Fault in the Constantine Province (North East Algeria). In <em>Recent Advances in Geo-Environmental Engineering, Geomechanics and Geotechnics, and Geohazards<\/em> (pp. 271\u2013273). Springer. https:\/\/doi.org\/10.1007\/978-3-030-01455-1_59<\/p><\/li><li><p>Mohammedi, Y., Yelles-Chaouche, A., &amp; Adjiri, S. (2021). The Mila 2020 seismic sequence in north-eastern Algeria: Seismotectonic context and geohazard consequences. <em>Mediterranean Geosciences Union (MedGU)<\/em>, 25\u201328 November 2021.<\/p><\/li><li><p>Raoult, J.-F. (1975). \u00c9volution pal\u00e9og\u00e9ographique et structurale de la cha\u00eene alpine entre le golfe de Skikda et Constantine (Alg\u00e9rie orientale). <em>Bulletin de la Soci\u00e9t\u00e9 G\u00e9ologique de France<\/em>, S7-XVII(3), 394\u2013409. <a href=\"https:\/\/doi.org\/10.2113\/gssgfbull.S7-XVII.3.394\">https:\/\/doi.org\/10.2113\/gssgfbull.S7-XVII.3.394<\/a><\/p><\/li><li><p>Vila J.M., 1980. La cha\u00eene alpine d\u2019Alg\u00e9rie \u03c4rientale et des confins alg\u00e9ro-tunisiens. Th\u00e8se de Doctorat, Universit\u00e9 P. et M. Curie-Paris.<\/p><\/li><\/ul><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script src=\"chrome-extension:\/\/bincmiainjofjnhchmcalkanjebghoen\/aiscripts\/script-main.js\"><\/script><\/p><p><script 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