Applied geophysics, EOS, UBC.

A)
B)
C) D)
From An introduction to applied and environmental geophysics, J. M. Reynolds, 1997.

Examples of contouring different patterns of data. (A) shows a set of radial lines, and (B) an even grid of data, both with 114 points per square kilometre. (C) has far too few data points unevenly spread over the same area (23 data points per square kilometre). The results are seriousl "aliased" - ie spacial information obtained is "wrong". (D) shows the result of contouring an even grid of 453 data points per square kilometre. The contours are lines of constant total magnetic field strength (in nanoteslas). The data are from a ground magnetometer investigation of north-west Dartmoor, England.