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<br />Table 1. Diaries from historical river trips in Grand Canyon used in this study. <br /> <br />Date ofTrip Author Part of Canyon Source of Material <br />1951 S. Reilly Lees Ferry to Phantom Unpublished diary <br />1952 F. Wright All Unpublished diary <br />1953 P.T. Reilly All Unpublished diary <br />1953 F. Wright All Unpublished diary <br />1953 G.White All Unpublished diary <br />1954 O. Marston All Unpublished diary <br />1954 G. White All Unpublished diary <br />1955 P.T. Reilly All Unpublished diary <br />1955 F. Wright All Unpublished diary <br />1956 P.T. Reilly All Unpublished diary <br />1956 F. Wright All Unpublished diary <br />1957 P.T. Reilly Lees Ferry to Phantom Unpublished diary <br />1957 F. Wright All Unpublished diary <br />1958 P.T. Reilly Phantom to Lava Falls Unpublished diary <br />1959 P.T. Reilly Lees Ferry to Pipe Creek Unpublished diary <br />1962 P. T. Reilly All Unpublished diary <br />1964 P. T. Reilly All Unpublished diary <br /> <br />knowing full well that Bedrock had and Dubendorff <br />had not. The Old Timers correctly recognized the <br />changes in Bedrock Rapid and the lack of change in <br />Dubendorff. By listening to the answers, we <br />established the credibility of the Old Timers as very <br />high in remembering specific and detailed information <br />about changes in Grand Canyon. We also established <br />that differences in water level between the pre-dam era <br />and the Old Timer's Trip was extremely important to <br />their memory of specific sites. Several did not <br />remember the debris bars at Vaseys Paradise and the <br />mouth of the Little Colorado River. These bars may <br />have changed significantly, but both bars may have <br />been covered with water when some of the Old Timers <br />passed them. <br />Some observations may seem trivial or <br />unremarkable. For example, the large invasion of non- <br />native tamarisk is generally recognized by scientists <br />and river runners alike (Turner and Karpiscak, 1980; <br />Stevens, 1989). On the other hand, tamarisk was <br />advancing its distribution before Glen Canyon Dam <br />was built and the rate of its spread is little known (see <br />Graf, 1978). Because of such subtleties, we include the <br />full set of observations. Other changes noted by the Old <br />Timers, particularly those concerning wildlife, are <br />probably inconclusive, a consequence of limited <br /> <br />observations and lack of independent scientific <br />verification. We include them anyway, albeit with <br />appropriate caveats, to spur discussion. <br /> <br />SPECIFIC CHANGES OBSERVED IN <br />GRAND CANYON <br /> <br />Aesthetics in Grand Canyon <br /> <br />The aesthetics of river trips were a common <br />theme among the Old Timers. Some, particularly <br />Sandy Nevills Reiff and Joan Nevills Staveley, <br />commented on how clean the canyon is now. Their <br />most recent canyon experiences were just before the <br />current policy of cleaning up trash and hauling human <br />waste from campsites. When they did most of their <br />trips from the late 1950s to the early 1970s, human <br />waste and garbage were buried in sandbars. Others <br />found the noise of aircraft overflights to be oppressive <br />compared to the noise from the rare airplane that <br />passed over the canyon in the pre-dam era. . <br />Several Old Timers missed the effects of a sllt- <br />laden river on the quality of the river trip. In particular, <br />they missed the sound of sand scraping on the sides and <br />bottoms of boats. The waves in rapids appeared to be <br />different; the pre-dam sediment-laden waves appeared <br /> <br />SPECIFIC CHANGES OBSERVED IN GRAND CANYON 7 <br />