{"id":6783,"date":"2024-02-16T06:18:38","date_gmt":"2024-02-16T06:18:38","guid":{"rendered":"http:\/\/www.backroadswest.com\/blog\/santa-clara-volcano-hike-near-st-george-copy\/"},"modified":"2025-10-02T03:45:30","modified_gmt":"2025-10-02T03:45:30","slug":"st-george-area-roadcut-reveals-colorful-geology","status":"publish","type":"post","link":"http:\/\/www.backroadswest.com\/blog\/st-george-area-roadcut-reveals-colorful-geology\/","title":{"rendered":"St. George Roadcut Reveals Colorful Geology"},"content":{"rendered":"<!--themify_builder_content-->\n<div id=\"themify_builder_content-6783\" data-postid=\"6783\" class=\"themify_builder_content themify_builder_content-6783 themify_builder tf_clear\">\n                    <div  data-lazy=\"1\" class=\"module_row themify_builder_row tb_amq7461 tb_first tf_w\">\n                        <div class=\"row_inner col_align_top tb_col_count_2 tf_box tf_rel\">\n                        <div  data-lazy=\"1\" class=\"module_column tb-column col3-2 tb_5bn6444 first\">\n                    <!-- module text -->\n<div  class=\"module module-text tb_e7sw477    wow\" data-tf-animation=\"zoomIn\" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <p><strong>Southwest Utah is well known for its dazzling scenery thanks to the world-class geology that is in plain sight for everyone to enjoy<\/strong>. Most of this scenery is created by natural erosion that goes on continually for centuries, exposing the hidden beauty underneath.<\/p>    <\/div>\n<\/div>\n<!-- \/module text -->        <\/div>\n                    <div  data-lazy=\"1\" class=\"module_column tb-column col3-1 tb_unqw980 last\">\n                    <!-- module image -->\n<div  class=\"module module-image tb_ql7z180 image-top rounded drop-shadow  tf_mw wow\" data-tf-animation=\"fadeInRightBig\" data-lazy=\"1\">\n        <div class=\"image-wrap tf_rel tf_mw\">\n            <a href=\"https:\/\/www.youtube.com\/watch?v=95meMSxr4Pk\" rel=\"noopener\" target=\"_blank\">\n                   <img loading=\"lazy\" decoding=\"async\" width=\"350\" height=\"319\" src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/Roadcut.jpg\" class=\"wp-post-image wp-image-6777\" title=\"Roadcut\" alt=\"Roadcut\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/Roadcut.jpg 350w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/Roadcut-300x273.jpg 300w\" sizes=\"auto, (max-width: 350px) 100vw, 350px\" \/>        <\/a>\n    \n        <\/div>\n    <!-- \/image-wrap -->\n    \n        <\/div>\n<!-- \/module image -->        <\/div>\n                        <\/div>\n        <\/div>\n                        <div  data-lazy=\"1\" class=\"module_row themify_builder_row tb_y1u0600 tf_w\">\n                        <div class=\"row_inner col_align_top tb_col_count_1 tf_box tf_rel\">\n                        <div  data-lazy=\"1\" class=\"module_column tb-column col-full tb_jajh000 first\">\n                    <!-- module callout -->\n<div  class=\"module ui module-callout tb_p463060 button-bottom-center red  rounded embossed shadow wow\" data-tf-animation=\"fadeInLeft\" data-tf-animation_delay=\"1\" data-lazy=\"1\" id=\"video\">\n    \n    <div class=\"callout-inner\">\n    <div class=\"callout-content tf_left\">\n        <h3 class=\"callout-heading\"><\/h3>\n        <div class=\"tb_text_wrap\">\n            <strong>Click image<\/strong> to watch Virtual Video Tour and see viewer comments.\nThen come back to get the rest of the story.        <\/div>\n    <\/div>\n    <!-- \/callout-content -->\n        <\/div>\n    <!-- \/callout-content -->\n<\/div>\n<!-- \/module callout -->\n<!-- module image -->\n<div  class=\"module module-image tb_kb6x668 image-center bordered  tf_mw wow\" data-tf-animation=\"lightSpeedIn\" data-tf-animation_delay=\"1.5\" data-lazy=\"1\">\n        <div class=\"image-wrap tf_rel tf_mw\">\n            <a href=\"https:\/\/www.youtube.com\/watch?v=dRg0WAQBzEI\" rel=\"noopener\" target=\"_blank\">\n                   <img loading=\"lazy\" decoding=\"async\" width=\"978\" height=\"550\" src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutYouTube.jpg\" class=\"wp-post-image wp-image-6792\" title=\"RoadcutYouTube\" alt=\"RoadcutYouTube\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutYouTube.jpg 978w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutYouTube-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutYouTube-768x432.jpg 768w\" sizes=\"auto, (max-width: 978px) 100vw, 978px\" \/>        <\/a>\n    \n        <\/div>\n    <!-- \/image-wrap -->\n    \n        <\/div>\n<!-- \/module image -->        <\/div>\n                        <\/div>\n        <\/div>\n                        <div  data-lazy=\"1\" class=\"module_row themify_builder_row tb_dlgp096 tf_w\">\n                        <div class=\"row_inner col_align_top tb_col_count_1 tf_box tf_rel\">\n                        <div  data-lazy=\"1\" class=\"module_column tb-column col-full tb_vx4s800 first\">\n                    <!-- module text -->\n<div  class=\"module module-text tb_6v7p100   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <p>Sometimes, however, this process is sped up when certain manmade events happen. One of these events is called a roadcut. In many ways, roadcuts are a geologist\u2019s best friend. They provide an opportunity to see what\u2019s below the earth\u2019s surface and get a good look at the unaltered, hidden layers that wouldn\u2019t normally have been seen without these necessities of civilization.<\/p>\n<p>One intriguing roadcut that was just made in 2023 is in the town of Toquerville, about 20 miles northeast of St. George, Utah. This roadcut reveals some rather colorful sedimentary layers, including their curious angle or tilt. This tilt shows us something we can\u2019t easily see elsewhere \u2013 what happened beneath the Earth\u2019s surface at a specific point in time and how the nearby Hurricane Fault caused this odd tilt.<\/p>\n<h2>The Roadcut<\/h2>\n<p>This road cut was made while building what\u2019s known as the Toquerville bypass. It re-routes Highway 17 that runs between La Verkin and Interstate 15. The goal of the bypass is to route traffic away from the small, picturesque town of Toquerville, and have it go to the west, where there is wide open, undeveloped land.<\/p>    <\/div>\n<\/div>\n<!-- \/module text --><!-- module image -->\n<div  class=\"module module-image tb_c6o2665 image-center   tf_mw wow\" data-tf-animation=\"fadeIn\" data-lazy=\"1\">\n        <div class=\"image-wrap tf_rel tf_mw\">\n            <a href=\"https:\/\/www.backroadswest.com\/brw\/geology-tour-st-george\/\" rel=\"noopener\" target=\"_blank\">\n                   <img loading=\"lazy\" decoding=\"async\" width=\"800\" height=\"500\" src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/Ad-800x500-GeologyTour2.gif\" class=\"wp-post-image wp-image-6759\" title=\"Ad-800x500-GeologyTour2\" alt=\"Ad-800x500-GeologyTour2\">        <\/a>\n    \n        <\/div>\n    <!-- \/image-wrap -->\n    \n        <\/div>\n<!-- \/module image --><!-- module text -->\n<div  class=\"module module-text tb_1wm8500   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <p>Certainly, construction workers and area residents didn\u2019t expect what to see once the digging was completed. What can now be seen are thin layers of colorful yellow, orange and purplish colors, all tilting in an odd direction. Unfortunately, these layers are not very easy to see, and one can hope that after the construction is complete, people that pass by on the new bypass road will be able to see it.<\/p>\n<p>The cross section of the roadcut reveals four episodes (or layers) of erosional deposition. The first, on top, is the newest addition, consisting of alluvial deposits and area sand that, in recent times, accumulated at the top. Next down is this layer of dense basalt, which was created from a lava flow originating about ten miles north of the site. The third layer down are more alluvial deposits with larger boulders.<\/p>\n<p>The fourth layer is the most interesting. It\u2019s what geologists call the Iron Springs Formation, and it consists of those colorful layers. Plus, it\u2019s the only layer that is at a 20\u00b0 angle \u2013 the other three layers lie flat. The site is quite unusual and, for someone that enjoys geology, it makes for a great geologic mystery to solve.<\/p>\n<h2>The Roadcut&#8217;s Geology<\/h2>\n<p>As mentioned, roadcuts are a geologist\u2019s best friend. And that couldn\u2019t be truer than at the site of the Toquerville bypass. Motorists that will soon be speeding by will only notice the unusually colored stripes on both sides of the road. Most likely, most will not stop and study the roadcut to ponder what\u2019s going on. When the road is complete, hopefully the decision isn\u2019t made to shore up the sides of the roadcut that would hide what was exposed during its construction.<\/p>\n<p>While the roadcut is exposed for all to see, our interpretation comes with a disclaimer: we are not trained geologists. Nonetheless, we offer our observations, viewing this roadcut as a single piece in the intricate puzzle of Southwest Utah&#8217;s landscape. Read on, and we\u2019ll explain three aspects to that single puzzle piece.<\/p>\n<p>More&#8230;<\/p>\n<div class=\"g g-11\"><div class=\"g-single a-28\"><a class=\"gofollow\" data-track=\"MjgsMTEsNjA=\" title=\"Snap Shots West\" href=\"http:\/\/www.backroadswest.com\/ssw\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" class=\" size-medium wp-image-2382 aligncenter\" src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2021\/01\/Ad-800x500-1b.gif\" width=\"800\" height=\"500\" \/><\/a><\/div><\/div>    <\/div>\n<\/div>\n<!-- \/module text --><!-- module text -->\n<div  class=\"module module-text tb_1399687   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <h3>Support Us<\/h3>\n<p style=\"text-align: left;\">Help us fill up our tank with gas for our next trip by donating $5 and we&#8217;ll bring you back more quality virtual tours of our trips!<\/p>\n<p style=\"text-align: left;\">Your credit card payment is safe and easy using PayPal. Click the [Donate] button to get started:<\/p>\n<p style=\"text-align: center;\"><!-- Begin PayPal Donations by https:\/\/www.tipsandtricks-hq.com\/paypal-donations-widgets-plugin -->\n\n<form action=\"https:\/\/www.paypal.com\/cgi-bin\/webscr\" method=\"post\">\n    <div class=\"paypal-donations\">\n        <input type=\"hidden\" name=\"cmd\" value=\"_donations\" \/>\n        <input type=\"hidden\" name=\"bn\" value=\"TipsandTricks_SP\" \/>\n        <input type=\"hidden\" name=\"business\" value=\"ilene@backroadswest.com\" \/>\n        <input type=\"hidden\" name=\"return\" value=\"http:\/\/www.backroadswest.com\/blog\" \/>\n        <input type=\"hidden\" name=\"item_name\" value=\"Help fund our travel cost to create more trips\" \/>\n        <input type=\"hidden\" name=\"item_number\" value=\"BackRoadsWest Blog Donation\" \/>\n        <input type=\"hidden\" name=\"amount\" value=\"5.00\" \/>\n        <input type=\"hidden\" name=\"rm\" value=\"0\" \/>\n        <input type=\"hidden\" name=\"currency_code\" value=\"USD\" \/>\n        <input type=\"image\" style=\"cursor: pointer;\" src=\"https:\/\/www.paypalobjects.com\/en_US\/i\/btn\/btn_donateCC_LG.gif\" name=\"submit\" alt=\"PayPal - The safer, easier way to pay online.\" \/>\n        <img loading=\"lazy\" decoding=\"async\" alt=\"\" src=\"https:\/\/www.paypalobjects.com\/en_US\/i\/scr\/pixel.gif\" width=\"1\" height=\"1\" \/>\n    <\/div>\n<\/form>\n<!-- End PayPal Donations -->\n<\/p>    <\/div>\n<\/div>\n<!-- \/module text --><!-- module text -->\n<div  class=\"module module-text tb_ow8p98   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <h3>Pictures<\/h3><p>Below are some pictures of what you will see along the way.<\/p>    <\/div>\n<\/div>\n<!-- \/module text --><div  class=\"module themify_builder_slider_wrap tf_clearfix module-slider tb_1p2e805  slider-default  \" data-lazy=\"1\">\n        <div class=\"themify_builder_slider tf_carousel tf_swiper-container tf_rel tf_overflow\" data-lazy=\"1\"        data-visible=\"1\"\n        data-tab-visible=\"1\"\n        data-mob-visible=\"1\"\n        data-scroll=\"1\"\n                            data-auto=\"4000\"\n            data-controller=\"0\"\n            data-pause_hover=\"1\"\n                data-speed=\"1\"\n        data-wrapvar=\"1\"\n        data-slider_nav=\"1\"\n        data-pager=\"1\"\n        data-effect=\"scroll\" \n        data-height=\"variable\"\n        data-css_url=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/themes\/pinboard\/themify\/themify-builder\/css\/modules\/sliders\/carousel,http:\/\/www.backroadswest.com\/blog\/wp-content\/themes\/pinboard\/themify\/themify-builder\/css\/modules\/sliders\/slider\"\n                    >\n        <div class=\"tf_swiper-wrapper tf_lazy tf_rel tf_w tf_h tf_textc\">\n                         <div class=\"tf_swiper-slide\">            <div class=\"slide-inner-wrap\">\n                                    <div class=\"tf_rel tf_lazy slide-image\">\n                                                                            <img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='800'%20height='450'%20viewBox=%270%200%20800%20450%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#5a3c3e 25%,#4b88d8 25% 50%,#487dc9 50% 75%,#4d82c8 75%),linear-gradient(to right,#604443 25%,#6da2e4 25% 50%,#85b1ee 50% 75%,#f7e2d1 75%),linear-gradient(to right,#4e3636 25%,#543a39 25% 50%,#463f37 50% 75%,#edc4b0 75%),linear-gradient(to right,#604348 25%,#7b4835 25% 50%,#d2ad93 50% 75%,#987d6c 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-800x450.jpg\" width=\"800\" height=\"450\" class=\"tf_svg_lazy wp-post-image wp-image-6778\" title=\"RoadcutSldr1\" alt=\"Toquerville Bypass Roadcut looking west\" data-tf-srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-768x432.jpg 768w\" data-tf-sizes=\"(max-width: 800px) 100vw, 800px\" \/><noscript><img loading=\"lazy\" decoding=\"async\" data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-800x450.jpg\" width=\"800\" height=\"450\" class=\"wp-post-image wp-image-6778\" title=\"RoadcutSldr1\" alt=\"Toquerville Bypass Roadcut looking west\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-768x432.jpg 768w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/noscript>                                            <\/div>\n                \n                                    <div class=\"slide-content tb_text_wrap\">\n                        \n                                                    <div>Toquerville Bypass Roadcut looking west<\/div>\n                                            <\/div>\n                            <\/div>\n        <\/div>                     <div class=\"tf_swiper-slide\" style=\"content-visibility:hidden\">            <div class=\"slide-inner-wrap\">\n                                    <div class=\"tf_rel tf_lazy slide-image\">\n                                                                            <img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='800'%20height='450'%20viewBox=%270%200%20800%20450%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#7d6153 25%,#bba194 25% 50%,#a2918a 50% 75%,#7abbf5 75%),linear-gradient(to right,#ae9c88 25%,#bb9580 25% 50%,#a9897e 50% 75%,#90d0f3 75%),linear-gradient(to right,#9c7e58 25%,#95705e 25% 50%,#857870 50% 75%,#b2e9ee 75%),linear-gradient(to right,#564f49 25%,#6a6373 25% 50%,#1e1c1f 50% 75%,#9b7a6b 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-800x450.jpg\" width=\"800\" height=\"450\" class=\"tf_svg_lazy wp-post-image wp-image-6779\" title=\"RoadcutSldr2\" alt=\"Tilted layers of the Iron Springs Formation\" data-tf-srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-768x432.jpg 768w\" data-tf-sizes=\"(max-width: 800px) 100vw, 800px\" \/><noscript><img loading=\"lazy\" decoding=\"async\" data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-800x450.jpg\" width=\"800\" height=\"450\" class=\"wp-post-image wp-image-6779\" title=\"RoadcutSldr2\" alt=\"Tilted layers of the Iron Springs Formation\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-768x432.jpg 768w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/noscript>                                            <\/div>\n                \n                                    <div class=\"slide-content tb_text_wrap\">\n                        \n                                                    <div>Tilted layers of the Iron Springs Formation<\/div>\n                                            <\/div>\n                            <\/div>\n        <\/div>                     <div class=\"tf_swiper-slide\" style=\"content-visibility:hidden\">            <div class=\"slide-inner-wrap\">\n                                    <div class=\"tf_rel tf_lazy slide-image\">\n                                                                            <img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='800'%20height='450'%20viewBox=%270%200%20800%20450%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#3e5e91 25%,#243f6a 25% 50%,#b5a08d 50% 75%,#9f7952 75%),linear-gradient(to right,#4d75a6 25%,#98826a 25% 50%,#c5ad89 50% 75%,#a8937e 75%),linear-gradient(to right,#a79070 25%,#c9bb9e 25% 50%,#97684c 50% 75%,#4b3e36 75%),linear-gradient(to right,#9f7454 25%,#bfbaa4 25% 50%,#af8f66 50% 75%,#12121a 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-800x450.jpg\" width=\"800\" height=\"450\" class=\"tf_svg_lazy wp-post-image wp-image-6780\" title=\"RoadcutSldr3\" alt=\"Some of the roadcut&#039;s layers are a bit twisted\" data-tf-srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-768x432.jpg 768w\" data-tf-sizes=\"(max-width: 800px) 100vw, 800px\" \/><noscript><img loading=\"lazy\" decoding=\"async\" data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-800x450.jpg\" width=\"800\" height=\"450\" class=\"wp-post-image wp-image-6780\" title=\"RoadcutSldr3\" alt=\"Some of the roadcut&#039;s layers are a bit twisted\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-768x432.jpg 768w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/noscript>                                            <\/div>\n                \n                                    <div class=\"slide-content tb_text_wrap\">\n                        \n                                                    <div>Some of the roadcut&#8217;s layers are a bit twisted<\/div>\n                                            <\/div>\n                            <\/div>\n        <\/div>                     <div class=\"tf_swiper-slide\" style=\"content-visibility:hidden\">            <div class=\"slide-inner-wrap\">\n                                    <div class=\"tf_rel tf_lazy slide-image\">\n                                                                            <img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='800'%20height='450'%20viewBox=%270%200%20800%20450%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#d1bfb1 25%,#ccc1bf 25% 50%,#be9a84 50% 75%,#cdae92 75%),linear-gradient(to right,#c7bda4 25%,#e0e1d3 25% 50%,#d5c1a6 50% 75%,#aa9383 75%),linear-gradient(to right,#ae8f63 25%,#d3bb8d 25% 50%,#ffd9aa 50% 75%,#93a2a9 75%),linear-gradient(to right,#968976 25%,#b3a292 25% 50%,#798183 50% 75%,#4d5967 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-800x450.jpg\" width=\"800\" height=\"450\" class=\"tf_svg_lazy wp-post-image wp-image-6781\" title=\"RoadcutSldr4\" alt=\"Closer look at the layers\" data-tf-srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-768x432.jpg 768w\" data-tf-sizes=\"(max-width: 800px) 100vw, 800px\" \/><noscript><img loading=\"lazy\" decoding=\"async\" data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-800x450.jpg\" width=\"800\" height=\"450\" class=\"wp-post-image wp-image-6781\" title=\"RoadcutSldr4\" alt=\"Closer look at the layers\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-768x432.jpg 768w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/noscript>                                            <\/div>\n                \n                                    <div class=\"slide-content tb_text_wrap\">\n                        \n                                                    <div>Closer look at the layers<\/div>\n                                            <\/div>\n                            <\/div>\n        <\/div>            <\/div>\n    <\/div>\n<\/div>\n        <\/div>\n                        <\/div>\n        <\/div>\n                        <div  data-lazy=\"1\" class=\"module_row themify_builder_row tb_0yfj601 tf_w\">\n                        <div class=\"row_inner col_align_top tb_col_count_2 tf_box tf_rel\">\n                        <div  data-lazy=\"1\" class=\"module_column tb-column col4-2 tb_pppz001 first\">\n                    <!-- module text -->\n<div  class=\"module module-text tb_gyvl313   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <p style=\"text-align: center;\">Help fund our next trip and your next adventure by purchasing a subscription to Gaia GPS. We will receive a small commission from your purchase.<\/p>\n<p><a href=\"https:\/\/classic.avantlink.com\/click.php?tool_type=ml&amp;merchant_link_id=8988a2bc-2458-428a-a722-9a326e4941c5&amp;website_id=cb6aacf1-7563-4b97-8b5d-48e9519fe173\" target=\"_blank\" rel=\"noopener sponsored\"><img loading=\"lazy\" decoding=\"async\" style=\"border: 0px;\" src=\"https:\/\/classic.avantlink.com\/gbi\/bd4517b4-b0f2-4660-8208-2ade3a1fdb4c\/8988a2bc-2458-428a-a722-9a326e4941c5\/a24ae5c1-c37a-45ea-b3f8-5480cc46d529\/cb6aacf1-7563-4b97-8b5d-48e9519fe173\/image.png\" alt=\"\" width=\"300\" height=\"250\" \/><\/a><\/p>    <\/div>\n<\/div>\n<!-- \/module text -->        <\/div>\n                    <div  data-lazy=\"1\" class=\"module_column tb-column col4-2 tb_4uf4068 last\">\n                    <!-- module text -->\n<div  class=\"module module-text tb_s6y8861   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <p><script async src=\"https:\/\/pagead2.googlesyndication.com\/pagead\/js\/adsbygoogle.js\"><\/script><br \/>\n<!-- Skyscraper160x600 --><br \/>\n<ins class=\"adsbygoogle\" style=\"display:block\" data-ad-client=\"ca-pub-7400034802659664\" data-ad-slot=\"8100341909\" data-ad-format=\"auto\" data-full-width-responsive=\"true\"><\/ins><br \/>\n<script>\n     (adsbygoogle = window.adsbygoogle || []).push({});\n<\/script><\/p>\n    <\/div>\n<\/div>\n<!-- \/module text -->        <\/div>\n                        <\/div>\n        <\/div>\n                        <div  data-lazy=\"1\" class=\"module_row themify_builder_row tb_a1o9018 tf_w\">\n                        <div class=\"row_inner col_align_top tb_col_count_1 tf_box tf_rel\">\n                        <div  data-lazy=\"1\" class=\"module_column tb-column col-full tb_xbxh001 first\">\n                    <!-- module text -->\n<div  class=\"module module-text tb_60ob858   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <div class=\"g g-11\"><div class=\"g-single a-30\"><a class=\"gofollow\" data-track=\"MzAsMTEsNjA=\" title=\"BackRoadsWest.com\" href=\"https:\/\/www.backroadswest.com\/brw\/tour-planning\/\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" class=\" size-medium wp-image-2382 aligncenter\" src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/01\/Ad-800x500-TripPlan1.gif\" width=\"800\" height=\"500\" \/><\/a><\/div><\/div>    <\/div>\n<\/div>\n<!-- \/module text --><!-- module divider -->\n<div  class=\"module tf_mw module-divider tb_porv605 solid   \" style=\"border-width: 1px;border-color: #000;\" data-lazy=\"1\">\n    <\/div>\n<!-- \/module divider -->\n<!-- module text -->\n<div  class=\"module module-text tb_r724003   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <h2>The Colors<\/h2>\n<p>The multi-colored layers are part of what geologists call the Iron Springs Formation. This chunk of earthen material was deposited during the late Cretaceous period, between 95 to 65 million years ago. To put some perspective to this timeline, you may recall that the dinosaurs went extinct around 65 million years ago. This formation is two major layers above Zion\u2019s famous Navajo Sandstone deposited in the Jurassic period, and two layers below Bryce\u2019s (or Cedar Breaks) colorful Claron Formation.<\/p>\n<p>In the Utah Geological Survey, the Iron Springs Formation is described as: <em>the formation is variously colored grayish orange, pale yellowish orange, dark yellowish orange, white, pale reddish brown, and greenish gray and is locally stained by iron-manganese oxides, which accounts for the reddish colors<\/em>. When you look at the pictures in this article, do those words describe it? I think they do.<\/p>\n<p>Learn more about the various formations in Southwest Utah by following these steps:<\/p>\n<ul>\n<li>Go to the Utah Geological Survey website at: <a href=\"https:\/\/geology.utah.gov\/map-pub\/maps\/geologic-maps\/\" target=\"_blank\" rel=\"noopener\">https:\/\/geology.utah.gov\/map-pub\/maps\/geologic-maps\/<\/a><\/li>\n<li>Then, on the map, select the square over the St. George area (the very lower-left corner).<\/li>\n<li>In the pop-up, select Open PDF. Since the PDF is a large file, it will take a few moments to download.<\/li>\n<li>The first page is the colorful geologic map. Scroll down to page 2.<\/li>\n<li>The stratigraphy chart used in the video is on page 2. Scroll down to find the Iron Springs Formation.<\/li>\n<li>Below is a snippet of the stratigraphy chart showing the formations near the Iron Springs:<\/li>\n<\/ul>\n<p><a href=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-6823\" src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy.jpg\" alt=\"\" width=\"1204\" height=\"949\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy.jpg 1204w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy-300x236.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy-1024x807.jpg 1024w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy-768x605.jpg 768w\" sizes=\"auto, (max-width: 1204px) 100vw, 1204px\" \/><\/a><\/p>\n<h3>Iron Springs Formation<\/h3>\n<p>The Iron Springs Formation is named after a locality that is about ten miles northwest of Cedar City, Utah. However, the formation is exposed mainly around the Pine Valley Mountains. In other parts of Utah, this formation is called the Straight Cliffs Formation. The two formations aren\u2019t exactly the same but were deposited about the same period of time and consist mostly of the same Earthen material.<\/p>\n<p>In the Grand Staircase-Escalante National Monument, about 90 miles east of the roadcut, sits the massive Kaiparowits Plateau. Most of the plateau is made up of the Straight Cliffs Formation. The Iron Springs Formation near St. George shares many of same characteristics to what\u2019s seen on the Kaiparowits.<\/p>\n<p>Now about the colorful layers. During the Cretaceous period, this large area was swampy and consisted of a lot of organic material. When that organic material was buried by the formations above it, heat and pressure mineralized the organic material. The pressure came from the weight of the additional earthen material above it. Millions of years later, thanks to erosion, the material was exposed to our atmosphere, which in turn oxidized the various minerals and created an array of colors.<\/p>\n<p>This same process, where minerals were oxidized and created colorful scenery, has occurred in other places of the Southwest. One formation in particular is called the Chinle Formation. It\u2019s the remains of another swampy time in Earth\u2019s history. It\u2019s two formations below the Navajo Sandstone Formation mentioned earlier. The Chinle is famous for creating what is now the Painted Desert in Arizona and the Paria townsite in Utah, both having very colorful scenery.<\/p>    <\/div>\n<\/div>\n<!-- \/module text --><!-- module image -->\n<div  class=\"module module-image tb_ld69514 image-center   tf_mw wow\" data-tf-animation=\"fadeIn\" data-lazy=\"1\">\n        <div class=\"image-wrap tf_rel tf_mw\">\n            <a href=\"https:\/\/www.backroadswest.com\/brw\/geology-tour-st-george\/\" rel=\"noopener\" target=\"_blank\">\n                   <img loading=\"lazy\" decoding=\"async\" width=\"800\" height=\"500\" src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/Ad-800x500-GeologyTour1.gif\" class=\"wp-post-image wp-image-6758\" title=\"Ad-800x500-GeologyTour1\" alt=\"Ad-800x500-GeologyTour1\">        <\/a>\n    \n        <\/div>\n    <!-- \/image-wrap -->\n    \n        <\/div>\n<!-- \/module image --><!-- module text -->\n<div  class=\"module module-text tb_eh5f155   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <h2>The Angle<\/h2>\n<p>How was that curious angle created? It was the fault, of the Hurricane Fault. This major fault is just one mile to the east of the roadcut. As you may know, the Hurricane Fault is the western boundary of the Colorado Plateau and is the fracture where land on the east side uplifted over a mile high creating the plateau.<\/p>\n<p>The uplift is the reason for the uniquely level and layered geology on the east side of the fault. On the west side of the fault, the geology is jumbled up and crumpled. The land closer to the fault also sank.<\/p>\n<p>The same geologic formations on the west side of the fault exist on the east side, but at a different elevation because of the uplift. At the roadcut, the elevation of the Iron Springs Formation is about 3,000 feet (900 m). On the east side of the fault in the Colorado Plateau, it is exposed at 6,000 to 7,000 feet (2,000 m). This is where it is called the Straight Cliffs Formation, mentioned earlier. That offset is about 4,000 feet (1,220 m), meaning the formation uplifted and rose quite a distance.<\/p>\n<p>When the land on the east side of the fault rose, it tilted slightly to the east. The opposite occurred on the west side of the fault. This mainly happened because of the Basin and Range Province, between the Hurricane Fault and the Sierra Nevada Mountains in California, was being stretched apart, causing the land closest to the fault to sink. Watch the video for an animated diagram showing the tilting action.<\/p>\n<ul>\n<li><strong>See our article on <a title=\"Southwest Utah: A Triple Junction of Landscapes\" href=\"http:\/\/www.backroadswest.com\/blog\/triple-junction-southwest-utah\/\" target=\"_blank\" rel=\"noopener\">Southwest Utah&#8217;s Triple Junction<\/a>\u00a0<\/strong>that explains more details about the Hurricane Fault and the Colorado Plateau<\/li>\n<\/ul>\n<p>This is most likely the reason why we see the tilt in the roadcut. The small hills and ridges near the roadcut are also tilted the same direction \u2013 sinking to the east and raising towards the west.<\/p>\n<div class=\"g g-11\"><div class=\"g-single a-29\"><a class=\"gofollow\" data-track=\"MjksMTEsNjA=\" title=\"BackRoadsWest.com\" href=\"https:\/\/www.backroadswest.com\/brw\/geology-tour-st-george\/\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" class=\" size-medium wp-image-2382 aligncenter\" src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/Ad-800x500-GeologyTour2.gif\" width=\"800\" height=\"500\" \/><\/a><\/div><\/div>\n<h2>Missing Formations?<\/h2>\n<p>In our roadcut, between the colorful layers of the Iron Springs Formation and the next visible layer above containing alluvial deposits, there are a few formations missing. When a layer is missing, it is known as an unconformity. We know the layer is missing because in other areas, the formation exists.<\/p>\n<p>Think of an unconformity as a hamburger with layers such as buns, hamburger patty, tomatoes, pickles and lettuce. The hamburger is cut in half and the patty is removed. Between the two halves, there is now an unconformity on one side, the side with the patty missing.<\/p>\n<h3>Great Unconformity<\/h3>\n<p>The most well-known unconformity is in the Grand Canyon. It\u2019s known as the Great Unconformity. Here, it is easy to see that several large layers of geology were removed by erosion. It\u2019s a mystery as to how big they were or what material they consisted of. The unconformity in the roadcut isn\u2019t as big but there are a few missing formations nonetheless. Plus, we know what layers are missing and thus what they consisted of.<\/p>\n<p>One well-known formation that is missing is the Claron Formation. The Claron is famous for the hoodoos of Bryce Canyon National Park and other locales in Utah. The Claron is exposed and visible on both sides of the Hurricane Fault. Near the roadcut, it is visible near the base of the Pine Valley Mountains.<\/p>\n<p>Fifty miles north of the roadcut, in a place called Parowan Gap, a large outcrop of Claron Formation can be seen sitting on top Iron Springs Formation. This is what the area around the roadcut may have looked like:<\/p>    <\/div>\n<\/div>\n<!-- \/module text --><div  class=\"module themify_builder_slider_wrap tf_clearfix module-slider tb_ag7798  slider-default  slide-image-fullwidth\" data-lazy=\"1\">\n        <div class=\"themify_builder_slider tf_carousel tf_swiper-container tf_rel tf_overflow\" data-lazy=\"1\"        data-visible=\"1\"\n        data-tab-visible=\"1\"\n        data-mob-visible=\"1\"\n        data-scroll=\"1\"\n                            data-auto=\"4000\"\n            data-controller=\"0\"\n            data-pause_hover=\"1\"\n                data-speed=\"1\"\n        data-wrapvar=\"1\"\n        data-slider_nav=\"1\"\n        data-pager=\"1\"\n        data-effect=\"fade\" \n        data-height=\"variable\"\n        data-css_url=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/themes\/pinboard\/themify\/themify-builder\/css\/modules\/sliders\/carousel,http:\/\/www.backroadswest.com\/blog\/wp-content\/themes\/pinboard\/themify\/themify-builder\/css\/modules\/sliders\/slider\"\n                    >\n        <div class=\"tf_swiper-wrapper tf_lazy tf_rel tf_w tf_h tf_textc\">\n                         <div class=\"tf_swiper-slide\">            <div class=\"slide-inner-wrap\">\n                                    <div class=\"tf_rel tf_lazy slide-image\">\n                                                                            <img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='360'%20height='200'%20viewBox=%270%200%20360%20200%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#bbcce8 25%,#013b8f 25% 50%,#0c3b81 50% 75%,#00439c 75%),linear-gradient(to right,#528ad5 25%,#534f44 25% 50%,#bd9e89 50% 75%,#948276 75%),linear-gradient(to right,#554434 25%,#d3bda5 25% 50%,#af9481 50% 75%,#271707 75%),linear-gradient(to right,#908474 25%,#a08a73 25% 50%,#614b3d 50% 75%,#3b2f23 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutClaron1-360x200.jpg\" width=\"360\" height=\"200\" class=\"tf_svg_lazy wp-post-image wp-image-6828\" title=\"RoadcutClaron1\" alt=\"Claron &amp; Iron Springs Formation\"><noscript><img loading=\"lazy\" decoding=\"async\" data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutClaron1-360x200.jpg\" width=\"360\" height=\"200\" class=\"wp-post-image wp-image-6828\" title=\"RoadcutClaron1\" alt=\"Claron &amp; Iron Springs Formation\"><\/noscript>                                            <\/div>\n                \n                                    <div class=\"slide-content tb_text_wrap\">\n                        \n                                                    <div>Claron Formation on top, Iron Springs Formation (small layers) below it<\/div>\n                                            <\/div>\n                            <\/div>\n        <\/div>                     <div class=\"tf_swiper-slide\" style=\"content-visibility:hidden\">            <div class=\"slide-inner-wrap\">\n                                    <div class=\"tf_rel tf_lazy slide-image\">\n                                                                            <img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='360'%20height='200'%20viewBox=%270%200%20360%20200%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#02469b 25%,#87564f 25% 50%,#130e12 50% 75%,#a48372 75%),linear-gradient(to right,#755c57 25%,#c29d8a 25% 50%,#5b3f3e 50% 75%,#ba6850 75%),linear-gradient(to right,#664c3d 25%,#baa590 25% 50%,#a1725e 50% 75%,#bd7b61 75%),linear-gradient(to right,#ddbba2 25%,#f7e5cf 25% 50%,#d5bba2 50% 75%,#976d55 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutClaron2-360x200.jpg\" width=\"360\" height=\"200\" class=\"tf_svg_lazy wp-post-image wp-image-6829\" title=\"RoadcutClaron2\" alt=\"Closeup of Claron &amp; Iron Springs Formation contact\"><noscript><img loading=\"lazy\" decoding=\"async\" data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutClaron2-360x200.jpg\" width=\"360\" height=\"200\" class=\"wp-post-image wp-image-6829\" title=\"RoadcutClaron2\" alt=\"Closeup of Claron &amp; Iron Springs Formation contact\"><\/noscript>                                            <\/div>\n                \n                                    <div class=\"slide-content tb_text_wrap\">\n                        \n                                                    <div>Closeup of contact between Claron &#038; Iron Springs Formations<\/div>\n                                            <\/div>\n                            <\/div>\n        <\/div>            <\/div>\n    <\/div>\n<\/div>\n<!-- module text -->\n<div  class=\"module module-text tb_1bbv543   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <p>Refer to the stratigraphy chart from the Utah Geological Survey referenced earlier to see where the Iron Springs Formation is in relation to the Claron. The Claron is basically two formations above the Iron Springs. So, between the colorful layers we see in the roadcut and the alluvial deposits above it, there used to be two other significant rock layers.<\/p>\n<h2>Summary<\/h2>\n<p>Isn\u2019t it amazing to see how all the pieces of a very large jigsaw puzzle come together? It\u2019s why geology is so fascinating to us. Yes, this landscape is beautiful but isn\u2019t it just a little more interesting when you know more about its complex nature? One doesn\u2019t need to be an expert in geology to see the puzzle pieces that put together the scenery of Southwest Utah.<\/p>\n<p>Now that you know more about this roadcut, we hope that when you take road trips from now on, you\u2019ll pay a little more attention to the roadcuts you drive through and wonder what geologic story they are telling. You might also start to wonder what\u2019s just below the surface of the landscapes you\u2019re passing over and what lays just below the surface.<\/p>\n<h2>Trip Map<\/h2>\n<p>To help plan your trip, use our interactive Google Map below. Be sure to switch to Satellite view to see the terrain.<\/p>\n<p>Most of the maps in our videos were created using Gaia GPS. Click the ad below to purchase a Gaia GPS subscription and we&#8217;ll earn a few dollars to fund our next trip.<\/p>\n<p><a href=\"https:\/\/classic.avantlink.com\/click.php?tool_type=ml&amp;merchant_link_id=2efe71d3-5569-4c72-a69e-e9258881dd0a&amp;website_id=cb6aacf1-7563-4b97-8b5d-48e9519fe173\" target=\"_blank\" rel=\"noopener sponsored\"><img loading=\"lazy\" decoding=\"async\" style=\"border: 0px;\" src=\"https:\/\/classic.avantlink.com\/gbi\/bd4517b4-b0f2-4660-8208-2ade3a1fdb4c\/2efe71d3-5569-4c72-a69e-e9258881dd0a\/a24ae5c1-c37a-45ea-b3f8-5480cc46d529\/cb6aacf1-7563-4b97-8b5d-48e9519fe173\/image.png\" alt=\"\" width=\"728\" height=\"90\" \/><\/a><\/p>\n<p><a href=\"http:\/\/www.backroadswest.com\/blog\/map\/\">Learn more<\/a> about our maps.<\/p>    <\/div>\n<\/div>\n<!-- \/module text --><!-- module maps pro -->\n<div  id=\"tb_r7uk678\" class=\"module module-maps-pro tb_r7uk678  tf_lazy\" data-zoom=\"13\" data-type=\"HYBRID\" data-address=\"37.22373, -113.28252\" data-scrollwheel=\"1\" data-draggable=\"enable\" data-disable_map_ui=\"\" data-polyline=\"\" data-geodesic=\"\" data-polylineStroke=\"2\" data-polylineColor=\"\" data-trigger=\"\" data-mapid=\"\" data-style_map=\"pale-dawn\" data-legacymarkers=\"\" data-lazy=\"1\">\n\t\n\t\t\t<div class=\"maps-pro-canvas-container\">\n\t\t\t<div class=\"maps-pro-canvas\" style=\"width:100%;height:500px\"><\/div>\n\t\t<\/div>\n\t\t\t\t\t<template>\n\t\t\t\t\t\t\t\t\t<div data-address=\"37.22373064116173,-113.282522814843\" data-image=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2015\/04\/icon-info.png\">\n\t\t\t\t\t\tSite of roadcut\t\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<\/template>\n\t\t\t\t\n\t<\/div>\n<!-- \/module maps pro --><!-- module text -->\n<div  class=\"module module-text tb_r2l7058   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <h3>Comments<\/h3>\n<p>Read and leave comments about this post on <a href=\"https:\/\/www.youtube.com\/watch?v=dRg0WAQBzEI\" target=\"_blank\" rel=\"noopener\">YouTube<\/a>.<\/p>    <\/div>\n<\/div>\n<!-- \/module text -->        <\/div>\n                        <\/div>\n        <\/div>\n                        <div  data-lazy=\"1\" class=\"module_row themify_builder_row tb_elpo600 tf_w\">\n                        <div class=\"row_inner col_align_top tb_col_count_2 tf_box tf_rel\">\n                        <div  data-lazy=\"1\" class=\"module_column tb-column col4-2 tb_jrs4010 first\">\n                    <!-- module text -->\n<div  class=\"module module-text tb_bb84062   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <h3>Support Us<\/h3><p>Help us fill up our tank with gas for our next trip by donating $5 and we&#8217;ll bring you back more quality virtual tours of our trips!<\/p><p>Your credit card payment is safe and easy using PayPal. Click the [Donate] button to get started:<\/p><!-- Begin PayPal Donations by https:\/\/www.tipsandtricks-hq.com\/paypal-donations-widgets-plugin -->\n\n<form action=\"https:\/\/www.paypal.com\/cgi-bin\/webscr\" method=\"post\">\n    <div class=\"paypal-donations\">\n        <input type=\"hidden\" name=\"cmd\" value=\"_donations\" \/>\n        <input type=\"hidden\" name=\"bn\" value=\"TipsandTricks_SP\" \/>\n        <input type=\"hidden\" name=\"business\" value=\"ilene@backroadswest.com\" \/>\n        <input type=\"hidden\" name=\"return\" value=\"http:\/\/www.backroadswest.com\/blog\" \/>\n        <input type=\"hidden\" name=\"item_name\" value=\"Help fund our travel cost to create more trips\" \/>\n        <input type=\"hidden\" name=\"item_number\" value=\"BackRoadsWest Blog Donation\" \/>\n        <input type=\"hidden\" name=\"amount\" value=\"5.00\" \/>\n        <input type=\"hidden\" name=\"rm\" value=\"0\" \/>\n        <input type=\"hidden\" name=\"currency_code\" value=\"USD\" \/>\n        <input type=\"image\" style=\"cursor: pointer;\" src=\"https:\/\/www.paypalobjects.com\/en_US\/i\/btn\/btn_donateCC_LG.gif\" name=\"submit\" alt=\"PayPal - The safer, easier way to pay online.\" \/>\n        <img loading=\"lazy\" decoding=\"async\" alt=\"\" src=\"https:\/\/www.paypalobjects.com\/en_US\/i\/scr\/pixel.gif\" width=\"1\" height=\"1\" \/>\n    <\/div>\n<\/form>\n<!-- End PayPal Donations -->\n    <\/div>\n<\/div>\n<!-- \/module text -->        <\/div>\n                    <div  data-lazy=\"1\" class=\"module_column tb-column col4-2 tb_w70v085 last\">\n                    <!-- module text -->\n<div  class=\"module module-text tb_28za500   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <h3 style=\"text-align: left;\">Subscribe<\/h3>\n\n    <\/div>\n<\/div>\n<!-- \/module text -->        <\/div>\n                        <\/div>\n        <\/div>\n                        <div  data-lazy=\"1\" class=\"module_row themify_builder_row tb_egvq618 tf_w\">\n                        <div class=\"row_inner col_align_top tb_col_count_1 tf_box tf_rel\">\n                        <div  data-lazy=\"1\" class=\"module_column tb-column col-full tb_a1qi616 first\">\n                    <!-- module text -->\n<div  class=\"module module-text tb_0mtn900   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <p style=\"text-align: center;\"><em>See all our comprehensive virtual tour guides at<\/em>:<\/p><p style=\"text-align: justify;\"><a title=\"BackRoadsWest\" href=\"http:\/\/www.backroadswest.com\/brw\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" class=\" size-medium wp-image-2382 aligncenter\" src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2015\/04\/BRWlogo-300x40.jpg\" alt=\"BRWlogo\" width=\"300\" height=\"40\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2015\/04\/BRWlogo-300x40.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2015\/04\/BRWlogo.jpg 438w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><\/p>    <\/div>\n<\/div>\n<!-- \/module text --><!-- module text -->\n<div  class=\"module module-text tb_ibhn554   \" data-lazy=\"1\">\n        <div  class=\"tb_text_wrap\">\n        <p><script async src=\"https:\/\/pagead2.googlesyndication.com\/pagead\/js\/adsbygoogle.js\"><\/script><br \/>\n<!-- Short-wide --><br \/>\n<ins class=\"adsbygoogle\" style=\"display:inline-block;width:728px;height:90px\" data-ad-client=\"ca-pub-7400034802659664\" data-ad-slot=\"1662640655\"><\/ins><br \/>\n<script>\n     (adsbygoogle = window.adsbygoogle || []).push({});\n<\/script><\/p>\n    <\/div>\n<\/div>\n<!-- \/module text --><!-- module callout -->\n<div  class=\"module ui module-callout tb_0rm1444 button-bottom red  rounded gradient shadow wow\" data-tf-animation=\"rubberBand\" data-lazy=\"1\">\n    \n    <div class=\"callout-inner\">\n    <div class=\"callout-content tf_left\">\n        <h3 class=\"callout-heading\">More Trips<\/h3>\n        <div class=\"tb_text_wrap\">\n            Would you like to go on more trips in Nevada?        <\/div>\n    <\/div>\n    <!-- \/callout-content -->\n                    <div class=\"callout-button tf_right tf_textr\">\n            <a href=\"http:\/\/www.backroadswest.com\/blog\/category\/nevada\/\" class=\"ui builder_button rounded gradient shadow yellow\">\n                <span class=\"tb_callout_text\">See More Trips in Nevada<\/span>\n            <\/a>\n        <\/div>\n            <\/div>\n    <!-- \/callout-content -->\n<\/div>\n<!-- \/module callout -->\n        <\/div>\n                        <\/div>\n        <\/div>\n        <\/div>\n<!--\/themify_builder_content-->","protected":false},"excerpt":{"rendered":"<p>Southwest Utah is well known for its dazzling scenery thanks to the world-class geology that is in plain sight for everyone to enjoy. Most of this scenery is created by natural erosion that goes on continually for centuries, exposing the hidden beauty underneath.<\/p>\n","protected":false},"author":2,"featured_media":6777,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[24,12,15,21],"tags":[],"class_list":["post-6783","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-geology","category-places","category-roadeasy","category-utah","has-post-title","has-post-date","has-post-category","has-post-tag","has-post-comment","has-post-author",""],"aioseo_notices":[],"aioseo_head":"\n\t\t<!-- All in One SEO 4.9.9 - aioseo.com -->\n\t<meta name=\"description\" content=\"This roadcut 20 miles northeast of St. George, Utah in Toquerville reveals some colorful geology and sedimentary layers, including its curious angle or tilt.\" \/>\n\t<meta name=\"robots\" content=\"max-image-preview:large\" \/>\n\t<meta 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06:18:42","updated":"2026-05-13 18:41:56","seo_analyzer_scan_date":null},"aioseo_breadcrumb":"<div class=\"aioseo-breadcrumbs\"><span class=\"aioseo-breadcrumb\">\n\t\t\t<a href=\"http:\/\/www.backroadswest.com\/blog\" title=\"Home\">Home<\/a>\n\t\t<\/span><span class=\"aioseo-breadcrumb-separator\">&raquo;<\/span><span class=\"aioseo-breadcrumb\">\n\t\t\t<a href=\"http:\/\/www.backroadswest.com\/blog\/category\/places\/\" title=\"Places\">Places<\/a>\n\t\t<\/span><span class=\"aioseo-breadcrumb-separator\">&raquo;<\/span><span class=\"aioseo-breadcrumb\">\n\t\t\tSt. George Roadcut Reveals Colorful Geology\n\t\t<\/span><\/div>","aioseo_breadcrumb_json":[{"label":"Home","link":"http:\/\/www.backroadswest.com\/blog"},{"label":"Places","link":"http:\/\/www.backroadswest.com\/blog\/category\/places\/"},{"label":"St. George Roadcut Reveals Colorful Geology","link":"http:\/\/www.backroadswest.com\/blog\/st-george-area-roadcut-reveals-colorful-geology\/"}],"builder_content":"<p><strong>Southwest Utah is well known for its dazzling scenery thanks to the world-class geology that is in plain sight for everyone to enjoy<\/strong>. Most of this scenery is created by natural erosion that goes on continually for centuries, exposing the hidden beauty underneath.<\/p>\n<a href=\"https:\/\/www.youtube.com\/watch?v=95meMSxr4Pk\" rel=\"noopener\" target=\"_blank\"> <img src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/Roadcut.jpg\" title=\"Roadcut\" alt=\"Roadcut\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/Roadcut.jpg 350w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/Roadcut-300x273.jpg 300w\" sizes=\"(max-width: 350px) 100vw, 350px\" \/> <\/a>\n<h3><\/h3> <strong>Click image<\/strong> to watch Virtual Video Tour and see viewer comments. Then come back to get the rest of the story.\n<a href=\"https:\/\/www.youtube.com\/watch?v=dRg0WAQBzEI\" rel=\"noopener\" target=\"_blank\"> <img src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutYouTube.jpg\" title=\"RoadcutYouTube\" alt=\"RoadcutYouTube\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutYouTube.jpg 978w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutYouTube-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutYouTube-768x432.jpg 768w\" sizes=\"(max-width: 978px) 100vw, 978px\" \/> <\/a>\n<p>Sometimes, however, this process is sped up when certain manmade events happen. One of these events is called a roadcut. In many ways, roadcuts are a geologist\u2019s best friend. They provide an opportunity to see what\u2019s below the earth\u2019s surface and get a good look at the unaltered, hidden layers that wouldn\u2019t normally have been seen without these necessities of civilization.<\/p> <p>One intriguing roadcut that was just made in 2023 is in the town of Toquerville, about 20 miles northeast of St. George, Utah. This roadcut reveals some rather colorful sedimentary layers, including their curious angle or tilt. This tilt shows us something we can\u2019t easily see elsewhere \u2013 what happened beneath the Earth\u2019s surface at a specific point in time and how the nearby Hurricane Fault caused this odd tilt.<\/p> <h2>The Roadcut<\/h2> <p>This road cut was made while building what\u2019s known as the Toquerville bypass. It re-routes Highway 17 that runs between La Verkin and Interstate 15. The goal of the bypass is to route traffic away from the small, picturesque town of Toquerville, and have it go to the west, where there is wide open, undeveloped land.<\/p>\n<a href=\"https:\/\/www.backroadswest.com\/brw\/geology-tour-st-george\/\" rel=\"noopener\" target=\"_blank\"> <img src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/Ad-800x500-GeologyTour2.gif\" title=\"Ad-800x500-GeologyTour2\" alt=\"Ad-800x500-GeologyTour2\"> <\/a>\n<p>Certainly, construction workers and area residents didn\u2019t expect what to see once the digging was completed. What can now be seen are thin layers of colorful yellow, orange and purplish colors, all tilting in an odd direction. Unfortunately, these layers are not very easy to see, and one can hope that after the construction is complete, people that pass by on the new bypass road will be able to see it.<\/p> <p>The cross section of the roadcut reveals four episodes (or layers) of erosional deposition. The first, on top, is the newest addition, consisting of alluvial deposits and area sand that, in recent times, accumulated at the top. Next down is this layer of dense basalt, which was created from a lava flow originating about ten miles north of the site. The third layer down are more alluvial deposits with larger boulders.<\/p> <p>The fourth layer is the most interesting. It\u2019s what geologists call the Iron Springs Formation, and it consists of those colorful layers. Plus, it\u2019s the only layer that is at a 20\u00b0 angle \u2013 the other three layers lie flat. The site is quite unusual and, for someone that enjoys geology, it makes for a great geologic mystery to solve.<\/p> <h2>The Roadcut's Geology<\/h2> <p>As mentioned, roadcuts are a geologist\u2019s best friend. And that couldn\u2019t be truer than at the site of the Toquerville bypass. Motorists that will soon be speeding by will only notice the unusually colored stripes on both sides of the road. Most likely, most will not stop and study the roadcut to ponder what\u2019s going on. When the road is complete, hopefully the decision isn\u2019t made to shore up the sides of the roadcut that would hide what was exposed during its construction.<\/p> <p>While the roadcut is exposed for all to see, our interpretation comes with a disclaimer: we are not trained geologists. Nonetheless, we offer our observations, viewing this roadcut as a single piece in the intricate puzzle of Southwest Utah's landscape. Read on, and we\u2019ll explain three aspects to that single puzzle piece.<\/p> <p>More...<\/p> <p>[adrotate group=\"11\"]<\/p>\n<h3>Support Us<\/h3> <p style=\"text-align: left;\">Help us fill up our tank with gas for our next trip by donating $5 and we'll bring you back more quality virtual tours of our trips!<\/p> <p style=\"text-align: left;\">Your credit card payment is safe and easy using PayPal. Click the [Donate] button to get started:<\/p> <p style=\"text-align: center;\">[paypal-donation]<\/p>\n<h3>Pictures<\/h3><p>Below are some pictures of what you will see along the way.<\/p>\n<img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='800'%20height='450'%20viewBox=%270%200%20800%20450%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#5a3c3e 25%,#4b88d8 25% 50%,#487dc9 50% 75%,#4d82c8 75%),linear-gradient(to right,#604443 25%,#6da2e4 25% 50%,#85b1ee 50% 75%,#f7e2d1 75%),linear-gradient(to right,#4e3636 25%,#543a39 25% 50%,#463f37 50% 75%,#edc4b0 75%),linear-gradient(to right,#604348 25%,#7b4835 25% 50%,#d2ad93 50% 75%,#987d6c 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-800x450.jpg\" width=\"800\" height=\"450\" title=\"RoadcutSldr1\" alt=\"Toquerville Bypass Roadcut looking west\" data-tf-srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-768x432.jpg 768w\" data-tf-sizes=\"(max-width: 800px) 100vw, 800px\" \/><noscript><img data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-800x450.jpg\" width=\"800\" height=\"450\" title=\"RoadcutSldr1\" alt=\"Toquerville Bypass Roadcut looking west\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr1-768x432.jpg 768w\" sizes=\"(max-width: 800px) 100vw, 800px\" \/><\/noscript> Toquerville Bypass Roadcut looking west <img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='800'%20height='450'%20viewBox=%270%200%20800%20450%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#7d6153 25%,#bba194 25% 50%,#a2918a 50% 75%,#7abbf5 75%),linear-gradient(to right,#ae9c88 25%,#bb9580 25% 50%,#a9897e 50% 75%,#90d0f3 75%),linear-gradient(to right,#9c7e58 25%,#95705e 25% 50%,#857870 50% 75%,#b2e9ee 75%),linear-gradient(to right,#564f49 25%,#6a6373 25% 50%,#1e1c1f 50% 75%,#9b7a6b 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-800x450.jpg\" width=\"800\" height=\"450\" title=\"RoadcutSldr2\" alt=\"Tilted layers of the Iron Springs Formation\" data-tf-srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-768x432.jpg 768w\" data-tf-sizes=\"(max-width: 800px) 100vw, 800px\" \/><noscript><img data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-800x450.jpg\" width=\"800\" height=\"450\" title=\"RoadcutSldr2\" alt=\"Tilted layers of the Iron Springs Formation\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr2-768x432.jpg 768w\" sizes=\"(max-width: 800px) 100vw, 800px\" \/><\/noscript> Tilted layers of the Iron Springs Formation <img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='800'%20height='450'%20viewBox=%270%200%20800%20450%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#3e5e91 25%,#243f6a 25% 50%,#b5a08d 50% 75%,#9f7952 75%),linear-gradient(to right,#4d75a6 25%,#98826a 25% 50%,#c5ad89 50% 75%,#a8937e 75%),linear-gradient(to right,#a79070 25%,#c9bb9e 25% 50%,#97684c 50% 75%,#4b3e36 75%),linear-gradient(to right,#9f7454 25%,#bfbaa4 25% 50%,#af8f66 50% 75%,#12121a 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-800x450.jpg\" width=\"800\" height=\"450\" title=\"RoadcutSldr3\" alt=\"Some of the roadcut&#039;s layers are a bit twisted\" data-tf-srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-768x432.jpg 768w\" data-tf-sizes=\"(max-width: 800px) 100vw, 800px\" \/><noscript><img data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-800x450.jpg\" width=\"800\" height=\"450\" title=\"RoadcutSldr3\" alt=\"Some of the roadcut&#039;s layers are a bit twisted\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr3-768x432.jpg 768w\" sizes=\"(max-width: 800px) 100vw, 800px\" \/><\/noscript> Some of the roadcut's layers are a bit twisted <img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='800'%20height='450'%20viewBox=%270%200%20800%20450%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#d1bfb1 25%,#ccc1bf 25% 50%,#be9a84 50% 75%,#cdae92 75%),linear-gradient(to right,#c7bda4 25%,#e0e1d3 25% 50%,#d5c1a6 50% 75%,#aa9383 75%),linear-gradient(to right,#ae8f63 25%,#d3bb8d 25% 50%,#ffd9aa 50% 75%,#93a2a9 75%),linear-gradient(to right,#968976 25%,#b3a292 25% 50%,#798183 50% 75%,#4d5967 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-800x450.jpg\" width=\"800\" height=\"450\" title=\"RoadcutSldr4\" alt=\"Closer look at the layers\" data-tf-srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-768x432.jpg 768w\" data-tf-sizes=\"(max-width: 800px) 100vw, 800px\" \/><noscript><img data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-800x450.jpg\" width=\"800\" height=\"450\" title=\"RoadcutSldr4\" alt=\"Closer look at the layers\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4.jpg 800w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-300x169.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/RoadcutSldr4-768x432.jpg 768w\" sizes=\"(max-width: 800px) 100vw, 800px\" \/><\/noscript> Closer look at the layers\n<p style=\"text-align: center;\">Help fund our next trip and your next adventure by purchasing a subscription to Gaia GPS. We will receive a small commission from your purchase.<\/p> <p><a href=\"https:\/\/classic.avantlink.com\/click.php?tool_type=ml&amp;merchant_link_id=8988a2bc-2458-428a-a722-9a326e4941c5&amp;website_id=cb6aacf1-7563-4b97-8b5d-48e9519fe173\" target=\"_blank\" rel=\"noopener sponsored\"><img loading=\"lazy\" decoding=\"async\" style=\"border: 0px;\" src=\"https:\/\/classic.avantlink.com\/gbi\/bd4517b4-b0f2-4660-8208-2ade3a1fdb4c\/8988a2bc-2458-428a-a722-9a326e4941c5\/a24ae5c1-c37a-45ea-b3f8-5480cc46d529\/cb6aacf1-7563-4b97-8b5d-48e9519fe173\/image.png\" alt=\"\" width=\"300\" height=\"250\" \/><\/a><\/p>\n<p><br \/> <br \/> <ins style=\"display:block\" data-ad-client=\"ca-pub-7400034802659664\" data-ad-slot=\"8100341909\" data-ad-format=\"auto\" data-full-width-responsive=\"true\"><\/ins><br \/> <\/p>\n<p>[adrotate group=\"11\"]<\/p>\n\n<h2>The Colors<\/h2> <p>The multi-colored layers are part of what geologists call the Iron Springs Formation. This chunk of earthen material was deposited during the late Cretaceous period, between 95 to 65 million years ago. To put some perspective to this timeline, you may recall that the dinosaurs went extinct around 65 million years ago. This formation is two major layers above Zion\u2019s famous Navajo Sandstone deposited in the Jurassic period, and two layers below Bryce\u2019s (or Cedar Breaks) colorful Claron Formation.<\/p> <p>In the Utah Geological Survey, the Iron Springs Formation is described as: <em>the formation is variously colored grayish orange, pale yellowish orange, dark yellowish orange, white, pale reddish brown, and greenish gray and is locally stained by iron-manganese oxides, which accounts for the reddish colors<\/em>. When you look at the pictures in this article, do those words describe it? I think they do.<\/p> <p>Learn more about the various formations in Southwest Utah by following these steps:<\/p> <ul> <li>Go to the Utah Geological Survey website at: <a href=\"https:\/\/geology.utah.gov\/map-pub\/maps\/geologic-maps\/\" target=\"_blank\" rel=\"noopener\">https:\/\/geology.utah.gov\/map-pub\/maps\/geologic-maps\/<\/a><\/li> <li>Then, on the map, select the square over the St. George area (the very lower-left corner).<\/li> <li>In the pop-up, select Open PDF. Since the PDF is a large file, it will take a few moments to download.<\/li> <li>The first page is the colorful geologic map. Scroll down to page 2.<\/li> <li>The stratigraphy chart used in the video is on page 2. Scroll down to find the Iron Springs Formation.<\/li> <li>Below is a snippet of the stratigraphy chart showing the formations near the Iron Springs:<\/li> <\/ul> <p><a href=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy.jpg\" alt=\"\" width=\"1204\" height=\"949\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy.jpg 1204w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy-300x236.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy-1024x807.jpg 1024w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutStratigraphy-768x605.jpg 768w\" sizes=\"auto, (max-width: 1204px) 100vw, 1204px\" \/><\/a><\/p> <h3>Iron Springs Formation<\/h3> <p>The Iron Springs Formation is named after a locality that is about ten miles northwest of Cedar City, Utah. However, the formation is exposed mainly around the Pine Valley Mountains. In other parts of Utah, this formation is called the Straight Cliffs Formation. The two formations aren\u2019t exactly the same but were deposited about the same period of time and consist mostly of the same Earthen material.<\/p> <p>In the Grand Staircase-Escalante National Monument, about 90 miles east of the roadcut, sits the massive Kaiparowits Plateau. Most of the plateau is made up of the Straight Cliffs Formation. The Iron Springs Formation near St. George shares many of same characteristics to what\u2019s seen on the Kaiparowits.<\/p> <p>Now about the colorful layers. During the Cretaceous period, this large area was swampy and consisted of a lot of organic material. When that organic material was buried by the formations above it, heat and pressure mineralized the organic material. The pressure came from the weight of the additional earthen material above it. Millions of years later, thanks to erosion, the material was exposed to our atmosphere, which in turn oxidized the various minerals and created an array of colors.<\/p> <p>This same process, where minerals were oxidized and created colorful scenery, has occurred in other places of the Southwest. One formation in particular is called the Chinle Formation. It\u2019s the remains of another swampy time in Earth\u2019s history. It\u2019s two formations below the Navajo Sandstone Formation mentioned earlier. The Chinle is famous for creating what is now the Painted Desert in Arizona and the Paria townsite in Utah, both having very colorful scenery.<\/p>\n<a href=\"https:\/\/www.backroadswest.com\/brw\/geology-tour-st-george\/\" rel=\"noopener\" target=\"_blank\"> <img src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/02\/Ad-800x500-GeologyTour1.gif\" title=\"Ad-800x500-GeologyTour1\" alt=\"Ad-800x500-GeologyTour1\"> <\/a>\n<h2>The Angle<\/h2> <p>How was that curious angle created? It was the fault, of the Hurricane Fault. This major fault is just one mile to the east of the roadcut. As you may know, the Hurricane Fault is the western boundary of the Colorado Plateau and is the fracture where land on the east side uplifted over a mile high creating the plateau.<\/p> <p>The uplift is the reason for the uniquely level and layered geology on the east side of the fault. On the west side of the fault, the geology is jumbled up and crumpled. The land closer to the fault also sank.<\/p> <p>The same geologic formations on the west side of the fault exist on the east side, but at a different elevation because of the uplift. At the roadcut, the elevation of the Iron Springs Formation is about 3,000 feet (900 m). On the east side of the fault in the Colorado Plateau, it is exposed at 6,000 to 7,000 feet (2,000 m). This is where it is called the Straight Cliffs Formation, mentioned earlier. That offset is about 4,000 feet (1,220 m), meaning the formation uplifted and rose quite a distance.<\/p> <p>When the land on the east side of the fault rose, it tilted slightly to the east. The opposite occurred on the west side of the fault. This mainly happened because of the Basin and Range Province, between the Hurricane Fault and the Sierra Nevada Mountains in California, was being stretched apart, causing the land closest to the fault to sink. Watch the video for an animated diagram showing the tilting action.<\/p> <ul> <li><strong>See our article on <a title=\"Southwest Utah: A Triple Junction of Landscapes\" href=\"http:\/\/www.backroadswest.com\/blog\/triple-junction-southwest-utah\/\" target=\"_blank\" rel=\"noopener\">Southwest Utah's Triple Junction<\/a>\u00a0<\/strong>that explains more details about the Hurricane Fault and the Colorado Plateau<\/li> <\/ul> <p>This is most likely the reason why we see the tilt in the roadcut. The small hills and ridges near the roadcut are also tilted the same direction \u2013 sinking to the east and raising towards the west.<\/p> <p>[adrotate group=\"11\"]<\/p> <h2>Missing Formations?<\/h2> <p>In our roadcut, between the colorful layers of the Iron Springs Formation and the next visible layer above containing alluvial deposits, there are a few formations missing. When a layer is missing, it is known as an unconformity. We know the layer is missing because in other areas, the formation exists.<\/p> <p>Think of an unconformity as a hamburger with layers such as buns, hamburger patty, tomatoes, pickles and lettuce. The hamburger is cut in half and the patty is removed. Between the two halves, there is now an unconformity on one side, the side with the patty missing.<\/p> <h3>Great Unconformity<\/h3> <p>The most well-known unconformity is in the Grand Canyon. It\u2019s known as the Great Unconformity. Here, it is easy to see that several large layers of geology were removed by erosion. It\u2019s a mystery as to how big they were or what material they consisted of. The unconformity in the roadcut isn\u2019t as big but there are a few missing formations nonetheless. Plus, we know what layers are missing and thus what they consisted of.<\/p> <p>One well-known formation that is missing is the Claron Formation. The Claron is famous for the hoodoos of Bryce Canyon National Park and other locales in Utah. The Claron is exposed and visible on both sides of the Hurricane Fault. Near the roadcut, it is visible near the base of the Pine Valley Mountains.<\/p> <p>Fifty miles north of the roadcut, in a place called Parowan Gap, a large outcrop of Claron Formation can be seen sitting on top Iron Springs Formation. This is what the area around the roadcut may have looked like:<\/p>\n<img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='360'%20height='200'%20viewBox=%270%200%20360%20200%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#bbcce8 25%,#013b8f 25% 50%,#0c3b81 50% 75%,#00439c 75%),linear-gradient(to right,#528ad5 25%,#534f44 25% 50%,#bd9e89 50% 75%,#948276 75%),linear-gradient(to right,#554434 25%,#d3bda5 25% 50%,#af9481 50% 75%,#271707 75%),linear-gradient(to right,#908474 25%,#a08a73 25% 50%,#614b3d 50% 75%,#3b2f23 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutClaron1-360x200.jpg\" width=\"360\" height=\"200\" title=\"RoadcutClaron1\" alt=\"Claron &amp; Iron Springs Formation\"><noscript><img data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutClaron1-360x200.jpg\" width=\"360\" height=\"200\" title=\"RoadcutClaron1\" alt=\"Claron &amp; Iron Springs Formation\"><\/noscript> Claron Formation on top, Iron Springs Formation (small layers) below it <img src=\"data:image\/svg+xml,%3Csvg%20xmlns=%27http:\/\/www.w3.org\/2000\/svg%27%20width='360'%20height='200'%20viewBox=%270%200%20360%20200%27%3E%3C\/svg%3E\" loading=\"lazy\" data-lazy=\"1\" data-tf-not-load=\"1\" style=\"background:linear-gradient(to right,#02469b 25%,#87564f 25% 50%,#130e12 50% 75%,#a48372 75%),linear-gradient(to right,#755c57 25%,#c29d8a 25% 50%,#5b3f3e 50% 75%,#ba6850 75%),linear-gradient(to right,#664c3d 25%,#baa590 25% 50%,#a1725e 50% 75%,#bd7b61 75%),linear-gradient(to right,#ddbba2 25%,#f7e5cf 25% 50%,#d5bba2 50% 75%,#976d55 75%)\" decoding=\"async\" data-tf-src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutClaron2-360x200.jpg\" width=\"360\" height=\"200\" title=\"RoadcutClaron2\" alt=\"Closeup of Claron &amp; Iron Springs Formation contact\"><noscript><img data-tf-not-load data-no-script src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2024\/03\/RoadcutClaron2-360x200.jpg\" width=\"360\" height=\"200\" title=\"RoadcutClaron2\" alt=\"Closeup of Claron &amp; Iron Springs Formation contact\"><\/noscript> Closeup of contact between Claron & Iron Springs Formations\n<p>Refer to the stratigraphy chart from the Utah Geological Survey referenced earlier to see where the Iron Springs Formation is in relation to the Claron. The Claron is basically two formations above the Iron Springs. So, between the colorful layers we see in the roadcut and the alluvial deposits above it, there used to be two other significant rock layers.<\/p> <h2>Summary<\/h2> <p>Isn\u2019t it amazing to see how all the pieces of a very large jigsaw puzzle come together? It\u2019s why geology is so fascinating to us. Yes, this landscape is beautiful but isn\u2019t it just a little more interesting when you know more about its complex nature? One doesn\u2019t need to be an expert in geology to see the puzzle pieces that put together the scenery of Southwest Utah.<\/p> <p>Now that you know more about this roadcut, we hope that when you take road trips from now on, you\u2019ll pay a little more attention to the roadcuts you drive through and wonder what geologic story they are telling. You might also start to wonder what\u2019s just below the surface of the landscapes you\u2019re passing over and what lays just below the surface.<\/p> <h2>Trip Map<\/h2> <p>To help plan your trip, use our interactive Google Map below. Be sure to switch to Satellite view to see the terrain.<\/p> <p>Most of the maps in our videos were created using Gaia GPS. Click the ad below to purchase a Gaia GPS subscription and we'll earn a few dollars to fund our next trip.<\/p> <p><a href=\"https:\/\/classic.avantlink.com\/click.php?tool_type=ml&amp;merchant_link_id=2efe71d3-5569-4c72-a69e-e9258881dd0a&amp;website_id=cb6aacf1-7563-4b97-8b5d-48e9519fe173\" target=\"_blank\" rel=\"noopener sponsored\"><img loading=\"lazy\" decoding=\"async\" style=\"border: 0px;\" src=\"https:\/\/classic.avantlink.com\/gbi\/bd4517b4-b0f2-4660-8208-2ade3a1fdb4c\/2efe71d3-5569-4c72-a69e-e9258881dd0a\/a24ae5c1-c37a-45ea-b3f8-5480cc46d529\/cb6aacf1-7563-4b97-8b5d-48e9519fe173\/image.png\" alt=\"\" width=\"728\" height=\"90\" \/><\/a><\/p> <p><a href=\"http:\/\/www.backroadswest.com\/blog\/map\/\">Learn more<\/a> about our maps.<\/p>\n<template> Site of roadcut <\/template>\n<h3>Comments<\/h3> <p>Read and leave comments about this post on <a href=\"https:\/\/www.youtube.com\/watch?v=dRg0WAQBzEI\" target=\"_blank\" rel=\"noopener\">YouTube<\/a>.<\/p>\n<h3>Support Us<\/h3><p>Help us fill up our tank with gas for our next trip by donating $5 and we'll bring you back more quality virtual tours of our trips!<\/p><p>Your credit card payment is safe and easy using PayPal. Click the [Donate] button to get started:<\/p><p>[paypal-donation]<\/p>\n<h3 style=\"text-align: left;\">Subscribe<\/h3> <p>[mc4wp_form]<\/p>\n<p style=\"text-align: center;\"><em>See all our comprehensive virtual tour guides at<\/em>:<\/p><p style=\"text-align: justify;\"><a title=\"BackRoadsWest\" href=\"http:\/\/www.backroadswest.com\/brw\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2015\/04\/BRWlogo-300x40.jpg\" alt=\"BRWlogo\" width=\"300\" height=\"40\" srcset=\"http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2015\/04\/BRWlogo-300x40.jpg 300w, http:\/\/www.backroadswest.com\/blog\/wp-content\/uploads\/2015\/04\/BRWlogo.jpg 438w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><\/p>\n<p><br \/> <br \/> <ins style=\"display:inline-block;width:728px;height:90px\" data-ad-client=\"ca-pub-7400034802659664\" data-ad-slot=\"1662640655\"><\/ins><br \/> <\/p>\n<h3>More Trips<\/h3> Would you like to go on more trips in Nevada? <a href=\"http:\/\/www.backroadswest.com\/blog\/category\/nevada\/\"> See More Trips in Nevada <\/a>","_links":{"self":[{"href":"http:\/\/www.backroadswest.com\/blog\/wp-json\/wp\/v2\/posts\/6783","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/www.backroadswest.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/www.backroadswest.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/www.backroadswest.com\/blog\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/www.backroadswest.com\/blog\/wp-json\/wp\/v2\/comments?post=6783"}],"version-history":[{"count":53,"href":"http:\/\/www.backroadswest.com\/blog\/wp-json\/wp\/v2\/posts\/6783\/revisions"}],"predecessor-version":[{"id":7953,"href":"http:\/\/www.backroadswest.com\/blog\/wp-json\/wp\/v2\/posts\/6783\/revisions\/7953"}],"wp:featuredmedia":[{"embeddable":true,"href":"http:\/\/www.backroadswest.com\/blog\/wp-json\/wp\/v2\/media\/6777"}],"wp:attachment":[{"href":"http:\/\/www.backroadswest.com\/blog\/wp-json\/wp\/v2\/media?parent=6783"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.backroadswest.com\/blog\/wp-json\/wp\/v2\/categories?post=6783"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.backroadswest.com\/blog\/wp-json\/wp\/v2\/tags?post=6783"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}