{"help": "https://uatweb.datansw.links.com.au/data/api/3/action/help_show?name=package_show", "success": true, "result": {"author_email": null, "creator_user_id": "8d2ac61a-d63a-4456-a00d-b35fee4c4025", "id": "04805525-8f42-4aaa-8539-57ff3becc9a2", "isopen": false, "license_id": "oeh", "license_title": "OEH licence", "maintainer": null, "maintainer_email": null, "metadata_created": "2025-10-08T05:54:18.668731", "metadata_modified": "2025-10-08T05:54:18.668738", "name": "rm-test-11-nov-2016", "notes": "__Lorem ipsum dolor sit amet,__ consectetur adipiscing elit, sed do eiusmod tempor incididunt ut labore et dolore magna aliqua. Ut enim ad minim veniam, quis nostrud exercitation ullamco laboris nisi ut aliquip ex ea commodo consequat. Duis aute irure dolor in reprehenderit in voluptate velit esse cillum dolore eu fugiat nulla pariatur. \r\n\r\nThe Soil Regolith Stability classification is used in the assessment of soil water erosion and water pollution hazards. It is currently in use as part of the EPA 1998/99 Pollution Control Licences within state forests. \r\nThis map identifies soil regolith stability classes using linework and soil information from published soil landscape mapping and reconnaissance soil landscapes of Northern and Southern Comprehensive Regional Assessment (CRA) mapping projects.  \r\nEach soil landscape unit on the coverage has been allocated a regolith stability classification (soil erodibility), comprising of four classes:\r\n\r\n* class R1 \u2013 High coherence soils with low sediment delivery potential\r\n* class R2 \u2013 Low coherence soils (when wet) with low sediment delivery potential\r\n* class R3 \u2013 High coherence soils with high sediment delivery potential\r\n* class R4 \u2013 Low coherence soils (when wet)\r\n\r\nA regolith stability classification consists of a dominant class and up to three sub-dominant classes (if necessary), for example, R1(R3,R4), where R1 is the dominant regolith stability class 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