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The calibration and test phase of the latter relied on morphometric conditions derived by terrain analyses of a digital elevation model as well as on geology and land use from thematic maps.
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Results of the digital terrain analyses further suggest that the ridges and mounds in the west and south-west of the study area are remains of the Pleistocene deposits and that the tells in the foreland - like Bubastis - witness the erosion history.
Identifying areas prone to salt accumulation by means of geomorphometry (i.e. terrain analyses using digital elevation models (DEMs)) can potentially save time and costs.
Insights into the formation of glaciated landscapes can, in principle, be obtained by analysing modern ice-sheet beds, but terrain analyses beneath modern ice sheets are restricted by the inaccessibility of the bed.
Exact position and analyses of parameters are computed in the digital models of terrain.
Analyses of Otzi's bones suggest that his lifestyle was far from sedentary and included long walks over hilly terrain.
The terrain consists of rolling hills.
Much of the terrain consists of rock deserts.
The terrain dimensions specified in the graph as "Terrain 2500" implies a terrain dimension of 2500 × 2500 square meters.
The terrain south of Ioannina provided excellent defensive ground.
Examination of the resulting highest-resolution imagery reveals at least five different types of terrain, including several regions of cratered terrain, regions of smooth (young) terrain, and lanes of ridged terrain often bordering the smooth areas.
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