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These satsumas were going to be my Tradition subjects for Macro Mondays, but I didn't get around to that in the end.
An in-camera double exposure still life, with one sharp and one blurred, blended with the Average setting.
Here is a shot from a year ago on my first visit to Devon Tower. This is just such a cool place that I always wanted to visit so I figured it was time to get a few of these up on Flickr too.
Anyway, while waiting for the P&W freight that was the reason for this trip I also saw a parade of Amtrak and commuter train. I know you may find this hard to believe but until this day I'd never shot a moving Metro North train! Despite being the busiest railroad in New England and the third busiest commuter railroad in the nation I'd never photographed them out on the line.
I suppose the fact that almost all their trains are electric multiple units just didn't excite me, but now I kind of regret never shooting the old Budd M2s and now have to settle for the new Kawaski M8s of which over 400 are in service.
The New Haven line ranks as the single busiest commuter line in the nation with an average of 125,000 daily weekday riders on the 74 mile mainline and its three branches. To put it in perspective the entire nearly 400 mile MBTA commuter system where I work hauls about that same number daily on the entire network!
In addition to Amtrak three MTA trains passed while hanging out here at Naugatuck Junction next to old New Haven Devon Tower (SS71). First up was an eastbound for New Haven in the shadows, then train 1916 a branch shuttle headed to Waterbury behind a Brookville BL20GH seen here, and then a Westbound for Grand Central in brilliant sunshine.
Milford, Connecticut
Friday November 8, 2019
Average red-bellied trogon of subtropical forests. Male is iridescent green on breast, head, and back; female is brown. Namesake dark mask is usually obvious, especially on females. Nearly identical to Collared Trogon but very little overlap; Masked is almost always found at higher elevations. Where both are possible, look especially at tail pattern on males: large white tips on underside of tail feathers, otherwise dark with very fine white barring.
This one was photographed in Ecuador guided by Neotropic Photo Tours. ISO 16,000.
4 April 2021: During the week from 25 to 31 March an average of 4,577 people tested positive for SARCoV-2. The figure is down 1% on the week. Less encouraging is that for the first time in four months the number of people being treated in a Belgian hospital for Covid has exceeded 3,000 and the number of patients in critical care has risen above 800. Thus far, only 1,404,877 people received their first shot of the corona vaccine. 546,555 people have had their second jab. From 6 April a central list for reserve candidates will be introduced. People who subscribed to the list will be contacted if any doses of the vaccine need to be used up urgently e.g. because of no-shows. The list has been introduced to avoid wasting valuable vaccines. Despite that the corona statistics are doing far from good and we’re muddling through vaccination, the 105th edition of the Tour of Flanders will take place today after being shifted to the end of the season in 2020 due to the corona crisis. It will feature the same iconic hills and the same legendary stretches of cobblestones. But since fans will be banned to watch Belgium’s iconic bicycle race from the roadside, I’m wondering if it will it feature the same passion? We went for a hike in the Flemish Ardennes yesterday to take a sneak preview of the trail and, believe it or not, we spotted the first cycling fanatic: a zebra… Happy Easter!
Two shots this evening but no need to comment on the second one, because it is just for talking purposes. The second shot is of Big Boy and he got that name by being THE largest gator on the bayou. Gary and I don’t like to exaggerate and so we set his length at 13 feet. Not a very good shot because of the backlighting and I don’t handle situations like that very well. I wasn’t willing to get out of the canoe and walk around the other side of so this scene will just have to do.
The second one is just your ol’ basic 9 or 10 foot gator that inhabits the bayou. He’s an average size and it is a male because the females don’t get this large. He was sunning himself on a gorgeous spring day on the bayou. Photos were all taken on Horsepen Bayou.
DSL_7873uls
Grábrók è un piccolo vulcano a nord del villaggio di Bifröst e del lago Hreðavatn(area di Borgarfjörður).
Il vulcano ha circa 3400 anni e ha formatouna montagna alta circa 170 metri.
Grábrók è uno dei tre crateri della zona, uno si chiama Grábrókarfell (il più grande) e un altro si chiama Litla Grábrók (Il più piccolo).
La lava che fuori uscita dai vulcani è di circa 7 km quadrati e il suo spessore medio è di circa 20 metri.
Grábrók is a small volcano north of the village of Bifröst and Lake Hreðavatn (Borgarfjörður area).
The volcano is about 3400 years old and has formed a mountain about 170 meters high.
Grábrók is one of the three craters in the area, one is called Grábrókarfell (the largest) and another is called Litla Grábrók (the smallest).
The lava that comes out of the volcanoes is about 7 square km and its average thickness is about 20 meters.
IMG_4011m
Fort Lauderdale is a city in the U.S. state of Florida, 25 miles (40 km) north of Miami. It is the county seat of Broward County. As of the 2019 census, the city has an estimated population of 182,437. Fort Lauderdale is a principal city of the Miami metropolitan area, which was home to an estimated 6,198,782 people in 2018.
The city is a popular tourist destination, with an average year-round temperature of 75.5 °F (24.2 °C) and 3,000 hours of sunshine per year. Greater Fort Lauderdale which takes in all of Broward County hosted 12 million visitors in 2012, including 2.8 million international visitors. The city and county in 2012 collected $43.9 million from the 5% hotel tax it charges, after hotels in the area recorded an occupancy rate for the year of 72.7 percent and an average daily rate of $114.48. The district has 561 hotels and motels comprising nearly 35,000 rooms. Forty six cruise ships sailed from Port Everglades in 2012. Greater Fort Lauderdale has over 4,000 restaurants, 63 golf courses, 12 shopping malls, 16 museums, 132 nightclubs, 278 parkland campsites, and 100 marinas housing 45,000 resident yachts.
Fort Lauderdale is named after a series of forts built by the United States during the Second Seminole War. The forts took their name from Major William Lauderdale (1782–1838), younger brother of Lieutenant Colonel James Lauderdale. William Lauderdale was the commander of the detachment of soldiers who built the first fort. However, development of the city did not begin until 50 years after the forts were abandoned at the end of the conflict. Three forts named "Fort Lauderdale" were constructed; the first was at the fork of the New River, the second at Tarpon Bend on the New River between the Colee Hammock and Rio Vista neighborhoods, and the third near the site of the Bahia Mar Marina.
The area in which the city of Fort Lauderdale would later be founded was inhabited for more than two thousand years by the Tequesta Indians. Contact with Spanish explorers in the 16th century proved disastrous for the Tequesta, as the Europeans unwittingly brought with them diseases, such as smallpox, to which the native populations possessed no resistance. For the Tequesta, disease, coupled with continuing conflict with their Calusa neighbors, contributed greatly to their decline over the next two centuries. By 1763, there were only a few Tequesta left in Florida, and most of them were evacuated to Cuba when the Spanish ceded Florida to the British in 1763, under the terms of the Treaty of Paris (1763), which ended the Seven Years' War. Although control of the area changed between Spain, the United Kingdom, the United States, and the Confederate States of America, it remained largely undeveloped until the 20th century.
The Fort Lauderdale area was known as the "New River Settlement" before the 20th century. In the 1830s there were approximately 70 settlers living along the New River. William Cooley, the local Justice of the Peace, was a farmer and wrecker, who traded with the Seminole Indians. On January 6, 1836, while Cooley was leading an attempt to salvage a wrecked ship, a band of Seminoles attacked his farm, killing his wife and children, and the children's tutor. The other farms in the settlement were not attacked, but all the white residents in the area abandoned the settlement, fleeing first to the Cape Florida Lighthouse on Key Biscayne, and then to Key West.
The first United States stockade named Fort Lauderdale was built in 1838, and subsequently was a site of fighting during the Second Seminole War. The fort was abandoned in 1842, after the end of the war, and the area remained virtually unpopulated until the 1890s. It was not until Frank Stranahan arrived in the area in 1893 to operate a ferry across the New River, and the Florida East Coast Railroad's completion of a route through the area in 1896, that any organized development began. The city was incorporated in 1911, and in 1915 was designated the county seat of newly formed Broward County.
Fort Lauderdale's first major development began in the 1920s, during the Florida land boom of the 1920s. The 1926 Miami Hurricane and the Great Depression of the 1930s caused a great deal of economic dislocation. In July 1935, an African-American man named Rubin Stacy was accused of robbing a white woman at knife point. He was arrested and being transported to a Miami jail when police were run off the road by a mob. A group of 100 white men proceeded to hang Stacy from a tree near the scene of his alleged robbery. His body was riddled with some twenty bullets. The murder was subsequently used by the press in Nazi Germany to discredit US critiques of its own persecution of Jews, Communists, and Catholics.
When World War II began, Fort Lauderdale became a major US base, with a Naval Air Station to train pilots, radar operators, and fire control, operators. A Coast Guard base at Port Everglades was also established.
On July 4, 1961, African Americans started a series of protests, wade-ins, at beaches that were off-limits to them, to protest "the failure of the county to build a road to the Negro beach". On July 11, 1962, a verdict by Ted Cabot went against the city's policy of racial segregation of public beaches.
Today, Fort Lauderdale is a major yachting center, one of the nation's largest tourist destinations, and the center of a metropolitan division with 1.8 million people.
Credit for the data above is given to the following website:
en.wikipedia.org/wiki/Fort_Lauderdale,_Florida
© All Rights Reserved - you may not use this image in any form without my prior permission.
Just another average Overland Route intermodal train lead by UP AC45CCTE 8034 leads this westbound ahead of the Big Boy a couple miles east of Rock Springs, Wyoming on May 4, 2019.
The mountains average 300+ inches of snow a year. The valley, in the immediate rain shadow of the mountains, averages about 40 inches a year. Because the sun 'burns' the valley snow off rather quickly, the valley is often open and without much snow cover. Winter pasture!
I wasn't going to post this one as I found the pose a little awkward. He was lovely and it is nice to see the back sometimes.
The Cattle Egret averages 17-21 inches in length with a wingspan just over three feet. Often observed feeding in open pastures & fields away from water. Follows grazing animals and tractors, feeding on disturbed insects.
Distinguished from the Great Egret & White Heron by its much smaller size, from immature Little blue Herons by having an orange bill.
In the United States, they are common year-round in Florida.
I found this one at Dinner Island Ranch WMA in Hendry County, Florida.
Thomas Woodworth was an average guy. He has a family who loves him very much, and he made his way through school not making any enemies. Though when it came time for graduation, he didn't know what to do with his life. He isn't very confident in himself, so he never pushed towards any of his dreams. Didn't help that his grades weren't the best. When it came to love, he was always stuck in the dreaded friend zone. One day when coming home, exhausted from work, he came upon what looked to be a homeless man begging for cash. Thomas felt bad for the guy and scrounged up $5 out of his wallet to give to the man. This man thanked him, and asked if he could have one wish, what would it be. Thomas replies saying that he just wants to be happy for a change. The man then touches Thomas on the shoulder, and there's a bright purple flash that appears for a second. Thomas backs away, confused of what's happening. But he wasn't scared at all. He was just happy.. From then on, whenever Thomas touches someone on the shoulder like the man did to him, it will give them this extreme euphoria. All fear is extinguished, and the person just feels happy. Thomas decided to use this power to make him some more money. He set up his own website, and anyone that wants to feel better than ever go to him. It's downside is that some people feel like they can then do anything, since they have no fear. People trying to jump off of a building, thinking they can fly, but end up dying from the fall.
Status: Alive and at large in Lowtown district of Cardinal.
Miami Beach is a coastal resort city in Miami-Dade County, Florida, United States. It was incorporated on March 26, 1915. The municipality is located on natural and man-made barrier islands between the Atlantic Ocean and Biscayne Bay, the latter of which separates the Beach from the mainland city of Miami. The neighborhood of South Beach, comprising the southernmost 2.5 square miles (6.5 km2) of Miami Beach, along with downtown Miami and the Port of Miami, collectively form the commercial center of South Florida. Miami Beach's estimated population is 92,307 according to the most recent United States census estimates. Miami Beach is the 26th largest city in Florida based on official 2017 estimates from the US Census Bureau. It has been one of America's pre-eminent beach resorts since the early 20th century.
In 1979, Miami Beach's Art Deco Historic District was listed on the National Register of Historic Places. The Art Deco District is the largest collection of Art Deco architecture in the world and comprises hundreds of hotels, apartments and other structures erected between 1923 and 1943. Mediterranean, Streamline Moderne and Art Deco are all represented in the District. The Historic District is bounded by the Atlantic Ocean on the East, Lenox Court on the West, 6th Street on the South and Dade Boulevard along the Collins Canal to the North. The movement to preserve the Art Deco District's architectural heritage was led by former interior designer Barbara Baer Capitman, who now has a street in the District named in her honor.
Miami Beach is governed by a ceremonial mayor and six commissioners. Although the mayor runs commission meetings, the mayor and all commissioners have equal voting power and are elected by popular election. The mayor serves for terms of two years with a term limit of three terms and commissioners serve for terms of four years and are limited to two terms. Commissioners are voted for citywide and every two years three commission seats are voted upon.
A city manager is responsible for administering governmental operations. An appointed city manager is responsible for administration of the city. The City Clerk and the City Attorney are also appointed officials.
In 1870, a father and son, Henry and Charles Lum, purchased the land for 75 cents an acre. The first structure to be built on this uninhabited oceanfront was the Biscayne House of Refuge, constructed in 1876 by the United States Life-Saving Service at approximately 72nd Street. Its purpose was to provide food, water, and a return to civilization for people who were shipwrecked. The next step in the development of the future Miami Beach was the planting of a coconut plantation along the shore in the 1880s by New Jersey entrepreneurs Ezra Osborn and Elnathan Field, but this was a failed venture. One of the investors in the project was agriculturist John S. Collins, who achieved success by buying out other partners and planting different crops, notably avocados, on the land that would later become Miami Beach. Meanwhile, across Biscayne Bay, the City of Miami was established in 1896 with the arrival of the railroad, and developed further as a port when the shipping channel of Government Cut was created in 1905, cutting off Fisher Island from the south end of the Miami Beach peninsula.
Collins' family members saw the potential in developing the beach as a resort. This effort got underway in the early years of the 20th century by the Collins/Pancoast family, the Lummus brothers (bankers from Miami), and Indianapolis entrepreneur Carl G. Fisher. Until then, the beach here was only the destination for day-trips by ferry from Miami, across the bay. By 1912, Collins and Pancoast were working together to clear the land, plant crops, supervise the construction of canals to get their avocado crop to market, and set up the Miami Beach Improvement Company. There were bath houses and food stands, but no hotel until Brown's Hotel was built in 1915 (still standing, at 112 Ocean Drive). Much of the interior land mass at that time was a tangled jungle of mangroves. Clearing it, deepening the channels and water bodies, and eliminating native growth almost everywhere in favor of landfill for development, was expensive. Once a 1600-acre, jungle-matted sand bar three miles out in the Atlantic, it grew to 2,800 acres when dredging and filling operations were completed.
With loans from the Lummus brothers, Collins had begun work on a 2½-mile-long wooden bridge, the world's longest wooden bridge at the time, to connect the island to the mainland. When funds ran dry and construction work stalled, Indianapolis millionaire and recent Miami transplant Fisher intervened, providing the financing needed to complete the bridge the following year in return for a land swap deal. That transaction kicked off the island's first real estate boom. Fisher helped by organizing an annual speed boat regatta, and by promoting Miami Beach as an Atlantic City-style playground and winter retreat for the wealthy. By 1915, Lummus, Collins, Pancoast, and Fisher were all living in mansions on the island, three hotels and two bath houses had been erected, an aquarium built, and an 18-hole golf course landscaped.
The Town of Miami Beach was chartered on March 26, 1915; it grew to become a City in 1917. Even after the town was incorporated in 1915 under the name of Miami Beach, many visitors thought of the beach strip as Alton Beach, indicating just how well Fisher had advertised his interests there. The Lummus property was called Ocean Beach, with only the Collins interests previously referred to as Miami Beach.
Carl Fisher was the main promoter of Miami Beach's development in the 1920s as the site for wealthy industrialists from the north and Midwest to and build their winter homes here. Many other Northerners were targeted to vacation on the island. To accommodate the wealthy tourists, several grand hotels were built, among them: The Flamingo Hotel, The Fleetwood Hotel, The Floridian, The Nautilus, and the Roney Plaza Hotel. In the 1920s, Fisher and others created much of Miami Beach as landfill by dredging Biscayne Bay; this man-made territory includes Star, Palm, and Hibiscus Islands, the Sunset Islands, much of Normandy Isle, and all of the Venetian Islands except Belle Isle. The Miami Beach peninsula became an island in April 1925 when Haulover Cut was opened, connecting the ocean to the bay, north of present-day Bal Harbour. The great 1926 Miami hurricane put an end to this prosperous era of the Florida Boom, but in the 1930s Miami Beach still attracted tourists, and investors constructed the mostly small-scale, stucco hotels and rooming houses, for seasonal rental, that comprise much of the present "Art Deco" historic district.
Carl Fisher brought Steve Hannagan to Miami Beach in 1925 as his chief publicist. Hannagan set-up the Miami Beach News Bureau and notified news editors that they could "Print anything you want about Miami Beach; just make sure you get our name right." The News Bureau sent thousands of pictures of bathing beauties and press releases to columnists like Walter Winchell and Ed Sullivan. One of Hannagan's favorite venues was a billboard in Times Square, New York City, where he ran two taglines: "'It's always June in Miami Beach' and 'Miami Beach, Where Summer Spends the Winter.'"
Post–World War II economic expansion brought a wave of immigrants to South Florida from the Northern United States, which significantly increased the population in Miami Beach within a few decades. After Fidel Castro's rise to power in 1959, a wave of Cuban refugees entered South Florida and dramatically changed the demographic make-up of the area. In 2017, one study named zip code 33109 (Fisher Island, a 216-acre island located just south of Miami Beach), as having the 4th most expensive home sales and the highest average annual income ($2.5 million) in 2015.
South Beach (also known as SoBe, or simply the Beach), the area from Biscayne Street (also known as South Pointe Drive) one block south of 1st Street to about 23rd Street, is one of the more popular areas of Miami Beach. Although topless sunbathing by women has not been officially legalized, female toplessness is tolerated on South Beach and in a few hotel pools on Miami Beach. Before the TV show Miami Vice helped make the area popular, SoBe was under urban blight, with vacant buildings and a high crime rate. Today, it is considered one of the richest commercial areas on the beach, yet poverty and crime still remain in some places near the area.
Miami Beach, particularly Ocean Drive of what is now the Art Deco District, was also featured prominently in the 1983 feature film Scarface and the 1996 comedy The Birdcage.
The New World Symphony Orchestra is based in Miami Beach, under the direction of Michael Tilson Thomas.
Lincoln Road, running east-west parallel between 16th and 17th Streets, is a nationally known spot for outdoor dining and shopping and features galleries of well known designers, artists and photographers such as Romero Britto, Peter Lik, and Jonathan Adler. In 2015, the Miami Beach residents passed a law forbidding bicycling, rollerblading, skateboarding and other motorized vehicles on Lincoln Road during busy pedestrian hours between 9:00am and 2:00am.
Credit for the data above is given to the following website:
The HWATR (Heavy Weaponized All Terrain Robot) Mk. 1 is a 3.4-meter-tall autonomous or remotely piloted combat mecha with impressive offensive capabilities. This mecha is equipped with three main armaments: a minigun with a 2,400-round cartridge; a compact railgun firing 6 rounds per minute and a 24-round cartridge, with a range of 1 km and capable of penetrating light armor such as that of LAVs and IFVs; and a single anti-tank TOW missile launcher. All weapons are manually reloadable. For defense, the HWATR has a drone jammer on top, smoke dischargers, and a laser detection system. Like all next-generation systems in the Plighia army, this mecha also features BODYGUARD technology. The weak points of this mecha are the lower joints, which are particularly exposed and poorly protected, to ensure maximum agility and speed (maximum speed similar to that of an average human running) on all types of terrain.
This satellite image was acquired over the edge of a salt marsh near the northeast Caspian Sea in southwestern Kazakhstan.
The Caspian Sea (not pictured) is the largest inland body of water by surface area. With an average depth of about 5 m, the northern part of the Caspian is very shallow, while the central and southern parts of the sea are much deeper. The salinity of the waters also change from north to south, being more saline in the northern, shallow waters and and less in the south.
The salt marsh in the upper section of this image was once a gulf of the Caspian Sea, but fluctuating sea levels over the last decades cause it to be cut off occasionally from the main body of water and even dry up. In this image, it appears that the water has evaporated, leaving behind a white salt crust.
Rock formations dominate the central part of the image, while a plateau stretches south and east (not pictured). The visible shapes in combination with the dark colour of the rocks may indicate that they are volcanic, with water erosion evident in the finger-like runoff patterns.
The grey rim between the land and salt pan comes from the sedimentary runoff from the land mixing with the saltwater. When the marsh is dry, a greyish colour is left behind.
The arid climate in this region makes it easy to acquire optical imagery from satellites, without the obstruction of visibility by clouds.
This image was acquired on 6 November 2012 by the Korea Aerospace Research Institute’s Kompsat-2 satellite and is featured on the Earth from Space video programme: www.esa.int/spaceinvideos/Videos/2014/04/Earth_from_Space...
Credit: KARI/ESA
The great white pelican (Pelecanus onocrotalus) also known as the eastern white pelican, rosy pelican or white pelican is a bird in the pelican family. It breeds from southeastern Europe through Asia and Africa, in swamps and shallow lakes.
The great white pelican is a huge bird—only the Dalmatian pelican is, on average, larger among pelicans. It measures 140 to 180 cm (55 to 71 in) in length with a 28.9 to 47.1 cm (11.4 to 18.5 in) enormous pink and yellow bill, and a dull pale-yellow gular pouch. The wingspan measures 226 to 360 cm (7.41 to 11.81 ft), the latter measurement being the highest among extant flying animals outside of the great albatross. The adult male measures about 175 cm (69 in) in length; it weighs from 9 to 15 kg (20 to 33 lb) and larger races from the Palaearctic are usually around 11 kg (24 lb), with few exceeding 13 kg (29 lb). It has a bill measuring 34.7 to 47.1 cm (13.7 to 18.5 in). The female measures about 148 cm (58 in) in length, and is considerably less bulky, weighing 5.4 to 9 kg (12 to 20 lb), and has a bill that measures 28.9 to 40.0 cm (11.4 to 15.7 in) in length. In Lake Edward, Uganda, the average weight of 52 males was found to 11.45 kg (25.2 lb) and in 22 females it was 7.59 kg (16.7 lb). In South Africa, the average weight of males was 9.6 kg (21 lb) and of females was 6.9 kg (15 lb). Thus the sexual dimorphism is especially pronounced in this species (perhaps the greatest known in any extant pelican), as at times the male can average more than 30% more massive than the female. Among standard measurements, the wing chord is 60 to 73 cm (24 to 29 in), the tail 16 to 21 cm (6.3 to 8.3 in), and the tarsus 13 to 14.9 cm (5.1 to 5.9 in) long. Standard measurements from different areas indicate that pelicans from the Western Palaearctic are somewhat larger than those from Asia and Africa.
The male has a downward bend in the neck and the female has a shorter, straighter beak. The plumage is predominantly white except on remiges, with a faint pink tinge on the neck and a yellowish base on the foreneck. The primary feathers are black, with white shafts at the bases, occasionally with paler tips and narrow fringes. The secondary feathers are also black, but with a whitish fringe. The upperwing coverts, underwing coverts, and tertials are white. The forehead is swollen and pinkish skin surrounds the bare, dark eyes having brown-red to dark brown irides. It has fleshy-yellow legs and pointed forehead-feathers where meeting the culmen. In breeding season, the male has pinkish skin while the female has orangey skin on its face. The bill is mostly bluish grey, with a red tip, reddish maxilla edges, and a cream-yellow to yolk-yellow gular pouch. The white plumage becomes tinged-pink with a yellow patch on the breast, and the body is tinged yellowish-rosy. It also has a short, shaggy crest on the nape. The white covert feathers contrast with the solid black primary and secondary feathers. The legs are yellow-flesh to pinkish orange. Both male and female are similar, but the female is smaller and has brighter orange facial skin in the breeding season.
The juvenile has darker, brownish underparts that are palest at the rump, center of the belly, and uppertail coverts. The underwing coverts are mostly dull-white, but the greater coverts are dark and there is a dark brownish bar over the lesser coverts. The rear tertials upperwing coverts mostly have paler tips with a silvery-grey tinge on the greater secondary coverts and tertials. It has dark flight feathers, and brown-edged wings. The head, neck, and upperparts, including the upperwing coverts, are mostly brown—this is the darkest part of the neck. The facial skin and the bill, including its gular pouch, are greyish to dusky greyish. The forehead, rump, and abdomen are white, and its legs and feet are grey. Its blackish tail occasionally has a silvery-grey tinge. Its underparts and back are initially browner and darker than those of the Dalmatian pelican, and the underwing is strongly patterned, similar to the juvenile brown pelican.
The great white pelican is distinguished from all other pelicans by its plumage. Its face is naked and the feathering on its forehead tapers to a fine point, whereas other species are completely feathered. In flight, the white underwing with black remiges of the adult are similar only to those of the American white pelican (P. erythrorhynchos), but the latter has white inner secondary feathers. It differs from the Dalmatian pelican in its pure white – rather than greyish-white – plumage, a bare pink facial patch around the eye, and pinkish legs. The spot-billed pelican (P. philippensis) of Asia is slightly smaller than the great white pelican, with greyish tinged white plumage, and a paler, duller-colored bill.[5] Similarly, the pink-backed pelican (P. rufescens) is smaller, with brownish-grey plumage, a light pink to off-grey bill, and a pinkish wash on the back.
The bird is mostly silent but has a variety of low-pitched lowing, grunting, and growling calls. The flight call is a deep, quiet croak., while at breeding colonies, it gives deep moooo calls.
The breeding range of the great white pelican extends to Ethiopia, Tanzania, Chad, northern Cameroons, and Nigeria in Africa, and has been observed or reported breeding in Zambia, Botswana, and South Africa. In the 1990s, 6,700 to 11,000 breeding pairs in 23 to 25 breeding sites, were found in the Palearctic region. A 1991 study noted about 3,070 to 4,300 pairs were present in the Soviet Union. Only two breeding colonies are located in the Mediterranean basin, one having 250 to 400 pairs in Turkey and the other having 50 to 100 pairs in northern Greece. The breeding colony at Lake Rukwa, Tanzania is the largest known breeding colony in Africa, followed by the Lake Shala, Ethiopia colony which is probably of crucial importance to the species in Africa.
The African population of about 75,000 pairs of the great white pelican is resident. The ones breeding in the Palearctic region are migrants, although it is possible that the majority of the western Palearctic populations stop-over in Israel during their autumn migration. The migration routes are only partially known. Migratory populations are found from Eastern Europe to Kazakhstan during the breeding season. More than 50% of Eurasian great white pelicans breed in the Danube Delta in Romania. They also prefer staying in the Lakes near Burgas, Bulgaria and in Srebarna Lake in Bulgaria. The pelicans arrive in the Danube in late March or early April and depart after breeding from September to late November. Wintering locations for European pelicans are not exactly known but wintering birds may occur in northeastern Africa through Iraq to north India, with a particularly large number of breeders from Asia wintering around Pakistan and Sri Lanka. Northern populations migrate to China, India, Myanmar, with stragglers reaching Java and Bali in Indonesia. These are birds that are found mostly in lowlands, though in East Africa and Nepal may be found living at elevations of up to 1,372 m (4,501 ft).
Overall, the great white pelican is one of the most widely distributed species. Although some areas still hold quite large colonies, it ranks behind the brown pelican and possibly the Australian pelican in overall abundance. Europe now holds an estimated 7,345–10,000 breeding pairs, with over 4,000 pairs that are known to nest in Russia. During migration, more than 75,000 have been observed in Israel and, in winter, over 45,000 may stay in Pakistan. In all its colonies combined, 75,000 pairs are estimated to nest in Africa. It is possibly extinct in Serbia and Montenegro, and regionally extinct in Hungary.
Great white pelicans usually prefer shallow, (seasonally or tropical) warm fresh water. Well scattered groups of breeding pelicans occur through Eurasia from the eastern Mediterranean to Vietnam. In Eurasia, fresh or brackish waters may be inhabited and the pelicans may be found in lakes, deltas, lagoons and marshes, usually with dense reed beds nearby for nesting purposes. Additionally, sedentary populations are found year-round in Africa, south of the Sahara Desert although these are patchy. In Africa, great white pelicans occur mainly around freshwater and alkaline lakes and may also be found in coastal, estuarine areas. Beyond reed beds, African pelicans have nested on inselbergs and flat inshore islands off of Banc d'Arguin National Park.
For more information, please visit en.wikipedia.org/wiki/Great_white_pelican
Tool bit vending machine. This was located in a local engineering company workshop. Any time they needed a new tool bit they just paid and got one from the machine. No waiting. The machine would send a stock message back to head office and they could keep track of which tools were most required and restock the racks accordingly.
I love shots like this. Nothing over the top and its almost like you can smell the country dirt when you look at the image. Just a natural girl, in a natural setting.. naturally beautiful!
Colorado Model Katie C.
I have titled this a little tounge in cheek. When me an my mate went to Castle Hill he said the sunset was only average. At the time he was fairly right but for a short time the sky had given a few very nice patterns and colours. A little processing and this has been brought out nicely on this one.
Me, sporting covid hair, wearing mask by Joe Average.
WIKI - "Joe Average (born October 10, 1957) is a Canadian artist who resides in Vancouver, British Columbia. Diagnosed HIV+ at age 27, Average made the decision to commit the rest of his life to art."
Joe is a beloved national icon, philanthropist and humanitarian. joeaverageart.com/
The common watersnake can grow up to 4 ft 5 in in total length. Per one study, the average total length of females was 2 ft 8 in, while that of males was 2 ft 3 1/2 in. From known studies of this species in the wild, adult females can weigh between 5 1⁄2 and 14 1⁄2 oz typically, while the smaller male can range from 2 7⁄8 to 5 3⁄8 oz). The largest females can weigh up to 20 oz while the largest males can scale 13 oz.
These snakes can be brown, gray, reddish, or brownish-black. It has dark crossbands on the neck and dark blotches on the rest of the body, often leading to misidentification as a cottonmouth or copperhead by novices. As they age, the color darkens, and the pattern becomes obscure. Some individuals become almost completely black. The belly also varies in color. It can be white, yellow, or gray; usually, it also has reddish or black crescents.
The common watersnake is nonvenomous and harmless to humans, but superficially resembles the venomous cottonmouth. It is often killed by humans out of fear; killing snakes greatly increases the chance of being bitten. The two can be easily distinguished: the watersnake has a longer, more slender body and a flattened head the same width as the neck, round pupils, and no heat-sensing pits. The cottonmouth has a fatter body, a wedge-shaped head with prominent venom glands that are wider than the neck, cat-like pupils, and heat-sensing pits between the eyes and the nostrils.
Goldfinch
(Carduelis carduelis)
The average goldfinch is 12–13 cm long with a wingspan of 21–25 cm and a weight of 14 to 19 grams. The sexes are broadly similar, with a red face, black and white head, warm brown upperparts, white underparts with buff flanks and breast patches, and black and yellow wings.
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No ND filter big enough for the 300mm, so a fake long exposure by way of averaging 64 images.
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.
Current estimates of average nodule abundance in four major locations.
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I like the some of the Outfits.
Denmark and Barcelona look like for old Ladys instead for an average Teenage Girl.
I wish there was a Picture on the site without the Jacket from the Denmark set. Maybe it would look younger without it.
We also see the problem with larger Dolls and Fabric.
It makes them look even larger.
Lammily turn from average to plus size cause the Fabric is to thick and stiff.
Its like we would make oure Clothes out of Carpet.
Thats the main reason Barbie and other Dols are so thin.
They look normal with Clothes on.
Also the Clothes are really expensive.
Now the quetion is why?
Is it because the production is so expensive and they use high quality ore do they take advantage of the fact Lammily can not wear Barbie Clothes?
Maybe Jem and Dusty Clothes would fit. At least Tops and Dresses.
When i order a Lammily i would buy the scotish and the London set. These look cool.