Page:The Atlantic Monthly, Volume 17.djvu/345

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1866.]
Communication with the Pacific.
337

9th of March the grass was fair, but little snow had fallen, and the weather was mild. The oxen and cows, owned here by the half-breeds and Indians, obtain good feed, and are in good condition."[1]

This village of St Mary's is sixty miles down the valley from the Big Hole Pass; yet, though so near, snow seldom falls, and the grass is so verdant that horses and cattle subsist the year round on the natural pasturage.

Lieutenant Mullan says of it: "The fact of the exceedingly mild winters in this valley has been noticed and remarked by all who have ever been in it during the winter season. It is the home of the Flathead Indians, who, through the instrumentality and exertions of the Jesuit priests, have built up a village,—not of logs, but of houses,—where they repair every winter, and, with this valley covered with an abundance of rich and nutritious grass, they live as comfortably as any tribe west of the Rocky Mountains. . . . .

"The numerous mountain rivulets, tributary to the Bitter Root River, that run through the valley, afford excellent and abundant mill-seats; and the land bordering these is fertile and productive, and has been found, beyond cavil or doubt, to be well suited to every branch of agriculture. I have seen oats, grown by Mr. John Owen, that are as heavy and as excellent as any I have ever seen in the States; and the same gentleman informs me that he has grown excellent wheat, and that, from his experience while in the mountains, he hesitated not in saying that agriculture might be carried on here in all its numerous branches, and to the exceeding great interest and gain of those engaged in it. The valley and mountain slopes are well timbered with an excellent growth of pine, which is equal, in every respect, to the well-known pine of Oregon. The valley is not only capable of grazing immense bands of stock of every kind, but is also capable of supporting a dense population.

"The provisions of Nature here, therefore, are on no small scale, and of no small importance; and let those who have imagined—as some have been bold to say it—that there exists only one immense bed of mountains at the head-waters of the Missouri to the Cascade Range, turn their attention to this section, and let them contemplate its advantages and resources, and ask themselves, since these things exist, can it be long before public attention shall be attracted and fastened upon this heretofore unknown region?"[2]

CLIMATE OF THE MOUNTAINS.

We have been accustomed to think of the Rocky Mountains as an impassable barrier, as a wild, dreary solitude, where the storms of winter piled the mountain passes with snow. How different the fact! In 1852-53, from the 28th of November to the 10th of January, there were but twelve inches of snow in the pass. The recorded observations during the winter of 1861-62 give the following measurements in the Big Hole Pass: December 4, eighteen inches; January 10, fourteen; January 14, ten; February 16, six; March 21, none.

We have been told that there could be no winter travel across the mountains,—that the snow would lie in drifts fifteen or twenty feet deep; but instead, there is daily communication by teams through the Big Hole Pass every day in the year! The belt of snow is narrow, existing only in the Pass.

Says Lieutenant Mullan, in his late Report on the wagon road: "The snow will offer no great obstacle to travel, with horses or locomotives, from the Missouri to the Columbia."

This able and efficient government officer, in the same Report, says of this section of the country:—

"The trade and travel along the Upper Columbia, where several steamers now ply between busy marts, of themselves attest what magical effects the years have wrought. Besides gold, lead for miles is found along the Kootenay.

  1. Governor Stevens's Report of the Pacific Railroad Survey.
  2. Pacific Railroad Survey. Lieutenant Mullan's Report.