2446 18
0000000016 00000 n
0000000656 00000 n
The map was generated using ArcGIS 8.3. 0000001774 00000 n
0000002194 00000 n
H�lUMs�6��W�(X|��n����X��遖h��>RO�3���]Prf��4$�ݷo�.�裡֓�rM�}s��ƪ�����ި���y�j.V+��}c�u��ߨ@I[[�*I��V;�|hZ��1�]7����vqՍ��/��_���[�A���ݸQ�~��v�����_�u�_�����I���ˊgg��_�Q�b��o�M?M�a�H]�q�T�AV;P5:0��)FZPk����ժ�����RJ$Ւ)�����NQ��alP�]s��Ϊ�C��,���,Y(+��YTa�|$����a����a�o��k�_����zشo��n��㰁�nI��Z�cu���s����ۧa�&���R�����Q���'#�a� ����B]�=c�➱jP
9��WM���5.�r�-�Y^cY2��?���)֏bQ� :�/NGxb= �䔣�C,���Q~�x�Pcg��AYRֆ�X
�-�w��.j�3h�,� ��AP��H9��O��^v:I|���7:xv�&���Q�-+��m�}���>k� <<762b5f2d8b44b54da352cea81afea09d>]>>
x�b```a``z������ "@����d�F���.�<
��2m�h������^6�~P��$��� ��2�2�qrps��p�! Earthquake Belt . 2448 0 obj<>stream
There are mainly three seismic zones on the earth.
2446 0 obj<>
endobj
This article was most recently revised and updated by History at your fingertips
0000007951 00000 n
By signing up for this email, you are agreeing to news, offers, and information from Encyclopaedia Britannica.Be on the lookout for your Britannica newsletter to get trusted stories delivered right to your inbox.
wu������'�t��c����z?��ߠ�o��A�p#s�e�pf��|h���-}�Q=c�^��{��
v(�f
The seismic zone is basically at the junction of the plates, dense in the earthquake zone, and scattered in the out-of-band earthquake. 0000001578 00000 n
Seismic belt, narrow geographic zone on the Earth’s surface along which most earthquake activity occurs.
�V��)g�B�0�i�W��8#�8wթ��8_�٥ʨQ����Q�j@�&�A)/��g�>'K�� �t�;\��
ӥ$պF�ZUn����(4T�%)뫔�0C&�����Z��i���8��bx��E���B�;�����P���ӓ̹�A�om?�W= �x������- �����[��� 0����}��y)7ta�����>j���T�7���@���tܛ�`q�2��ʀ��&���6�Z�L�Ą?�_��yxg)˔z���çL�U���*�u�Sk�Se�O4?�c����.� � �� R�
߁��-��2�5������ ��S�>ӣV����d�`r��n~��Y�&�+`��;�A4�� ���A9� =�-�t��l�`;��~p���� �Gp| ��[`L��`� "A�YA�+��Cb(��R�,� *�T�2B-� Categories This has long been apparent from early catalogs of felt earthquakes and is even more readily discernible in modern seismicity maps, which show instrumentally determined epicentres.
at the local, regional and continental level.
%PDF-1.4
%����
2y�.-;!���K�Z� ���^�i�"L��0���-��
@8(��r�;q��7�L��y��&�Q��q�4�j���|�9�� 0000004442 00000 n
A synthesis of earthquake studies and active deformation exposed in theseismotectonic map N'��)�].�u�J�r� The seismic zone refers to the concentrated distribution of earthquakes.