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This is an action of trespass in which the defendant is charged with having stripped the bark from a large number of trees growing on plaintiff's land, described as lots 1, 3, and 4, in section 31, township 5 south, range 2 east, Humboldt meridian, and the southwest quarter of the southeast quarter of section 30 of the same township. The shaded portion of the accompanying map shows the position
of these lots in their relation to each other as well as in relation to the township lines and the principal natural objects and artificial monuments delineated and noted on that portion of the official map of the township survey, to which reference must be had in construing the patent and determining the location of the land. The plaintiff, as successor in interest to the original patentee, is the unquestioned owner of the lots of land thus delineated and described, and the only serious question in the case is as to their real boundaries on the ground. Whether, in other words, the stripping of the bark, which is not denied, was done upon plaintiff's land or upon other subdivisions of the said section 31, or in an adjoining section. The plaintiff succeeded in convincing the jury that the defendant had trespassed upon his land, and was awarded damages in the sum of five thousand dollars. The appeal by the defendant is from the order of the superior court overruling his motion for a new trial.
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The cause was first submitted in Department, where the order of the lower court was affirmed. The opinion then rendered contains a very full and generally satisfactory discussion of numerous alleged errors in the rulings of the superior court upon objections to evidence, and in the instructions given to the jury, and with a few trifling exceptions, hereinafter noted, is here readopted as to those points. The rehearing, indeed, was granted only because we desired to consider more carefully the question whether the verdict of the jury was supported by the evidence, or to state the question more specifically, whether the plaintiff's land was correctly located by the survey upon which he rested his case. With the opportunity of examining and comparing the voluminous and somewhat confusing evidence contained in the record, in the light of the additional argument on that point, we are convinced that the location contended for by plaintiff, and upon which his case depends, was not correctly made, and that in this respect the verdict of the jury is wholly unsupported.
In disposing of its public lands the government causes them to be laid off into townships six miles square, bounded by meridian lines on the east and west and by parallels of latitude on the north and south. This, at least, is the ideal township, but owing to faulty location of the boundary lines or to proximity to the seacoast, or to both causes, as in this case, and to the convergence of meridian lines — as in all cases — a township never contains thirty-six sections each exactly a mile square, into which they are supposed to be divided. The rules for making the subdivisional surveys, however, are well understood, and there is a uniform method of numbering and designating the sections and their smaller subdivisions, of all of which matters the courts take judicial notice. Section 31 is at the southwest corner of the township, next on the east is section 32, and so on to section 36 at the southeast corner. We also take judicial notice that under the laws of the United States and the regulations of the land office no sales of public lands are made until the plat and field-notes of the subdivisional survey of the township in which they lie have been returned and approved, and that the patents issued to purchasers describe the lands patented as they are delineated on the approved plat — which remains a public record in the office of the surveyor-general, and copies
of which, officially certified, are deposited in the local land office. We also know that it is made the duty of the surveyors employed to make these subdivisional surveys to mark the section corners with posts properly lettered, or other monuments, and also the intersection of quarter-section lines with the section lines, and more especially to preserve accurate field-notes of their surveys showing the natural features of the country, such as streams, mountain ridges, the ocean shore, nature of the soil, whether barren or fertile, wooded or meadow; distance and bearing of witness-trees from section and quarter-section corners, etc.
These field-notes are, like the township plat, preserved in the office of the surveyor-general as a public record, and their principal purpose is to enable the purchasers of public lands and their successors to correctly relocate the section and quarter-section corners within the township when by accident or design the artificial monuments placed by the official surveyor have been removed or destroyed, — a very common occurrence, as the records of this court and the decisions of other courts abundantly prove.
And so in this case, when the plaintiff came to the conclusion that the defendant was collecting tanbark by stripping his trees, he found himself under the necessity of employing a private surveyor to find the corners of section 31, in which his land is situate. The evidence offered by him at the trial (the map and field-notes of the official surveyor) shows that these corners, as well as the quarter-section corners, were marked by posts or other monuments, properly lettered at the time of the survey, and many of them identified by the distance and bearing of witness-trees as well as by their relation to the shore of the ocean, the stream known as Whale Gulch, and the crest of the high ridge dividing that stream from the ocean. There is no evidence in the record that any search was made for the corner posts or witness-trees, which, if found, would have ended the question as to the true location of plaintiff's land. But assuming that the proper effort was made to find the corner posts and witness-trees, and that it was fruitless, the most obvious alternative was to trace the township line to its intersection with the line of ordinary high tide on the ocean shore, — that being the southwest corner of the township, — then measure 1.80 chains east from that point
and thence twenty chains north for the southeast corner of plaintiff's land, thence eighty chains on the same course for the northeast corner, thence twenty chains west for its northwest corner, thence south to the ocean shore, thence along the shore to a point due west of the southeast corner, and then close upon that.
This, indeed, is precisely what plaintiff's surveyor (Chapman) undertook to do, but did not do. There is a very serious question in the case, whether he ever found the line which bounds the township on the south. He places it in utter disregard of the field-notes and plat of the official survey, which he had in his hands and assumed to follow. But conceding for the moment that he may have found the true south boundary of the township, his method of tracing it to the ocean and his views as to what constitutes the shore of the ocean are most peculiar. The township plat and the field-notes of the official surveyor show that the trend of the ocean shore is from northwest to southeast for many miles north and south of the township line; that east of the ocean shore at a distance of 86.20 chains this line intersects a small creek (Whale Gulch) which flows south and empties into the ocean about one mile south of that point. Between this stream and the ocean is a high ridge rising from the shore at a very steep angle for a distance of 25.80 chains, more gently for about fourteen chains further and thence descending somewhat less abruptly than on the ocean side to Whale Gulch. Chapman, in order to find the intersection of the township line with the ocean shore, went over into Whale Gulch where he discovered an "Old Settler" who pointed out to him the quarter-section post on the south line of section 32. This corner, which, according to the plat and field-notes, ought to have been found twenty-five chains west of Whale Gulch, was at some distance east of that stream, but the "old settler" showed him a line indicated by "old blazes" on trees which led him to what he assumed to be the quarter-section corner, and having by this remarkable process located the quarter-section corner in defiance of the official plat and field-notes, he immediately falls back upon the same field-notes for the purpose of locating the ocean shore. They tell him that this quarter-section is 61.80 chains east of the shore, and therefore, of course, he has only to go that distance west from the
corner to find himself on the beach. He accordingly goes due west to a point exactly on the crest of the ridge which divides the watershed of the ocean from that of Whale Gulch, and, having measured the distance, finds that, by a happy coincidence, he is just 61.84 chains west of the "old settler" corner, and knows, therefore, that he is at the ocean shore, or, to be strictly accurate, that he is four links beyond it. Here, again, he forgets his field-notes, which tell him that this ridge is at least 25.80 chains east of the shore line on the southern boundary of the township (and its summit, judged by the angle of ascent, about eight hundred feet above the sea-level). He is not, however, daunted by a trifle like this, but plants his post to mark the southwest corner of the township right on the "crest of the ocean" or the "cone of the ocean" according to his own varied and picturesque terminology. Having fixed this point, the rest of his task is easy. He has only to measure twenty chains north and 1.80 chains east, to find the southeast corner of plaintiff's land; thence north eighty chains, west twenty chains, south to the intersection of a meander line somewhere east of the shore line, thence with its meanders to a point due west of the southeast corner and east till he closes on that point. This he proceeds to do, and the result is he has located plaintiff's land on the eastern slope of the ridge in Whale Gulch, when the field-notes of the official surveyor show that not only those subdivisions of section 31 belonging to plaintiff, but the whole section, extending twenty chains further east, are on the western slope of the ridge, looking down upon the ocean. And, of course, no portion of it touches the ocean shore, or comes any nearer the ocean shore than a point 1.80 chains east of the summit of the ridge. Mr. Chapman reconciles this discrepancy by assuming that the shore line of the township is coincident with the meander line by which it was measured, and he gratuitiously assumes that the meander line was run along the summit of the ridge. There is not in the whole record any credible evidence to show that the meander line was so run, and in the absence of testimony the presumption is that it was run along the beach, if the beach was passable, and, if not, by some other method that would enable the surveyor correctly to locate the line of ordinary high tide, — that being the line to which the public surveys extend. There is no evidence that the beach north-ward
from the township line is impassable at any point, while it does affirmatively appear that south of the township line as far as the mouth of Whale Gulch it is passable, and that the same government surveyor (Perrin) who measured the west boundary of section 31 north of the line, also measured south as far as Whale Gulch, and that his measurements were made along the beach. Besides, the meander line is not itself the shore line. It is only a means of measuring and correctly locating the shore line. The survey itself extends to the line of ordinary high tide, and all the land included within that line passes to the patentee of the subdivisions shown to be so bounded by the township plat. Mr. Kimball, therefore, owns to the ocean shore on the south half of his claim. Nothing can stop him short of that natural boundary. Not even the government can come between him and the actual shore line. If, therefore, Mr. Chapman's survey is to prevail, he has made the plaintiff a present of a strip of land extending a half mile along the shore and as wide as the distance between the line of ordinary high tide and the summit of the dividing ridge between the ocean and Whale Gulch. And in doing this he has deprived plaintiff's coterminous owner on the east of a strip of equal width and a whole mile in length. I have said that there is no credible evidence to support the claim that the meander line of the seashore was run along the summit of the ridge. There was, on the contrary, conclusive evidence in Mr. Chapman's hands, at the time he chose to make that assumption, that it was not so run. He had the field-notes of Perrin, who ran the meander line of the shore to the township line and the township line eastward from the ocean as far as the quarter-section corner in section 34. He had also the field-notes of Foreman, who made the official subdivisional survey of the township, and whose field-notes of the township line correspond exactly with Perrin's, — one (Perrin) measuring from the west, and the other (Foreman) measuring from the east. Now, take Perrin's notes, commencing at the end of his meander line which was run for the sole purpose of locating the township line at its intersection with the ocean, they read as follows: —
"East, of corner, Tp. 5 s., R. 2 E., H.M. set post 4 ft. long, 4x4 in mound of rock 4 ft. base, 2 ft. high.
Cor., fractional sec. 31, from which cor. I run East on south boundary sec. 31.
Varia. 17 degs. 35 min. East.
Ascending steep rocky sides.
21.80 Set post 4 ft. long, 4x4 in mound of rock 8 1/2 ft. base 2 ft. high, cor., Secs. 31 and 32 land rough and broken.
Soil 3rd. rate, rocky.
February 14th, 1876.
East, on south Boundary Sec. 32.
Vari. 17 degs. 35 mins. East.
Ascending steep rocky side
4.00 Top of slide and enter grassy opening
18.00 Ridge bears N.W. S.E.
19.00 Enter brush
26.00 timber.
40.00 Mark leaning Madrona 10 in., dia. for 1/4 sec. cor. from which a madrona 8 ins. dia., bears N. 18 deg. W., 46 lks. dist. a tan oak 8 ins. dia., bears S. 30 degs., W. 37 lks. dist. 64.40 Stream in deep gulch 10 links wide course South." Etc.
It will be observed that to mark the southwest corner of the township he sets his post not at, but east of, the corner, and this, for a reason sufficiently obvious. Set at the line of ordinary high tide, it would have been exposed to the wash of every spring tide, and with its mound of stones would have been obliterated by the first storm. Set east of the corner it exactly indicated the point of intersection of the shore and township lines — the true southwest corner of the township. Having thus established this corner, he proceeded to lay out the township line to the eastward. If he understood his duty (and a public officer is presumed not only to know, but to perform, his duty), he commenced his measurement at the true shore line, which is, indeed, the proper construction of his notes; for that corner of the fractional section 31 coincides with the southwest corner of the township. Wherever one is, the other necessarily is, and the notes clearly show that he ran east from the corner and not from the post which he set on the line east of the corner. But if it were conceded that he commenced at the post, and not at the corner, it would only be so much the worse for Mr. Chapman's deductions. Instead
of bringing the true shore line nearer to the summit of the ridge, it would put it farther away, by just the distance between the corner and the post. From whichever point he measured he found that it was 21.80 chains to the common corner of sections 31 and 32, and at least four chains farther, on any construction of his field-notes, to the summit of the ridge, where Chapman takes the liberty of locating the ocean shore, and where he found some scattered stones, which he concludes are the remains of the mound erected by Perrin to mark the southwest corner of the township. Enough has been said, I think, to demonstrate how absurdly fallacious were the means resorted to by Chapman for locating the shore line of the ocean, — a natural monument that locates itself, — how gratuitous his assumption that the meander line was traced along the top and sides of a lofty ridge more than a quarter of a mile from the beach, and how inconsequential that fact would have been if it had been a fact.
Having no guide for the location of that part of the township line except the field-notes of Perrin and Foreman, which exactly agreed as to such conspicuous natural monuments as Whale Gulch, the summit of a high ridge, and the ocean shore, he discards all these, in his search for a starting-point, in favor of a stake pointed out by an old settler, more than a quarter of a mile from the place indicated by the natural monuments, and not otherwise identified, than by a line of "old blazes on trees," — a kind of mark not mentioned in any surveyor's field-notes, and not explained or given any significance by his own testimony or that of any other witness. The genesis of this "old settler" corner will be shown when we come to consider the York survey, evidence of which was introduced for the purpose of corroborating Chapman, and it will appear to be an extremely frail foundation for the structure that has been reared upon it. At this point it is sufficient to say that Chapman, by adopting it as the basis of his survey, has made a location of plaintiff's land which utterly falsifies every important feature of the official survey which it was his duty to follow. An instance of its discrepancies not before mentioned is the distance on his line, according to his estimate (he did not take the trouble to measure it) between Whale Gulch and the seashore. He testifies that it was not more than five chains from his post on the ridge down
to the ocean, and only ten chains in the opposite direction to Whale Gulch, making the total distance only fifteen chains. Foreman's field-notes and the approved plat show the true distance to be 86.20 chains. If his estimate of the distance is even approximately correct, his line must have been run within a quarter of a mile of the mouth of Whale Gulch — three quarters of a mile south of the true line as platted on the township map. It is probable, however, that he greatly underestimated the distance from the summit of the ridge to the ocean, for the shorter the distance the less the absurdity of making the summit the ocean shore. And all plaintiff's other witnesses on this point exceeded his estimate, one placing the distance at twelve hundred feet or over. If this witness was correct, Chapman's survey locates plaintiff's land a quarter of a mile away from the ocean, which by the official survey is the western boundary; if Chapman was correct his township line was located much too far south.
I have thus far discussed Chapman's survey with sole reference to the field-notes (Perrin's and Foreman's) by which he professes to have been guided. He had, it is true, the field-notes of another surveyor (Glover), but since his survey was altogether east of section 33, they did not touch section 31 or section 32, and could not possibly have aided Chapman at this stage of the proceedings. But after he had completed his survey of plaintiff's land by measuring it off and setting boundary posts at the corners and along the sides, he made a survey for another party to locate the southeast quarter of section 34, and in that connection ran some lines and made some measurements from one of Glover's corners which are supposed to corroborate the survey he made for plaintiff.
For the purpose of considering this part of plaintiff's case, it is necessary to give a brief outline of the proceedings of three official surveyors employed at different times in the survey of township 5 south, range 2 east, Humboldt meridian, and two adjoining townships. The history of these surveys is plainly written upon the face of the township plats, and in the field-notes from which they were compiled, copies of which were introduced in evidence by the plaintiff. Bearing in mind that in laying off townships to the east of the Humboldt base and meridian, those in range 1 east were naturally marked out before those in range 2, and that the meridian
line bounding range 1 on the east became necessarily the western boundary of range 2, it appears that this common boundary was established by the official survey of S.W. Foreman in 1874. By his survey, it was found that the length of the township line from the northeast corner of township 5 south, range 1 east, to the Pacific Ocean was three hundred and eighty-five chains, or, in other words, ninety-five chains short of six miles, and the plat shows that the established common corner of the two townships on the shore line (the southeast corner of 1 and southwest corner of 2) was just sixty-five chains south of the southeast corner of section 24 of township 5 south, range 1 east, Humboldt meridian.
In 1876, another surveyor (George H. Perrin) was employed to complete the subdivisional survey of township 24 north, range 19 west, Mt. Diablo base and meridian. The north boundary of this tier of townships in the Mt. Diablo system did not quite coincide with the south boundary of township 5 south of the Humboldt system. It seems that there was a space between them, and that Perrin was instructed to locate the south line of township 5 south, range 2 east of the Humboldt system in order to close his survey of township 24 north, range 19 west of the Mt. Diablo system upon that line. The method adopted by him for locating the southern boundary of township 5 south, range 2 east, was to start from the southern extremity of its western boundary at its intersection with the shore line of the ocean, and meander that line to a point ninety-five chains south of his starting-point. This was a perfectly correct method, and, since his measurements seem to have been carefully made, would have yielded a correct result if, unfortunately, he had not mistaken his proper starting-point. He commenced his meander line a little more than twenty chains south and a little less than forty chains east from the right point, and in consequence placed the township line a quarter of a mile too far to the south, and added a half mile to the west border of the township. The subdivisional survey subsequently made shows this. By reference to the map it will be seen that the western tier of sections (18, 19, 30, etc.) are thirty-eight and a fraction chains over a mile in width from east to west, and the common corner of sections 19 and 30 in 2 east, instead of coinciding with the common corner of sections 24 and 25 in 1 east, are
20.60 chains south of it. This mistake of Perrin's seems to have been the occasion of much of the confusion which has since arisen. He, however, unconscious of his error, proceeded to lay off the township line from the southern extremity of his meander line as far east as the quarter-section corner of section 34, and it is the field-notes of this survey to which reference has heretofore been made.
About a year after the completion of Perrin's survey of the township line, as far as the quarter-section corner in section 34, another surveyor (J.R. Glover) seems to have been employed to continue that survey and establish the township line as far as the southwest corner of township 5 south, range 5 east. At all events, that is what he assumes to have done, as appears by a copy of his field-notes certified by the surveyor-general. But there is no evidence that any subdivisional survey was ever based on this survey of the township line. It was in 1883, six years after Glover's survey, that Foreman was employed to make the subdivisional survey of this township and to resurvey its east and south boundaries. This he did, and his survey was adopted and approved, and the land sold by reference to a plat compiled from his field-notes, a circumstance which puts Glover's survey and notes completely out of the case. They either conform to Foreman's notes or they do not. In the former case they are superfluous, in the latter incompetent, and only serve the purpose of further confusing an inquiry which is sufficiently confused without them. It is to Foreman's field-notes and the official plat that we must look for guidance in relocating the lost corners of the subdivisional survey, and whatever Glover did not only may, but must be, left out of the consideration, if it conflicts with what Foreman did. His survey was superseded by the resurvey. It could, at most, have the effect of corroborating the latter in some collateral way, but cannot be allowed to contradict it. The question is not where Glover put the township line, but where Foreman finally established it, and the only evidence we have of that is his field-notes, and the official plats of township 5 south, range 2 east, Humboldt meridian, and township 24 north, range 19 west, Mt. Diablo meridian, of which that township line is the common boundary. These show a perfect correspondence with Perrin's field-notes as to the western portion of the line — noting at the same distances
the seashore, Whale Gulch, section and quarter-section corners, and witness-trees.
To return now to the survey made by Chapman of the southeast quarter of section 34, and the measurements based upon that, by which he claims to have confirmed the correctness of his location of plaintiff's land: His testimony shows that he selected as the starting-point of that survey a corner described in Glover's
field-notes. In other words, he prefers a corner established by a superseded survey to all the conspicuous landmarks noted in the later official survey, and the only conclusion is that, if he surveyed correctly from the point so selected, there is no correspondence between Glover's survey and Foreman's survey — a very probable supposition on other grounds; for Glover's method of locating the east end of Perrin's line, as described in his (Glover's) field-notes and the testimony of the witness Riley, was not such as to inspire much confidence in the result of his labors.
The first survey made for the purpose of locating plaintiff's land after the approval of Foreman's official survey, was made in 1894 by Richard York, county surveyor of Mendocino County, for Stewart, the original patentee and plaintiff's grantor. Evidence of York's location of the land was introduced for the purpose of corroborating Chapman's survey. York, himself, was not called as a witness, and his field-notes — which should have been on file in the county surveyor's office — were not produced; but Breeden and Howard, who as chainmen assisted in making the survey, testified from recollection as to the manner in which it was made, and that the location of plaintiff's land by York was practically identical with Chapman's location. But their testimony also showed that this survey corresponded with Chapman's only because, like Chapman's, it was based exclusively upon an erroneous location of the quarter-section corner of section 32. York's method of locating that corner was to start from the southeast corner of the township at a distance of four and a half miles to the east, and chain that distance on a course which the witnesses are unable to state. As to whether it was due west or only approximating that course, there is no competent evidence; and there is likewise no competent evidence that he started from the southeast corner of the township. Neither Breeden nor Howard pretends to be a surveyor, or to know
of his own knowledge that the point from which they commenced their chain measurement was the true southeast corner of the township. Howard says: "We started on the east line of 36; they [meaning, I suppose, York] called it the township line; I don't know; we found a post at the corner of 36, from that course we ran west clear to the ocean — the bluff," etc. Breeden's testimony upon this point is the same in effect as Howard's, except that he does not expressly state that he did not know of his own knowledge that the post from which York started was on the township line. Fairly construed, however, all the testimony as to this essential fact was pure hearsay. But, passing this objection, and allowing that the measurement was made from the true southeast corner of the township, the mode of locating the corner at or near the end of the measured course was contrary to law. There is nothing better settled by authority or statute than the rule that courses and distances are controlled in the fixing of boundaries by visible monuments, unless there are other sufficient circumstances to corroborate the former. (See Code Civ. Proc., sec. 2077, and Miller v. Grunsky, 141 Cal. 450, [66 P. 858, 75 P. 48].) And this is especially true when the boundaries themselves are permanent and visible, such as the bank of a navigable river or the shore of an ocean. As to the mode of locating this quarter-section corner of section 32, Breeden, who admits that he cannot remember the exact distances they ran except where they set or found corners, says that when they got to section 32 "we found a part of a stake or some object there, I don't know what it was; we found a stake having the appearance of a corner," etc. Howard says: "They found a stub there that they thought would prove to be a stake, the stake had been burned years before, it was so rotten you could not tell — we set astake there, then we went on west to 31 and 32, and then we located Mr. Stewart's claim." This tells the whole story. Neither Breeden nor Howard knows whether York had any field-notes to guide him. If he had any, they were probably Glover's, as may be inferred from the fact that his survey co-ordinates itself with Chapman's survey from a Glover corner. Certainly, if he had Foreman's notes, — identical with Perrin's, — and the only notes he was at liberty to follow, he entirely disregarded them. They, if they had been consulted, would have told
him that the quarter-section corner of section 32 was marked, not by a stake, but by a leaning madroño tree ten inches in diameter, and by the distance and bearing of two witness-trees — a madroño and oak; that instead of being nearly a quarter of a mile east of Whale Gulch, it was more than a quarter of a mile west of it, and that instead of being nearly one hundred chains from the ocean shore it was only 61.60 chains from that imposing landmark. Here, then, was a corner located by course and distance alone, and absurdly out of relation to a fixed and unmistakable natural boundary, and to every monument and landmark called for in the field-notes of the official survey. A location of lost corners by a survey from a corner so established is utterly worthless; it is a survey made contrary to law. (Code Civ. Proc., sec. 2077.) York's survey, therefore, instead of corroborating Chapman's, merely serves to explain Chapman's mistake. It furnishes, as above intimated, the genesis of the "old settler" corner. For Howard testifies that they replaced the rotten fragment of a stake with a new stake; and that no doubt soon acquired among the neighboring settlers the reputation of being what it purported to be — the proper mark of that quarter-section corner. As such it was pointed out to Chapman who made it the basis of his survey without regard to mountain, stream, or ocean.
Plaintiff also called as a witness a Mr. Champagne, who had acted as a chainman for one Sandow in making a survey of plaintiff's land about two years before the trial. His survey assumed to start from the quarter-section corner between sections 20 and 21, and resulted practically in the same location as Chapman's. If Champagne knew of his own knowledge where the quarter-section corner between sections 20 and 21 was, his testimony would lend some faint support to plaintiff's case, but he does not say that he knew the corner — he saw a corner marked by a stake and a tree, but does not explain how it was identified as the corner which Sandow took it to be; and Sandow himself did not testify, having, as it is stated, left the country. Champagne's testimony, standing by itself, would leave it very uncertain whether Sandow really started from the quarter-section corner between 20 and 21, while the fact that his survey coincides with those of York and Chapman tends strongly to prove that he must have started
from another York corner established by him in surveying from a Glover corner, or from his erroneous location of the quarter-section corner of section 32. But whether this surmise is correct, or not, it is certain that the Sandow survey cannot impart vitality to one so fatally at variance with natural boundaries and monuments as Chapman's is.
The southwest corner of section 31 is the southwest corner of the township, and that is marked by the intersection of the township line with the shore of the ocean. To locate subdivisions of that section the survey should start from that corner, and if a survey from that corner locates them in one place, with their west boundary at the shore line, a survey starting from an interior quarter-section corner, nearly two miles distant from the nearest corner of section 31, which locates the same subdivisions in a different place and entirely away from the ocean shore, cannot be said to raise a substantial conflict. For, in the first place, a township corner is a monument of higher grade than any interior corner, and, in the next place, natural monuments — such as the shore of the ocean — which are incapable of being moved or mistaken, are always preferred to artificial monuments, and especially to artificial monuments at remoter distances.
In this review of the evidence, I have not forgotten the witness Burg, and I have not forgotten Perrin. Burg merely acted as axman for Chapman in making the survey from the Glover corner, which, as explained above, counts for nothing. Perrin was taken on the ground after the completion of Chapman's survey for the purpose of seeing whether he had correctly located the township line. He went on the ground twenty-five years after the survey, without his field-notes, and, looking at Chapman's stake at the summit of the ridge, concluded from his recollection of the topography that it was placed at or very near — practically at the same point — where he had set a post to mark the end of his meander line and the southwest corner of the township. This evidence given on his direct examination, it is needless to say was flatly contradicted by his own field-notes, as above quoted, and on his cross-examination he admitted over and over again that where his testimony differed from his field-notes his recollection was at fault. So that if, as he testified from recollection, he set his post at the end of his meander line to mark the southwest corner of the township,
that line must have ended at least 25.80 chains west of the ridge, instead of directly on top of it, where Chapman's post was set, and must have been run, as I have assumed it was run, along or near the beach. The evidence of Perrin, so far from supporting Chapman, is directly against him, for at last he swears by his field-notes, and nothing confutes Chapman more completely than they do — corroborated as they are in every particular by Foreman's notes.
An important topographical feature to which frequent reference has been made is Whale Gulch. Its distance from the ocean and its relation to section and quarter-section corners have been extensively commented upon in the foregoing discussion of the evidence, and it would not be proper to omit all reference to the iterated and reiterated assertion of counsel for respondent, based apparently on Mr. Chapman's testimony, that neither Perrin nor Foreman mention or refer to Whale Gulch in their field-notes. It is somewhat surprising that counsel should have been so easily misled in so simple a matter; for the only basis of Chapman's claim that the notes do not mention Whale Gulch, is that they do not mention it by name. They both mention it — Perrin, as a stream in a deep gulch, ten links wide, course south; Foreman, as a small creek in a gulch running east. All the evidence in the case, including Chapman's own testimony, shows that this small stream, or creek, was Whale Gulch, and nothing else. The official map of the adjoining township on the south shows it at the same distance from the ocean on the township line that Foreman places it in township 5 south, range 2 east, Humboldt meridian, and also shows its course from that point to its mouth in the ocean. The photographs also put in evidence by plaintiff, and taken from a point near the mouth of Whale Gulch, corroborate the map. They show the relation of the gulch to the ridge, and to Chapman's stake. It was not necessary to give a name to the gulch in the field-notes, even if it had acquired a name at the dates of the surveys, which does not appear.
The fact has been mentioned that Perrin located the township line a fraction over twenty chains too far south. It is not to be understood that it can now be correctly relocated. For it appears that Foreman in his resurvey adopted Perrin's line and based his subdivisional survey upon it. He must have discovered at an early stage of the subdivisional survey the fact
that the township line was too far south, and to satisfy himself as to the source of the error, he carefully retraced the meander line of the ocean, and discovered, as his field-notes show, the error of Perrin in starting from the point "a" instead of the point "A" when he undertook to locate a point on the seashore ninety-five chains south of "A," which marks the southeast corner of township 5 south, range 1 east, Humboldt meridian. He, however, resumed his subdivisional survey on the line upon which he had started — Perrin's line — and completed it by closing on the eastern line of the adjoining township, adding, as the map shows, nearly a half mile to the western boundary of that which he was surveying. His field-notes of the survey of section 31 — which correspond exactly with the official plat — show that he commenced at the common corner of sections 31 and 32 on the township line 21.80 chains east of the seashore, that he ran north forty chains, between sections 31 and 32 along a southwest slope, and there set a marked post and stone witnessed by two trees — at sixty chains he entered dense chaparral, at eighty chains he set a post to mark the common corner of sections 29, 30, 31 and 32, properly marked, and witnessed by four trees — giving distances and bearings. He describes the land along this course as mountainous, soil third rate, first half mile in open prairie, balance dense chaparral, scattering oak, and madroño. His notes as to the next course running west to the ocean, read as follows:
"As this line ends in the ocean in less than a mile
I run W. on true line bet. secs. 30-31 Var. 17 degs. 42 min. E. Steep descent 40. Set a post 4 ft. long 4 ins. sq., 24 ins., in the ground with mkd stone for 1/4 sec. Cor. in stone mound 4x2 ft. mkd. 1/4 S. on N. face.
No tree in limits.
50.35. Intersect the Pacific ocean on station No. 3 of meanders in sec. 30 and set a post 4 ft. long 4 ins. sq., 24 ins., in the ground for cor., to fractional secs., 30, 31 mkd., T. 5 S., R. 2 E. on E.S. 30 on N. and S. 31 on S. faces; raises a mound of stones around post.
No trees in limits.
land steep W. slope Soil 3rd rate partly open grass land and partly dense chaparral."
These notes clearly show that the whole of the section was surveyed on the west slope of the ridge, that on its south boundary the section line was 21.80 chains and on its north boundary 50.35 chains from the ocean. Plaintiff's east line is twenty chains west of the east line of the section, and the south half of his west line is the seashore. In relocating the corners of this section these notes and their calls for natural monuments are not to be disregarded in favor of a quarter-section post in Whale Gulch, placed, as it appears, by County Surveyor York in utter disregard of every call in the official survey, — and upon no better evidence as to its proper location than a chain measurement of a course four and a half miles in length from a point assumed to be the southeast corner of the township by witnesses who do not pretend to be surveyors, and whose testimony upon that point is essentially hearsay.
It is urged by counsel for respondent that even conceding an error in Chapman's survey, and that plaintiff's land is west of his location, the verdict ought not to be disturbed, because there is evidence in the record that defendant peeled the trees on the western slope of the ridge. There is such evidence; but it also appears that while the growth of tan-oak east of the ridge is very abundant, there are but few trees scattered along certain ravines on the west slope, and the verdict for five thousand dollars was based upon proof of a large quantity of bark stripped from the trees in Whale Gulch. The verdict, therefore, is not supported by the evidence as to the comparatively trifling amount cut on the west slope.
The principal errors of the court in ruling upon objections to evidence consisted in admitting the testimony of Breeden, Howard, and Champagne as to the York and Sandow surveys, without sufficient preliminary evidence that they were made from correctly located starting-points. Minor errors need not be noticed in detail. In view of the foregoing discussion they are not likely to be repeated on a retrial of the issues.
The order denying a new trial is reversed and the cause remanded.
Henshaw, J., Harrison, J., and Lorigan, J., concurred.