The Bannock War of 1878 was an armed conflict between the U.S. military and Bannock and Paiute warriors in Idaho and northeastern Oregon from June to August 1878. The Bannock totaled about 600 to 800 in 1870 because of other Shoshone peoples being included with Bannock numbers. They were led by Chief Buffalo Horn , who was killed in action on June 8, 1878. After his death, Chief Egan led the Bannocks. He and some of his warriors were killed in July by a Umatilla party that entered his camp in subterfuge .
190-586: The U.S. military, consisting of the 21st Infantry Regiment and volunteers, was led by Brigadier General Oliver O. Howard . Nearby states also sent militias to the region. The conflict ended in August and September 1878, when the remaining scattered Bannock-Paiute forces surrendered; many returned to Fort Hall Reservation . The U.S. Army forced some 543 Paiute from Nevada and Oregon and Bannock prisoners to be interned at Yakama Indian Reservation in southeastern Washington Territory . The Bannock people had developed as
380-413: A Japanese attack, Diamond was mortally wounded while he fired a machine gun, holding off Japanese troops from a patrol evacuating wounded from the 1st Battalion. The regiment attacked north from Mintal along Route 1-D and another road on 17 May. The 21st captured Tugbok on 21 May against fierce Japanese resistance. The regiment's right flank advanced to a road junction east of Tugbok by 27 May. The regiment
570-508: A May 30 letter that he had dispatched Col. Reuben F. Bernard 's cavalry from Boise to the plains that evening as a show of force; he did not want to provoke further conflict. Bernard's cavalry reached the Bannock camp on June 2 and drove them to retreat to the Lava Beds. The military noted this was better for defense. The Bannock group moved west and raided Glenn's Ferry and King Hill station, both on
760-565: A Presidential Unit Citation. K Company Private First Class Mack A. Jordan was posthumously awarded the Medal of Honor for his actions near Kumsong on 15 November. These battles resulted in a stalemate between UN forces and the PVA/KPA around the 38th Parallel. In January 1952, the 24th Division, including the 21st Regiment, was removed from the line and sent to Japan. It became part of the US strategic reserve in
950-593: A Shoshone war party attacked a wagon train in the Boise Valley, and the U.S. Army mounted a counterattack, the Winnas Expedition . The situation became so unstable that Fort Boise was abandoned, and the Army had to escort wagon trains through the area. While early settlers had simply passed through this area on their way to Oregon, gold strikes brought renewed interest in the 1860s. The Army rebuilt Fort Boise further east of
1140-484: A battalion to Pusan . The remainder of the regiment and the rest of the division were to follow by sea transport. 1st Battalion, led by Lieutenant Colonel Charles Smith , became the advance force. It was designated as Task Force Smith and comprised B & C Companies, half of Headquarters Company, two 75mm M20 recoilless rifles , four M2 4.2 inch mortars and a battery of 105 mm howitzers. Task Force Smith airlifted into Pusan and then travelled by rail and truck to
1330-622: A distinct group from the Northern Paiute nation of northern Idaho. During the 18th century, these Paiutes had traveled south to the Snake River plain of present-day Idaho, attracted by the prospect of an alliance with the linguistically similar and equestrian Shoshone people . It was during this period that these Paiutes became known as Bannocks. The Bannocks quickly adopted the Shoshone equestrian culture and made other ties through intermarriage with
1520-492: A lack of adequate food supplies by the government. Many Shoshone-Bannock left Fort Hall to attempt survival on their own. Simultaneously, the 1877 Nez Perce War drove officials to crack down on the nation and require them to stay within the reservation boundaries. The Bannock War of 1878 resulted from numerous factors. The terrible conditions caused divisions within the Shoshone-Bannock communities. The Bannock began to view
1710-518: A large network of canals and pump stations. The Minidoka Project would eventually bring water to a million acres (2,500 km ) of the Magic Valley. During World War II, many Japanese Americans interned at Minidoka were made to work on the project. The Boise Project , which would ultimately water 500,000 acres (200,000 ha) in and around the Boise Valley, was another major early reclamation undertaking. At its completion, Arrowrock Dam (1915) on
1900-667: A minimum daily mean of 2,000 cu ft/s (57 m /s) on November 29, 1961. A historic June 1894 flood at the Ice Harbor site reached an estimated peak of 409,000 cu ft/s (11,600 m /s). In terms of discharge, the Snake River is the twelfth largest river in the United States, and it contributes about one-fifth of the Columbia's total outflow into the Pacific. The volume of
2090-477: A position north of Osan , 45 kilometers south of Seoul . Task Force Smith dug in and prepared to engage KPA forces on 4 July. At 08:16 on 5 July, the task force opened fire on a column of 33 KPA T-34/85 tanks, supported by two regiments of infantry. Due to the lack of anti-tank weapons , the task force could only destroy four T-34/85s as the tank column continued south. KPA infantry then attacked Task Force Smith both frontally and around its flanks. Task Force Smith
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#17328454498942280-505: A rapid, forcing their retreat. On the Snake River above Hells Canyon, several steamboats were built at great expense (as manufactured parts such as engines had to be hauled in overland), the first being the Shoshone in 1866. However, running the upper Snake proved unprofitable, due to lack of demand. The owners of Shoshone decided to move her to the lower Snake River, and in April 1870, they made
2470-488: A record high of 86,240 cu ft/s (2,442 m /s) in 1965, to a low of 27,890 cu ft/s (790 m /s) in 1997. In southern Idaho, Snake River flows are significantly influenced by the Eastern Snake River Plain Aquifer . One of the largest groundwater reserves in the US, the aquifer is founded in porous volcanic rock underneath the plain. It absorbs and stores large volumes of water from
2660-495: A semi-arid climate, with about 10 in (250 mm) of rain and 5 in (130 mm) of snow as measured at Ice Harbor Dam. January is the coldest month with a mean temperature of 34.3 °F (1.3 °C), and July is the hottest month at 74.6 °F (23.7 °C). Semi-arid shrubland and rangeland covers about 50 percent of the Snake River watershed. Natural vegetation is primarily sagebrush , mixed with wheatgrasses and bunchgrasses . About 30 percent of
2850-619: A series of lakes, enabling heavy barges to travel between the Columbia River and the Port of Lewiston. About 10 miles (16 km) downstream from Ice Harbor Dam, the Snake empties into the Columbia River at Burbank, Washington , southeast of the Tri-Cities . The confluence is located on Lake Wallula , the impoundment behind McNary Dam on the Columbia, 341 feet (104 m) above sea level. From there,
3040-567: A series of massive flood basalt events that engulfed the Columbia Basin and surrounding lands, reshaped the landscape and erased most evidence of the pre-volcanic river channels starting about 17 Ma. Erupting from fissures in the southern Columbia Basin, the first basalt flows pushed the ancient Salmon-Clearwater much further north than its present course. About 12–10 Ma, the Blue Mountains region began to experience uplift, raising
3230-478: A steep grade, was connected three years later. In addition to commerce, the railroad also opened the Snake River region – which just a few years ago had been seen as a remote, rough frontier – to recreation. The Union Pacific heavily promoted tourism in places like Shoshone Falls, Payette Lake and Soda Springs, Idaho . Countering the reputation of southern Idaho as a wasteland, a brochure described Shoshone Falls: "Shoshone differs from every other waterfall in this or
3420-425: A tank deck and gave fire support. For his actions, Bacon was awarded the Medal of Honor. On 28 June 1971, the 4th Battalion was withdrawn from Vietnam and inactivated on the same day at Fort Lewis. On 5 June 1972, the 1st Battalion was reactivated and assigned to the 25th Infantry Division at Schofield Barracks. 2nd Battalion reactivated on 21 June 1975 and was sent to the 24th Infantry Division at Fort Stewart , but
3610-535: A threatened Cheyenne outbreak. During the winter of 1890-91, the regiment sent six companies to the Rosebud Indian Reservation in response to Sioux unrest. The regiment fought in the Spanish–American War in 1898. On 22 June 1898, the regiment fought in the attack on Santiago . It was part of the 2nd Brigade of V Corps 1st Division. On 1 July, the regiment was positioned on the left flank of
3800-563: Is January, with a mean temperature of 13 °F (−11 °C), and the hottest is July at 57.7 °F (14.3 °C). Twin Falls experiences a semi-arid climate , with about 9 in (230 mm) of rain and 13 in (330 mm) of snow. Monthly mean temperatures range from 29.4 °F (−1.4 °C) in January to 73.1 °F (22.8 °C) in July. The Columbia Basin around the river's mouth also has
3990-651: Is a United States Army infantry regiment. The 1st Battalion currently exists as part of 2nd Infantry Brigade Combat Team, 25th Infantry Division . The regiment fought in World War II , the Korean War and the Vietnam War , as well as Operation Iraqi Freedom . Task Force Smith , the first American unit to see action in the Korean War, was derived from the regiment's 1st Battalion. The 21st Infantry traces its history back to
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#17328454498944180-589: Is a major river in the interior Pacific Northwest region of the United States. About 1,080 miles (1,740 km) long, it is the largest tributary of the Columbia River , which is the largest North American river that empties into the Pacific Ocean . Beginning in Yellowstone National Park , western Wyoming , it flows across the arid Snake River Plain of southern Idaho , the rugged Hells Canyon on
4370-528: Is joined from the left by the Tucannon River , then from the right by the Palouse River , which forms Palouse Falls about 8 miles (13 km) upstream of its confluence with the Snake. The Lower Snake River Project consists of four dams equipped with navigation locks – Lower Granite , Little Goose , Lower Monumental and Ice Harbor – which have transformed the once fast-flowing lower Snake River into
4560-489: The 11th Airborne Division during its drive on Manila in the Battle of Luzon . For its fire support of the division, Cannon Company was awarded a Presidential Unit Citation for actions between 31 January and 5 February. The regiment fought in the Battle of Mindanao . On 17 April, it conducted an amphibious assault on Mindanao's south-central coast. The 3rd Battalion landed at Malabang and linked up with Filipino soldiers under
4750-503: The 162nd RCT allowed the 21st to return to divisional control. On 30 April, the regiment attacked to clear the Libby Airdrome , Route 1-D and Mintal . A battalion of the regiment reached Mintal from the southwest on 3 May. The remainder of the regiment, reinforced by a battalion from the 34th Infantry Regiment , had cleared the airdrome by 5 May. However, the troops were unable to advance along Route 1-D toward Mintal. A battalion of
4940-474: The 53rd , 58th , and 59th Infantry Regiments in late September–early October 1921, while the enlisted personnel in Alaska were concurrently transferred to the 7th Infantry Regiment . The officers, records, and colors of the regiment were transferred 7 October 1921 to Schofield Barracks, Territory of Hawaii , and the regiment was reorganized 28 November 1921 at Schofield Barracks using the personnel and equipment of
5130-512: The 8th Infantry Regiment and were the lead skirmishers of the II Corps ' 2nd Division. They helped to initially break through Confederate lines, but Confederate numerical superiority forced a Union withdraw. During the retreat, the 2nd Battalion's companies suffered heavy losses while covering the retreat. The battalion also fought at the Second Battle of Manassas and formed the rearguard during
5320-662: The Basin and Range Province , such as the Independence and Albion Mountains . To the east are more ranges of the Rockies including the Tetons and the Wind River Range ; the latter includes Gannett Peak , the highest point in the Snake River basin at 13,816 feet (4,211 m). Surface volcanic features – such as lava fields, cones , and thermal springs – are replete in the southern part of
5510-622: The Battle of Gettysburg and suffered heavy losses. The battalion advanced southward against the retreating Confederate Army and fought in the Overland Campaign during May 1864. The battalion served at the Battle of the Wilderness , Battle of Spotsylvania Court House and the Battle of Cold Harbor . By June, the Union Army was beginning the Siege of Petersburg . The battalion fought in the siege but
5700-640: The Cayuse against the Shoshone, Bannock and Northern Paiute, and stopped the latter from expanding their territory towards the Columbia Plateau. Both the Nez Perce and Shoshone acquired horses in the late 1600s or early 1700s, enabling far-reaching trade and hunting expeditions. With horses, the Nez Perce were able to travel east of the Bitterroot Mountains to hunt bison, via the trail over Lolo Pass , which
5890-487: The Fort Hall Indian Reservation on the Snake River in southeast Idaho. Tribal resistance would continue for years to come. In 1877 the US government attempted to force the remaining Nez Perce onto their reservation, at which point Chief Joseph's band and several others opted to seek refuge elsewhere. After a treacherous crossing of the Snake at Dug Bar, Hells Canyon on May 31, the Nez Perce were pursued by
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6080-609: The Grande Ronde River from the left. From the end of Hells Canyon at Asotin, Washington , it flows north to Lewiston, Idaho , where it is joined from the right by the Clearwater River , its largest tributary by volume. The Snake then turns sharply west to enter Washington. The final stretch of the Snake River flows through steep-sided valleys in the Palouse Hills of southeast Washington. Near Lyons Ferry State Park , it
6270-630: The Inchon landings on 15 September, the KPA forces besieging the Pusan Perimeter began to retreat. The 21st Regiment broke out of the perimeter on 19 September. In a rapid advance northward, it took Waegwan , Kumchon and Taejon. The regiment crossed the 38th parallel north in mid-October. At the peak of its advance on 2 November, the regiment was 17 miles (27 km) south of the Chinese border. On 3 November,
6460-632: The Montana Trail providing access to gold strikes in Montana Territory. This crossed the Snake River by the Eagle Rock Ferry and later a bridge which the city of Idaho Falls would soon grow around. As the flow of settlers increased, the Nez Perce and their neighbors the Cayuse and Walla Walla came under pressure to cede portions of their territory. Tensions flared in 1855 after tribes were coerced into relinquishing huge amounts of territory in
6650-508: The North West Company near the confluence of the Snake and Columbia Rivers. The following year, Mackenzie traveled up the Snake River and reached Boise Valley by making the first recorded river ascent of Hells Canyon. Mackenzie's goal was to bypass the arduous trek over the Blue Mountains. He wrote that "the passage by water is now proved to be safe and practicable for loaded boats, without one single carrying place or portage; therefore,
6840-681: The Owyhee River to the Juniper Mountains and Lava Canyon. On June 8 a group of 26 volunteer military men from Silver City, Idaho , led by Captain J.B. Harber, encountered Chief Buffalo Horn and his warriors. At South Mountain, a small mining village, they exchanged fire, resulting in the deaths of two Silver City volunteers and several Bannock, among them the chief. The Bannock selected a new leader, Chief Egan , and headed to Juniper Mountain in Idaho and Steens Mountain in southeastern Oregon to meet with
7030-572: The Paiute . Other states began sending militia troops to the region, including California, Nevada, and Utah. As the Bannock traveled westward, they continued to raid camps, resulting in some settler deaths. People in Idaho and neighboring states feared that the violence would soon spread their way. Bernard arrived in Silver City on June 9 and quickly headed out to the Jordan Valley. The troops moved to meet
7220-513: The Palisades Dam forms Palisades Reservoir . From there it flows northwest through Swan Valley to join the Henrys Fork on an alluvial plain near Rexburg . The Henrys Fork is sometimes called the "North Fork" of the Snake River, while the section of the main Snake River above their confluence is sometimes called the "South Fork". Turning southwest, the river begins its long journey across
7410-589: The Philippine Commonwealth Army , Philippine Constabulary and recognized guerrillas there who had captured the Malabang Airfield . The remainder of the regiment landed at Baras, thirty miles southeast. The regiment embarked on landing craft of the 533d Engineer Boat and Shore Regiment and was transported to Kabacan using the Mindanao River . There, it became X Corps reserve. The arrival of
7600-646: The Powder and Burnt Rivers from the left. Continuing north, the river enters Hells Canyon , which slices between the Rocky Mountains of Idaho and the Blue Mountains of Oregon and Washington. The Hells Canyon Hydroelectric Complex includes the Brownlee , Oxbow and Hells Canyon Dams in the upper reaches of the canyon. Since its construction in 1967, Hells Canyon Dam has been the upriver limit for migrating salmon; in
7790-739: The Rocky Mountain fur trade , which ended about 1840. This era of positive cooperation with American trade declined in the 1850s, along with the fur trade, under pressure of increased migration of Euro-Americans to the Snake Valley plain. The discovery of gold in the Boise Basin and the Beaverhead country of Montana had attracted prospectors and traders, who moved through the Snake region, competing for game and water resources as they traveled. The American traders and migrants were an established presence in
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7980-753: The Sea of Cortez ) and the Yellowstone and upper Missouri Rivers (part of the Mississippi River system which drains to the Gulf of Mexico ). On the north it borders the watersheds of the Clark Fork and Spokane Rivers , both part of the Columbia River system. To the northwest it borders several other tributary watersheds of the Columbia River, including those of the John Day and Umatilla Rivers . Fifty-four named tributaries of
8170-564: The Treaty of Walla Walla . In retaliation for Lt. Col. Edward Steptoe 's defeat at the 1858 Battle of Pine Creek , a force led by Col. George Wright entered the lower Snake River country in 1859 and constructed Fort Taylor at the confluence of the Tucannon River below present-day Starbuck, Washington . Over several months Wright fought the natives along the river, killing their horses and destroying stored food. The sternwheeler Colonel Wright
8360-483: The rain shadow effect of the Cascades , precipitation as a whole is scant, averaging 14 inches (360 mm) across the entire watershed. Most precipitation falls at higher elevations as snow, thus, most runoff in the Snake River watershed derives from snowmelt. Jackson Hole, Wyoming experiences an alpine climate with an average of 30 in (760 mm) of rain and 252 in (6,400 mm) of snow. The coldest month
8550-426: The 1855 treaty. The US government sided with the settlers, and pressured some Nez Perce leaders into signing a second treaty which shrank their reservation by 90 percent. Many Nez Perce including Chief Joseph 's band refused to leave, calling the new treaty the "thief treaty". In March 1863, the Idaho Territory was split from Oregon, and Lewiston became its capital. More than 60,000 prospectors and others entered
8740-453: The 1950s, public agencies, tribal governments and private utilities have invested heavily in fishery restoration and hatchery programs, with limited success. The proposed removal of the four lower Snake River dams for fish passage is a significant ongoing policy debate in the Pacific Northwest. The Snake River begins on Two Oceans Plateau near the southern border of Yellowstone National Park , about 9,200 feet (2,800 m) above sea level in
8930-406: The 2nd Battalion and was transferred to Warner Kaserne. On 15 April 1970, the 24th Division and the two 21st Infantry battalions were inactivated. The 3rd Battalion of the regiment was activated on 10 September 1965 at Fort Devens . It was subordinated to the 196th Light Infantry Brigade . On 26 August 1966, it was sent to South Vietnam . The brigade was attached to the 25th Infantry Division and
9120-415: The 2nd Battalion of the 12th Infantry Regiment , formed on 3 May 1861 for the American Civil War . Companies A, B, E and G were activated at Fort Hamilton on 20 May 1862. They were sent to Harpers Ferry and on 26 May fought in a skirmish with a Confederate States Army brigade. The companies fought at the Battle of Cedar Mountain on 9 August. The companies were formed into a battalion with elements of
9310-448: The 7th and participated in Operation Just Cause from 1989 to 1990 as well as the 1992 Los Angeles riots in May of that year. It was inactivated on 15 September 1993. Beginning in 2005 the 2nd Brigade including the 1st Battalion, 21st Infantry underwent reorganization as a Stryker brigade combat team. The brigade arrived in Iraq for a fifteen-month tour of duty in November 2007and was based at Camp Taji northwest of Baghdad. Serving with
9500-400: The Army for over 1,000 miles (1,600 km) east, through Yellowstone before turning north through Montana, fighting several battles along the way. On October 5, 1877, Chief Joseph surrendered to US forces. thus ending the Nez Perce War . The survivors were distributed to various reservations across the western US. In 1878, an uprising occurred in response to overcrowding and food shortages at
9690-414: The Bannock at Steens Mountain. Bernard's cavalry followed Chief Egan's Bannock west into Oregon, eventually meeting them in battle on June 23 by Silver Creek. The fight resulted in the deaths of three U.S. soldiers, the wounding of three others, and an unknown number of Bannock casualties. Col. Bernard moved to nearby Camp Curry to meet with General Howard on June 25. On June 29, there was a skirmish between
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#17328454498949880-406: The Bannock forces in the canyon of the North Fork of the John Day River . The conflict did not result in many casualties, but interrupted the Bannock, forcing their retreat. By July 27, Gen. Howard's strategy changed from one against a united enemy to pursuing the fractured Bannock groups. He had numerous Army units operating in Idaho. Most of the concluding conflicts between the remaining bands and
10070-467: The Bannock warriors and Crescent City volunteer militia. Bernard and his cavalry of 350 arrived shortly after and secured the city. The Bannock were traveling toward Fox Valley, estimated to number between 350 and 400. US forces thought they intended to travel further north to join the Cayuse and other Native American groups in that region who shared their discontent. On July 6, a volunteer group by Sheriff Sperry encountered hostiles near Willows Springs at
10260-430: The Blue Mountains to bypass Hells Canyon and reach the lower Snake River. After the hazardous experience, Hunt gave it the name "Mad River". A group led by Robert Stuart , a member of the Hunt expedition, returned eastward across the plain the following year. The route they mapped would eventually become that section of the Oregon Trail . In 1818 Donald Mackenzie and Alexander Ross established Fort Nez Percés for
10450-479: The Boise Project. Palisades Dam was built in 1956, providing flood control and irrigation for the Snake River above Idaho Falls, an area which the Bureau of Reclamation had previously overlooked. Near Rexburg, the Teton Dam was also built to provide water for this area. In 1976, the Teton Dam failed catastrophically, killing eleven people and causing at least $ 400 million in damage along the Henrys Fork and Snake Rivers. The political fallout from this disaster marked
10640-435: The Boise River was the tallest dam in the world, and its construction process was an important prototype for future federal projects such as Hoover Dam . Starting around the 1950s, farmers made heavy use of the Snake River aquifer, bringing large new areas into production. Surface water development also increased with projects such as Cascade Dam (1948) and Anderson Ranch Dam (1950), which provided additional storage for
10830-432: The Boise Valley, and a new city quickly grew around the U.S. Army post at Fort Boise. With Hells Canyon impractical for river navigation, interest grew in connecting the area by rail. By 1884, the Oregon Railroad & Navigation Company (later integrated into Union Pacific ) had connected Portland, Oregon , to the Union Pacific line at Granger, Wyoming , via Huntington and Pocatello . Boise, initially bypassed due to
11020-432: The Carey Act were in Idaho, and almost all of that utilized Snake River water. I. B. Perrine , who homesteaded near Shoshone Falls in the 1880s, went on to develop one of the most successful Carey Act projects. In 1900 Perrine filed a claim for water from the Snake River, and backed by significant private capital, oversaw the construction of Milner Dam and a canal system to irrigate some 250,000 acres (100,000 ha) of
11210-437: The Chinese People's Volunteer Army (PVA) entered the war. PVA attacks forced UN forces to retreat back across the Han River by 3 January 1951. The 21st Regiment fought in the First United Nations Counteroffensive. The regiment then fought in the defense against the Chinese Spring Offensive . C Company Sergeant First Class Ray E. Duke was posthumously awarded the Medal of Honor for actions near Mugok on 26 April. On 27 May,
11400-428: The Columbia Basin about 10.5 Ma, the Elephant Mountain basalt eruption forced the Salmon-Clearwater River into roughly its present course through southeast Washington. By 8.5 Ma the Salmon-Clearwater was established in the Columbia River's modern path through Wallula Gap , although the Columbia itself still flowed somewhere to the west. The last of the Columbia basalt flows occurred around 6 Ma; by then,
11590-452: The Columbia River flows another 325 miles (523 km) west to empty into the Pacific Ocean. The U.S. Army Corps of Engineers has measured the discharge , or flow rate, of the Snake River at Ice Harbor Dam since 1962. The mean annual discharge for the 61-year period between 1962 and 2023 was 49,580 cubic feet per second (1,404 m /s), with a maximum recorded daily mean of 305,000 cu ft/s (8,600 m /s) on June 19, 1974, and
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#173284544989411780-458: The DMZ to deter North Korean aggression. On 15 October 1957, the 24th was replaced in line by the 1st Cavalry Division . In 1958, elements of the regiment was sent with the 24th to replace the 11th Airborne Division in Germany. The US Army introduced the Combat Arms Regimental System , and the regiment was reorganized into battle groups. A Company became the regiment's 1st Battle Group at Warner Kaserne in Munich during July 1958. B Company became
11970-399: The Far East. On 25 July 1953, the regiment returned to South Korea, where it guarded the Geoje POW Camp . The Korean Armistice Agreement was signed on 27 July, and the regiment oversaw POW exchanges at the camp. After the end of Operation Big Switch , the regiment was moved into reserve positions behind the Demilitarized Zone . In March 1955, the regiment was sent to forward positions on
12160-436: The First and Second Battles of the Stronghold. In June 1877, the regiment was ordered into the field in reaction to Nez Perce massacres in Idaho. The regiment pursued the Nez Perce and fought at the Battle of the Clearwater on 11 and 12 July. The regiment continued to pursue the Indians through the Bitterroot Valley to the Bears Paw Mountains , where Chief Joseph finally surrendered. The 21st covered 1,632 miles during
12350-500: The Fort Hall Reservation, leading to the Bannock War . The US army defeated the Bannock and their Paiute allies and proceeded to restrict travel in and out of the reservation. While Lewiston was now well connected by river, travel to Boise and other points upstream on the Snake River remained difficult due to the formidable obstacle of Hells Canyon. In 1865, Thomas Stump attempted to pilot the Colonel Wright up Hells Canyon, making it 80 miles (130 km) upriver before hitting rocks in
12540-409: The Lewis and Clark expedition would later follow in order to reach the Snake and Columbia Rivers. The river's modern name comes from a misunderstanding of the Shoshone Tribal Sign in PISL . The Plains Indians referred to the Shoshone people as "Snake People", while the Shoshone are believed to have referred to themselves as "People of the River of Many Fish". However, the Shoshone sign for "salmon"
12730-483: The Lewiston Valley by 1863. Many new steamboats were pressed into service, including the Spray , Cascadilla , Tenino , Okanogan , and Nez Perce Chief . The river's rapids posed a major navigation hazard, and from November to April the river was generally too low for ships. Despite these challenges, the water transport of freight and passengers was greatly profitable. Up river, the Shoshone and other tribes were also becoming increasingly wary of settlers; in 1854
12920-513: The Malheur Reservation to internment at Yakama Indian Reservation in southeastern Washington Territory. They suffered privation for years. In 1879 the Malheur Reservation was closed, "discontinued" through pressure from settlers. Northern Paiutes from Idaho and Nevada were eventually released and relocated from Yakama to an expanded Duck Valley Indian Reservation with their Western Shoshone brethren in 1886. 21st Infantry Regiment (United States) The 21st Infantry Regiment ("Gimlet" )
13110-404: The Medal of Honor in 2017 for his actions near Tam Kỳ between 13 and 15 May. On 15 July, it was attached to the 23rd Infantry Division until that division's withdrawal from Vietnam in November 1971. The 3rd Battalion then formed Task Force Gimlet , patrolling the "rocket belt" around Da Nang . From 5 to 11 August 1972, Delta Company, 3/21st Infantry undertook the last patrol by U.S. troops in
13300-442: The Multi-National Division-Baghdad, the brigade was responsible for the rural areas northwest and west of Baghdad with the 1st Battalion operating near Abu Ghuraib. The 1st Battalion, working closely with their Iraqi counterparts, was especially successful in eliminating terrorist cells and uncovering and destroying multiple weapons caches. The 1st Battalion returned to Schofield Barracks in February 2009. In February 2016, soldiers of
13490-407: The Nez Perces, who they visited again on their return trip in 1806. Other explorers quickly followed, many of them fur trappers who began scouting the upper Snake River watershed for beaver. John Colter , a former member of the Lewis and Clark expedition, explored the Jackson Hole area in 1808. In 1810, Andrew Henry explored and named the Henrys Fork of the Snake River. He established Fort Henry,
13680-462: The North Korean People's Army (KPA) invaded South Korea , beginning the Korean War . On 30 June, President Harry Truman decided to defend South Korea with American ground forces. The Pentagon selected the 24th Division to deploy first, with the 21st regiment being the first to go to South Korea. Due to a shortage of air transport, the regiment could only airlift a force comprising less than
13870-513: The Oregon Trail reached the Snake River at Fort Hall, Idaho , and stayed south of the river until Three Island Crossing near modern-day Glenns Ferry . Here the trail diverged, with the northern route fording the river to reach the HBC trading post at Fort Boise while the southern route continued into what is now the eastern Oregon desert. While the northern route passed through more favorable country,
14060-563: The Republic forces to retreat, preventing them from attacking Manila . After several defeats, the Republic forces discarded conventional tactics and began a guerrilla war in November. The regiment then fought in the pacification campaign and left the Philippines after the war was declared over on 1 June 1902. Between 1905 and 1906, the regiment returned to the Philippines for garrison duty. In 1909,
14250-628: The Rocky Mountains of Wyoming . From there, it flows west then south into Grand Teton National Park , where it feeds Jackson Lake , a natural glacial lake enlarged by Jackson Lake Dam . It flows south through the alpine valley of Jackson Hole , which is situated between the Teton Range (to the west) and the Gros Ventre Range . Below the town of Jackson it forms the Snake River Canyon of Wyoming , turns west and crosses into Idaho , where
14440-638: The Salmon River at what is now Salmon, Idaho , naming the stream "Lewis's River". Thwarted by the river's rapids, they were forced to cross the Bitterroot Mountains via the Nez Perce trail at Lolo Pass. After paddling down the Kooskooskee (Clearwater River), they reached the junction with the Snake and camped there with the Nez Perces on October 10, 1805. They correctly surmised that the river coming from
14630-585: The Shoshone as intruders and committed theft and other crimes against the group. Friction between the Native Americans and the Euroamericans increased as well, resulting in violence when Pe-tope, a Fort Hill Native American, shot and wounded two teamsters in August 1877. Agent William Danilson, the government-appointed agent of the Fort Hall reservation at the time, pressed the tribal leaders to charge Pe-tope for
14820-426: The Shoshone-Bannock cosmology and their religious connection to the land, as their cultural practices were based in local seasonal changes in the Snake Valley. They believed their ancestors' spirits still resided in the land. Leadership among the Shoshone-Bannock was believed to be directly connected to the land which these ancestors inhabited, granting the chief his position. After complex and controversial deliberation,
15010-684: The Shoshone-Bannock leaders and American government officials formally agreed to relocate the Boise refugees to the Fort Hall Reservation. They completed relocation in 1869. The Fort Hall Reservation was a 1.8 million-acre plot along the Upper Snake River in eastern Idaho, on the river's southeastern banks. The region had potential for irrigation and agriculture, but the Shoshone-Bannock faced immediate survival challenges due to their dependence on native foods and buffalo found off-reservation, and
15200-902: The Shoshones. The Bannocks provided increased security and population for the Shoshone people, who had lost many members due to epidemics of infectious disease contracted from Europeans. By the time the American Lewis and Clark Expedition arrived in this area of present-day southern Idaho in 1805, the Bannock-Shoshones had been trading for some time with representatives of the Hudson's Bay Company and North West Company from Canada . They quickly opened trade with Americans for firearms and horses, as they had done with other European traders for years. The Shoshone-Bannock remained independent, despite their continued reliance on American trade. They participated in
15390-647: The Snake River Plain and the Palouse, though the majority of the Snake River Plain is Bureau of Land Management land. The Snake River watershed borders several other major North American watersheds. To the south it borders the endorheic Great Basin , including the area draining to Utah's Great Salt Lake . To the east it borders the watersheds of the Green River (part of the Colorado River system which drains to
15580-520: The Snake River Plain between 600 and 1500 CE. By the time of first European contact, the Snake River watershed was populated by several Native American tribes. The territory of the Nez Perce (Nimiipuu) stretched across what is now north-central Idaho, southeast Washington and northeast Oregon, including much of the lower Snake River below Hells Canyon, most of the Clearwater and Grande Ronde River, and
15770-580: The Snake River Plain formed as the North American Plate moved westward over the Yellowstone hotspot. Upwelling magma caused the continental crust to rise, forming highlands in a similar fashion to the modern Yellowstone plateau and leaving behind enormous basalt flows in its wake. As the hotspot migrated east relative to the North American Plate, the land behind it collapsed and sank, creating
15960-479: The Snake River Plain, passing through Idaho Falls and receiving the Blackfoot River from the left before entering the 20-mile (32 km)-long American Falls Reservoir , formed by American Falls Dam . From American Falls it turns west, flowing through Minidoka Dam and Milner Dam , where large volumes of water are diverted for irrigation. Below Milner Dam it enters the Snake River Canyon of Idaho , where
16150-399: The Snake River Plain. Completed in 1905, the project was an immediate success. The rapid transformation of the barren landscape into productive farmland led to the moniker " Magic Valley ", and led to massive growth of the city of Twin Falls. During certain times of the year, almost all the Snake River's flow was diverted at Milner Dam, and since then, Shoshone Falls has regularly run dry in
16340-518: The Snake River drain more than 100 square miles (260 km ). Of these, the twelve listed below drain an area greater than 2,000 square miles (5,200 km ). The present-day course of the Snake River was pieced together over millions of years from several formerly disconnected drainage systems. Much of what would become the Pacific Northwest lay under shallow seas until it was uplifted starting about 60 million years ago (Ma). The outlet of
16530-476: The Snake River in the eastern Plain to re-emerge further west as springs in the Snake River Canyon. Water from the lost streams of Idaho , several rivers that disappear underground in the eastern Plain, travels through the aquifer to reach the Snake River, as does excess irrigation water absorbed into the ground. The major spring complexes at American Falls and Thousand Springs (near Hagerman, Idaho ) keep
16720-613: The Snake River peaks in late spring and early summer as snow melts in the Rocky Mountains, and reaches its lowest point in the fall. Despite the numerous dams regulating its flow, its discharge into the Columbia remains highly seasonal. At Ice Harbor Dam, the mean monthly discharge is highest in May and June at over 100,000 cu ft/s (2,800 m /s), and lowest in September and October at less than 25,000 cu ft/s (710 m /s). Mean annual discharge also fluctuates significantly, from
16910-466: The Snake River posed a formidable barrier; during high water, many travelers were forced to take the hot, dry southern route, or risk drowning. Travelers going via Fort Boise had to cross the river one more time to rejoin the trail heading west. A ferry existed at Fort Boise since at least 1843; the Three Island crossing was also replaced by a ferry in 1869. A new wave of travelers came in the 1860s with
17100-477: The Snake River took several thousand salmon in one afternoon by means of spears." To the east and upriver of the falls, many Shoshone and Bannock lived in more nomadic groups, traveling to the falls during the spring salmon run then gathering camas bulbs and hunting bison through the summer and autumn months. The Snake River at Hells Canyon formed a natural dividing line between the Nez Perce and Shoshone, who considered each other enemies. The Nez Perce allied with
17290-508: The Snake River, moving to the Big Camas Prairie to set up camp. At that time the region between the Big Camas Prairie and the Snake River was occupied by a few white settlers, 2500 cattle, and 80 horses. On May 30 the Bannock group, after trying to sell a buffalo skin robe to cowboys on the plain, shot two in an altercation. Lou Kensler and George Nesby survived their wounds and traveled with the third member of their party, William Silvey, to
17480-482: The Snake River. Next, they moved along the river, killing several settlers along the way. Bernard's cavalry traveled by road to Rattlesnake station, where they joined with more military cavalry, as well as local militia volunteers from Alturas. At this time, Bernard claimed there were 300 Bannock warriors in the Lava Beds, plus 200 who had raided Glenn's Ferry and King Hill Station. The Bannock were rushing westward to meet with their Paiute allies, who were traveling down
17670-545: The Snake Valley. In 1866, in order to protect the Shoshone-Bannock groups in the Boise Snake Valley from fearful and aggressive settlers, Governor Lyon created a refugee camp for a few hundred of the Bannock near Boise City. The camp's lack of sufficient resources forced the Shoshone-Bannock to depend on the local settlers for work and food. Many Shoshone-Bannock asked to be given the security of their own reservation land. The proposed relocation to eastern Idaho challenged
17860-541: The Snake headwaters was sculpted by multiple Ice Age glaciations. Starting about 200,000 years ago, the Buffalo glaciation filled Jackson Hole to a depth of 2,000 feet (610 m). Ice flowed down the Snake River Canyon all the way to Idaho. The Bull Lake glaciation, about 80,000–35,000 years ago, and the Pinedale glaciation, ending about 15,000 years ago, were much smaller and did not fill the entire valley. These glaciations carved
18050-485: The Snake region by the mid-1860s, affecting a vast majority of the Shoshone-Bannock inhabitants. The Shoshone-Bannock were dramatically influenced by arrival of Euro-Americans and the rapid expansion of the trade-based economy. On a cultural level, the Euro-Americans' way of life challenged the values and seasonal traditions of the Shoshone-Bannock. New practices of agriculture, managing livestock, and production replaced
18240-423: The Snake watershed touches Montana for a long distance, but does not extend into it. The Snake drains by far the largest area of any Columbia River tributary, making up about 40 percent of the entire Columbia River watershed. Compared with the Columbia above their confluence, the Snake River is about 180 miles (290 km) longer and drains a similarly sized area, though the Columbia carries more than twice
18430-471: The Snake watershed, from Craters of the Moon National Monument northeast of Twin Falls to the Yellowstone caldera, while ancient lava flows of the Columbia River basalts underlie the western part of the watershed. The Snake River Plain is the largest area without mountains, but it still features rugged terrain, being crisscrossed by canyons formed by the Snake River and its tributaries. Due to
18620-647: The Snake, Clearwater and Salmon Rivers. Clans gathered at communal fishing sites starting about May or June. Fishing moved from the lower rivers to higher elevation streams throughout the summer, while fall-run fish were preserved for winter use. Shoshones in the western part of the Snake River Plain also depended heavily on the salmon run. At Shoshone Falls and the smaller cataracts downstream, fishing platforms, temporary brush weirs, spears, baskets and fish traps were employed at large scale. Captain Benjamin Bonneville in 1832 observed that "Indians at Salmon Falls on
18810-534: The Tetons, and a graben valley developed between the Hoback and Teton fault zones, creating Jackson Hole. As the valley dropped, water filled it to create Lake Teewinot, which drained east into the Green River – Colorado River system. About 1 Ma, the Snake River captured the Jackson Hole watershed, draining Lake Teewinot and finally connecting the modern-day Snake headwaters to the rest of the river. This landscape around
19000-619: The Umatilla Agency, a reservation near the Umatilla River whose people were potential allies of the Bannock band, accidentally encountered a large band of Umatilla warriors. Feeling threatened by the increased movements of state militias around their territories, the Umatilla had ridden out in defense. The Umatilla quickly surrendered and offered to fight with Miles against the Bannock. Historian Brigham D. Madsden suggested they were attracted to
19190-503: The Union retreat at that battle. The battalion then became part of V Corps and fought in the Battle of Antietam and the Battle of Fredericksburg . In March 1863, three companies of the battalion were disbanded due to a shortage of replacements. It fought in the Battle of Chancellorsville and was part of the rearguard during the retreat across the Rappahannock . The battalion then fought in
19380-539: The West Coast. While dam construction, commercial fishing and other human activities have greatly reduced anadromous fish populations since the late 19th century, the Snake River watershed is still considered important habitat for these fish. The Snake and its tributary, the Salmon River , host the longest sockeye salmon run in the world, stretching 900 miles (1,400 km) from the Pacific to Redfish Lake , Idaho. Since
19570-639: The adjacent Seven Devils Mountains rising up to 8,000 feet (2,400 m) above the river, Hells Canyon is one of the deepest canyons in North America, almost one-third deeper than the Grand Canyon . Within the canyon it is joined from the left by the Imnaha River , then from the right by its longest tributary, the Salmon River . Further north, it begins to form the Idaho– Washington border, and receives
19760-509: The ancestral Columbia River to the Pacific was established about 40 Ma. By about 17 Ma, the "Salmon-Clearwater River", or the modern day lower Snake River, flowed west into the Columbia and on to the Pacific. Another ancient river system drained what is now the western Snake River Plain. Some geologists propose that this flowed to the Columbia on a course south of the present-day Blue Mountains, while others propose it drained towards Northern California . The Columbia River basalts ,
19950-494: The area were dug in and offered fierce resistance to the regiment's advance. On 8 November, the regiment attacked the ridge but the attack was hampered by a typhoon. After four days of heavy fighting and casualties, the regiment secured Breakneck Ridge. The capture of the ridge ended the last significant Japanese resistance on Leyte. On 30 December 1944, the regiment was attached to the Western Visayas Task Force for
20140-479: The attack on San Juan Hill . The regiment helped capture the heights on 1 July after fierce fighting with Spanish troops. The Spanish troops surrendered on 16 July. Due to disease issues, the 21st Infantry was withdrawn from Cuba on 23 August. On 18 April 1899, the regiment was sent to the Philippines to reinforce US Army units fighting against forces of the recently declared First Philippine Republic . On 13 June,
20330-417: The basalt layers to form a plateau. From about 11–9 Ma, crustal deformation related to the Yellowstone hotspot caused the western half of the Snake River Plain to sink, creating a graben -type valley between parallel fault zones to the northeast and southwest. The outlet of the ancient Snake River was blocked, and water accumulated to form the vast Lake Idaho starting about 10 Ma. The eastern half of
20520-554: The borders of Idaho, Oregon and Washington , and finally the rolling Palouse Hills of southeast Washington. It joins the Columbia River just downstream from the Tri-Cities, Washington , in the southern Columbia Basin . The river's watershed , which drains parts of six U.S. states , is situated between the Rocky Mountains to the north and east, the Great Basin to the south, and the Blue Mountains and Oregon high desert to
20710-734: The campaign and suffered no desertions. In June 1878, the Bannock tribe left their reservation in southern Idaho, beginning the Bannock War . After marching 35 miles in a day, the regiment overtook the tribe on 13 August, scattering it so that it no longer posed a threat and had to return to the reservation. In June 1884, the regiment was sent to the Department of the Platte and stationed in Nebraska and Wyoming. The regiment then moved to southern Kansas to discourage
20900-444: The capture of Mindoro . During the next month, the regiment cleared the island of Japanese troops. In this phase of the battle, the regiment suffered casualties of one killed and seven wounded while killing dozens of Japanese troops. Meanwhile, K Company captured Marinduque on 3 January 1945. The island was previously cleared of most Japanese troops by Filipino soldiers and recognized guerrillas. The regiment's cannon company supported
21090-540: The creation of the Reclamation Service (now the Bureau of Reclamation ) in 1902, the federal government began to play a more direct role in water resources development. The expansive Minidoka Project was the first federal reclamation project in Idaho. Starting with Minidoka Dam in 1906, the project would grow over the next few decades to include major reservoirs at Jackson Lake , American Falls and Island Park , and
21280-409: The crime. In response to the crackdown, a friend of Pe-tope, Nampe-yo-go, killed Alexander Rhodan, a beef contractor for the reservation. Agent Danilson asked the nation to capture the killer and turn him over to the US officials, but he was resisted by the Shoshone-Bannock. According to their tradition of reconciliation, they said it was the duty of the family of Nampe-yo-go to resolve his crime, not
21470-441: The distinctive peaks of the Tetons into their present form and scoured lake basins in the valley floor, including modern-day Jackson Lake. While the Snake River course beyond Jackson Hole was not directly impacted by glaciations, its landscape was dramatically changed by Ice Age flooding events. About 30,000 years ago, the climate of western North America was much wetter than today. The Great Salt Lake Basin filled with water to form
21660-484: The division's deployment schedule would not have allowed the battalions to be prepared for combat. On 1 November 1967, the 4th Battalion was reactivated at Schofield Barracks to become the fourth battalion of the 11th Light Infantry Brigade , which was already serving in Vietnam. 4th Battalion deployed to Vietnam on 14 April 1968 and was based in Đức Phổ District . The battalion also operated west of Tam Kỳ and at Đông Hà . It
21850-544: The doubtful question is set at rest forever. Yet from the force of the current and the frequency of rapids, it may still be advisable, and perhaps preferable, to continue the land transport." Canadian fur trappers with the British Hudson's Bay Company (HBC) reached the Snake River watershed in 1819. As American fur trappers kept coming to the region, the HBC ordered the Canadians to kill as many beavers as they could, under
22040-505: The easily farmable land was soon developed, and they could not raise the capital for further expansion. In addition, low water by late summer posed a challenge to farmers, and the irrigation companies could not afford to build dams to provide water storage. With many private irrigation companies verging on insolvency, the federal government began to explore programs assisting agricultural development. The 1894 Carey Act granted large tracts of dry federal land to western states, which then sold
22230-511: The end of large new irrigation developments not only for the Snake River system, but for the Bureau of Reclamation as a whole. Agriculture has significantly impacted water quality in the Snake River upstream of Hells Canyon. Water removed from the river for irrigation becomes contaminated with chemical fertilizers and manure, and percolates into the Snake River Aquifer. Pollutants collect in
22420-442: The first American fur trading post west of the Rocky Mountains, but abandoned it after that year's harsh winter. The 1811 Pacific Fur Company expedition led by Wilson Price Hunt attempted to find a route from Henrys Fork to the Columbia River. After suffering a wreck in the falls of the Snake River Canyon, they took an overland route through the Snake River Plain, through what is now the Boise Valley or Treasure Valley, then crossed
22610-555: The first non-natives to see the river. Fur trappers explored more of the watershed, and drove beaver to near extinction as the Americans and British vied for control of Oregon Territory . Although travelers on the Oregon Trail initially shunned the dry and rocky Snake River region, a flood of settlers followed gold discoveries in the 1860s, leading to decades of military conflict and the eventual expulsion of tribes to reservations. At
22800-474: The first successful river descent of Hells Canyon, a harrowing ride that skirted disaster several times. In 1895 the steamboat Norma , which had been built to haul copper ore on the Snake River above Hells Canyon, also made the run under similar circumstances. In the 1870s, Boise (to which Idaho's capital was moved in 1866) expanded rapidly as growth slowed in Lewiston. Gold drew more than 25,000 prospectors to
22990-576: The geographic depression of the eastern Snake River Plain. The gradual eastward migration of this topographic high had the effect of pushing the Continental Divide to the east. Prior to the formation of the eastern Snake River Plain, the drainage area east of about Arco, Idaho – the modern headwaters and upper course of the Snake River – flowed towards the Atlantic Ocean via the Mississippi River system. The migrating Continental Divide tilted
23180-410: The government's encouragement for them to abandon this practice. The population was very dense for the land, numbering 1,037 in 1872. The Shoshone-Bannock struggled to live by subsistence. While the government made sizable appropriations to purchase the supplies necessary to feed the community, food crises arose during the winters of 1874–1875 and 1876–1877, resulting from diminished game for hunters and
23370-457: The groundwater and eventually enter the river via spring flows. Excess nitrogen, phosphorus and bacterial loads occur in many locations across southern Idaho. Large algae blooms are a recurring issue in summer. The U.S. Environmental Protection Agency has established water quality guidelines for Snake River flows entering Hells Canyon, which cover bacteria, mercury, excess nutrients, pesticides, sediments and water temperature. Implementation of
23560-606: The head of a small canyon, North of what is now known as Battle Mountain State Park in Oregon. Gen. Howard encountered the Bannock at the junction of Butter Creek and the Columbia River on July 7, resulting in conflict. Five U.S. soldiers were injured, and one died from his wounds. The fight resulted in an unknown number of casualties on the Bannock side, and they left going to the southeast. The next fight occurred on July 12, when Captain Miles of
23750-567: The hemp weed". Another Nez Perce name for the Snake River was Pikúunen , specifically referring to the stretch upstream of the Clearwater confluence. The Wanapum and Walla Walla people called the lower Snake River below the Clearwater Naxíyam Wána . The Shoshone called the river Yampapah , after the yampah plant that grew profusely along its banks. Downriver of Shoshone Falls, salmon and their cousins such as steelhead trout – anadromous fish which spend their adult lives in
23940-403: The high bounty that had been placed on Chief Egan's head. The conflict resulted in the deaths of five Bannock warriors and their eventual flight. That night, Umatilla leaders pursued the Bannock. They entered the camp posing to conduct negotiations, and killed Chief Egan and several other warriors. On July 20, one of Bernard's battalions, under the leadership of Lieutenant Colonel Forsyth, met
24130-452: The inactivating 44th Infantry Regiment. It was at this point that the regiment adopted the name "Gimlet". The primary wartime mission of the 21st Infantry was to conduct a mobile defense of the beaches and inland sectors of the northern half of the island of Oahu . It was assigned on paper to the 24th Infantry Division on 26 August 1941. After the Attack on Pearl Harbor , the regiment guarded
24320-454: The land to farmers and solicited private investors to organize irrigation districts. Investors would then recoup their capital by selling water rights to farmers. Irrigation plans were reviewed by engineers, who determined the economic feasibility of the projects. Although the Carey Act saw little success in most states, it greatly benefited Idaho. Some 60 percent of all lands developed under
24510-457: The landscape of the Snake River Plain, creating the Snake River Canyon and its waterfalls, vast boulder fields, cliffs and coulees . The floodwaters then emptied through Hells Canyon; however, most evidence of their effects on the lower Snake River was erased by the much larger Missoula Floods that engulfed the Columbia Basin during the same period. Caused by the repeated collapse of an ice dam in western Montana, dozens of floods overflowed into
24700-408: The largest North American runs of salmon and other anadromous fish . For thousands of years, salmon fishing has played a central role in the culture and diet of indigenous peoples. The Shoshone and Nez Perce were the largest of several tribes that lived along the river by the turn of the 19th century. In 1805, while searching for a route from the eastern US to the Pacific, Lewis and Clark became
24890-510: The last significant Japanese unit in the Philippines that had not yet been attacked. In October 1945, the regiment, along with the rest of the 24th Division, arrived in Japan for occupation duties . It was stationed at Camp Wood near Kumamoto on Kyushu . Due to the postwar demobilization, the regiment was left with two understrength battalions. It also suffered from shortages of crew-served weapons, radios, field gear and boots. On 24 June 1950,
25080-466: The lower Salmon River. The Northern Shoshone and the Bannock , a Northern Paiute group that became culturally associated with the Shoshone, occupied an area stretching from the Snake River Plain east to the Rocky Mountains and south towards the Great Basin, as well as valleys of the upper Salmon River. A Nez Perce name for the river was Kimooenim or variations thereof, meaning "the stream/place of
25270-481: The lower Snake River from the north, backing water as far upstream as Lewiston. The formerly west-flowing Palouse River was rerouted to flow south into the Snake River, forming Palouse Falls, whose outsized plunge pool attests to the force of the floods. Starting around the end of the last glacial period, the Snake River Plain was inhabited by hunter-gatherers of the ancient Clovis (10000–9000 BCE), Folsom (9000–8000 BCE) and Plano (8600–5800 BCE) cultures. Along
25460-603: The lower Snake River in Washington, the Marmes Rockshelter – flooded in 1968 after the construction of Lower Monumental Dam – has yielded archeological evidence of continuous human occupation from about 9000 BCE until about 1300 CE. Starting about 2200 BCE, people in the western Snake River basin began to adopt a semi-sedentary lifestyle, with an increased reliance on fish (primarily salmon) and food preservation and storage. Shoshoni -speaking peoples arrived in
25650-469: The lower one-fourth of its course. By the time it reaches Hells Canyon Dam , 247 miles (398 km) from the mouth, the mean annual discharge is about 19,000 cu ft/s (540 m /s) – just over a third of the discharge at the mouth. Just two downstream tributaries, the Clearwater and Salmon Rivers, contribute about half of the total flow of the Snake. The 107,500-square-mile (278,000 km ) Snake River watershed drains about 87 percent of
25840-430: The massive Lake Bonneville , about the size of modern-day Lake Michigan . About 15,000 years ago the lip of Red Rock Pass south of present-day Pocatello, Idaho abruptly collapsed, releasing a tremendous volume of water from Lake Bonneville into the Snake River Plain. The peak of the flood was about 500 times bigger than the largest recorded flood of the Snake at Idaho Falls in modern times. The flood completely altered
26030-567: The military were led by Miles in August and September. The rest of the Bannock returned to the Fort Hall Reservation or pursued peaceful hunting on their own in groups. A few more skirmishes between the scattered Bannock and military forces occurred, such as on August 9 in Bennett's Creek by the Snake River, but no casualties were recorded. After the Bannock War of 1878, the American government restricted
26220-470: The mining industry and the difficulty of importing goods set off an agricultural boom in the Boise Valley. By the 1880s, settlers also came to the upper Snake River north of Idaho Falls, where fertile, sandy soils presented ideal conditions for the iconic russet potato ("Idaho potato"). The dry climate made irrigation necessary, and numerous private irrigation companies were formed. Private canal systems around Boise and Idaho Falls saw some success, but all
26410-632: The movements of the Bannock in and out of the Fort Hall Reservation. Connections with other tribal groups were restricted, as well as the Bannock freedom to use local resources. Subdued from the battles and lack of resources, the Bannock worked to construct community within the reservation. Other Bannock and Paiute prisoners were interned at the Malheur Reservation in Oregon. While the Paiutes had been more peripherally involved, in November 1878, General Howard moved about 543 Bannock and Paiute prisoners from
26600-462: The nation. That summer, a large number of the Shoshone-Bannock left the reservation, because of the lack of supplies, violence between the Native Americans and the Euroamericans, conflicts between the nations, and Danilson's actions. This sparked the Bannock War of 1878, as the US government ordered the Army to return the people to the reservation to control them. In May 1878, Chief Buffalo assembled 200 Bannock warriors from Fort Hall at Payne's Ferry on
26790-479: The nearby Baker's camp. Not long after this incident, the Bannock at a camp near the Lava Beds were attacked by white men. They killed a settler in the conflict but lost their camp's resources. The news of the increased violence spread to Idaho's territorial capital at Boise City. Governor Brayman notified Brigadier General O. O. Howard , commander of the Military Department of the Columbia. Brayman wrote in
26980-454: The newly completed First Transcontinental railroad . Between 9 and 31 August, each company of the 21st arrived in Arizona and consolidated with the corresponding company of the 32d. In Arizona, the 21st Infantry protected transportation routes, escorted US mail deliveries, scouted Indian movements and built new wagon routes. The regiment's troops frequently clashed with Apache Indians . In 1872,
27170-481: The northern shore of Oahu from Japanese attacks. During May 1943, the division underwent combat training and departed for Australia. It arrived at Rockhampton on 8 September 1943. For the next few months, it conducted additional training in amphibious and jungle warfare. In January 1944, the regiment, along with the rest of the division moved to Goodenough Island to prepare for the Hollandia landings . On 22 April,
27360-450: The ocean, returning to fresh water to spawn – were a key food source for indigenous peoples, and were of great cultural importance. Rituals such as the first salmon ceremony were widely observed along the Columbia, Snake and other Northwest rivers, and so were strict catch limits, such that a healthy number of salmon would survive to reach their natal streams. The Nez Perce had more than seventy permanent villages among their fishing grounds on
27550-408: The old country. It is its lonely grandeur that impresses one so deeply; all of the other historic places have the adjuncts of civilization, and one is almost overshadowed by a city while in their presence." Most travelers on the Oregon Trail regarded the arid Snake River Plain as an obstacle to be crossed, not a land to be settled. This began to change with the Boise gold strikes, where the demands of
27740-513: The original site in 1863. A military detachment was stationed there to quell any further violence; however, tensions continued to increase, and more wagon trains and mining parties were attacked. Starting in 1864, the Snake War was fought across much of southern Idaho, with numerous battles between the U.S. Army and the Shoshone, Bannock and Paiute. By 1868, exhausted after years of fighting, Chief Pocatello and many others surrendered and relocated to
27930-524: The outflow carved Hells Canyon, emptying Lake Idaho and integrating the upper Snake and Salmon-Clearwater into a single river system. The Teton Range, a defining topographic feature of the modern Snake River headwaters, first began to rise about 10 Ma as the Teton Fault began to move, displacing the mountain block upward as the surrounding land dropped. About 2 Ma, the Hoback Fault formed east of
28120-487: The past, salmon swam as far upriver as Shoshone Falls. Emerging from Hells Canyon Dam, the Snake surges northward through the Hells Canyon Wilderness , where the majority of the river corridor is accessible only by boat and numerous Class III-IV rapids historically posed a major barrier to navigation. Today, the canyon and the surrounding Hells Canyon National Recreation Area are a popular location for whitewater boating, fishing, horseback riding and backpacking. With
28310-400: The present-day confluence of the Columbia River and Salmon-Clearwater had been established, with the combined flow draining through Wallula Gap. About 2.5 Ma, Lake Idaho reached a maximum elevation of 3,600 feet (1,100 m) above modern sea level, and overflowed northward into the Salmon-Clearwater drainage near present-day Huntington, Oregon . Over a period of about two million years,
28500-409: The rationale that "if there are no beavers, there will be no reason for the Yanks to come," and even if the Americans did ultimately gain control, the HBC would already have taken all the profit. Focused primarily on the upper Snake River region, the "fur desert" policy was carried out in nine expeditions from about 1824–1831 and aimed to decrease the Americans' economic interest in the Oregon Country ,
28690-476: The regiment by 8 July. 1st and 3rd Battalions repelled the North Korean advance until 12 July. During the Battle of Chochiwon , the 21st Regiment suffered 531 killed, wounded or missing. On 30 August, the 34th Infantry's 3rd Battalion became the 21st's 2nd Battalion. The regiment fought on the Naktong River line until 19 September. The 24th Division, including the 21st, was awarded a Presidential Unit Citation for its actions between 2 July and 15 September. After
28880-427: The regiment conducted an amphibious landing at Tanahmerah Bay in conjunction with the 19th Infantry Regiment . During the Battle of Hollandia , the regiment was able to advance quickly despite terrain conditions to overrun the airfields at Hollandia, which were defended by Japanese service troops. Four days later, the 21st Infantry linked up with the 41st Infantry Division , completing the pincer movement and trapping
29070-430: The regiment crossed the Talomo River near Mintal on 8 May but had to withdraw two days later due to Japanese resistance. Two battalions of the regiment attacked again along the east bank of the Taloma on 12 May. By 14 May, the regiment had cleared Japanese positions enough that the regiment could secure Route 1-D to Mintal. During the battle for Mintal, PFC James H. Diamond earned the Medal of Honor posthumously. During
29260-416: The regiment fought in defense of the southern approaches to Manila . The Republic forces massed on the Zapote River , which divided the two armies on the edge of Manila Bay . The regiment faced 5,000 entrenched Republic soldiers. I and F companies skirmished with the Republic forces at a bridge over the river. The fighting then escalated into artillery duels. After several hours, the American artillery forced
29450-457: The regiment inflicted at least 2,000 casualties on Japanese troops. On 12 July, a battalion combat team of the 21st landed on the northwest shore of Sarangani Bay , where Japanese troops still held out. Along with other American & Filipino military units and recognized guerrillas, the battalion combat team cleared the Japanese from the area. The battalion combat team returned to Davao City on 11 August. The Japanese troops at Sarangani Bay were
29640-453: The regiment was transferred to the Department of the Columbia , with the regimental headquarters located at Fort Vancouver . The companies were based at posts throughout Washington, Oregon and Idaho. In late 1872, the regiment was ordered to provide troops for the expedition against the Modoc . The regiment provided a three-company battalion, which fought in the expedition's battles between January and April 1873. B, C and F Companies fought at
29830-512: The regiment went back to the Philippines for more garrison duty and stayed there until 1912. Upon its return, the 21st was garrisoned at Vancouver Barracks. From March 1916, the regiment protected the Arizona and California borders from Villista raids across the border. In December 1916, second battalion of the regiment participated in the Panama–California Exposition , defending against a simulated attack from two Navy cruisers, Frederick and San Diego , and several aircraft. In April 1917, it
30020-435: The regiment's 2nd Battle Group and was assigned to the 25th Infantry Division at Schofield Barracks during February 1957. C Company became the regiment's 3rd Battle Group and was assigned to the 63rd Infantry Division in May 1959. The 3rd Battle Group was inactivated on 1 April 1963. During the same year, the army was reorganized, dividing infantry divisions into brigades composed of three battalions. The 2nd Battle Group became
30210-444: The regiment's first battalion participated in Exercise Lightning Forge with other units of the 25th Division's 2nd Stryker Brigade Combat Team. Between 2019 and 2020, 3rd Battalion deployed with 1st Stryker Brigade Combat Team, 25th Infantry Division out of Fort Wainwright , Alaska in support of Operation Inherent Resolve . On 8 June 2023, 3rd Battalion was inactivated at Fort Wainwright . Snake River The Snake River
30400-415: The regiment's headquarters and medical companies earned the regiment another Presidential Unit Citation for their defense against PVA attempts to overrun the regimental command post and aid station at Sanghongjong-ni . The UN renewed the attack in the UN May–June 1951 counteroffensive . During fighting between 14 and 15 November, G Company captured two heavily defended hills against PVA resistance, earning it
30590-462: The regional slope such that drainage flowed west into Lake Idaho, whose water levels saw a significant increase about 4.5 Ma. The Snake River Plain drainage system continued to expand east, towards what is now Yellowstone National Park. During this expansion, the Snake also captured the Bear River , which was only rerouted towards its modern outlet in the Great Salt Lake Basin about 50,000 or 60,000 years ago by lava flows in southeast Idaho. In
30780-429: The remaining Japanese troops. The regiment remained to defend Hollandia until fall 1944. For the recapture of Leyte, the regiment became a separate regimental combat team (RCT). It was given the task of securing the Panaon Straits, located at the southern tip of Leyte. Capture of the straits would enable Naval forces to move to the western side of the island. The regiment captured the northern coast of Panaon Island and
30970-422: The river flowing steadily even in the driest of summers. At King Hill , about 50 miles (80 km) northwest of Twin Falls, water levels remain about 10,000 cu ft/s (280 m /s) for most of the year, increasing about 20 percent during snowmelt and decreasing about 20 percent with late summer irrigation diversions. Despite its great length, the Snake River accumulates most of its water in
31160-473: The river narrows, forming rapids and waterfalls. In the 70-mile (110 km) stretch between Milner Dam and the confluence with the Malad River near Hagerman Fossil Beds National Monument , the Snake River descends a total of 1,300 feet (400 m) over a series of cataracts and rapids, chief of which include Caldron Linn , Twin , Shoshone , Pillar , Auger, and Salmon Falls . Idaho Power operates several small hydroelectric plants along this stretch of
31350-434: The river. The largest single drop is 212-foot (65 m) Shoshone Falls , which in the spring flows with such force that 19th-century writers called it the "Niagara of the West". The Snake River continues flowing west, through the C. J. Strike Reservoir where it is joined from the left by the Bruneau River , then through the Morley Nelson Snake River Birds of Prey National Conservation Area before entering farmland on
31540-439: The south was a continuation of "Lewis's" or Salmon River. The expedition journals note the Nez Perce called it Kimooenim , although William Clark later erased mentions of the name to replace with "Lewis's". Six days later they reached the confluence of the Snake and Columbia Rivers, after noting a number of dangerous rapids as well as many native fishing sites on the lower Snake. The expedition established friendly relations with
31730-401: The southern shore of Leyte without meeting resistance, an hour before the main landings farther to the north. The 24th Division met heavy Japanese resistance during its landings, and the 21st was returned to control of the division on 30 October. On 5 November, the regiment replaced the 34th Infantry Regiment at Breakneck Ridge, west of Pinamopoan on Leyte's northern shores. Japanese troops in
31920-411: The state of Idaho, 18 percent of Washington and 17 percent of Oregon, in addition to small portions of Wyoming, Utah and Nevada . From the Lost Trail Pass north of Salmon, Idaho to Tri-Basin Divide south of Afton, Wyoming , the eastern edge of the Snake River watershed follows the Continental Divide . As the Continental Divide also forms the Idaho–Montana border south of Lost Trail Pass,
32110-433: The summer. The Idaho State Historical Society writes that "Perrine’s venture contrasted remarkably with private canal company failures that led to congressional provision for federal reclamation projects after 1902. As a rare successful example of state supervised private irrigation development provided for in [the Carey Act] of 1894, Milner Dam and its canal system have national significance in agricultural history." With
32300-401: The traditional resources on which the Shoshone-Bannocks had relied. They became more dependent on Euro-American methods and products. American leaders were eager to acquire lands from the Shoshone-Bannock and in the 1860s, began to work to trade goods for titles to the Snake River Plains. The land trade attracted new waves of migrants to the Idaho territory , especially in the Boise region of
32490-419: The turn of the 20th century, some of the first large irrigation projects in the western US were developed along the Snake River. South-central Idaho earned the nickname " Magic Valley " with the rapid transformation of desert into farmland. Numerous hydroelectric dams were also constructed, and four navigation dams on its lower section created a shipping channel to Lewiston, Idaho – the furthest inland seaport on
32680-434: The vast region of the Pacific Northwest centering on modern-day British Columbia, Washington, Oregon and Idaho. By the time the Americans annexed Oregon Territory in 1848, beaver were nearly extirpated across much of the Rocky Mountains. Starting in the 1840s, the Oregon Trail became well established, and thousands of settlers passed through the Snake River Plain on their way to the Willamette Valley . Coming from Wyoming,
32870-450: The volume of water. The Snake River watershed is very mountainous, with the northern two-thirds of it occupied by vast mountain ranges of the Rockies, primarily the Salmon River Mountains of central Idaho and the Bitterroot Range along the Idaho–Montana border. The Blue Mountains form much of the western boundary of the Snake watershed from southeast Washington down into Oregon. To the south are numerous small isolated mountain ranges of
33060-418: The war with two soldiers wounded by booby traps. The unit was relieved by South Vietnamese soldiers. The battalion was withdrawn from South Vietnam on 23 August 1972 and inactivated in Oakland on the same day. The regiment's 4th and 5th Battalions were activated at Schofield Barracks on 6 December 1965 to serve with the 25th Infantry Division. However, both battalions were inactivated on 3 January 1966 because
33250-403: The watershed is barren desert, and only about 1 percent is urbanized. Most of the Snake River watershed is public land, with the U.S. Forest Service managing the Nez Perce , Clearwater , Bitterroot , Umatilla , Wallowa–Whitman , Payette , Boise , Salmon–Challis , Sawtooth , Caribou–Targhee and Bridger–Teton National Forests that cover much of the northern and eastern parts of
33440-630: The watershed is farmland; irrigated farming of potatoes, sugar beets, onions, cereal grains and alfalfa are dominant in the Snake River Plain, while the Palouse Hills of the northwest host mainly dryland wheat and legume production. About 15 percent of the watershed is forested, distributed across two temperate coniferous forest ecoregions : South Central Rockies forests , consisting primarily of Douglas fir , Engelmann spruce , subalpine fir , and lodgepole pine , and North Central Rockies forests , which include mountain hemlock , white spruce , alpine fir and western larch . About 4 percent of
33630-400: The watershed. The forests contain numerous designated wilderness areas, including the Sawtooth , Selway–Bitterroot , Frank Church-River of No Return , Gospel Hump , Hells Canyon , Teton and Gros Ventre . National Park Service land includes Craters of the Moon National Monument and Yellowstone and Grand Teton National Parks. Large areas of privately owned farmland are concentrated in
33820-442: The west. The region has a long history of volcanism ; millions of years ago, Columbia River basalts covered vast areas of the western Snake River watershed, while the Snake River Plain was a product of the Yellowstone volcanic hotspot . The river was further altered by catastrophic flooding in the most recent Ice Age , which created such features as the Snake River Canyon and Shoshone Falls . The Snake River once hosted some of
34010-407: The western side of Idaho's Treasure Valley . Passing 30 miles (48 km) west of Boise , it crosses briefly into Oregon before turning north to form the Oregon–Idaho border. It is joined by several major tributaries in quick succession – the Boise River from the right, the Owyhee and Malheur Rivers from the left, the Payette and Weiser Rivers from the right near Ontario, Oregon , then
34200-439: Was able to hold off the KPA infantry for six hours, but was forced to withdraw, suffering heavy casualties. During the Battle of Osan , Task Force Smith suffered casualties of 60 killed, 21 wounded and 80 captured, out of a total strength of 540. The remainder of the 21st Infantry arrived at Chochiwon by 7 July. Chochiwon was located along one of two roads to the Kum River and Taejon . The remnants of Task Force Smith joined
34390-402: Was attached to the 23rd Infantry Division between 15 February 1969 and the battalion's withdrawal on 28 June 1971. On 26 August 1968, Staff Sergeant Nick Bacon of B Company took command after two platoon leaders were wounded. He led the two platoons against the Viet Cong forces, destroying a bunker and machine gun nest as well as personally killing four Viet Cong soldiers. Bacon then climbed onto
34580-489: Was based at Tây Ninh . 3rd Battalion fought in Operation Attleboro between September and November 1966. In January 1967, the battalion participated in Operation Cedar Falls . Between February and April, it participated in Operation Junction City . The 196th was then transferred to Chu Lai . On 14 May 1969, medic Daniel J. Shea posthumously earned the Medal of Honor for rescuing wounded soldiers while mortally wounded. 3rd Battalion C Company medic James McCloughan received
34770-402: Was combat ineffective due to losses by July. The surviving men were assigned to the 12th Infantry Regiment's 1st Battalion. By 20 September, the battalion was composed of just 48 men. It was withdrawn on 2 November and moved back to Fort Hamilton. The regiment was brought up to full strength at Fort Hamilton and moved back to Virginia for reconstruction duties by December 1865. The 2nd Battalion
34960-427: Was commissioned to haul supplies up the Snake River to Fort Taylor. Captained by veteran Oregon river pilot Len White, the Wright was the first steamboat to run on the Snake River and the Columbia above The Dalles . Two years later, Elias D. Pierce discovered gold to the east on Nez Perce treaty land. As thousands of fortune seekers flocked to the area, the city of Lewiston was founded in 1861, in violation of
35150-425: Was inactivated on 15 December 1987. 3rd Battalion reactivated at Schofield Barracks with the 25th Division and inactivated on 15 July 1995. It reactivated with the 25th Division's 1st Brigade at Fort Lewis on 16 March 2002. 4th Battalion reactivated on 16 January 1986 with the 7th Infantry Division at Fort Ord . It was inactivated on 15 September 1993. 5th Battalion was reactivated on 16 May 1985 also at Fort Ord with
35340-401: Was located as follows: HQ and Company E at Fort William H. Seward , Territory of Alaska (TA); Company F at Fort Liscum , TA; Company G at Fort Gibbon , TA; Company H at Fort St. Michael , TA. The 3rd Battalion was stationed at Fort Douglas , Utah . The regiment was assigned to the Hawaiian Division on 22 October 1921; enlisted personnel stationed at Fort George Wright were transferred to
35530-413: Was relieved by the 34th Infantry Regiment on 29 May. During the past two weeks, the regiment had inflicted heavy casualties on a battalion of the Japanese 100th Division . On 31 May, the regiment attacked north from Lamogan on the left flank of the 24th Division. It captured Wangan on 9 June. The regiment then advanced on Calinan and was withdrawn from combat on 19 June. During its campaign in Mindanao,
35720-408: Was stationed at Camp Winthrop , near Richmond . As part of the Army expansion in 1866, the 2nd Battalion became the 21st Infantry Regiment on 7 December 1866. In 1869, the Army was reduced in size and the 32d Infantry Regiment consolidated with the 21st. The 32d was based in the Arizona Territory and the 21st departed Richmond on 12 April. The regiment was the first military unit to be transported by
35910-406: Was the same or similar to the Plains Indian common sign for "snake." The English name for the river was likely derived from this interpretation of the hand gesture, although it is uncertain when the name was first used. The first Euro-Americans to reach the Snake River watershed were the Lewis and Clark Expedition, who in August 1805 crossed the Continental Divide at Lemhi Pass and descended to
36100-418: Was transferred to Camp Kearny and was subordinated to the 16th Division 's 31st Infantry Brigade. The regiment trained troops for fighting in France with the American Expeditionary Forces . In March 1919, the regiment returned to Vancouver Barracks. The 21st Infantry, less the 2nd and 3rd Battalions, was stationed at Fort George Wright , Washington, as of June 1919 as a separate regiment. The 2nd Battalion
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