endobj This deformation is the result of forces that are strong enough to move ocean sediments to an eleveation many thousands meters above sea level. %PDF-1.5 <> <>>> <> <> Faulting occurs when rocks fracture under the accumulation of extreme stress created by compression and extensional forces.
<>/XObject<>/Pattern<>/Font<>/ProcSet[/PDF/Text/ImageB/ImageC/ImageI] >>/MediaBox[ 0 0 720 540] /Contents 4 0 R/Group<>/Tabs/S/StructParents 0>> x��TQ��@~�?̣�:3;�fA|P���Vڇ���6�S�w7��jrW�R$�$�o����G��{�ч1�` ��~� *D$f4`!��E�|��2Mz�3Xnӄ`y|sB����|�&Oiw�@��:�g��⥄�ֽa`;/=���U��p+��n+���ȿ�D���5�US��1dh�a���Q ���ױ=�"�e��2*���3"�rD���%Z�+d�/U�+��\�I��(��)TH��F9� o�Դs2$�Sb��q���+�F��AX���[��T�5��P���z&�v�N��R �n�� �A�g /��8ٝXLz �TB\��C�N�?=�ɷ�d�/w]ݙ�J����p�Z�X���w�~L��iC��:F��n+���c��=+Q�r:�0w"z��nF�x�} .��������>mD���L��`}�jn��N�μz3핞��*VK�Ws�߬��ܤ���a�����-�{��)��-����ݪ+���W���F���ȩq�!_�F:��|Vn�+��N �� endstream ;�d�b��F��������c��ktttpu����ctrv��"�B#iF�-����w�.o%�V��l�ʗ�T��Z�jRln&DQ"w?�~���)B�2�(o��������#�1ap5�24y�'��Ms��J�M��W�4u:�c���L��Zx:���xDH�I ��6-����¦��4N�K��-_J��d)J`m崄�J �8� ���YT��TDf��R !u�����7D�����h�6�Tb��ł����!#Ҧ`G,�v=$�"K9��(��`TX��pdF��1x�h�u�ArJ1dyGm��h���qT��� �����R��ɖ���Z��t�QKȍ�����"�X����C�w!��Ġ/�IaՆ�� C]�0�H1��)(n��ƃ~�",��t� �3D�-$y�T��֣}���J2��,�C�5:vj�Y0!Y�� ~� <> Faults and Faulting Earth Structure (2 nd Edition), 2004 W.W. Norton & Co, New York Slide show by Ben van der Pluijm © WW Norton; unless noted otherwise Lecture 8 endstream Folding and faulting 1. 6 0 obj Land between the faults sinks, ... EARTH MOVEMENTS- Folding & faulting Author: stream endobj <>
",#(7),01444'9=82 Mountains by Folding…cont’d This occurs along convergent plate boundaries where 2 plates move towards each other. <>
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endobj N4�I���C��K���j��B�Iii�SC�s���"� 1 0 obj When forces are applied to solid materials they may bend or break. $.' <>>> Fold mountains form from sedimentary rocks; accumulated layers crumple and fold like a table cloth being pushed across a table!
5 0 obj X���r�h�,_a��'�mix{6��.6?���� ��b���Ʊ�e�K�c�!�e�B�m�\xCUh|�f�`4�=�������t�m�f ҫ�1�Ô�m��5vֽ�n������b�W�!�0�@i��ǂ�c��j7�~��m����! Are formed as a result of folding in the upper layers of the earth’s crust; This is as a direct result of compression forces when tectonic plates move against each other from opposite directions i.e. stream 3 0 obj 2 0 obj %PDF-1.5 forces acting against one another <> normal faulting grahcn under gravily = Ornpression compression overhang'ng escarpments reverse fault fault scarp Block Mountain (i) B Tensional forces cause rocks to break and fractures to form. Crustal Deformation Processes: Folding and Faulting: The topographic map illustrated in Figure 10l-1 suggests that the Earth's surface has been deformed. "j ϋ�_�0ng��%�9�7��B0`���[v���C���4v��!�q�*�r&��ܔ�����W����(���d[���>F�#h6l`o��E���"�g�ϳ�hP UF#��x����� B�YUJ����o ^�vI��6D��0�놘v���A�f�makU��d�f/�ބ+��ߴ�p�tN���e�!��Ą��������#�s�ۍ�&���-biP,b@WJ�Txj��(|1�1��#S����ph�Y^�7���aܭf�m�hf����t��u��|��y.� >�W�N��0�hX�c �pS�i!�qi�t�->�&�o������ stream endobj Folding and FaultingFolding and FaultingBy Gulbahar JamaliBy Gulbahar JamaliContact: 03023076659Contact: 03023076659Email: Gulbaharjamali@gmail.comEmail: Gulbaharjamali@gmail.comUniveristy of SindhUniveristy of Sindh 2. Folding occurs when rocks are compressed such that the layers buckle and fold. Folding and Faulting - Free download as Powerpoint Presentation (.ppt), PDF File (.pdf), Text File (.txt) or view presentation slides online. endobj %���� FoldsFolds• A fold is when the earth’s crust is pushed up from its sides. 4 0 obj %���� endobj stream
��8ȒC6�*�t�$8M�,k� stream endobj endobj x�+T04��3 D�&��{�&���+��+ � y �xb��d�jwcX��X��a1Ҥ����d?�1�A�u�MX&�J�U#ùa m�2��t�v �0����G1�>kF�L�5�^����hQP��%舅)���-5�Tښ�"�r��jC��^��z��bg�����k�8Ç/(�0t��p$�(EBa��$ÂP7���j�F��wo.���#B�8��?� P�00��lEC����9�қWn��|*V٬���H~Y�ӼȫY����b�Y�P.�լ,FM���T��H�%��h��lSr���@��A(f��7E]um�p؏�r���r~?+���4�P.�{�ŭ��ͅ=��!nOȏ;{�d��ˮ��-p����}Ç1�}��=!/�����Y���B �t������i�W( ���*�}i(���(5�B��R�g�wcq�uS�z��?��_՞qV>Z Folding and faulting are the most common deformation processes.
endobj folding and faulting-geography 5 0 obj 3 0 obj x���]o�6�� �?�j���7� �|��e��]����5�H�����! Brittle Deformation. Fold Mountains. <> A <>>>/Filter/FlateDecode/Length 35>>
6 0 obj x����0 ��� � v@��{U��M"��S�(�3-z���\rm�Z��k��ٌn����ҲTv�'}�p`�G��>�ax���맪F���X�����Ll�0�,l��qr��� 6. 4 0 obj endobj �eR{ON� endobj endstream (seconds [faulting] to millions of years [folding, faulting, metamorphism during mountain building]) Activity: This activity shows how folded and faulted rocks can provide evidence of the size and direction of the forces which produced the deformation. 2 0 obj Ductile deformation. ���� JFIF K K ��MSO Palette �������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������� C 1 0 obj
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