I. Strange Land of “Volcanoes” and “Shining Mountains”

The Yellowstone-Grand Teton region was not officially discovered and its

scenic marvels were not publicly proclaimed until the 1870’s, beginning

with the Washburn-Langford-Doane expedition. For thirty years before,

from 1841 to 1869, this region was a Paradise Lost, rarely visited by

white men. But for thirty years before that, or from 1807 to 1840, this

region had hundreds of appreciative visitors. These were the Rocky

Mountain fur trappers. While searching for the golden-brown fur of the

beaver, destined for the St. Louis market, these adventurers thoroughly

explored this fabulous region. Although news of their discoveries

received scant public notice back in the settlements, or was discounted

as tall tales, to them belongs the honor of being the first actual

explorers of these twin parks.

Neighboring Yellowstone and Grand Teton, established as National Parks

in 1872 and 1929, respectively, are separately managed today as units of

our National Park System. But geographically, now as well as in the

early nineteenth century, they embrace one unique region, characterized

by topographic and geologic features that are the crescendo of a great

scenic symphony. Here, at the heart of the continent, the source of the

three major river systems of the continent—the Columbia, the Colorado,

and the Missouri-Mississippi—may be found the greatest geyser basins,

the largest mountain lake, the most colorful of kaleidoscopic canyons,

one of the richest arrays of wildlife, and one of the most spectacularly

beautiful mountain ranges in the world. The Yellowstone-Grand Teton

region has historical unity, also, particularly during the obscure but

heroic age of the Rocky Mountain fur trade.

“Colter’s Hell”—bearing the name of the legendary discoverer, and

conjuring up visions of a primitive “Dante’s Inferno”—is the term which

visitors today associate with the early history of Yellowstone National

Park and its universally famous hydrothermal wonders. Actually, the

wandering, bearded, buck-skinned beaver trappers never referred to the

geyser region of the upper Madison as Colter’s Hell. As we will see, the

real Colter’s Hell in Jim Bridger’s day was another place altogether,

having nothing to do with anything within Yellowstone Park itself. In

trapper times the Yellowstone geyser area had no fixed name but was

variously described by them as a region of “great volcanoes,” “boiling

springs” or “spouting fountains.” On the recently discovered Hood and

Ferris maps (see below) it is labeled “the Burnt Hole” (although this

name seems to have been restricted by Russell and others to the Hebgen

Lake Valley). Captain Bonneville tells us that his men knew of this

region as “the Firehole” and this name, as applied to the river draining

the geyser basins, survives today.

Yellowstone Park, carved out of territorial Wyoming, Montana, and Idaho,

is a rough-edged rectangle of 3,500 square miles that straddles the

twisting course of the Continental Divide. It is a geological circus, a

unique creation of ancient volcanoes and glaciers, flanked on the

southeast and east by the Absaroka Range, on the north by the Snowy

Range, on the northwest by the Gallatin and Madison ranges, on the west

by the Centennial Range, and on the south by the Teton Mountains.

From the Park flow the headwaters of two continental rivers and their

major tributaries. From here the Snake River arcs southward toward

Jackson’s Hole and the cathedral-like Tetons, destined to join the

Columbia River and the Pacific Ocean. Here the Firehole and Gibbon

rivers, draining the principal geyser basins, unite to become the

Madison River, and here also arises the Gallatin, these being two of the

Three Forks of the Missouri. Here arises a branch of the North Fork of

the Shoshone River, a tributary of the Bighorn. And here, after its

birth near Two Ocean Pass, begins the mighty Yellowstone River which,

after passing through its vast mirror-like lake and its prismatic

canyon, flows out onto the plains to receive the Bighorn and join the

Missouri on its marathon journey to the Mississippi River and the Gulf

of Mexico.

[Illustration: Indians at Jackson Lake.]

This region held a fortune in coveted beaver skins, but it was remote,

snowbound, haunted by the vindictive Blackfeet, and plagued by weird

visions, sulphurous fumes, and uncanny noises. Here indeed was fertile

soil for a legend.

On a clear day Yellowstone Park visitors can see to the south the

mountain spires which identify Grand Teton National Park of Wyoming, an

indefinable shape of 500 square miles. (The actual boundaries of these

neighboring parks are separated by a scant five miles.) The Tetons are

perhaps the most distinctive of the granite giants which comprise the

Rocky Mountains. A series of sharp pyramids of naked rock, the peaks

stand like sharks’ teeth against the sky. The most precipitous sides and

the most needle-like summit belong to the highest of these, the Grand

Teton, which rises over 7,000 feet from its immediate base, nearly

14,000 feet above the level of the distant sea.

The Teton Mountains are the most conspicuous landmarks of a region which

contains the scrambled sources of the three greatest river systems of

continental United States. As we have seen, Yellowstone Park to the

north gives birth to the eastward-flowing Missouri and the westward

flowing Columbia waters. East of the Tetons, in the Wind River

Mountains, is the head of Green River which rolls southward to merge

into the mighty Colorado River, tumbling through the arid lands to the

Gulf of California.

Jackson’s Hole is that part of the Upper Snake River Valley which lies

at the eastern base of the Teton Range. One of the largest enclosed

valleys in the Rocky Mountains, its glaciated floor extends about sixty

miles north and south, and varies up to twelve miles in width. It is

bounded on the west by the Tetons, on the east and south by the less

pretentious Mount Leidy Highlands and the Gros Ventre and Hoback

Mountains. The Gros Ventres merge imperceptibly into the Wind River

Mountains farther east, the crest of which forms the Continental Divide.

The southern extremity of the Tetons merges with the eastern end of the

Snake River Range near the canyon where the Snake River escapes from the

valley.

Historic Jackson’s Hole, also known as “Jackson’s Big Hole”—but now

politely refined to just plain Jackson Hole—was named in 1829 for David

Jackson, one of the partners of the Rocky Mountain Fur Company. To the

early trapper a “hole” was a sizeable valley abounding in game, and

usually (with the exception of Yellowstone’s “Firehole”) associated with

some distinctive personality—hence Brown’s Hole, Pierre’s Hole,

Gardner’s Hole, etc. However, Jackson’s Hole was more than just a

pleasant spot for trapping and camping. Research gives substance to the

view that this was the historic crossroads of the Rocky Mountain fur

trade.

Jackson’s Hole was destined by geography to become a traffic center of

the Western fur trade. Between South Pass at the head of the Little

Sandy and the northern passes above the Three Forks of the Missouri it

offered the most feasible route across the Rocky Mountain barrier. In

addition, it was the focal point of a region that was highly prized and

vigorously contested because of its populous beaver streams. Here

trappers’ trails converged like the spokes of a great wheel and, after

Lewis and Clark, most of the important trapper-explorers crossed

Jackson’s Hole on their journeys.

[Illustration: Indian “Buffalo Jump”—Yellowstone Valley.]

In historic times there were seven gateways to and from Jackson’s Hole:

northward up Snake River; northeastward up Pacific Creek to Two Ocean

Pass; eastward up Buffalo Fork to Twogwotee Pass; eastward up the Gros

Ventre to Union Pass; southward up the Hoback to Green River; westward

via Teton Pass or Conant Pass (at the south and north extremities of the

Teton Range) to Pierre’s Hole.

[Illustration: “Dawn of Discovery”—Exhibit in Fur Trade Museum, Grand

Teton National Park.]

The Tetons received their name from French-Canadian trappers who

accompanied the earliest British expeditions into this territory. As

they approached the range from the west, they beheld three towering

mountains upon which they bestowed the name of “Trois Tetons” (“Three

Breasts”). This romantic designation was readily adopted by the lonely

trapping fraternity to whom the sharp snowy peaks (now known as the

Grand, Middle and South Tetons) became a beacon to guide them through

the hostile wilderness. To the Indians the Tetons were variously known

as “The Three Brothers,” “The Hoaryheaded Fathers,” and “Tee Win-at,”

meaning “The Pinnacles.” The earliest Americans in the region, being

more practical than romantic, could find no better name for the silvery

spires than “The Pilot Knobs,” while an official Hudson’s Bay Company

map indicates with equal homeliness, “The Three Paps.” The name “Three

Tetons” survived, however, and was officially recognized by

cartographers. The name first appeared publicly in the Bonneville Map of

1837.

The Upper Snake River (i.e., above the mouth of Henry’s Fork) was called

“Mad River” by the Astorians. Others simply referred to it as the

“Columbia River” or “the headwaters of the Columbia,” but to most of the

fur trappers it was “Lewis River” or “Lewis Fork,” so originally named

in the Clark Map of 1810 for Capt. Meriwether Lewis, as Clark’s Fork of

the Columbia was named after his fellow explorer, Capt. William Clark.

This name was much more appropriate than its present one, which is

derived from the Snake or Shoshone Indians, and first appears on the

Greenhow Map of 1840.

In spite of past efforts by water power advocates to “improve” it by a

dam, Yellowstone Lake remains just as it was when first discovered by

John Colter, the original “Lake Eustis” of the Clark Map of 1810.

Jackson Lake, however, was enlarged by a dam built in 1916 by the Bureau

of Reclamation. This lake is identifiable with the “Lake Biddle” of the

Clark Map of 1810, the “Teton Lake” of Warren A. Ferris, and the “Lewis

Lake” referred to frequently by another trapper, Joseph L. Meek. There

is today a tributary of the Upper Snake known as Lewis River, heading in

a Lewis Lake within the confines of Yellowstone National Park, neither

of which are to be confused with the historic “Lewis River” and “Lewis

Lake.”

[Illustration: Grand Canyon of the Yellowstone.]

[Illustration: POWDER HORN]

Colter's Hell and Jackson's Hole The Fur Trappers' Exploration of the Yellowstone and Grand Teton Park Region · 第 3 / 11 题