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The Mount Olivet strand of the East Bench fault is mapped just to the east of the East Bench fault. The Nibley Park fault is mapped to the west of the East Bench fault, timing of most recent movement is uncertain. There is also evidence for an older basin-bounding normal fault, the Foothill fault, along the mountain front, that lacks evidence for Holocene offset.", "geometryType": "esriGeometryPolygon", "sourceSpatialReference": { "wkid": 102100, "latestWkid": 3857, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -20037700, "falseY": -30241100, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 }, "copyrightText": "Program Manager: Grant C. Willis (UGS)\nProject Manager: Jon K. King (UGS)\nGIS and Cartography: Adam P. McKean, and Lori Steadman (UGS)\nGeology review: Adolph Yonkee (Weber State University); Jon K. 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