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This line feature class contains 1:24,000-scale geologic fold axes locations and descriptive data for areas of Washington State. |
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This line feature class contains 1:24,000-scale geologic fold axes locations and descriptive data for areas of Washington State. |
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5000 |
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[] |
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<DIV STYLE="text-align:Left;"><DIV><DIV><P><SPAN>A fold occurs when originally flat surfaces, such as sedimentary strata, are bent or curved as a result of tectonic movements. The trace of the "fold axis" is commonly displayed on geologic maps. The fold axis is the line that traces the top or bottom curve of the fold. Folds can be small, measuring centimeters to meters across, or can be so large they may be viewed from space.</SPAN></P></DIV></DIV></DIV> |
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<DIV STYLE="text-align:Left;"><DIV><DIV><P><SPAN>The Washington Geological Survey (WGS) shall not be held liable for improper or incorrect use of the data described and/or contained herein. This product is provided 'as is' without warranty of any kind, either expressed or implied, including, but not limited to, the implied warranties of merchantability and fitness for a particular use. The Washington State Department of Natural Resources and the authors of this product will not be liable to the user of this product for any activity involving the product with respect to the following: (a) lost profits, lost savings, or any other consequential damages; (b) the fitness of the product for a particular purpose; or (c) use of the product or results obtained from use of the product. Although these data have been processed successfully on computers of WGS, no warranty, expressed or implied, is made by WGS regarding the use of these data on any other system, nor does the fact of distribution constitute or imply any such warranty.</SPAN></P></DIV></DIV></DIV> |
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| title:
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fold |
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["monocline","overturned syncline","plunge","USA","axial trace","map","anticline","Washington State","overturned anticline","syncline","fold","synclinal bend","anticlinal bend","geologic map","growth fold","geologic"] |
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en-US |
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50000 |
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