nal
upheaval. It seems possible that there may have been in this region some
great lake which lifted the waters up to the top of the ridge to begin
their work of corrasion. Such lakes did exist; but lack of space forbids
the further pursuit of this discussion here.
* The character of the Grand River is similar to that of the Green,
but the canyons above the mouth of the Dolores are not so long nor so
deep. The river also carries less water.
Brown's Park, originally called Brown's Hole, after one of the early
trappers, is a fine valley about 35 miles long and 5 or 6 miles wide. It
is, like the few other valleys, an expansion of the canyon walls.
There is considerable arable land, and the place possesses a remarkable
climate. Though its general level is so high, around 5500 feet, it
receives hardly any snow, and for this reason was long a favourite place
for wintering cattle on the drive from Texas to California. It was a
great rendezvous, also, for the early trappers and traders, and here
stood Fort Davy Crockett, in those days famous. It was one of those
necessary places of refuge and meeting, established when the trappers
were pursuing their extermination of the beaver, which once were so
numerous in all the Western country. The river enters this park from
the solitudes of Red Canyon, a splendid chasm, 25 miles long, 2500 feet
deep, and abounding in plunging waters. The name is from the colour
of the sandstone walls. Above it are three short canyons, Kingfisher,
Horseshoe, and Flaming Gorge, aggregating about 10 miles. There are
there no rapids worth mentioning, but the scenic beauty is entrancing.
The walls are from 1200 to 1600 feet, in places extremely precipitous.
Flaming Gorge, with walls 1300 feet, is particularly distinguished
by being the beginning of the long series of close canyons. The river
enters suddenly from Green River Valley, repeating on a smaller scale
the conditions at the entrance to Lodore. From here on up to the Wind
River Range the stream is flanked by occasional cliffs and buttes, but
the country is comparatively open, and the many tributaries often have
fine grassy bottoms. This was the locality of the great rendezvous of
the period from 1825 to 1835, and even later.
Green River Valley is an elevated region, from six thousand to seven
thousand feet above sea. It stretches from the Wind River Mountains on
the north to the Uintas on the south, and is bounded westwardly by
the Wyomi
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