June 1, 1974
A new method for ordering archeological deposits, called the minimum path length method, is introduced and discussed in relation to previous work on the problem. Among it's advantages are easy computability, independence of input order, and minimization of reasonably intuitive function of the similarity matrix. Also when the similarity matrix is a Robinson matrix, (which is 'perfect' data for this problem) the minimum path length permutation yields the Robinson order (which is the 'correct' order for a Robinson matrix.)
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