Late Arrivals

Later arrivals in and near Arches National Park included first Spanish

explorers, then trappers, cattlemen, cattle rustlers and horse thieves,

followed in the present century by oil drillers, uranium hunters,

jeepsters, and tourists. Butch Cassidy, the Sundance Kid, and other

members of The Wild Bunch are known to have frequented parts of what is

now Canyonlands National Park (Baker, Pearl, 1971), but it is not

certain whether or not any of them traversed what is now Arches National

Park.

The first settler in what is now Arches National Park was a Civil War

veteran named John Wesley Wolfe, who was discharged from the Union Army

about 3 weeks before the Battle of Bull Run because he suffered from

varicose veins. In 1888 his doctor told him he had to leave Ohio for a

dryer climate or he would not live 6 months, so he took his son Fred

west and settled on a tract of 150 acres along the west bank of Salt

Wash, where his “Wolfe cabin” still stands (figs. 1, 3). From family

letters and newspaper clippings compiled by Mrs. Maxine Newell and other

members of the National Park Service (Maxine Newell, written commun.,

1971), we learn what life in the area was like:

We have started a cattle spread on a desert homestead. We call it the

Bar-DX Ranch. Fred and I live in a little log house on the bank of a

creek that is sometimes dry, sometimes flooded from bank to bank with

roaring muddy water. We are surrounded with rocks—gigantic red rock

formations, massive arches and weird figures, the like of which youve

[sic] never seen. The desert is a hostile, demanding country, hot in

summer, cold in winter. The Bar-DX Ranch is a day’s ride from the

nearest store, out of the range of schools.

Although John Wolfe had promised his wife and his other children that he

would return home the first fall that his cattle sales netted enough

money, he and Fred stayed on and on, and his wife refused to go west and

join her husband and son. Eighteen years later he sent money from his

pension check to his daughter, Mrs. Flora Stanley, his son-in-law, Ed

Stanley, and his two grandchildren, Esther and Ferol, to join him and

Fred at the ranch. Their train was met at Thompson Springs (now

Thompson), Utah (fig. 7), by John Wolfe for the 30-mile ride to the

ranch by horse and wagon. Sight of the tiny log cabin with only a dirt

floor brought tears to his daughter’s eyes, but her spirits rose

considerably after John Wolfe promised to build a new log cabin with a

wooden floor. But the children were enchanted with this strange country,

with the building of the new cabin, and, especially, with getting to go

rabbit hunting with Grandpa Wolfe. The Stanleys stayed at the ranch

until Esther was 10, then moved to Moab to await the arrival of their

third child, Volna.

In 1910 John Wolfe sold the Bar-DX Ranch, and the entire family moved to

Kansas. John Wolfe later moved back to Ohio, and died at Etna, Licking

County, on October 22, 1913, at the age of 84, 25 years after his doctor

had warned him to move to a dryer climate or face an early death.

Wolfe had sold his spread to Tommy Larson, who later sold it to J. Marv

Turnbow and his partners, Lester Walker and Stib Beeson. The old log

cabin gradually came to be known as the “Turnbow cabin,” and this name

appeared on early maps of the area by the U.S. Geological Survey and on

early pamphlets by the National Park Service, partly because Marv

Turnbow served as a camphand in 1927 assisting in the first detailed

geologic mapping of the area (Dane, 1935, p. 4). In 1947 the ranch was

sold to Emmett Elizondo, who later sold it to the Government for

inclusion in what was then the monument.

From information supplied by Wolfe’s granddaughter, Mrs. Esther Stanley

Rison, and his great-granddaughter, Mrs. Hazel Wolfe Hastler, who

visited the cabin in July 1970, the original name Wolfe cabin, or Wolfe

Ranch, has been restored, and appears on the newer maps and pamphlets.

(See fig. 1.) What remains of Wolfe’s Bar-DX Ranch is shown in figure 3.

[Illustration: WOLFE’S BAR-DX RANCH, on west bank of Salt Wash at

start of trail to Delicate Arch. Left to right: Corral, wagon, “new”

cabin, and root cellar. “Old” cabin, which formerly was to right of

photograph, was washed away by a flood in 1906. (Fig. 3)]

Arches National Park is surrounded by active uranium and vanadium mines

and by many test wells for oil, gas, and potash; it is underlain by

extensive salt and potash deposits. Oil and gas are produced a few miles

to the north and east, and potash is being produced about 12 miles to

the south (Lohman, 1974).

Uranium and vanadium have been mined on the Colorado Plateau since 1898

(Dane, 1935, p. 176) and in the Yellow Cat area (also called Thompson’s

area), just north of the park (fig. 1), since about 1911 (Stokes, 1952,

p. 7). The deposits in the Yellow Cat area occur in the Salt Wash

Sandstone Member of the Morrison Formation (fig. 4). According to Pete

Beroni (U.S. Atomic Energy Commission, oral commun., August 6, 1973),

some ore is still being produced in the Yellow Cat area, and the

production of vanadium ore will increase as soon as the uranium mill at

Moab is converted to also handle vanadium ore. The Corral and so-called

Shinarump mines along the southwest side of Moab Canyon just north of

Sevenmile Canyon (fig. 1) are still actively producing uranium ore from

the Moss Back Member of the Chinle Formation, according to Mr. Beroni.

The occurrences of salt and potash in and near the park and the attempts

to find oil and gas nearby are discussed in a recent report (Hite and

Lohman, 1973), and the deposits beneath Moab, Salt, and Cache Valleys

are discussed in later chapters.

In 1955 and 1956 the Pacific Northwest Pipeline, known also as the

“Scenic Inch,” was constructed by the Pacific Northwest Pipeline Corp.

to transmit natural gas from wells in the San Juan Basin of northwestern

New Mexico for a total of 1,487 miles to the Pacific Northwest, with

additional pickups from gas fields in northeastern Utah, northwestern

Colorado, and southwestern Wyoming (Walters, 1956). This 26-inch

pipeline follows the general route of U.S. Highway 163 from Cortez,

Colo., past Moab to Sevenmile Canyon 10 miles northwest of Moab, where

it turns abruptly to the northeast and crosses about the middle of

Arches National Park. It crosses the park road and the flat area between

the Fiery Furnace and the southeast end of Devils Garden, but the scars

are so well healed that most visitors are unaware of its existence

unless they happen to look southwestward across Salt Valley, where the

filled excavation is still visible. The filled trench also appears in

the lower middle of figure 23.

Unlike Canyonlands National Park a few miles to the south, Arches was

not on the route of the famous early-day river expeditions of John

Wesley Powell or of most of those that followed; however, the

southeastern boundary of the park is the Colorado River, formerly the

Grand, which was traversed by the first leg of the ill-fated

Brown-Stanton expedition (Dellenbaugh, 1902, p. 343-369; Lohman, 1974).

The canyon of the Colorado River along the southeastern park boundary is

deep and beautiful and is a favorite stretch of quiet water for boaters

and floaters. Partly paved State Highway 128 on the east bank is a part

of a most scenic drive from Moab to Cisco—a small railroad town about 32

miles northeast of the eastern border of figure 1 (fig. 7). This road

has been variously called the “Moab Mail Road,” the “Cisco Cutoff,” the

“Dewey Road,” or the “Dewey Bridge Road” after an old suspension bridge

(fig. 7) across the Colorado River at the old townsite of Dewey about 12

miles south of Cisco. During the summer this deep colorful canyon may be

viewed at night by artificial illumination. Each evening one-half hour

after sundown, an 80-passenger jet boat leaves a dock north of the

highway bridge, carries passengers several miles upstream, then floats

slowly downstream followed by a truck on the highway carrying 40,000

watts of searchlights which play back and forth on the colorful red

canyon walls, while the passengers listen to a taped discourse. The

entire trip requires about 2 hours.

The spectacular arches and red rocks of Arches and vicinity have been

used to advantage in making color movies and color TV shows. Parts of

the recent Walt Disney film “Run, Cougar, Run” were filmed beneath

Delicate Arch (fig. 43), in Professor Valley of the Colorado River just

east of the park (fig. 7), and in other sections of the canyon country.

Ever since military jet aircraft broke the sound barrier, there has been

a growing number of protests from concerned citizens, organizations, and

National Park Service officials concerning the dangers sonic booms have

posed to Indian ruins and delicate erosional forms in our national parks

and monuments, such as natural bridges, arches and windows, balanced

rocks, and natural spires or towers. Many instances of damaged ruins,

roads, erosional forms, and broken windows were reported. My wife and I

can vouch for the destructive power of such booms, for in October 1969,

while we were having breakfast at Squaw Flat Campground in The Needles

section of Canyonlands National Park, a particularly severe blast from a

low-flying jet not only violently rocked our jack-supported trailer but

broke the windshield of our car.

At Arches National Park, particular fear was felt for Landscape Arch

(fig. 53), thought to be the longest natural stone arch in the world,

and many a special round trip from headquarters involving 47 road miles

and 2 trail miles was made to check on the condition of this arch after

especially loud sonic booms were heard. Finally, in April 1972,

following a rash of newspaper and magazine articles that spread across

the nation, the Secretary of the Air Force put a virtual stop to this

danger by ruling that, except in an emergency (Moab Times-Independent,

April 12, 1972):

Supersonic flights must not only avoid passing over national parks,

they also may not fly near them, according to the new regulation. For

each 1,000 feet of altitude, the pilot must allow one-half mile

between the flight path and the park boundary. The regulation also

prohibits supersonic flights below 30,000 feet (over land) so the high

speed planes must allow 15 miles between the nearest park boundary and

the flight path.

Let us hope that with the aid of this long-needed regulation and

cooperation from visitors, the arches will remain intact for many more

generations to see.

[Illustration: Petroglyph figure]

The Geologic Story of Arches National Park Geological Survey Bulletin 1393 · 第 9 / 32 题