6 Nev. 393 | Nev. | 1871
By the Court,
In the years 1858 and 1859, one J. H. Rose appropriated a certain quantity of water from the Carson River, by diverting the same for mining purposes, to be used some four miles below the point of diversion. The water thus diverted was conducted to the locality where it was used by means of a ditch and flumes. In the year 1860, the grantors of the respondent also appropriated water from, the river, diverting it at a point below the head of the Rose ditch, and using it as motive power for a quartz mill. In the winter of 1861 this ditch was improved and enlarged; and again it is claimed by appellants that it was very much enlarged in the year 1865 — a fact important to be determined in the case, for the reason that in the year 1862 the Rose ditch was also greatly enlarged ; hence, although admitted that these appellants as the suc
The Court below found the capacity of the flume, just below the head of the Rose ditch, and which seems to be admitted was the point of smallest capacity, to be four and forty-eight one hundredths cubic feet per second, being the quantity capable of being carried by a flume twenty by eighteen and three-fourths inches, on a grade ■ of one-eighth of an inch to the rod. We have not been able to find testimony in the record, sufficient to sustain this conclusion. The •only persons who appear to have testified respecting the dimensions and grade of this flume were Rose, Hunt, Rosenbecker and Chapin. As to the size of the flume in question, the finding that it was twenty by eighteen and three-fourths inches is, perhaps, sustained by the testimony; but there appears to be no evidence directly ■sustaining the finding that its grade was only one-eighth of an inch ■to the rod. Rose himself swears that the ditch had a grade of
Hunt testified that his survey showed the general grade of the old Rose ditch to be about two and seven-tenths feet to the mile. The general grade of the ditch may very well have been as stated by Hunt, and still the grade of the various flumes have been more than that. It is not claimed that he testified to the grade of the flume in question, or any flume specially ; and it is perfectly manifest the grade of the flumes was greater than that of the ditch. So Hunt’s testimony need not and does not necessarily conflict with the other evidence showing the flumes to have been upon a grade of one half inch to the twelve feet, or more. Chapin’s testimony goes only to the dimensions of the long flume, a fact which we accept as found by the Court below. The witness Rosbnbecker swears positively that the grade -of the flumes in the Rose ditch was three-eighths of an inch to the rod; and he also swears that there was no flume in the ditch of less grade. The witness testifies that he measured the flume in question and took its grade. Hence, his testimony was based upon no conjecture or speculation, but upon actual measurement. This evidence, together with that of Rose, is not — as we interpret it — directly contradicted by any witness or any calculation presented in the record. And as their testimony makes the capacity of the Rose ditch much larger than the Court found it to be, we are compelled to set aside that finding, and award a new trial.
Our conclusion upon this point renders it unnecessary to make any inquiry as to the relative capacity of the respondent’s ditch of 1862, and that now used by it.
New trial ordered.