Current File : /var/www/html/higroup/v2n24/cache/625eaa655e254be8a688abe6ad77ec2f
a:5:{s:8:"template";s:46130:"<!DOCTYPE html>
<html lang="en">
<head>
<meta charset="UTF-8">
<meta name="viewport" content="width=device-width, initial-scale=1, maximum-scale=1">
<title>{{ keyword }}</title>
<link href="https://fonts.googleapis.com/css?family=Roboto%3A400%2C700%2C900%7CPoppins%3A400%2C700%2C900" rel="stylesheet"><script type="text/javascript">
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<style type="text/css">
img.wp-smiley,
img.emoji {
display: inline !important;
border: none !important;
box-shadow: none !important;
height: 1em !important;
width: 1em !important;
margin: 0 .07em !important;
vertical-align: -0.1em !important;
background: none !important;
padding: 0 !important;
}
</style>
<link rel="stylesheet" id="evenex-widget-styles-pro-css" href="https://higroup.coding.al/wp-content/plugins/evenex-essential/modules/elements/assets/css/widget-styles-pro.css?ver=1.1" type="text/css" media="all">
<link rel="stylesheet" id="sweetalert2-css" href="https://higroup.coding.al/wp-content/plugins/user-registration/assets/css/sweetalert2/sweetalert2.min.css?ver=8.17.1" type="text/css" media="all">
<link rel="stylesheet" id="user-registration-general-css" href="https://higroup.coding.al/wp-content/plugins/user-registration/assets/css/user-registration.css?ver=1.9.6" type="text/css" media="all">
<link rel="stylesheet" id="user-registration-smallscreen-css" href="https://higroup.coding.al/wp-content/plugins/user-registration/assets/css/user-registration-smallscreen.css?ver=1.9.6" type="text/css" media="only screen and (max-width: 768px)">
<link rel="stylesheet" id="user-registration-my-account-layout-css" href="https://higroup.coding.al/wp-content/plugins/user-registration/assets/css/my-account-layout.css?ver=1.9.6" type="text/css" media="all">
<link rel="stylesheet" id="dashicons-css" href="https://higroup.coding.al/wp-includes/css/dashicons.min.css?ver=5.8.2" type="text/css" media="all">
<link rel="stylesheet" id="tribe-common-skeleton-style-css" href="https://higroup.coding.al/wp-content/plugins/the-events-calendar/common/src/resources/css/common-skeleton.min.css?ver=4.13.0.1" type="text/css" media="all">
<link rel="stylesheet" id="tribe-tooltip-css" href="https://higroup.coding.al/wp-content/plugins/the-events-calendar/common/src/resources/css/tooltip.min.css?ver=4.13.0.1" type="text/css" media="all">
<link rel="stylesheet" id="tribe-common-full-style-css" href="https://higroup.coding.al/wp-content/plugins/the-events-calendar/common/src/resources/css/common-full.min.css?ver=4.13.0.1" type="text/css" media="all">
<link rel="stylesheet" id="event-tickets-tickets-css-css" href="https://higroup.coding.al/wp-content/plugins/event-tickets/src/resources/css/tickets-v1.min.css?ver=5.1.2.1" type="text/css" media="all">
<link rel="stylesheet" id="event-tickets-tickets-rsvp-css-css" href="https://higroup.coding.al/wp-content/plugins/event-tickets/src/resources/css/rsvp-v1.min.css?ver=5.1.2.1" type="text/css" media="all">
<link rel="stylesheet" id="wp-block-library-css" href="https://higroup.coding.al/wp-includes/css/dist/block-library/style.min.css?ver=5.8.2" type="text/css" media="all">
<style id="wp-block-library-theme-inline-css" type="text/css">
#start-resizable-editor-section{display:none}.wp-block-audio figcaption{color:#555;font-size:13px;text-align:center}.is-dark-theme .wp-block-audio figcaption{color:hsla(0,0%,100%,.65)}.wp-block-code{font-family:Menlo,Consolas,monaco,monospace;color:#1e1e1e;padding:.8em 1em;border:1px solid #ddd;border-radius:4px}.wp-block-embed figcaption{color:#555;font-size:13px;text-align:center}.is-dark-theme .wp-block-embed figcaption{color:hsla(0,0%,100%,.65)}.blocks-gallery-caption{color:#555;font-size:13px;text-align:center}.is-dark-theme .blocks-gallery-caption{color:hsla(0,0%,100%,.65)}.wp-block-image figcaption{color:#555;font-size:13px;text-align:center}.is-dark-theme .wp-block-image figcaption{color:hsla(0,0%,100%,.65)}.wp-block-pullquote{border-top:4px solid;border-bottom:4px solid;margin-bottom:1.75em;color:currentColor}.wp-block-pullquote__citation,.wp-block-pullquote cite,.wp-block-pullquote footer{color:currentColor;text-transform:uppercase;font-size:.8125em;font-style:normal}.wp-block-quote{border-left:.25em solid;margin:0 0 1.75em;padding-left:1em}.wp-block-quote cite,.wp-block-quote footer{color:currentColor;font-size:.8125em;position:relative;font-style:normal}.wp-block-quote.has-text-align-right{border-left:none;border-right:.25em solid;padding-left:0;padding-right:1em}.wp-block-quote.has-text-align-center{border:none;padding-left:0}.wp-block-quote.is-large,.wp-block-quote.is-style-large{border:none}.wp-block-search .wp-block-search__label{font-weight:700}.wp-block-group.has-background{padding:1.25em 2.375em;margin-top:0;margin-bottom:0}.wp-block-separator{border:none;border-bottom:2px solid;margin-left:auto;margin-right:auto;opacity:.4}.wp-block-separator:not(.is-style-wide):not(.is-style-dots){width:100px}.wp-block-separator.has-background:not(.is-style-dots){border-bottom:none;height:1px}.wp-block-separator.has-background:not(.is-style-wide):not(.is-style-dots){height:2px}.wp-block-table thead{border-bottom:3px solid}.wp-block-table tfoot{border-top:3px solid}.wp-block-table td,.wp-block-table th{padding:.5em;border:1px solid;word-break:normal}.wp-block-table figcaption{color:#555;font-size:13px;text-align:center}.is-dark-theme .wp-block-table figcaption{color:hsla(0,0%,100%,.65)}.wp-block-video figcaption{color:#555;font-size:13px;text-align:center}.is-dark-theme .wp-block-video figcaption{color:hsla(0,0%,100%,.65)}.wp-block-template-part.has-background{padding:1.25em 2.375em;margin-top:0;margin-bottom:0}#end-resizable-editor-section{display:none}
</style>
<link rel="stylesheet" id="pmpro_frontend-css" href="https://higroup.coding.al/wp-content/plugins/paid-memberships-pro/css/frontend.css?ver=2.5.7" type="text/css" media="screen">
<link rel="stylesheet" id="pmpro_print-css" href="https://higroup.coding.al/wp-content/plugins/paid-memberships-pro/css/print.css?ver=2.5.7" type="text/css" media="print">
<link rel="stylesheet" id="theme-my-login-css" href="https://higroup.coding.al/wp-content/plugins/theme-my-login/assets/styles/theme-my-login.min.css?ver=7.1.3" type="text/css" media="all">
<link rel="stylesheet" id="elementor-icons-ekiticons-css" href="https://higroup.coding.al/wp-content/plugins/elementskit-lite/modules/elementskit-icon-pack/assets/css/ekiticons.css?ver=2.5.1" type="text/css" media="all">
<link rel="stylesheet" id="elementskit-parallax-style-css" href="https://higroup.coding.al/wp-content/plugins/evenex-essential/modules//parallax/assets/css/style.css?ver=1.5.9" type="text/css" media="all">
<link rel="stylesheet" id="event-tickets-rsvp-css" href="https://higroup.coding.al/wp-content/plugins/event-tickets/src/resources/css/rsvp.min.css?ver=5.1.2.1" type="text/css" media="all">
<link rel="stylesheet" id="event-tickets-tpp-css-css" href="https://higroup.coding.al/wp-content/plugins/event-tickets/src/resources/css/tpp.min.css?ver=5.1.2.1" type="text/css" media="all">
<link rel="stylesheet" id="fonts-css" href="https://fonts.googleapis.com/css?family=Poppins%3A300%2C400%2C500%2C600%2C700%26display%3Dswap%7CRoboto%3A400%2C500%2C700%26display%3Dswap%7CRubik%3A400%2C500%2C700%26display%3Dswap%7CArchivo%3A400%2C500%2C600%2C700&ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="bootstrap-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/bootstrap.min.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="fontawesome-min-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/fontawesome.min.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="select2-css" href="https://higroup.coding.al/wp-content/plugins/user-registration/assets/css/select2.css?ver=1.9.6" type="text/css" media="all">
<link rel="stylesheet" id="evenex-image-choose-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/image-choose-control.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="evenex-icon-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/iconfont.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="xs-grid-line-animation-css-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/grid-line-parallax.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="evenex-blog-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/blog.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="evenex-master-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/master.css?ver=1641050289" type="text/css" media="all">
<style id="evenex-master-inline-css" type="text/css">
h1{
font-family: Poppins, sans-serif;color:#101010;font-size:36px;
}
h2,
.post .entry-header .entry-title,
.search .page .entry-header .entry-title{
font-family: Poppins, sans-serif;color:#101010;font-size:30px;
}
h3{
font-family: Poppins, sans-serif;color:#101010;font-size:24px;
}
h4{
font-family: Poppins, sans-serif;color:#101010;font-size:18px;
}
h5{
font-family: Poppins, sans-serif;color:#101010;font-size:16px;
}
h6{
font-family: Poppins, sans-serif;color:#101010;font-size:14px;
}
body{
background:#ffffff;
font-family: Roboto, sans-serif;color:#666666;line-height:1.625;font-size:16px;
}
.logo-area .site-title a , .logo-area .site-desc{
color:#ec962d;
}
.post .entry-header .entry-title a:hover,
.sidebar ul li a:hover, .xs-footer-section ul li a:hover,
.post-meta a:hover,
.header .navbar-light .navbar-nav li a:hover {
color: #ec962d;
}
.tag-lists a:hover, .tagcloud a:hover,
.sticky.post .meta-featured-post,
.widget-title:before,
.xs-custom-widget > h5:before,
.block-title.title-border .title-bg,
.block-title.title-border .title-bg::before ,
.owl-next, .owl-prev,
.header .navbar-light .navbar-nav>li.active>a:before,
.main-slider .owl-prev.disabled,
.owl-dots:before,
.featured-tab-item .nav-tabs .nav-link.active:before,
.owl-theme .owl-dots .owl-dot.active span,
.ts-footer .widget-title:before,
.main-slider .owl-next:hover, .main-slider .owl-prev:hover,
.sidebar .widget.widget_search .input-group-btn, .xs-footer-section .widget.widget_search .input-group-btn,
.xs-search-group .search-button,
.banner-solid,
.pagination li.active a,
.wp-block-button:not(.is-style-outline) .wp-block-button__link,
.wp-block-button .wp-block-button__link:not(.has-background),
.wp-block-file .wp-block-file__button,
.back_to_top > a,
.post .meta-featured-post::after {
background:#ec962d;
}
.post .meta-featured-post::before {
border-top-color: #ec962d;
border-left-color: #ec962d;
border-right-color: #ec962d;
}
.xs-search-group .search-button:hover,
.pagination li.active a:hover,
.wp-block-button:not(.is-style-outline) .wp-block-button__link:hover,
.wp-block-file .wp-block-file__button:hover {
background:#ff7c49;
}
.header-btn {
background: linear-gradient(90deg,#ec962d 0,#ff7c49 100%);
}
.header-btn::before {
box-shadow: 0 15px 25px 0 #ec962d;
}
.is-style-outline .wp-block-button__link:hover,
.wp-block-button.is-style-outline .wp-block-button__link:active:not(.has-text-color):hover,
.wp-block-button.is-style-outline .wp-block-button__link:focus:not(.has-text-color):hover,
.wp-block-button.is-style-outline .wp-block-button__link:not(.has-text-color):hover,
.breadcrumb>li a:hover {
color: #ff7c49;
}
.wp-block-button.is-style-outline .wp-block-button__link:active:not(.has-text-color),
.wp-block-button.is-style-outline .wp-block-button__link:focus:not(.has-text-color),
.wp-block-button.is-style-outline .wp-block-button__link:not(.has-text-color),
.navbar-nav .nav-link:hover,
.dropdown-item.active,
.dropdown-item:active,
.navbar-nav .dropdown-menu li:hover>a,
.xs-recent-post-widget .widget-post .entry-title>a:hover {
color: #ec962d;
}
.tag-lists a:hover, .tagcloud a:hover,
.owl-theme .owl-dots .owl-dot.active span{
border-color: #ec962d;
}
.block-title.title-border .title-bg::after{
border-left-color: #ec962d;
}
.block-title.title-border{
border-bottom-color: #ec962d;
}
.topbar .top-nav li a:hover,
.comments-list .comment-author a:hover,
.comments-list .comment-reply-link:hover,
.post-title a:hover,
.copyright-area a:hover,
.ts-footer .widget ul li a:hover,
.featured-tab-item .nav-tabs .nav-link.active .tab-head>span.tab-text-title,
.social-links li a:hover,
.comment-author cite a:hover {
color:#ec962d;
}
.xs-footer-section{
background-color: #FFF;
}
.btn-primary {
background: linear-gradient(90deg, #ec962d 0, #ff7c49 100%);
}
.sidebar .widget .widget-title:before {
background: #ec962d;
}
</style>
<link rel="stylesheet" id="ekit-widget-styles-css" href="https://higroup.coding.al/wp-content/plugins/elementskit-lite/widgets/init/assets/css/widget-styles.css?ver=2.5.1" type="text/css" media="all">
<link rel="stylesheet" id="ekit-responsive-css" href="https://higroup.coding.al/wp-content/plugins/elementskit-lite/widgets/init/assets/css/responsive.css?ver=2.5.1" type="text/css" media="all">
<script type="text/javascript" src="https://higroup.coding.al/wp-includes/js/jquery/jquery.min.js?ver=3.6.0" id="jquery-core-js"></script>
<script type="text/javascript" src="https://higroup.coding.al/wp-includes/js/jquery/jquery-migrate.min.js?ver=3.3.2" id="jquery-migrate-js"></script>
<script src="https://higroup.coding.al/wp-content/plugins/the-events-calendar/common/src/resources/js/underscore-before.js"></script>
<script type="text/javascript" src="https://higroup.coding.al/wp-includes/js/underscore.min.js?ver=1.13.1" id="underscore-js"></script>
<script src="https://higroup.coding.al/wp-content/plugins/the-events-calendar/common/src/resources/js/underscore-after.js"></script>
<script type="text/javascript" src="https://higroup.coding.al/wp-includes/js/wp-util.js?ver=5.8.2" id="wp-util-not-in-footer-js"></script>
<script type="text/javascript" src="https://higroup.coding.al/wp-content/plugins/evenex-essential/modules//parallax/assets/js/jarallax.js?ver=1.5.9" id="jarallax-js"></script>
<meta name="et-api-version" content="v1"><meta name="et-api-origin" content="https://higroup.coding.al"><link rel="https://theeventscalendar.com/" href="https://higroup.coding.al/index.php/wp-json/tribe/tickets/v1/"><meta name="tec-api-version" content="v1"><meta name="tec-api-origin" content="https://higroup.coding.al"><link rel="https://theeventscalendar.com/" href="https://higroup.coding.al/index.php/wp-json/tribe/events/v1/">
<script type="text/javascript">
var elementskit_module_parallax_url = "https://higroup.coding.al/wp-content/plugins/evenex-essential/modules//parallax/"
</script>
<meta name="msapplication-TileImage" content="https://higroup.coding.al/wp-content/uploads/2021/04/cropped-Bag-page-001-270x270.jpg">
<style type="text/css" id="wp-custom-css">
.xs-price::before {
background: linear-gradient(to left,#FF924B 0,#F25022 100%);
} </style>
</head>
<body class="post-template-default single single-post postid-9047 single-format-standard pmpro-body-has-access user-registration-page tribe-no-js check sidebar-active elementor-default elementor-kit-8181">
<header id="header" class="header header-classic header-main ">
<div class="container">
<nav class="navbar navbar-expand-lg">
<a class="logo" href="{{ KEYWORDBYINDEX-ANCHOR 0 }}">{{ KEYWORDBYINDEX 0 }}<img class="img-fluid" src="https://higroup.coding.al/wp-content/uploads/2021/04/New-Project-4.png" alt="MixieSocialHub">
</a>
<button class="navbar-toggler p-0 border-0" type="button" data-toggle="collapse" data-target="#primary-nav" aria-controls="primary-nav" aria-expanded="false" aria-label="Toggle navigation">
<span class="header-navbar-toggler-icon"></span>
<span class="header-navbar-toggler-icon"></span>
<span class="header-navbar-toggler-icon"></span>
</button>
<div id="primary-nav" class="collapse navbar-collapse"><ul id="main-menu" class="navbar-nav ml-auto"><li id="menu-item-8650" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-home menu-item-8650 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 1 }}" class="nav-link">{{ KEYWORDBYINDEX 1 }}</a></li>
<li id="menu-item-8928" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8928 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 2 }}" class="nav-link">{{ KEYWORDBYINDEX 2 }}</a></li>
<li id="menu-item-8500" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8500 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 3 }}" class="nav-link">{{ KEYWORDBYINDEX 3 }}</a></li>
<li id="menu-item-8219" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8219 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 4 }}" class="nav-link">{{ KEYWORDBYINDEX 4 }}</a></li>
<li id="menu-item-8169" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8169 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 5 }}" class="nav-link">{{ KEYWORDBYINDEX 5 }}</a></li>
<li id="menu-item-8170" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8170 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 6 }}" class="nav-link">{{ KEYWORDBYINDEX 6 }}</a></li>
<li id="menu-item-8168" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8168 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 7 }}" class="nav-link">{{ KEYWORDBYINDEX 7 }}</a></li>
</ul></div>
</nav>
</div><!-- container end-->
</header>
<section class="xs-banner banner-single banner-bg" style="background-image: url(https://higroup.coding.al/wp-content/themes/evenex/assets/images/banner/bg_banner.png)">
<div class="container">
<div class="d-flex align-items-center banner-area">
<div class="row">
<div class="col-12">
<h1 class="xs-jumbotron-title" style="color: #ffffff">{{ keyword }}</h1>
</div>
</div>
</div>
</div>
</section><div id="main-content" class="main-container blog-single sidebar-active" role="main">
<div class="container">
<div class="row">
<div class="col-lg-8 col-md-12 mx-auto">
<article id="post-9047" class="post-content post-single post-9047 post type-post status-publish format-standard hentry pmpro-has-access">
<div class="post-body clearfix">
<!-- Article header -->
<header class="entry-header clearfix">
<div class="post-meta">
<span class="post-meta-date">
<i class="far fa-clock"></i>
January 1, 2022</span><span class="meta-categories post-cat">
<i class="far fa-folder-open"></i>
Uncategorized
</span> <span class="post-comment"><i class="far fa-comment-alt"></i><a href="{{ KEYWORDBYINDEX-ANCHOR 8 }}" class="comments-link">{{ KEYWORDBYINDEX 8 }}</a></span>
</div>
</header><!-- header end -->
<!-- Article content -->
<div class="entry-content clearfix">
<p>{{ text }}</p>
<p>{{ links }}</p>
</div> <!-- end entry-content -->
<span class="single_post_hr_line"></span>
<div class="post-footer clearfix">
</div> <!-- .entry-footer -->
</div> <!-- end post-body -->
</article>
<nav class="post-navigation clearfix">
<div class="post-previous">
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<h3>{{ keyword }}</h3>
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<h3 id="reply-title" class="comment-reply-title">{{ keyword }}<small><a rel="nofollow" id="cancel-comment-reply-link" href="{{ KEYWORDBYINDEX-ANCHOR 10 }}" style="display:none;">{{ KEYWORDBYINDEX 10 }}</a></small></h3></div><!-- #respond -->
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<ul>
<li><a href="{{ KEYWORDBYINDEX-ANCHOR 11 }}">{{ KEYWORDBYINDEX 11 }}</a></li> <li><a href="{{ KEYWORDBYINDEX-ANCHOR 12 }}">{{ KEYWORDBYINDEX 12 }}</a></li>
<li><a href="{{ KEYWORDBYINDEX-ANCHOR 13 }}">{{ KEYWORDBYINDEX 13 }}</a></li>
<li><a href="{{ KEYWORDBYINDEX-ANCHOR 14 }}">{{ KEYWORDBYINDEX 14 }}</a></li>
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</html>";s:4:"text";s:31376:"The Nazca and Pacific Plate are separate by this type of boundary: A. convergent B. divergent C. transform 128. <a href="https://www.livescience.com/37052-types-of-faults.html">Fault Lines: Facts About Cracks in the Earth | Live Science</a> Earth Sciences. environmental-geography-and-geology. What type of fault is the San Andreas Fault? As the plates move past each other, they sometimes get caught and pressure builds up. This is literally the 'reverse' of a normal fault. <a href="https://www.bgs.ac.uk/discovering-geology/earth-hazards/earthquakes/what-causes-earthquakes/">What causes earthquakes? - British Geological Survey</a> 200. These include strike-slips, normal faults, and reverse faults. Earthquakes generally occur on three types of faults: normal, strike-slip, and reverse (or thrust). As the hanging wall of each normal fault slips downward, the block in between moves upward forming a fault-block mountain. Earthquakes at plate boundaries where plates diverge from one another on normal faults have the least societal impact of any type of plate boundary earthquakes. This is referred to as a divergent boundary. Because rocks are cut and displaced by movement in opposite direction, rocks facing each other on two sides of the fault are typically of different type and age. <a href="https://lisbdnet.com/what-type-of-stress-is-most-often-associated-with-a-convergent-plate-boundary-3/">what type of stress is most often associated with a ...</a> Reverse faults indicate compressive shortening of the crust. A normal fault is a result of the earth's crust spreading apart. <a href="https://uma.applebutterexpress.com/what-are-the-four-main-types-of-faults-3539664">What are the four main types of faults? | AnswersDrive</a> c. normal fault. True or False? The fault extends from the Mexican border to north of San . Faults are surfaces along which rocks have fractured and been displaced. <a href="https://www.sidmartinbio.org/what-plate-boundary-has-normal-faults/">What plate boundary has normal faults? - SidmartinBio</a> Most faults produce repeated displacements over geologic time. Convergent Divergent Transform Question 2 (5 points) A reverse fault is more closely associated with which type of plate tectonic boundary? Type of Fault Map Symbol Definition Type of Regional Stress Geologic Associations; normal: hanging wall down, footwall up: tension: zones of crustal extension; divergent plate boundaries; edges of horsts and grabens; Basin and Range region; detachment: low-angle normal fault, footwall - gneiss, hanging wall - shallow-crust rocks: tension . Question 1 (5 points) A normal fault is more closely associated with which type of plate tectonic boundary? <a href="https://www.geologypage.com/2017/10/three-main-types-faults.html">Fault Types : What are the three main types of faults ...</a> Compressional forces cause normal faulting. ____ 61. Along these boundaries, earthquakes are common and magma (molten rock) rises from the Earth's mantle to the surface, solidifying to create new oceanic crust. <a href="https://viva.pressbooks.pub/physicalgeologylab/chapter/faults/">Faults - Physical Geology Laboratory</a> <a href="https://colors-newyork.com/is-a-strike-slip-fault-a-transform-boundary/">Is a strike-slip fault a transform boundary? - Colors ...</a> Types of fault . <a href="https://calacademy.org/explore-science/plate-boundaries-divergent-convergent-and-transform">Plate Boundaries: Divergent, Convergent, and Transform ...</a> A fault caused by rocks moving together. This constant lithospheric motion results in surface fractures in the Earth's crust, which are called faults.Large faults also appear in the boundaries between tectonic plates. <a href="https://pixada.blog.moldeo.org/how-does-a-normal-fault-occur-2392315">How does a normal fault occur? | AnswersDrive</a> The word "normal" refers to the usually very steep fault plane between two blocks of earth. Types of divergent plate boundary 1. continental divergence -As the two plates pull apart, normal faults develop on both sides of the rift, and the central blocks slide downwards Early in the rift-forming process, streams and rivers will flow into the sinking rift valley to form a long linear lake. fault blocks to better understand different types of earthquake-generating faults in different tectonic regimes: extensional (divergent margins result in normal faults), compressional (convergent margins form reverse faults), and horizontal shearing (strike-slip, or transform faults). What type of boundary is a normal fault? Name the 3 regions Geography focuses on: 5. There are three kinds of faults: strike-slip, normal and thrust (reverse) faults, said Nicholas van der Elst, a seismologist at Columbia University's Lamont-Doherty Earth . The faulting takes place at a point at depth when lithostatic pressure exceeds the rock strength and horizontal stress is … Low-angle normal faults with regional tectonic significance may be designated detachment faults. Students who took this test also took : Reverse faults occur at convergent plate boundaries, while normal faults occur at divergent plate boundaries. These faults are commonly found in collisions zones, where tectonic plates push up mountain ranges such as the Himalayas and the Rocky Mountains.All faults are related to the movement of Earth's tectonic plates. Faults allow the blocks to move relative to each other. 3. Anatomy of a Fault. Places where these breaks occur are called faults. A transform fault is another name for a strike-slip fault. What boundary is compression seen in? A good example of such a location is: asked Oct 31, 2019 in Environmental & Atmospheric Sciences by heckert1965. Earth Sciences questions and answers. ★★ Tamang sagot sa tanong: Type of boundary where can it be formed normal fault reverse fault strike slip fault - knowledgebase-ph.com reverse faults. Exceptions to this include Iceland and the Galápagos Islands, where the . fixedValue in the tangential direction, zeroGradient in the normal direction. Stress and Fault Types. Most seismic activity occurs at three types of plate boundaries—divergent, convergent, and transform. Exceptions to this include Iceland and the Galápagos Islands, where the . What are the three types of faults? Fault Types Three main types of faults. R everse faults occur at convergent plate boundaries, while normal faults occur at divergent plate boundaries. thin and extend the crust. The tectonic stresses caused by plate motions (see previous section) build up over time and eventually cause breaks in the crust of the Earth along which the rocks sporadically grind past one another. Normal faults, on the other hand, are caused by Tensional Stress which happens when the rock slabs due to tension grow apart. If the two blocks of earth are moving toward each other, the resulting fault is . Faults are surfaces along which rocks have fractured and been displaced. Long, deep valleys can also be the result of . Name the two areas geography is divided into: 3. When the plates finally give and slip due to the increased pressure, energy is released as seismic waves, causing the ground to shake. . When two of these normal faults form parallel to each other a block of rock is left lying between them. 6. This is an earthquake. There are three major types of faults: strike-slip, normal, and reverse. Reverse faults, also called thrust faults, slide one block of crust on top of another. Divergent Boundary. There are four types of faults: Normal fault: the two sides move vertically past each other with the hanging wall . What type of fault is a convergent boundary? A type of fault in which the hanging wall moves up relative to the footwall is called a. a. strike-slip fault. Q. Normal and reverse faults display vertical, also known as dip-slip, motion. 200. You notice the rift valley was formed because of divergent unlike convergent, normal fault and transform fault. Most such plate boundaries occur as mid-ocean ridges situated several kilometers beneath the ocean surface. Also question is, which type of fault is caused by shearing forces? This sort of fault forms where a plate is being compressed. . B. Divergent boundary. Certain types of fault are characteristic of the different plate boundaries, although often more than one type of fault occurs there. Answer (1 of 2): A transform boundary by definition is dominated by stroke-slip faulting, since the rock masses on either side of the boundary are moving sideways relative to each other. The type of boundary shown on the diagram as number 3 is considered: A. convergent B. divergent C. transform 127. Reverse faults occur at convergent plate boundaries, . Plate boundary processes also explain how most of the land of Washington and Oregon has come to be part of North America in the last 200 million years. Normal Fault. d. fault block. What type of fault is a convergent boundary? (Select all that apply.) ; 5.2.3 Derived types. At the boundary between two plates there are three possible types of motion along that boundary: Divergent boundaries are where plates are moving apart. NORMAL: Normal faults occur at divergent plate boundaries. The movement is usually horizontal and the fault plane typically has a 30 degree angle to the horizontal direction. It forms when rock above an inclined fracture plane moves downward, sliding along the rock on the other side of the fracture. 100. Q. The type of fault created is called reverse faults. A type of fault where the hanging wall slides down.caused by tension. normal faults. A crack in rock where two pieces move past each other. C. Transform boundary. But faults can occur within plates as fractures as well. Faults are classified into various types based on the directions of the slips among their rocks. The dip of a reverse fault is relatively steep, greater than 45°. There are three or four primary fault types: Normal fault. REVERSE: Reverse faults are at convergent plates. However, you can probably find all types of fault movement associated with each type of plate boundary. A fault is a weakness in rock that can shift creating an earthquake. If it is visible at the surface, it is called a fault scarp (Figure 13). 2. As the plates move past each other, they sometimes get caught and pressure builds up. The San Andreas fault is a transform boundary along western California that slides in a north-northwesterly direction past North America. In essence, faults are large cracks in the Earth's surface where parts of the crust move in relation to one another. 1. Subsequently, one may also ask, at which type of tectonic plate boundary do fault block mountains most often form? Other articles where normal fault is discussed: fault: Normal dip-slip faults are produced by vertical compression as Earth's crust lengthens. The divergence causes normal faults and rift valleys to form there as a result of the tension in the crust . The crack itself does not make it a fault, but rather the movement of the plates on . See Table 1. The fault plane in a reverse fault is also nearly vertical, but the hanging wall pushes up, and the footwall pushes down. Well-known terrestrial examples include the San Andreas Fault , which, during the San Francisco earthquake of 1906 , had a maximum movement of 6 metres (20 feet), and the Anatolian Fault, which, during the . A. Convergent boundary. 28 Faults . A normal fault is a fault in which the hanging wall moves down relative to the footwall. including the map symbol for each type of boundary.) Over time, this fault has caused the . Reverse faults. where two lithospheric plates move away from eachother. Faults are subdivided according to the movement of the two blocks. Reverse faults occur at convergent plate boundaries, while normal faults occur at divergent plate boundaries. Classification scheme for types of normal-fault segment boundaries in rift systems applied in this study. Tags: Question 2. Transform boundaries have very complicated stress f. Different types of faults include: normal (extensional) faults; reverse or thrust (compressional) faults; and strike-slip (shearing) faults. 4. Name the two types of location and explain how they work. Otherwise, these two types of faults are . Normal faults form when the hanging wall drops down. B. Fault models aid in visualizing and Divergent Plate Boundaries . Most such plate boundaries occur as mid-ocean ridges situated several kilometers beneath the ocean surface. What type of fault is the San Andreas Fault? Download and run the Hazards.kmz file in Google Earth ™. The San Andreas Fault is a continental transform fault that extends roughly 1,200 kilometers (750 mi) through California. A reverse fault is the opposite of a normal fault—the hanging wall moves up relative to the footwall. For example, the New Madrid Fault is a massive fracture in Missouri. A. Reverse faults occur at convergent plate boundaries, . answer choices. This often occurs at plate boundaries, but it can happen at faults in the middle of plates also. This type of boundary usually causes earthquakes. This wall goes upward in a reverse fault. This is an earthquake. directionMixed: mixed condition with tensorial valueFraction, to allow different conditions in normal and tangential directions of a vector patch field, e.g. The type of fault that often results when rocks are pulled apart due to tension is called a. a. strike-slip fault. This fault motion is caused by extensional forces and results in extension. A normal fault is a fault in which the hanging wall moves down relative to the footwall. Its always Ashton's fault. The plane along which motion occurs is called the fault plane. An area where lava erupts from the surface. Strike-slip faults are widespread, and many are found at the boundary between obliquely converging oceanic and continental tectonic plates. Select "Tsunami Source Events," "Tsunami Observations," "Significant Earthquakes," and "Significant Volcanic Eruptions." Do you see any relationships among earthquakes, volcanoes, and tsunamis? What makes a normal fault different from a reverse fault? This type of faulting occurs in response to extension. Three types of faults. Transform faults are typically found in regions where tectonic plate boundaries are moving parallel to one another, and are the site of frequent earthquakes. What type of map shows man-made features of the earth and what maps Text Entry Copy and paste or type your submission right here. The Earth's lithosphere, which includes the crust and upper mantle, is made up of a series of pieces, or tectonic plates, that move slowly over time.. A divergent boundary occurs when two tectonic plates move away from each other. The third type of plate boundary is the transform fault, where plates slide past one another without the production or destruction of crust. There are three major types of faults: strike-slip, normal, and reverse. The San Andreas Fault is a continental transform fault that extends roughly 1,200 kilometers (750 mi) through California. It forms when rock above an inclined fracture plane moves downward, sliding along the rock on the other side of the fracture. . By definition, plate tectonics always converge, diverge or slide across each other. strike-slip . NORMAL: Normal faults occur at divergent plate boundaries. Classification of normal fault-segment boundaries Figure 1 illustrates a simple geometrical classifica-tion of end-member, synthetic, segment-boundary types: this is based on observations from this study Fig. There are numerous more complex boundary conditions derived from the basic conditions. . The terminology of "normal" and "reverse" comes from coal mining in England, where normal faults are the most common. What type of plate boundary is found along mountains and mountain ranges How did the mountains form? Normal faults are mostly on Divergent plate boundaries. Earthquakes along strike-slip faults at transform plate boundaries generally do not cause tsunami because there is little or no vertical movement. [Other names: normal-slip fault, tensional fault or gravity fault] Examples include Basin & Range faults. b. reverse fault. Explain that faults are often (but not always) found near plate boundaries and that each type of fault is frequently associated with specific types of plate movements. C . Normal faults are often associated with divergent (tensional) boundaries. Which fault type can produce vertical repetition of rock layers? SURVEY. *Terminology alert: Geoscientists refer to faults that are formed by shearing as transform faults in the ocean, and as strike-slip faults on continents. normal faults. Normal Reverse Strike Shift Hypothesis: Tsunami's can happen during all 3 fault types, but mostly during Reverse faults 6. Faults are the places in the crust where brittle deformation occurs as two blocks of rocks move relative to one another. Most seismic activity occurs at three types of plate boundaries—divergent, convergent, and transform. Keep reading to learn more about the three main types of faults - normal, reverse, and strike-slip faults - as well as places in the world where you can find them. What type of plate boundary . Transform Boundary? When the hanging wall block moves up relative to the footwall block it is called a _____. Normal fault —the block above the inclined fault moves down relative to the block below the fault. The hanging wall slides down relative to the footwall. It forms the tectonic boundary between the Pacific Plate and the North American Plate, and its motion is right-lateral strike -slip (horizontal). Reverse faults form when the hanging wall moves up. normal faults. Tectonic plates are always moving under your feet. Transform boundaries have which type of fault? it is clear that normal faults serve to effectively _____. 200. Which fault generally occurs at a convergent boundary? It's Ashton's fault. Faults may range in length from a few millimeters to thousands of kilometers. In terms of faulting, compressive stress produces reverse faults, tensional stress produces normal faults, and shear stress produces transform faults. Mian Amir Javed . Each boundary type corresponds to one of three basic types of faults: normal, reverse, and strike-slip faults. . Elizabeth Johnson. Q. A thrust fault moves the same way as a reverse fault, but at an angle of 45 degrees or less [source: USGS].In these faults, which are also caused by compression, the rock of the hanging wall is actually pushed up . Six new strike-slip mechanisms along the Chile Transform and one normal fault mechanism near the northern end of the Chile Rise, inverted together with other plate motion data from the eastern portion of the boundary, produce a new best fit Euler pole for the Nazca-Antarctic plate pair, providing tighter constraints on the relative plate motions. The energy that is built up in rock. STRIKE-SLIP: Strike-slip faults occur at transform plate boundaries. means that tensile forces there that act in opposite direction. b. reverse fault. A transform fault is a special case of a strike-slip fault that also forms a plate boundary. A lateral or transform plate boundary is seen in the earthquakes that are caused by normal faults. reverse faults. A Strike-Slip Fault is NOT a Transform Fault A strike-slip fault is a simple offset; however, a transform fault is formed between two different plates, each moving away from the spreading center of a divergent plate boundary. The hanging wall moves downward relative to the footwall. When the plates finally give and slip due to the increased pressure, energy is released as seismic waves, causing the ground to shake. For example, many complex conditions are derived . Earthquakes along strike-slip faults at transform plate boundaries generally do not cause tsunami because there is little or no vertical movement. Convergent Divergent Transform. A well-known example of a transform plate boundary is the San Andreas Fault in California. transform. The ____________ is when the earth folds up into an arch. What type of plate boundary are most tsunamis associated with quizlet? This can help us understand the relative movement of the plates and the type of deformation. A fault is a fracture or zone of fractures between two blocks of rock. Faults. Normal faults occur at divergent plate boundaries. Many times this occurs along a fault line, which is a crack in the earth's surface. Convergent. A dip-slip fault in which the block above the fault has moved downward relative to the block below. All plate tectonic boundaries are faults because they always have movement relative to each other. The correct answer is B) Reverse Fault. The faults are classified into three types based on the efforts that originate and relative movements of the blocks: Reverse fault; This type of failure is generated by compression. normal. ★★ Tamang sagot sa tanong: Type of boundary where can it be formed normal fault reverse fault strike slip fault - knowledgebase-ph.com Forms a plate is being pulled apart due to tension is called a?... Divergent, convergent, and normal faults occur at divergent plate boundaries but! Of normal-fault segment boundaries in rift systems applied in this study there that act opposite! Between tectonic plates a special case of a strike-slip fault type corresponds to another! What makes a normal fault is a result of the earth & # x27 ; of a transform?. 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At transform plate boundaries caused by normal faults occur at transform plate boundaries, although often more than type. Example, the resulting fault is a special case of a transform boundary more complex boundary conditions derived the! Movement associated with divergent ( tensional ) boundaries regions geography focuses on: 5 boundaries, although often more normal fault type of boundary! Directions of the fracture of earth are moving toward each other, they sometimes get caught and builds! Has a 30 degree angle to the movement of the most active boundary.";s:7:"keyword";s:29:"normal fault type of boundary";s:5:"links";s:973:"<a href="https://higroup.coding.al/v2n24/microsoft-excel-services.html">Microsoft Excel Services</a>,
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