CHAPTER XXII.

Ascent of the Mississippi above Queen Anne's Lake--Reach the primary

forks of the river--Ascend the left-hand, or minor branch--Lake

Irving--Lake Marquette--Lake La Salle--Lake Plantagenet--Encamp at

the Naiwa rapids at the base of the Height of Land, or Itasca

Summit.

A short halt was made on entering Queen Anne's Lake, to examine an

object of Indian superstition on its east shore. This consisted of one

of those water-worn boulders which assume the shape of a rude image, and

to which the Chippewas apply the name _Shingabawassin_, or image-stone.

Nothing artificial appeared about it, except a ring of paint, of some

ochreous matter, around the fancied neck of the image.[161] We were an

hour in crossing the lake southwardly from this point, which would give

a mean rate of five miles. At the point of landing, stood a small,

deserted, long building, which Ozawindib informed me had been used as a

minor winter trading station. I observed on the beach at this spot some

small species of unios, and, at higher points on the shore, helices. We

here noticed the passenger pigeon. The forest exhibited the elm, soft

maple, and white ash. Proceeding directly south from this spot a short

distance, we entered the Mississippi, which was found to flow in with a

broad channel and rapid current. This channel Lieutenant Allen estimated

to be but one hundred yards long, at which distance we entered into a

beautiful little lake of pellucid water and a picturesque margin,

spreading transversely to our track, to which I gave the name of Irving.

Ozawindib held his way directly south through this body of water,

striking the river again on its opposite shore. We had proceeded but

half a mile above this lake, when it was announced that we had reached

the primary forks of the Mississippi. We were now in latitude 47° 28´

46´´. Up to this point, the river had carried its characteristics in a

remarkable manner. Of the two primary streams before us, the one flowing

from the west, or the Itascan fork, contributes by far the largest

volume of water, possessing the greatest velocity and breadth of

current. The two streams enter each other at an acute angle, which

varies but little from due south, as denoted in the diagram.

[161] An object of analogous kind was noticed, during the prior

expedition of 1820, at an island in Thunder Bay of Lake Huron. _Vide_

p. 55.

[Illustration: Primary forks of the Mississippi River, in lat. 47° 28´

46´´.]

Ozawindib hesitated not a moment which branch to ascend, but shooting

his canoe out of the stronger current of the Itascan fork, entered the

other. His wisdom in this movement was soon apparent. He had not only

entered the shallower and stiller branch, but one that led more directly

to the base of the ultimate summit of Itasca. This stream soon narrowed

to twenty feet. We could distinctly descry the moving sands at its

bottom; but its diminished velocity was apparent from the intrusion of

aquatic plants along its shores. It was manifest also from the forest

vegetation, that we were advancing into regions of a more alpine flora.

The branches of the larches, spruce, and gray pines, were clothed with

lichens and floating moss to their very tops, denoting an atmosphere of

more than the ordinary humidity. Clumps of gray willows skirted the

margin of the stream.

It was found that the river had made its utmost northing in Queen Anne's

Lake. From the exit from that point, the course was nearly due south,

and from this moment to our arrival at the ultimate forks, which cannot

exceed a mile and a half or two miles, it was evident why the actual

source of this celebrated river had so long eluded scrutiny. We were

ascending at every curve so far _south_, as to carry the observer out of

every old line of travel or commerce in the fur trade (the sole interest

here), and into a remote elevated region, which is never visited indeed,

except by Indian hunters, and is never crossed, even by them, to visit

the waters of the Red River--the region in immediate juxtaposition

north. This semi Alpine plateau, or height of land for which we were now

pushing directly, is called in the parlance of the fur trade _Hauteurs

de Terre_. It was evident that we were ascending to this continental

plateau by steps, denoted by a series of rapids, presenting step by

step, in regular succession, widespread areas of flat surface spotted

with almost innumerable lakes, small and large, and rice-ponds and

lagoons. Thus, after surmounting the step of the Packagama Falls, we

enter on a wide and far stretching plateau which embraces the great area

of Leech Lake, and its numerous lacustrine beds. This step or plateau

may, in the descending order of the Mississippi, be called the fifth

plateau, and is, by barometrical observation, 1,356 feet above the Gulf

of Mexico. The next, or fourth step, is that of the plateau of Cass

Lake, caused chiefly by the lively waters of the Leech Lake, the Upper

Red Cedar, and the Winnepek outlets. The Cass Lake level extends west of

this lake to the foot of the Metoswa rapids. This is forty-six feet

above the Leech Lake level. The third plateau, on which the Mississippi

spreads itself, is that of the Queen Anne summit, which is elevated by

the Metoswa rapids sixty-four feet above the former. We had now entered

on this third plateau, on which we found the river flowing with a just

perceptible current, and frequently expanding itself in small lakes. On

the first of these, after ascending the left hand, or minor fork, I

bestowed the name of Marquette; and on the second, that of La Salle. We

proceeded beyond these to a third lake of larger dimension, which the

Chippewas call Kubba-Kunna, or the Rest in the Path, being the site of

crossing of one of their noted land-trails; I named it Lake Plantagenet.

Lt. Allen deemed this lake ten miles long and five wide. At a point a

short distance above the head of this lake, we encamped at a late hour.

It was now seven o'clock P. M., and we had been in our canoes sixteen

hours, and travelled fifty-five miles. It was not easy to find ground

dry enough to encamp on, and while we were searching for it, rain

commenced. We had pushed through the ample borders of the Scirpus

lacustris and other aquatic plants, to a point of willows, alders, and

spruce and tamarack, with pinus banksiana in the distance. The ground

was low and wet, the foot sinking into a carpet of green moss at every

tread. The lower branches of the trees were dry and dead, exhibiting

masses of flowing gray moss. Dampness, frigidity, and gloom marked the

dreary spot, and when a camp fire had been kindled it threw its red

glare around on strange masses of thickets and darkness, which might

have well employed the pencil of a Michael Angelo. Tired and overwearied

men are not, however, much given to the poetic on these occasions, and

they addressed themselves at once to the pacification of that uneasy

organ, the stomach. Travelling with men who strangely mix up two foreign

languages, one falls insensibly into the same jargon habits, of which I

convicted myself of a notable instance this evening. I had on landing

and pushing into the forest, laid a green morocco portfolio on the

branches of a little spruce, and could not find it. _Kewau bemuasee_, I

said to one of the men, _en petite chose ver, mittig onsing_? Have you

not seen a small green roll in a sapling? not recollecting that the

middle clause of the sentence, though in regimen with the Ojibwa, could

have only been construed by one familiar both with the Canadian French

and the Algonquin. Such, however, proved to be the case, and he soon

handed me the missing portfolio.

I observed, as the crews of the several canoes threw down their day's

game before the cook, there was a species of duck, the anas canadensis,

I think, which had a small unio attached to one of its mandibles, having

been engaged in opening the shell at the moment it was shot. With every

aid, however, from the tent and the tea-kettle, and our cook's art in

spitting ducks, the night here, in a gloomy and damp thicket, just

elevated above the line of the river flags, and quite in the range of

the frogs and lizards, proved to be one of the most dreary and forlorn.

It was felt that we were no longer on the open Mississippi, but were

winding up a close and very serpentine tributary, nowhere over thirty

feet wide, which unfolded itself in a savanna, or bog, bordered closely

with lagoons and rice ponds. Indian sagacity, it was clear, had led

Ozawindib up this tributary as the best, shortest, and easiest possible

way of reaching to, and surmounting the Itasca plateau, but it required

a perpetual use of hand, foot, paddle, and pole; nor was there a gleam

of satisfaction to be found in anything but the most intense onward

exertion. Besides, I had agreed to meet the Indians at the mouth of the

Crow-Wing River on the 24th of July, and that engagement must be

fulfilled.

At five o'clock the next morning (12th) we were on our feet, and resumed

the ascent. The day was rainy and disagreeable. There was little

strength of current, but quite a sufficient depth of water; the stream

was excessively tortuous. Owing to the sudden bends, we often frightened

up the same flocks of brant, ducks, and teals again and again, who did

not appear to have been in times past much subjected to these

intrusions. The flora of this valley appeared unfavorable. Dr. Houghton

has reported a new species of malva and some five or six other species

or varieties from the general region, but these have not, I think, been

elaborately described. The localities of the known species of fauna

might be marked by the occurrence, on this fork, of the cervus

virginianus, which had not been seen after leaving the Sandy Lake summit

till after getting above the primary forks, which flow from the south

and west.

We toiled all day without intermission from daybreak till dark. The

banks of the river are fringed with a species of coarse marshland grass.

Clumps of willows fringe the stream. Rush and reed occupy spots

favorable to their growth. The forest exhibits the larch, pine, and

tamarack. Moss attaches itself to everything. Water-fowls seem alone to

exult in their seclusion. After we had proceeded for an hour above Lake

Plantagenet, an Indian in the advance canoe fired at and killed a deer.

Although fairly shot, the animal ran several hundred yards. It then fell

dead. The man who had killed it brought the carcass to the banks of the

river. The dexterity with which he skinned and cut it up, excited

admiration. He gave the _moze_, which I understood to mean the hide and

feet, to my guide, Ozawindib. Signs of this animal were frequent along

the stream. But we were impelled forward by higher objects than hunting.

It was, indeed, geographical and scientific facts that we were hunting

for. To trace to its source an important river, and to fix the actual

point of its origin, furnished the mental stimulus which led us to care

but little where we slept or what we ate.

When the usual hour for breakfast arrived, the banks of the river proved

too marshy to land, and we continued on till a quarter past twelve P.

M., before a convenient landing could be made. After this recruit to

stomach and spirits, the men again pushed forward, threading the stream

as it wound about in a savanna, seldom halting more than a few minutes

at a time. Frequently, a shot was fired at the numerous water-fowl, so

abundant on these waters. Sometimes a small unio or anadonta was picked

up from the shores; occasionally a plant pulled up, for the botanical

press. Nowhere was the water found too shallow for our canoes, which

were only embarrassed at some points by the density of vegetable tissue.

Rain showers were encountered during the whole of the day, the

equilibrium of the atmosphere being disturbed by rolling, cumulous

clouds, which often poured down their contents with little warning, and

without, indeed, driving us from our canoes. For, on these occasions,

where a fixed point is to be made, and the showers are not anticipated

to be long or heavy, it is better to travel in the rain and submit to

the wetting, than to attempt landing. Neither can the meal of dinner be

stopped for. At length, at half past five o'clock in the evening, we

came to the base of the highlands of the Itasca or Hauteurs de Terre

summit. The flanks of this elevation revealed themselves in a high,

naked precipice of the drift and boulder stratum, on the immediate

margin of the stream which washed against it. Our pilot, Ozawindib, was

at the moment in the rear; halting a few moments for him to come up, he

said that we were within a few hundred yards of the Naiwa rapids, and

that the portage around them commenced at this escarpment. We had seen

no rock of any species, in place, thus far.

A general landing was immediately made at the foot of the hill, and as

the five canoes came up the baggage was prepared in bundles and packages

for being carried, the canoe-paddles and poles securely tied in bundles,

and the canoes lifted from the water and dried in the sun to make the

transportation of them as light as possible, and mended and pitched

wherever they leaked. It was found that the whole baggage, canoes and

all, could be arranged for eleven back-loads, this being the precise

number of our carriers, white and red; and being ready, Ozawindib led

the way, having a single canoe for his share, and he was soon followed

by the whole line, each one of our sitters falling in this line, charged

with the particular instrument of his observation, or record of it. The

hill was steep, and the footing soft and yielding in the crumbling

diluvion, and the scene, as the party struggled up the ascent, presented

quite a study for the picturesque. Lieutenant Allen carried his

canoe-compass, which I had had mounted by an artisan of Detroit; Dr.

Houghton grasped his hortus siccus under his arms; Mr. Johnston, our

interpreter, had his pipe and fowling-piece, and Mr. Boutwell had

wellnigh lost his pocket-bible and notes, while staying himself against

the treacherous influence of a steep sand cliff. While the party thus

took their way over the hill to cross a peninsula of a mile or two, and

strike the river above the junction of the Naiwa River, I went to

observe the rapids. The river, at this point, is forced through a narrow

gorge, where the water descends with loud murmuring over a series of

rapids, which form a complete check to navigation. The portage is two

miles. I judged the entire descent of the channel, from the beginning to

the terminus of the portage, to be forty-eight feet. Boulders of the

peculiar northern sienite, highly charged with hornblende, and of

trap-rock, or greenstone, quartz, and sandstone, were scattered over

this elevation, and mixed with the more finely comminuted portions of

the same rocks, and of amygdaloids and schistose fragments. Among these,

I observed some specimens of the zoned agate, which identifies the

stratum with the extensive drift formation of the upper Mississippi. It

would seem that extensive amygdaloidal strata formerly extended over

these heights, which have been broken down by the fierce and general

rush of the oceanic currents of the north, which once manifestly swept

over these elevations.

Darkness fell as we reached an elevation overlooking the river above the

Naiwa Rapids, and after some deliberation as to the spot where we should

suffer less annoyance from mosquitos, I proceeded to the lower part of

the valley near the river, and set up my tent there for the night. On

questioning Ozawindib of the Naiwa River, he informed me that it was a

stream of considerable size, and that it originated in a lake on a

distant part of the plateau, which was infested with the copper-head

snake; hence the name. Mr. Allen's estimate of this day's journey was

fifty-two miles. We had reached the second, or Assawa plateau of the

Mississippi, which is, barometrically, seventy-six feet above the Queen

Anne summit, and now had but one more to surmount.

Summary Narrative of an Exploratory Expedition to the Sources of the Mississippi River, in 1820 Resumed and Completed, by the Discovery of its Origin in Itasca Lake, in 1832 · 第 22 / 33 章