United States v. Romaine

255 F. 253, 166 C.C.A. 423, 1919 U.S. App. LEXIS 1471
CourtCourt of Appeals for the Ninth Circuit
DecidedJanuary 6, 1919
DocketNo. 3153
StatusPublished
Cited by25 cases

This text of 255 F. 253 (United States v. Romaine) is published on Counsel Stack Legal Research, covering Court of Appeals for the Ninth Circuit primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
United States v. Romaine, 255 F. 253, 166 C.C.A. 423, 1919 U.S. App. LEXIS 1471 (9th Cir. 1919).

Opinion

GILBERT, Circuit Judge

(after stating the facts as above). The appellant introduced in evidence certain hydrographic maps made by the United States Coast and Geodetic Survey, one in 1856 and one in 1887. The court below disregarded these maps, saying, “I do not think that the hydrographic maps are of any weight in this testimony in contradiction to the evidence that is presented”; and, relying upon the testimony of certain white witnesses, the court reached the conclusion that the testimony of the Indian witnesses and the other evidence adduced by the appellant were insufficient to sustain its contention.

[1] We are unable to agree with the trial court as to the effect which should be given to tire hydrographic maps of the United States Coast and Geodetic Survey as evidence in this case. We think the maps should be given full credence, and should be taken as absolutely establishing the truth of all that they purport to show. The map of 1856 indicates a large area of tideland at the mouth of the Nooksack river, and the river flowing in an easterly direction past the land which subsequently became the Hedge donation claim. The map of the survey made in 1887 shows the main channel of the river flowing along the south boundary of the Hedge donation claim, and thence easterly and in the direction of Treaty Rock, and, while it shows two or. more small streams diverging therefrom and passing through the lands in controversy near the center thereof, it shows that there was no channel or stream whatever at or near the westerly side of the lands. Capt. George R. Campbell, United States engineer and hydrographic surveyor, testified to the accuracy of official hydrographic maps, stating that all the features connecting the shores with the water are accurately outlined and surveyed and tied to permanent landmarks, that these surveys are made, with extreme accuracy, and that all are worked on a,n astronomical basis and are chained and taped a number of times, and that the government is always careful to do as accurate., work as is possible on a coast line and in its marine coast survey work. Such testimony was hardly necessary, we think, for the [255]*255court might properly take judicial notice of the accuracy of the official plats of the United States Coast and Geodetic Survey.

[2] The evidence shows that in the interval since the date of the treaty the position of the mouth of the river has not always been the same: that from 1855 to 1888 the main channel ran past the cottonwoods and easterly along the south side of the Hedge donation claim, and thence southeasterly to a point near Treaty Rock; that in 1889 the river cut through the south bank near the cottonwoods, and flowed thence into the bay in a southerly direction; that in 1908 the river made a new channel through the low-lying lands of sections 8 and 17, cutting in twain the east half of the Hedge donation land claim, and flowing thence, as it still continues to flow, southeasterly in the old channel- of 1855; that during these periods there was a small intermediate channel between the old channel of 1855 and the new channel of 1889, containing in different seasons varying amounts of water, and there is evidence to indicate that 8 or 10 years before 1889 there were times when a quantity of water ran substantially in the line which became the main channel of the years 1889 to 1908.

A. R. Campbell, who was employed by the United States to survey portions of the Uummi Indian reservation in the year 1905, produced a plat of the survey, which was admitted in evidence. He testified, and. it is conceded, that at that time the main channel was west of the lauds in controversy. . His instructions were to survey that portion of the reservation lying east of the main channel of the Nooksack river as it existed at that time, and south of the old channel. The outlines of his map are shown in the following diagram:

[256]*256Capt. George R. Campbell testified that in 1917, in pursuance <of instructions from Washington, he surveyed the northeast boundaries of the Lummi Indian reservation, and the map of his survey was received in evidence. He testified that an old channel, which he marked on the map “1855 to 1888,” was traceable' on the ground, and that the same was marked by old stumps of trees on the hank. A diagram of the outlines of his map is subjoine.d:

Several of the Indians of the Lummi reservation testified as to the understanding of the Indians at the time of the treaty, and the position at that time of the eastern mouth of the Nooksack river. George Tsilano, in his 100th year, who was 38 years of age at the time of the treaty, testified that Gov. Stevens, on behalf of the government, pointed out to the Indians the ground which would be given to them, and told them that the eastern side of the reservation would be a line running from Point Francis to Treaty Rock. He testified that it was always understood that the big rock would be the eastern boundary of the reservation, and that the eastern boundary line was from Point Francis to that rock; that he remembered very accurately the location' .of the mouth of the Nooksack river in 1855, and that it was a little bit above the rock; that there was a well-defined bank on the south bank of the river; that the river was deep, and that there was a large body of land south and west of it, always exposed at high tide. Henry JECavina, an Indian, who was 15 years of age at the time of the treaty, testified that he was present at the making of the treaty, that his father was one of the chiefs who participated in making it, that the easterly boundary line ran from Treaty Rock down to Point Francis, and that the mouth of the river was near Treaty Rock. Albert Descanum, [257]*257who was 18 years of age at the time of the treaty, testified that Henry Kavina’s father, who was an old chief, and a number of other old men who were at the treaty, all had said that the eastern line of the reservation was from Point Francis out to Treaty Rock; that the mouth of the river was at that time between McDonough’s wharf and Treaty Rock, and that it had no other mouth. George Warbes, 15 years old at the time of the treaty, heard Kavina’s father and other Indians speak of the eastern boundary of Chah-choo-sen, and they all said that the big rock is where the line would be on the eastern side of the reservation. There were younger Indians who testified as to the same understanding, an understanding which they had received from the old men of the tribe.

George Bremner testified that he came to the reservation in 1880; that at that time the mouth of the river was a little distance above Treaty Rock; that he came again to the reservation in 1893, and found that the river was then flowing on the other side of the land in controversy; that in the year 1908 he went to the reservation to- teach; that he knew Flenry Kavina’s father, the old chief, and many other old men, now dead, who lived on the reservation, and talked with them many times, and had always heard them refer to the mouth of the Nook-sack river when the reservation was established as located at Treaty Rock; and that it was the understanding through the treaty negotiations that the eastern line of the reservation was to extend from Point Francis to Treaty Rock.

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Cite This Page — Counsel Stack

Bluebook (online)
255 F. 253, 166 C.C.A. 423, 1919 U.S. App. LEXIS 1471, Counsel Stack Legal Research, https://law.counselstack.com/opinion/united-states-v-romaine-ca9-1919.