virtual plate tectonics
?�`cqr4�����b]�D�z�"X��c�(��cR�]���G��(�WKD7������*�I?�E~N���2�a�$Pbz�i�)]�������j�1 �%*e^��)���WV;�x��g����~o5��_N�S��C{8�eU�{/�:��k]Ԣ/��'W�q��j(�!���A��4��~�CVk���O�P&B8�b4�u@g�?,�j#�S�ӟ�x��H���9g�cF�a)��7s�)������:�W;W?&{$f�XE=��P�8�5yA��>P�rH���教ϭ*��Y.��>OdX�I�WYM�m%����}��Us���~}O�!2Xr�����n:X4��f�_��T�:�暈)i^Z'w�t�=��fl{oR�7��$�& ��rAnp� m��cd����~�t�*G���X����C$��N=zr"����W��]g��tH��=�`��Q���u�q��sI��!eX�! x�Z�s���οG 13th Webinar: Putting Anti-Bias/Anti-Racist Education Into Practice with Scott Thomas. x��MHa�����ї���$T&R��+S�e�L b�}w�g���-E"��u�.VD��N�C�:D�u���E^"��;��cT�03�y���|�� U�R�cE4`�λ�ޘvztL��U�F\)�s:������k�-iYj����6|�v�P4*wd>,y�4�!7�C�N�-��l��C��T�S�3�q";�-E#+c> �vڴ��=�S��79ڸ��@�`Ӌ�m��v�Ul�5��`�P��=��G����j��)�k�P*}�6� ~^/�~�.�~�a���2 You can learn or you can get frustrated. 3. Go to the following website: http://www.learner.org/interactives/dynamicearth/index.html 2. Students visit four websites focused on plate tectonics. << /Length 17 0 R /N 3 /Alternate /DeviceRGB /Filter /FlateDecode >> How fast are the plates moving apart?_____ Add arrows to the diagram below to show how the tectonic plates are moving. Plate tectonics primer: subduction at the corner of Alaska, BC and the Yukon.
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INTERACTIVE: Subduction: Major mountain belts are typically formed by compression during convergence between two continental or oceanic plates that make up the earth’s crust. ***************************************************************************Teachers Pay Teachers is an online marketplace where teachers buy and sell original educational materials.Are you getting the free resources, updates, and special offers we send out every week in our teacher newsletter?Aug. Then the next best thing is this virtual field trip! Use 3 search engines using the same word (i.e. This exercise will help you to choice the correct word, to see if the different search engines can help you. << /Type /Page /Parent 3 0 R /Resources 6 0 R /Contents 4 0 R /MediaBox [0 0 612 792] Study the animation. Write answers on your own paper to turn in. /TT5 12 0 R /TT7 14 0 R /TT2 9 0 R /TT8 15 0 R >> >> You will be taking a test at the end of the lab. If you have access, you could upload into a student server so that they can easily click on the links. endobj Plate Tectonics Virtual Lab Directions 1. 2 0 obj
6 0 obj 2362 Which one gives you the best picture of how the plates may have moved through time. 4 0 obj �O�����r�c^����x�r���r�B���Mx�k妝e�ζ���x��Z/��⊙H�5ϧ��K����I\=)�c�ӈ���(�~".��b4�e�A&�Y��s�N��C�w�|iV��P���|�Ʒ�.z���(F��,�Sx��x &D���t ��gC㪵$�2�β���{�sNA8�UP��aY>�t��x�������g�����w����5o��ͣ 16 0 obj stream Pay attention and complete each activity. ��b,[�^�Z���"Dc��E�[c�îK뚱t��IS7X�Y_��X*��=՞~����X���S�Bkz`��ٓ;��ٔ��!���e׳r���[�=fn��5�3$���X"�y�Dބ���{c������u� �8#)�����b9 =�D"8�o�!ӓ>?i � ���ń�����8�U%�c����ԭ�N �}E���B�b�@����}x�RNIo�����]�[�2Ϸ��c㥳���"o���\gu�'{ɭ����bX��M� HEc�����Nds��W5�T���EJ)�wx'�� ����~ Vcp��"��A�,��B#>,�'ʇ�^R���=��z����! Or in a submarine to the Mid-Atlantic Ridge? Students visit four websites focused on plate tectonics. endobj Word used . They read important facts about convergent and divergent plate movement. Then the next best thing is this virtual field trip! Or in a submarine to the Mid-Atlantic Ridge? Plate Tectonics (Convergent and Divergent Plates) Virtual Field Trip (Aligned with VA SOL 5.7) Can’t afford to take your class to the Himalayas? >> plate tectonics). Along the west coast of North America, the Pacific plate is moving northwestward at about 5.5 cm per year. Look at the websites given to you by your teacher. ?_~̎���.��J�����>˻�:�e]4yw�m�k�˿��ˆ�{���98ۆ�2�RY��6��3���2d���n�!��67��6~����ʹ�ε��v@2��7�U�d��rЬ�nw �Т���sS�6e6��cm�dr=۔w�(�K1��U��F Compare the sites. As students "travel," they record important information on their graphic organizer. *************************************************************************** *************************************************************************** • Click it and you will be taken to a page where you can give a quick rating and leave a short comment for the product. ���@�a�Du�I�Rqݢ�O��3�L���oq81���z��l���������=����~�Z��j�t��N�}�������������f>fj���~GI��k�B-�uC��A��?f�.�M?
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virtual plate tectonics
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