{"id":2213,"date":"2016-06-07T16:03:28","date_gmt":"2016-06-07T16:03:28","guid":{"rendered":"https:\/\/courses.lumenlearning.com\/geologyxwaymakerxmaster\/?post_type=chapter&#038;p=2213"},"modified":"2025-10-13T17:04:23","modified_gmt":"2025-10-13T17:04:23","slug":"reading-falls","status":"publish","type":"chapter","link":"https:\/\/courses.lumenlearning.com\/geo\/chapter\/reading-falls\/","title":{"raw":"Reading: Falls","rendered":"Reading: Falls"},"content":{"raw":"[caption id=\"attachment_875\" align=\"alignright\" width=\"350\"]<img class=\"wp-image-875\" src=\"https:\/\/s3-us-west-2.amazonaws.com\/courses-images-archive-read-only\/wp-content\/uploads\/sites\/459\/2015\/06\/21062344\/Fig_10_1_4.jpg\" alt=\"Green hills with white streaks\" width=\"350\" height=\"186\" \/> Figure 1. The white areas on green hillsides mark scars from numerous mudflows.[\/caption]\r\n\r\nFalls are abrupt movements of masses of geologic materials, such as rocks and boulders, that become detached from steep slopes or cliffs. Separation occurs along discontinuities such as fractures, joints, and bedding planes, and movement occurs by free-fall, bouncing, and rolling. Falls are strongly influenced by gravity, mechanical weathering, and the presence of interstitial water.\r\n<h2>Lahars and Mudflow<\/h2>\r\nAdded water creates natural hazards produced by gravity (figure 1). On hillsides with soils rich in clay, little rain, and not much vegetation to hold the soil in place, a time of high precipitation will create a <strong>mudflow<\/strong>. Mudflows follow river channels, washing out bridges, trees, and homes that are in their path.\r\n<p id=\"x-ck12-NmVhOWY4ODBiYjI3OGQwZjMwMDYzZjg4ZDU0OGMyMDY.-x1x\">A lahar is mudflow that flows down a composite volcano (figure 2). Ash mixes with snow and ice melted by the eruption to produce hot, fast-moving flows. The lahar caused by the eruption of Nevado del Ruiz in Columbia in 1985 killed more than 23,000 people.<\/p>\r\n\r\n\r\n[caption id=\"attachment_876\" align=\"aligncenter\" width=\"500\"]<img class=\"wp-image-876 size-full\" src=\"https:\/\/s3-us-west-2.amazonaws.com\/courses-images-archive-read-only\/wp-content\/uploads\/sites\/459\/2015\/06\/21062345\/Fig_10_1_5.jpg\" alt=\"An erupted volcano with a lava stream flowing down\" width=\"500\" height=\"274\" \/> Figure 2. A lahar is a mudflow that forms from volcanic ash and debris.[\/caption]","rendered":"<div id=\"attachment_875\" style=\"width: 360px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-875\" class=\"wp-image-875\" src=\"https:\/\/s3-us-west-2.amazonaws.com\/courses-images-archive-read-only\/wp-content\/uploads\/sites\/459\/2015\/06\/21062344\/Fig_10_1_4.jpg\" alt=\"Green hills with white streaks\" width=\"350\" height=\"186\" \/><\/p>\n<p id=\"caption-attachment-875\" class=\"wp-caption-text\">Figure 1. The white areas on green hillsides mark scars from numerous mudflows.<\/p>\n<\/div>\n<p>Falls are abrupt movements of masses of geologic materials, such as rocks and boulders, that become detached from steep slopes or cliffs. Separation occurs along discontinuities such as fractures, joints, and bedding planes, and movement occurs by free-fall, bouncing, and rolling. Falls are strongly influenced by gravity, mechanical weathering, and the presence of interstitial water.<\/p>\n<h2>Lahars and Mudflow<\/h2>\n<p>Added water creates natural hazards produced by gravity (figure 1). On hillsides with soils rich in clay, little rain, and not much vegetation to hold the soil in place, a time of high precipitation will create a <strong>mudflow<\/strong>. Mudflows follow river channels, washing out bridges, trees, and homes that are in their path.<\/p>\n<p id=\"x-ck12-NmVhOWY4ODBiYjI3OGQwZjMwMDYzZjg4ZDU0OGMyMDY.-x1x\">A lahar is mudflow that flows down a composite volcano (figure 2). Ash mixes with snow and ice melted by the eruption to produce hot, fast-moving flows. The lahar caused by the eruption of Nevado del Ruiz in Columbia in 1985 killed more than 23,000 people.<\/p>\n<div id=\"attachment_876\" style=\"width: 510px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-876\" class=\"wp-image-876 size-full\" src=\"https:\/\/s3-us-west-2.amazonaws.com\/courses-images-archive-read-only\/wp-content\/uploads\/sites\/459\/2015\/06\/21062345\/Fig_10_1_5.jpg\" alt=\"An erupted volcano with a lava stream flowing down\" width=\"500\" height=\"274\" \/><\/p>\n<p id=\"caption-attachment-876\" class=\"wp-caption-text\">Figure 2. A lahar is a mudflow that forms from volcanic ash and debris.<\/p>\n<\/div>\n\n\t\t\t <section class=\"citations-section\" role=\"contentinfo\">\n\t\t\t <h3>Candela Citations<\/h3>\n\t\t\t\t\t <div>\n\t\t\t\t\t\t <div id=\"citation-list-2213\">\n\t\t\t\t\t\t\t <div class=\"licensing\"><div class=\"license-attribution-dropdown-subheading\">CC licensed content, Shared previously<\/div><ul class=\"citation-list\"><li>10.5: Erosion and Deposition by Gravity. <strong>Provided by<\/strong>: CK-12. <strong>Located at<\/strong>: <a target=\"_blank\" href=\"http:\/\/www.ck12.org\/book\/CK-12-Earth-Science-For-High-School\/section\/10.5\/\">http:\/\/www.ck12.org\/book\/CK-12-Earth-Science-For-High-School\/section\/10.5\/<\/a>. <strong>License<\/strong>: <em><a target=\"_blank\" rel=\"license\" href=\"https:\/\/creativecommons.org\/licenses\/by-nc\/4.0\/\">CC BY-NC: Attribution-NonCommercial<\/a><\/em><\/li><\/ul><div class=\"license-attribution-dropdown-subheading\">Public domain content<\/div><ul class=\"citation-list\"><li>Landslide Types and Processes. <strong>Provided by<\/strong>: USGS. <strong>Located at<\/strong>: <a target=\"_blank\" href=\"http:\/\/pubs.usgs.gov\/fs\/2004\/3072\/fs-2004-3072.html\">http:\/\/pubs.usgs.gov\/fs\/2004\/3072\/fs-2004-3072.html<\/a>. <strong>License<\/strong>: <em><a target=\"_blank\" rel=\"license\" href=\"https:\/\/creativecommons.org\/about\/pdm\">Public Domain: No Known Copyright<\/a><\/em><\/li><\/ul><\/div>\n\t\t\t\t\t\t <\/div>\n\t\t\t\t\t <\/div>\n\t\t\t <\/section>","protected":false},"author":17,"menu_order":4,"template":"","meta":{"_candela_citation":"[{\"type\":\"cc\",\"description\":\"10.5: Erosion and Deposition by Gravity\",\"author\":\"\",\"organization\":\"CK-12\",\"url\":\"http:\/\/www.ck12.org\/book\/CK-12-Earth-Science-For-High-School\/section\/10.5\/\",\"project\":\"\",\"license\":\"cc-by-nc\",\"license_terms\":\"\"},{\"type\":\"pd\",\"description\":\"Landslide Types and Processes\",\"author\":\"\",\"organization\":\"USGS\",\"url\":\"http:\/\/pubs.usgs.gov\/fs\/2004\/3072\/fs-2004-3072.html\",\"project\":\"\",\"license\":\"pd\",\"license_terms\":\"\"}]","CANDELA_OUTCOMES_GUID":"1c9be8cb-cf46-46f6-807a-de2ac6ff571a, 764bf22d-308a-4438-b08b-110d49cb063e","pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[],"contributor":[],"license":[],"class_list":["post-2213","chapter","type-chapter","status-publish","hentry"],"part":30,"_links":{"self":[{"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/pressbooks\/v2\/chapters\/2213","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/wp\/v2\/users\/17"}],"version-history":[{"count":8,"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/pressbooks\/v2\/chapters\/2213\/revisions"}],"predecessor-version":[{"id":3436,"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/pressbooks\/v2\/chapters\/2213\/revisions\/3436"}],"part":[{"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/pressbooks\/v2\/parts\/30"}],"metadata":[{"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/pressbooks\/v2\/chapters\/2213\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/wp\/v2\/media?parent=2213"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/pressbooks\/v2\/chapter-type?post=2213"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/wp\/v2\/contributor?post=2213"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/geo\/wp-json\/wp\/v2\/license?post=2213"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}