{"id":5385,"date":"2022-02-02T12:41:56","date_gmt":"2022-02-02T11:41:56","guid":{"rendered":"https:\/\/lyon-geologie.univ-lyon1.fr\/?page_id=5385"},"modified":"2023-01-17T12:13:58","modified_gmt":"2023-01-17T11:13:58","slug":"m2_geomorpho","status":"publish","type":"page","link":"https:\/\/lyongeologie.fr\/en\/m2-geosciences\/m2_geomorpho\/","title":{"rendered":"M2 G\u00e9omorphologie physique"},"content":{"rendered":"<div data-elementor-type=\"wp-page\" data-elementor-id=\"5385\" class=\"elementor elementor-5385\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-6109939d elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"6109939d\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-35a7f9c0\" data-id=\"35a7f9c0\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-688ce926 elementor-widget elementor-widget-text-editor\" data-id=\"688ce926\" data-element_type=\"widget\" data-e-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\t\t<h2><strong>Earth Surface Processes<br \/><\/strong><\/h2>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-5cb590b1 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"5cb590b1\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-33 elementor-top-column elementor-element elementor-element-3bfbd4b5\" data-id=\"3bfbd4b5\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-5ec95403 elementor-widget elementor-widget-text-editor\" data-id=\"5ec95403\" data-element_type=\"widget\" data-e-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\t\t<p><em>3 Credits<\/em><\/p><p><em>Contact: <a href=\"mailto:vincent.langlois@univ-lyon1.fr\">Vincent LANGLOIS<\/a><br \/><\/em><\/p>\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-649a75d elementor-widget elementor-widget-image\" data-id=\"649a75d\" data-element_type=\"widget\" data-e-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\t\t<img decoding=\"async\" width=\"150\" height=\"150\" src=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/vincent_langlois.png\" class=\"attachment-large size-large wp-image-8927\" alt=\"\" \/>\t\t\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-df279fa elementor-align-center elementor-widget elementor-widget-button\" data-id=\"df279fa\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"button.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div class=\"elementor-button-wrapper\">\n\t\t\t\t\t<a class=\"elementor-button elementor-button-link elementor-size-sm\" href=\"https:\/\/lyon-geologie.univ-lyon1.fr\/en\/m2-geosciences\/#m2_opt\">\n\t\t\t\t\t\t<span class=\"elementor-button-content-wrapper\">\n\t\t\t\t\t\t\t\t\t<span class=\"elementor-button-text\">Back to the previous page<\/span>\n\t\t\t\t\t<\/span>\n\t\t\t\t\t<\/a>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-66 elementor-top-column elementor-element elementor-element-10c1c02b\" data-id=\"10c1c02b\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-7e47679a elementor-widget elementor-widget-text-editor\" data-id=\"7e47679a\" data-element_type=\"widget\" data-e-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\t\t<p>Wind, water and ice all shape the landscapes of the Earth and other planets. In this course you will learn about the different processes that erode and transport sediment, and discover how they control the long-term dynamics of reliefs. We will in particular address the following topics:<\/p><ul><li><strong>Sand dunes:<\/strong> what determines their variety of shapes? Why are they larger on Mars than on Earth? What do they teach us about local weather conditions?<\/li><li><strong>Gravitational flows: <\/strong>from rockslides to pyroclastic flows and turbidity currents.<\/li><li><strong>Transport by rivers: <\/strong>how much sediment can a river deliver to the ocean? How do ripple marks, alternate sand bars and meanders form?<\/li><li><strong>River networks:<\/strong> how fast does a river cut through its bedrock? What is its equilibrium shape? What are the fractal properties of river networks?<\/li><li><strong>Periglacial geomorphology: <\/strong>rocky glaciers, polygonal patterns, thermal erosion.<\/li><\/ul><p>\u00a0<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<section class=\"elementor-section elementor-inner-section elementor-element elementor-element-3fec21e elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"3fec21e\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-33 elementor-inner-column elementor-element elementor-element-7dfc037\" data-id=\"7dfc037\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-d79857a elementor-widget elementor-widget-image\" data-id=\"d79857a\" data-element_type=\"widget\" data-e-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<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img fetchpriority=\"high\" decoding=\"async\" width=\"515\" height=\"400\" src=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/barchanes_mars.png\" class=\"attachment-medium_large size-medium_large wp-image-7699\" alt=\"\" srcset=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/barchanes_mars.png 515w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/barchanes_mars-300x233.png 300w\" sizes=\"(max-width: 515px) 100vw, 515px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\"><i><small>Barchan dunes on Mars<\/small><\/i><\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-33 elementor-inner-column elementor-element elementor-element-459e151\" data-id=\"459e151\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-dbce086 elementor-widget elementor-widget-image\" data-id=\"dbce086\" data-element_type=\"widget\" data-e-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<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"525\" height=\"291\" src=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/M2_geomorpho.png\" class=\"attachment-large size-large wp-image-5403\" alt=\"\" srcset=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/M2_geomorpho.png 525w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/M2_geomorpho-300x166.png 300w\" sizes=\"(max-width: 525px) 100vw, 525px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\"><i><small>Numerical model (Badlands) of the evolution of a mountainous landscape<\/small><\/i><\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-33 elementor-inner-column elementor-element elementor-element-88ec43f\" data-id=\"88ec43f\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-aa43e88 elementor-widget elementor-widget-image\" data-id=\"aa43e88\" data-element_type=\"widget\" data-e-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<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"882\" src=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/reunionrivers2-1024x882.png\" class=\"attachment-large size-large wp-image-7701\" alt=\"\" srcset=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/reunionrivers2-1024x882.png 1024w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/reunionrivers2-300x258.png 300w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/reunionrivers2-768x662.png 768w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/reunionrivers2.png 1214w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\"><i><small>River network of La R\u00e9union island<\/small><\/i><\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-inner-section elementor-element elementor-element-721bb07 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"721bb07\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-inner-column elementor-element elementor-element-d8d19e2\" data-id=\"d8d19e2\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-0150b07 elementor-widget elementor-widget-text-editor\" data-id=\"0150b07\" data-element_type=\"widget\" data-e-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\t\t<div>For all themes you will learn about field observations, new imagery techniques and simple theoretical models, as well as the most recent insights of analogical experiments and numerical simulations.<\/div><div>\u00a0<\/div><p>This course extends the L3 courses 'Geomorphology' and 'Solar System', and the M1 course 'Sedimentary dynamics'.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>","protected":false},"excerpt":{"rendered":"<p>G\u00e9omorphologie physique Cr\u00e9dits : 3 ECTS Responsable : Vincent LANGLOIS Retour \u00e0 la liste des UEs Le vent, l&rsquo;eau, la glace fa\u00e7onnent les paysages de la surface de la Terre et des autres plan\u00e8tes. Dans cette UE vous explorerez les diff\u00e9rents processus d&rsquo;\u00e9rosion et de transport s\u00e9dimentaires et d\u00e9couvrirez comment ils gouvernent la dynamique des [&hellip;]<\/p>\n","protected":false},"author":5,"featured_media":0,"parent":521,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"site-sidebar-layout":"no-sidebar","site-content-layout":"page-builder","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"disabled","ast-breadcrumbs-content":"","ast-featured-img":"disabled","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"class_list":["post-5385","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/5385","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/users\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/comments?post=5385"}],"version-history":[{"count":54,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/5385\/revisions"}],"predecessor-version":[{"id":16347,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/5385\/revisions\/16347"}],"up":[{"embeddable":true,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/521"}],"wp:attachment":[{"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/media?parent=5385"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}