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ASRIS Technical Specifications V1.6

ASRIS Technical Specifications V1.6

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agglomerative approach. Furthermore, different criteria for mapping emerge at these more generalizedlevels and many of the criteria used at lower levels lose significance (and vice versa).In <strong>ASRIS</strong>, tracts at levels 1–2 delineate regions comprised of contiguous land units rather than multipleinstances of the same land-unit type. This is necessary for cartographic efficiency at broad scales.Table 3: The spatial hierarchy of land-unit tracts (after Speight 1988). Note that the database design for <strong>ASRIS</strong>allows intermediate Levels to be characterized (e.g. a System with a characteristic dimension significantly less that100 m would be designated as Level 5.1 or 5.2 in the hierarchy)LevelOrder ofland-unittractSpeightCharacteristicdimensionDescriptive or defining attributes0 Division 300km 30 km Broad physiography (slope andrelief) and geology1.0 Province 100 km 10 km Physiography, water balance,dominant soil order and substrate2.0 Region 3 km Physiography, regolith materials,age of land surface, waterbalance, dominant soil suborderAppropriate map scale1:10 million1: 2.5 million1:1 million<strong>ASRIS</strong> Mapping HiatusLevels above are based on subdivisions of the continentLevels below are aggregated from surveys.3.0 Zone 30 km 3 km Groupings of geomorphicallyrelated systems4.0 District 5 km 1 km Groupings of geomorphicallyrelated systems1:1 million1:250 0005.0 System 600 m 300 m Local climate, relief, modal slope,single lithology or single complexof lithologies, similar drainage netthroughout, related soil profileclasses (soil-landscape*)1:100 0005.1 100 m As for Level 5 1:25 0006.0 Facet 40 m 30 m Slope, aspect, soil profile class 1:100006.1 10 m 1:25006.2 3 m 1:10007.0 Site 20 m 10 m Soil properties, surface condition,microrelief* Thompson and Moore (1984)rarely mapped inconventional survey12

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