233 F. 547 | D. Mont. | 1916
An apex controversy, both parties seeking to quiet title and damages. The premises are in the Butte district. The Realty Company called plaintiff, owns the Elm Orlu claim, and defendant owns the Blackrock and other cla.i^ns. Only the two named need be referred to, save in the decree. They have a common side line for 850 feet of the Elm Orlu east end and of the Black-rock west end. '
It is'now admitted that the Rainbow vein at the apex crosses the Elm Orlu w'est end line, courses easterly, crosses the common side line and branches in the Blackrock, one strand crossing the Black-rock north side line, and one coursing easterly a disputed distance;
Plaintiff alleges that the Elm Orlu is the older location, and defendant alleges the Blackrock is. Plaintiff alleges that the apex of the Pyle strand is in the Elm Orlu and crosses the Elm Orlu east end line, and that the vein on strike and dip unites with the Rainbow vein; and defendant denies all thereof at points east of the Rainbow apex crossing of the common side line that would give extralateral rights to plaintiff. Defendant: alleges that the Rainbow and Jersey Blue unite on strike and dip, and plaintiff denies it and alleges that on strike and dip the latter crosses the Rainbow. Defendant alleges the easterly strand of the Rainbow crosses the Blackrock east end line, and plaintiff denies it. Defendant asserts some ownership of ore bodies under both claims by virtue of estoppel by deed executed by plaintiff to defendant’s predecessor in interest, and plaintiff denies estoppel. Both parties allege and deny trespass and damages, and accounting is deferred. Appropriate legal consequences and rights arc asserted by both parties. The trial consumed 16 da3/“S. There are nearly 1,600 pages of testimony,-and 130 exhibits." iVlaps and models are duplicated, save in more or less theoretical geology, from which unwarranted impressions are to be avoided. The testimony is of five experts for each party, all men of eminence in geology, or mining engineering, or both. For plaintiffs are Greene, of Butte, Irving, of Yale, Weed, of New York, Searls, of Nevada, and Winchell, of Minneapolis. For defendant are Finch, of Denver, Emmons, of Minnesota, Salisbury, of Chicago, and Burch and Wiley, of California. There is some conflict of facts and more of argument, opinions, and conclusions. Most of it can be imputed to the complex geological and other problems, conditions underground, difficulties of observation, and honest differences of interpretation by reasonable and learned men. But in instances partisanship apparently impaired judgment. As a whole, however, the testimony inspires confidence and deserves careful consideration. The judge gave two days to inspection of the premises, but since som'e places in evidence had been stoped and others obscured by fallen ground or timbering, with intermittent crevices and small openings through which to peer and distinguish granite, altered and otherwise, slips, faults, gouges, aplite, quartz seams, and veins, he has not been greatly aided to determine what evidence is more credible and weighty. The complexities which learned doctors studied for weeks, months, or
In the matter of priority of location, plaintiff attached to the complaint as exhibits a copy of the declaratory statement of each claim, alleged the locations, that based thereon patent had issued upon each claim, and defendant by answer in effect admits all thereof. Plaintiff offered in evidence the patent proceedings, and introduced oral testimony of the Elm Orlu location, to all of which defendant objected that both locations were invalid when made, and neither could be established, save as of date of patent entry. Defendant’s patent entry is the older, and on it defendant relies as the date of the Blackrock location. The Elm Orlu declaratory statement recites location of the “lode” in April, 1875, and it was recorded a few days later, and that of the Blackrock recites location of the “claim” in November, 1875, and it was recorded a few days later. At that time a Montana statute provided that all discoverers of lodes or veins “shall” record a declaratory statement thereof “on oath,” but prescribed no forfeiture for noncompliance. The oral testimony sufficiently proves that at least in 1875, and shortly after the Blackrock location, its owners knew the Elm Orlu was then claimed; that at least in 1876 a vein had been discovered in the Elm Orlu and the corners staked; and that thereafter annual labor was continuously performed, the claim leased, and ore mined; and it was well known and to the knowledge of the owners of the Blackrock thenceforward. In November, 1880, the Blackrock owners applied for patent based on the aforesaid declaratory statement, no adverse claim was filed, entry was made, and patent issued in February, 1882. In December, 1882, the Elm Orlu owners applied for patent based on its aforesaid declaratory statement. The proceedings showed and excluded a conflict area with the Blackrock, and theretofore included in' the Blackrock patent. Entry was made and patent issued in January, 1884.
True, the posted notice is temporary, and the recorded one permanent. But the principle is the same, viz., that the failure to' comply with local rules or statutes that do not prescribe forfeiture as a consequence is immaterial so far as those with knowledge of. the locations are concerned. If one such statutory requirement does not imply forfeiture for failure, why should another? If in the case cited partial failure was not fatal, why should it be in the case at bar? No reason appears why the rule of the Yosemite^ Case does not control this at bar. The state rule of decision, now set aside by statute, does not commend itself as sound, and cannot be followed here.
The court finds that the northerly wall of the Rainbow apex crosses the common side line 190 feet fr.om the southwest corner of the Black-rock, and that the southerly wall so crosses 301 feet from said corner. For plaintiff the testimony is that the latter crossing is “about” 308 ■ — -“rather the extreme and indefinite limit of the mineralization which accompanies the vein”- — to 314 feet; for defendant, “about” 300 to 301 feet. All agree there is no defined wall — that it is indefinite and leaves much to judgment. Considering the evidence in light of inspection and that the burden of proof is upon plaintiff, it" is believed that the concession of defendant is more nearly right and as favorable to plaintiff as the facts warrant. The exposure is in a surface trench, and it is difficult to distinguish vein matter in place from mere seepage effect in adjacent country, whether of vein solutions or surface waters, and perhaps mushrooming beyond the limits of the vein proper below. A shaft might have contributed to accuracy. Finch testified that within the limits of the 300 feet he included 15 feet to the extreme limit of rock alteration, with a few little seams in it “to be consistent with the interpretation of a vein at other points.” This is admirable frankness, but imports that at vital points and to indefinite extent he characterized that as vein which in his judgment is not vein, to serve his client and avoid hazard of comparison. The difficulty is that, when an expert shades his testimony upon the principle of do ut des, partisanship is likely, if not certain, to favor his client, and the court cannot determine to what extent, inevitably detracting from the weight of his opinion.
Adverting to the Pyle strand, it is known to diverge from the south side of the Rainbow at and above the Elm Orlu 1,200 level, and coursing easterly and at points 100 feet south of the Rainbow it crosses the common side line at the elevation of the Blackrock 1,100 level, 250 feet west of the Elm Orlu northeast corner, and unites on strike and dip with the Rainbow in the Blackrock- at said level, 230 feet east of said crossing and 60 feet north of said corner. At this union it is a strong vein, 15 feet wide. One hundred feet west of the union there is a raise upon the Pyle, which, offsetting west, ends 40 feet above the
Three hundred and fifty feet above the raise the country has been thoroughly crosscut by the Clark tunnel and connected workings, in which are slips, seams, and more than 15 small veins, some in each claim, some of those in one claim as reasonably to be correlated with the Pyle as those in the other. These premises are filled with slips, gouges, seams, veinlets, and veins, and will not permit correlation nor projection of small features like the Pyle at the Elm Orlu 500, save for slight distances. Plaintiff’s witnesses are in doubt whether the Pyle ends in the raise or continues to the surface. Defendant’s witnesses incline to the opinion it continues upward; that the southerly dipping slip in the raise is the Pyle fissure and should apex in the Blackrock. This slip, if the Pyle fissure, may contain ore above though mineralization ceased in the raise, and have its apex in some indefinite place above. Where is the apex of that part of the Pyle at the union on the Blackrock, 1,100 level is conjecture. Even if that “sliver” of the Pyle crossing the Elm Orlu east end line at the 800 level could serve as a vein to confer extralateral rights, where is its apex, and whether on dip it unites with the Rainbow, are also conjecture. And to what extent, if at all, the Pyle from its western divergence from the Rainbow unites with the latter on dip is not apparent. At the west it may be a part of the considerable ore body in which is the Bruce raise, and may go down vertically indefinitely, or epd in lenticular form, or feather out and not unite on dip with the Rainbow. The patent presumption that the apex of a vein in the Elm Orlu, discovered before entry, extends across the east end line, cannot attach to the Pyle; and all that is proven is that the Pyle is known at its western divergence from the Rainbow and at other points, making it clear that at the points of divergence and for some undefinable distance easterly its apex is in the Elm Orlu. ■
Plaintiff classifies the Jersey Blue as a “Blue” vein, and defendant denies it, contending it is a strand of the Rainbow and an east-west vein. The Rainbow is one of the greatest veins in the district. It was early and extensively mined for some 2 miles in length and in places to 1,500 feet in depth. In general, it is a broad zone of multiple and complex shattering, wherein largely by replacement mineralization occurred — at some places, in a wide, continuous vein; at others, in several roughly parallel strands, which may unite on strike or dip, or both; at others, in detached lenticular bodies; at others, in spurs or strands diverging from the main portion on strike, dip, or rise, and either feathering out or ending in lenticular form. At places in these premises it is 200 or more feet in width and largely commercial ore, while at others it narrows to a few feet, if not to a mere fissure, so far as ore is concerned. It has been greatly disturbed and faulted, not only by the “Blue” veins and other northwest fractures, but also by a later great series of multiple postmineral fractures designated the Blackrock fault. In these premises, the general course of this fault is tjiat of the Rainbow. It is sometimes in four or more strands, sometimes parallel in and along the Rainbow, branching and uniting — sometimes in the vein or along and now the old wall of the vein or itself defining the line of least resistance at the limits of mineralization, and now itself the wall of the vein; perhaps sometimes a strand in the Jersey Blue, sometimes diverging into the country. The direction and extent of movement along it is vague. The several segments of country and vein between its strands all may have diversely moved. Most of the witnesses appear to believe the south side moved west at least, though Emmons testifies that to seek the segment of the Jersey Blue vein on the south side of the Rainbow and the Blackrock fault, if it cresses them, you could look for 200 feet either way from the Jersey Blue vein on the north side. The Rainbow apex in the Elm Orlu is from 50 to 100 feet wide. It dips steeply south'to the Elm Orlu 800 level, then flatly north 55 degrees. It is probable that the Rainbow or a strand of it also descends vertically, having branched near or below where it dips flatly north. As it descends it widens. Where from the west it approaches and crosses the common side line it may be 200 feet wide, largely of commercial ore; and of these magnificent dimensions it courses easterly practically throughout the Blackrock. The Jersey Blue at the Blackrock west end line is 250 feet from the Rainbow. It courses more easterly than the latter and is of a dip more steeply maintained, so that from surface somewhere 300 feet east of the Rainbow apex crossing of the common side line to beyond the Blackrock west end line, and there 1,300 to 1,600 feet below the surface, the two veins have converged to union or nonunion, if not crossing.
The Jersey Blue is relatively regular arid narrow, 2 to 30 feet in width. It is little mineralized, especially in the upper levels, having less than 1 per cent, stoping ground; the Rainbow having 40 to 50 per cent. Even at the point where it does or does not unite with the Rain
Defendant’s witnesses describe this as more or less conjugated fracturing, hut forming a “horse-tail” structure uniting the two veins, though Emmons testified it did not make them one vein, but is an ore body between the veins. Finch imputes it to tension fracturing; Emmons to that of compression. It is apparent that they include in this “liorse-tail” structure much that is internal transverse structure, of the Rainbow and south of the Rainbow’s well-defined hanging wall. Dei'eiubni’s maps show it, and it is clear from the testimony of Finch and Emmons. When they admit that the Rainbow hanging wall is in the raise from the Blackrock 1,300 level (and it is also conclusively proven), they admit the Rainbow hanging wall both ways from the raise and north of the “horse-tail” structure. Finch testified that south of said hanging wall the Rainbow structure parallels the wall, and south of that is the “horse-tail” structure transverse the Rainbow, pointing to the Elm Orlu 1,300 level stopes. They also testified that this “horse-tail” structure diverges from the south side of the Jersey Blue and extends to the north hanging wall of the. Rainbow, pointing it out on defendant’s maps, where it is so painted but — in wholly undeveloped country.
This mineralization outside of and between the veins is o-f little extent and consequence. It doubtless at some places extends from vein to vein and some thereof in transverse fissures. But little of it is of commercial value and it by no means merges the veins. Both, as Emmons testified, retain their identity by reason of a “pretty definite limiting zone outside the two master fractures” of the two veins. It is not near as extensive as painted by defendant; otherwise, and if Finch’s theory is correct (all the fissuring here is steep and seems normal — of tension), it ought to also appear where it does not, north of the veins at depth where the north country is the hanging wall side. The fracturing may be there, but not the mineralized “horse-tail” structure; and it is fair to infer that the mineralization between tifie veins came in connection with the great mineralization of the Rainbow and little from the barren Jersey Blue. These two veins have points of resemblance, but more of difference. The Jersey Blue more approximates to the “Blue” veins than to the Rainbow. Defendant’s witnesses are of the opinion the Rainbow and Jersey Blue are of the same age and unite, the latter a strand of the former. Plaintiff’s witnesses are of contrary opinion. The latter definitely describe places where the Jersey Blue crosses the Rainbow, from observation. But it is difficult to determine whether the testimony of defendant’s witnesses that the veins unite is theory, inferences from or reflection of
It is surprising in view of what is irivolved, that so little development has been done at the points of first contact between these veins, and where union or nonunion or crossing ought to be more open to determination than elsewhere. It is realized development is expensive. The ground is heavy and difficult to hold. Each party did some development work for the other. Their workings unite at many points. But in instances both parties halted development at seeming vital points, as -though fearful of results damaging to their theories. To briefly review this development, it is largely post-litigation. In all the years subsequent to location of the Blackrock and until this litigation threatened,, no workings from the discovery shaft were on the Jersey Blue. This shaft is in the easterly Rainbow strand about 100 feet from where the Rainbow branches. But on the tunnel level, 50 feet below the surface and 400 feet west of the discovery shaft, was the face of a drift on the Jersey Blue, and on the 400 level was a drift through the country for 1,200 feet west of the shaft, from which three or four crosscuts were run to the Jersey Blue. After this litigation threatened, defendant ran two parallel drifts, with crosscuts, from the drift face aforesaid, easterly to the discovery shaft. For the first 100 feet one drift is on a clay slip, the other on the vein. There the vein ended. Defendant’s witnesses testified it was cut off by the Deadwood, and, as the Deadwood is admitted a “Blue” vein, urge this as proof that the Jersey Blue is of older age than the Deadwood, and so not a “Blue” vein. For the next 150 feet, and to the Rainbow, defendant’s witnesses testified the workings are in highly mineralized and altered granite, filled with what Finch described as, crisscross quartz seams or stockwork and Emmons as a sheeted zone of closely-spaced parallel quartz seams with some cross quartz seams, and which is claimed by them to unite the Jersey Blue, so continued, with the
On suggestion that they were virtually describing the Jersey Blue as crossing the Rainbow, they explained both veins merged into each other, or in a hub of mineralization around the discovery shaft, and as one vein branched in four directions. Defendant’s sampler testified that, as these workings were run, he sampled all vein matter and quartz disclosed; that from where the Jersey Blue ended, 100 feet from, the old drift face in the new drift, he went east 36 feet for the next sample, then east 53 feet for the next, then east 83 feet for the next, which was in the Rainbow; that in the parallel drift from opposite the point aforesaid he went east 22 feet for the next sample, then east 60 feet for the next, then east 22 feet, then 20 feet, then 20 feet for the next in the Raiubow. Westward in old workings, where the vein is unquestioned, he sampled at 10-foot intervals. Plaintiff’s witnesses testified that the Jersey Blue ended and was not cut off by the Deadwood; that from there to the Rainbow is only unaltered granite, with no stockwork or sheeted zone and no quartz seams, save the insignificant ones and joint seams in the granite of the district everywhere; that from near the old drift face the main part of the Jersey Blue coursed southeasterly, along which a drift was run until it reached and was cut off by the Blackrock fault along the north side of the Rainbow; that the drift was continued through and to the south side of the Rainbow and the Jersey Blue there found and drifted upon for 100 feet. No segment of the Jersey Blue was found in the Rainbow where the drift crosscut it, and this, plaintiff’s witnesses explained, is due to the fact that there the Rainbow is between two branches of the fault; that they did not think to develop to find it, though movement had so crushed the Rainbow it probably would not be found. Defendant’s witnesses testified that what in plaintiff’s behalf is there described as the Jersey Blue is only a fault gouge transverse to Jersey Blue structure and having in it some irregular bunches of quartz.
On the Blackrock 400 level, the Jersey Blue is not developed to the north side of the Rainbow, but from a crosscut entirely through both claims plaintiff drifted west 100 feet 'to the Rainbow, upon what its witnesses claimed is the Jersey Blue, consisting of parallel gouges'and quartz 2 feet wide, faulting the Rainbow and ending within the latter against the Blackrock fault. Defendant’s witnesses describe this as nothing but a branch of the Blackrock fault, and not the Jersey Blue. On the Blackrock 700 level conditions and testimony are like to that in relation to the level last mentioned, save that the Rainbow is plainly more faulted by what plaintiff’s witnesses describe as the Jersey Blue on the south side of the Rainbow; and upon this is a raise to the Elm Orlu 800 level, 40 feet above. On the 800 level the Jersey Blue is developed on the north side of the Rainbow, and plaintiff’s witnesses testified it curves northeasterly for a distance along the Blackrock fault,
On the Blackrock 900 level Greene testified that on the south side of the Rainbow the latter is cut off by the Jersey Blue, and he is unable to say why the western segment of the Rainbow does not reappear in workings farther west, unless faulted beyond them. There are no workings on the Jersey Blue immediately north of the Rainbow, and no other witness refers to this place. On the Blackrock 1,000 level Greene and Irving testified that on the south side of the Rainbow the latter’s ore body is cut off by the Jersey Blue,, and that the Rainbow’s western segment is not observable. The working in which this is said to be seen crosses through to the north side of the Rainbow and then along the Jersey Blue on the said north side. Greene further testified that the Jersey Blue there north of the Rainbow is but 8 to 10 inches wide, and on the south side it is 4 feet wide. No other witness referred to this place, save Einch, who testified that in a working north of .the Rainbow is a positive, actual junction developed between the two veins; but the point he refers to is in what defendant’s map depicts! as “horse-tail” structure from the Jersey Blue and north of the Blackrock fault, which is along the hanging wall of the Rainbow. In reference to the Blackrock 1,100 and 1,200 levels Searls testified that in stopes below the 1,100 and across the Rainbow he saw the Jersey Blue cutting and “terminating absolutely” the bands of zinc ore of the Rainbow, “just as distinct in the stope as it is here on this paper” (an illustrative sketch), and that it was unquestionably the Jersey Blue, because also visible in a drift four feet below. Greene testified-that .the stopes at the 1,100 on the south side of the Rainbow end against a northwest fault he believes to be the Jersey Blue; that he could not say how wide the Jersey Blue is there, as it was lagged, but in the stope it was 3 or 4 feet wide; that on the 1,200 on the north side "of the Rainbow the Jersey Blue faults the Rainbow, and that on the south side of the Rainbow for 80 feet it cut off the big stopes in the Rainbow ore body. No other witness refers to these places, save Einch, who testified that on the 1,200 in the crosscut a little farther west and.on the north side of the Rainbow is a “definite junction of the two veins developed,” though, he says, undoubtedly they also join farther west at this elevation; that the junction is not along gouge, but in the midst of a mass of ore. And there again he pointed it out on defendant’s map in “horse-tail” structure from the Jersey Blue and north of the Rainbow hanging wall. In reference to the Blackrock 1,300 level plaintiff’s map depicted the Jersey Blue within the Rainbow and crossing it at an acute angle, for 400 -feet. Plaintiff’s witnesses
In defendant’s case in chief, its witnesses testified that the Jersey Blue and Rainbow veins are to be seen in the bottom of that raise; that on the level the lagging had been removed from the raise to the south side of the Rainbow; that the exposure across was solid zinc oref without transverse fissures or gouge, and for 35 feet. Finch testified that in the raise and 25 feet above the sill of the 1,300 level the Jersey Blue and Rainbow “are seen to be united,” but as it conclusively appears that the veins are converging at the first floor of the raise, he again places the union in “horse-tail” structure, if anything, and north of the hanging wall of the Rainbow. Salisbury testified he was in the raise, and the veins “should come together about at the sill floor,” which was “not now open to observation”; that in the stopes east of the raise “there is well exposed the so-called crossing of the Jersey Blue vein of the plaintiff in the midst of the so-called Rainbow lode of the plaintiffs”; that “the crossing is not very evident, but the thing which seems as I interpret it to be the Jersey Blue vein of the plaintiff * * * is, as I interpret it, a slip through the ore of” the Rainbow; that “the slip is distinct”; that in reference to the structure of the ore following the slip he did “not so interpret it”; that at the Rainbow north wall the structure parallels it for 3 or 4 feet very distinctly, but further south ceased to be banded, and he would speak of it as having the structure of the granite it had displaced, and it is that structure which is the so-called Jersey Blue crossing; that the slip has gouge, with walls perfectly well defined, and “if you stand at just the right place” there seems, so far as the walls of the gouge “are concerned, a structure of ore running in that direction, hut I could make out” that there was other structure “than that which seems to be outlined by the two walls of the gouge”; that on the south “that structure does not seem to me to obtain”; and that the so-called Jersey Blue had a strike more nearly east than on plaintiff’s map and seemed to be. merely a fault slip made after the ore was formed. Burch testified that on the level he could not find the Jersey Blue where plaintiff’s map placed it; that from the raise south, where the timbers were removed for the width of 30 feet of the Rainbow, is almost solid zinc ore, without gouges or slips or transverse structure; that looking up at the foot of the raise he could not tell how the structure of the zinc ore dipped; that it is not appreciably banded, but is irregular blocks, appearing more like the original granite structure; that he did not see anything that looked like “the ore coming down and being faulted”; that looking at the ore and rocks just southerly of the foot of the raise it is not evident that the bands of the Rainbow vein coming down are faulted by a southerly dipping fault — nothing that he “could possibly interpret in that line.” Wiley testified that in the raise the veins united and below are one — “come down and join as in that model can be seen”; that east of the raise, in the stope and in the Rain
Two days before the testimony concluded, plaintiff's witnesses visited'the raise at that 1,300 level, and after defendant rested Greene testified that in the west side of the raise at the first floor is a well-defined vein with two wall gouges separated 5 feet, and in which next the south wall are 6 or 8 inches of quartz practically vertical, and next the north wall is about the same amount of quartz and zinc ore, between them being altered granite containing little seams of quartz and zinc; that immediately south of this vein is rich zinc ore banding, approaching and abutting against it at a dip of north 53 degrees; that the north wall gouge (referred to as the Jersey Blue) appears east of the raise and diagonally crossing the drift at the first floor, still dipping steeply; that along the north side of that drift and the stope farther east is a strong gouge wall dipping north 80 degrees to apparently normal Rainbow dip of north 64 degrees; that south of this wall is very solid zinc ore, and six sets south is a gouge having along it 8 inches of quartz, with some pyrite and a little zinc in it, striking north 73 degrees west and dipping south 79 degrees; that it goes up to and across the back of the stope and “could be followed as you would follow one of these pilasters” of the courtroom, disappearing in the stoping; that south of that gouge is the solid zine ore of the Rainbow. On cross-examination he sought to explain his former testimony and the map, and testified that in his opinion the Jersey Blue in five branches crosses the Rainbow on that level. He also testified to gouges in the Rainbow and due to internal movement.
Irving testified that in the west side of the raise at the first floor he saw and entered in his notes “10 to 18 inches of quartz with-some gouge cutting the Rainbow banding”; that the Rainbow banding seemed to come in on the south side of the raise and toward .the vein described; that the vein last aforesaid dipped practically vertical and is of strike probably more west than north 70 degrees west; that it is the Jersey Blue, or a strand of it; that east of the raise in the stope he saw that vein in the Rainbow, and he described it about as did Greene, his notes reading, “nearly vertical very strong wall opening Rainbow material, good gouge, north 80 degrees west”; that in the west end of the stope and in the roof he saw, as he read from his notes, “beautiful vein, unmistakably Jersey Blue, about 6 or 8 inches good vertical zinc in it,” which he considered the Jersey Blue or a strand of it. On cross-examination he testified that he could not see the bottom of the raise; that he thinks there are two strands of the Jersey Blue at that level, one in the raise and one in the stope, probably overlapping, and that there may be more; that the strike of the strand in the stope is north 80 to 85 degrees west and the dip is south
Searls testified that in the raise the Rainbow plain banded structure dips north 55 degrees, and across and cutting and breaking it down is a plain south wall of at least that portion of the Jersey Blue, nothing obscure nor hard to see, dipping vertically; that the polishing and slickensiding of the previously existing ore with striations to the east at an angle of 15 degrees to the strike are plainly observable on the Jersey Blue south wall, which strikes north 77 degrees west; that the wall is a thin gouge, and next to and plainly across the severed strands of ore are 10 inches of parallel quartz, lying right against the north dipping structure of the Rainbow; that the Jersey Blue the width of the raise to the north is vertical structure, zinc and quartz banded, absolutely vertical; that in the drift east from the raise the Jersey Blue can be seen in a corner at least 6 feet wide, diverging to the south, with a strike north 60 to 65 degrees west; that the angle between the hanging walls of the veins, 30 degrees, can be seen very clearly defined in the roof of the drift, and that it is perfectly obvious that the Jersey Blue departs southeast from the drift; that where these two hanging wall gouges are together it is impossible to see one gouge cut through the other, and they are apparently merged for 6 feet on strike, though the intersection on dip is plain, as in the raise can be seen the Jersey Blue gouge of vertical dip; that the Jersey Blue south wall cutting across the Rainbow in the raise and its north wall cutting across the Rainbow in the drift are “just as plain as that same wall of the courtroom” ; that in the level and stopes the Jersey Blue structure does not all persist, but is interrupted strands, which is common where veins cross from one variety of country rock to another, the Rainbow here being of the nature of country rock to the Jersey Blue; that four floors below the level he could see the Jersey Blue with a strong blue gouge and parallel zinc handing cutting the Rainbow wall and traversing it diagonally, the same Jersey Blue he saw in the workings at the level. On cross-examination he testified that from the raise he saw no strand that died out; that 10 feet up in the roof of the stope, where Irving saw the beautiful vein, he saw some white material which he thought is quartz, though he did not try to inspect it closer; that in Rainbow stopes are almost innumerable small cracks like one on the 1,300 level he thought might have occurred at the time the Jersey Blue faulted the Rainbow.
Winchell testified 'that a pile of muck concealed the level below the raise, but at the first floor he saw the Rainbow solid mass of zinc ore
Weed .testified he agreed generally with Greene, Irving, and Searls in reference to the situation in the raise and stopes on that level.
In rebuttal Finch testified that in a new westerly drift from the stope of the 1,300 a strand described as of, the Jersey Blue by plaintifFs witnesses is a mud seam or gouge, taking a strike of south 73 degrees west. Burch testified that “mud séam” dwindled to a crack, as did Wiley.
The judge twice visited this raise at the level, but conditions were such at the last visit that it added nothing to judgment. On the Blackrock 1,400 level and stopes above it, all below the point of alleged union, Greene testified that in stopes and crosscuts the Jersey Blue could be seen in the Rainbow. Irving testified that in a stope four floors above the level the Jersey Blue is found cutting the Rainbow. Searls testified that on the ninth floor above the level the appearance is <of another vein coming in the stope; that the banded zinc ore of the Rainbow striking slightly northeast comes up against and is terminated by a distinct vertical gouge, the zinc ore being dragged around slightly and crushed into breccia; that “this structure” strikes north 70 degrees west, dips vertical, and is traceable across the stope to the end of that floor; that the conclusion is irresistible that the Rainbow is there broken and cut off by a later vein. He further testified veins often cross without faulting. Winchell testified on this level the Rainbow is faulted along its south side, in the stopes, by the Jersey Blue; that the Jersey Blue is about 8 feet wide in a crosscut there south of the Rainbow. Finch testified that on this level, to his knowledge, no vein crosses the Rainbow as depicted on plaintiff’s map, though there are some fault slips. Burch testified to transverse seams of gouge there, but so far as he could see or find for lagging there is only the Rainbow. S'o, likewise, Wiley.
The Elm Orlu 1,500 level is 40 feet above the Blackrock 1,400 level, and from the former a crosscut was run into the Blackrock. Greene testified that therein the Jersey Blue is found cutting through the Rainbow and that the veins showed different structure. Irving testified that there at one point the Jersey Blue is wholly in the Rainbow; that the latter dips north 45 to 50 degrees, and the former dips 87 degrees — nearly vertical; that the Jersey Blue banding goes directly through the Rainbow banding and it is a vein made up of pink manganese — “the clearest case” of crossing lie knowá of. Finch testified that what the plaintiff’s witnesses call the Jersey Blue on this level
In reference to the Credeu vein defendant’s witnesses testified if united the Rainbow and Jersey Blue, and plaintiff’s witnesses that it diverges from the Rainbow and is cut off by the Jersey Blue. So far as appears it is a strand of the Rainbow, diverges from the latter’s north side in the Elm Orlu at depths of 1,000 to 1,200 feet, extends no farther east than crosscut 1,218 on the 1,200 level and the Black-rock west end line on the 1,300 level, strikes northwesterly under both claims, and unites with or is cut off by the Jersey Blue. It is not proven to unite with the Jersey Blue. Its apex is probably in both claims. Neither party seems much interested in it, and it is oí little importance in itself, though careful investigation might have furnished light upon this issue.
Taking into consideration ail the evidence, the inspection, and the undefinable impressions received during the trial, the court is not persuaded that by a preponderance of the evidence it is proven that the Jersey Blue vein and the Rainbow vein unite. Consequently the finding must he and is that they do not unite. At the tunnel level the Jersey Blue ends 150 feet west of the Rainbow. The stockwork claimed to continue it, even if there, has neither strike nor limits. It answers no definition of a vein. Apparently here is one place where Finch found it necessary to some indefinite extent to characterize as vein what in his judgment is not vein. The sampler’s conduct during the progress of the work speaks loudly. Be found no vein matter or quartz for 53 feet in one drift and for 60 feet opposite in the parallel drift, when the ground was fresh and no timbering to obstruct his view. Plaintiff’s evidence that here is only country rock permeated with the joint and quartz seams common throughout the district is persuasive and superior in weight to that of the defendant. Defendant’s contention that the Jersey Blue is faulted by the Deadwood is not supported by the evidence. Some small slips are probably at or near the termination of the Jersey Blue, but to correlate them with the Deadwood requires a series of sweeping curves and projections unwarranted by any development upon the Deadwood there or below, and impossible in these premises. On the Elm Orlu 800 level, where union is next claimed, the Blackrock fault separates the veins, and by Finch the union is placed in the slightly mineralized country in undeveloped territory between veins. The other points of developed union claimed are on the Blackrock 1,000, 1,200, and 1,300 levels, and in every instance by Finch, who alone purports to have perhaps seen them, are placed in the mineralized country between the veins. This is not union within the meaning of the statute. The veins have not merged and lost their
The conditions at the Blackrock 1,300 level and the testimony in relation to- them are somewhat surprising. It is remarkable that defendant’s witnesses said so little, not only in chief, but in rebuttal, of the appearance of the veins at the first floor of the raise and in the walls of the stope. They, too, returned and reviewed the place about the time that plaintiff’s witnesses first viewed it. Finch testified that in the raise and 25 feet above the level the veins “are seen to be united,” and his colleagues testified they should come together at or blow the level. Finch previously testified the Jersey Blue branches wherever it approaches the Rainbow, so whatever he saw might have been a branch of the Jersey Blue departing from the raise, and which might be one of the strands plaintiff’s witnesses testified are in the workings below. Not only did defendant not lower the raise-to disclose the actual point of contact of the veins and their relation there, but the floor .of the level and the west wall of the raise were obscured, so that none of even its own witnesses saw either. It is apparent that a very limited additional development, or even clearing away obstructions, might have furnished evidence to fully determine the issue. This appears to be the most favorable point of approach of the veins to determine the issue. In so far as the crossing of the veins is concerned, the evidence equally fails to persuade that they do. It is true that conditions and appearances in the raise of the Blackrock 1,300 level tend to support the interpretation of plaintiff’s witnesses, but not to the extent claimed by them. It is also true some of the plaintiff’s witnesses testified definitely to and described crossings of tire veins at points whereon defendant is wholly silent. And this is significant in this: Tt is obvious, and also admitted, that if the veins cross at any one point, they must cross at all points, even though so obscurely as to be undiscoverable. But this is not so of union. Every appearance of union and merger may exist at many' places, but if one point of crossing is proven, all evidence of union avails nothing and the veins are proven to cross throughout. Healing and cementation may destroy evidence of crossing in many places. Where the “Blue” fractures crossed the well mineralized east-west veins, in most places there was nothing to replace.and the fractures healed. Only where there was yet unreplaced granite would there be much evidence of cross-vein structure.
At the same time, there are so many slips and gouges in the Rainbow, as well as out of it, so much transverse structure in the Rainbow, and so much obstruction to the view, that it is easy for the expert to be deceived, or to deceive himself, and to misinterpret geological phenomena there. “If you stand at just the right place,” as Salisbury puts it, may to some extent be taken figuratively as well as literally. The Blackrock faults have so complicated the situation that it is doubtful if the problem is capable of solution. Whether they
It is probable that the eastern segment of the easterly strand was faulted to the north and may appear in a trench north of the Black-rock north side line. And this may be the apex of the great ore bodies at depth in the .easterly part of the Blackrock. Considering the evidence in. connection with the patent presumption, it does not persuade that the easterly strand crosses the east end line.
“does remise, release and forever quitclaim unto the said party of the second part, and to his successors forever, all the right, title, interest, claim and demand of the party of the first part in and to that certain portion, claim and mining right, title and property on those certain ledges, veins, lodes or deposits of quartz and other rock in place, containing precious metals of gold, silver and other metals, * * * the following described mining property, to wit: An undivided one-quarter interest in and| to that certain quartz lode mining claim known a,s the ‘Blackrock’ quartz lode mining- claim. * * ' * It being the intention of the party of the first part to convey to the party of the second part all its right, title and interest in and to the above described property. Together' with all the dips, spurs and angles and also all the metals, ores, gold, silver and metal-bearing quartz, rock and earth therein, and all the rights, privileges and franchises thereunto incident, appendant and appurtenant, or therewith usually had and enjoyed; and, also, all the estate,*573 right, title, interest, possession, claim and demand whatsoever of the said party of the first part of, in or to the said premises and every part or parcel thereof.”
November 1, 1906, the optionee and grantee in said deed conveyed all received by virtue of it to others, who in turn conveyed to defendant. Defendant’s contention is that in any event by this deed plaintiff conveyed one-quarter of any ore bodies beneath the Blackrock that apex in the Elrn Orlu and also the like portion of any ore bodies beneath the Elm Orlu that apex in the Blackrock and which otherwise might belong to plaintiff. To maintain this contention defendant appeal:; to Montana Mining Co. v. St. Louis Mining Co., 204 U. S. 204, 27 Sup. Ct. 254, 51 L. Ed. 444. But that case is distinguishable from this. There the deed was to settle litigation and was of a portion ol the St. Louis claim, “together with all the minerals therein contained.” A vein apexing in said claim dipped under the deeded portion. And the court held that the segment of the vein under the deeded portion was “therein contained” and so was conveyed by the deed. Although the court rested the decision somewhat on the rule of common law, it seems clear that in any view the segment of the vein was in the deeded portion — was “therein contained” — -and within the intent of the deed. A vein apexing in a claim is in every part of that claim under which it dips. But in the case at bar there was no litigation to settle. Veins apexing in the Elm Orlu and to which that claim possessed extralatcral rights were not in the Blackrock, though they dipped under its surface. Nor were they carved out of the Blackrock, for never were they in it. The property conveyed by the Elm Orlu patent was not a rectangular block to the center of the earth, but was such block with all projecting veins apexing therein wherever they extended; and those projecting veins were as distinct and separate from the surface beyond the Elm Orlu under which they dipped as like surface projections nearly surrounded by adjacent property would be from it; and no more in it in the former case than in the latter. Clearly, a deed of land and all therein would not convey land projecting in and nearly surrounded by it.
Suppose this deed was of warranty; would plaintiff be liable when the owners of other veins dipping under the Blackrock, of which there are doubtless some, assert their rights thereto? Are those veins in the Blackrock? And if not, why are these of the Elm Orlu? The option was to convey the Blackrock only, not any part of the Elm Orlu. There is nothing to show that the optionee had any knowledge plaintiff owned the Elm Orlu. The circumstances and the language of the deed warrant the construction that only the Blackrock and its ex-tralateral rights were within the intent of the parties. Giving effect to every one of the profuse words in the deed, this seems the right conclusion. The same is true of such portions of veins apexing in the Blackrock and dipping under the Elm Orlu. If the facts are such that by virtue of location and patent, not the Blackrock’s extralateral rights/ but the Elm Orlu’s attached thereto, those portions were not in the Blackrock, but were in the Elm Orlu from the beginning. The claim of estoppel fails.
A great chancellor once said that the test of a good decree was that it satisfied neither party. If that quality attaches to this decision some consolation ought to be found in the reflection, not of influence in the decision, however, that each party is awarded everything and deprived of nothing that, apparently, it thought itself entitled to until recently.
Upon accounting had, defendant waived in respect to its ores taken by plaintiff. It appears defendant’s taking of plaintiff’s ores was continuous from March, 1910, to May, 1913, both inclusive. The place was the Blackrock 1,200, between the Blackrock west end, and the 301 plane established at the Rainbow apex crossing of the common side line, and from said vein where bisected on strike by said side line. In 1910 there were no workings above that point that served to determine what vein (and where was its apex) was being mined by defend•ant.
Plaintiff having access at all times to defendant’s workings with its consent, in June, 1910, observed defendant was taking said ores from beneath the Elm Orlu, and claimed a trespass. Eater inspection disclosed like taking by defendant from beneath the Blackrock. At some time subsequent to March, 1910, plaintiff took some of defendant’s ores from the same vein beneath the Blackrock. A controversy arose in respect to all said ores and more, and was the subject of discussions, negotiations, understandings, and agreements between the parties. In March, 1912, they agreed that “to facilitate the settlement of the controversy as to the ownership of said ores and ore bodies from which ore has been extracted, if any, by either of the parties hereto, and to provide a reasonable length of time within which the parties may negotiate, * * * and endeavor to complete a settlement as to the
Later in the same month, to determine the location, position, and apices of the veins and ore bodies and to facilitate the settlement of the disputes, they agreed that each with diligence would do certain development for and at the expense of the other. Development work progressed, and in July, 1914, so far determined “the disputed matter to the satisfaction” of plaintiff, but not defendant, that plaintiff commenced this suit. The next month, in lieu of injunction pendente lite, for economic reasons, and not by way of limiting rights or admitting claims, they agreed upon areas wherein neither would mine, and areas wherein each might mine to the exclusion of the other, expressly stipulating that each was given the right pending suit to mine ore bodies claimed by the other, each to keep account of ore mined and places where, to he furnished the other on request, that the agreement would endure until decree herein, and that prior understandings and agreements in reference to reciprocal development work would continue,
In deference to the argument herein it may be observed that though in equity relief is limited to compensation, and damages in the sense understood at law are not determined and allowed, save where a court sitting in equity is so authorized by some statute (see Root v. Railway Co., 105 U. S. 215, 26 L. Ed. 975; 2 Dan. Ch. *1080), yet in view of the duty to herein administer local law (see Railway Co. v. Telegraph Co., 234 U. S. 376, 34 Sup. Ct. 810, 58 L. Ed: 1356; Trust Co. v. Krumseig, 172 U. S. 358, 19 Sup. Ct. 179, 43 L. Ed. 474) no reason is perceived why the local statute authorizing the injured party to elect the highest value between conversion and decision, creating a substantive right, should not be applied herein, had conversion been counted on and maintained.
Defendant mined and milled the ores in connection with operations .of which these ores were about 7.6 per cent. Allowances to defendant are, per ton of ore, $2.33 for mining, 17 cents for freight to mill, $1.19 for milling, and $2.06 for freight to the nearest purchasing smelter. For general expenses nothing is allowed, in that segregation is impossible, and nothing appears to show that defendant expended anything during the trespass that it otherwise would not. For instance, engineers, firemen, supervision, office help, shaft repairs, pumping, power, air, etc., were doubtless not appreciably increased. The theory of allowances is that the trespasser expended what the owner otherwise would have. But here, aside from direct mining and milling and freight, none such was expended.
A decree should be as definite as the case admits of, and it is believed that a decree conforming to the findings is sufficiently so herein. The evidence demonstrates that the Creden apex is in both Elm Orlu and Blackrock, but does not disclose the point where it crosses the common side line. The same may be true of the Pyle strand. A decree that each party is 'entitled to so much of said veins as lies within -the determined end line planes projected where the apices cross the common side line, can be made certain by following the apices to the crossing.
True, the parties may later dispute the point of crossing, and so new litigation arise to identify, to determine it — the boundary line; but that is no more than is probable in respect to the Rainbow, ‘the apex crossing of which is determined. At 100 places where the Rainbow dips beneath the claim not having the apex, what is the Rainbow, where is the bounding wall, what is ore in the Rainbow, and what adjacent, but without it, may furnish the subject-matter of a hundred suits. A decree may quiet title on a vein but partly developed, on presumptions, from end line to end line, which later may be found to cross side lines and between the same parties require new litigation to identify and fix the point of crossing. Other like situations may be conceived. The inherent nature of the property involved must be had in mind.
It must be noted the suit is not confined to specific ore bodies, but by defendant at least, by virtue of its claim of estoppel by deed, was broadened to involve every part of the Elm Qrlu — every vein apexing in the Elm Orlu, unknown as well as known, that may dip beneath the Blackrock. There are unknown veins within the Elm Orlu; that is, many veins the development of which is too slight to admit of definitely fixing where on strike they cross the Elm Orlu boundaries, or where they dip, as undoubtedly some of them do, beneath the Black-rock. Doubtless, too, are veins wholly unknown in unexplored Elm Orlu territory. Is not plaintiff entitled to a decree quieting its title to all such veins in so far as their apices may be found to be within the Elm Orlu bounding planes fixed or projected, and that may be found to dip beneath the Blackrock? Is not such a decree sufficiently definite in view of the circumstances? It is believed the answer must be in the affirmative. And the decree will be as deñnite as the patent that conveyed such veins as a part of the Him Orlu to plaintiff.
The Pyle strand undoubtedly apexes in the Elm Orlu, and since it
A decree conforming to the findings and quieting each party’s title to all veins apcxing in its claim, wherever they dip, would not be impaired, should deeper development disclose union of veins owned by them respectively. For at the union the junior location’s vein would be at an end, and below would he only the senior location’s vein. Some of the like difficulties attendant upon apex litigation are noted in Keely v. Mining Co., 169 Fed. 603, 95 C. C. A. 99.
Decree accordingly.
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