NaturalGreen

<span style="font-size: large;"><span style="font-family: "calibri" , "sans-serif"; line-height: 115%;">The </span><span style="font-family: "calibri" , "sans-serif"; line-height: 115%;">Earth crust is divided into large 7 plates
include African, North American, South American, Eurasian, Australian,
Antarctic, and Pacific plates and few small plates such as Arabian. Those
plates are regularly moved in different directions at different speeds apart
from each other or towards each other.</span></span><br />
<span style="font-family: "calibri" , "sans-serif"; font-size: 12.0pt; line-height: 115%;"><br /></span>
<br />
<div class="separator" style="clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjg7cyYV2FVGDh0NKmOTtmQN2uH0wN3XRnZZb7pRiHmyqIVnEqinTz6tPMi_AiOp78nfFzd7nxpZ9V3mIIWK-L7P5qvoWHXI-gCpKv7wMHxA53wmi5Nn3RUYK3fsgEPvjlN46DDyudUgzIT/s1600/Continental_drift.gif" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" height="346" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjg7cyYV2FVGDh0NKmOTtmQN2uH0wN3XRnZZb7pRiHmyqIVnEqinTz6tPMi_AiOp78nfFzd7nxpZ9V3mIIWK-L7P5qvoWHXI-gCpKv7wMHxA53wmi5Nn3RUYK3fsgEPvjlN46DDyudUgzIT/s640/Continental_drift.gif" width="640" /></a></div>
<span style="font-family: "calibri" , "sans-serif"; font-size: 12.0pt; line-height: 115%;"><br /></span>
<br />
<div class="MsoNormal" style="margin-left: .5in;">
<h3>
<b><u><span style="font-size: large; line-height: 115%;">Plat boundary:</span></u></b></h3>
</div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: large; line-height: 115%;">The place where the two plates are met defined as the plate
boundaries.<o:p></o:p></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: large; line-height: 115%;"><br /></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<h3>
<b><u><span style="font-size: large; line-height: 115%;">Types of plat
boundaries:</span></u></b></h3>
</div>
<div class="MsoNormal" style="margin-left: .5in;">
<b><u><span style="font-size: large; line-height: 115%;"><br /></span></u></b></div>
<div class="MsoListParagraph" style="margin-left: 1.0in; mso-add-space: auto; mso-list: l0 level1 lfo1; text-indent: -.25in;">
<h4>
<span style="font-size: large;"><b><span style="line-height: 115%;">1)<span style="font-stretch: normal; font-weight: normal; line-height: normal;">     
</span></span></b><b><span style="line-height: 115%;">Divergent boundaries:<o:p></o:p></span></b></span></h4>
</div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: large; line-height: 115%;">Plate boundaries move apart from each other. <o:p></o:p></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: large; line-height: 115%;">As a result of the conversion, currents arise from the mantle, sea the floor is spread and creates magma. <o:p></o:p></span></div>
<span style="font-size: large;"><br /></span>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="line-height: 115%;"><span style="font-size: large;">Results: Mid oceanic ridges, sea floor spreading and volcanic
activity.</span><span style="font-size: 12pt;"><o:p></o:p></span></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: 12.0pt; line-height: 115%;"><br /></span></div>
<div class="separator" style="clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiriVaT25eLd-nz71m-4k97dpiiocP6_SuGLjrGhMQrAvqxYInQCJbGMEBPobHGaYYc8UA2k3FR_v9mHMErEbbxRBpA2VPH5k2tNU-jMjuJVtjdmZMfLFIuQXvIBZya3Ge44yIg4TJFX3TE/s1600/Continental_drift_1.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" height="179" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiriVaT25eLd-nz71m-4k97dpiiocP6_SuGLjrGhMQrAvqxYInQCJbGMEBPobHGaYYc8UA2k3FR_v9mHMErEbbxRBpA2VPH5k2tNU-jMjuJVtjdmZMfLFIuQXvIBZya3Ge44yIg4TJFX3TE/s320/Continental_drift_1.jpg" width="320" /></a></div>
<br />
<div class="separator" style="clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhLvCd4YCbQaBcByrw-h3-MGgT5XvbYQmhrh7qEXxb2drw0Wp_vB7SkzYzZzdfODBofIOGreBXToFU3qALNv6ZIX-2LXOlyqNwRlTIvAHaljH3J7qK1TYKzDiMeeeSQDqsF_61FIv6ajCf1/s1600/Continental_drift_2.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" height="240" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhLvCd4YCbQaBcByrw-h3-MGgT5XvbYQmhrh7qEXxb2drw0Wp_vB7SkzYzZzdfODBofIOGreBXToFU3qALNv6ZIX-2LXOlyqNwRlTIvAHaljH3J7qK1TYKzDiMeeeSQDqsF_61FIv6ajCf1/s320/Continental_drift_2.jpg" width="320" /></a></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: 12.0pt; line-height: 115%;"><br /></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: 12.0pt; line-height: 115%;"><br /></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<h3>
<span style="font-size: large; line-height: 115%;">2) <b>Convergent
boundaries</b>:</span></h3>
</div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: large; line-height: 115%;">Plate boundaries move towards each other.<o:p></o:p></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: large; line-height: 115%;">Both plates have collided and one plate uplift over another. <o:p></o:p></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
</div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: large; line-height: 115%;">Results: Mountain, Trenches, earthquakes and volcanic
activity.</span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: 12.0pt; line-height: 115%;"><br /></span></div>
<div class="separator" style="clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiik9jQhL6gp_oQ6SC9VbThssr7NyUHMhfZJrGFGjCiZGSYWSVNWif51szUah7kBSRVrZYL4NQsl459T2_cKf6pswZWpdwHQlvbKMGv54pPzYkYOzevOrj1atDRJT_5Ur9I_JVB9T8Gbpop/s1600/Continental_drift_3.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" height="213" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiik9jQhL6gp_oQ6SC9VbThssr7NyUHMhfZJrGFGjCiZGSYWSVNWif51szUah7kBSRVrZYL4NQsl459T2_cKf6pswZWpdwHQlvbKMGv54pPzYkYOzevOrj1atDRJT_5Ur9I_JVB9T8Gbpop/s320/Continental_drift_3.jpg" width="320" /></a></div>
<br />
<div class="separator" style="clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi3xndJn5x_Y8WawTg2EeW6fkWC1LNQUCZH3jeNOU2nC_pi_IzgTBanOBUl-p6I-Bl-ddZBhBqxlxGEtHKDFnNvfYulcf6HA7ZTYQp4fUeP3nUnNGsDd8NtiZGCeJG7-UJGOffIu82_FLBf/s1600/Continental_drift_4.png" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" height="186" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi3xndJn5x_Y8WawTg2EeW6fkWC1LNQUCZH3jeNOU2nC_pi_IzgTBanOBUl-p6I-Bl-ddZBhBqxlxGEtHKDFnNvfYulcf6HA7ZTYQp4fUeP3nUnNGsDd8NtiZGCeJG7-UJGOffIu82_FLBf/s320/Continental_drift_4.png" width="320" /></a></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: 12.0pt; line-height: 115%;"><br /></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: 12.0pt; line-height: 115%;"><br /></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: 12.0pt; line-height: 115%;"><br /></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: large; line-height: 115%;">3) <b>Transform
boundaries:</b><o:p></o:p></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: large; line-height: 115%;">Two plates are slightly passed parallel to each other.<o:p></o:p></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: large; line-height: 115%;">Results: Earthquakes</span><span style="line-height: 115%;"><span style="font-size: large;"> </span><span style="font-size: 12pt;"><o:p></o:p></span></span></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: 12.0pt; line-height: 115%;"><br /></span></div>
<div class="separator" style="clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiNpF4dicDkCK8N8K1ZyYsUGpRVjXmPX647JRJrA04UreqmhzP8ZugWSgd7xCH_TM3W_SwtA5Bb30HL_4Twctr4_U5ZJFNI67MpUOPujTn833_aYf47LVdNUfBmejcJjngRIKBlGTz18r14/s1600/Continental_drift_5.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" height="177" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiNpF4dicDkCK8N8K1ZyYsUGpRVjXmPX647JRJrA04UreqmhzP8ZugWSgd7xCH_TM3W_SwtA5Bb30HL_4Twctr4_U5ZJFNI67MpUOPujTn833_aYf47LVdNUfBmejcJjngRIKBlGTz18r14/s320/Continental_drift_5.jpg" width="320" /></a></div>
<br />
<div class="separator" style="clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi5ALebrNCqLOOcpo3Eu61RuHW3oS1TCyD3d_JDEKJq_NKMyVAN5kF1zEhr_q03VWAJfxYzzwNET3yB7VBt36QbCkV-TxzcHDotg3tj-sPOzXo1OM_FnYtJcrBj_nTG-lXi2rtC-CpPIhmj/s1600/Continental_drift_6.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" height="218" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi5ALebrNCqLOOcpo3Eu61RuHW3oS1TCyD3d_JDEKJq_NKMyVAN5kF1zEhr_q03VWAJfxYzzwNET3yB7VBt36QbCkV-TxzcHDotg3tj-sPOzXo1OM_FnYtJcrBj_nTG-lXi2rtC-CpPIhmj/s320/Continental_drift_6.jpg" width="320" /></a></div>
<div class="MsoNormal" style="margin-left: .5in;">
<span style="font-size: 12.0pt; line-height: 115%;"><br /></span></div>
<script>
  (function(i,s,o,g,r,a,m){i['GoogleAnalyticsObject']=r;i[r]=i[r]||function(){
  (i[r].q=i[r].q||[]).push(arguments)},i[r].l=1*new Date();a=s.createElement(o),
  m=s.getElementsByTagName(o)[0];a.async=1;a.src=g;m.parentNode.insertBefore(a,m)
  })(window,document,'script','//www.google-analytics.com/analytics.js','ga');

ga('create', 'UA-65880709-1', 'auto');
  ga('send', 'pageview');

</script>

Continental Drift and Plate Tectonics

The Earth crust is divided into large 7 plates include African, North American, South American, Eurasian, Australian, Antarctic, and Pacific...

Continental Drift and Plate Tectonics

Contact Form