With the advancements in technology and the combined knowledge of District staff, we can present the data you need to be better informed by harnessing GIS's powerful ability to graphically illustrate and organize that data. 0000002472 00000 n Search. 26 23 H�b```��L�� cc`a��`@V4�x93� �ɷ�!�� ���'l�6��1�w�y�����Ac�k���/��R��W�n4d4���.�Q����5�T�7h�d��u2�Le���t��h�T�Sm�����.��Wg��y�(�8vl���tDØ-B1��y�'���㲠�3�*��,Y\CV��]:��lE�xy$Ui���%���R��-��<1і��g�u=��_^Lj�&��p�e��,sW�&߂'�& 0000004661 00000 n This location's average precipitation levels are 0000002381 00000 n
0000001007 00000 n 0000002163 00000 n 0000007245 00000 n Hurricane Fault is covered by higher than 57% of other locations on record. Hurricane Fault view northeast from Silver Reef. The Toroweap Fault of northwest Arizona and southwest Utah is part of a fault system of the west Grand Canyon region, Arizona, USA; also the west perimeter regions of the Coconino and Colorado Plateaus.The Hurricane Fault originates at the Toroweap Fault, in the region of the Colorado River, and strikes as the westerly depression of the Toroweap Fault.. The Cascadia Subduction Zone, Pacific Northwest The American Geosciences Institute represents and serves the geoscience community by providing collaborative leadership and information to connect Earth, science, and people. These maps are seperated into rectangular quadrants that are Photos provided by Flickr are under the copyright of their owners. 0000092201 00000 n Preliminary map of young faults in the United States as a guide to possible fault activity. F����r�ӿ�}/@�,�d|@��IlAj��@��_��'\��w�x,�H!=���^O�Yz�14��2�d� ��g��%�g�L/����Oc���~&70Z��2 �wX�A��*p��� Keu ݊��d�RX�[ybݖ��m��~��A�Ml@/�7p4m�����8�w���i��wEh� topographic maps of the U.S. called US Topo that are separated into ?r0h1H���k�%�#��G�[Rx�Dž#˯Z� ]X������������>Of���'a\��k'ZrrK,���pDb1��J ���Q,��i �0R���\X� (�ftq���HBt�ԡ��CA�@�B;: f3��L��% 4���J 1 ��cA�0 �v`G�а �3����ݫ� �Pʰ�Ɉa/S�J`.cX���`����p��R;q5.�3��n�N��2�`�ax�k�ks 0�1����T�9@� �� ��j endstream endobj 132 0 obj 576 endobj 111 0 obj << /Type /Page /Parent 103 0 R /Resources 112 0 R /Contents 118 0 R /MediaBox [ 0 0 612 792 ] /CropBox [ 0 0 612 792 ] /Rotate 0 >> endobj 112 0 obj << /ProcSet [ /PDF /Text /ImageB ] /Font << /F1 121 0 R /TT2 115 0 R /TT4 113 0 R /TT6 120 0 R /TT8 122 0 R >> /XObject << /Im1 130 0 R >> /ExtGState << /GS1 127 0 R >> /ColorSpace << /Cs6 117 0 R >> >> endobj 113 0 obj << /Type /Font /Subtype /TrueType /FirstChar 32 /LastChar 176 /Widths [ 278 0 0 0 0 0 0 191 333 333 0 0 278 333 278 0 556 556 556 556 556 556 556 556 556 556 0 0 0 0 0 0 0 667 667 722 722 667 611 778 722 278 500 667 556 833 722 778 667 778 722 667 611 722 667 944 0 0 611 0 0 0 0 0 0 556 556 500 556 556 278 556 556 222 0 500 222 833 556 556 556 0 333 500 278 556 500 722 0 500 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 400 ] /Encoding /WinAnsiEncoding /BaseFont /IPKICC+Arial /FontDescriptor 116 0 R >> endobj 114 0 obj << /Type /FontDescriptor /Ascent 891 /CapHeight 656 /Descent -216 /Flags 34 /FontBBox [ -568 -307 2028 1007 ] /FontName /IPKIBB+TimesNewRoman /ItalicAngle 0 /StemV 94 /XHeight 0 /FontFile2 125 0 R >> endobj 115 0 obj << /Type /Font /Subtype /TrueType /FirstChar 32 /LastChar 189 /Widths [ 250 0 0 500 0 0 778 180 333 333 0 0 250 333 250 278 500 500 500 500 500 500 500 500 500 500 278 278 0 0 0 444 921 722 667 667 722 611 556 722 722 333 389 722 611 889 722 722 556 722 667 556 611 722 722 944 722 722 611 333 0 333 0 500 0 444 500 444 500 444 333 500 500 278 278 500 278 778 500 500 500 500 333 389 278 500 500 722 500 500 444 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 333 333 444 444 0 0 1000 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 549 0 0 0 0 0 0 0 0 310 0 750 750 ] /Encoding /WinAnsiEncoding /BaseFont /IPKIBB+TimesNewRoman /FontDescriptor 114 0 R >> endobj 116 0 obj << /Type /FontDescriptor /Ascent 905 /CapHeight 718 /Descent -211 /Flags 32 /FontBBox [ -665 -325 2028 1006 ] /FontName /IPKICC+Arial /ItalicAngle 0 /StemV 94 /FontFile2 124 0 R >> endobj 117 0 obj [ /ICCBased 128 0 R ] endobj 118 0 obj << /Length 596 /Filter /FlateDecode >> stream
The valleys on the west sank, creating what is known as the Hurricane Fault. The Hurricane Fault begins at the north end of Cedar Valley and goes in an almost straight line south, across Grand Canyon, and ends at Pete Springs, east of Kingman, Arizona. Data sources include the United States Board on Geographic Names, National Weather Service, U.S. Census Bureau, NASA, and Google. The Hurricane Fault is an intracrustal seismic fault that runs along the boundary between the Colorado Plateau block and the Basin and Range geologic province of western North America. (���!Θ��8�e����n��Q���NJ=�娭�� ��� G���\MJ.mlc�s���j�梧����k�����f|s�j��d4�S��� The Hurricane Fault (GC17E2K) was created by TerryDad2 (adopted by Supertbone) on 11/16/2007.
American Geosciences Institute. North American Datum 1983. It's located in Utah, United States.The Hurricane Fault marks one of the edges of the Colorado Plateau. Find local businesses, view maps and get driving directions in Google Maps. startxref
0000005673 00000 n
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lower than 89% of other locations on record. The Hurricane Fault and Monocline are the major structural features of the map area. H��T�n�0}�+�c7-6`��ڴi����=[�����(���$-J�bT�ͻ�*�.V6m�'��9�4G)�I�����K�� J3D�&�>4�:�]�Ѵ, `(_"�j��ʒ�'�qe�*�ܿ��|*yhz�NR��� 0qH�s(��ڧ�s�I(�!�C�qL|��!�B�Zo$�%ۂ~[ x�{a�3Fr��dmL�C�&a South Dakota Department of Environment and Natural Resources, Delaware Department of Natural Resources and Environmental Control, National Oceanic and Atmospheric Administration, Interactive map of California earthquake hazard zones, Interactive map of post-fire debris-flow hazards in the Western United States, Interactive map of hazardous waste cleanups in the United States, Interactive map of spills in South Dakota, Interactive map of real-time flood information for Texas, Interactive map of sea level rise impacts in Delaware.
SURFACE-FAULT-RUPTURE-HAZARD MAP FOR THE ST. GEORGE–HURRICANE METROPOLITAN AREA Basemap consists of National Agricultural Imagery Program natural color aerial photography. Related terms: barranca, canyon, chasm, cove, draw, glen, gorge, gulch, gulf, hollow, ravine.
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DESCRIPTION The black rocks above Toquerville, La Verkin, and Hurricane are part of an ancient lava flow. H����jA�{ݧ�eZ�V��f և��um'r��-�:i܄�~5�&��M!ea�I�~n!0#ٔ��@�I:��6�t�� ,�>��{:خ���õ0%t����~�R�;Gz8ZΚr�As�Y�u3��ޯ�-�z�&o����zL�X�FS�&%�(����"�t��+��&�ʵ�`T})8� 0000089444 00000 n This location's average winter low temps are 0000031163 00000 n xref �wS���~�T/[�G�M������ Free printable topographic map of Hurricane Fault (aka Hurricane Lodge Fault) in Iron County, UT including photos, elevation & GPS coordinates. 0000089523 00000 n differences in elevation and topography, the historic weather at the two separate locations The 1992 St. George earthquake (magnitude 5.8), which triggered a damaging landslide, has been attributed to the Hurricane Fault.
It's a Not chosen size geocache, with difficulty of 2, terrain of 1. 0000006853 00000 n rectangular quadrants that are printed at 22.75"x29" or OK. SITE MAP. The Hurricane fault is a major, active, high-angle west-dipping normal fault Because the strike of the fault changes along its length, the Hurricane fault is a segmented fault. 1.
The National Oceanic and Atmospheric Administration's Historical Hurricane Tracks tool shows the tracks and characteristics of over 6,000 tropical cyclones around the world dating back to 1842.
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0000001512 00000 n 0000005092 00000 n Because the nearest station and this geographic feature may have In Washington County, for example, the plateaus east of the Hurricane Cliffs move up along the Hurricane fault zone relative to the downward movement of the Below are weather averages from 1971 to 2000 according to data gathered from the nearest �&̵�mbr���ㄮWU�*���:K�� ٱ\�1ϣ��љFo��IE#{璊����"��$2���X5U�eӜ��4wjS:���c��%)3��1Q>+c��z!0z5l�����]���Y��4�)*��>��Ʀ�����/Y�Nۙ} Search Catalog Data Catalog Data & text in Documents Search By Date Range; Advanced Search A fault is a break in the earth’s crust along which movement has taken place causing an earthquake. 0000009105 00000 n !ic ,�st��9� {y{�f�:,�g�I8��~��.������Y�I�Q��a�F.����6J�==�̨����pyI�F[�1�0��aqa�C��y�ZG�}��� temperature measurements is PAROWAN POWER PL which is approximately 9 miles away and has an elevation of 6,000 feet (1,103 feet lower than Hurricane Fault). official weather station. Free printable topographic map of Hurricane Fault (aka Hurricane Lodge Fault) in Iron County, UT including photos, elevation & GPS coordinates. Map via USGS. 0000002838 00000 n �m�ֻ��8Z�\�7{)o�j��+�B�N�(,�b�bU��Ss?���4M�B�$����C����e �v���y�cYy�&;��7��u��%X$�7. The National Oceanic and Atmospheric Administration's Historical Hurricane Tracks tool shows the tracks and characteristics of over 6,000 tropical cyclones around the world dating back to 1842. All rights reserved.
The resulting fault scarp, the Hurricane Cliffs, exposes more than 610 m of Permian strata. What are the most dangerous fault lines in the USA?
The map now contains brown squares outlining nearby US Topo Map quadrants. H�\T tT�����7�0�d��&����@( �dY@'$��$HȰ�hd!t�H%�lA*��@��-�P�*ֲ���� Vd^�H����ݷ�� !�;� 9���lv�2wlI��^��� PCɼ9Z���X�Mu�W��-l��L�(�^;��P�H� �wT��J�C�ob����
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It is a 250-km-long, north-south striking, high-angle, down-to-the-west normal fault, running from about Cedar City, Utah southward into northwestern Arizona. AGI's Critical Issues Program is generously underwritten in memory of Charles L. Weiner. This map gives an overview of geologically young faults and is intended to help in evaluation of the potential activity of faulting nationally.
Privacy Policy. lower than 65% of other locations on record. The intended to be printed at 22.75"x29" or larger. 0000004589 00000 n
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