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29 <br />7 adnd bark formation must indicate that the plant is old with respect to others in <br />the vicinity. With two exceptions, plants that were aged were from below the <br />historic flood line. All cuts were made completely through the trunk within six <br />inches of the ground surf ace. <br />At Big Joe Rapids on the Yampa River, 17 plants were cut and aged. Three <br />distinct terraces were observed here at low water, each having established <br />tamarisk plants. Plants were cut from all three terraces. It was hoped that <br />from this collection a correlation could be established between stem diameter <br />and age, and therefore an effort was made to collect a range of diameter sizes <br />from this site. Otherwise, the criteria for selection and the method of cutting <br />were the same as for the Green. <br />Comparative Photographs <br />Two types of comparative photographs were used, recent and historic. The <br />recent photo pairs were taken as color slides and show the same location in <br />June and September (high and low flood stages) of the study period. Only <br />the Yampa River was included in this aspect of the study. <br />Historical photographs from the Monument library included all river <br />corridors but the majority were from the Canyon of Lodore. The oldest were from <br />the 1871 Powell expedition taken by E.O. Beaman and J.K. Hillers. The photo <br />stations of this collection were relocated and rephotographed in 1969 by E.M. <br />Shoemaker and H.G. Stephens (1969, 1975) for the US Geological Survey. Thus in <br />some cases, we were able to produce a series of three comparative photos for a <br />single location. All historical re-photos were taken as 35mm black-and-white. <br />Many of the 1871 and 1969 photographs were taken with a wider angle lens than we <br />had available. When we were unable to incorporate the entire field of view of <br />the older photograph, our interest was in the portion showing vegetation along <br />the river. <br />