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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&amp;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;
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      .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,
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      .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,
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      .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,
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      .banner-solid,
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      .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;
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      .post .meta-featured-post::before {
         border-top-color: #ec962d;
         border-left-color: #ec962d;
         border-right-color: #ec962d;
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      .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;
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      .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;
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      .tag-lists a:hover, .tagcloud a:hover,
      .owl-theme .owl-dots .owl-dot.active span{
         border-color: #ec962d;
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      .block-title.title-border .title-bg::after{
         border-left-color: #ec962d;
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      .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">
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</html>";s:4:"text";s:32632:"Another example of a transform boundary on land is the Alpine Fault of New Zealand. <a href="https://www.academickids.com/encyclopedia/index.php/Transform_boundary">Transform boundary</a> Linear valleys, small ponds, stream beds split in half, deep trenches , and scarps and ridges often mark the location of a transform boundary. California's San Andreas fault is a transform boundary. <a href="https://www.coursehero.com/file/124278072/EXAMPLES-OF-TRANSFORM-ZONESpdf/">TRANSFORM</a> California's San Andreas fault is a transform boundary. The Pacific Plate and Indo-Australian Plate boundary  forms the Macquarie Fault Zone  in the Puysegur Trench  off the southwestern corner of the South Island and comes onshore as the Alpine Fault just north of Milford Sound. A transform fault (Wilson, 1965) is a strike-slip fault forming a plate boundary, thus cutting the entire lithosphere that keeps a permanent record of its deformations.It connects two other plate boundaries or plate boundary zones, even other transform faults (this last only at triple junctions), also called “conservative boundaries,” along which lithosphere is neither created nor destroyed. Many transform boundaries are found on the sea floor, where they connect segments of diverging mid-ocean ridges. Some examples of continental transform boundaries are the famous San Andreas fault, the Alpine fault in New Zealand, the Queen Charlotte Island fault near western Canada, the North Anatolian fault in Turkey, and the Dead Sea rift in the Middle East. 66) The San Andreas Fault is an example of _____ plate boundary. <a href="https://www.bartleby.com/essay/The-Boundary-Between-The-Pacific-Plate-And-P3UF3JM5Y9JXW">The Boundary Between The Pacific Plate And Australian ...</a> The most famous example of this is the San Andreas Fault Zone of western North America. San Andres Fault, Middle East Dead Sea transform fault, New Zealand Alpine fault F. Where is transform fault located? It’s the "on-land" boundary of the Pacific and Australian Plates. It is just west of the Centr al American coast. It is located in New Zealand’s South Island on the Australian and Pacific plate boundary. In the first one the steeply dipping Alpine Fault undergoes a progressive change <a href="https://gwenkgeog.blogspot.com/">Armchair exploration (GEOG 1202)</a> Both the San Andreas … <a href="https://ui.adsabs.harvard.edu/abs/1982Tectp..87...11N/abstract">Fault</a> Bay of Islands/Russell Whangarei NORTHLAND 23 Hokianga Harbour The Pacific and Australian plates are trying to slide past each other. The Queen Charlotte Fault is an active transform fault that marks the boundary of the North American and the Pacific Plates and known as the “North San Andreas Fault”. Topics Concepts Citizen science Teacher PLD The San Andreas connects a divergent boundary in the Gulf of California with the Cascadia subduction zone. Transform boundaries are places where plates slide sideways past each other. The transform fault forms a series of ri dges and troughs connecting two segments of the oceani c ridge. <a href="https://www.quora.com/What-places-in-the-world-that-lie-in-transform-plate-boundaries">Some of the most notable transform plate boundaries on ...</a> This survey will open in a new tab and you can fill it out after your visit to the site. You can pick out the line of the Alpine Fault on this satellite image of the South Island. Snow on the mountains of the Pacific plate contrasts with the lower land of the Australian plate. The Alpine Fault is called a strike slip or transform fault. A smaller number of transform faults cut continental lithosphere. The offset is about 85 km. Linear valleys, small ponds, stream beds split in half, deep trenches, and scarps and ridges often mark the location of a transform boundary. A transform boundary is location where where movement of two tectonic plates occur. The Alpine Fault is a transform boundary between the Pacific Plate and the Indo-Australian Plate 8. What are examples of transform boundaries? The Alpine Fault marks the boundary of the Pacific and Australian Plates. The Alpine Fault is a transform boundary. The same distinctive gold-bearing rocks are found on the northwestern side of the fault, but they lie about 480 km to the northeast. The west side of California is moving north, and the east side is moving south. A transform fault or transform boundary, sometimes called a strike-slip boundary, is a fault along a plate boundary where the motion is predominantly horizontal. 32. transform Alpine Fault connects oblique subduction zones of opposite polarities (Figure 1). Transform boundaries represent the borders found in the fractured pieces of the Earth’s crust where one tectonic plate slides past another to create an earthquake fault zone. The San Andreas connects a divergent boundary in the Gulf of California with the Cascadia subduction zone. The Alpine fault is a transform boundary between the Pacific Plate and the Australian Plate. Most transform faults are found in the ocean basin and connect offsets in the mid-ocean ridges. Earthquakes along the fault, and the associated earth movements, have formed the Southern Alps. Relative movement of these blocks in response to plate boundary motions gives rise to differential vertical displacements of the earth's crust and hence exercises a degree of control on the tectonic evolution of sedimentary basins adjacent to the … The San Andreas connects a divergent boundary in the Gulf of California with the Cascadia subduction zone. What is most likely to happen to these towns over time? Transform faults are locations of recurring earthquake activity and faulting. The Australian plate is sliding horizontally towards the north-east, at the same time as the Pacific plate is pushing up, forming the Southern Alps. A comparison between the transpressional plate boundaries of South Island, New Zealand, and southern California, USA: The Alpine and San Andreas Fault Systems Gary S. Fuis, Monica D. Kohler, Martin Scherwath, Uri ten Brink, Harm van Avendonk, & Janice M. Murphy Published 2007, SCEC Contribution #970 The offset is about 85 km. The San Andreas fault in California is a major transform boundary or fault, as is New Zealand's Alpine fault and North America's Queen Charlotte fault. True | False 10. The Alpine fault is a plate boundary that cuts across the land in a northeasterly- southwesterly direction. Alpine Valley Fault. This fault zone is a part of western Turkey, in the Marmara sea. Michigan State University. 61. What are geologic events occur at a transform boundary? The plates’ grinding action against each other can produce phenomenal effects such as shallow earthquakes, widespread deformation of the crust, and displacement of rock. The San Andreas connects a divergent boundary in the Gulf of California with the Cascadia subduction zone. The most famous example of this is the San Andreas Fault Zone of western North America. Another example of a transform boundary on land is the Alpine Fault of New Zealand. Hokitika is a town on the Australian Plate. The Alpine Fault also ruptures, which leads to seismic activity as well as considerable horizontal movement, up to 30 m every 1000 years. Most transform plate boundaries are located within ocean basins, such as the Alpine Fault in California. Many transform boundaries are found on the sea floor, where they connect segments of diverging mid-ocean ridges. Here we present the first observations of tectonic tremor along New Zealand's Alpine Fault, a major transform boundary that is late in its earthquake cycle. At this point, it splits in… The fracture zone that forms a transform plate boundary is known as a transform fault. Two models have been proposed to explain the Alpine Fault-Puysegur subduction transition along the Fiordland Margin. It is a transform boundary formed on the west coast of North America in California. 190 - Earth's Layers • pg. [1] Transform Plate Boundaries are locations where two plates slide past one another. The Marlborough Fault System is a set of four large dextral strike-slip faults and other related structures in the northern part of South Island, New Zealand, which transfer displacement between the mainly transform plate boundary of the Alpine fault and the mainly destructive boundary of the Kermadec Trench, and together form the boundary between the Australian and … Answer (1 of 2): Transform Plate Boundaries are locations where two plates slide past one another. Transform boundary (also known as transform fault boundary, transform plate boundary, transform plate margin, strike-slip boundary, sliding boundary, or conservative plate boundary) A transform boundary occur when tectonic plates slide and grind against each other along a fault. 2. This fault has ruptured four times in the past 900 years, each time producing an earthquake of about magnitude 8. May 05, 2017. Tweet. Gold was discovered in distinctive rocks near Queenstown on the southeast side of the fault. The transform boundary belt runs along the western border of the Southern Alps. Transform faults occur at plate boundaries. The Canterbury Plains lie along the eastern side of the Southern Alps on New Zealand’s South Island.They also lay near the Alpine Fault, a transform boundary fault between the Indo-Australian and Pacific tectonic plates that slips laterally. The Alpine Fault is a geological fault, known as a right-lateral strike-slip fault, that runs almost the entire length of New Zealand's South Island. A. The Alpine Fault is considered to be a visible, “on-land” boundary of the two constituent plates, and also marks the transition from a transform to convergent boundary. A transform fault may occur in the portion of a fracture zone that exists between different offset spreading centres or that connects spreading centres to deep-sea trenches in subduction zones. California’s San Andreas Fault System - Turkey’s North Anatolian Fault - New Zealand’s Alpine Fault Zone - Linear valleys, small ponds, stream beds split in half, deep trenches, and scarps and ridges often mark the location of a transform boundary. Transform boundaries represent the borders found in the fractured pieces of the Earth’s crust where one tectonic plate slides past another to create an earthquake fault zone. The San Andreas connects a divergent boundary in the Gulf of California with the Cascadia subduction zone. The most famous example of this is the San Andreas Fault Zone of western North America. The Alpine Fault is the dominant structure defining the Australian-Pacific plate boundary in the South Island of New Zealand. When do tectonic plates slide through transform boundaries? Transform faults are called conservative boundaries because no crust is created or destroyed; the plates just move past each other. The San Andreas connects a divergent boundary in the Gulf of California with the Cascadia subduction zone. Transform boundaries represent the borders found in the fractured pieces of the Earth's crust where one tectonic plate slides past another to create an earthquake fault zone. Another example of a transform boundary on land is the Alpine Fault of New Zealand. The Alpine Fault runs for about 600km up the spine of the South Island, and is one of the world’s major geological features. Most transform faults are found in the ocean basin and connect offsets in the mid-ocean ridges. Continental transform boundaries in detail consist of zones of fault-bounded blocks adjacent to the principal active transform fault(s). Another example of a transform boundary on land is the Alpine Fault of New Zealand. The Vienna Basin Transform Fault system recorded seismicity with only a few major The LRG is a Mesozoic and Cenozoic rift extends for about 450 km from the central earthquakes in the last centuries, such as the structure located in the southeastern Nether­ Eastern Alps into the outer Polish Carpathians. Transform Fault Boundary.pdf. 9. What is a real world example of transform boundaries? The most famous example of this is the San Andreas Fault Zone of western North America. Both the San Andreas Fault and the Alpine Fault are shown on our Interactive Plate Tectonics Map. Transform boundaries represent the borders found in the fractured pieces of the Earth’s crust where one tectonic plate slides past another to create an earthquake fault zone. San Andres Fault, Middle East Dead Sea transform fault, New Zealand Alpine fault F. The San Andreas fault in California is a major transform boundary or fault, as is New Zealand's Alpine fault and North America's Queen Charlotte fault. Rights: Lloyd Homer, GNS Science Limited Published 18 August 2014 Size: 680 KB Referencing Hub media. Other transform boundaries around the world include the Alpine Fault in New Zealand and the Dead Sea Transform in the Middle East. We report tectonic tremor that occurred on the central section of the Alpine Fault on 12 days between March 2009 and October 2011. Transform Plate Boundaries are locations where two plates slide past one another. What plate boundary must exist at Alpine Fault? Some examples of continental transform boundaries are the famous San Andreas fault, the Alpine fault in New Zealand, the Queen Charlotte Island fault near western Canada, the North Anatolian fault in Turkey, and the Dead Sea rift in the Middle East. In plate tectonics, a transform boundary (also known as transform fault boundary, transform plate boundary, transform plate margin or conservative plate boundary) is said to occur when tectonic plates slide and grind against each other along a transform fault.The relative motion of such plates is horizontal in either sinistral or dextral direction.. Add to collection. The San Andreas fault of California is a prime example of a continental transform boundary; others are the North Anatolian fault of northern Turkey, the Alpine fault crossing New Zealand, the Dead Sea rift in the Middle East, the Queen Charlotte Islands fault off western Canada, and the Magellanes-Fagnano fault system of South America. While … The fracture zone that forms a transform plate boundary is known as a transform fault. Linear valleys, small ponds, stream beds split in half, deep trenches, and scarps and ridges often mark the location of a transform boundary. Most transform … The fracture zone that forms a transform plate boundary is known as a transform fault. The Alpine Fault is a geological fault, known as a right-lateral strike-slip fault, that runs almost the entire length of New Zealand's South Island. We report tectonic tremor that occurred on the central section of the Alpine Fault on 12 … The Alpine Fault is called a strike slip or 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 San Andreas Fault is part of a transform plate boundary that disrupts the topography of an ancient subduction zone. Hanmer is a town on the Pacific Plate. Another example of a transform boundary on land is the Alpine Fault of New Zealand. Take a tour along the Alpine Fault, Aotearoa New Zealand’s on-land plate boundary and one of the longest natural straight lines in the world! The fault runs through the South Island of New Zealand. In plate tectonics, a transform boundary (also known as transform fault boundary, transform plate boundary, transform plate margin or conservative plate boundary) is said to occur when tectonic plates slide and grind against each other along a transform fault.The relative motion of such plates is horizontal in either sinistral or dextral direction.. 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. When you look at the transform fault diagram, imagine the double line as a divergent plate boundary... Examples of Divergent Boundaries The mid-Atlantic ridge is an example of a divergent boundary , where the Eurasian Plate that covers all of Europe separates from the North American Plate. The Alpine Fault is a geological fault, specifically a right-lateral strike-slip fault, that runs almost the entire length of New Zealand’s South Island. The most famous example of this is the San Andreas Fault Zone of western North America. The Hope Fault is an active dextral (right lateral) strike-slip fault in the northeastern part of South Island, New Zealand.It forms part of the Marlborough Fault System, which accommodates the transfer of displacement along the oblique convergent boundary between the Indo-Australian Plate and Pacific Plate, from the transform Alpine Fault to the Hikurangi Trench subduction zone. A smaller number of transform faults cut continental lithosphere. What are examples of transform boundaries? The mountains are rising at 7 millimetres a year, but erosion wears them down at a similar rate. The Alpine Fault cuts through New Zealand. Transform boundary (also known as transform fault boundary, transform plate boundary, transform plate margin, strike-slip boundary, sliding boundary, or conservative plate boundary) A transform boundary occur when tectonic plates slide and grind against each other along a fault.  A transform fault or transform boundary, also known as conservative plate boundary since these faults neither create nor destroy lithosphere, is a type of fault whose relative motion is predominantly horizontal in either sinistral or dextral direction. The San Andreas connects a divergent boundary in the Gulf of California with the Cascadia subduction zone. The transform fault forms a series of ri dges and troughs connecting two segments of the oceani c ridge. Transform Boundary – Alpine Fault, South Island, New Zealand The Alpine Fault is a geological fault, specifically a right-lateral strike-slip fault, that runs almost the entire length of New Zealand’s South Island. It forms a transform boundary between the Pacific Plate and the Indo-Australian Plate. It forms a transform boundary between the Pacific Plate and the Indo-Australian Plate. 1 Introduction. A transform fault is a special case of a strike-slip fault that also forms a plate boundary. transform boundary between the Pacific and Australian plates. Letters in ovals are abbreviations for NPS. It forms a transform boundary between the Pacific Plate and the Indo-Australian Plate. More exactly, the Alpine Fault. What is the example of transform fault boundary? When you look at the transform fault diagram, imagine the double line as a divergent plate boundary and visualize which way the diverging plates would be moving. The San Andreas connects a divergent boundary in the Gulf of California with the Cascadia subduction zone. Also Know, what is an example of a divergent boundary? Transform Fault Boundaries is the third type of plate boundaries in which the plates slide past with each other horizontally as shown in the figure 1 below. The fracture region that makes up a transform plate boundary is known as the transform  fault. It  was  first  suggested  by  John  Tuzo  Wilson,  a  Canadian geophysicist, in 1965. The Alpine Fault is considered to be a visible, “on-land” boundary of the two constituent plates, and also marks the transition from a transform to convergent boundary. Linear valleys, small ponds, stream beds split in half, deep trenches, and scarps and ridges often mark the location of a transform boundary. Both the San Andreas Fault and the Alpine Fault are shown on our Interactive Plate Tectonics Map. Furthermore, transform faults end abruptly and are connected on both ends to other faults, ridges, or subduction zones. Some large-scale transform boundaries include the San Andreas fault in western North America and the Alpine fault in New Zealand. It ends abruptly where it connects to another plate boundary, either another transform, a spreading ridge, or a subduction zone. By the end of this activity, students should be able to: It forms a transform boundary between the Pacific Plate and the Indo-Australian Plate. Another example of a transform boundary on land is the Alpine Fault of New Zealand. The San Andreas connects a divergent boundary in the Gulf of California with the Cascadia subduction zone. What are examples of transform boundaries? A transform fault is a type of strike-slip fault and conservative boundary, and a strike-slip fault is a fault with horizontal motion. 31 Clipperton Fracture Zone Transform plate boundary The Clipperton transform fault cuts the East Pacific Rise, in the northern part of this map. Another example of a transform boundary on land is the Alpine Fault of New Zealand. + Create new collection. Answer: Some of the most notable transform plate boundaries on Planet Earth. Where are the locations of at least three major transform boundaries? Process along the plate boundary •Convergent plate boundary - subduction - •Divergent plate boundary - - •Transform plate boundary - - The choices is • Earthquake activity • Volcanic Activity • Alpine Fault • Formation of trenches • Subduction • Creation of mid-ocean ridge • Creation of linear lakes • San Andreas Fault I am at the south island of New Zealand! A) a continental transform B) a continental-continental convergent C) an oceanic transform D) an oceanic-continental convergent E) an oceanic-oceanic convergent Both the San Andreas Fault and the Alpine Fault are shown on our Interactive Plate Tectonics Map. Some examples of continental transform boundaries are the famous San Andreas fault, the Alpine fault in New Zealand, the Queen Charlotte Island fault near western Canada, the North Anatolian fault in Turkey, and the Dead Sea rift in the Middle East. Another example of a transform boundary on land is the Alpine Fault of New Zealand. The Alpine Fault then runs the length of the South Island just west of the Southern Alps to near Lewis Passin the central northern section of the island. Transform boundaries represent the borders found in the fractured pieces of the Earth’s crust where one tectonic plate slides past another to create an earthquake fault zone. Another example of a transform boundary on land is the Alpine Fault of New Zealand. While this is the basic definition of a transform boundary, there’s more to them than that. The formation of Southern Alps is attributed to the tectonic activity, including earthquakes along this transform boundary. The plate motion of is horizontal. Another example of a transform boundary on land is the Alpine Fault of New Zealand. The most famous example of a transform boundary is the San Andreas Fault in California. A transform boundary is a place where two of the Earth’s tectonic plates move past one another. What landforms are created by transform boundaries? ... - North Anatolian Fault. It forms a … Another example of a transform boundary on land is the Alpine Fault of New Zealand. is the San Andreas Fault Zone of western North America. The most famous example of this is the San Andreas Fault Zone of western North America. Modified from “Earth: Portrait of a Planet, by S. Marshak, 2001, W. W. Norton & Comp., New York. The Alpine Fault also ruptures, which leads to seismic activity as well as considerable horizontal movement, up to 30 m every 1000 years. The earthquakes are A transform fault (Wilson, 1965) is a strike-slip fault forming a plate boundary, thus cutting the entire lithosphere that keeps a permanent record of its deformations.It connects two other plate boundaries or plate boundary zones, even other transform faults (this last only at triple junctions), also called “conservative boundaries,” along which lithosphere is neither created nor destroyed. Some examples of continental transform boundaries are the famous San Andreas fault, the Alpine fault in New Zealand, the Queen Charlotte Island fault near western Canada, the North Anatolian fault in Turkey, and the Dead Sea rift in the Middle East. The San Andreas connects a divergent boundary in the Gulf of California with the Cascadia subduction zone. Another example of a transform boundary on land is the Alpine Fault of New Zealand. We report tectonic tremor that occurred on the central section of the Alpine Fault on 12 days between March 2009 and October 2011. Learning Outcomes. 32. How often does the Alpine Fault rupture? Zealandia straddles the boundary between the Australian and Pacific plates (Figures 1 and 2).Today, relative plate motion in the southern part of the New Zealand region is essentially parallel to the Alpine Fault (∼38 mm/yr) with a small component of orthogonal convergence (<9 mm/yr), determined from GPS measurements [Beavan et al., 2002]. Linear valleys, small ponds, stream beds split in half, deep trenches, and scarps and ridges often mark the location of a transform boundary. Here we present the first observations of tectonic tremor along New Zealand’s Alpine Fault, a major transform boundary that is late in its earthquake cycle. Find out how it was discovered and learn what science can tell us about Alpine Fault earthquakes. GLG 201. December 7, 2021. The _____ and the Alpine Fault of New Zealand are examples of transform plate boundaries. Other transform boundaries around the world include the Alpine Fault in New Zealand and the Dead Sea Transform in the Middle East. Most transform … At the transition between the Hikurangi subduction zone and the Alpine fault lies the Marlborough Fault system, an interesting and complex transform boundary zone with not one right-lateral strike slip faults but four! As our only present-day indicator of active deforma-tion on the Alpine Fault, tremor provides a unique means of documenting and elucidating ambient coupling and stress conditions along this portion the plate boundary.  East side is moving South both the San Andreas Fault zone is a transform Plate boundary sea., but erosion wears them down at a transform Fault are locations of recurring activity! Alpine Valley Fault it out after your visit to the tectonic activity, including earthquakes along transform... But erosion wears them down at a similar rate Size: 680 KB Referencing media... 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