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	<id>https://colorado.wiki/index.php?action=history&amp;feed=atom&amp;title=Colorado_River_History</id>
	<title>Colorado River History - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://colorado.wiki/index.php?action=history&amp;feed=atom&amp;title=Colorado_River_History"/>
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	<updated>2026-07-13T11:15:05Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://colorado.wiki/index.php?title=Colorado_River_History&amp;diff=2953&amp;oldid=prev</id>
		<title>FrontRangeBot: Structural cleanup: ref-tag (automated)</title>
		<link rel="alternate" type="text/html" href="https://colorado.wiki/index.php?title=Colorado_River_History&amp;diff=2953&amp;oldid=prev"/>
		<updated>2026-05-12T07:55:03Z</updated>

		<summary type="html">&lt;p&gt;Structural cleanup: ref-tag (automated)&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 07:55, 12 May 2026&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l28&quot;&gt;Line 28:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 28:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Notable&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Notable&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
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		<author><name>FrontRangeBot</name></author>
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	<entry>
		<id>https://colorado.wiki/index.php?title=Colorado_River_History&amp;diff=1483&amp;oldid=prev</id>
		<title>FrontRangeBot: Drip: Colorado.Wiki article</title>
		<link rel="alternate" type="text/html" href="https://colorado.wiki/index.php?title=Colorado_River_History&amp;diff=1483&amp;oldid=prev"/>
		<updated>2026-04-06T03:22:38Z</updated>

		<summary type="html">&lt;p&gt;Drip: Colorado.Wiki article&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;The &amp;#039;&amp;#039;&amp;#039;Colorado River&amp;#039;&amp;#039;&amp;#039; is the second-longest river in the Western United States, spanning approximately 1,450 miles from its headwaters in the San Juan Mountains of Colorado to its terminus in the Gulf of California in Mexico. The river drains a watershed of approximately 246,000 square miles and serves as the primary water source for millions of people across seven U.S. states and Mexico. Its history encompasses tens of thousands of years of human habitation, exploration, and development, from indigenous peoples to Spanish colonizers, American explorers, and modern water management systems that have transformed the American West. The Colorado River&amp;#039;s story is fundamentally intertwined with the settlement and development of the western United States, representing both the opportunities and challenges of managing a critical natural resource in an arid region experiencing increasing population and competing demands.&amp;lt;ref&amp;gt;{{cite web |title=Colorado River Basin Overview |url=https://www.usbr.gov/lc/region/g1000/historicalpubs.html |work=U.S. Bureau of Reclamation |access-date=2026-02-26}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
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== History ==&lt;br /&gt;
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The Colorado River&amp;#039;s human history extends back millennia before European contact. Archaeological evidence suggests that indigenous peoples inhabited the Colorado River basin for at least 10,000 years, with numerous Native American tribes establishing settlements along its banks and tributaries. The Ancestral Puebloans, also known as the Anasazi, developed sophisticated irrigation systems and agricultural communities in the Colorado River basin from approximately 100 CE to 1600 CE. These early peoples demonstrated remarkable engineering knowledge, constructing terraces, check dams, and canal systems that allowed them to cultivate crops in the arid southwestern environment. The Hohokam culture in present-day Arizona and the Fremont culture in present-day Utah similarly relied on the river&amp;#039;s waters for survival, developing complex societies centered on agricultural production. When Spanish explorers arrived in the sixteenth century, they encountered the Yuma, Mojave, Maricopa, and other tribes who maintained active trade networks and settlements throughout the Colorado River valley.&lt;br /&gt;
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Spanish exploration of the Colorado River began in earnest during the sixteenth and seventeenth centuries. In 1539, Spanish conquistador Francisco Vázquez de Coronado led an expedition northward from Mexico, seeking the legendary cities of gold. While Coronado&amp;#039;s expedition did not reach the Colorado River directly, it prompted subsequent Spanish expeditions to explore northern Mexico and present-day southwestern United States. In 1540, García López de Cárdenas, a member of Coronado&amp;#039;s expedition, became the first European to view the Grand Canyon, approaching it from the South Rim. Spanish explorers and Jesuit missionaries gradually pushed northward along various routes, with Father Eusebio Francisco Kino conducting extensive explorations in the late seventeenth and early eighteenth centuries. Kino&amp;#039;s work helped establish Spanish understanding of the Colorado River&amp;#039;s geography and its indigenous peoples, though Spanish colonization efforts remained limited compared to regions further south.&lt;br /&gt;
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The American era of Colorado River exploration began in the early nineteenth century. In 1826, American fur trapper Jedediah Smith led an expedition that traced the Colorado River southward from the Great Salt Lake toward the Pacific Ocean, becoming the first American to cross the Sierra Nevada mountains. Smith&amp;#039;s expedition provided valuable geographic information about the river&amp;#039;s course and the surrounding terrain. American trappers and mountain men increasingly ventured into the Colorado River basin during the 1820s and 1830s, establishing trading posts and conducting fur operations. The most famous American exploration of the Colorado River occurred in 1869 when John Wesley Powell, a naturalist and Civil War veteran, led an expedition down the entire length of the river from Wyoming to the Grand Canyon and beyond. Powell&amp;#039;s expedition provided the first comprehensive scientific documentation of the Colorado River&amp;#039;s geography, geology, and hydrology, revolutionizing American understanding of the river and the southwestern landscape. His observations regarding the river&amp;#039;s power, volume, and seasonal fluctuations would later inform water management decisions that shaped the modern American West.&amp;lt;ref&amp;gt;{{cite web |title=John Wesley Powell and the Colorado River Expedition |url=https://www.usgs.gov/faqs/who-was-john-wesley-powell |work=U.S. Geological Survey |access-date=2026-02-26}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
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The twentieth century witnessed the transformation of the Colorado River from a wild, unpredictable waterway into a managed resource supporting millions of people. The Colorado River Compact, signed in 1922, represented the first major attempt to allocate the river&amp;#039;s waters among the seven states of the Colorado River basin: Colorado, Utah, Wyoming, New Mexico, Arizona, Nevada, and California. The Compact allocated 15 million acre-feet of water annually to the upper basin states (Colorado, Utah, Wyoming, and New Mexico) and the lower basin states (Arizona, Nevada, and California), with an additional 1.5 million acre-feet allocated to Mexico through a 1944 treaty. The Compact was based on flow measurements taken during an unusually wet period, leading to subsequent allocation disputes as the river&amp;#039;s actual average flow proved lower than anticipated. The construction of major dams, including Hoover Dam (completed in 1936), Glen Canyon Dam (completed in 1964), and numerous other reservoirs, transformed the Colorado River into a series of regulated pools that could be managed for flood control, hydroelectric power generation, and water supply. These engineering projects enabled the rapid development of cities like Las Vegas, Los Angeles, and Phoenix, which would not have been possible without reliable water supplies diverted from the Colorado River.&amp;lt;ref&amp;gt;{{cite web |title=Colorado River Compact History and Terms |url=https://www.usbr.gov/lc/region/g1000/ава/crbhistory.html |work=U.S. Bureau of Reclamation |access-date=2026-02-26}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
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Modern challenges facing the Colorado River include sustained drought, increasing water demands, and competing interests among stakeholders. Beginning in the early 2000s, the Colorado River basin experienced a prolonged drought that significantly reduced inflows and lowered reservoir levels. Lake Mead and Lake Powell, the two largest reservoirs created by Hoover and Glen Canyon dams respectively, fell to historically low levels, prompting concerns about future water availability. Climate change has exacerbated these challenges, with studies suggesting that warming temperatures increase evaporation rates and reduce snowpack in the Rocky Mountains, which feeds the river. Agricultural interests, municipal water suppliers, environmental groups, and Native American tribes all maintain different priorities regarding water allocation and management. The 2007 Interim Guidelines and subsequent negotiations have attempted to address these competing demands through conservation measures, capacity sharing arrangements, and voluntary reduction agreements. The future of the Colorado River remains uncertain as the region continues to grow and climate conditions become increasingly unpredictable.&lt;br /&gt;
&lt;br /&gt;
== Geography ==&lt;br /&gt;
&lt;br /&gt;
The Colorado River originates in the San Juan Mountains of southwestern Colorado, specifically in the La Poudre Pass area near the Continental Divide at approximately 10,000 feet elevation. The river begins as a small stream born from mountain springs and snowmelt, gradually gathering water from numerous tributaries as it flows westward through Colorado. Major Colorado tributaries include the Gunnison River, which joins the main stem near Palisade, Colorado, and the Roaring Fork River near Glenwood Springs. After flowing through western Colorado and briefly through Utah, the Colorado River enters Arizona at Lee&amp;#039;s Ferry, a historically significant crossing point that marked the boundary between the upper and lower Colorado River basins in water management contexts. From Arizona, the river flows through the Grand Canyon, one of North America&amp;#039;s most iconic geological formations, carved by the river over millions of years. The Grand Canyon section spans approximately 277 miles and showcases Precambrian bedrock, dramatic geological formations, and a wealth of paleontological and archaeological evidence.&lt;br /&gt;
&lt;br /&gt;
Continuing south from the Grand Canyon, the Colorado River flows through lower Arizona and forms the international boundary between Arizona and California, then Arizona and Nevada. The river passes through or creates several major reservoirs, including Lake Havasu, which supplies water to Southern California through the Colorado River Aqueduct. In the lower reaches, the river enters Mexico, passing through Baja California before terminating in the Gulf of California, also known as the Sea of Cortez. The Colorado River basin encompasses portions of seven American states, with the upper basin including Colorado, Utah, Wyoming, and New Mexico, and the lower basin including Arizona, Nevada, and California. The total drainage area covers approximately 246,000 square miles, making it one of the largest watersheds in North America. Significant tributaries include the San Juan River, the Little Colorado River, the Green River, and the Gila River, all of which contribute substantial flows to the main stem. The river&amp;#039;s gradient changes considerably along its length, dropping rapidly in mountainous sections and gradually through desert regions, creating varied ecological zones and hydroelectric generation opportunities.&amp;lt;ref&amp;gt;{{cite web |title=Colorado River Basin Tributaries and Geography |url=https://water.usgs.gov/edu/riversofus.html |work=U.S. Geological Survey |access-date=2026-02-26}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
== Economy ==&lt;br /&gt;
&lt;br /&gt;
The Colorado River&amp;#039;s economic significance extends across multiple sectors and millions of people throughout the western United States and Mexico. Agricultural irrigation represents one of the river&amp;#039;s most important economic uses, with approximately 80 percent of the Colorado River&amp;#039;s allocated water supporting agriculture. The river irrigates approximately 3 million acres of farmland across the seven basin states, producing crops including alfalfa, cotton, lettuce, melons, and numerous fruit varieties. In California&amp;#039;s Imperial Valley, Colorado River water enables agricultural production on roughly 500,000 acres, generating billions of dollars in annual crop revenue. The river also supplies irrigation water for agricultural regions in Arizona, including the Pinal County area, and supports farming operations throughout Utah, Colorado, and New Mexico.&lt;br /&gt;
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Municipal and industrial water supply constitutes the second major economic use of the Colorado River. Cities including Los Angeles, San Diego, Las Vegas, Phoenix, and Denver rely on Colorado River water for residential consumption, commercial operations, and industrial processes. The Metropolitan Water District of Southern California, which supplies water to approximately 19 million residents in the Los Angeles area, derives roughly 50 percent of its supply from the Colorado River. Las Vegas and southern Nevada obtain approximately 90 percent of their water supply from Lake Mead on the Colorado River, making water security critical to the region&amp;#039;s continued development and tourism economy. The Colorado River Aqueduct, completed in 1941, transports water 242 miles from Lake Havasu to metropolitan Los Angeles, representing one of the most significant engineering projects in American history.&lt;br /&gt;
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Hydroelectric power generation provides substantial economic benefits throughout the Colorado River system. The Bureau of Reclamation operates multiple dams that generate electricity sold to regional utilities and transmitted throughout the western power grid. Hoover Dam, Glen Canyon Dam, and other facilities produce thousands of megawatts of electricity annually, with revenues supporting operations, maintenance, and water management programs. The tourism economy also benefits significantly from Colorado River resources, with recreational activities including boating, fishing, hiking, and white-water rafting drawing millions of visitors annually. The Grand Canyon receives approximately 4 million visitors yearly, many of whom experience the Colorado River through various recreational activities. Lake Mead, Lake Powell, and other reservoirs support major recreation industries providing employment and tax revenue to surrounding communities.&lt;br /&gt;
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== Notable&lt;/div&gt;</summary>
		<author><name>FrontRangeBot</name></author>
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