''Helioseismic tomography'' is a method using observations to construc
t slices of the Sun's internal structure. It is based on a reduction o
f observations to time-distance surfaces and hypersurfaces. We present
a procedure for measuring time-distance surfaces and hypersurfaces, a
nd thereby a method of studying localized inhomogeneities in the inter
ior of the Sun, such as abnormalities in the sound speed (e.g., a ther
mal shadow, Parker 1987a), or local subsurface flows, or magnetic fiel
ds. We also present a simulation of measuring time-distance surfaces a
nd illustrate how to measure the size of an inhomogeneity, its locatio
n in depth, and the deviation of its sound speed compared to its local
surroundings.