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The faults are color-coded and designated into one of four categories: historic (red), Holocene (orange), late Quaternary (green), undivided Quaternary (purple).", "geometryType": "esriGeometryPolyline", "sourceSpatialReference": { "wkid": 102100, "latestWkid": 3857 }, "copyrightText": "USGS Earthquake Hazards Program (http://earthquake.usgs.gov/) and California Department of Conservation (http://www.conservation.ca.gov/cgs/rghm/ap/Pages/Index.aspx)", "parentLayer": null, "subLayers": [], "minScale": 2.0000000000000004E7, "maxScale": 750000, "drawingInfo": { "renderer": { "type": "uniqueValue", "field1": "AGE", "field2": null, "field3": null, "defaultSymbol": null, "defaultLabel": null, "uniqueValueInfos": [ { "symbol": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 255, 170, 0, 255 ], "width": 2 }, "value": "<15,000", "label": "Displacement in the last 11,700 years", "description": "Holocene fault displacement (during past 11,700 years) without historic record. Geomorphic evidence for\nHolocene faulting includes sag ponds, scarps showing little erosion, or the following features in Holocene\nage deposits: offset stream courses, linear scarps, shutter ridges, and triangular faceted spurs. 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