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@@ -168,7 +168,33 @@ of aspect categories is very uneven, with peaks at 0, 45,..., 360 categories.
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When working with floating point elevation models, no such aspect bias occurs.
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-<h2>REFERENCE</h2>
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+<h2>EXAMPLES</h2>
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+
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+In this example a slope, aspect, profile and tangential curvature map
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+are computed from an elevation raster map (North Carolina sample
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+dataset):
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+
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+<div class="code"><pre>
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+g.region raster=elevation
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+r.slope.aspect elevation=elevation slope=slope aspect=aspect pcurvature=pcurv tcurvature=tcurv
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+
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+# set nice color tables for output raster maps
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+r.colors -n map=slope color=sepia
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+r.colors map=aspect color=aspectcolr
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+r.colors map=pcurv color=curvature
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+r.colors map=tcurv color=curvature
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+</pre></div>
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+
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+<center>
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+ <img src="r_slope_aspect_slope.png" border="0">
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+ <img src="r_slope_aspect_aspect.png" border="0">
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+ <img src="r_slope_aspect_pcurv.png" border="0">
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+ <img src="r_slope_aspect_tcurv.png" border="0">
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+ <p>
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+Figure: Slope, aspect, profile and tangential curvature raster map (North Carolina dataset)
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+</center>
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+
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+<h2>REFERENCES</h2>
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<ul>
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<li> Horn, B. K. P. (1981). <i>Hill Shading and the Reflectance Map</i>, Proceedings
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