For contouring the relief of small palaeontological or sedimentologica
l objects the method of Shadow Moire Topography, already successfully
applied in other fields, is recommended. When a whitened three-dimensi
onal object is seen or photographed through a grating and the illumini
ng light bundle passes through the same grating, equidistant planes of
shadow can be produced. The latter generate contour lines on the obje
ct where they intersect its surface. The theory of Shadow Moire Topogr
aphy is explained by the principles of geometric optics. A simple and
cost effective apparatus is proposed and examples of contoured objects
are figured.