In the spring and summer of 1934 age determinations were made of a considerable number of southern short leaf pine trees, Pious echinata Miller, in Howard County, southwestern Arkansas. In the stony foothills of the Ouachita Mountains three areas of locally-designated virgin pine were studied and in each there existed a certain uniformity of age of trees that contrasted with true virgin stands, in which a wide and even distribution of age classes is usually found. The following is a table showing the age distribution of all trees on designated numbers of one-fourth acre plots. Table I shows that 68.57 per cent of the stand in area A became established in the nine year period between 1858 and 1867; similarly in area B, 63.16 per cent of the stand in the ten year period between 1812 and 1822, and in area C 85 per cent in the fifteen years from 1772 to 1787. The percentage of stand which came in before these periods is area AX 8.57; area B, 8.27; and area C, 5.0. Trees coming in after the periods made up the following percentage area A, 22.86; area B, 28.57; and area C, 10.0. In all three instances the closing of the period of intensive reoccupation was not as sharply marked as the beginning. It is known among southern foresters and lumbermen that purity of composition and uniformity of age in pine forests are the usual indicators of an old field stand, or the consequence of some catastrophe that wholly annihilated the previous plant cover. This is to say, a denuded area which is edaphically favorable, and which has seed-trees near, is soon seeded to pine and within the span of a few years a plant cover develops which for the most part resists further invasion of both hardwoods and members of its own species. From the foregoing data the natural inference is that some catastrophe destroyed practically all the forest in areas designated A, B, and C near the years 1857, 1811, and 1770 respectively. As enumerated above, certain seedlings and some older trees escaped. There followed a certain period in which the areas were intensively reoccupied by a growth of pine, followed in turn by a longer period during which a greatly diminished number of trees came in at irregular intervals. Hence the present stand is composed of three hypothetical classes, (1) older trees of the original stand and (2) seedlings that survived, and (3) reproduction following the disaster.