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World Environmental and Water Resources Congress 2017                                                    402




               "admirable  in  conception  and  outline"  in  their  report  released  during  the  fall  of  1906.  Few
               engineers dared to criticize the project after the panel's review was released, due in large part to the
               clout and credibility of John R. Freeman, one of the principal consultants for New York’s New
               Croton Aqueduct.

               Final Plans and Construction. The aqueduct intake was intended to divert water from the Owens
               River at a pair of headgates about 12 miles north of Independence, at an elevation of 3714 feet (Fig.
               4). Whenever Owens Lake filled to capacity, the overflow continued southward, sculpting the lower
               Owens Gorge, intermittently flowing through Rose Valley, across a series of lava dams at Little
               Lake, into Indian Wells Valley, which contains China Lake at its eastern end. It was in this channel
               just above the lower Owens Gorge waterfalls that Mulholland decided to build the principal storage
               and regulation reservoir, known as Haiwee Dam and Reservoir (Fig. 5). With a storage capacity of
               almost 60,000 acre-feet, Haiwee controlled discharge entering the covered sections and sag  pipe
               crossings between the Owens Valley and Mojave.































               Figure 4. Profile of the Los Angeles Aqueduct, between Loing Valley Dam/Crowley Lake (A)
               and Sawtelle (14), just north of the downtown area (LOC-HAER).

                       From its intake north of Independence south to Haiwee the aqueduct was constructed mostly
               as  an  open  channel.  South  of  Haiwee  the  Owens  Valley  narrows  and  the  crosses  increasingly
               rugged country. In this area most of the aqueduct was built as a cut-and-cover box channel. The
               flatter  sections  were  excavated  using  rail-mounted  steam  shovels  and  immediately  lined  with
               concrete. This system advanced at an average rate of about four miles per month. The life blood of
               the project was a standard gage rail line constructed by the Southern Pacific Railroad between May

               1908 and October 1910, extending northward from Mojave to the Owens Valley. 320,000 tons of
               construction hardware would be carried along this line before the aqueduct was finished.
                       More than a million barrels of Portland cement was needed to line the canals, tunnels and
               cut-and-cover sections. J. B. Lippincott (1913) engaged in some local geologic studies and discov-








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