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Lake Superior Provincial Park. A personal hiking/photography vacation away from my smartphone and away from Donald Trump.
Bought me a new hat this week, it makes Lee laugh, I can't think why!! ; ) I'm assured no cats were harmed in the making of this headgear!
SOLD Burle Ash handle scales, this is a custom knife with lanyard hole, and scandinavian grind blade. This is for sale at $150 USD. contact me if interested.
SOLD
Located on Lac Bryson. Was discovered by the owners of the lake a few years ago. They do not know who lived there and what happened to them.
Rushmore Cave is the closest show cave to Mount Rushmore National Memorial in the United States. It contains a wide variety of natural formations. It is the ninth longest cave in South Dakota. It measures a distance of 3,652.6 feet (1,113.3 m).
It was discovered in 1876 when a log flume that supplied water to mining operations in town of Hayward broke and spilled onto the side of the hill. As the water flowed down the hill it started flowing into a small hole in the hillside. The local miners who went up to fix the flume noticed this abnormality and became suspicious of where this water was going. After fixing the flume, the men decided to go inside and explore. After about 30 feet (9.1 m), the men came to a large drop off which went down about 15 feet (4.6 m). They exited the cave, and went out into the woods where they cut down a tree and then used this tree as a ladder to access the cave. The miners then noticed that the majority of the cave was made out of limestone. Knowing that limestone doesn't contain any gold deposits, they abandoned the cave as a mining opportunity, and left it alone. Some of the local townspeople heard news of this discovery, and became very curious as to what they might find inside the cave.
The cave was created by a very long process stretching over a 360 million year time period. It started during the Mississippian Period, during which the entire Black Hills area was covered by a large inland sea. In this sea lived many kinds of sea creatures, and crustaceans. As these sea creatures died, their bodies sunk down to the sea floor. The flesh rotted away leaving behind many solid bone fragments which then compressed, and over time hardened into a rock known as limestone.
The cave has a cornucopia of rooms including the Entrance Room, Post Office, Image Room, Big Room, Fairyland, Rope Room, Geode Room, The Rouge Room (Party Room), Arrowhead Room, and the Floral Room.
The cave also includes boxwork and many dripstone formations including stalactites, stalagmites, columns, helictites and flowstone.
South Dakota is a landlocked U.S. state in the North Central region of the United States. It is also part of the Great Plains. South Dakota is named after the Dakota Sioux tribe, which comprises a large portion of the population with nine reservations currently in the state and has historically dominated the territory. South Dakota is the 17th largest by area, but the 5th least populous, and the 5th least densely populated of the 50 United States. Pierre is the state capital, and Sioux Falls, with a population of about 213,900, is South Dakota's most populous city. The state is bisected by the Missouri River, dividing South Dakota into two geographically and socially distinct halves, known to residents as "East River" and "West River". South Dakota is bordered by the states of North Dakota (to the north), Minnesota (to the east), Iowa (to the southeast), Nebraska (to the south), Wyoming (to the west), and Montana (to the northwest).
Humans have inhabited the area for several millennia, with the Sioux becoming dominant by the early 19th century. In the late 19th century, European-American settlement intensified after a gold rush in the Black Hills and the construction of railroads from the east. Encroaching miners and settlers triggered a number of Indian wars, ending with the Wounded Knee Massacre in 1890. As the southern part of the former Dakota Territory, South Dakota became a state on November 2, 1889, simultaneously with North Dakota. They are the 39th and 40th states admitted to the union; President Benjamin Harrison shuffled the statehood papers before signing them so that no one could tell which became a state first.
Key events in the 20th century included the Dust Bowl and Great Depression, increased federal spending during the 1940s and 1950s for agriculture and defense, and an industrialization of agriculture that has reduced family farming. Eastern South Dakota is home to most of the state's population, and the area's fertile soil is used to grow a variety of crops. West of the Missouri River, ranching is the predominant agricultural activity, and the economy is more dependent on tourism and defense spending. Most of the Native American reservations are in West River. The Black Hills, a group of low pine-covered mountains sacred to the Sioux, is in the southwest part of the state. Mount Rushmore, a major tourist destination, is there. South Dakota has a temperate continental climate, with four distinct seasons and precipitation ranging from moderate in the east to semi-arid in the west. The state's ecology features species typical of a North American grassland biome.
While several Democrats have represented South Dakota for multiple terms in both chambers of Congress, the state government is largely controlled by the Republican Party, whose nominees have carried South Dakota in each of the last 14 presidential elections. Historically dominated by an agricultural economy and a rural lifestyle, South Dakota has recently sought to diversify its economy in other areas to both attract and retain residents. South Dakota's history and rural character still strongly influence the state's culture.
The history of South Dakota describes the history of the U.S. state of South Dakota over the course of several millennia, from its first inhabitants to the recent issues facing the state.
Human beings have lived in what is today South Dakota for at least several thousand years. Early hunters are believed to have first entered North America at least 17,000 years ago via the Bering land bridge, which existed during the last ice age and connected Siberia with Alaska. Early settlers in what would become South Dakota were nomadic hunter-gatherers, using primitive Stone Age technology to hunt large prehistoric mammals in the area such as mammoths, sloths, and camels. The Paleolithic culture of these people disappeared around 5000 BC, after the extinction of most of their prey species.
Between AD 500 and 800, much of eastern South Dakota was inhabited by a people known as the 'Mound Builders'. The Mound Builders were hunters who lived in temporary villages and were named for the low earthen burial mounds they constructed, many of which still exist. Their settlement seems to have been concentrated around the watershed of the Big Sioux River and Big Stone Lake, although other sites have been excavated throughout eastern South Dakota. Either assimilation or warfare led to the demise of the Mound Builders by the year 800. Between 1250 and 1400 an agricultural people, likely the ancestors of the modern Mandan of North Dakota, arrived from the east and settled in the central part of the state. In 1325, what has become known as the Crow Creek Massacre occurred near Chamberlain. An archeological excavation of the site has discovered 486 bodies buried in a mass grave within a type of fortification; many of the skeletal remains show evidence of scalping and decapitation.
The Arikara, also known as the Ree, began arriving from the south in the 16th century. They spoke a Caddoan language similar to that of the Pawnee, and probably originated in what is now Kansas and Nebraska. Although they would at times travel to hunt or trade, the Arikara were far less nomadic than many of their neighbors, and lived for the most part in permanent villages. These villages usually consisted of a stockade enclosing a number of circular earthen lodges built on bluffs looking over the rivers. Each village had a semi-autonomous political structure, with the Arikara's various subtribes being connected in a loose alliance. In addition to hunting and growing crops such as corn, beans, pumpkin and other squash, the Arikara were also skilled traders, and would often serve as intermediaries between tribes to the north and south It was probably through their trading connections that Spanish horses first reached the region around 1760. The Arikara reached the height of their power in the 17th century, and may have included as many as 32 villages. Due both to disease as well as pressure from other tribes, the number of Arikara villages would decline to only two by the late 18th century, and the Arikara eventually merged entirely with the Mandan to the north.
The sister tribe of the Arikaras, the Pawnee, may have also had a small amount of land in the state. Both were Caddoan and were among the only known tribes in the continental U.S. to have committed human sacrifice, via a religious ritual that occurred once a year. It is said that the U.S. government worked hard to halt this practice before their homelands came to be heavily settled, for fear that the general public might react harshly or refuse to move there.
The Lakota Oral histories tell of them driving the Algonquian ancestors of the Cheyenne from the Black Hills regions, south of the Platte River, in the 18th century. Before that, the Cheyenne say that they were, in fact, two tribes, which they call the Tsitsistas & Sutaio After their defeat, much of their territory was contained to southeast Wyoming & western Nebraska. While they had been able to hold off the Sioux for quite some time, they were heavily damaged by a smallpox outbreak. They are also responsible for introducing the horse to the Lakota.
The Ioway, or Iowa people, also inhabited the region where the modern states of South Dakota, Minnesota & Iowa meet, north of the Missouri River. They also had a sister nation, known as the Otoe who lived south of them. They were Chiwere speaking, a very old variation of Siouan language said to have originated amongst the ancestors of the Ho-Chunk of Wisconsin. They also would have had a fairly similar culture to that of the Dhegihan Sioux tribes of Nebraska & Kansas.
By the 17th century, the Sioux, who would later come to dominate much of the state, had settled in what is today central and northern Minnesota. The Sioux spoke a language of the Siouan language family, and were divided into two culture groups – the Dakota & Nakota. By the early 18th century the Sioux would begin to move south and then west into the plains. This migration was due to several factors, including greater food availability to the west, as well as the fact that the rival Ojibwe & other related Algonquians had obtained rifles from the French at a time when the Sioux were still using the bow and arrow. Other tribes were also displaced during some sort of poorly understood conflict that occurred between Siouan & Algonquian peoples in the early 18th century.
In moving west into the prairies, the lifestyle of the Sioux would be greatly altered, coming to resemble that of a nomadic northern plains tribe much more so than a largely settled eastern woodlands one. Characteristics of this transformation include a greater dependence on the bison for food, a heavier reliance on the horse for transportation, and the adoption of the tipi for habitation, a dwelling more suited to the frequent movements of a nomadic people than their earlier semi-permanent lodges.
Once on the plains, a schism caused the two subgroups of the Sioux to divide into three separate nations—the Lakota, who migrated south, the Asiniboine who migrated back east to Minnesota & the remaining Sioux. It appears to be around this time that the Dakota people became more prominent over the Nakota & the entirety of the people came to call themselves as such.
The Lakota, who crossed the Missouri around 1760 and reached the Black Hills by 1776, would come to settle largely in western South Dakota, northwestern Nebraska, and southwestern North Dakota. The Yankton primarily settled in southeastern South Dakota, the Yanktonnais settled in northeastern South Dakota and southeastern North Dakota, and the Santee settled primarily in central and southern Minnesota. Due in large part to the Sioux migrations, a number of tribes would be driven from the area. The tribes in and around the Black Hills, most notably the Cheyenne, would be pushed to the west, the Arikara would move further north along the Missouri, and the Omaha would be driven out of southeastern South Dakota and into northeastern Nebraska.
Later, the Lakota & Assiniboine returned to the fold, forming a single confederacy known as the Oceti Sakowin, or Seven council fire. This was divided into four cultural groups—the Lakota, Dakota, Nakota & Nagoda-- & seven distinct tribes, each with their own chief—the Nakota Mdewakan (Note—Older attempts at Lakota language show a mistake in writing the sound 'bl' as 'md', such as summer, Bloketu, misprinted as mdoketu. Therefore, this word should be Blewakan.) & Wahpeton, the Dakota Santee & Sisseton, the Nagoda Yankton & Yanktonai & the Lakota Teton. In this form, they were able to secure from the U.S. government a homeland, commonly referred to as Mni-Sota Makoce, or the Lakotah Republic. However, conflicts increased between Sioux & American citizens in the decades leading up the Civil War & a poorly funded & organized Bureau of Indian Affairs had difficulty keeping peace between groups. This eventually resulted in the United States blaming the Sioux for the atrocities & rendering the treaty which recognized the nation of Lakotah null and void. The U.S., however, later recognized their fault in a Supreme Court case in the 1980s after several decades of failed lawsuits by the Sioux, yet little has been done to smooth the issue over to the best interests of both sides.
France was the first European nation to hold any real claim over what would become South Dakota. Its claims covered most of the modern state. However, at most a few French scouting parties may have entered eastern South Dakota. In 1679 Daniel G. Duluth sent explorers west from Lake Mille Lacs, and they may have reached Big Stone Lake and the Coteau des Prairies. Pierre Le Sueur's traders entered the Big Sioux River Valley on multiple occasions. Evidence for these journeys is from a 1701 map by William De L'Isle that shows a trail to below the falls of the Big Sioux River from the Mississippi River.
After 1713, France looked west to sustain its fur trade. The first Europeans to enter South Dakota from the north, the Verendrye brothers, began their expedition in 1743. The expedition started at Fort La Reine on Lake Manitoba, and was attempting to locate an all-water route to the Pacific Ocean. They buried a lead plate inscribed near Ft. Pierre; it was rediscovered by schoolchildren in 1913.
In 1762, France granted Spain all French territory west of the Mississippi River in the Treaty of Fontainebleau. The agreement, which was signed in secret, was motivated by a French desire to convince Spain to come to terms with Britain and accept defeat in the Seven Years' War. In an attempt to secure Spanish claims in the region against possible encroachment from other European powers, Spain adopted a policy for the upper Missouri which emphasized the development of closer trade relations with local tribes as well as greater exploration of the region, a primary focus of which would be a search for a water route to the Pacific Ocean. Although traders such as Jacques D'Eglise and Juan Munier had been active in the region for several years, these men had been operating independently, and a determined effort to reach the Pacific and solidify Spanish control of the region had never been undertaken. In 1793, a group commonly known as the Missouri Company was formed in St. Louis, with the twin goals of trading and exploring on the upper Missouri. The company sponsored several attempts to reach the Pacific Ocean, none of which made it further than the mouth of the Yellowstone. In 1794, Jean Truteau (also spelled Trudeau) built a cabin near the present-day location of Fort Randall, and in 1795 the Mackay-Evans Expedition traveled up the Missouri as far as present-day North Dakota, where they expelled several British traders who had been active in the area. In 1801, a post known as Fort aux Cedres was constructed by Registre Loisel of St. Louis, on Cedar Island on the Missouri about 35 miles (56 km) southeast of the present location of Pierre. This trading post was the major regional post until its destruction by fire in 1810.[30] In 1800, Spain gave Louisiana back to France in the Treaty of San Ildefonso.
In 1803, the United States purchased the Louisiana Territory from Napoleon for $11,000,000. The territory included most of the western half of the Mississippi watershed and covered nearly all of present-day South Dakota, except for a small portion in the northeast corner of the state. The region was still largely unexplored and unsettled, and President Thomas Jefferson organized a group commonly referred to as the Lewis and Clark Expedition to explore the newly acquired region over a period of more than two years. The expedition, also known as the Corps of Discovery, was tasked with following the route of the Missouri to its source, continuing on to the Pacific Ocean, establishing diplomatic relations with the various tribes in the area, and taking cartographic, geologic, and botanical surveys of the area. The expedition left St. Louis on May 14, 1804, with 45 men and 15 tons of supplies in three boats (one keelboat and two pirogues). The party progressed slowly against the Missouri's current, reaching what is today South Dakota on August 22. Near present-day Vermillion, the party hiked to the Spirit Mound after hearing local legends of the place being inhabited by "little spirits" (or "devils"). Shortly after this, a peaceful meeting took place with the Yankton Sioux, while an encounter with the Lakota Sioux further north was not as uneventful. The Lakota mistook the party as traders, at one point stealing a horse. Weapons were brandished on both sides after it appeared as though the Lakota were going to further delay or even halt the expedition, but they eventually stood down and allowed the party to continue up the river and out of their territory. In north central South Dakota, the expedition acted as mediators between the warring Arikara and Mandan. After leaving the state on October 14, the party wintered with the Mandan in North Dakota before successfully reaching the Pacific Ocean and returning by the same route, safely reaching St. Louis in 1806. On the return trip, the expedition spent only 15 days in South Dakota, traveling more swiftly with the Missouri's current.
Pittsburgh lawyer Henry Marie Brackenridge was South Dakota's first recorded tourist. In 1811 he was hosted by fur trader Manuel Lisa.
In 1817, an American fur trading post was set up at present-day Fort Pierre, beginning continuous American settlement of the area. During the 1830s, fur trading was the dominant economic activity for the few white people who lived in the area. More than one hundred fur-trading posts were in present-day South Dakota in the first half of the 19th century, and Fort Pierre was the center of activity.[citation needed] General William Henry Ashley, Andrew Henry, and Jedediah Smith of the Rocky Mountain Fur Company, and Manuel Lisa and Joshua Pilcher of the St. Louis Fur Company, trapped in that region. Pierre Chouteau Jr. brought the steamship Yellowstone to Fort Tecumseh on the Missouri River in 1831. In 1832 the fort was replaced by Fort Pierre Chouteau Jr.: today's town of Fort Pierre. Pierre bought the Western Department of John Jacob Astor's American Fur Company and renamed it Pratte, Chouteau and Company, and then Pierre Chouteau and Company. It operated in present-day South Dakota from 1834 to 1858. Most trappers and traders left the area after European demand for furs dwindled around 1840.
Main articles: Kansas–Nebraska Act, Nebraska Territory, Organic act § List of organic acts, and Dakota Territory
In 1855, the U.S. Army bought Fort Pierre but abandoned it the following year in favor of Fort Randall to the south. Settlement by Americans and Europeans was by this time increasing rapidly, and in 1858 the Yankton Sioux signed the 1858 "Treaty of Washington", ceding most of present-day eastern South Dakota to the United States.
Land speculators founded two of eastern South Dakota's largest present-day cities: Sioux Falls in 1856 and Yankton in 1859. The Big Sioux River falls was the spot of an 1856 settlement established by a Dubuque, Iowa, company; that town was quickly removed by native residents. But in the following year, May 1857, the town was resettled and named Sioux Falls. That June, St. Paul, Minnesota's Dakota Land Company came to an adjacent 320 acres (130 ha), calling it Sioux Falls City. In June 1857, Flandreau and Medary, South Dakota, were established by the Dakota Land Company. Along with Yankton in 1859, Bon Homme, Elk Point, and Vermillion were among the new communities along the Missouri River or border with Minnesota. Settlers therein numbered about 5,000 in 1860. In 1861, Dakota Territory was established by the United States government (this initially included North Dakota, South Dakota, and parts of Montana and Wyoming). Settlers from Scandinavia, Germany, Ireland, Czechoslovakia[citation needed] and Russia,[citation needed] as well as elsewhere in Europe and from the eastern U.S. states increased from a trickle to a flood, especially after the completion of an eastern railway link to the territorial capital of Yankton in 1872, and the discovery of gold in the Black Hills in 1874 during a military expedition led by George A. Custer.
The Dakota Territory had significant regional tensions between the northern part and the southern part from the beginning, the southern part always being more populated – in the 1880 United States census, the population of the southern part (98,268) was more than two and a half times of the northern part (36,909), and southern Dakotans saw the northern part as bit of disreputable, "controlled by the wild folks, cattle ranchers, fur traders” and too frequently the site of conflict with the indigenous population. Also, the new railroads built connected the northern and southern parts to different hubs – northern part was closer tied to Minneapolis–Saint Paul area; and southern part to Sioux City and from there to Omaha. The last straw was territorial governor Nehemiah G. Ordway moving the territorial capital from Yankton to Bismarck in modern-day North Dakota. As the Southern part had the necessary population for statehood (60,000), they held a separate convention in September 1883 and drafted a constitution. Various bills to divide the Dakota Territory in half ended up stalling, until in 1887, when the Territorial Legislature submitted the question of division to a popular vote at the November general elections, where it was approved by 37,784 votes over 32,913. A bill for statehood for North Dakota and South Dakota (as well as Montana and Washington) titled the Enabling Act of 1889 was passed on February 22, 1889, during the Administration of Grover Cleveland, dividing Dakota along the seventh standard parallel. It was left to his successor, Benjamin Harrison, to sign proclamations formally admitting North and South Dakota to the Union on November 2, 1889. Harrison directed his Secretary of State James G. Blaine to shuffle the papers and obscure from him which he was signing first and the actual order went unrecorded.
With statehood South Dakota was now in a position to make decisions on the major issues it confronted: prohibition, women's suffrage, the location of the state capital, the opening of the Sioux lands for settlement, and the cyclical issues of drought (severe in 1889) and low wheat prices (1893–1896). In early 1889 a prohibition bill passed the new state legislature, only to be vetoed by Governor Louis Church. Fierce opposition came from the wet German community, with financing from beer and liquor interests. The Yankee women organized to demand suffrage, as well as prohibition. Neither party supported their cause, and the wet element counter-organized to block women's suffrage. Popular interest reached a peak in the debates over locating the state capital. Prestige, real estate values and government jobs were at stake, as well as the question of access in such a large geographical region with limited railroads. Huron was the temporary site, centrally located Pierre was the best organized contender, and three other towns were in the running. Real estate speculators had money to toss around. Pierre, population 3200, made the most generous case to the voters—its promoters truly believed it would be the next Denver and be the railway hub of the Dakotas. The North Western railroad came through but not the others it expected. In 1938 Pierre counted 4000 people and three small hotels.
The national government continued to handle Indian affairs. The Army's 1874 Custer expedition took place despite the fact that the western half of present-day South Dakota had been granted to the Sioux by the Treaty of Fort Laramie as part of the Great Sioux Reservation. The Sioux declined to grant mining rights or land in the Black Hills, and the Great Sioux War of 1876 broke out after the U.S. failed to stop white miners and settlers from entering the region. The Sioux were eventually defeated and settled on reservations within South Dakota and North Dakota.
In 1889 Harrison sent general George Crook with a commission to persuade the Sioux to sell half their reservation land to the government. It was believed that the state would not be viable unless more land was made available to settlers. Crook used a number of dubious methods to secure agreement and obtain the land.
On December 29, 1890, the Wounded Knee Massacre occurred on the Pine Ridge Indian Reservation. It was the last major armed conflict between the United States and the Sioux Nation, the massacre resulted in the deaths of 300 Sioux, many of them women and children. In addition 25 U.S. soldiers were also killed in the episode.
Railroads played a central role in South Dakota transportation from the late 19th century until the 1930s, when they were surpassed by highways. The Milwaukee Road and the Chicago & North Western were the state's largest railroads, and the Milwaukee's east–west transcontinental line traversed the northern tier of the state. About 4,420 miles (7,110 km) of railroad track were built in South Dakota during the late nineteenth and early twentieth centuries, though only 1,839 miles (2,960 km) were active in 2007.
The railroads sold land to prospective farmers at very low rates, expecting to make a profit by shipping farm products out and home goods in. They also set up small towns that would serve as shipping points and commercial centers, and attract businessmen and more farmers. The Minneapolis and St. Louis Railway (M&StL) in 1905, under the leadership of vice president and general manager L. F. Day, added lines from Watertown to LeBeau and from Conde through Aberdeen to Leola. It developed town sites along the new lines and by 1910, the new lines served 35 small communities.
Not all of the new towns survived. The M&StL situated LeBeau along the Missouri River on the eastern edge of the Cheyenne River Indian Reservation. The new town was a hub for the cattle and grain industries. Livestock valued at one million dollars were shipped out in 1908, and the rail company planned a bridge across the Missouri River. Allotment of the Cheyenne River Reservation in 1909 promised further growth. By the early 1920s, however, troubles multiplied, with the murder of a local rancher, a fire that destroyed the business district, and drought that ruined ranchers and farmers alike. LeBeau became a ghost town.
Most of the traffic was freight, but the main lines also offered passenger service. After the European immigrants settled, there never were many people moving about inside the state. Profits were slim. Automobiles and busses were much more popular, but there was an increase during World War II when gasoline was scarce. All passenger service was ended in the state by 1969.
In the rural areas farmers and ranchers depended on local general stores that had a limited stock and slow turnover; they made enough profit to stay in operation by selling at high prices. Prices were not marked on each item; instead the customer negotiated a price. Men did most of the shopping, since the main criterion was credit rather than quality of goods. Indeed, most customers shopped on credit, paying off the bill when crops or cattle were later sold; the owner's ability to judge credit worthiness was vital to his success.
In the cities consumers had much more choice, and bought their dry goods and supplies at locally owned department stores. They had a much wider selection of goods than in the country general stores and price tags that gave the actual selling price. The department stores provided a very limited credit, and set up attractive displays and, after 1900, window displays as well. Their clerks—usually men before the 1940s—were experienced salesmen whose knowledge of the products appealed to the better educated middle-class housewives who did most of the shopping. The keys to success were a large variety of high-quality brand-name merchandise, high turnover, reasonable prices, and frequent special sales. The larger stores sent their buyers to Denver, Minneapolis, and Chicago once or twice a year to evaluate the newest trends in merchandising and stock up on the latest fashions. By the 1920s and 1930s, large mail-order houses such as Sears, Roebuck & Co. and Montgomery Ward provided serious competition, making the department stores rely even more on salesmanship and close integration with the community.
Many entrepreneurs built stores, shops, and offices along Main Street. The most handsome ones used pre-formed, sheet iron facades, especially those manufactured by the Mesker Brothers of St. Louis. These neoclassical, stylized facades added sophistication to brick or wood-frame buildings throughout the state.
During the 1930s, several economic and climatic conditions combined with disastrous results for South Dakota. A lack of rainfall, extremely high temperatures and over-cultivation of farmland produced what was known as the Dust Bowl in South Dakota and several other plains states. Fertile topsoil was blown away in massive dust storms, and several harvests were completely ruined. The experiences of the Dust Bowl, coupled with local bank foreclosures and the general economic effects of the Great Depression resulted in many South Dakotans leaving the state. The population of South Dakota declined by more than seven percent between 1930 and 1940.
Prosperity returned with the U.S. entry into World War II in 1941, when demand for the state's agricultural and industrial products grew as the nation mobilized for war. Over 68,000 South Dakotans served in the armed forces during the war, of which over 2,200 were killed.
In 1944, the Pick-Sloan Plan was passed as part of the Flood Control Act of 1944 by the U.S. Congress, resulting in the construction of six large dams on the Missouri River, four of which are at least partially located in South Dakota.[83] Flood control, hydroelectricity and recreational opportunities such as boating and fishing are provided by the dams and their reservoirs.
On the night of June 9–10, 1972, heavy rainfall in the eastern Black Hills caused the Canyon Lake Dam on Rapid Creek to fail. The failure of the dam, combined with heavy runoff from the storm, turned the usually small creek into a massive torrent that washed through central Rapid City. The flood resulted in 238 deaths and destroyed 1,335 homes and around 5,000 automobiles.[84] Damage from the flood totaled $160 million (the equivalent of $664 million today).
On April 19, 1993, Governor George S. Mickelson was killed in a plane crash in Iowa while returning from a business meeting in Cincinnati. Several other state officials were also killed in the crash. Mickelson, who was in the middle of his second term as governor, was succeeded by Walter Dale Miller.
In recent decades, South Dakota has transformed from a state dominated by agriculture to one with a more diversified economy. The tourism industry has grown considerably since the completion of the interstate system in the 1960s, with the Black Hills being especially impacted. The financial service industry began to grow in the state as well, with Citibank moving its credit card operations from New York to Sioux Falls in 1981, a move that has since been followed by several other financial companies. In 2007, the site of the recently closed Homestake gold mine near Lead was chosen as the location of a new underground research facility. Despite a growing state population and recent economic development, many rural areas have been struggling over the past 50 years with locally declining populations and the emigration of educated young adults to larger South Dakota cities, such as Rapid City or Sioux Falls, or to other states. The Cattleman's Blizzard of October 2013 killed tens of thousands of livestock in western South Dakota, and was one of the worst blizzards in the state's history.
"Trapper Boy, Turkey Knob Mine, Macdonald, W. Va. Boy had to stoop on account of low roof, photo taken more than a mile inside the mine. Witness E. N. Clopper. Location: MacDonald, West Virginia. October 1908."
Lewis Hine. Library of Congress, LC-USZ62-23737.
Trapper Lake is a 200 yard (180 meter) by 100 yard (91 meter) glacial lake located 4.6 miles (7.4 km) from the trail-head at String Lake at the base of Mt. Moran. I had been trying to get there for over four years, but forest fires, snow, and a knee malfunction had prevented me from getting there. I finally made it on an unplanned trek, way to late in the day. I did not have very long to scout the area because I arrived there just forty-five minutes before sunset and I had a long hike back.
So after all that wait I did not even get much of a shot, but at least I finally have one. I only hope I can get back there someday.
By the way, there is a great looking camp site at the northeast end or the lake, Luke.
Grand Teton National Park, Wyoming, USA
Looking west from Highway 93, Bitterroot National Forest, Ravalli County, Montana.
11:07 26 March 2016
Trapper Peak is the highest point (10,157 ft, 3,096 m) in the Bitterroot Mountains, part of the larger Bitterroot Range in western Montana.
- Wikipedia
An old cabin abandoned along the shore of Great Slave Lake.
Nikon D200
Nikon 12-24mm f/4G IF-ED AF-S DX Zoom-Nikkor
Set at 12mm
200 ASA
The Vos Trapper is a standby safety vessel working in the North Sea. She sails under the Liberian flag and is registered in Monrovia.
She is pictured here in Gt.Yarmouth, Norfolk.
Three Valley Gap Heritage Ghost Town,
Three Valley Gap, British Columbia, Canada,
For my video; youtu.be/SdS_StWOhVk
Craters of the Moon National Monument and Preserve is a U.S. national monument and national preserve in the Snake River Plain in central Idaho. It is along US 20 (concurrent with US 93 and US 26), between the small towns of Arco and Carey, at an average elevation of 5,900 feet (1,800 m) above sea level.
The Monument was established on May 2, 1924. In November 2000, a presidential proclamation by President Clinton greatly expanded the Monument area. The 410,000-acre National Park Service portions of the expanded Monument were designated as Craters of the Moon National Preserve in August 2002. It spreads across Blaine, Butte, Lincoln, Minidoka, and Power counties. The area is managed cooperatively by the National Park Service and the Bureau of Land Management (BLM).
The Monument and Preserve encompass three major lava fields and about 400 square miles (1,000 km2) of sagebrush steppe grasslands to cover a total area of 1,117 square miles (2,893 km2). The Monument alone covers 343,000 acres (139,000 ha). All three lava fields lie along the Great Rift of Idaho, with some of the best examples of open rift cracks in the world, including the deepest known on Earth at 800 feet (240 m). There are excellent examples of almost every variety of basaltic lava, as well as tree molds (cavities left by lava-incinerated trees), lava tubes (a type of cave), and many other volcanic features.
Craters of the Moon is in south-central Idaho, midway between Boise and Yellowstone National Park. The lava field reaches southeastward from the Pioneer Mountains. Combined U.S. Highway 20–26–93 cuts through the northwestern part of the monument and provides access to it. However, the rugged landscape of the monument itself remains remote and undeveloped, with only one paved road across the northern end.
The Craters of the Moon Lava Field spreads across 618 square miles (1,601 km2) and is the largest mostly Holocene-aged basaltic lava field in the contiguous United States. The Monument and Preserve contain more than 25 volcanic cones, including outstanding examples of spatter cones. The 60 distinct solidified lava flows that form the Craters of the Moon Lava Field range in age from 15,000 to just 2,000 years. The Kings Bowl and Wapi lava fields, both about 2,200 years old, are part of the National Preserve.
This lava field is the largest of several large beds of lava that erupted from the 53-mile (85 km) south-east to north-west trending Great Rift volcanic zone, a line of weakness in the Earth's crust. Together with fields from other fissures they make up the Lava Beds of Idaho, which in turn are in the much larger Snake River Plain volcanic province. The Great Rift extends across almost the entire Snake River Plain.
Elevation at the visitor center is 5,900 feet (1,800 m) above sea level.
Total average precipitation in the Craters of the Moon area is between 15–20 inches (380–510 mm) per year. Most of this is lost in cracks in the basalt, only to emerge later in springs and seeps in the walls of the Snake River Canyon. Older lava fields on the plain have been invaded by drought-resistant plants such as sagebrush, while younger fields, such as Craters of the Moon, only have a seasonal and very sparse cover of vegetation. From a distance this cover disappears almost entirely, giving an impression of utter black desolation. Repeated lava flows over the last 15,000 years have raised the land surface enough to expose it to the prevailing southwesterly winds, which help to keep the area dry. Together these conditions make life on the lava field difficult.
Paleo-Indians visited the area about 12,000 years ago but did not leave much archaeological evidence. Northern Shoshone created trails through the Craters of the Moon Lava Field during their summer migrations from the Snake River to the camas prairie, west of the lava field. Stone windbreaks at Indian Tunnel were used to protect campsites from the dry summer wind. No evidence exists for permanent habitation by any Native American group. A hunting and gathering culture, the Northern Shoshone pursued elk, bears, American bison, cougars, and bighorn sheep — all large game who no longer range the area. The most recent volcanic eruptions ended about 2,100 years ago and were likely witnessed by the Shoshone people. Ella E. Clark has recorded a Shoshone legend which speaks of a serpent on a mountain who, angered by lightning, coiled around and squeezed the mountain until liquid rock flowed, fire shot from cracks, and the mountain exploded.
In 1879, two Arco cattlemen named Arthur Ferris and J.W. Powell became the first known European-Americans to explore the lava fields. They were investigating its possible use for grazing and watering cattle but found the area to be unsuitable and left.
U.S. Army Captain and western explorer B.L.E. Bonneville visited the lava fields and other places in the West in the 19th century and wrote about his experiences in his diaries. Washington Irving later used Bonneville's diaries to write the Adventures of Captain Bonneville, saying this unnamed lava field is a place "where nothing meets the eye but a desolate and awful waste, where no grass grows nor water runs, and where nothing is to be seen but lava."
In 1901 and 1903, Israel Russell became the first geologist to study this area while surveying it for the United States Geological Survey (USGS). In 1910, Samuel Paisley continued Russell's work and later became the monument's first custodian. Others followed and in time much of the mystery surrounding this and the other Lava Beds of Idaho was lifted.
The few European settlers who visited the area in the 19th century created local legends that it looked like the surface of the Moon. Geologist Harold T. Stearns coined the name "Craters of the Moon" in 1923 while trying to convince the National Park Service to recommend protection of the area in a national monument.
The Snake River Plain is a volcanic province that was created by a series of cataclysmic caldera-forming eruptions which started about 15 million years ago. A migrating hotspot thought to now exist under Yellowstone Caldera in Yellowstone National Park has been implicated. This hot spot was under the Craters of the Moon area some 10 to 11 million years ago but 'moved' as the North American Plate migrated northwestward. Pressure from the hot spot heaves the land surface up, creating fault-block mountains. After the hot spot passes the pressure is released and the land subsides.
Leftover heat from this hot spot was later liberated by Basin and Range-associated rifting and created the many overlapping lava flows that make up the Lava Beds of Idaho. The largest rift zone is the Great Rift; it is from this 'Great Rift fissure system' that Craters of the Moon, Kings Bowl, and Wapi lava fields were created. The Great Rift is a National Natural Landmark.
In spite of their fresh appearance, the oldest flows in the Craters of the Moon Lava Field are 15,000 years old and the youngest erupted about 2000 years ago, according to Mel Kuntz and other USGS geologists. Nevertheless, the volcanic fissures at Craters of the Moon are considered to be dormant, not extinct, and are expected to erupt again in less than a thousand years. There are eight major eruptive periods recognized in the Craters of the Moon Lava Field. Each period lasted about 1000 years or less and were separated by relatively quiet periods that lasted between 500 and as long as 3000 years. Individual lava flows were up to 30 miles (50 km) long with the Blue Dragon Flow being the longest.
Kings Bowl Lava Field erupted during a single fissure eruption on the southern part of the Great Rift about 2,250 years ago. This eruption probably lasted only a few hours to a few days. The field preserves explosion pits, lava lakes, squeeze-ups, basalt mounds, and an ash blanket. The Wapi Lava Field probably formed from a fissure eruption at the same time as the Kings Bowl eruption. More prolonged activity over a period of months to a few years led to the formation of low shield volcanoes in the Wapi field. The Bear Trap lava tube, between the Craters of the Moon and the Wapi lava fields, is a cave system more than 15 miles (24 km) long. The lava tube is remarkable for its length and for the number of well-preserved lava cave features, such as lava stalactites and curbs, the latter marking high stands of the flowing lava frozen on the lava tube walls. The lava tubes and pit craters of the monument are known for their unusual preservation of winter ice and snow into the hot summer months, due to shielding from the sun and the insulating properties of basalt.
A typical eruption along the Great Rift and similar basaltic rift systems starts with a curtain of very fluid lava shooting up to 1,000 feet (300 m) high along a segment of the rift up to 1 mile (1.6 km) long. As the eruption continues, pressure and heat decrease and the chemistry of the lava becomes slightly more silica rich. The curtain of lava responds by breaking apart into separate vents. Various types of volcanoes may form at these vents: gas-rich pulverized lava creates cinder cones (such as Inferno Cone – stop 4), and pasty lava blobs form spatter cones (such as Spatter Cones – stop 5). Later stages of an eruption push lava streams out through the side or base of cinder cones, which usually ends the life of the cinder cone (North Crater, Watchmen, and Sheep Trail Butte are notable exceptions). This will sometimes breach part of the cone and carry it away as large and craggy blocks of cinder (as seen at North Crater Flow – stop 2 – and Devils Orchard – stop 3). Solid crust forms over lava streams, and lava tubes (a type of cave) are created when lava vacates its course (examples can be seen at the Cave Area – stop 7).
Geologists feared that a large earthquake that shook Borah Peak, Idaho's tallest mountain, in 1983 would restart volcanic activity at Craters of the Moon, though this proved not to be the case. Geologists predict that the area will experience its next eruption some time in the next 900 years with the most likely period in the next 100 years.
All plants and animals that live in and around Craters of the Moon are under great environmental stress due to constant dry winds and heat-absorbing black lavas that tend to quickly sap water from living things. Summer soil temperatures often exceed 150 °F (66 °C) and plant cover is generally less than 5% on cinder cones and about 15% over the entire monument. Adaptation is therefore necessary for survival in this semi-arid harsh climate.
Water is usually only found deep inside holes at the bottom of blow-out craters. Animals therefore get the moisture they need directly from their food. The black soil on and around cinder cones does not hold moisture for long, making it difficult for plants to establish themselves. Soil particles first develop from direct rock decomposition by lichens and typically collect in crevices in lava flows. Successively more complex plants then colonize the microhabitat created by the increasingly productive soil.
The shaded north slopes of cinder cones provide more protection from direct sunlight and prevailing southwesterly winds and have a more persistent snow cover (an important water source in early spring). These parts of cinder cones are therefore colonized by plants first.
Gaps between lava flows were sometimes cut off from surrounding vegetation. These literal islands of habitat are called kīpukas, a Hawaiian name used for older land surrounded by younger lava. Carey Kīpuka is one such area in the southernmost part of the monument and is used as a benchmark to measure how plant cover has changed in less pristine parts of southern Idaho.
Idaho is a landlocked state in the Mountain West subregion of the United States. It shares a small portion of the Canada–United States border to the north, with the province of British Columbia. It borders Montana and Wyoming to the east, Nevada and Utah to the south, and Washington and Oregon to the west. The state's capital and largest city is Boise. With an area of 83,570 square miles (216,400 km2), Idaho is the 14th largest state by land area. With a population of approximately 1.8 million, it ranks as the 13th least populous and the 6th least densely populated of the 50 U.S. states.
For thousands of years, and prior to European colonization, Idaho has been inhabited by native peoples. In the early 19th century, Idaho was considered part of the Oregon Country, an area of dispute between the U.S. and the British Empire. It officially became a U.S. territory with the signing of the Oregon Treaty of 1846, but a separate Idaho Territory was not organized until 1863, instead being included for periods in Oregon Territory and Washington Territory. Idaho was eventually admitted to the Union on July 3, 1890, becoming the 43rd state.
Forming part of the Pacific Northwest (and the associated Cascadia bioregion), Idaho is divided into several distinct geographic and climatic regions. The state's north, the relatively isolated Idaho Panhandle, is closely linked with Eastern Washington, with which it shares the Pacific Time Zone—the rest of the state uses the Mountain Time Zone. The state's south includes the Snake River Plain (which has most of the population and agricultural land), and the southeast incorporates part of the Great Basin. Idaho is quite mountainous and contains several stretches of the Rocky Mountains. The United States Forest Service holds about 38% of Idaho's land, the highest proportion of any state.
Industries significant for the state economy include manufacturing, agriculture, mining, forestry, and tourism. Several science and technology firms are either headquartered in Idaho or have factories there, and the state also contains the Idaho National Laboratory, which is the country's largest Department of Energy facility. Idaho's agricultural sector supplies many products, but the state is best known for its potato crop, which comprises around one-third of the nationwide yield. The official state nickname is the "Gem State."
The history of Idaho is an examination of the human history and social activity within the state of Idaho, one of the United States of America located in the Pacific Northwest area near the west coast of the United States and Canada. Other associated areas include southern Alaska, all of British Columbia, Washington, Oregon, western Montana and northern California and Nevada.
Humans may have been present in Idaho for 16,600 years. Recent findings in Cooper's Ferry along the Salmon River in western Idaho near the town of Cottonwood have unearthed stone tools and animal bone fragments in what may be the oldest evidence of humans in North America. Earlier excavations in 1959 at Wilson Butte Cave near Twin Falls revealed evidence of human activity, including arrowheads, that rank among the oldest dated artifacts in North America. Native American tribes predominant in the area in historic times included the Nez Perce and the Coeur d'Alene in the north; and the Northern and Western Shoshone and Bannock peoples in the south.
Idaho was one of the last areas in the lower 48 states of the US to be explored by people of European descent. The Lewis and Clark expedition entered present-day Idaho on August 12, 1805, at Lemhi Pass. It is believed that the first "European descent" expedition to enter southern Idaho was by a group led in 1811 and 1812 by Wilson Price Hunt, which navigated the Snake River while attempting to blaze an all-water trail westward from St. Louis, Missouri, to Astoria, Oregon. At that time, approximately 8,000 Native Americans lived in the region.
Fur trading led to the first significant incursion of Europeans in the region. Andrew Henry of the Missouri Fur Company first entered the Snake River plateau in 1810. He built Fort Henry on Henry's Fork on the upper Snake River, near modern St. Anthony, Idaho. However, this first American fur post west of the Rocky Mountains was abandoned the following spring.
The British-owned Hudson's Bay Company next entered Idaho and controlled the trade in the Snake River area by the 1820s. The North West Company's interior department of the Columbia was created in June 1816, and Donald Mackenzie was assigned as its head. Mackenzie had previously been employed by Hudson's Bay and had been a partner in the Pacific Fur Company, financed principally by John Jacob Astor. During these early years, he traveled west with a Pacific Fur Company's party and was involved in the initial exploration of the Salmon River and Clearwater River. The company proceeded down the lower Snake River and Columbia River by canoe, and were the first of the Overland Astorians to reach Fort Astoria, on January 18, 1812.
Under Mackenzie, the North West Company was a dominant force in the fur trade in the Snake River country. Out of Fort George in Astoria, Mackenzie led fur brigades up the Snake River in 1816-1817 and up the lower Snake in 1817-1818. Fort Nez Perce, established in July, 1818, became the staging point for Mackenzies' Snake brigades. The expedition of 1818-1819 explored the Blue Mountains, and traveled down the Snake River to the Bear River and approached the headwaters of the Snake. Mackenzie sought to establish a navigable route up the Snake River from Fort Nez Perce to the Boise area in 1819. While he did succeed in traveling by boat from the Columbia River through the Grand Canyon of the Snake past Hells Canyon, he concluded that water transport was generally impractical. Mackenzie held the first rendezvous in the region on the Boise River in 1819.
Despite their best efforts, early American fur companies in this region had difficulty maintaining the long-distance supply lines from the Missouri River system into the Intermountain West. However, Americans William H. Ashley and Jedediah Smith expanded the Saint Louis fur trade into Idaho in 1824. The 1832 trapper's rendezvous at Pierre's Hole, held at the foot of the Three Tetons in modern Teton County, was followed by an intense battle between the Gros Ventre and a large party of American trappers aided by their Nez Perce and Flathead allies.
The prospect of missionary work among the Native Americans also attracted early settlers to the region. In 1809, Kullyspell House, the first white-owned establishment and first trading post in Idaho, was constructed. In 1836, the Reverend Henry H. Spalding established a Protestant mission near Lapwai, where he printed the Northwest's first book, established Idaho's first school, developed its first irrigation system, and grew the state's first potatoes. Narcissa Whitman and Eliza Hart Spalding were the first non-native women to enter present-day Idaho.
Cataldo Mission, the oldest standing building in Idaho, was constructed at Cataldo by the Coeur d'Alene and Catholic missionaries. In 1842, Father Pierre-Jean De Smet, with Fr. Nicholas Point and Br. Charles Duet, selected a mission location along the St. Joe River. The mission was moved a short distance away in 1846, as the original location was subject to flooding. In 1850, Antonio Ravalli designed a new mission building and Indians affiliated with the church effort built the mission, without nails, using the wattle and daub method. In time, the Cataldo mission became an important stop for traders, settlers, and miners. It served as a place for rest from the trail, offered needed supplies, and was a working port for boats heading up the Coeur d'Alene River.
During this time, the region which became Idaho was part of an unorganized territory known as Oregon Country, claimed by both the United States and Great Britain. The United States gained undisputed jurisdiction over the region in the Oregon Treaty of 1846, although the area was under the de facto jurisdiction of the Provisional Government of Oregon from 1843 to 1849. The original boundaries of Oregon Territory in 1848 included all three of the present-day Pacific Northwest states and extended eastward to the Continental Divide. In 1853, areas north of the 46th Parallel became Washington Territory, splitting what is now Idaho in two. The future state was reunited in 1859 after Oregon became a state and the boundaries of Washington Territory were redrawn.
While thousands passed through Idaho on the Oregon Trail or during the California gold rush of 1849, few people settled there. In 1860, the first of several gold rushes in Idaho began at Pierce in present-day Clearwater County. By 1862, settlements in both the north and south had formed around the mining boom.
The Church of Jesus Christ of Latter-Day Saints missionaries founded Fort Lemhi in 1855, but the settlement did not last. The first organized town in Idaho was Franklin, settled in April 1860 by Mormon pioneers who believed they were in Utah Territory; although a later survey determined they had crossed the border. Mormon pioneers reached areas near the current-day Grand Teton National Park in Wyoming and established most of the historic and modern communities in Southeastern Idaho. These settlements include Ammon, Blackfoot, Chubbuck, Firth, Idaho Falls, Iona, Pocatello, Rexburg, Rigby, Shelley, and Ucon.
Large numbers of English immigrants settled in what is now the state of Idaho in the late 19th and early 20th century, many before statehood. The English found they had more property rights and paid less taxes than they did back in England. They were considered some of the most desirable immigrants at the time. Many came from humble beginnings and would rise to prominence in Idaho. Frank R. Gooding was raised in a rural working-class background in England, but was eventually elected as the seventh governor of the state. Today people of English descent make up one fifth of the entire state of Idaho and form a plurality in the southern portion of the state.
Many German farmers also settled in what is now Idaho. German settlers were primarily Lutheran across all of the midwest and west, including Idaho, however there were small numbers of Catholics amongst them as well. In parts of Northern Idaho, German remained the dominant language until World War I, when German-Americans were pressured to convert entirely to English. Today, Idahoans of German ancestry make up nearly one fifth of all Idahoans and make up the second largest ethnic group after Idahoans of English descent with people of German ancestry being 18.1% of the state and people of English ancestry being 20.1% of the state.
Irish Catholics worked in railroad centers such as Boise. Today, 10% of Idahoans self-identify as having Irish ancestry.
York, a slave owned by William Clark but considered a full member of Corps of Discovery during expedition to the Pacific, was the first recorded African American in Idaho. There is a significant African American population made up of those who came west after the abolition of slavery. Many settled near Pocatello and were ranchers, entertainers, and farmers. Although free, many blacks suffered discrimination in the early-to-mid-late 20th century. The black population of the state continues to grow as many come to the state because of educational opportunities, to serve in the military, and for other employment opportunities. There is a Black History Museum in Boise, Idaho, with an exhibit known as the "Invisible Idahoan", which chronicles the first African-Americans in the state. Blacks are the fourth largest ethnic group in Idaho according to the 2000 census. Mountain Home, Boise, and Garden City have significant African-American populations.
The Basque people from the Iberian peninsula in Spain and southern France were traditionally shepherds in Europe. They came to Idaho, offering hard work and perseverance in exchange for opportunity. One of the largest Basque communities in the US is in Boise, with a Basque museum and festival held annually in the city.
Chinese in the mid-19th century came to America through San Francisco to work on the railroad and open businesses. By 1870, there were over 4000 Chinese and they comprised almost 30% of the population. They suffered discrimination due to the Anti-Chinese League in the 19th century which sought to limit the rights and opportunities of Chinese emigrants. Today Asians are third in population demographically after Whites and Hispanics at less than 2%.
Main articles: Oregon boundary dispute, Provisional Government of Oregon, Oregon Treaty, Oregon Territory, Washington Territory, Dakota Territory, Organic act § List of organic acts, and Idaho Territory
On March 4, 1863, President Abraham Lincoln signed an act creating Idaho Territory from portions of Washington Territory and Dakota Territory with its capital at Lewiston. The original Idaho Territory included most of the areas that later became the states of Idaho, Montana and Wyoming, and had a population of under 17,000. Idaho Territory assumed the boundaries of the modern state in 1868 and was admitted as a state in 1890.
After Idaho became a territory, legislation was held in Lewiston, the capital of Idaho Territory at the time. There were many territories acts put into place, and then taken away during these early sessions, one act being the move of the capital city from Lewiston to Boise City. Boise was becoming a growing area after gold was found, so on December 24, 1864, Boise City was made the final destination of the capital for the Territory of Idaho.
However, moving the capital to Boise City created a lot of issues between the territory. This was especially true between the north and south areas in the territory, due to how far south Boise City was. Problems with communicating between the north and south contributed to some land in Idaho Territory being transferred to other territories and areas at the time. Idaho’s early boundary changes helped create the current boundaries of Washington, Wyoming, and Montana States as currently exist.
In a bid for statehood, Governor Edward A. Stevenson called for a constitutional convention in 1889. The convention approved a constitution on August 6, 1889, and voters approved the constitution on November 5, 1889.
When President Benjamin Harrison signed the law admitting Idaho as a U.S. state on July 3, 1890, the population was 88,548. George L. Shoup became the state's first governor, but resigned after only a few weeks in office to take a seat in the United States Senate. Willis Sweet, a Republican, was the first congressman, 1890 to 1895, representing the state at-large. He vigorously demanded "Free Silver" or the unrestricted coinage of silver into legal tender, in order to pour money into the large silver mining industry in the Mountain West, but he was defeated by supporters of the gold standard. In 1896 he, like many Republicans from silver mining districts, supported the Silver Republican Party instead of the regular Republican nominee William McKinley.
During its first years of statehood, Idaho was plagued by labor unrest in the mining district of Coeur d'Alene. In 1892, miners called a strike which developed into a shooting war between union miners and company guards. Each side accused the other of starting the fight. The first shots were exchanged at the Frisco mine in Frisco, in the Burke-Canyon north and east of Wallace. The Frisco mine was blown up, and company guards were taken prisoner. The violence soon spilled over into the nearby community of Gem, where union miners attempted to locate a Pinkerton spy who had infiltrated their union and was passing information to the mine operators. But agent Charlie Siringo escaped by cutting a hole in the floor of his room. Strikers forced the Gem mine to close, then traveled west to the Bunker Hill mining complex near Wardner, and closed down that facility as well. Several had been killed in the Burke-Canyon fighting. The Idaho National Guard and federal troops were dispatched to the area, and union miners and sympathizers were thrown into bullpens.
Hostilities would again erupt at the Bunker Hill facility in 1899, when seventeen union miners were fired for having joined the union. Other union miners were likewise ordered to draw their pay and leave. Angry members of the union converged on the area and blew up the Bunker Hill Mill, killing two company men.
In both disputes, the union's complaints included pay, hours of work, the right of miners to belong to the union, and the mine owners' use of informants and undercover agents. The violence committed by union miners was answered with a brutal response in 1892 and in 1899.
Through the Western Federation of Miners (WFM) union, the battles in the mining district became closely tied to a major miners' strike in Colorado. The struggle culminated in the December 1905 assassination of former Governor Frank Steunenberg by Harry Orchard (also known as Albert Horsley), a member of the WFM. Orchard was allegedly incensed by Steunenberg's efforts as governor to put down the 1899 miner uprising after being elected on a pro-labor platform.
Pinkerton detective James McParland conducted the investigation into the assassination. In 1907, WFM Secretary Treasurer "Big Bill" Haywood and two other WFM leaders were tried on a charge of conspiracy to murder Steunenberg, with Orchard testifying against them as part of a deal made with McParland. The nationally publicized trial featured Senator William E. Borah as prosecuting attorney and Clarence Darrow representing the defendants. The defense team presented evidence that Orchard had been a Pinkerton agent and had acted as a paid informant for the Cripple Creek Mine Owners' Association. Darrow argued that Orchard's real motive in the assassination had been revenge for a declaration of martial law by Steunenberg, which prompted Orchard to gamble away a share in the Hercules silver mine that would otherwise have made him wealthy.
Two of the WFM leaders were acquitted in two separate trials, and the third was released. Orchard was convicted and sentenced to death. His sentence was commuted, and he spent the rest of his life in an Idaho prison.
Mining in Idaho was a major commercial venture, bringing a great deal of attention to the state. From 1860-1866 Idaho produced 19% of all gold in the United States, or 2.5 million ounces.
Most of Idaho's mining production, 1860–1969, has come from metals equating to $2.88 billion out of $3.42 billion, according to the best estimates. Of the metallic mining areas of Idaho, the Coeur d'Alene region has produced the most by far, and accounts for about 80% of the total Idaho yield.
Several others—Boise Basin, Wood River Valley, Stibnite, Blackbirg, and Owyhee—range considerably above the other big producers. Atlanta, Bear Valley, Bay Horse, Florence, Gilmore, Mackay, Patterson, and Yankee Fork all ran on the order of ten to twenty million dollars, and Elk City, Leesburg, Pierce, Rocky Bar, and Warren's make up the rest of the major Idaho mining areas that stand out in the sixty or so regions of production worthy of mention.
A number of small operations do not appear in this list of Idaho metallic mining areas: a small amount of gold was recovered from Goose Creek on Salmon Meadows; a mine near Cleveland was prospected in 1922 and produced a little manganese in 1926; a few tons of copper came from Fort Hall, and a few more tons of copper came from a mine near Montpelier. Similarly, a few tons of lead came from a property near Bear Lake, and lead-silver is known on Cassia Creek near Elba. Some gold quartz and lead-silver workings are on Ruby Creek west of Elk River, and there is a slightly developed copper operation on Deer Creek near Winchester. Molybdenum is known on Roaring River and on the east fork of the Salmon. Some scattered mining enterprises have been undertaken around Soldier Mountain and on Chief Eagle Eye Creek north of Montour.
Idaho proved to be one of the more receptive states to the progressive agenda of the late 19th century and early 20th century. The state embraced progressive policies such as women's suffrage (1896) and prohibition (1916) before they became federal law. Idahoans were also strongly supportive of Free Silver. The pro-bimetallism Populist and Silver Republican parties of the late 1890s were particularly successful in the state.
Eugenics was also a major part of the Progressive movement. In 1919, the Idaho legislature passed an Act legalizing the forced sterilization of some persons institutionalized in the state. The act was vetoed by governor D.W. Davis, who doubted its scientific merits and believed it likely violated the Equal Protection clause of the US Constitution. In 1925, the Idaho legislature passed a revised eugenics act, now tailored to avoid Davis's earlier objections. The new law created a state board of eugenics, charged with: the sterilization of all feebleminded, insane, epileptics, habitual criminals, moral degenerates and sexual perverts who are a menace to society, and providing the means for ascertaining who are such persons.
The Eugenics board was eventually folded into the state's health commission; between 1932 and 1964, a total of 30 women and eight men in Idaho were sterilized under this law. The sterilization law was formally repealed in 1972.
After statehood, Idaho's economy began a gradual shift away from mining toward agriculture, particularly in the south. Older mining communities such as Silver City and Rocky Bar gave way to agricultural communities incorporated after statehood, such as Nampa and Twin Falls. Milner Dam on the Snake River, completed in 1905, allowed for the formation of many agricultural communities in the Magic Valley region which had previously been nearly unpopulated.
Meanwhile, some of the mining towns were able to reinvent themselves as resort communities, most notably in Blaine County, where the Sun Valley ski resort opened in 1936. Others, such as Silver City and Rocky Bar, became ghost towns.
In the north, mining continued to be an important industry for several more decades. The closure of the Bunker Hill Mine complex in Shoshone County in the early 1980s sent the region's economy into a tailspin. Since that time, a substantial increase in tourism in north Idaho has helped the region to recover. Coeur d'Alene, a lake-side resort town, is a destination for visitors in the area.
Beginning in the 1980s, there was a rise in North Idaho of a few right-wing extremist and "survivalist" political groups, most notably one holding Neo-Nazi views, the Aryan Nations. These groups were most heavily concentrated in the Panhandle region of the state, particularly in the vicinity of Coeur d'Alene.
In 1992 a stand-off occurred between U.S. Marshals, the F.B.I., and white separatist Randy Weaver and his family at their compound at Ruby Ridge, located near the small, northern Idaho town of Naples. The ensuing fire-fight and deaths of a U.S. Marshal, and Weaver's son and wife gained national attention, and raised a considerable amount of controversy regarding the nature of acceptable force by the federal government in such situations.
In 2001, the Aryan Nations compound, which had been located in Hayden Lake, Idaho, was confiscated as a result of a court case, and the organization moved out of state. About the same time Boise installed an impressive stone Human Rights Memorial featuring a bronze statue of Anne Frank and quotations from her and many other writers extolling human freedom and equality.
The demographics of the state have changed. Due to this growth in different groups, especially in Boise, the economic expansion surged wrong-economic growth followed the high standard of living and resulted in the "growth of different groups". The population of Idaho in the 21st Century has been described as sharply divided along geographic and cultural lines due to the center of the state being dominated by sparsely-populated national forests, mountain ranges and recreation sites: "unless you're willing to navigate a treacherous mountain pass, you can't even drive from the north to the south without leaving the state." The northern population gravitates towards Spokane, Washington, the heavily Mormon south-east population towards Utah, with an isolated Boise "[being] the closest thing to a city-state that you'll find in America."
On March 13, 2020, officials from the Idaho Department of Health and Welfare announced the first confirmed case of the novel coronavirus COVID-19 within the state of Idaho. A woman over the age of 50 from the southwestern part of the state was confirmed to have the coronavirus infection. She contracted the infection while attending a conference in New York City. Conference coordinators notified attendees that three individuals previously tested positive for the coronavirus. The Idahoan did not require hospitalization and was recovering from mild symptoms from her home. At the time of the announcement, there were 1,629 total cases and 41 deaths in the United States. Five days beforehand, on March 8, a man of age 54 had died of an unknown respiratory illness which his doctor had believed to be pneumonia. The disease was later suspected to be – but never confirmed as – COVID-19.
On March 14, state officials announced the second confirmed case within the state. The South Central Public Health District, announced that a woman over the age of 50 that resides in Blaine County had contracted the infection.[44] Like the first case, she did not require hospitalization and she was recovering from mild symptoms from home. Later on in the day, three additional confirmed cases of COVID-19 were reported in the state by three of the seven health districts in the state, which brought the confirmed total cases of coronavirus to five in Idaho. Officials from Central District Health announced their second confirmed case, which was a male from Ada County in his 50s. He was not hospitalized and was recovering at home. South Central Public Health reported their second confirmed case in a female that is over the age of 70 who was hospitalized. Eastern Idaho Public Health reported a confirmed positive case in a woman under the age of 60 in Teton County. She had contracted the coronavirus from contact with a confirmed case in a neighboring state; she was not hospitalized. The South Central Public Health District announced that a woman over the age of 50 that resides in Blaine County had contracted the infection. Like the first case, she did not require hospitalization and she was recovering from mild symptoms from home.
On March 17, two more confirmed cases of the infection were reported, bringing the total to seven. The first case on this date was by officials from Central District Health reported that a female under the age of 50 in Ada County was recovering at home and was not hospitalized. The second confirmed case was a female over the age of 50 as reported by South Central Public Health officials.
On March 18, two additional confirmed cases were announced by South Central Public Health District officials. One is a male from Blaine County in his 40s and the other a male in his 80s from Twin Falls County. These cases were the first known community spread transmission of the coronavirus in South Central Idaho.
January 15, 2025 / Time: 8:48 a.m.
24° F / Real Feel: 10° F
Still walking to work & Loving it!
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Part of the album: Walk/Commute to/fro Work
(click to view the entire album)
Dainty little diecast of the motorists sworn enemy ;-p
The Matchbox Speed Trapper is a rather unusual choice of machine to model but for children is probably a source of fun and novelty. Rather low tech with its swivelling plastic speed recorder but is nicely detailed at the rear and rides on chrome disc wheels. Part of the very latest Case D. Mint and boxed.