{
 "culture": "en-NZ",
 "name": "",
 "guid": "",
 "catalogPath": "",
 "snippet": "",
 "description": "There are two main data fields. 'ACCURACY' identifies the basis on which the line was mapped; 'schematic' (where the landform feature is sharply defined in a topographic sense, and thus the line denotes the general presence of a feature, not an exact location) and 'approx-lidar' (the feature is identifiable topographically in lidar data, but it is not mapped in fine detail). 'TYPE' identifies the nature of the mapped feature; only two types of feature are mapped, 'edge high ground' (indicating the crest of a slope between higher ground and lower ground), and 'terrace edge' (the approximatelocation of a step between a higher and a lower river terrace). The line is positioned at about the lower side of the step.Thisdatasethasbeen compiled for presentation at a scale of 1:35,000, but the data were captured at more detailed scales. The landform feature lines were mapped on-screen at a scale of approximately 1:10,000, and are considered to be accurate to about +/- 30 m. The accompanying report is Barrell, D. J. A.; Van Dissen, R. J. 2014. Assessment of active fault ground deformation hazards associated with the Ashley Fault Zone, Loburn, North Canterbury, GNS Science Consultancy Report 2013/173 / Environment Canterbury Report No. R14/77(Figure 2).",
 "summary": "",
 "title": "Ashley Fault Zone landform feature lines 2014",
 "tags": [],
 "type": "",
 "typeKeywords": [],
 "thumbnail": "",
 "url": "",
 "minScale": 0,
 "maxScale": 0,
 "spatialReference": "",
 "accessInformation": "Mapping by D.J.A. Barrell, GNS Science, 2014.",
 "licenseInfo": ""
}