Fifty Years In The Northwest Part 34

Located in the town of Milo, has a steam saw mill, spoke and hub factory, around which are several residences.

PRINCETON.

The village of Princeton is located at the junction of the two branches of the Rum river, on a beautiful prairie, surrounded by rich prairie and timber lands. The first log house was built in 1849, and kept as a stopping place by a mulatto known as "Banjo Bill." This house is still standing. The first permanent settlers were A. B.

Damon, O. E. Garrison, C. H. Chadbourne, Edwin Allen, John W. Allen, Chas. Whitcomb, Joseph L. Cater, W. F. Dunham, and Samuel Ross. They were also the first settlers in the county, and came in 1853-7. In 1855 Messrs. Damon and Allen farmed on the present site of the village. The village was surveyed and platted Feb. 11, 1859, by S.

Ross & Co. S. Ross also built a hotel where the North Star Hotel now stands. This year the first frame building was erected and used as a store. W. F. Dunham built a steam saw mill. The first school house was built, although school organization was not effected until 1858. James M. Dayton taught the first school. A post office was established with O. E. Garrison as postmaster. Samuel Ross brought the mail once a week from Anoka. A Congregational church was established, of which Rev.

Royal Twich.e.l.l was chosen as pastor. The Methodists organized a society the following year.

The village was incorporated March 13, 1877, by legislative enactment.

The commissioners appointed under the organic act were E. C. Giles, H.

B. Cowles, C. H. Rines, B. F. Whiting, and Charles Keith. At the election ordered by them the following officers were chosen: President, C. H. Rines; trustees. F. M. Campbell, Isaiah S. Mudgett, Thomas F. Caly; recorder, Silas L. Staples; treasurer, D. H. Murray; justices of the peace, Scott M. Justice, Charles Keith. The Princeton _Appeal_ was established by Rev. John Quigley in 1873, but discontinued in 1875. In December, 1876, Robert C. Dunn started the Princeton _Union_, which he still publishes.

The Manitoba branch railroad from Elk River to Milacca village pa.s.ses through Princeton. The first train arrived Nov. 30, 1880. The county contributed $47,000 in bonds at five per cent interest for twenty years, to aid in building the road. The St. Paul, Mille Lacs, Brainerd, Leech Lake & Crookston railroad will, when completed, pa.s.s through Princeton. An excellent school building was erected in 1885, at a cost of about $7,000. Guy Ewing is princ.i.p.al of the school, which is graded. The Grand Army of the Republic have a post here known as the Wallace Rines post. The Masons have an organization, with a splendid hall. A three story hotel, built by Samuel Ross, is kept by his only daughter, Mrs. Barker. A two story brick hotel, the Commercial House, Henry Newbert, proprietor, a handsome structure, was built in 1887. The Mille Lacs County Bank, located here, has a paid up capital of $20,000. Charles Erickson is president; L. P. Hyberg, vice president; Frank Hewse, clerk. Princeton has one steam saw mill, two flouring mills, one feed mill, two elevators with a capacity of 60,000 bushels, and one brewery. A court house and jail are in process of erection at an estimated cost of $10,000.

BIOGRAPHICAL.

SAMUEL ROSS was born Aug. 22, 1812. He attended Western Reserve College, but through ill health did not graduate. He came to Iowa in 1839, where he was married to Mary Vaughn in 1841. He came to Princeton in 1855, where he took an active part in building up the town and county, filled many prominent and responsible positions in the village and county, and served as representative of the first state legislature. Mrs. Ross died in 1851; Mr. Ross died in 1881, leaving an only daughter, Olive R., widow of A. P. Barker, who was a prominent lawyer of Princeton. Mrs. Barker was elected superintendent of schools in 1880, to which position she has been re-elected and is at present filling the office efficiently. She was the first female superintendent elected in Minnesota.

JOSEPH L. CATER was born in Strafford county, New Hampshire, in 1828.

He came to Princeton in 1855 and engaged in farming. His name appears in all the original organizations of town and county. M. V. B. Cater and sons have also been active and prominent citizens of Princeton. M.

V. B. Cater died some years since.

EDWIN ALLEN, originally from Welton, Maine, came to Princeton in 1855 and engaged in farming.

JOHN H. ALLEN came from Maine to Princeton in 1854, engaged in farming and became prominent as a public spirited citizen. He held various positions of trust in the county and was appointed receiver of the land office at Fergus Falls by President Hayes, and resides there.

A. B. DAMON came from Maine to Princeton in 1853 and made the first claim on the town site.

C. H. CHADBOURNE was born at Lexington, Ma.s.sachusetts. At the age of sixteen he embarked in a seafaring life in which he continued nine years. Mr. Chadbourne, wishing to abandon his seafaring ways, and to put himself beyond danger of resuming them, came to the centre of the continent and located on a farm near Princeton in 1856. He has since followed farming continuously. His farm consists of 900 acres under cultivation, 500 of which is devoted to tame gra.s.s and pasturage, on which he feeds 150 head of blooded stock. He has a large dairy which nets him $1,200 annually. He was a member of the state legislatures of 1874-5 and was seven years county commissioner of Sherburne county.

Mr. Chadbourne was married in 1852 to Deborah Crowell. They have three sons and two daughters.

CHAPTER XII.

CHISAGO COUNTY.

LOCATION--SURFACE--SCENERY.

Chisago county, located on the west bank of the St. Croix river, between the counties of Pine on the north and Washington on the south, the St. Croix river on the east and the counties of Isanti and Anoka on the west, presents an agreeable variety of surface, upland and generally undulating, covered with hard and soft wood timber, well watered by lakes and streams. Its princ.i.p.al streams are the St. Croix and its tributaries, Rush and Sunrise rivers and Goose creek, and its princ.i.p.al lakes are Chisago, Sunrise, Green, Rush, and Goose lakes.

Its lake scenery is unsurpa.s.sed in beauty. The county takes the name of its largest and most beautiful lake. In its original, or rather aboriginal, form it was Ki-chi-sago, from two Chippewa words meaning "kichi," large, and "saga," fair or lovely. For euphonic considerations the first syllable was dropped.

CHISAGO LAKE.

This lake is conspicuous for its size, the clearness of its waters, its winding sh.o.r.e and islands, its bays, peninsulas, capes, and promontories. It has fully fifty miles of meandering sh.o.r.e line. Its sh.o.r.es and islands are well timbered with maple and other hard woods.

It has no waste swamps, or marsh borders. When the writer first came to Taylor's Falls, this beautiful lake was unknown to fame. No one had seen it or could point out its location. Indians brought fish and maple sugar from a lake which they called Ki-chi-sago Sagi-a-gan, or "large and lovely lake." This lake, they said, abounded with "kego,"

fish.

In 1851 the writer, with Bart Emery, made a visit to this beautiful sheet of water. We found it what its Indian name imports, "fair and lovely water." The government had, the year before, completed a survey of the lake, and it was high time that it should be given a name by which it should be designated on the map and recognized by civilized visitors. What name more beautiful and appropriate than that which the Indians had already given it. That name we at once recognized and used all our influence to perpetuate under somewhat adverse influences; for Swedish emigrants having settled in its neighborhood, a strong effort was made to christen it "Swede Lake," but the lake is to-day known as Chisago, and Chisago it is likely to remain. We believe in the policy of retaining the old Indian names whenever possible. As a rule they are far more musical and appropriate than any we can apply. The Indians have left us their lands, their lakes, their streams; let us accept with them the names by which they were known. Some have been translated into English and appear on the maps as Goose, Elk, Beaver and Snake. By all means let us retranslate them in memory of the race that once owned them.

DALLES OF ST. CROIX.

Chisago county shares with Polk county in the ownership of the wildest and most peculiar scenery in the valley of the St. Croix. At Taylor's Falls, the head of navigation, the river flows between ledges of trap rock, varying in height from fifty to two hundred and fifty feet, for the most part perpendicular, but wildly irregular, as is common in trap rock formations. These ledges are crowned with pine trees and a dense undergrowth of bushes and vines. The prevailing color of the rock is a cold or bluish gray, but broken occasionally by brilliant patches of coloring, red, yellow or green, as they may be stained by oxides of the metals, or covered with lichens and mosses. This formation is known as "The Dalles," sometimes improperly styled "Dells." The rocks composing it are porphyritic trap, an igneous rock forced upward from the interior of the earth through crevices in the crust while still in a liquid state and then solidifying in ma.s.ses, sometimes prismatic but oftener in irregular polygons, and broken by parallel lines of cleavage. Some geological experts claim that these rocks are "in place" as forming a part of the original crust of the earth, but the balance of evidence seems to be in favor of their having been erupted at a comparatively modern period. This is evidenced by the presence of water-worn boulders and pebbles, imbedded in the trap, somewhat like plums in a pudding, while it was yet plastic; and now forming a species of conglomerate as hard and compact as the trap itself. These rocks are supposed to be rich in copper and silver, and miners have spent much time in prospecting for these metals.

Whatever the origin of the rocks, it is conceded that they were once plastic, at which time this region could not have been a safe or pleasant dwelling place for such beings as now inhabit the world. The theory of a comparatively recent eruption of these rocks is not a pleasant one, for the suggestion forces itself upon the mind that that which has been, at least in recent times, may occur again. The occasional recurrence of earthquakes on our western coast, and the recent severe disturbances in South Carolina and Georgia, raise the query whether this region may not again be visited with an outburst and overflow of trap, terrible and destructive as the first. The foundations, however, seem firm enough to last forever. The rocks are of unusual hardness, and the crust of the earth is probably as solid and thick here as elsewhere. The Dalles proper are about one mile in length. The river, in its pa.s.sage through them, varies in width from one hundred and fifty to three hundred feet. It was formerly reported unfathomable, but in recent years, owing to a filling up process caused by the debris of the log drivers, it is found to be not more than a hundred feet in its deepest place. The river makes an abrupt bend about a bold promontory of trap known as Angle or Elbow Rock. To the first voyageurs this seemed to be the end of the river, and gave rise to the story that at this point the river burst out of the rocks.

Much of the frontage of the rocks upon the river is smooth and perpendicular, and stained with oxides of iron and copper. In places it is broken. The upper rocks are disintegrated by the action of rain and frost, and, where far enough from the river, have fallen so as to form a talus or slope of angular fragments to the water's edge.

[Ill.u.s.tration: THE DEVIL'S CHAIR.]

THE DEVIL'S CHAIR.

There are some instances in which, by the breaking away and falling of smaller rocks, larger rocks have been left standing in the form of columns. Most notable of these are the "Devil's Pulpit," and the "Devil's Chair." The former, owing to surrounding shrubbery, is not easily seen. The latter is a conspicuous object on the western sh.o.r.e of the river a few rods below the lower landing. It stands on the slope formed by the debris of a precipice that rises here about 120 feet above the river. Its base is about 40 feet above low water mark; the column itself reaches 45 feet higher. It is composed of many angular pieces of trap, the upper portion bearing a rude resemblance to a chair. It is considered quite a feat to climb to the summit. The face of the rocks is disfigured by the names of ambitious and undeserving persons. The nuisance of names and advertis.e.m.e.nts painted upon the most prominent rocks in the Dalles is one that every lover of Nature will wish to have abated. To spend an hour climbing amongst these precipices to find in some conspicuous place the advertis.e.m.e.nt of a quack medicine, ill.u.s.trates the adage: "There is but one step from the sublime to the ridiculous."

THE WELLS.

A more remarkable curiosity may be found on that bench or middle plateau of the Dalles, lying between the upper and the lower Taylor's Falls landings, in what has been not inaptly styled "The Wells." These are openings, or pits, not much unlike wells, in places where the trap is not more than 50 feet above water level, varying in width from a few inches to 30 or 40 feet, the deepest being from 20 to 25 feet.

These seem to have been formed by the action of water upon pebbles or boulders, much as "pot holes" are now being formed in the rocky bottoms of running streams. The water falls upon the pebbles or boulders in such a way as to cause them to revolve and act as a drill, boring holes in the rock proportioned to the force of the agencies employed. Some of these boulders and pebbles, worn to a spherical shape, were originally found at the bottoms of these wells, but have been mostly carried away by the curious. Some of the wells are cut through solid pieces of trap. The walls of others are seamed and jointed; in some cases fragments have fallen out, and in others the entire side of the wells has been violently disrupted and partly filled with debris. The extreme hardness of the trap rock militates somewhat against the theory of formation above given. It is, however, not improbable that this hardness was acquired after long exposure to the air.

SETTLEMENT AND ORGANIZATION.

In the history of St. Croix Falls mention has been made of some of the pioneers of Chisago county. St. Croix Falls and Taylor's Falls, the pioneer settlement of Chisago county, though a river divides them which is also the boundary line of two states, have much that is common in their early history. The inhabitants were always greatly interested in what was going on over the river. We may add, that although they now stand in the att.i.tude of rival cities, their interests are still identical, and we believe that, but for the unwise policy of making St. Croix river a state line, they might be to-day under one city government, and as compact and harmonious as though no St. Croix river rolled between them. The river is their joint property; both have the same heritage of trap rocks and pines, the same milling privileges, the same lumbering interests, and, it must be confessed, they remain up to the present time about equally mated. J.

R. Brown was unquestionably the pioneer of the settlement. Frank Steele says he found J. R. Brown trading, in 1837, on the spot now the site of Taylor's Falls.

He was not, however, the first white man upon the soil. There is some doc.u.mentary evidence of the establishment by the French of a fort forty leagues up the St. Croix some time between the years 1700 and 1703. This fort was in all probability erected on the plateau below the Dalles, the distance given, forty leagues, being exaggerated after the fashion of the early voyageurs. It was called Fort St. Croix.

There was also a prehistoric settlement, the ruins of which the writer noted as early as 1851, on the school land addition to Taylor's Falls.

These were the foundations of nine houses, plainly visible. Over some of them trees two feet in diameter were growing. The rock foundations ranged in size from twenty to thirty feet, with the hearth containing ashes underlying the debris of ages, on smooth hearthstones showing years of service, being apparently a century old. These were the homes, undoubtedly, of a civilized people, and we may claim for Taylor's Falls, Chisago county, one of the first improvements made by whites in the limits of Minnesota.

During the last half of the last century a prominent trading post was established and maintained for many years on the St. Croix river, which was founded by Pierre Grinow, and during the close of the last century it was in the charge of one James Perlier, who afterward became one of the most useful citizens of Green Bay, Wisconsin.

Lawrence Barth was also here in 1793. The evidence of the existence of this trading post rests upon traditions and the ruins referred to.

Recurring to the pioneer Brown, the most irrepressible of all the advance guard of civilization, we find him only a transient inhabitant. He stayed long enough to cut 200,000 feet of pine logs from the present site of Taylor's Falls, when the neighborhood lost its attractions. These were the first pine saw logs cut in the St.

Croix valley.

In 1838 a French trader, Robinet, was located at the same place, but in the summer of the same year came Mr. Jesse Taylor from Fort Snelling where he had been following the business of a stonemason. He had heard of the ratification of the Indian treaty by Congress, and he greatly coveted some of the rich lands brought into market by that treaty. Mr. Taylor, with an Indian guide, came to the Dalles of the St. Croix. As Mr. Steele had already claimed the east side, Mr. Taylor concluded that he would claim the west side. Returning to Fort Snelling he reported to an a.s.sociate, Benjamin F. Baker, formed a partnership and returned with men, boats, provisions and building material, but on his return to the falls he found Robinet, the trader, in a bark shanty (at the present junction of Bridge and River streets). Robinet was in actual possession of the coveted acres.

Robinet having no other function than that of a trader, and consequently having no serious designs on the lands was easily bought off, and Baker & Taylor, in August, 1838, commenced improvements, building a log house, a blacksmith shop, a mill, and commencing a mill race which had to be blasted. They also built piers and a wing dam just above the present location of the bridge. The mill was located at what has since become the upper steamboat landing. Mr. Taylor named the lower falls Baker's falls, and the settlement, Taylor's Place.

When the town was platted, in 1850, it was called Taylor's Falls. The name came also to be applied to the lower falls.

The mill enterprise was a melancholy failure. The builders were not practical mill men. The improvements were expensive. The work of blasting rock and building made slow progress. There was no income as long as the mill was in process of building. In the midst of these embarra.s.sments, in 1840, Mr. Baker died. Mr. Taylor took entire possession with no other right than that of a squatter sovereign. In 1843 Mr. Taylor sold the unfinished mill to parties in Osceola, and in 1844 everything movable was transferred to that place. The double log cabin remained, and there Mr. Taylor lived for eight years on the proceeds of the sale, performing in all that time no work more worthy of the historian's notice than fixing his name upon the settlement and falls. Many of the later residents query as to why it was ever called Taylor's Falls. It takes a keen eye to discover any fall in the river at the point named. The falls indeed were once far more conspicuous than they are now, owing to the fact that a large rock rose above the water at the ordinary stage, around which the crowded waters roared and swirled. That rock, never visible in later days, was called Death Rock, because three hapless mariners in a skiff were hurled against it by the swift current and drowned.

The old log house, the sole remnant of the Baker and Taylor project, if we may except some holes in the rock made by blasting, and some submerged ruins of the wing dam and pier, has pa.s.sed through various changes. It has been used as a store, as a boarding house, as a warehouse, as a church, as a school house, and as a stable. Part of it still remains and is habitable. It is located on lot 18, block 15. In 1846 Jesse Taylor sold his claim to Joshua L. Taylor for two hundred dollars. This claim, like most of the claims made prior to the survey of government lands, was not accurately defined. It included, however, all the lands, on the west side of the river, extending northward to the St. Croix Company's claim, at the upper falls, and including the present site of Taylor's Falls.