{"id":1431,"date":"2024-07-24T12:21:40","date_gmt":"2024-07-24T10:21:40","guid":{"rendered":"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/?page_id=1431"},"modified":"2024-11-29T14:33:48","modified_gmt":"2024-11-29T13:33:48","slug":"zone-de-montpellier","status":"publish","type":"page","link":"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/?page_id=1431","title":{"rendered":"R\u00e9gion de Montpellier"},"content":{"rendered":"\n<p style=\"font-family:Helvetica ;font-size: 16px; line-height: 22px; text-indent:2em; \", align=\"justify\"> \nLa <strong>r\u00e9gion de Montpellier<\/strong> est marqu\u00e9e par deux r\u00e9gimes de d\u00e9formation majeurs.\n<\/p>\n<ul style=\"font-family:Helvetica ;font-size: 16px; line-height: 22px;\" align=\"justify\">\n<li>Un <u>grand chevauchement<\/u> E-W qui affecte les roches M\u00e9sozo\u00efque. Il est marqu\u00e9 par des d\u00e9p\u00f4ts de br\u00e8ches vitrolliennes au Nord. Cela indique un <u>r\u00e9gime compressif<\/u> N-S qui date du vitrollien (66-54Ma).<\/li>\n<li>Des <u>failles normales<\/u> NE-SW qui forment des h\u00e9mi-grabens remplis de s\u00e9diments syn- rift oligoc\u00e8ne. Cela montre un r\u00e9gime extensif NW-SE \u00e0 l\u2019oligoc\u00e8ne (30-20Ma) associ\u00e9 \u00e0 l\u2019<u>ouverture de l\u2019oc\u00e9an liguro-proven\u00e7al<\/u>.<\/li>\n<\/ul>\n<\/p>\n\n\n            <div class=\"oxi-addons-container noLightbox oxi-image-hover-wrapper-59 \" id=\"oxi-image-hover-wrapper-59\">\r\n                <div class=\"oxi-addons-row\">\r\n                                <div class=\"oxi-addons-main-wrapper-image-comparison-style-1 oxi-addons-main-wrapper-image-comparison oxi-bt-col-lg-12 oxi-bt-col-md-12 oxi-bt-col-sm-12  \">\r\n                <div class=\"oxi-addons-main 0\">\r\n                    <div class=\"oxi-addons-comparison-59_0\">\r\n                      \r\n                                                    <img decoding=\"async\"  src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/11\/IMG_1316.jpg\"  class=\"oxi-img\"\/>\r\n                                                        <img decoding=\"async\"  src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/11\/IMG_1317.jpg\"  class=\"oxi-img\" \/>\r\n                                                <\/div>\r\n                <\/div>\r\n                            <\/div>\r\n                            <\/div>\r\n            <\/div>\r\n        \n\n\n\n<p style=\"font-family:Helvetica ;font-size: 16px; line-height: 22px; text-indent:2em; \", align=\"justify\"> \nL&#8217;ensemble de ces points d&#8217;int\u00e9r\u00eat d\u00e9taill\u00e9s seront disponibles ult\u00e9rieurement sur le site de la <a href=\"https:\/\/lithotheque.ac-montpellier.fr\/geoduc\" target=\"_blanck\" rel=\"noopener\">lithoth\u00e8que nationale<\/a>. \n<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 style=\"font-family:Helvetica; font-size: 30px\">\nLe chevauchement de Montpellier\n<\/h2>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-1 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<iframe loading=\"lazy\" width=\"250\" height=\"240\" frameborder=\"0\" scrolling=\"no\" marginheight=\"0\" marginwidth=\"0\" sandbox=\"allow-forms allow-scripts allow-same-origin\" src=\"https:\/\/www.geoportail.gouv.fr\/embed\/visu.html?c=3.924587618179265,43.65955910220194&#038;z=13&#038;l0=ORTHOIMAGERY.ORTHOPHOTOS::GEOPORTAIL:OGC:WMTS(1)&#038;l1=GEOLOGY.GEOLOGY::EXTERNAL:OGC:EXTERNALWMS(1)&#038;d2=5313050(1)&#038;permalink=yes\" allowfullscreen><\/iframe>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"724\" height=\"723\" src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.45.34.png\" alt=\"\" class=\"wp-image-1667\" srcset=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.45.34.png 724w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.45.34-300x300.png 300w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.45.34-150x150.png 150w\" sizes=\"(max-width: 724px) 100vw, 724px\" \/><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p style=\"font-family:Helvetica ;font-size: 16px; line-height: 22px; text-indent:2em; \", align=\"justify\"> \nL\u2019affleurement d\u2019une cinquantaine de m\u00e8tre de long est situ\u00e9 au bord des rails du tramway 2, entre Jacou et Castelnau-le-Lez. Il s\u2019agit d\u2019une grande zone de faille avec des strates \u00e0 orientations variables tr\u00e8s tectonis\u00e9e par de nombreuses <strong>failles inverses<\/strong> E-W.\n<\/p>\n<\/div>\n<\/div>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 style=\"font-family:Helvetica; font-size: 30px\">\nLe pli de la mosson\n<\/h2>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-2 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<iframe loading=\"lazy\" width=\"240\" height=\"250\" frameborder=\"0\" scrolling=\"no\" marginheight=\"0\" marginwidth=\"0\" sandbox=\"allow-forms allow-scripts allow-same-origin\" src=\"https:\/\/www.geoportail.gouv.fr\/embed\/visu.html?c=3.815183745769497,43.63425257463609&#038;z=13&#038;d0=5313050(1)&#038;l1=GEOLOGY.GEOLOGY::EXTERNAL:OGC:EXTERNALWMS(1)&#038;d2=5314211(1)&#038;d3=5314214(1)&#038;permalink=yes\" allowfullscreen><\/iframe>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"887\" height=\"892\" src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.47.58.png\" alt=\"\" class=\"wp-image-1672\" srcset=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.47.58.png 887w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.47.58-298x300.png 298w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.47.58-150x150.png 150w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.47.58-768x772.png 768w\" sizes=\"(max-width: 887px) 100vw, 887px\" \/><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p style=\"font-family:Helvetica ;font-size: 16px; line-height: 22px; text-indent:2em; \", align=\"justify\"> \nCe fameux pli (couverture du livre <I>Ce que disent les pierres de Maurice Mattauer)<\/I> affecte les s\u00e9diments jurassiques. C\u2019est un <strong>pli anticlinal isopaque<\/strong> typique d\u2019une d\u00e9formation ductile. Ce plissement est d\u00fb \u00e0 un r\u00e9gime compressif N-S lors de l\u2019<u>orog\u00e8ne pyr\u00e9n\u00e9ene<\/u>.\n<\/p>\n<\/div>\n<\/div>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 style=\"font-family:Helvetica; font-size: 30px\">\nLes br\u00e8ches du Vitrollien\n<\/h2>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-3 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<iframe loading=\"lazy\" width=\"240\" height=\"250\" frameborder=\"0\" scrolling=\"no\" marginheight=\"0\" marginwidth=\"0\" sandbox=\"allow-forms allow-scripts allow-same-origin\" src=\"https:\/\/www.geoportail.gouv.fr\/embed\/visu.html?c=3.8095826219790605,43.642246825875475&#038;z=14&#038;d0=5313050(1)&#038;l1=GEOLOGY.GEOLOGY::EXTERNAL:OGC:EXTERNALWMS(1)&#038;d2=5314211(1)&#038;d3=5314214(1)&#038;d4=5314222(1)&#038;permalink=yes\" allowfullscreen><\/iframe>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"898\" height=\"899\" src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.49.17.png\" alt=\"\" class=\"wp-image-1673\" srcset=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.49.17.png 898w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.49.17-300x300.png 300w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.49.17-150x150.png 150w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-09.49.17-768x769.png 768w\" sizes=\"(max-width: 898px) 100vw, 898px\" \/><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p style=\"font-family:Helvetica ;font-size: 16px; line-height: 22px; text-indent:2em; \", align=\"justify\">\nL\u2019affleurement des <strong>br\u00e8ches vitroliennes<\/strong> se situe uniquement au nord du chevauchement au niveau de la Mosson. Ces d\u00e9p\u00f4ts sont des br\u00e8ches s\u00e9dimentaires syn-tectonique, qui se sont d\u00e9pos\u00e9es sous le chevauchement de Montpellier. Elles permettent de dater le <u>chevauchement<\/u> \u00e0 66-54Ma.\n<\/p>\n<\/div>\n<\/div>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 style=\"font-family:Helvetica; font-size: 30px\">\nLa dalle des Matelles\n<\/h2>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-4 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<iframe loading=\"lazy\" width=\"240\" height=\"250\" frameborder=\"0\" scrolling=\"no\" marginheight=\"0\" marginwidth=\"0\" sandbox=\"allow-forms allow-scripts allow-same-origin\" src=\"https:\/\/www.geoportail.gouv.fr\/embed\/visu.html?c=3.804384653869251,43.74415280315418&#038;z=13&#038;d0=5313050(1)&#038;l1=GEOLOGY.GEOLOGY::EXTERNAL:OGC:EXTERNALWMS(1)&#038;d2=5314211(1)&#038;permalink=yes\" allowfullscreen><\/iframe>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-cb-carousel cb-single-slide\" data-slick=\"{&quot;slidesToShow&quot;:1,&quot;slidesToScroll&quot;:1,&quot;speed&quot;:300,&quot;arrows&quot;:true,&quot;dots&quot;:true,&quot;autoplay&quot;:true,&quot;autoplaySpeed&quot;:3000,&quot;infinite&quot;:true,&quot;responsive&quot;:[{&quot;breakpoint&quot;:769,&quot;settings&quot;:{&quot;slidesToShow&quot;:1,&quot;slidesToScroll&quot;:1}}]}\">\n<div class=\"wp-block-cb-slide\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"716\" height=\"714\" src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.21.png\" alt=\"\" class=\"wp-image-1640\" srcset=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.21.png 716w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.21-300x300.png 300w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.21-150x150.png 150w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.21-301x300.png 301w\" sizes=\"(max-width: 716px) 100vw, 716px\" \/><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-cb-slide\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"714\" height=\"715\" src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.33.png\" alt=\"\" class=\"wp-image-1641\" srcset=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.33.png 714w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.33-300x300.png 300w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.33-150x150.png 150w\" sizes=\"(max-width: 714px) 100vw, 714px\" \/><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-cb-slide\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"716\" height=\"713\" src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.45.png\" alt=\"\" class=\"wp-image-1642\" srcset=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.45.png 716w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.45-300x300.png 300w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.45-150x150.png 150w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.31.45-301x300.png 301w\" sizes=\"(max-width: 716px) 100vw, 716px\" \/><\/figure>\n<\/div>\n<\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p style=\"font-family:Helvetica ;font-size: 16px; line-height: 22px; text-indent:2em; \", align=\"justify\">\nC\u2019est un affleurement d\u2019exception o\u00f9 l\u2019on trouve un ensemble d\u2019objets de d\u00e9formation fragile racontant une histoire g\u00e9ologique complexe. La dalle de calcaire est marqu\u00e9e par des <u>fractures pyr\u00e9n\u00e9ennes<\/u>, celles-ci sont recoup\u00e9es par des tectoglyphes d\u00fb \u00e0 un <u>r\u00e9gime extensif N-S<\/u>. Cette d\u00e9formation extensive est associ\u00e9e \u00e0 la faille normale des Matelles et s\u2019est form\u00e9e lors de l\u2019<u>ouverture de l\u2019oc\u00e9an liguro-proven\u00e7al<\/u>.\n<\/p>\n<\/div>\n<\/div>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 style=\"font-family:Helvetica; font-size: 30px\">\nLa faille de Saint Cl\u00e9ment\n<\/h2>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-5 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<iframe loading=\"lazy\" width=\"250\" height=\"240\" frameborder=\"0\" scrolling=\"no\" marginheight=\"0\" marginwidth=\"0\" sandbox=\"allow-forms allow-scripts allow-same-origin\" src=\"https:\/\/www.geoportail.gouv.fr\/embed\/visu.html?c=3.8380286298494215,43.704616972047376&#038;z=13&#038;d0=5313050(1)&#038;l1=GEOLOGY.GEOLOGY::EXTERNAL:OGC:EXTERNALWMS(1)&#038;d2=5313928(1)&#038;d3=5313935(1)&#038;permalink=yes\" allowfullscreen><\/iframe>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-cb-carousel cb-single-slide\" data-slick=\"{&quot;slidesToShow&quot;:1,&quot;slidesToScroll&quot;:1,&quot;speed&quot;:300,&quot;arrows&quot;:true,&quot;dots&quot;:true,&quot;autoplay&quot;:true,&quot;autoplaySpeed&quot;:3000,&quot;infinite&quot;:true,&quot;responsive&quot;:[{&quot;breakpoint&quot;:769,&quot;settings&quot;:{&quot;slidesToShow&quot;:1,&quot;slidesToScroll&quot;:1}}]}\">\n<div class=\"wp-block-cb-slide\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"717\" height=\"714\" src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.33.58.png\" alt=\"\" class=\"wp-image-1645\" srcset=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.33.58.png 717w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.33.58-300x300.png 300w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.33.58-150x150.png 150w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.33.58-301x300.png 301w\" sizes=\"(max-width: 717px) 100vw, 717px\" \/><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-cb-slide\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"718\" height=\"713\" src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.33.48.png\" alt=\"\" class=\"wp-image-1646\" srcset=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.33.48.png 718w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.33.48-300x298.png 300w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.33.48-150x150.png 150w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.33.48-302x300.png 302w\" sizes=\"(max-width: 718px) 100vw, 718px\" \/><\/figure>\n<\/div>\n<\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p style=\"font-family:Helvetica ;font-size: 16px; line-height: 22px; text-indent:2em; \", align=\"justify\">\nLa <strong>faille normale du Lez<\/strong> permet la r\u00e9surgence de la source du Lez gr\u00e2ce au d\u00e9veloppement d\u2019<u>un r\u00e9seau karstique<\/u> le long des failles. L\u2019eau circule dans les couches perm\u00e9ables du Jurassique et la structure en h\u00e9mi-graben permet le drainage de l\u2019aquif\u00e8re vers la surface.\n<\/p>\n<\/div>\n<\/div>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 style=\"font-family:Helvetica; font-size: 30px\">\nLe volcanisme de Montferrier\n<\/h2>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-6 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<iframe loading=\"lazy\" width=\"250\" height=\"240\" frameborder=\"0\" scrolling=\"no\" marginheight=\"0\" marginwidth=\"0\" sandbox=\"allow-forms allow-scripts allow-same-origin\" src=\"https:\/\/www.geoportail.gouv.fr\/embed\/visu.html?c=3.868402232885715,43.66466711969639&#038;z=13&#038;l0=ORTHOIMAGERY.ORTHOPHOTOS::GEOPORTAIL:OGC:WMTS(1)&#038;l1=GEOLOGY.GEOLOGY::EXTERNAL:OGC:EXTERNALWMS(1)&#038;d2=5313050(1)&#038;d3=5313928(1)&#038;permalink=yes\" allowfullscreen><\/iframe>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-cb-carousel cb-single-slide\" data-slick=\"{&quot;slidesToShow&quot;:1,&quot;slidesToScroll&quot;:1,&quot;speed&quot;:300,&quot;arrows&quot;:true,&quot;dots&quot;:true,&quot;autoplay&quot;:true,&quot;autoplaySpeed&quot;:3000,&quot;infinite&quot;:true,&quot;responsive&quot;:[{&quot;breakpoint&quot;:769,&quot;settings&quot;:{&quot;slidesToShow&quot;:1,&quot;slidesToScroll&quot;:1}}]}\">\n<div class=\"wp-block-cb-slide\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"899\" height=\"900\" src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.23.01.png\" alt=\"\" class=\"wp-image-1617\" srcset=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.23.01.png 899w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.23.01-300x300.png 300w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.23.01-150x150.png 150w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.23.01-768x769.png 768w\" sizes=\"(max-width: 899px) 100vw, 899px\" \/><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-cb-slide\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"897\" height=\"898\" src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.22.40.png\" alt=\"\" class=\"wp-image-1618\" srcset=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.22.40.png 897w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.22.40-300x300.png 300w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.22.40-150x150.png 150w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.22.40-768x769.png 768w\" sizes=\"(max-width: 897px) 100vw, 897px\" \/><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-cb-slide\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"902\" height=\"900\" src=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.22.25.png\" alt=\"\" class=\"wp-image-1619\" srcset=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.22.25.png 902w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.22.25-300x300.png 300w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.22.25-150x150.png 150w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.22.25-768x766.png 768w, https:\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-25-a-16.22.25-301x300.png 301w\" sizes=\"(max-width: 902px) 100vw, 902px\" \/><\/figure>\n<\/div>\n<\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p style=\"font-family:Helvetica ;font-size: 16px; line-height: 22px; text-indent:2em; \", align=\"justify\">\nLe vieux village de Montferrier est construit sur une <strong>chemin\u00e9e volcanique basaltique<\/strong>, que l\u2019on peut voir sous l\u2019\u00e9glise. Ce volcanisme s\u2019est mis en place le long d\u2019une <u>faille normale d\u2019\u00e9chelle crustale<\/u>. Le basalte est dat\u00e9 \u00e0 l\u2019oligoc\u00e8ne, ce qui valide la syn- cin\u00e9matique avec l\u2019<u>ouverture de l\u2019oc\u00e9an liguro-proven\u00e7al<\/u>.<\/p>\n<\/div>\n<\/div>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n<div class=\"wptb-table-container wptb-table-1692\" data-wptb-horizontal-scroll-status=\"true\"><div class=\"wptb-table-container-matrix\" id=\"wptb-table-id-1692\" data-wptb-version=\"1.4.15\" data-wptb-pro-status=\"false\"><table class=\"wptb-preview-table wptb-element-main-table_setting-232\" style=\"border: 0px solid rgb(255, 255, 255);\" data-reconstraction=\"1\" data-wptb-table-tds-sum-max-width=\"580\" data-wptb-cells-width-auto-count=\"5\" data-wptb-horizontal-scroll-status=\"true\" data-wptb-extra-styles=\"LyogRW50ZXIgeW91ciBjdXN0b20gQ1NTIHJ1bGVzIGhlcmUgKi8=\" role=\"table\" data-wptb-responsive-directives=\"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\" data-wptb-adaptive-table=\"0\" data-table-columns=\"5\" data-wptb-header-background-color=\"#FFFFFFFF\" data-wptb-table-alignment=\"center\" data-wptb-even-row-background-color=\"#FFFFFFFF\" data-wptb-odd-row-background-color=\"#FFFFFFFF\"><tbody><tr class=\"wptb-row\" style=\"background-color: rgb(255, 255, 255);\"><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"0\" data-y-index=\"0\" data-wptb-css-td-auto-width=\"true\"><div class=\"wptb-image-container wptb-ph-element wptb-element-image-16\" data-wptb-image-alignment=\"center\"><div class=\"wptb-image-wrapper\">            <a class=\"wptb-link-target\" style=\"float: none;\" href=\"https:\/\/www.umontpellier.fr\/\" target=\"_blank\">                                <img loading=\"lazy\" decoding=\"async\" class=\"wptb-image-element-target\" height=\"295\" width=\"808\" style=\"width: 100%;\" src=\"\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/logo_um_2022_rouge_RVB-1.png\">            <\/a>        <\/div><\/div><\/td><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"1\" data-y-index=\"0\" data-wptb-css-td-auto-width=\"true\"><div class=\"wptb-image-container wptb-ph-element wptb-element-image-14\" data-wptb-image-alignment=\"center\"><div class=\"wptb-image-wrapper\">            <a class=\"wptb-link-target\" style=\"float: none;\" rel=\"noreferrer\" target=\"_blank\" href=\"https:\/\/www.umontpellier.fr\/universite\/projets-emblematiques\/programme-dexcellence-i-site\">                                <img loading=\"lazy\" decoding=\"async\" class=\"wptb-image-element-target\" style=\"width: 100%;\" src=\"\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/muse-logo.jpg\" width=\"679\" height=\"385\">            <\/a>        <\/div><\/div><\/td><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"2\" data-y-index=\"0\" data-wptb-css-td-auto-width=\"true\"><div class=\"wptb-image-container wptb-ph-element wptb-element-image-15\" data-wptb-image-alignment=\"center\"><div class=\"wptb-image-wrapper\">            <a class=\"wptb-link-target\" style=\"float: none;\" target=\"_blank\" href=\"https:\/\/sciences.edu.umontpellier.fr\/\">                                <img loading=\"lazy\" decoding=\"async\" class=\"wptb-image-element-target\" style=\"width: 100%;\" src=\"\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Faculte-des-Sciences-2022-CMJN-scaled-1.jpg\" width=\"2560\" height=\"1038\">            <\/a>        <\/div><\/div><\/td><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"3\" data-y-index=\"0\" data-wptb-css-td-auto-width=\"true\"><div class=\"wptb-image-container wptb-ph-element wptb-element-image-17 edit-active\" data-wptb-image-alignment=\"center\"><div class=\"wptb-image-wrapper\">            <a class=\"wptb-link-target\" style=\"float: none;\" href=\"https:\/\/www.gm.umontpellier.fr\/\" target=\"_blank\">                                <img loading=\"lazy\" decoding=\"async\" class=\"wptb-image-element-target\" height=\"110\" width=\"255\" style=\"width: 100%;\" src=\"\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/UR-GM.png\">            <\/a>        <\/div><\/div><\/td><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"4\" data-y-index=\"0\" data-wptb-css-td-auto-width=\"true\"><div class=\"wptb-image-container wptb-ph-element wptb-element-image-18\" data-wptb-image-alignment=\"center\"><div class=\"wptb-image-wrapper\">            <a class=\"wptb-link-target\" style=\"float: none;\" href=\"https:\/\/lithotheque.ac-montpellier.fr\/geoduc\" target=\"_blank\">                                <img loading=\"lazy\" decoding=\"async\" class=\"wptb-image-element-target\" height=\"165\" width=\"191\" style=\"width: 100%;\" src=\"\/\/collectionsgeol3d.gm.umontpellier.fr\/wp-content\/uploads\/2024\/07\/Capture-decran-2024-07-26-a-10.05.21.png\">            <\/a>        <\/div><\/div><div class=\"wptb-text-container wptb-ph-element wptb-element-text-5\" style=\"color: rgb(0, 0, 0); font-size: 15px;\"><div class=\"\" style=\"position: relative;\"><p><\/p><\/div><\/div><\/td><\/tr><tr class=\"wptb-row\" style=\"--hover-bg-color: undefined; background-color: rgb(255, 255, 255);\"><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"0\" data-y-index=\"1\" data-wptb-css-td-auto-width=\"true\"><\/td><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"1\" data-y-index=\"1\" data-wptb-css-td-auto-width=\"true\"><\/td><td class=\"wptb-cell\" data-y-index=\"1\" data-x-index=\"2\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-wptb-css-td-auto-width=\"true\" data-sorted-vertical=\"ask-disabled\"><\/td><td class=\"wptb-cell\" data-y-index=\"1\" data-x-index=\"3\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-wptb-css-td-auto-width=\"true\" data-sorted-vertical=\"ask-disabled\"><\/td><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"4\" data-y-index=\"1\" data-wptb-css-td-auto-width=\"true\"><div class=\"wptb-text-container wptb-ph-element wptb-element-text-6\"><div class=\"\" style=\"position: relative;\"><p><\/p><\/div><\/div><\/td><\/tr><tr class=\"wptb-row\" style=\"background-color: rgb(255, 255, 255); --hover-bg-color: undefined;\"><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"0\" data-y-index=\"2\" data-wptb-css-td-auto-width=\"true\"><div class=\"wptb-text-container wptb-ph-element wptb-element-text-1\"><div class=\"\" style=\"position: relative;\"><p><\/p><\/div><\/div><\/td><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"1\" data-y-index=\"2\" data-wptb-css-td-auto-width=\"true\"><div class=\"wptb-text-container wptb-ph-element wptb-element-text-2\" style=\"color: rgb(0, 0, 0); font-size: 15px;\"><div class=\"\" style=\"position: relative;\"><p><br><\/p><\/div><\/div><\/td><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"2\" data-y-index=\"2\" data-wptb-css-td-auto-width=\"true\"><div class=\"wptb-text-container wptb-ph-element wptb-element-text-3\"><div class=\"\" style=\"position: relative;\"><p><br><\/p><\/div><\/div><\/td><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"3\" data-y-index=\"2\" data-wptb-css-td-auto-width=\"true\"><div class=\"wptb-text-container wptb-ph-element wptb-element-text-4\"><div class=\"\" style=\"position: relative;\"><p><\/p><\/div><\/div><\/td><td class=\"wptb-cell\" style=\"border: 1px none rgb(255, 255, 255); padding: 8px;\" data-x-index=\"4\" data-y-index=\"2\" data-wptb-css-td-auto-width=\"true\"><div class=\"wptb-text-container wptb-ph-element wptb-element-text-7\"><div class=\"\" style=\"position: relative;\"><p><\/p><\/div><\/div><\/td><\/tr><\/tbody><\/table><\/div><\/div>\n\n","protected":false},"excerpt":{"rendered":"<p>La r\u00e9gion de Montpellier est marqu\u00e9e par deux r\u00e9gimes de d\u00e9formation majeurs. Un grand chevauchement E-W qui affecte les roches M\u00e9sozo\u00efque. Il est marqu\u00e9 par des d\u00e9p\u00f4ts de br\u00e8ches vitrolliennes au Nord. Cela indique un r\u00e9gime compressif N-S qui date &hellip; <a href=\"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/?page_id=1431\">Continuer la lecture <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":4,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"_links":{"self":[{"href":"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/index.php?rest_route=\/wp\/v2\/pages\/1431"}],"collection":[{"href":"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/index.php?rest_route=\/wp\/v2\/users\/4"}],"replies":[{"embeddable":true,"href":"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=1431"}],"version-history":[{"count":71,"href":"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/index.php?rest_route=\/wp\/v2\/pages\/1431\/revisions"}],"predecessor-version":[{"id":1907,"href":"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/index.php?rest_route=\/wp\/v2\/pages\/1431\/revisions\/1907"}],"wp:attachment":[{"href":"https:\/\/collectionsgeol3d.gm.umontpellier.fr\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=1431"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}