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Arkansas River at Wellsville

The Arkansas River


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"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.

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The Mountains

Mt. White, Mt. Antero of the Sawatch Range
" 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 Yale
14,196 (21st Highest)

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.

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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.

Black Bear
Colorado Mtn Sheep in Wells Gulch Fawn

   

Constraints That Exist Where Wildlife is Present

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.

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Chaffee County Wildlife

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.

Remember, when viewing wildlife to be cognizant of watchable wildlife guidelines.

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Bird Watching

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.

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