Little Colorado River

{{Short description|River in Arizona, United States}}

{{Infobox river

| name = Little Colorado River

| name_native =

| name_native_lang =

| name_other = {{spell-nv|Tółchíʼíkooh}} {{in lang|nv}}
{{lang|es|Colorado Chiquito}} {{in lang|es}}

| name_etymology =

| image = Grand Canyon North.jpg

| image_size = 300

| image_caption = The Little Colorado River carves a deep canyon just above its confluence with the Colorado

| map = Littlecoloradomap.png

| map_size = 300

| map_caption = Map showing the Little Colorado River basin. The Little Colorado River flows northwest through eastern Arizona to join the Colorado north of Flagstaff.

| pushpin_map =

| pushpin_map_size =

| pushpin_map_caption=

| subdivision_type1 = Country

| subdivision_name1 = United States

| subdivision_type2 = States

| subdivision_name2 = Arizona, New Mexico

| subdivision_type3 = Region

| subdivision_name3 = Apache County, Navajo County, Coconino County

| subdivision_type4 =

| subdivision_name4 =

| subdivision_type5 =

| subdivision_name5 =

| length = {{convert|338|mi|km|abbr=on}}{{cite web

|url=http://nationalatlas.gov/streamer/Streamer/streamer.html

|title=USGS National Atlas Streamer

|publisher=United States Geological Survey

|access-date=2015-01-10

|url-status=dead

|archive-url=https://web.archive.org/web/20140528115344/http://nationalatlas.gov/streamer/Streamer/streamer.html

|archive-date=2014-05-28

}}

| width_min =

| width_avg =

| width_max =

| depth_min =

| depth_avg =

| depth_max =

| discharge1_location=

| discharge1_min = {{convert|150|cuft/s|m3/s|abbr=on}}

| discharge1_avg = {{convert|405|cuft/s|m3/s|abbr=on}}

| discharge1_max = {{convert|120000|cuft/s|m3/s|abbr=on}}

| source1 = West Fork Little Colorado River

| source1_location = Mount Baldy, White Mountains

| source1_coordinates=

| source1_elevation = {{convert|10000|ft|abbr=on}}

| source2 = East Fork Little Colorado River

| source2_location =

| source2_coordinates=

| source2_elevation =

| source_confluence =

| source_confluence_location = Greer

| source_confluence_coordinates= {{coord|34|00|15|N|109|27|24|W|display=inline}}

| source_confluence_elevation = {{convert|8359|ft|abbr=on}}

| mouth = Colorado River

| mouth_location = Grand Canyon, Coconino County

| mouth_coordinates = {{coord|36|11|28|N|111|48|14|W|display=inline,title}}

| mouth_elevation = {{convert|2700|ft|abbr=on}}

| progression =

| river_system = Colorado River

| basin_size = {{convert|26500|sqmi|abbr=on}}

| tributaries_left = Silver Creek

| tributaries_right = Zuni River, Puerco River

| custom_label =

| custom_data =

| extra =

}}

The Little Colorado River ({{Langx|hop|Paayu}}) is a tributary of the Colorado River in the U.S. state of Arizona, {{GNIS|31050}} providing the principal drainage from the Painted Desert region. Together with its major tributary, the Puerco River, it drains an area of about {{convert|26500|mi2|km2}} in eastern Arizona and western New Mexico. Although it stretches almost {{convert|340|mi|km}}, only the headwaters and the lowermost reaches flow year-round. Between St. Johns and Cameron, most of the river is a wide, braided wash, only containing water after heavy snowmelt or flash flooding.

The lower {{convert|57.2|mi|km}} is known as the Little Colorado River Gorge{{GNIS|7095|Little Colorado River Gorge}} and forms one of the largest arms of the Grand Canyon, at over {{convert|3000|ft|m}} deep where it joins the Colorado near Desert View in Grand Canyon National Park. An overlook of the gorge is a Navajo Nation Tribal Park.

Course

The river rises as two forks in the White Mountains of mid-eastern Arizona, in Apache County. The West Fork starts in a valley on the north flank of Mount Baldy at an elevation of nearly {{convert|10000|ft|m}}, while the East Fork starts nearby. The forks meet in a canyon near the town of Greer, forming the main Little Colorado River. It flows into River Reservoir, then leaves the canyon near Eagar. The river then turns north, meandering through Richville Valley, before emptying into Lyman Lake, impounded by an irrigation dam built in 1912.{{cite web |title=Lyman Lake State Park |url=https://azstateparks.com/lyman-lake |access-date=2024-06-12 |website=Arizona State Parks and Trails |publisher=Arizona State Parks}} From there the river continues north, past the town of St. Johns. Shortly afterwards, the river transforms from a perennial stream to an ephemeral wash as it travels northwestwards through Hunt Valley, where it receives the Zuni River, then receiving Silver Creek and the Puerco River—its main tributaries—near the town of Holbrook as it flows into the Painted Desert.{{cite map

|publisher=ACME Mapper

|title=USGS Topo Maps for United States

|cartography=United States Geological Survey

|access-date=2010-01-17

|url=http://mapper.acme.com/}}

Image:Grand Falls of the Little Colorado River near Flagstaff, Arizona.jpg

The Little Colorado passes Joseph City and crosses the Southern Transcon route of the BNSF Railway (originally the Atchison, Topeka and Santa Fe Railroad), now winding north into Coconino County. The river enters the Navajo Nation, and drops over the {{convert|185|ft|m|adj=on}} Grand Falls of the Little Colorado shortly after. Below Grand Falls, the river flows through a short but rugged canyon for about {{convert|15|mi|km}}. Emerging into the desert again, the Little Colorado skirts the eastern edge of Wupatki National Monument and passes the town of Cameron, where it is bridged by U.S. Highway 89.

From Cameron, the Little Colorado River carves an extremely steep and narrow gorge into the Colorado Plateau, eventually achieving a maximum depth of about {{convert|3200|ft|m}}. The depth of the canyon is such that groundwater is forced to the surface, forming numerous springs that restore a perennial river flow. It joins the Colorado deep inside the Grand Canyon, miles from any major settlement. The confluence marks the end of the Marble Canyon segment of the Grand Canyon and the beginning of Upper Granite Gorge.{{cite web|url=http://fire.biol.wwu.edu/trent/alles/GrandCanyon.pdf |title=Grand Canyon of the Colorado |website=Fire.biol.wwu.edu |access-date=2016-07-16}}

=Discharge=

File:Littlecolorado.jpg

The Little Colorado River is one of the two major tributaries of the Colorado River in Arizona, the other being the Gila River.See :File:Coloradorivermap.jpg; the other is the Gila River. Runoff typically peaks twice a year, first in the early spring (February–April) from snow melt and highland rain; and in the summer (July–September) from monsoon storms. The annual runoff is extremely variable with the possibility of no flow occurring due to a weak snow pack or lack of summer rain. Conversely, years such as 1949, 1973, 1979, 1983 and 1993 have seen massive volumes of spring snowmelt while large monsoon runoff has occurred in 1955, 1964, 1984 and 2006. Monthly average flows in the springtime average several hundred cfs and can reach {{convert|2000|to|3000|cuft/s|m3/s}}. Only the upper reaches of the river above St. Johns, and the lowermost stretch below Cameron, flow year round; the middle section is basically a huge arroyo that carries water only during the wet seasons.

According to a streamflow gauge near Cameron, before the river enters the Grand Canyon, the river's average annual flow was {{convert|367.2|cuft/s|m3/s}} from 1948 to present. The highest annual average was {{convert|1127|cuft/s|m3/s}} in 1973, and the lowest was {{convert|14.1|cuft/s|m3/s}} in 2000.{{cite web

|url=http://waterdata.usgs.gov/nwis/annual/?referred_module=sw&site_no=09402000&por_09402000_9=19282,00060,9,1947,2009&year_type=W&format=html_table&date_format=YYYY-MM-DD&rdb_compression=file&submitted_form=parameter_selection_list

|title=USGS Gage #09402000 on the Little Colorado River near Cameron (Average Annual Streamflow)

|publisher=U.S. Geological Survey

|work=National Water Information System

|format=1947–present

|access-date=2010-01-17}} The river's peak flows can be far higher than its average flow, because of quick desert runoff from cloudbursts. At the same gauge, peak flows were recorded from 1923 to 2008, with spotty data from 1924 to 1947. The highest recorded peak was {{convert|120000|cuft/s|m3/s}} on September 20, 1923, while the lowest was {{convert|1590|cuft/s|m3/s}} in 1974.{{cite web

|url=http://nwis.waterdata.usgs.gov/nwis/peak?site_no=09402000&agency_cd=USGS&format=html

|title=USGS Gage #09402000 on the Little Colorado River near Cameron (Peak Streamflow)

|publisher=U.S. Geological Survey

|work=National Water Information System

|format=1923–present

|access-date=2010-01-17}}

History

File:Navaho Indians crossing the Little Colorado River, ca.1900 (CHS-5136).jpg

Human activity in the Little Colorado River watershed dates back to the early Holocene epoch, in the last glacial period. Nomadic hunter-gatherers inhabited the relatively water-rich and diverse upper basin of the Little Colorado for almost 8,000 years before the Navajo, Apache and Hopi tribes populated the area. Many of these people practiced small-scale irrigation in riverside villages, located in sheltered canyons and cliffs that provided defense.{{cite web

|url = http://cpluhna.nau.edu/Places/littlecolr.htm

|title = The Little Colorado River Basin in Arizona

|publisher = Land Use History of North America

|work = Land Use History of the Colorado Plateau

|access-date = 2010-10-17

|url-status = dead

|archive-url = https://web.archive.org/web/20100926053819/http://cpluhna.nau.edu/Places/littlecolr.htm

|archive-date = 2010-09-26

}}

Early Spanish explorers exploring the Grand Canyon area were most likely the first Europeans to see the Little Colorado River. They called it Colorado Chiquito, the Little Colorado.{{cite web

|url=http://southwest.library.arizona.edu/azas/body.1_div.6.html

|title=Rivers of Arizona: Size, Extent, Etc.

|publisher=University of Arizona Library

|work=Books of the Southwest

|page=39

|access-date=2010-01-17

|archive-date=2010-06-30

|archive-url=https://web.archive.org/web/20100630022549/http://southwest.library.arizona.edu/azas/body.1_div.6.html

|url-status=dead

}} Other than fur trappers and mountain men, one of the first organized expeditions into the area of the Little Colorado River was led by Amiel Weeks Whipple in 1853–54{{cite book | last = Worster | first = Donald | title = A River Running West: The Life of John Wesley Powell| year = 2001 | isbn = 978-0-19-509991-1 | url = https://archive.org/details/riverrunningwest00wors | url-access = registration }} during one of the expeditions to map out a route for a transcontinental railroad. Called The Great Railroad Expeditions, or Pacific Railroad Surveys, Whipple's expedition consisted of several teams going roughly along the 35th parallel from Albuquerque to the Pacific, following the Santa Fe Trail route.

File:LittleBigColorado.jpg trapping sediment.]]

File:Joseph City-St. Joseph Bridge-1917-1x.jpg

File:Little Colorado River confluence with Big Canyon.jpg

The Little Colorado River, also known as the Flax River, and the first Rio Chiquito, is depicted and labelled as such on a map compiled by Lt. Joseph C. Ives and published in the official volumes of those expeditions. Ives would again return to the area in 1858 after navigating a steamboat named the Explorer up the Colorado from south of Yuma northwards to Black Canyon, at which point his party went ashore and attempted to go up into the Grand Canyon until the sheer cliffs prevented them from doing so. Leaving the canyon they proceeded overland and someplace in the vicinity of the Grand Falls (also known as the Chocolate Falls) on the Little Colorado, picked up the Whipple trail from four years prior.also see Goetzmann, William H. "Army Exploration in the American West, 1803–1863," 1959.

The Powell Geographic Expedition, on August 10, 1869, was one of the first American parties to sight the Little Colorado River.{{cite book

|last=Dolnick

|first=Edward

|title=Down the Great Unknown: John Wesley Powell's 1869 Journey of Discovery and Tragedy Through the Grand Canyon

|publisher=HarperCollins

|year=2002

|isbn=0-06-095586-4

|page=234}} Powell and some of his crew explored a segment of the Little Colorado River canyon, although they mainly found it impassable. In diary entries, they recorded its name as "Flax River", for the flax that makes up much of the river's riparian zone{{cite web

|last=Euler

|first=Robert C.

|url=http://www.nps.gov/history/history/online_books/geology/publications/pp/670/sec2.htm

|archive-url=https://web.archive.org/web/20110604200206/http://www.nps.gov/history/history/online_books/geology/publications/pp/670/sec2.htm

|url-status=dead

|archive-date=June 4, 2011

|title=The Archaeology of the Canyon Country

|publisher=U.S. Geological Survey

|work=Geological Survey Professional Paper 670: John Wesley Powell and the Anthropology of the Canyon Country

|date=2009-01-13

|access-date=2010-01-17}}—and "Colorado Chiquito"—so, presumably they already knew about the river before they had come on the expedition.{{cite book

|last=Powell

|first=John Wesley

|editor=Cooley, John

|title=Exploring the Colorado River: Firsthand Accounts by Powell and His Crew

|publisher=Courier Dover Publications

|year=2004

|pages=148–150

|isbn=0-486-43525-3}}

{{quote|It is a lo[a]thesome little stream, so filthy and muddy that it fairly stinks. It is only 30 to 50 [yards] wide now and in many places a man can cross it on the rocks without going on to his knees ... [The Little Colorado was] as disgusting a stream as there is on the continent ... half of its volume and 2/3 of its weight is mud and silt. [It was little but] slime and salt ... a miserably lonely place indeed, with no signs of life but lizards, bats and scorpions. It seemed like the first gates of hell. One almost expected to see Cerberus poke his ugly head out of some dismal hole and growl his disapproval of all who had not Charon's pass.|George Y. Bradley and John Colton "Jack" Sumner, August 1869}}

This was in fact an inaccurate depiction of the Little Colorado, as the muddy flow they observed was the result of a rare flash flood. The river is normally a bright blue color caused by dissolved travertine and limestone in the water, similar to Havasu Creek, another major tributary of the Colorado within the Grand Canyon.

In the 1870s, Mormon colonists migrated southwards from Salt Lake City and settled in the lower part of the Little Colorado River valley.{{cite book

|last=Abruzzi

|first=William S.

|title=Dam that river! Ecology and Mormon settlement in the Little Colorado River Basin

|publisher=University Press of America

|year=1993

|isbn=0-8191-9126-4

}} Expeditions had been sent into the basin about five years before to determine the qualities of the area. The Mormons founded Joseph City near the confluence with the Puerco River, and four others nearby, although Joseph City is the only one that still exists. Settlers continued traveling into the area through 1876, although many of them had great difficulty in crossing the Little Colorado. Although shallow and slow-flowing, the river flows through soft sand and in some places, even quicksand, creating non-ideal conditions for their wagons.Dam that river! Ecology and Mormon settlement in the Little Colorado River Basin, p. 20

There were two primary crossings of the Little Colorado—one at the Grand Falls, and one at Black Falls, a smaller waterfall some {{convert|10|mi|km}} downstream. It was easier to ford the river at the two waterfalls because at that point, it flows over hard bedrock, making the crossing much easier. The Mormons also made many attempts to construct dams on the river to provide irrigation water—as far upstream as the confluence of the river's forks and as far downstream as below Grand Falls—but most of them failed because of the Little Colorado's fickle variations in discharge.{{cite web

|last = Abruzzi

|first = William S.

|url = http://cpluhna.nau.edu/Research/ecology_and_mormon_colonization.htm

|title = Ecology and Mormon Colonization in the Little Colorado River Basin, Arizona

|publisher = Land Use History of North America

|work = Land Use History of the Colorado Plateau

|access-date = 2010-10-17

|url-status = dead

|archive-url = https://web.archive.org/web/20110111012003/http://cpluhna.nau.edu/Research/ecology_and_mormon_colonization.htm

|archive-date = 2011-01-11

}} Finally, they managed to construct one at Joseph City that lasted for 29 years. Despite the continued hardships, the Mormons persisted, successfully established their colonies, and survived in the region for many decades.{{cite web

|last=Abruzzi

|first=William S.

|url=http://cpluhna.nau.edu/Research/grazinglitcolr.htm

|title=The social and ecological consequences of early cattle ranching in the Little Colorado River Basin

|publisher=Land Use History of North America

|work=Land Use History of the Colorado Plateau

|access-date=2010-10-17

|url-status=dead

|archive-url=https://web.archive.org/web/20120302145245/http://cpluhna.nau.edu/Research/grazinglitcolr.htm

|archive-date=2012-03-02

}} Later, Hispanics began to move into the Little Colorado River watershed from the Rio Grande area, establishing St. Johns and Concho. American ranchers from New Mexico also began to colonize the region, creating Eagar and Springerville.Dam that river! Ecology and Mormon settlement in the Little Colorado River Basin, p. 21 For many years, Mormons were the primary group living in the watershed until the 1960s, when their independent towns and farms were absorbed into the growing Arizonan economy.

River modifications

File:Little Colorado River to Springerville AZ.jpg, and the region of the source of the Little Colorado River. Some farm land in the river bottom land is visible at the bottom.]]

Because of its isolation, most of the Little Colorado has remained free of human development. However, near its headwaters, the river is dammed twice, first in River Reservoir, then in Lyman Lake, where its water is stored for irrigation. Another reservoir downstream of Springerville, where Mormon colonists dammed the river in 1905 to form Zion Reservoir, is now completely silted in. Many other earthen and masonry dams originally built along the river by the Mormons no longer exist. At very few points is the river confined by levees, with the exception of a {{convert|2300|ft|m|adj=on}} floodwall near Holbrook. There are also few bridges for a river of its length.

In one of the worst radioactive spills in the U.S. history, on July 16, 1979, {{convert|100|e6gal}} of radioactive water containing uranium tailings breached into the North Fork of the Puerco River from a tailing pond of a uranium mine owned by Kerr-McGee Company and United Nuclear Corporation. Approximately 1,100 tons of uranium mine waste contaminated {{convert|250|acre|km2}} of land and up to {{convert|50|mi|km}} of the Puerco River, traveling into the Little Colorado River as far as the Navajo Nation. Traces of the spill can still be found today.Brendan Giusti, Radiation Spill in Church Rock Still Haunts 30 Years Later, The Daily Times (Farmington, New Mexico), July 16, 2009, Section: LocalCarl Jensen, Project Censored (U.S.) [http://www.projectcensored.org/static/1979/1979-story6.htm 20 Years of Censored News] {{webarchive|url=https://web.archive.org/web/20100106050729/http://www.projectcensored.org/static/1979/1979-story6.htm |date=2010-01-06 }} Seven Stories Press, July 1, 2003, p. 84, {{ISBN|1-888363-52-5}}

{{wide image|USA little colorado pano AZ.jpg|852px|The Little Colorado River gorge, near Grand Canyon National Park}}

See also

References