"A river sings a holy song conveying the mysterious truth that
we are a river, and if we are ignorant of this natural law, we are
lost."
- From The Re-Enchantment of Everyday
Life
In
the land of wicked whitewater, the Arkansas River rules the roost.
One of the most popular rafting
rivers in the world, the Arkansas cascades through Chaffee County
carving its way into the granite canyons of Chaffee, Lake and Fremont
Counties. With a length of
1,450 miles it is the longest tributary in the Missouri-Mississippi
system, and is the 4th longest river in the United
States. Beginning as a small
trout stream south of Fremont Pass at the Continental Divide, the
Arkansas plunges 5,000
feet in its first 125 miles. After its rambunctious beginnings,
when it finally reaches the Mississippi, it is almost depleted from
irrigation in the midwest. The Arkansas River Basin, draining 24,904
square miles, is Colorado's largest river basin. Major reservoirs
in the Arkansas Basin include Pueblo Reservoir, John Martin Reservoir,
Great Plains Reservoir System, Twin Lakes Reservoir, and Turquoise
Lake. Major tributaries to the Arkansas include Fountain River and
Purgatoire River.
One of the reasons for the popularity of the Arkansas is that.
much of it flows through areas easily accessible by road, so the
possibility of a put-in or a hired run are always good. The whitewater
can range from great to downright breathtaking. Finding an outfitter
is only a problem if they're all booked, as can happen during the
peak season, but there are also stretches of the Arkansas that offer
a little more peace and quiet if you're not up for thrashing the
waves. Below Canyon City, the river becomes noticeably more docile.
As on any river, hazards like submerged trees and occasional riffles
can result in an unexpected swim, but the float between Canyon and
Pueblo Reservoir is ideal for families.
Origins and Geology The Sawatch Range of the
Rocky Mountains was formed between 70 and 72 million years ago during
the Laramide Orogeny (mountain building.)when this massive dome
was lifted up from the low lying central Colorado trough which contained
lated Paleozoic sedimentary rocks. (Karnuta, p. 9) To drain off
the Sawatch Range, streams began flowing eastward forming valleys.
The Arkansas Valley is the northernmost of these valleys and conclusive
geologic evidence establishes that this valley was formed no earlier
than 29 million years ago.
Among the most outstanding features
of the upper Arkansas Valley are the glacial characteristics of
the topography throughout the area. Glacial cirques and U-shaped
valleys can be seen in connection with many tributary streams and
side canyons in the valley. Rocky remnants of giant moraines are
evident from Buena Vista to Salida making the upper Arkansas different
than other major rivers of the region.
History
The Arkansas River is one
of the most historically and economically important rivers in the
United States. Its origins date back to the Pliocene epoch. The
first recorded crossing of the Arkansas River at the ford of the later
Taos or Trappers Trail was made by the Spaniard Ulibarri in 1706.
Ulibarri was in command of a force comprising twenty soldiers, twelve
settlers and one hundred Indian allies, all marching from Santa Fe
to rescue a band of enslaved Picuris from the Cuartelejo Apaches of
present eastern Colorado. He name the Arkansas the Napestle for its
muddy color.
The Arkansas River, named for the
Arkansas Indians of Oklahoma and Kansas through which the river
flows, provided one of the best natural highways into Colorado.
The first white man to explore the upper reaches of the river was
probably Zebulon Pike in 1806 when he led an expedition west of
Pike's Peak. On that same trip he camped for Christmas next to the
Arkansas River at Squaw Creek about four miles north of Poncha Springs
where a historical marker is now located. He was followed by Gen
John C. Fremont who also explored the upper Arkansas. From 1820
to 1846, the River formed the international boundary between the
United States and Mexico. It was therefore the natural route for
traders and trappers. It was
Native Americans hunted along its length and early explorers followed
it westward.
The Arkansas River has three faces. It is first a wild mountain
stream full of rapids and, in Colorado, provides some of the best
white water rafting in the country. It was part of the old Santa
Fe Trail through Kansas, where it becomes a typical braided prairie
river meandering across the flatlands. As it moves south into Oklahoma
and Arkansas, it becomes a significant river for barge traffic as
well as for recreation. From there it travels through hardwood forests
and empties into the Mississippi.
Arkansas Headwaters Recreation Area
Stretching for 148 miles from Leadville
through Chaffee and Fremont Counties to the Pueblo Reservoir, the
Arkansas Headwaters
Recreation Area is a unique park managed by both the Colorado
Division of Parks and the U.S. Bureau of Land Management. Within the
park are numerous recreation sites--some improved and some not. Since
this is a new park, it remains a work in progress with projects such
as its Watchable Wildlife area at Five Points, in Fremont County in
the making. The Park system includes sites in Fremont County at Pinnacle
Rock, Five Points and lone Pine as well as sites in Chaffee County
including Railroad Bridge, north of Buena Vista; Fisherman's Bridge
and Ruby Mountain, near Nathrop; Hecla Junction between nathrop and
Salida: and Rincon, southeast of Salida.
"
Society speaks and all men listen, mountains speak and wise men
listen. "
- John Muir
The legendary Rocky Mountains are perhaps the most prominent asset
of the state of Colorado and of Chaffee County. Few geographic formations
boast the majesty and rugged splendor of these peaks, and equally
few have had such a profound influence on the peoples of the surrounding
regions.
About 70 million years ago, the
shallow inland sea retreated from Colorado for the last time. The
cause of the retreat was a tremendous uplift, the Laramide Orogeny,
of the entire Rocky Mountain chain. A very important consequence
of this orogeny was the deposition of minerals in Colorado. During
the Quartenary Period that followed a vast cooling took place and
as a result immense mountain glaciers were formed. These glaciers
began near the crest of the mountains and slowly ground their ways
down to the valleys.In their paths they left steepened slopes, carved
cirques and deposited great masses of rock at their terminus. The
effects of these glaciers can readily be seen in the glacier carved
cirques of the Sawatch Range.
Sometimes referred to as "the
backbone of the Continent", the Sawatch
Range towers above the Arkansas valley below.The early surveyor
Hayden called the range one of the grandest of eruptive masses on
the continent. Fifteen fourteeners rise in the Sawatch, including
the three highest peaks of the Rockies, more than any other range
in the contiguous 48 states. The Range averages about 20 miles in
width and stretches for 90 miles. The Continental Divide is an integral
part of this portion of the Rocky Mountains. More impressive for
their massiveness and altitude than their ruggedness-----The name
"sawatch" comes from
an Indian word meaning " blue earth."
An expedition in 1869 led by a geology professor at Harvard traversed
Trout Creek Pass to behold three massive, prominent peaks. The three
peaks were named Harvard, Yale and Princeton often referred to as
the Collegiate Peaks of the Sawatch Range. Mt. Columbia was named
later by one of Columbia's alumni, not to be outdone by other academics,
who ascended the peak and named it.
Both the Mosquito Range and the
Sawatch Range are a part of the Laramide Uplift. Sedimentary rocks
of the Mosquito Range dip east and those of the Sawatch, dip west.
Under stream deposits near the town of Granite is Precambrian granite
that is 1750 million years old.
The Upper Arkansas Fourteeners are:
Mount
of the Holy Cross
14,005 (53rd highest)
The northernmost of the Sawatch fourteeners. A remote and rugged
site that was not officially documented until Wm. H. Jackson photographed
it on glass plate in 1873. The Holy Cross areas has been a religious
shrine, a national monument and a bombing range. The cross is a
natural rock formation made visible at distances by snowy conditions.
Mount
Massive
14,421 (2nd highest)
Mt. Massive has seven summits over 14,000 feet and dominates the
Leadville area.
Mount
Elbert
14,433 (Highest point in Colorado)
The highest peak in the Rockies. It was named for Samuel T. Elbert,
territorial governor.
La
Plata Peak
14,336 (5th Highest)
This fourteener sits between Leadville and Aspen. It is an impressive
site seen from Independence Pass.Its north ridge is a destination
for mountaineers who enjoy technical climbing.
Mount
Oxford
14,153 (27th Highest)
Was named by Jerome Hart of the Colorado Mountain Club in 1931.
A Rhodes scholar, he found an appropriate tag for the unnamed peak.
Mount
Belford
14, 197 (19th Highest)
Mount Belford and its neighbors, Mount Oxford and Missouri Mountain
lie along the divide between Clear and Pine Creeks in the northern
part of the county near the ghost towns of Winfield and Vicksburg.
Belford was named for colorado's first US congressman, Rep. jame
Belford,
Missouri
Mountain
14,067 (36th Highest)
Probably named by miners from the state of Missouri.
Huron
Peak
14,005 (52nd Highest)
Located in the same area as the Missouri, Oxford, Belford triad,
this peak can be accessed via the ghosttown of Winfield.
Mount
Havard
14,420 (3rd Highest)
The highest peak in Chaffee County was named in 1864 by a geology
professor from Harvard.
Mount
Columbia 14,073 (35th Highest) Was named in 1916 by Roger Toll of the Colorado Mountain Club
when he found an unnamed peak and christened it with his alma mater's
name.
Mount
Princeton
14,197 (18th Highest)
Mt. Princeton is located at the junction of four USGS maps--Harvard,
Garfield, Buena Vista and Poncha springs. It's magnificent profile
dominates the scenery and is the first peak you see as you make
the descent from Trout Creek Pass.
Mount
Antero 14,269 (10th Highest)
Mount Antero is the tallest peak in Colorado named for an Indian,
Chief Antero of the Uintah band of Ute Indians, who helped keep
peace during the uprisings in the 1860's and 1870's. Antero was
one of the signatories of the Washington Treaty of 1880 which revised
an earlier treaty and led to the Utes losing most of their land.
Antero was a proponent of peace during thedifficult relations between
the Ute and the whites in the late 1860's and 1870's.
Early prospectors in the area looked
at Mt. Antero to be a source of silver--but none was found and no
claim was staked. What was missed was that the peak was a rich source
of gemstones and in 1884, Nathaniel Wanemaker discovered a number
of blue aquamarines near the peak. Since that time, Mt. Antero has
proved an extraordinary source of aquamarines, topaz and clear and
smoky quartz crystals. Some of the clear crystals have been huge
and common smoky quartz crystals have weighed as much as fifty pounds.
Another highly prized mineral found
on Mt. Antero is beryllium, a lightweight, corrosion-resistant,
rigid, steel-gray metal. It is valued as an aerospace structural
material, as a moderator and reflector in nuclear reactors, and
in a copper alloy used for springs, electrical contacts, and non-sparking
tools.
Mount
Shavano 14,229 (17th Highest) Named for Chief Shavano of the Tabeguache band of Ute Indians,
Shavano is usually climbed in tandem with Mt. Tabeguache. Mt. Shavano
Snow Angel is a local legend during the winter.
Tabeguache
Mountain 14,155 (26th Highest)
Named for a band of Ute Indians, Mt. Tabeguache was not considered
to be a separate mountain until 1931.
Wildlife Grab your camera, binoculars,
and spotting scopes to watch wildlife in their natural setting. Colorado's
960 species of wildlife make an extraordinary contribution to the quality
of life we all enjoy in this state and in Chaffee County! The abundance
of wildlife provides a myriad of opportunities for various outdoor activities.
Coexistence with wildlife is an enjoyable part of living in the mountainous
environment of Colorado. The key to coexistence is to respect the wildness
of wildlife. As more houses are built in the mountainous areas and in
the foothills, human and domestic animal encounters with wildlife will
increase. Elk, deer, mountain lion, bear, fox, turkey, beaver, porcupine,
coyote, birds, and other animals are found in this environment.
There are 110 watchable
wildlife viewing areas throughout the state, 25 of which are located
on BLM lands. The official Colorado "Wildlife Viewing Guide"
provides a detailed description of each area, including a map, type of
wildlife in the area, and time of year that is best for viewing. To order,
contact the Colorado Wildlife Heritage Foundation, Attn: Viewing Guide
P.O. Box 211512, Denver, CO 80221: or phone 303-291-7212
The following Colorado Division of Wildlife guidelines are provided to
assist the mountain dweller to better coexist with wildlife:
1. Be aware that mountain lions and bear are most active from dusk
to dawn.
2. Keep your pet under control at all times. Roaming pets are easy
prey for larger predators and more susceptible to injury and disease.
Bring pets in at night or keep them in a kennel with a secure top. Feeding
pets outside can attract mountain lions and bears. Store all garbage
securely.
3. Closely supervise children whenever they play outdoors.
4. Planting non-native shrubs and plants that deer and elk often prefer
to eat encourages wildlife to come onto your property. This can be a
problem because predators follow prey. Note: Elk prefer tulips - but
don't like daffodils.
5. Do not feed wildlife other than songbirds.
6. Place livestock in enclosed sheds or barns at night.
The Valley winters provide an excellent opportunity for viewing wildlife.
Winter snows and cold usually drive game down to lower elevations where
there is more forage. For viewing elk, the best place to look is along
U.S. 285 between Poncha Springs and Centerville where alfalfa fields are
frequent grazing areas and in the Brown's Creek area southwest of Nathrop.In
addition, there is a large herd of elk often visible off County Rd. 306
north of Buena Vista. Another favorite grazing spot is along U.S. 50 from
just below CR 226 to Garfield.The best time to view elk is early morning
or dusk.
Big Horn sheep are
often visible in Chaffee and Fremont counties. The best place to view
them is at Chalk Creek, five or six miles west of US 285 on CR 162 west
of Nathrop near Love Ranch where there is a feeding station. Above the
baiting grounds you can often see rocky mountain goats. The goats frequent
higher, steeper elevations and can be approached up to a moderate distance
before being scared off. Big Horn sheep are also often visible on the
hillsides (and sometimes in the road) in Big Horn Sheep Canyon between
Salida and Parkdale and they have been known to be seen atop Tenderfoot
Mountain.
If you plan a hike up Mt. Shavano,
Mt. Tabeguache or Mt. Antero, you may catch a lucky siting of a mountain
goat. These magnificent animals were first brought into the Upper Arkansas
Valley by the Salida Chapter of the International Order of Rocky Mountain
Goats founded in 1966. The organization encourages the preservation of
the Rocky Mountain goat herd in the Collegiate Peaks area. The work of
this organization has resulted in over 400 of the mountain goats living
in the area around Mt. Princeton. The goats may also be seen on the cliffs
above Cottonwood Lake.
Mule deer and antelope are other large
animals that are highly visible. Mule deer can be seen in many locations
particularly in the early mornings or late evenings.(You can almost always
find some on the golf course in Salida.) Antelope can be observed four
or five miles over Poncha Pass in the open flats and on the mesa north
of Mesa Antero. They may also be seen on the northeast side of CO 291.
Many other species may be observed at
various times. Some, like bobcats and mountain lions, are secretive animals
and sightings are rare. It is not unusual to spot a black bear in late
summer to early fall before hibernation when bears are stocking up for
a long winter's sleep.Though encounters are minimal, campgrounds are a
likely spot to see them and if you are a camper, make sure you take necessary
precautions to prevent them from visiting. Coyotes abound but are elusive
animals so if you see one, look quickly before he is gone.
Photographing wildlife is an exciting and challenging experience. It is
recommended that you use a 400 or faster speed film to capture them.
Birding is a simple past time that requires
little special equipment. Field guides and binoculars combined with a
bit of patience are all that one needs to spend hours of enjoyment studying
the local bird species. But just what types of birds would you expect
to see at 7,000 feet +? Amateur ornithologists might be surprised at the
variety of birds present in the Upper Arkansas Valley. Though there may
be fewer resident species of birds in the Valley than in other places,
it is a natural north-south migration path for various species.The valley's
migration pathway gives one the opportunity to watch birds that migrate
to higher elevations such as Towhees, grosbeaks, tanagers, hummingbirds,
wrens, creepers and nuthatches.
Summer residents of the valley include:
Western and pied-billed grebes, double-crested cormorants, great blue
heron, blue-winged and cinnamon teals, wood duck, Canada goose, mallard,
common merganser and redhead, red-tailed hawk, golden eagle, American
kestrel, ringnecked pheasant, Virginia rail, sora and American coot, killdeer,
spotted sandpiper, California gulls, ringbilled gull, rock dove, mourning
dove, yellow-billed cuckoo, common screech owl, great horned owl, burrowing
owl, common nighthawk, white-throated swift and the broad-tailed hummingbird,
rufous hummingbird, belted kingfisher, common flicker, downy woodpecker,
Eastern and Western kingbirds, Western wood peewee, horned lark, tree,
barn and cliff swallows, Steller's, blue and pinon jays, black-billed
magpie, American crow and black capped and mountain chickadees, house
wren, american dipper, rock wren, gray catbird, American robin, Swainson's
thrush, European starling, red-eyed vireo, warbling vireo, virginia's
warbler, yellow warbler, yellow-ruped warbler, common yellowthroat,yellow-breasted
chat, American redstart, house sparrow, Western meadowlark, yellow-headed
blackbird, red-winged blackbird, Northern oriole, Brewer's blackbird,
common grackle and brown-headed cowbird, blue grosbeak, indigo buting,
lazuli bunting, Cassins and house finches, American goldfinch, lesser
goldfinch, rufous-sided towhee, lark sparrow, chipping sparrows and song
sparrows.
A complete Upper
Arkansas Valley bird checklist will be available at the Heart of the Rockies
Chamber of Commerce information center. The checklist, provided by the
Heart of the Rockies Audubon, will include a list of previously sighted
birds with notations on residence and migratory status.This local chapter
of the National Audubon Society encompasses a large geographic area which
includes Leadville and Texas Creek in the south. A good description of
many species of birds mentioned above can be found on the Colorado
Guide.