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Niagara Falls is a group of three waterfalls at the southern end of Niagara Gorge, spanning the border between the province of Ontario in Canada and the state of New York in the United States. The largest of the three is Horseshoe Falls, which straddles the international border of the two countries. It is also known as the Canadian Falls. The smaller American Falls and Bridal Veil Falls lie within the United States. Bridal Veil Falls is separated from Horseshoe Falls by Goat Island and from American Falls by Luna Island, with both islands situated in New York.
Formed by the Niagara River, which drains Lake Erie into Lake Ontario, the combined falls have the highest flow rate of any waterfall in North America that has a vertical drop of more than 50 m (160 ft). During peak daytime tourist hours, more than 168,000 m3 (5.9 million cu ft) of water goes over the crest of the falls every minute. Horseshoe Falls is the most powerful waterfall in North America, as measured by flow rate. Niagara Falls is famed for its beauty and is a valuable source of hydroelectric power. Balancing recreational, commercial, and industrial uses has been a challenge for the stewards of the falls since the 19th century.
Niagara Falls is 27 km (17 mi) northwest of Buffalo, New York, and 69 km (43 mi) southeast of Toronto, between the twin cities of Niagara Falls, Ontario, and Niagara Falls, New York. Niagara Falls was formed when glaciers receded at the end of the Wisconsin glaciation (the last ice age), and water from the newly formed Great Lakes carved a path over and through the Niagara Escarpment en route to the Atlantic Ocean.
Horseshoe Falls is about 57 m (187 ft) high, while the height of the American Falls varies between 21 and 30 m (69 and 98 ft) because of the presence of giant boulders at its base. The larger Horseshoe Falls is about 790 m (2,590 ft) wide, while the American Falls is 320 m (1,050 ft) wide. The distance between the American extremity of Niagara Falls and the Canadian extremity is 1,039 m (3,409 ft).
The peak flow over Horseshoe Falls was recorded at 6,370 m3 (225,000 cu ft) per second. The average annual flow rate is 2,400 m3 (85,000 cu ft) per second. Since the flow is a direct function of the Lake Erie water elevation, it typically peaks in late spring or early summer. During the summer months, at least 2,800 m3 (99,000 cu ft) per second of water traverse the falls, some 90% of which goes over Horseshoe Falls, while the balance is diverted to hydroelectric facilities and then on to American Falls and Bridal Veil Falls. This is accomplished by employing a weir – the International Control Dam – with movable gates upstream from Horseshoe Falls.
The water flow is halved at night and during the low tourist season winter months and only attains a minimum flow of 1,400 cubic metres (49,000 cu ft) per second. Water diversion is regulated by the 1950 Niagara Treaty and is administered by the International Niagara Board of Control. The verdant green color of the water flowing over Niagara Falls is a byproduct of the estimated 60 tonnes/minute of dissolved salts and rock flour (very finely ground rock) generated by the erosive force of the Niagara River.
The Niagara River is an Important Bird Area due to its impact on Bonaparte's gulls, ring-billed gulls, and herring gulls. Several thousand birds migrate and winter in the surrounding area.
The features that became Niagara Falls were created by the Wisconsin glaciation about 10,000 years ago. The retreat of the ice sheet left behind a large amount of meltwater (see Lake Algonquin, Lake Chicago, Glacial Lake Iroquois, and Champlain Sea) that filled up the basins that the glaciers had carved, thus creating the Great Lakes as we know them today. Scientists posit there is an old valley, St David's Buried Gorge, buried by glacial drift, at the approximate location of the present Welland Canal.
When the ice melted, the upper Great Lakes emptied into the Niagara River, which followed the rearranged topography across the Niagara Escarpment. In time, the river cut a gorge through the north-facing cliff, or cuesta. Because of the interactions of three major rock formations, the rocky bed did not erode evenly. The caprock formation is composed of hard, erosion-resistant limestone and dolomite of the Lockport Formation (Middle Silurian). That hard layer of stone eroded more slowly than the underlying materials. Immediately below the caprock lies the weaker, softer, sloping Rochester Formation (Lower Silurian). This formation is composed mainly of shale, though it has some thin limestone layers. It also contains ancient fossils. In time, the river eroded the soft layer that supported the hard layers, undercutting the hard caprock, which gave way in great chunks. This process repeated countless times, eventually carving out the falls. Submerged in the river in the lower valley, hidden from view, is the Queenston Formation (Upper Ordovician), which is composed of shales and fine sandstones. All three formations were laid down in an ancient sea, their differences of character deriving from changing conditions within that sea.
About 10,900 years ago, the Niagara Falls was between present-day Queenston, Ontario, and Lewiston, New York, but erosion of the crest caused the falls to retreat approximately 6.8 miles (10.9 km) southward. The shape of Horseshoe Falls has changed through the process of erosion, evolving from a small arch to a horseshoe bend to the present day V-shape. Just upstream from the falls' current location, Goat Island splits the course of the Niagara River, resulting in the separation of Horseshoe Falls to the west from the American and Bridal Veil Falls to the east. Engineering has slowed erosion and recession.
Future of the falls
The current rate of erosion is approximately 30 centimeters (0.98 feet) per year, down from a historical average of 0.91 m (3.0 ft) per year. At this rate, in about 50,000 years Niagara Falls will have eroded the remaining 32 km (20 mi) to Lake Erie, and the falls will cease to exist.
Preservation efforts
In the 1870s, sightseers had limited access to Niagara Falls and often had to pay for a glimpse, and industrialization threatened to carve up Goat Island to further expand commercial development. Other industrial encroachments and lack of public access led to a conservation movement in the U.S. known as Free Niagara, led by such notables as Hudson River School artist Frederic Edwin Church, landscape designer Frederick Law Olmsted, and architect Henry Hobson Richardson. Church approached Lord Dufferin, governor-general of Canada, with a proposal for international discussions on the establishment of a public park.
Goat Island was one of the inspirations for the American side of the effort. William Dorsheimer, moved by the scene from the island, brought Olmsted to Buffalo in 1868 to design a city park system, which helped promote Olmsted's career. In 1879, the New York state legislature commissioned Olmsted and James T. Gardner to survey the falls and to create the single most important document in the Niagara preservation movement, a "Special Report on the preservation of Niagara Falls". The report advocated for state purchase, restoration and preservation through public ownership of the scenic lands surrounding Niagara Falls. Restoring the former beauty of the falls was described in the report as a "sacred obligation to mankind". In 1883, New York Governor Grover Cleveland drafted legislation authorizing acquisition of lands for a state reservation at Niagara, and the Niagara Falls Association, a private citizens group founded in 1882, mounted a great letter-writing campaign and petition drive in support of the park. Professor Charles Eliot Norton and Olmsted were among the leaders of the public campaign, while New York Governor Alonzo Cornell opposed.
Preservationists' efforts were rewarded on April 30, 1885, when Governor David B. Hill signed legislation creating the Niagara Reservation, New York's first state park. New York State began to purchase land from developers, under the charter of the Niagara Reservation State Park. In the same year, the province of Ontario established the Queen Victoria Niagara Falls Park for the same purpose. On the Canadian side, the Niagara Parks Commission governs land usage along the entire course of the Niagara River, from Lake Erie to Lake Ontario.
In 1887, Olmsted and Calvert Vaux issued a supplemental report detailing plans to restore the falls. Their intent was "to restore and conserve the natural surroundings of the Falls of Niagara, rather than to attempt to add anything thereto", and the report anticipated fundamental questions, such as how to provide access without destroying the beauty of the falls, and how to restore natural landscapes damaged by man. They planned a park with scenic roadways, paths and a few shelters designed to protect the landscape while allowing large numbers of visitors to enjoy the falls. Commemorative statues, shops, restaurants, and a 1959 glass and metal observation tower were added later. Preservationists continue to strive to strike a balance between Olmsted's idyllic vision and the realities of administering a popular scenic attraction.
Preservation efforts continued well into the 20th century. J. Horace McFarland, the Sierra Club, and the Appalachian Mountain Club persuaded the United States Congress in 1906 to enact legislation to preserve the falls by regulating the waters of the Niagara River. The act sought, in cooperation with the Canadian government, to restrict diversion of water, and a treaty resulted in 1909 that limited the total amount of water diverted from the falls by both nations to approximately 56,000 cubic feet per second (1,600 m3/s). That limitation remained in effect until 1950.
Erosion control efforts have always been of importance. Underwater weirs redirect the most damaging currents, and the top of the falls has been strengthened. In June 1969, the Niagara River was completely diverted from American Falls for several months through construction of a temporary rock and earth dam. During this time, two bodies were removed from under the falls, including a man who had been seen jumping over the falls, and the body of a woman, which was discovered once the falls dried. While Horseshoe Falls absorbed the extra flow, the U.S. Army Corps of Engineers studied the riverbed and mechanically bolted and strengthened any faults they found; faults that would, if left untreated, have hastened the retreat of American Falls. A plan to remove the huge mound of talus deposited in 1954 was abandoned owing to cost, and in November 1969, the temporary dam was dynamited, restoring flow to American Falls. Even after these undertakings, Luna Island, the small piece of land between the American Falls and Bridal Veil Falls, remained off limits to the public for years owing to fears that it was unstable and could collapse into the gorge.
Commercial interests have continued to encroach on the land surrounding the state park, including the construction of several tall buildings (most of them hotels) on the Canadian side. The result is a significant alteration and urbanisation of the landscape. One study found that the tall buildings changed the breeze patterns and increased the number of mist days from 29 per year to 68 per year, but another study disputed this idea.
In 2013, New York State began an effort to renovate Three Sisters Islands located south of Goat Island. Funds were used from the re-licensing of the New York Power Authority hydroelectric plant downriver in Lewiston, New York, to rebuild walking paths on the Three Sisters Islands and to plant native vegetation on the islands. The state also renovated the area around Prospect Point at the brink of American Falls in the state park.
Toponymy
Theories differ as to the origin of the name of the falls. The Native American word Ongiara means thundering water; The New York Times used this in 1925. According to Iroquoian scholar Bruce Trigger, Niagara is derived from the name given to a branch of the local native Neutral Confederacy, who are described as the Niagagarega people on several late-17th-century French maps of the area. According to George R. Stewart, it comes from the name of an Iroquois town called Onguiaahra, meaning "point of land cut in two". In 1847, an Iroquois interpreter stated that the name came from Jaonniaka-re, meaning "noisy point or portage". To Mohawks, the name refers to "the neck", pronounced "onyara"; the portage or neck of land between lakes Erie and Ontario onyara.
History
Many figures have been suggested as first circulating a European eyewitness description of Niagara Falls. The Frenchman Samuel de Champlain visited the area as early as 1604 during his exploration of what is now Canada, and members of his party reported to him the spectacular waterfalls, which he described in his journals. The first description of the falls is credited to Belgian missionary, Father Louis Hennepin in 1677, after traveling with the explorer René-Robert Cavelier, Sieur de La Salle, thus bringing the falls to the attention of Europeans. French Jesuit missionary Paul Ragueneau likely visited the falls some 35 years before Hennepin's visit while working among the Huron First Nation in Canada. Jean de Brébeuf also may have visited the falls, while spending time with the Neutral Nation. The Finnish-Swedish naturalist Pehr Kalm explored the area in the early 18th century and is credited with the first scientific description of the falls. In 1762, Captain Thomas Davies, a British Army officer and artist, surveyed the area and painted the watercolor, An East View of the Great Cataract of Niagara, the first eyewitness painting of the falls.
During the 19th century, tourism became popular, and by the mid-century, it was the area's main industry. Theodosia Burr Alston (daughter of Vice President Aaron Burr) and her husband Joseph Alston were the first recorded couple to honeymoon there in 1801. Napoleon Bonaparte's brother Jérôme visited with his bride in the early 19th century. In 1825, British explorer John Franklin visited the falls while passing through New York en route to Cumberland House as part of his second Arctic expedition, calling them "so justly celebrated as the first in the world for grandeur".
In 1843, Frederick Douglass joined the American Anti-Slavery Society's "One Hundred Conventions" tour throughout New York and the midwest. Sometime on this tour, Douglass visited Niagara Falls and wrote a brief account of the experience: "When I came into its awful presence the power of discription failed me, an irrisistible power closed my lips." Being on the Canadian border, Niagara Falls was on one of the routes of the Underground Railroad. The falls were also a popular tourist attraction for Southern slaveowners, who would bring their enslaved workers on the trip. "Many a time the trusted body-servant, or slave-girl, would leave master or mistress in the discharge of some errand, and never come back." This sometimes led to conflict. Early town father Peter Porter assisted slavecatchers in finding runaway slaves, even leading, in the case of runaway Solomon Moseby, to a riot in Niagara-on-the-Lake, Canada. Much of this history is memorialized in the Niagara Falls Underground Railroad Heritage Center. After the American Civil War, the New York Central Railroad publicized Niagara Falls as a focus of pleasure and honeymoon visits. After World War II, the auto industry, along with local tourism boards, began to promote Niagara honeymoons.
In about 1840, the English industrial chemist Hugh Lee Pattinson traveled to Canada, stopping at Niagara Falls long enough to make the earliest known photograph of the falls, a daguerreotype in the collection of Newcastle University. It was once believed that the small figure standing silhouetted with a top hat was added by an engraver working from imagination as well as the daguerreotype as his source, but the figure is clearly present in the photograph. Because of the very long exposure required, of ten minutes or more, the figure is assumed by Canada's Niagara Parks agency to be Pattinson. The image is left-right inverted and taken from the Canadian side. Pattinson made other photographs of Horseshoe Falls; these were then transferred to engravings to illustrate Noël Marie Paymal Lerebours' Excursions Daguerriennes (Paris, 1841–1864).[55]
On August 6, 1918, an iron scow became stuck on the rocks above the falls. The two men on the scow were rescued, but the vessel remained trapped on rocks in the river, and is still visible there in a deteriorated state, although its position shifted by 50 meters (160 ft) during a storm on October 31, 2019. Daredevil William "Red" Hill Sr. was particularly praised for his role in the rescue.
After the First World War, tourism boomed as automobiles made getting to the falls much easier. The story of Niagara Falls in the 20th century is largely that of efforts to harness the energy of the falls for hydroelectric power, and to control the development on both sides that threaten the area's natural beauty. Before the late 20th century, the northeastern end of Horseshoe Falls was in the United States, flowing around the Terrapin Rocks, which were once connected to Goat Island by a series of bridges. In 1955, the area between the rocks and Goat Island was filled in, creating Terrapin Point. In the early 1980s, the U.S. Army Corps of Engineers filled in more land and built diversion dams and retaining walls to force the water away from Terrapin Point. Altogether, 400 ft (120 m) of Horseshoe Falls were eliminated, including 100 ft (30 m) on the Canadian side. According to author Ginger Strand, the Horseshoe Falls is now entirely in Canada. Other sources say "most of" Horseshoe Falls is in Canada.
The only recorded freeze-up of the river and falls was caused by an ice jam on March 29, 1848. No water (or at best a trickle) fell for as much as 40 hours. Waterwheels stopped, and mills and factories shut down for having no power. In 1912, American Falls was completely frozen, but the other two falls kept flowing. Although the falls commonly ice up most winters, the river and the falls do not freeze completely. The years 1885, 1902, 1906, 1911, 1932, 1936, 2014, 2017 and 2019 are noted for partial freezing of the falls. A so-called ice bridge was common in certain years at the base of the falls and was used by people who wanted to cross the river before bridges had been built. During some winters, the ice sheet was as thick as 40 to 100 feet (12 to 30 m), but that thickness has not occurred since 1954. The ice bridge of 1841 was said to be at least 100 feet thick. On February 12, 1912, the ice bridge which had formed on January 15 began breaking up while people were still on it. Many escaped, but three died during the event, later named the Ice Bridge Tragedy.
Bridge crossings
A number of bridges have spanned the Niagara River in the general vicinity of the falls. The first, not far from the whirlpool, was a suspension bridge above the gorge. It opened for use by the public in July 1848 and remained in use until 1855. A second bridge in the Upper Falls area was commissioned, with two levels or decks, one for use by the Great Western Railway. This Niagara Falls Suspension Bridge opened in 1855. It was used by conductors on the Underground Railroad to escort runaway slaves to Canada. In 1882, the Grand Trunk Railway took over control of the second deck after it absorbed the Great Western company. Significant structural improvements were made in the late 1870s and then in 1886; this bridge remained in use until 1897.
Because of the volume of traffic, the decision was made to construct a new arch bridge nearby, under and around the existing bridge. After it opened in September 1897, a decision was made to remove and scrap the railway suspension bridge. This new bridge was initially known as the Niagara Railway Arch, or Lower Steel Arch Bridge; it had two decks, the lower one used for carriages and the upper for trains. In 1937, it was renamed the Whirlpool Rapids Bridge and remains in use today. All of the structures built up to that time were referred to as Lower Niagara bridges and were some distance from the falls.
The first bridge in the so-called Upper Niagara area (closer to the falls) was a two-level suspension structure that opened in January 1869; it was destroyed during a severe storm in January 1889. The replacement was built quickly and opened in May 1889. In order to handle heavy traffic, a second bridge was commissioned, slightly closer to American Falls. This one was a steel bridge and opened to traffic in June 1897; it was known as the Upper Steel Arch Bridge but was often called the Honeymoon Bridge. The single level included a track for trolleys and space for carriages and pedestrians. The design led to the bridge being very close to the surface of the river and in January 1938, an ice jam twisted the steel frame of the bridge which later collapsed on January 27, 1938.
Another Lower Niagara bridge had been commissioned in 1883 by Cornelius Vanderbilt for use by railways at a location roughly approximately 200 feet south of the Railway Suspension Bridge. This one was of an entirely different design; it was a cantilever bridge to provide greater strength. The Niagara Cantilever Bridge had two cantilevers which were joined by steel sections; it opened officially in December 1883, and improvements were made over the years for a stronger structure. As rail traffic was increasing, the Michigan Central Railroad company decided to build a new bridge in 1923, to be located between the Lower Steel Arch Bridge and the Cantilever Bridge. The Michigan Central Railway Bridge opened in February 1925 and remained in use until the early 21st century. The Cantilever Bridge was removed and scrapped after the new rail bridge opened. Nonetheless, it was inducted into the North America Railway Hall of Fame in 2006.
There was a lengthy dispute as to which agency should build the replacement for the Niagara Railway Arch, or Lower Steel Arch Bridge in the Upper Niagara area. When that was resolved, construction of a steel bridge commenced in February 1940. Named the Rainbow Bridge, and featuring two lanes for traffic separated by a barrier, it opened in November 1941 and remains in use today.
Industry and commerce
The enormous energy of Niagara Falls has long been recognized as a potential source of power. The first known effort to harness the waters was in 1750, when Daniel Joncaire built a small canal above the falls to power his sawmill. Augustus and Peter Porter purchased this area and all of American Falls in 1805 from the New York state government, and enlarged the original canal to provide hydraulic power for their gristmill and tannery. In 1853, the Niagara Falls Hydraulic Power and Mining Company was chartered, which eventually constructed the canals that would be used to generate electricity. In 1881, under the leadership of Jacob F. Schoellkopf, the Niagara River's first hydroelectric generating station was built. The water fell 86 feet (26 m) and generated direct current electricity, which ran the machinery of local mills and lit up some of the village streets.
The Niagara Falls Power Company, a descendant of Schoellkopf's firm, formed the Cataract Company headed by Edward Dean Adams, with the intent of expanding Niagara Falls' power capacity. In 1890, a five-member International Niagara Commission headed by Sir William Thomson among other distinguished scientists deliberated on the expansion of Niagara hydroelectric capacity based on seventeen proposals but could not select any as the best combined project for hydraulic development and distribution. In 1893, Westinghouse Electric (which had built the smaller-scale Ames Hydroelectric Generating Plant near Ophir, Colorado, two years earlier) was hired to design a system to generate alternating current on Niagara Falls, and three years after that a large-scale AC power system was created (activated on August 26, 1895). The Adams Power Plant Transformer House remains as a landmark of the original system.
By 1896, financing from moguls including J. P. Morgan, John Jacob Astor IV, and the Vanderbilts had fueled the construction of giant underground conduits leading to turbines generating upwards of 100,000 horsepower (75 MW), sent as far as Buffalo, 20 mi (32 km) away. Some of the original designs for the power transmission plants were created by the Swiss firm Faesch & Piccard, which also constructed the original 5,000 hp (3.7 MW) waterwheels. Private companies on the Canadian side also began to harness the energy of the falls. The Government of Ontario eventually brought power transmission operations under public control in 1906, distributing Niagara's energy to various parts of the Canadian province.
Other hydropower plants were being built along the Niagara River. But in 1956, disaster struck when the region's largest hydropower station was partially destroyed in a landslide. This drastically reduced power production and put tens of thousands of manufacturing jobs at stake. In 1957, Congress passed the Niagara Redevelopment Act, which granted the New York Power Authority the right to fully develop the United States' share of the Niagara River's hydroelectric potential.
In 1961, when the Niagara Falls hydroelectric project went online, it was the largest hydropower facility in the Western world. Today, Niagara is still the largest electricity producer in New York state, with a generating capacity of 2.4 GW. Up to 1,420 cubic metres (380,000 US gal) of water per second is diverted from the Niagara River through conduits under the city of Niagara Falls to the Lewiston and Robert Moses power plants. Currently between 50% and 75% of the Niagara River's flow is diverted via four huge tunnels that arise far upstream from the waterfalls. The water then passes through hydroelectric turbines that supply power to nearby areas of Canada and the United States before returning to the river well past the falls. When electrical demand is low, the Lewiston units can operate as pumps to transport water from the lower bay back up to the plant's reservoir, allowing this water to be used again during the daytime when electricity use peaks. During peak electrical demand, the same Lewiston pumps are reversed and become generators.
To preserve Niagara Falls' natural beauty, a 1950 treaty signed by the U.S. and Canada limited water usage by the power plants. The treaty allows higher summertime diversion at night when tourists are fewer and during the winter months when there are even fewer tourists. This treaty, designed to ensure an "unbroken curtain of water" flowing over the falls, states that during daylight time during the tourist season (April 1 to October 31) there must be 100,000 cubic feet per second (2,800 m3/s) of water flowing over the falls, and during the night and off-tourist season there must be 50,000 cubic feet per second (1,400 m3/s) of water flowing over the falls. This treaty is monitored by the International Niagara Board of Control, using a NOAA gauging station above the falls. During winter, the Power Authority of New York works with Ontario Power Generation to prevent ice on the Niagara River from interfering with power production or causing flooding of shoreline property. One of their joint efforts is an 8,800-foot-long (2,700 m) ice boom, which prevents the buildup of ice, yet allows water to continue flowing downstream. In addition to minimum water volume, the crest of Horseshoe falls was reduced to maintain an uninterrupted "curtain of water".
In August 2005, Ontario Power Generation, which is responsible for the Sir Adam Beck stations, started a major civil engineering project, called the Niagara Tunnel Project, to increase power production by building a new 12.7-metre (42 ft) diameter, 10.2-kilometre-long (6.3 mi) water diversion tunnel. It was officially placed into service in March 2013, helping to increase the generating complex's nameplate capacity by 150 megawatts. It did so by tapping water from farther up the Niagara River than was possible with the preexisting arrangement. The tunnel provided new hydroelectricity for approximately 160,000 homes.
Transport
Ships can bypass Niagara Falls by means of the Welland Canal, which was improved and incorporated into the Saint Lawrence Seaway in the mid-1950s. While the seaway diverted water traffic from nearby Buffalo and led to the demise of its steel and grain mills, other industries in the Niagara River valley flourished with the help of the electric power produced by the river. However, since the 1970s the region has declined economically.
The cities of Niagara Falls, Ontario, Canada, and Niagara Falls, New York, United States, are connected by two international bridges. The Rainbow Bridge, just downriver from the falls, affords the closest view of the falls and is open to non-commercial vehicle traffic and pedestrians. The Whirlpool Rapids Bridge lies one mile (1.6 km) north of the Rainbow Bridge and is the oldest bridge over the Niagara River. Nearby Niagara Falls International Airport and Buffalo Niagara International Airport were named after the waterfall, as were Niagara University, countless local businesses, and even an asteroid.
Over the falls
The first recorded publicity stunt using the Falls was the wreck of the schooner Michigan in 1827. Local hotel owners acquired a former Lake Erie freighter, loaded it with animals and effigies of people, towed it to a spot above the falls and let it plunge over the brink. Admission of fifty cents was charged.
In October 1829, Sam Patch, who called himself "the Yankee Leapster", jumped from a high tower into the gorge below the falls and survived; this began a long tradition of daredevils trying to go over the falls. Englishman Captain Matthew Webb, the first man to swim the English Channel, drowned in 1883 trying to swim the rapids downriver from the falls.
On October 24, 1901, 63-year-old Michigan school teacher Annie Edson Taylor became the first person to go over the falls in a barrel as a publicity stunt; she survived, bleeding, but otherwise unharmed. Soon after exiting the barrel, she said, "No one ought ever do that again." Days before Taylor's attempt, her domestic cat was sent over the falls in her barrel to test its strength. The cat survived the plunge unharmed and later posed with Taylor in photographs. Since Taylor's historic ride, over a dozen people have intentionally gone over the falls in or on a device, despite her advice. Some have survived unharmed, but others have drowned or been severely injured. Survivors face charges and stiff fines, as it is now illegal, on both sides of the border, to attempt to go over the falls. Charles Stephens, a 58-year-old barber from Bristol, England, went over the falls in a wooden barrel in July 1920 and was the first person to die in an endeavor of this type. Bobby Leach went over Horseshoe Falls in a crude steel barrel in 1911 and needed rescuing by William "Red" Hill Sr. Hill again came to the rescue of Leach following his failed attempt to swim the Niagara Gorge in 1920. In 1928, "Smiling Jean" Lussier tried an entirely different concept, going over the falls in a large rubber ball; he was successful and survived the ordeal.
Annie Edson Taylor posing with her wooden barrel (1901)
In the "Miracle at Niagara", on July 9, 1960, Roger Woodward, a seven-year-old American boy, was swept over Horseshoe Falls after the boat in which he was cruising lost power; two tourists pulled his 17-year-old sister Deanne from the river only 20 ft (6.1 m) from the lip of the Horseshoe Falls at Goat Island. Minutes later, Woodward was plucked from the roiling plunge pool beneath Horseshoe Falls after grabbing a life ring thrown to him by the crew of the Maid of the Mist boat. The children's uncle, Jim Honeycutt, who had been steering the boat, was swept over the edge to his death.
On July 2, 1984, Canadian Karel Soucek from Hamilton, Ontario, plunged over Horseshoe Falls in a barrel with only minor injuries. Soucek was fined $500 for performing the stunt without a license. In 1985, he was fatally injured while attempting to re-create the Niagara drop at the Houston Astrodome. His aim was to climb into a barrel hoisted to the rafters of the Astrodome and to drop 180 ft (55 m) into a water tank on the floor. After his barrel released prematurely, it hit the side of the tank, and he died the next day from his injuries.
In August 1985, Steve Trotter, an aspiring stuntman from Rhode Island, became the youngest person ever (age 22) and the first American in 25 years to go over the falls in a barrel. Ten years later, Trotter went over the falls again, becoming the second person to go over the falls twice and survive. It was also the second "duo"; Lori Martin joined Trotter for the barrel ride over the falls. They survived the fall, but their barrel became stuck at the bottom of the falls, requiring a rescue.
On September 28, 1989, Niagara natives Peter DeBernardi and Jeffery James Petkovich became the first "team" to make it over the falls in a two-person barrel. The stunt was conceived by DeBenardi, who wanted to discourage youth from following in his path of addictive drug use. The pair emerged shortly after going over with minor injuries and were charged with performing an illegal stunt under the Niagara Parks Act.
On June 5, 1990, Jesse Sharp, a whitewater canoeist from Tennessee paddled over the falls in a closed deck canoe. He chose not to wear a helmet to make his face more visible for photographs of the event. He also did not wear a life vest because he believed it would hinder his escape from the hydraulics at the base of the falls. His boat flushed out of the falls, but his body was never found. On September 27, 1993, John "David" Munday, of Caistor Centre, Ontario, completed his second journey over the falls. On October 1, 1995, Robert Douglas "Firecracker" Overacker went over the falls on a Jet Ski to raise awareness for the homeless. His rocket-propelled parachute failed to open and he plunged to his death. Overacker's body was recovered before he was pronounced dead at Niagara General Hospital.
Kirk Jones of Canton, Michigan, became the first known person to survive a plunge over Horseshoe Falls without a flotation device on October 20, 2003. According to some reports, Jones had attempted to commit suicide, but he survived the fall with only battered ribs, scrapes, and bruises. Jones tried going over the falls again in 2017, using a large inflatable ball, but died in the process. Later reports revealed that Jones had arranged for a friend to shoot video clips of his stunt.
On March 11, 2009, a man survived an unprotected trip over Horseshoe Falls. When rescued from the river he suffered from severe hypothermia and a large wound to his head. His identity was never released. Eyewitnesses reported seeing the man intentionally enter the water. On May 21, 2012, an unidentified man became the fourth person to survive an unprotected trip over Horseshoe Falls. Eyewitness reports show he "deliberately jumped" into the Niagara River after climbing over a railing. On July 8, 2019, at roughly 4 am, officers responded to a report of a person in crisis at the brink of the Canadian side of the falls. Once officers got to the scene, the man climbed the retaining wall, jumped into the river and went over Horseshoe Falls. Authorities subsequently began to search the lower Niagara River basin, where the man was found alive but injured sitting on the rocks at the water's edge.
Tightrope walkers
Tightrope walkers drew huge crowds to witness their exploits. Their wires ran across the gorge, near the current Rainbow Bridge, not over the waterfall. Jean François "Blondin" Gravelet was the first to cross Niagara Gorge on June 30, 1859, and did so again eight times that year. His most difficult crossing occurred on August 14, when he carried his manager, Harry Colcord, on his back.[114] His final crossing, on September 8, 1860, was witnessed by the Prince of Wales. Author Ginger Strand argues that these performances may have had symbolic meanings at the time relating to slavery and abolition.
Between 1859 and 1896 a wire-walking craze emerged, resulting in frequent feats over the river below the falls. One inexperienced walker slid down his safety rope. Only one man fell to his death, at night and under mysterious circumstances, at the anchoring place for his wire.
Maria Spelterini, a 23-year-old Italian was the first and only woman to cross the Niagara River gorge; she did so on a tightrope on July 8, 1876. She repeated the stunt several times during the same month. During one crossing she was blindfolded and during another, her ankles and wrists were handcuffed.
Among the many competitors was Ontario's William Hunt, who billed himself as "The Great Farini"; his first crossing was in 1860. Farini competed with Blondin in performing outrageous stunts over the gorge. On August 8, 1864, however, an attempt failed and he needed to be rescued.
On June 15, 2012, high wire artist Nik Wallenda became the first person to walk across the falls area in 116 years, after receiving special permission from both governments. The full length of his tightrope was 1,800 feet (550 m). Wallenda crossed near the brink of Horseshoe Falls, unlike walkers who had crossed farther downstream. According to Wallenda, it was the longest unsupported tightrope walk in history. He carried his passport on the trip and was required to present it upon arrival on the Canadian side of the falls.
Tourism
A ring-billed gull flies by a rainbow over the Horseshoe Falls
Peak visitor traffic occurs in the summertime, when Niagara Falls is both a daytime and evening attraction. From the Canadian side, floodlights illuminate both sides of the falls for several hours after dark (until midnight). The number of visitors in 2007 was expected to total 20 million, and by 2009 the annual rate was expected to top 28 million tourists.
The oldest and best known tourist attraction at Niagara Falls is the Maid of the Mist boat cruise, named for an alleged ancient Ongiara Indian mythical character, which has carried passengers into the rapids immediately below the falls since 1846. Cruise boats operate from boat docks on both sides of the falls, with the Maid of the Mist operating from the American side and Hornblower Cruises (originally Maid of the Mist until 2014) from the Canadian side. In 1996, Native American groups threatened to boycott the boat companies if they would not stop playing what they said was a fake story on their boats. The Maid of the Mist dropped the audio.
From the U.S. side, American Falls can be viewed from walkways along Prospect Point Park, which also features the Prospect Point Observation Tower and a boat dock for the Maid of the Mist. Goat Island offers more views of the falls and is accessible by foot and automobile traffic by bridge above American Falls. From Goat Island, the Cave of the Winds is accessible by elevator and leads hikers to a point beneath Bridal Veil Falls. Also on Goat Island are the Three Sisters Islands, the Power Portal where a statue of Nikola Tesla (the inventor whose patents for the AC induction motor and other devices for AC power transmission helped make the harnessing of the falls possible) can be seen, and a walking path that enables views of the rapids, the Niagara River, the gorge, and all of the falls. Most of these attractions lie within the Niagara Falls State Park.
The Niagara Scenic Trolley offers guided trips along American Falls and around Goat Island. Panoramic and aerial views of the falls can also be viewed by helicopter. The Niagara Gorge Discovery Center showcases the natural and local history of Niagara Falls and the Niagara Gorge. A casino and luxury hotel was opened in Niagara Falls, New York, by the Seneca Indian tribe. The Seneca Niagara Casino & Hotel occupies the former Niagara Falls Convention Center. The new hotel is the first addition to the city's skyline since completion of the United Office Building in the 1920s.
On the Canadian side, Queen Victoria Park features manicured gardens, platforms offering views of American, Bridal Veil, and Horseshoe Falls, and underground walkways leading into observation rooms that yield the illusion of being within the falling waters. Along the Niagara River, the Niagara River Recreational Trail runs 35 mi (56 km) from Fort Erie to Fort George, and includes many historical sites from the War of 1812.
The observation deck of the nearby Skylon Tower offers the highest view of the falls, and in the opposite direction gives views as far as Toronto. Along with the Tower Hotel (built as the Seagrams Tower, later renamed the Heritage Tower, the Royal Inn Tower, the Royal Center Tower, the Panasonic Tower, the Minolta Tower, and most recently the Konica Minolta Tower before receiving its current name in 2010), it is one of two towers in Canada with a view of the falls. The Whirlpool Aero Car, built in 1916 from a design by Spanish engineer Leonardo Torres Quevedo, is a cable car that takes passengers over the Niagara Whirlpool on the Canadian side. The Journey Behind the Falls consists of an observation platform and series of tunnels near the bottom of the Horseshoe Falls on the Canadian side. There are two casinos on the Canadian side of Niagara Falls, the Niagara Fallsview Casino Resort and Casino Niagara.
Touring by helicopter over the falls, from both the US and the Canadian side, was described by The New York Times as still popular a year after a serious crash. Although The New York Times had long before described attempting to tour the falls as "bent on suicide" and despite a number of fatal crashes, the "as many as 100 eight-minute rides each day" are hard to regulate; two countries and various government agencies would have to coordinate. These flights have been available "since the early 1960s."
Niagara Falls is a group of three waterfalls at the southern end of Niagara Gorge, spanning the border between the province of Ontario in Canada and the state of New York in the United States. The largest of the three is Horseshoe Falls, which straddles the international border of the two countries. It is also known as the Canadian Falls. The smaller American Falls and Bridal Veil Falls lie within the United States. Bridal Veil Falls is separated from Horseshoe Falls by Goat Island and from American Falls by Luna Island, with both islands situated in New York.
Formed by the Niagara River, which drains Lake Erie into Lake Ontario, the combined falls have the highest flow rate of any waterfall in North America that has a vertical drop of more than 50 m (160 ft). During peak daytime tourist hours, more than 168,000 m3 (5.9 million cu ft) of water goes over the crest of the falls every minute. Horseshoe Falls is the most powerful waterfall in North America, as measured by flow rate. Niagara Falls is famed for its beauty and is a valuable source of hydroelectric power. Balancing recreational, commercial, and industrial uses has been a challenge for the stewards of the falls since the 19th century.
Niagara Falls is 27 km (17 mi) northwest of Buffalo, New York, and 69 km (43 mi) southeast of Toronto, between the twin cities of Niagara Falls, Ontario, and Niagara Falls, New York. Niagara Falls was formed when glaciers receded at the end of the Wisconsin glaciation (the last ice age), and water from the newly formed Great Lakes carved a path over and through the Niagara Escarpment en route to the Atlantic Ocean.
Horseshoe Falls is about 57 m (187 ft) high, while the height of the American Falls varies between 21 and 30 m (69 and 98 ft) because of the presence of giant boulders at its base. The larger Horseshoe Falls is about 790 m (2,590 ft) wide, while the American Falls is 320 m (1,050 ft) wide. The distance between the American extremity of Niagara Falls and the Canadian extremity is 1,039 m (3,409 ft).
The peak flow over Horseshoe Falls was recorded at 6,370 m3 (225,000 cu ft) per second. The average annual flow rate is 2,400 m3 (85,000 cu ft) per second. Since the flow is a direct function of the Lake Erie water elevation, it typically peaks in late spring or early summer. During the summer months, at least 2,800 m3 (99,000 cu ft) per second of water traverse the falls, some 90% of which goes over Horseshoe Falls, while the balance is diverted to hydroelectric facilities and then on to American Falls and Bridal Veil Falls. This is accomplished by employing a weir – the International Control Dam – with movable gates upstream from Horseshoe Falls.
The water flow is halved at night and during the low tourist season winter months and only attains a minimum flow of 1,400 cubic metres (49,000 cu ft) per second. Water diversion is regulated by the 1950 Niagara Treaty and is administered by the International Niagara Board of Control. The verdant green color of the water flowing over Niagara Falls is a byproduct of the estimated 60 tonnes/minute of dissolved salts and rock flour (very finely ground rock) generated by the erosive force of the Niagara River.
The Niagara River is an Important Bird Area due to its impact on Bonaparte's gulls, ring-billed gulls, and herring gulls. Several thousand birds migrate and winter in the surrounding area.
The features that became Niagara Falls were created by the Wisconsin glaciation about 10,000 years ago. The retreat of the ice sheet left behind a large amount of meltwater (see Lake Algonquin, Lake Chicago, Glacial Lake Iroquois, and Champlain Sea) that filled up the basins that the glaciers had carved, thus creating the Great Lakes as we know them today. Scientists posit there is an old valley, St David's Buried Gorge, buried by glacial drift, at the approximate location of the present Welland Canal.
When the ice melted, the upper Great Lakes emptied into the Niagara River, which followed the rearranged topography across the Niagara Escarpment. In time, the river cut a gorge through the north-facing cliff, or cuesta. Because of the interactions of three major rock formations, the rocky bed did not erode evenly. The caprock formation is composed of hard, erosion-resistant limestone and dolomite of the Lockport Formation (Middle Silurian). That hard layer of stone eroded more slowly than the underlying materials. Immediately below the caprock lies the weaker, softer, sloping Rochester Formation (Lower Silurian). This formation is composed mainly of shale, though it has some thin limestone layers. It also contains ancient fossils. In time, the river eroded the soft layer that supported the hard layers, undercutting the hard caprock, which gave way in great chunks. This process repeated countless times, eventually carving out the falls. Submerged in the river in the lower valley, hidden from view, is the Queenston Formation (Upper Ordovician), which is composed of shales and fine sandstones. All three formations were laid down in an ancient sea, their differences of character deriving from changing conditions within that sea.
About 10,900 years ago, the Niagara Falls was between present-day Queenston, Ontario, and Lewiston, New York, but erosion of the crest caused the falls to retreat approximately 6.8 miles (10.9 km) southward. The shape of Horseshoe Falls has changed through the process of erosion, evolving from a small arch to a horseshoe bend to the present day V-shape. Just upstream from the falls' current location, Goat Island splits the course of the Niagara River, resulting in the separation of Horseshoe Falls to the west from the American and Bridal Veil Falls to the east. Engineering has slowed erosion and recession.
Future of the falls
The current rate of erosion is approximately 30 centimeters (0.98 feet) per year, down from a historical average of 0.91 m (3.0 ft) per year. At this rate, in about 50,000 years Niagara Falls will have eroded the remaining 32 km (20 mi) to Lake Erie, and the falls will cease to exist.
Preservation efforts
In the 1870s, sightseers had limited access to Niagara Falls and often had to pay for a glimpse, and industrialization threatened to carve up Goat Island to further expand commercial development. Other industrial encroachments and lack of public access led to a conservation movement in the U.S. known as Free Niagara, led by such notables as Hudson River School artist Frederic Edwin Church, landscape designer Frederick Law Olmsted, and architect Henry Hobson Richardson. Church approached Lord Dufferin, governor-general of Canada, with a proposal for international discussions on the establishment of a public park.
Goat Island was one of the inspirations for the American side of the effort. William Dorsheimer, moved by the scene from the island, brought Olmsted to Buffalo in 1868 to design a city park system, which helped promote Olmsted's career. In 1879, the New York state legislature commissioned Olmsted and James T. Gardner to survey the falls and to create the single most important document in the Niagara preservation movement, a "Special Report on the preservation of Niagara Falls". The report advocated for state purchase, restoration and preservation through public ownership of the scenic lands surrounding Niagara Falls. Restoring the former beauty of the falls was described in the report as a "sacred obligation to mankind". In 1883, New York Governor Grover Cleveland drafted legislation authorizing acquisition of lands for a state reservation at Niagara, and the Niagara Falls Association, a private citizens group founded in 1882, mounted a great letter-writing campaign and petition drive in support of the park. Professor Charles Eliot Norton and Olmsted were among the leaders of the public campaign, while New York Governor Alonzo Cornell opposed.
Preservationists' efforts were rewarded on April 30, 1885, when Governor David B. Hill signed legislation creating the Niagara Reservation, New York's first state park. New York State began to purchase land from developers, under the charter of the Niagara Reservation State Park. In the same year, the province of Ontario established the Queen Victoria Niagara Falls Park for the same purpose. On the Canadian side, the Niagara Parks Commission governs land usage along the entire course of the Niagara River, from Lake Erie to Lake Ontario.
In 1887, Olmsted and Calvert Vaux issued a supplemental report detailing plans to restore the falls. Their intent was "to restore and conserve the natural surroundings of the Falls of Niagara, rather than to attempt to add anything thereto", and the report anticipated fundamental questions, such as how to provide access without destroying the beauty of the falls, and how to restore natural landscapes damaged by man. They planned a park with scenic roadways, paths and a few shelters designed to protect the landscape while allowing large numbers of visitors to enjoy the falls. Commemorative statues, shops, restaurants, and a 1959 glass and metal observation tower were added later. Preservationists continue to strive to strike a balance between Olmsted's idyllic vision and the realities of administering a popular scenic attraction.
Preservation efforts continued well into the 20th century. J. Horace McFarland, the Sierra Club, and the Appalachian Mountain Club persuaded the United States Congress in 1906 to enact legislation to preserve the falls by regulating the waters of the Niagara River. The act sought, in cooperation with the Canadian government, to restrict diversion of water, and a treaty resulted in 1909 that limited the total amount of water diverted from the falls by both nations to approximately 56,000 cubic feet per second (1,600 m3/s). That limitation remained in effect until 1950.
Erosion control efforts have always been of importance. Underwater weirs redirect the most damaging currents, and the top of the falls has been strengthened. In June 1969, the Niagara River was completely diverted from American Falls for several months through construction of a temporary rock and earth dam. During this time, two bodies were removed from under the falls, including a man who had been seen jumping over the falls, and the body of a woman, which was discovered once the falls dried. While Horseshoe Falls absorbed the extra flow, the U.S. Army Corps of Engineers studied the riverbed and mechanically bolted and strengthened any faults they found; faults that would, if left untreated, have hastened the retreat of American Falls. A plan to remove the huge mound of talus deposited in 1954 was abandoned owing to cost, and in November 1969, the temporary dam was dynamited, restoring flow to American Falls. Even after these undertakings, Luna Island, the small piece of land between the American Falls and Bridal Veil Falls, remained off limits to the public for years owing to fears that it was unstable and could collapse into the gorge.
Commercial interests have continued to encroach on the land surrounding the state park, including the construction of several tall buildings (most of them hotels) on the Canadian side. The result is a significant alteration and urbanisation of the landscape. One study found that the tall buildings changed the breeze patterns and increased the number of mist days from 29 per year to 68 per year, but another study disputed this idea.
In 2013, New York State began an effort to renovate Three Sisters Islands located south of Goat Island. Funds were used from the re-licensing of the New York Power Authority hydroelectric plant downriver in Lewiston, New York, to rebuild walking paths on the Three Sisters Islands and to plant native vegetation on the islands. The state also renovated the area around Prospect Point at the brink of American Falls in the state park.
Toponymy
Theories differ as to the origin of the name of the falls. The Native American word Ongiara means thundering water; The New York Times used this in 1925. According to Iroquoian scholar Bruce Trigger, Niagara is derived from the name given to a branch of the local native Neutral Confederacy, who are described as the Niagagarega people on several late-17th-century French maps of the area. According to George R. Stewart, it comes from the name of an Iroquois town called Onguiaahra, meaning "point of land cut in two". In 1847, an Iroquois interpreter stated that the name came from Jaonniaka-re, meaning "noisy point or portage". To Mohawks, the name refers to "the neck", pronounced "onyara"; the portage or neck of land between lakes Erie and Ontario onyara.
History
Many figures have been suggested as first circulating a European eyewitness description of Niagara Falls. The Frenchman Samuel de Champlain visited the area as early as 1604 during his exploration of what is now Canada, and members of his party reported to him the spectacular waterfalls, which he described in his journals. The first description of the falls is credited to Belgian missionary, Father Louis Hennepin in 1677, after traveling with the explorer René-Robert Cavelier, Sieur de La Salle, thus bringing the falls to the attention of Europeans. French Jesuit missionary Paul Ragueneau likely visited the falls some 35 years before Hennepin's visit while working among the Huron First Nation in Canada. Jean de Brébeuf also may have visited the falls, while spending time with the Neutral Nation. The Finnish-Swedish naturalist Pehr Kalm explored the area in the early 18th century and is credited with the first scientific description of the falls. In 1762, Captain Thomas Davies, a British Army officer and artist, surveyed the area and painted the watercolor, An East View of the Great Cataract of Niagara, the first eyewitness painting of the falls.
During the 19th century, tourism became popular, and by the mid-century, it was the area's main industry. Theodosia Burr Alston (daughter of Vice President Aaron Burr) and her husband Joseph Alston were the first recorded couple to honeymoon there in 1801. Napoleon Bonaparte's brother Jérôme visited with his bride in the early 19th century. In 1825, British explorer John Franklin visited the falls while passing through New York en route to Cumberland House as part of his second Arctic expedition, calling them "so justly celebrated as the first in the world for grandeur".
In 1843, Frederick Douglass joined the American Anti-Slavery Society's "One Hundred Conventions" tour throughout New York and the midwest. Sometime on this tour, Douglass visited Niagara Falls and wrote a brief account of the experience: "When I came into its awful presence the power of discription failed me, an irrisistible power closed my lips." Being on the Canadian border, Niagara Falls was on one of the routes of the Underground Railroad. The falls were also a popular tourist attraction for Southern slaveowners, who would bring their enslaved workers on the trip. "Many a time the trusted body-servant, or slave-girl, would leave master or mistress in the discharge of some errand, and never come back." This sometimes led to conflict. Early town father Peter Porter assisted slavecatchers in finding runaway slaves, even leading, in the case of runaway Solomon Moseby, to a riot in Niagara-on-the-Lake, Canada. Much of this history is memorialized in the Niagara Falls Underground Railroad Heritage Center. After the American Civil War, the New York Central Railroad publicized Niagara Falls as a focus of pleasure and honeymoon visits. After World War II, the auto industry, along with local tourism boards, began to promote Niagara honeymoons.
In about 1840, the English industrial chemist Hugh Lee Pattinson traveled to Canada, stopping at Niagara Falls long enough to make the earliest known photograph of the falls, a daguerreotype in the collection of Newcastle University. It was once believed that the small figure standing silhouetted with a top hat was added by an engraver working from imagination as well as the daguerreotype as his source, but the figure is clearly present in the photograph. Because of the very long exposure required, of ten minutes or more, the figure is assumed by Canada's Niagara Parks agency to be Pattinson. The image is left-right inverted and taken from the Canadian side. Pattinson made other photographs of Horseshoe Falls; these were then transferred to engravings to illustrate Noël Marie Paymal Lerebours' Excursions Daguerriennes (Paris, 1841–1864).[55]
On August 6, 1918, an iron scow became stuck on the rocks above the falls. The two men on the scow were rescued, but the vessel remained trapped on rocks in the river, and is still visible there in a deteriorated state, although its position shifted by 50 meters (160 ft) during a storm on October 31, 2019. Daredevil William "Red" Hill Sr. was particularly praised for his role in the rescue.
After the First World War, tourism boomed as automobiles made getting to the falls much easier. The story of Niagara Falls in the 20th century is largely that of efforts to harness the energy of the falls for hydroelectric power, and to control the development on both sides that threaten the area's natural beauty. Before the late 20th century, the northeastern end of Horseshoe Falls was in the United States, flowing around the Terrapin Rocks, which were once connected to Goat Island by a series of bridges. In 1955, the area between the rocks and Goat Island was filled in, creating Terrapin Point. In the early 1980s, the U.S. Army Corps of Engineers filled in more land and built diversion dams and retaining walls to force the water away from Terrapin Point. Altogether, 400 ft (120 m) of Horseshoe Falls were eliminated, including 100 ft (30 m) on the Canadian side. According to author Ginger Strand, the Horseshoe Falls is now entirely in Canada. Other sources say "most of" Horseshoe Falls is in Canada.
The only recorded freeze-up of the river and falls was caused by an ice jam on March 29, 1848. No water (or at best a trickle) fell for as much as 40 hours. Waterwheels stopped, and mills and factories shut down for having no power. In 1912, American Falls was completely frozen, but the other two falls kept flowing. Although the falls commonly ice up most winters, the river and the falls do not freeze completely. The years 1885, 1902, 1906, 1911, 1932, 1936, 2014, 2017 and 2019 are noted for partial freezing of the falls. A so-called ice bridge was common in certain years at the base of the falls and was used by people who wanted to cross the river before bridges had been built. During some winters, the ice sheet was as thick as 40 to 100 feet (12 to 30 m), but that thickness has not occurred since 1954. The ice bridge of 1841 was said to be at least 100 feet thick. On February 12, 1912, the ice bridge which had formed on January 15 began breaking up while people were still on it. Many escaped, but three died during the event, later named the Ice Bridge Tragedy.
Bridge crossings
A number of bridges have spanned the Niagara River in the general vicinity of the falls. The first, not far from the whirlpool, was a suspension bridge above the gorge. It opened for use by the public in July 1848 and remained in use until 1855. A second bridge in the Upper Falls area was commissioned, with two levels or decks, one for use by the Great Western Railway. This Niagara Falls Suspension Bridge opened in 1855. It was used by conductors on the Underground Railroad to escort runaway slaves to Canada. In 1882, the Grand Trunk Railway took over control of the second deck after it absorbed the Great Western company. Significant structural improvements were made in the late 1870s and then in 1886; this bridge remained in use until 1897.
Because of the volume of traffic, the decision was made to construct a new arch bridge nearby, under and around the existing bridge. After it opened in September 1897, a decision was made to remove and scrap the railway suspension bridge. This new bridge was initially known as the Niagara Railway Arch, or Lower Steel Arch Bridge; it had two decks, the lower one used for carriages and the upper for trains. In 1937, it was renamed the Whirlpool Rapids Bridge and remains in use today. All of the structures built up to that time were referred to as Lower Niagara bridges and were some distance from the falls.
The first bridge in the so-called Upper Niagara area (closer to the falls) was a two-level suspension structure that opened in January 1869; it was destroyed during a severe storm in January 1889. The replacement was built quickly and opened in May 1889. In order to handle heavy traffic, a second bridge was commissioned, slightly closer to American Falls. This one was a steel bridge and opened to traffic in June 1897; it was known as the Upper Steel Arch Bridge but was often called the Honeymoon Bridge. The single level included a track for trolleys and space for carriages and pedestrians. The design led to the bridge being very close to the surface of the river and in January 1938, an ice jam twisted the steel frame of the bridge which later collapsed on January 27, 1938.
Another Lower Niagara bridge had been commissioned in 1883 by Cornelius Vanderbilt for use by railways at a location roughly approximately 200 feet south of the Railway Suspension Bridge. This one was of an entirely different design; it was a cantilever bridge to provide greater strength. The Niagara Cantilever Bridge had two cantilevers which were joined by steel sections; it opened officially in December 1883, and improvements were made over the years for a stronger structure. As rail traffic was increasing, the Michigan Central Railroad company decided to build a new bridge in 1923, to be located between the Lower Steel Arch Bridge and the Cantilever Bridge. The Michigan Central Railway Bridge opened in February 1925 and remained in use until the early 21st century. The Cantilever Bridge was removed and scrapped after the new rail bridge opened. Nonetheless, it was inducted into the North America Railway Hall of Fame in 2006.
There was a lengthy dispute as to which agency should build the replacement for the Niagara Railway Arch, or Lower Steel Arch Bridge in the Upper Niagara area. When that was resolved, construction of a steel bridge commenced in February 1940. Named the Rainbow Bridge, and featuring two lanes for traffic separated by a barrier, it opened in November 1941 and remains in use today.
Industry and commerce
The enormous energy of Niagara Falls has long been recognized as a potential source of power. The first known effort to harness the waters was in 1750, when Daniel Joncaire built a small canal above the falls to power his sawmill. Augustus and Peter Porter purchased this area and all of American Falls in 1805 from the New York state government, and enlarged the original canal to provide hydraulic power for their gristmill and tannery. In 1853, the Niagara Falls Hydraulic Power and Mining Company was chartered, which eventually constructed the canals that would be used to generate electricity. In 1881, under the leadership of Jacob F. Schoellkopf, the Niagara River's first hydroelectric generating station was built. The water fell 86 feet (26 m) and generated direct current electricity, which ran the machinery of local mills and lit up some of the village streets.
The Niagara Falls Power Company, a descendant of Schoellkopf's firm, formed the Cataract Company headed by Edward Dean Adams, with the intent of expanding Niagara Falls' power capacity. In 1890, a five-member International Niagara Commission headed by Sir William Thomson among other distinguished scientists deliberated on the expansion of Niagara hydroelectric capacity based on seventeen proposals but could not select any as the best combined project for hydraulic development and distribution. In 1893, Westinghouse Electric (which had built the smaller-scale Ames Hydroelectric Generating Plant near Ophir, Colorado, two years earlier) was hired to design a system to generate alternating current on Niagara Falls, and three years after that a large-scale AC power system was created (activated on August 26, 1895). The Adams Power Plant Transformer House remains as a landmark of the original system.
By 1896, financing from moguls including J. P. Morgan, John Jacob Astor IV, and the Vanderbilts had fueled the construction of giant underground conduits leading to turbines generating upwards of 100,000 horsepower (75 MW), sent as far as Buffalo, 20 mi (32 km) away. Some of the original designs for the power transmission plants were created by the Swiss firm Faesch & Piccard, which also constructed the original 5,000 hp (3.7 MW) waterwheels. Private companies on the Canadian side also began to harness the energy of the falls. The Government of Ontario eventually brought power transmission operations under public control in 1906, distributing Niagara's energy to various parts of the Canadian province.
Other hydropower plants were being built along the Niagara River. But in 1956, disaster struck when the region's largest hydropower station was partially destroyed in a landslide. This drastically reduced power production and put tens of thousands of manufacturing jobs at stake. In 1957, Congress passed the Niagara Redevelopment Act, which granted the New York Power Authority the right to fully develop the United States' share of the Niagara River's hydroelectric potential.
In 1961, when the Niagara Falls hydroelectric project went online, it was the largest hydropower facility in the Western world. Today, Niagara is still the largest electricity producer in New York state, with a generating capacity of 2.4 GW. Up to 1,420 cubic metres (380,000 US gal) of water per second is diverted from the Niagara River through conduits under the city of Niagara Falls to the Lewiston and Robert Moses power plants. Currently between 50% and 75% of the Niagara River's flow is diverted via four huge tunnels that arise far upstream from the waterfalls. The water then passes through hydroelectric turbines that supply power to nearby areas of Canada and the United States before returning to the river well past the falls. When electrical demand is low, the Lewiston units can operate as pumps to transport water from the lower bay back up to the plant's reservoir, allowing this water to be used again during the daytime when electricity use peaks. During peak electrical demand, the same Lewiston pumps are reversed and become generators.
To preserve Niagara Falls' natural beauty, a 1950 treaty signed by the U.S. and Canada limited water usage by the power plants. The treaty allows higher summertime diversion at night when tourists are fewer and during the winter months when there are even fewer tourists. This treaty, designed to ensure an "unbroken curtain of water" flowing over the falls, states that during daylight time during the tourist season (April 1 to October 31) there must be 100,000 cubic feet per second (2,800 m3/s) of water flowing over the falls, and during the night and off-tourist season there must be 50,000 cubic feet per second (1,400 m3/s) of water flowing over the falls. This treaty is monitored by the International Niagara Board of Control, using a NOAA gauging station above the falls. During winter, the Power Authority of New York works with Ontario Power Generation to prevent ice on the Niagara River from interfering with power production or causing flooding of shoreline property. One of their joint efforts is an 8,800-foot-long (2,700 m) ice boom, which prevents the buildup of ice, yet allows water to continue flowing downstream. In addition to minimum water volume, the crest of Horseshoe falls was reduced to maintain an uninterrupted "curtain of water".
In August 2005, Ontario Power Generation, which is responsible for the Sir Adam Beck stations, started a major civil engineering project, called the Niagara Tunnel Project, to increase power production by building a new 12.7-metre (42 ft) diameter, 10.2-kilometre-long (6.3 mi) water diversion tunnel. It was officially placed into service in March 2013, helping to increase the generating complex's nameplate capacity by 150 megawatts. It did so by tapping water from farther up the Niagara River than was possible with the preexisting arrangement. The tunnel provided new hydroelectricity for approximately 160,000 homes.
Transport
Ships can bypass Niagara Falls by means of the Welland Canal, which was improved and incorporated into the Saint Lawrence Seaway in the mid-1950s. While the seaway diverted water traffic from nearby Buffalo and led to the demise of its steel and grain mills, other industries in the Niagara River valley flourished with the help of the electric power produced by the river. However, since the 1970s the region has declined economically.
The cities of Niagara Falls, Ontario, Canada, and Niagara Falls, New York, United States, are connected by two international bridges. The Rainbow Bridge, just downriver from the falls, affords the closest view of the falls and is open to non-commercial vehicle traffic and pedestrians. The Whirlpool Rapids Bridge lies one mile (1.6 km) north of the Rainbow Bridge and is the oldest bridge over the Niagara River. Nearby Niagara Falls International Airport and Buffalo Niagara International Airport were named after the waterfall, as were Niagara University, countless local businesses, and even an asteroid.
Over the falls
The first recorded publicity stunt using the Falls was the wreck of the schooner Michigan in 1827. Local hotel owners acquired a former Lake Erie freighter, loaded it with animals and effigies of people, towed it to a spot above the falls and let it plunge over the brink. Admission of fifty cents was charged.
In October 1829, Sam Patch, who called himself "the Yankee Leapster", jumped from a high tower into the gorge below the falls and survived; this began a long tradition of daredevils trying to go over the falls. Englishman Captain Matthew Webb, the first man to swim the English Channel, drowned in 1883 trying to swim the rapids downriver from the falls.
On October 24, 1901, 63-year-old Michigan school teacher Annie Edson Taylor became the first person to go over the falls in a barrel as a publicity stunt; she survived, bleeding, but otherwise unharmed. Soon after exiting the barrel, she said, "No one ought ever do that again." Days before Taylor's attempt, her domestic cat was sent over the falls in her barrel to test its strength. The cat survived the plunge unharmed and later posed with Taylor in photographs. Since Taylor's historic ride, over a dozen people have intentionally gone over the falls in or on a device, despite her advice. Some have survived unharmed, but others have drowned or been severely injured. Survivors face charges and stiff fines, as it is now illegal, on both sides of the border, to attempt to go over the falls. Charles Stephens, a 58-year-old barber from Bristol, England, went over the falls in a wooden barrel in July 1920 and was the first person to die in an endeavor of this type. Bobby Leach went over Horseshoe Falls in a crude steel barrel in 1911 and needed rescuing by William "Red" Hill Sr. Hill again came to the rescue of Leach following his failed attempt to swim the Niagara Gorge in 1920. In 1928, "Smiling Jean" Lussier tried an entirely different concept, going over the falls in a large rubber ball; he was successful and survived the ordeal.
Annie Edson Taylor posing with her wooden barrel (1901)
In the "Miracle at Niagara", on July 9, 1960, Roger Woodward, a seven-year-old American boy, was swept over Horseshoe Falls after the boat in which he was cruising lost power; two tourists pulled his 17-year-old sister Deanne from the river only 20 ft (6.1 m) from the lip of the Horseshoe Falls at Goat Island. Minutes later, Woodward was plucked from the roiling plunge pool beneath Horseshoe Falls after grabbing a life ring thrown to him by the crew of the Maid of the Mist boat. The children's uncle, Jim Honeycutt, who had been steering the boat, was swept over the edge to his death.
On July 2, 1984, Canadian Karel Soucek from Hamilton, Ontario, plunged over Horseshoe Falls in a barrel with only minor injuries. Soucek was fined $500 for performing the stunt without a license. In 1985, he was fatally injured while attempting to re-create the Niagara drop at the Houston Astrodome. His aim was to climb into a barrel hoisted to the rafters of the Astrodome and to drop 180 ft (55 m) into a water tank on the floor. After his barrel released prematurely, it hit the side of the tank, and he died the next day from his injuries.
In August 1985, Steve Trotter, an aspiring stuntman from Rhode Island, became the youngest person ever (age 22) and the first American in 25 years to go over the falls in a barrel. Ten years later, Trotter went over the falls again, becoming the second person to go over the falls twice and survive. It was also the second "duo"; Lori Martin joined Trotter for the barrel ride over the falls. They survived the fall, but their barrel became stuck at the bottom of the falls, requiring a rescue.
On September 28, 1989, Niagara natives Peter DeBernardi and Jeffery James Petkovich became the first "team" to make it over the falls in a two-person barrel. The stunt was conceived by DeBenardi, who wanted to discourage youth from following in his path of addictive drug use. The pair emerged shortly after going over with minor injuries and were charged with performing an illegal stunt under the Niagara Parks Act.
On June 5, 1990, Jesse Sharp, a whitewater canoeist from Tennessee paddled over the falls in a closed deck canoe. He chose not to wear a helmet to make his face more visible for photographs of the event. He also did not wear a life vest because he believed it would hinder his escape from the hydraulics at the base of the falls. His boat flushed out of the falls, but his body was never found. On September 27, 1993, John "David" Munday, of Caistor Centre, Ontario, completed his second journey over the falls. On October 1, 1995, Robert Douglas "Firecracker" Overacker went over the falls on a Jet Ski to raise awareness for the homeless. His rocket-propelled parachute failed to open and he plunged to his death. Overacker's body was recovered before he was pronounced dead at Niagara General Hospital.
Kirk Jones of Canton, Michigan, became the first known person to survive a plunge over Horseshoe Falls without a flotation device on October 20, 2003. According to some reports, Jones had attempted to commit suicide, but he survived the fall with only battered ribs, scrapes, and bruises. Jones tried going over the falls again in 2017, using a large inflatable ball, but died in the process. Later reports revealed that Jones had arranged for a friend to shoot video clips of his stunt.
On March 11, 2009, a man survived an unprotected trip over Horseshoe Falls. When rescued from the river he suffered from severe hypothermia and a large wound to his head. His identity was never released. Eyewitnesses reported seeing the man intentionally enter the water. On May 21, 2012, an unidentified man became the fourth person to survive an unprotected trip over Horseshoe Falls. Eyewitness reports show he "deliberately jumped" into the Niagara River after climbing over a railing. On July 8, 2019, at roughly 4 am, officers responded to a report of a person in crisis at the brink of the Canadian side of the falls. Once officers got to the scene, the man climbed the retaining wall, jumped into the river and went over Horseshoe Falls. Authorities subsequently began to search the lower Niagara River basin, where the man was found alive but injured sitting on the rocks at the water's edge.
Tightrope walkers
Tightrope walkers drew huge crowds to witness their exploits. Their wires ran across the gorge, near the current Rainbow Bridge, not over the waterfall. Jean François "Blondin" Gravelet was the first to cross Niagara Gorge on June 30, 1859, and did so again eight times that year. His most difficult crossing occurred on August 14, when he carried his manager, Harry Colcord, on his back.[114] His final crossing, on September 8, 1860, was witnessed by the Prince of Wales. Author Ginger Strand argues that these performances may have had symbolic meanings at the time relating to slavery and abolition.
Between 1859 and 1896 a wire-walking craze emerged, resulting in frequent feats over the river below the falls. One inexperienced walker slid down his safety rope. Only one man fell to his death, at night and under mysterious circumstances, at the anchoring place for his wire.
Maria Spelterini, a 23-year-old Italian was the first and only woman to cross the Niagara River gorge; she did so on a tightrope on July 8, 1876. She repeated the stunt several times during the same month. During one crossing she was blindfolded and during another, her ankles and wrists were handcuffed.
Among the many competitors was Ontario's William Hunt, who billed himself as "The Great Farini"; his first crossing was in 1860. Farini competed with Blondin in performing outrageous stunts over the gorge. On August 8, 1864, however, an attempt failed and he needed to be rescued.
On June 15, 2012, high wire artist Nik Wallenda became the first person to walk across the falls area in 116 years, after receiving special permission from both governments. The full length of his tightrope was 1,800 feet (550 m). Wallenda crossed near the brink of Horseshoe Falls, unlike walkers who had crossed farther downstream. According to Wallenda, it was the longest unsupported tightrope walk in history. He carried his passport on the trip and was required to present it upon arrival on the Canadian side of the falls.
Tourism
A ring-billed gull flies by a rainbow over the Horseshoe Falls
Peak visitor traffic occurs in the summertime, when Niagara Falls is both a daytime and evening attraction. From the Canadian side, floodlights illuminate both sides of the falls for several hours after dark (until midnight). The number of visitors in 2007 was expected to total 20 million, and by 2009 the annual rate was expected to top 28 million tourists.
The oldest and best known tourist attraction at Niagara Falls is the Maid of the Mist boat cruise, named for an alleged ancient Ongiara Indian mythical character, which has carried passengers into the rapids immediately below the falls since 1846. Cruise boats operate from boat docks on both sides of the falls, with the Maid of the Mist operating from the American side and Hornblower Cruises (originally Maid of the Mist until 2014) from the Canadian side. In 1996, Native American groups threatened to boycott the boat companies if they would not stop playing what they said was a fake story on their boats. The Maid of the Mist dropped the audio.
From the U.S. side, American Falls can be viewed from walkways along Prospect Point Park, which also features the Prospect Point Observation Tower and a boat dock for the Maid of the Mist. Goat Island offers more views of the falls and is accessible by foot and automobile traffic by bridge above American Falls. From Goat Island, the Cave of the Winds is accessible by elevator and leads hikers to a point beneath Bridal Veil Falls. Also on Goat Island are the Three Sisters Islands, the Power Portal where a statue of Nikola Tesla (the inventor whose patents for the AC induction motor and other devices for AC power transmission helped make the harnessing of the falls possible) can be seen, and a walking path that enables views of the rapids, the Niagara River, the gorge, and all of the falls. Most of these attractions lie within the Niagara Falls State Park.
The Niagara Scenic Trolley offers guided trips along American Falls and around Goat Island. Panoramic and aerial views of the falls can also be viewed by helicopter. The Niagara Gorge Discovery Center showcases the natural and local history of Niagara Falls and the Niagara Gorge. A casino and luxury hotel was opened in Niagara Falls, New York, by the Seneca Indian tribe. The Seneca Niagara Casino & Hotel occupies the former Niagara Falls Convention Center. The new hotel is the first addition to the city's skyline since completion of the United Office Building in the 1920s.
On the Canadian side, Queen Victoria Park features manicured gardens, platforms offering views of American, Bridal Veil, and Horseshoe Falls, and underground walkways leading into observation rooms that yield the illusion of being within the falling waters. Along the Niagara River, the Niagara River Recreational Trail runs 35 mi (56 km) from Fort Erie to Fort George, and includes many historical sites from the War of 1812.
The observation deck of the nearby Skylon Tower offers the highest view of the falls, and in the opposite direction gives views as far as Toronto. Along with the Tower Hotel (built as the Seagrams Tower, later renamed the Heritage Tower, the Royal Inn Tower, the Royal Center Tower, the Panasonic Tower, the Minolta Tower, and most recently the Konica Minolta Tower before receiving its current name in 2010), it is one of two towers in Canada with a view of the falls. The Whirlpool Aero Car, built in 1916 from a design by Spanish engineer Leonardo Torres Quevedo, is a cable car that takes passengers over the Niagara Whirlpool on the Canadian side. The Journey Behind the Falls consists of an observation platform and series of tunnels near the bottom of the Horseshoe Falls on the Canadian side. There are two casinos on the Canadian side of Niagara Falls, the Niagara Fallsview Casino Resort and Casino Niagara.
Touring by helicopter over the falls, from both the US and the Canadian side, was described by The New York Times as still popular a year after a serious crash. Although The New York Times had long before described attempting to tour the falls as "bent on suicide" and despite a number of fatal crashes, the "as many as 100 eight-minute rides each day" are hard to regulate; two countries and various government agencies would have to coordinate. These flights have been available "since the early 1960s."
Surf 2024, Luke took a private lesson this time. I am impressed, since this would scare me! He is getting the hang of it, I would be using it as a flotation device!
COLIJN, dr A.H. (1937). Naar de eeuwige sneeuw van tropisch Nederland. De bestijging van het Carstenszgebergte in Nederlandsch Nieuw Guinee. Scheltens & Giltay, Amsterdam.
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Puncak Jaya (Carstensz Pyramid (4,884 m [16,024 ft]) is the highest summit of Mount Jayawijaya or Mount Carstensz in the Sudirman Range of the western central highlands of Papua Province, Indonesia (within Puncak Jaya Regency). Other summits are East Carstensz Peak (4,808 m [15,774 ft]), Sumantri (4,870 m [15,980 ft]) and Ngga Pulu (4,863 m [15,955 ft]). Other names include Nemangkawi in the Amungkal language, Carstensz Toppen and Gunung Soekarno.
At 4,884 metres (16,024 ft) above sea level, Puncak Jaya is the highest mountain in Indonesia, on the island of New Guinea (which consists of West Papua province in Indonesia plus Papua New Guinea), on the continent of Australia (which consists of New Guinea, the Australian Mainland, Tasmania, other islands, and the submerged continental shelf), and in Oceania, the tallest island mountain on Earth, as well as the 5th highest mountain in political Southeast Asia.
It is also the highest point between the Himalayas and the Andes. Some sources claim Papua New Guinea's Mount Wilhelm, 4,509 m (14,793 ft), as the highest mountain peak in Oceania, on account of Indonesia being part of Asia (Southeast Asia). The massive, open cut Grasberg mine is within 4 km (2.5 mi) of Puncak Jaya.
The highlands surrounding the peak were inhabited before European contact, and the peak was known as Nemangkawi in Amungkal. Puncak Jaya was named "Carstensz Pyramid" after Dutch explorer Jan Carstenszoon who first sighted the glaciers on the peak of the mountain on a rare clear day in 1623. The sighting went unverified for over two centuries, and Carstensz was ridiculed in Europe when he said he had seen snow near the equator.
The snowfield of Puncak Jaya was reached as early as 1909 by a Dutch explorer, Hendrik Albert Lorentz with six of his Dayak Kenyah porters recruited from the Apo Kayan in Borneo. The predecessor of the Lorentz National Park, which encompasses the Carstensz Range, was established in 1919 following the report of this expedition.
In 1936 the Dutch Carstensz Expedition, unable to establish definitively which of the three summits was the highest, attempted to climb each. Anton Colijn, Jean Jacques Dozy and Frits Wissel reached both the glacier-covered East Carstensz and Ngga Pulu summits on December 5, but through bad weather failed in their attempts to climb the bare Carstensz Pyramid. Because of extensive snow melt Ngga Pulu has become a 4,862 m (15,951 ft) subsidiary peak, but it has been estimated that in 1936 (when glaciers still covered 13 km2 (5.0 sq mi) of the mountain; see map) Ngga Pulu was indeed the highest summit, reaching over 4,900 m (16,100 ft).
The now-highest Carstensz Pyramid summit was not climbed until 1962, by an expedition led by the Austrian mountaineer Heinrich Harrer (of Seven Years in Tibet fame, and climber of the Eiger North Face) with three other expedition members – the New Zealand mountaineer Philip Temple, the Australian rock climber Russell Kippax, and the Dutch patrol officer Albertus (Bert) Huizenga. Temple had previously led an expedition into the area and pioneered the access route to the mountains.
When Indonesia took control of the province in 1963, the peak was renamed 'Poentja Soekarno' (Simplified Indonesian: Puncak Sukarno) or Sukarno Peak, after the first President of Indonesia; later this was changed to Puncak Jaya. Puncak means peak or mountain and Jaya means 'victory', 'victorious' or 'glorious'. The name Carstensz Pyramid is still used among mountaineers.
Geology
Puncak Jaya is the highest point on the central range, which was created in the late Miocene Melanesian orogeny, caused by oblique collision between the Australian and Pacific plates and is made of middle Miocene limestones.
Access to the peak requires a government permit. The mountain was closed to tourists and climbers between 1995 and 2005. As of 2006, access is possible through various adventure tourism agencies (Wikipedia).
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The Grasberg mine is the largest gold mine and the second largest copper mine in the world. It is located in the province of Papua in Indonesia near Puncak Jaya, the highest mountain in Papua. It has 19,500 employees. It is mostly owned by Freeport-McMoRan (FCX), which owns 48.74% of PT Freeport Indonesia (PT-FI), the principal operating subsidiary in Indonesia, including 9.36% owned through its wholly owned subsidiary, PT Indocopper Investama. The government of Indonesia owns 51.23% of PT Freeport Indonesia through Indonesia Asahan Aluminium.
FCX operates under a Contract of Work (CoW) agreement with the government of Indonesia, which allows Freeport to conduct exploration, mining and production activities in a 11,100-hectare (27,400-acre) area (Block A). It also conducts exploration activities in a 167,000 ha (413,000 acres) area (Block B). All of Freeport's proven and probable mineral reserves and current mining operations are located in Block A. The mine has three mining operations: the open pit, the Deep Ore Zone underground mine, and the Big Gossan underground mine. A fourth, the Deep Mill Level Zone, is being developed. The 2016 production was 482,000,000 kilograms (1,063,000,000 lb) of copper, 33,000,000 grams (1,061,000 ozt) of gold; and in 2016 sales of 90,000,000 grams (2,900,000 ozt) of silver.
In August 2017, FCX announced that it will divest its ownership in PT-FI so that Indonesia owns 51%. In return the CoW will be replaced by a special license (IUPK) with mining rights to 2041 and FCX will build a new smelter by 2022.
In 1936, Dutch geologist Jean Jacques Dozy was a member of an expedition that scaled Mount Carstensz, the highest mountain in the Dutch East Indies. While there, he made notes of a peculiar black rock with greenish coloring, and spent several weeks estimating the extent of the gold and copper deposits. In 1939, he filed a report about the Ertsberg (Dutch for "ore mountain"). He was working for Nederlandsche Nieuw Guinea Petroleum Maatschappij (NNGPM), an exploration company formed by Shell in 1935, with 40% Standard Vacuum Oil Company interest and 20% Far Pacific investments (Chevron subsidiary).
In March 1959, the New York Times published an article revealing the Dutch were searching for the mountain source of alluvial gold which had been flowing into the Arafura Sea. Geologist Forbes Wilson, working for the Freeport mining company in August 1959 after reading Dozy's 1936 report, immediately prepared to explore the Ertsberg site. In 1960 the expedition, led by Forbes Wilson and President of Freeport McMoRan Copper and Gold-George Mealey, confirmed the huge copper deposits at the Ertsberg. It was financed by Freeport Sulphur, whose directors included Godfrey Rockefeller, Texaco chairman Augustus Long, George Mealey, and Robert Lovett.
In 1963 the administration of Dutch New Guinea was transferred to Indonesia, and the mine was the first under the new Suharto administration's 1967 foreign investment laws intended to attract foreign investment to Indonesia's then ruined economy. Built at 4,100 metres (14,000 ft) above sea level in one of West Papua's most remote areas, it involved a capital and technology input well beyond Indonesia's resources at the time. Construction cost was $175 million, $55 million above the original budget. A 116 km road and pipeline, port, airstrip, power plant and a new town called "Tembagapura" (literally: copper town) were built. It officially opened in 1973 (although the first ore shipment was in December 1972), and was expanded by Ertsberg East, which opened in 1981. Steep aerial tramways are used to transport equipment and people. Ore is dropped 600 metres (2,000 ft) from the mine, concentrated and mixed with water to form a 60:40 slurry. The slurry is then pumped through a 166 km pipeline through mountains, jungle and swamp to the port at Amamapare, dried and shipped. Each tonne of dry concentrate contains 317 kilograms of copper, 30 grams of gold and 30 grams of silver.
In 1977 the rebel group Free Papua Movement attacked the mine. The group dynamited the main slurry pipe, which caused tens of millions of dollars in damage, and attacked the mine facilities. The Indonesian military reacted harshly, killing at least 800 people.
By the mid-1980s, the original mine had been largely depleted. Freeport explored for other deposits in the area. In 1988, Freeport identified reserves valued at $40 billion at Grasberg (Dutch, "Grass Mountain"), just 3 kilometres (1.9 miles) from the Ertsberg mine. The winding road to Grasberg, the H.E.A.T. (Heavy Equipment Access Trail), was estimated to require $12 million to $15 million to be built. An Indonesian road-builder who had contributed to the Ertsberg road took a bulldozer and drove it downhill sketching the path. The road cost just $2 million when completed.
The 2003–2006 boom in copper prices increased the profitability of the mine. The extra consumption of copper for Asian electrical infrastructure overwhelmed copper supply and caused prices to increase from around $1500/ton to $8100/ton ($0.70/lb to $4.00/lb).
In 2005, the New York Times reported that between 1998 and 2004 Freeport had given senior military and police officers and military units nearly $20 million.
Mine workings
The Grasberg Mine complex from space in 2005. Puncak Jaya is the high point of the snow-covered ridge to the east of the mine. The peak is at 4,884 metres (16,024 ft) above sea level. The rim of the open pit is at about 4,270 metres (14,010 ft).
The workings include a very large open pit mine, an underground mine and four concentrators. The open pit mine – which forms a mile-wide crater at the surface – is a high-volume, low-cost operation, producing more than 67 million tonnes of ore and providing over 75% of the mill feed in 2006.
Ore undergoes primary crushing at the mine, before being delivered by ore passes to the mill complex for further crushing, grinding and flotation. Grasberg's milling and concentrating complex is the largest in the world, with four crushers and two giant semi-autogenous grinding (SAG) units processing a daily average of 240,000 metric tonnes of ore in 2006.
A flotation reagent is used to separate a copper-gold concentrate from the ore. Slurry containing the copper-gold concentrate is delivered by three pipelines to the seaport of Amamapare, over 70 miles away, where it is dewatered. Once filtered and dried, the concentrate – containing copper, gold and silver – is shipped to smelters around the world.
The facilities at the port also include a coal-fired power station, which supplies the Grasberg operations.
The concentrator's tailings, generated at a rate of 700,000 tonnes per day, are the subject of considerable environmental concern, as they wash into the Aikwa riverine system and Arafura Sea. Some 130 square kilometres (50 sq mi) (eventually 230 square kilometres (89 sq mi)) of lowland areas along the Aikwa River, are covered by braided sedimentary channels indicative of high sediment load (similar to glacial runoff). Native fish have nearly disappeared from now-turbid waters of the Aikwa River which are unsuitable for aquatic life. The overburden (700 kt/d) remains in the highlands, up to 480 m deep and covering 8 square kilometres (3 sq mi). Its acidic runoff, dissolved copper, and the finer material gets washed into the headwaters of the Wanagon River. It settles out along the river course and then into the ocean, and will continue to do so indefinitely. Freeport's official response is that overburden is placed in the highlands as part of its Overburden Management Plan, at "sites capped with limestone and constantly monitored. Tailings are transported to the lowlands in a designated river system. Once reaching the lowlands, they are captured in an engineered system of levees built for that purpose." An Indonesian Environment Ministry's field report in 2004, found levels of sediment 37,500 milligrams per litre as the river entered the lowlands and 7,500 milligrams as the river entered the Arafura Sea, while the maximum under Indonesian law is not to exceed 400 milligrams per litre.
In 1995, the Overseas Private Investment Corporation (OPIC) revoked Freeport's insurance policy for environmental violations of a sort that would not be allowed in the US. It was the first action of this sort by OPIC, and Freeport responded with a lawsuit against them. Freeport said an environmental report reached inaccurate conclusions, the result of a single 1994 visit to Grasberg. The company later underwent an independent environmental audit by Dames & Moore and passed. In April 1996, Freeport canceled its policy with the OPIC, stating that their corporate activities had outgrown the policy's limits. However, the OPIC report was later publicly released.
Environmental damage
The mine is located within what used to be a small equatorial mountain glacier. Steepening of slopes related to mining activities, as well as earthquakes and frequent heavy rainfall, have resulted in landslides within the open pit mine.
While landscape reclamation projects have begun at the mine, environmental groups and local citizens are concerned with the potential for copper contamination and acid mine drainage from the mine tailings into surrounding river systems, land surfaces, and groundwater. Freeport argues that its actions meet industry standards and have been approved by the requisite authorities. It was reported in 2005 that since 1997 Freeport had been breaching Indonesian environmental laws. Freeport estimates it will generate six billion tons of waste.
Both Freeport and its partner Rio Tinto have been excluded from the investment portfolio of The Government Pension Fund of Norway, the world's second-largest pension fund, due to criticism over the environmental damages caused by the Grasberg mine. Stocks at a value of ca. US$870 million were divested from the fund as a result of the decisions.
Attacks on the mine
Violent ambushes near the Grasberg mine have occurred as early as August 2002, when three contract school teachers were killed. Kopassus, the Indonesian Special Forces, allegedly instigated the incident.
A series of attacks started on 11 July 2009, and continued for more than five days. A Freeport employee, 29-year-old Australian Drew Grant was shot and killed while sitting in the back of a car on the way to a game of golf. Indonesian police indicated that Grant was killed by five shots he sustained to the neck, chest and stomach by unknown assailants using military-issue weapons. The attack also killed Freeport security guard Markus Ratealo and a number of police officers.
On 7 April 2011, two Freeport employees were killed when the company car they were traveling in caught fire. Bullets were found inside the car, giving weight to the suspicion that the car was fired on by unknown gunmen. This incident sparked a protest by hundreds of Freeport employees concerned about the security along the jungle road leading up to the mine.
The Grasberg mine has been a frequent source of friction in Papua. Possible causes of friction are the mine's environmental impact on Papua, the perceived low share of profits going to local Papuans (Freeport's annual report shows it made $4.1billion in operating profit on revenue of $6.4billion in 2010) and the questionable legality of the payments made to Indonesian security forces for their services to guard the site.
Accidents and incidents
On May 14, 2013, a training facility tunnel collapsed trapping at least 33 workers underground. A mine official at the mine said three workers were killed, but the main office in Arizona said there were no fatalities. As of 20 May, 10 miners were rescued and 14 bodies were recovered bringing the total deaths to 17. Eleven other men are believed to be buried under the rubble (Wikipedia).
By the side of the pond in Gordon Gardens, Gravesend: a lifebelt and its rope. Both made of plastic(s) - nylon or polypropelene, synthetic fibre in the case of the personal flotation device. Plastic is (or can be) a synthetic fibre, probberly. A personal floatation device is a lifebelt...blah blah blah.
[DSC_7444a]
Someone mentioned a news item that Mariah Carey (the mostly almost undressed singer) needed 20 suitcases for a 3-day trip. Not sure what they carried. Here's a catamaran (sailboat) called Mariah that can carry Mariah Carey and 20 suitcases (whose extra large boobs can provide flotation in case of capsizing).
Shot from my 37th floor balcony in Singer Island (Palm Beaches) Florida with a 5MP Nikon 5700.
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Niagara Falls is a group of three waterfalls at the southern end of Niagara Gorge, spanning the border between the province of Ontario in Canada and the state of New York in the United States. The largest of the three is Horseshoe Falls, which straddles the international border of the two countries. It is also known as the Canadian Falls. The smaller American Falls and Bridal Veil Falls lie within the United States. Bridal Veil Falls is separated from Horseshoe Falls by Goat Island and from American Falls by Luna Island, with both islands situated in New York.
Formed by the Niagara River, which drains Lake Erie into Lake Ontario, the combined falls have the highest flow rate of any waterfall in North America that has a vertical drop of more than 50 m (160 ft). During peak daytime tourist hours, more than 168,000 m3 (5.9 million cu ft) of water goes over the crest of the falls every minute. Horseshoe Falls is the most powerful waterfall in North America, as measured by flow rate. Niagara Falls is famed for its beauty and is a valuable source of hydroelectric power. Balancing recreational, commercial, and industrial uses has been a challenge for the stewards of the falls since the 19th century.
Niagara Falls is 27 km (17 mi) northwest of Buffalo, New York, and 69 km (43 mi) southeast of Toronto, between the twin cities of Niagara Falls, Ontario, and Niagara Falls, New York. Niagara Falls was formed when glaciers receded at the end of the Wisconsin glaciation (the last ice age), and water from the newly formed Great Lakes carved a path over and through the Niagara Escarpment en route to the Atlantic Ocean.
Horseshoe Falls is about 57 m (187 ft) high, while the height of the American Falls varies between 21 and 30 m (69 and 98 ft) because of the presence of giant boulders at its base. The larger Horseshoe Falls is about 790 m (2,590 ft) wide, while the American Falls is 320 m (1,050 ft) wide. The distance between the American extremity of Niagara Falls and the Canadian extremity is 1,039 m (3,409 ft).
The peak flow over Horseshoe Falls was recorded at 6,370 m3 (225,000 cu ft) per second. The average annual flow rate is 2,400 m3 (85,000 cu ft) per second. Since the flow is a direct function of the Lake Erie water elevation, it typically peaks in late spring or early summer. During the summer months, at least 2,800 m3 (99,000 cu ft) per second of water traverse the falls, some 90% of which goes over Horseshoe Falls, while the balance is diverted to hydroelectric facilities and then on to American Falls and Bridal Veil Falls. This is accomplished by employing a weir – the International Control Dam – with movable gates upstream from Horseshoe Falls.
The water flow is halved at night and during the low tourist season winter months and only attains a minimum flow of 1,400 cubic metres (49,000 cu ft) per second. Water diversion is regulated by the 1950 Niagara Treaty and is administered by the International Niagara Board of Control. The verdant green color of the water flowing over Niagara Falls is a byproduct of the estimated 60 tonnes/minute of dissolved salts and rock flour (very finely ground rock) generated by the erosive force of the Niagara River.
The Niagara River is an Important Bird Area due to its impact on Bonaparte's gulls, ring-billed gulls, and herring gulls. Several thousand birds migrate and winter in the surrounding area.
The features that became Niagara Falls were created by the Wisconsin glaciation about 10,000 years ago. The retreat of the ice sheet left behind a large amount of meltwater (see Lake Algonquin, Lake Chicago, Glacial Lake Iroquois, and Champlain Sea) that filled up the basins that the glaciers had carved, thus creating the Great Lakes as we know them today. Scientists posit there is an old valley, St David's Buried Gorge, buried by glacial drift, at the approximate location of the present Welland Canal.
When the ice melted, the upper Great Lakes emptied into the Niagara River, which followed the rearranged topography across the Niagara Escarpment. In time, the river cut a gorge through the north-facing cliff, or cuesta. Because of the interactions of three major rock formations, the rocky bed did not erode evenly. The caprock formation is composed of hard, erosion-resistant limestone and dolomite of the Lockport Formation (Middle Silurian). That hard layer of stone eroded more slowly than the underlying materials. Immediately below the caprock lies the weaker, softer, sloping Rochester Formation (Lower Silurian). This formation is composed mainly of shale, though it has some thin limestone layers. It also contains ancient fossils. In time, the river eroded the soft layer that supported the hard layers, undercutting the hard caprock, which gave way in great chunks. This process repeated countless times, eventually carving out the falls. Submerged in the river in the lower valley, hidden from view, is the Queenston Formation (Upper Ordovician), which is composed of shales and fine sandstones. All three formations were laid down in an ancient sea, their differences of character deriving from changing conditions within that sea.
About 10,900 years ago, the Niagara Falls was between present-day Queenston, Ontario, and Lewiston, New York, but erosion of the crest caused the falls to retreat approximately 6.8 miles (10.9 km) southward. The shape of Horseshoe Falls has changed through the process of erosion, evolving from a small arch to a horseshoe bend to the present day V-shape. Just upstream from the falls' current location, Goat Island splits the course of the Niagara River, resulting in the separation of Horseshoe Falls to the west from the American and Bridal Veil Falls to the east. Engineering has slowed erosion and recession.
Future of the falls
The current rate of erosion is approximately 30 centimeters (0.98 feet) per year, down from a historical average of 0.91 m (3.0 ft) per year. At this rate, in about 50,000 years Niagara Falls will have eroded the remaining 32 km (20 mi) to Lake Erie, and the falls will cease to exist.
Preservation efforts
In the 1870s, sightseers had limited access to Niagara Falls and often had to pay for a glimpse, and industrialization threatened to carve up Goat Island to further expand commercial development. Other industrial encroachments and lack of public access led to a conservation movement in the U.S. known as Free Niagara, led by such notables as Hudson River School artist Frederic Edwin Church, landscape designer Frederick Law Olmsted, and architect Henry Hobson Richardson. Church approached Lord Dufferin, governor-general of Canada, with a proposal for international discussions on the establishment of a public park.
Goat Island was one of the inspirations for the American side of the effort. William Dorsheimer, moved by the scene from the island, brought Olmsted to Buffalo in 1868 to design a city park system, which helped promote Olmsted's career. In 1879, the New York state legislature commissioned Olmsted and James T. Gardner to survey the falls and to create the single most important document in the Niagara preservation movement, a "Special Report on the preservation of Niagara Falls". The report advocated for state purchase, restoration and preservation through public ownership of the scenic lands surrounding Niagara Falls. Restoring the former beauty of the falls was described in the report as a "sacred obligation to mankind". In 1883, New York Governor Grover Cleveland drafted legislation authorizing acquisition of lands for a state reservation at Niagara, and the Niagara Falls Association, a private citizens group founded in 1882, mounted a great letter-writing campaign and petition drive in support of the park. Professor Charles Eliot Norton and Olmsted were among the leaders of the public campaign, while New York Governor Alonzo Cornell opposed.
Preservationists' efforts were rewarded on April 30, 1885, when Governor David B. Hill signed legislation creating the Niagara Reservation, New York's first state park. New York State began to purchase land from developers, under the charter of the Niagara Reservation State Park. In the same year, the province of Ontario established the Queen Victoria Niagara Falls Park for the same purpose. On the Canadian side, the Niagara Parks Commission governs land usage along the entire course of the Niagara River, from Lake Erie to Lake Ontario.
In 1887, Olmsted and Calvert Vaux issued a supplemental report detailing plans to restore the falls. Their intent was "to restore and conserve the natural surroundings of the Falls of Niagara, rather than to attempt to add anything thereto", and the report anticipated fundamental questions, such as how to provide access without destroying the beauty of the falls, and how to restore natural landscapes damaged by man. They planned a park with scenic roadways, paths and a few shelters designed to protect the landscape while allowing large numbers of visitors to enjoy the falls. Commemorative statues, shops, restaurants, and a 1959 glass and metal observation tower were added later. Preservationists continue to strive to strike a balance between Olmsted's idyllic vision and the realities of administering a popular scenic attraction.
Preservation efforts continued well into the 20th century. J. Horace McFarland, the Sierra Club, and the Appalachian Mountain Club persuaded the United States Congress in 1906 to enact legislation to preserve the falls by regulating the waters of the Niagara River. The act sought, in cooperation with the Canadian government, to restrict diversion of water, and a treaty resulted in 1909 that limited the total amount of water diverted from the falls by both nations to approximately 56,000 cubic feet per second (1,600 m3/s). That limitation remained in effect until 1950.
Erosion control efforts have always been of importance. Underwater weirs redirect the most damaging currents, and the top of the falls has been strengthened. In June 1969, the Niagara River was completely diverted from American Falls for several months through construction of a temporary rock and earth dam. During this time, two bodies were removed from under the falls, including a man who had been seen jumping over the falls, and the body of a woman, which was discovered once the falls dried. While Horseshoe Falls absorbed the extra flow, the U.S. Army Corps of Engineers studied the riverbed and mechanically bolted and strengthened any faults they found; faults that would, if left untreated, have hastened the retreat of American Falls. A plan to remove the huge mound of talus deposited in 1954 was abandoned owing to cost, and in November 1969, the temporary dam was dynamited, restoring flow to American Falls. Even after these undertakings, Luna Island, the small piece of land between the American Falls and Bridal Veil Falls, remained off limits to the public for years owing to fears that it was unstable and could collapse into the gorge.
Commercial interests have continued to encroach on the land surrounding the state park, including the construction of several tall buildings (most of them hotels) on the Canadian side. The result is a significant alteration and urbanisation of the landscape. One study found that the tall buildings changed the breeze patterns and increased the number of mist days from 29 per year to 68 per year, but another study disputed this idea.
In 2013, New York State began an effort to renovate Three Sisters Islands located south of Goat Island. Funds were used from the re-licensing of the New York Power Authority hydroelectric plant downriver in Lewiston, New York, to rebuild walking paths on the Three Sisters Islands and to plant native vegetation on the islands. The state also renovated the area around Prospect Point at the brink of American Falls in the state park.
Toponymy
Theories differ as to the origin of the name of the falls. The Native American word Ongiara means thundering water; The New York Times used this in 1925. According to Iroquoian scholar Bruce Trigger, Niagara is derived from the name given to a branch of the local native Neutral Confederacy, who are described as the Niagagarega people on several late-17th-century French maps of the area. According to George R. Stewart, it comes from the name of an Iroquois town called Onguiaahra, meaning "point of land cut in two". In 1847, an Iroquois interpreter stated that the name came from Jaonniaka-re, meaning "noisy point or portage". To Mohawks, the name refers to "the neck", pronounced "onyara"; the portage or neck of land between lakes Erie and Ontario onyara.
History
Many figures have been suggested as first circulating a European eyewitness description of Niagara Falls. The Frenchman Samuel de Champlain visited the area as early as 1604 during his exploration of what is now Canada, and members of his party reported to him the spectacular waterfalls, which he described in his journals. The first description of the falls is credited to Belgian missionary, Father Louis Hennepin in 1677, after traveling with the explorer René-Robert Cavelier, Sieur de La Salle, thus bringing the falls to the attention of Europeans. French Jesuit missionary Paul Ragueneau likely visited the falls some 35 years before Hennepin's visit while working among the Huron First Nation in Canada. Jean de Brébeuf also may have visited the falls, while spending time with the Neutral Nation. The Finnish-Swedish naturalist Pehr Kalm explored the area in the early 18th century and is credited with the first scientific description of the falls. In 1762, Captain Thomas Davies, a British Army officer and artist, surveyed the area and painted the watercolor, An East View of the Great Cataract of Niagara, the first eyewitness painting of the falls.
During the 19th century, tourism became popular, and by the mid-century, it was the area's main industry. Theodosia Burr Alston (daughter of Vice President Aaron Burr) and her husband Joseph Alston were the first recorded couple to honeymoon there in 1801. Napoleon Bonaparte's brother Jérôme visited with his bride in the early 19th century. In 1825, British explorer John Franklin visited the falls while passing through New York en route to Cumberland House as part of his second Arctic expedition, calling them "so justly celebrated as the first in the world for grandeur".
In 1843, Frederick Douglass joined the American Anti-Slavery Society's "One Hundred Conventions" tour throughout New York and the midwest. Sometime on this tour, Douglass visited Niagara Falls and wrote a brief account of the experience: "When I came into its awful presence the power of discription failed me, an irrisistible power closed my lips." Being on the Canadian border, Niagara Falls was on one of the routes of the Underground Railroad. The falls were also a popular tourist attraction for Southern slaveowners, who would bring their enslaved workers on the trip. "Many a time the trusted body-servant, or slave-girl, would leave master or mistress in the discharge of some errand, and never come back." This sometimes led to conflict. Early town father Peter Porter assisted slavecatchers in finding runaway slaves, even leading, in the case of runaway Solomon Moseby, to a riot in Niagara-on-the-Lake, Canada. Much of this history is memorialized in the Niagara Falls Underground Railroad Heritage Center. After the American Civil War, the New York Central Railroad publicized Niagara Falls as a focus of pleasure and honeymoon visits. After World War II, the auto industry, along with local tourism boards, began to promote Niagara honeymoons.
In about 1840, the English industrial chemist Hugh Lee Pattinson traveled to Canada, stopping at Niagara Falls long enough to make the earliest known photograph of the falls, a daguerreotype in the collection of Newcastle University. It was once believed that the small figure standing silhouetted with a top hat was added by an engraver working from imagination as well as the daguerreotype as his source, but the figure is clearly present in the photograph. Because of the very long exposure required, of ten minutes or more, the figure is assumed by Canada's Niagara Parks agency to be Pattinson. The image is left-right inverted and taken from the Canadian side. Pattinson made other photographs of Horseshoe Falls; these were then transferred to engravings to illustrate Noël Marie Paymal Lerebours' Excursions Daguerriennes (Paris, 1841–1864).[55]
On August 6, 1918, an iron scow became stuck on the rocks above the falls. The two men on the scow were rescued, but the vessel remained trapped on rocks in the river, and is still visible there in a deteriorated state, although its position shifted by 50 meters (160 ft) during a storm on October 31, 2019. Daredevil William "Red" Hill Sr. was particularly praised for his role in the rescue.
After the First World War, tourism boomed as automobiles made getting to the falls much easier. The story of Niagara Falls in the 20th century is largely that of efforts to harness the energy of the falls for hydroelectric power, and to control the development on both sides that threaten the area's natural beauty. Before the late 20th century, the northeastern end of Horseshoe Falls was in the United States, flowing around the Terrapin Rocks, which were once connected to Goat Island by a series of bridges. In 1955, the area between the rocks and Goat Island was filled in, creating Terrapin Point. In the early 1980s, the U.S. Army Corps of Engineers filled in more land and built diversion dams and retaining walls to force the water away from Terrapin Point. Altogether, 400 ft (120 m) of Horseshoe Falls were eliminated, including 100 ft (30 m) on the Canadian side. According to author Ginger Strand, the Horseshoe Falls is now entirely in Canada. Other sources say "most of" Horseshoe Falls is in Canada.
The only recorded freeze-up of the river and falls was caused by an ice jam on March 29, 1848. No water (or at best a trickle) fell for as much as 40 hours. Waterwheels stopped, and mills and factories shut down for having no power. In 1912, American Falls was completely frozen, but the other two falls kept flowing. Although the falls commonly ice up most winters, the river and the falls do not freeze completely. The years 1885, 1902, 1906, 1911, 1932, 1936, 2014, 2017 and 2019 are noted for partial freezing of the falls. A so-called ice bridge was common in certain years at the base of the falls and was used by people who wanted to cross the river before bridges had been built. During some winters, the ice sheet was as thick as 40 to 100 feet (12 to 30 m), but that thickness has not occurred since 1954. The ice bridge of 1841 was said to be at least 100 feet thick. On February 12, 1912, the ice bridge which had formed on January 15 began breaking up while people were still on it. Many escaped, but three died during the event, later named the Ice Bridge Tragedy.
Bridge crossings
A number of bridges have spanned the Niagara River in the general vicinity of the falls. The first, not far from the whirlpool, was a suspension bridge above the gorge. It opened for use by the public in July 1848 and remained in use until 1855. A second bridge in the Upper Falls area was commissioned, with two levels or decks, one for use by the Great Western Railway. This Niagara Falls Suspension Bridge opened in 1855. It was used by conductors on the Underground Railroad to escort runaway slaves to Canada. In 1882, the Grand Trunk Railway took over control of the second deck after it absorbed the Great Western company. Significant structural improvements were made in the late 1870s and then in 1886; this bridge remained in use until 1897.
Because of the volume of traffic, the decision was made to construct a new arch bridge nearby, under and around the existing bridge. After it opened in September 1897, a decision was made to remove and scrap the railway suspension bridge. This new bridge was initially known as the Niagara Railway Arch, or Lower Steel Arch Bridge; it had two decks, the lower one used for carriages and the upper for trains. In 1937, it was renamed the Whirlpool Rapids Bridge and remains in use today. All of the structures built up to that time were referred to as Lower Niagara bridges and were some distance from the falls.
The first bridge in the so-called Upper Niagara area (closer to the falls) was a two-level suspension structure that opened in January 1869; it was destroyed during a severe storm in January 1889. The replacement was built quickly and opened in May 1889. In order to handle heavy traffic, a second bridge was commissioned, slightly closer to American Falls. This one was a steel bridge and opened to traffic in June 1897; it was known as the Upper Steel Arch Bridge but was often called the Honeymoon Bridge. The single level included a track for trolleys and space for carriages and pedestrians. The design led to the bridge being very close to the surface of the river and in January 1938, an ice jam twisted the steel frame of the bridge which later collapsed on January 27, 1938.
Another Lower Niagara bridge had been commissioned in 1883 by Cornelius Vanderbilt for use by railways at a location roughly approximately 200 feet south of the Railway Suspension Bridge. This one was of an entirely different design; it was a cantilever bridge to provide greater strength. The Niagara Cantilever Bridge had two cantilevers which were joined by steel sections; it opened officially in December 1883, and improvements were made over the years for a stronger structure. As rail traffic was increasing, the Michigan Central Railroad company decided to build a new bridge in 1923, to be located between the Lower Steel Arch Bridge and the Cantilever Bridge. The Michigan Central Railway Bridge opened in February 1925 and remained in use until the early 21st century. The Cantilever Bridge was removed and scrapped after the new rail bridge opened. Nonetheless, it was inducted into the North America Railway Hall of Fame in 2006.
There was a lengthy dispute as to which agency should build the replacement for the Niagara Railway Arch, or Lower Steel Arch Bridge in the Upper Niagara area. When that was resolved, construction of a steel bridge commenced in February 1940. Named the Rainbow Bridge, and featuring two lanes for traffic separated by a barrier, it opened in November 1941 and remains in use today.
Industry and commerce
The enormous energy of Niagara Falls has long been recognized as a potential source of power. The first known effort to harness the waters was in 1750, when Daniel Joncaire built a small canal above the falls to power his sawmill. Augustus and Peter Porter purchased this area and all of American Falls in 1805 from the New York state government, and enlarged the original canal to provide hydraulic power for their gristmill and tannery. In 1853, the Niagara Falls Hydraulic Power and Mining Company was chartered, which eventually constructed the canals that would be used to generate electricity. In 1881, under the leadership of Jacob F. Schoellkopf, the Niagara River's first hydroelectric generating station was built. The water fell 86 feet (26 m) and generated direct current electricity, which ran the machinery of local mills and lit up some of the village streets.
The Niagara Falls Power Company, a descendant of Schoellkopf's firm, formed the Cataract Company headed by Edward Dean Adams, with the intent of expanding Niagara Falls' power capacity. In 1890, a five-member International Niagara Commission headed by Sir William Thomson among other distinguished scientists deliberated on the expansion of Niagara hydroelectric capacity based on seventeen proposals but could not select any as the best combined project for hydraulic development and distribution. In 1893, Westinghouse Electric (which had built the smaller-scale Ames Hydroelectric Generating Plant near Ophir, Colorado, two years earlier) was hired to design a system to generate alternating current on Niagara Falls, and three years after that a large-scale AC power system was created (activated on August 26, 1895). The Adams Power Plant Transformer House remains as a landmark of the original system.
By 1896, financing from moguls including J. P. Morgan, John Jacob Astor IV, and the Vanderbilts had fueled the construction of giant underground conduits leading to turbines generating upwards of 100,000 horsepower (75 MW), sent as far as Buffalo, 20 mi (32 km) away. Some of the original designs for the power transmission plants were created by the Swiss firm Faesch & Piccard, which also constructed the original 5,000 hp (3.7 MW) waterwheels. Private companies on the Canadian side also began to harness the energy of the falls. The Government of Ontario eventually brought power transmission operations under public control in 1906, distributing Niagara's energy to various parts of the Canadian province.
Other hydropower plants were being built along the Niagara River. But in 1956, disaster struck when the region's largest hydropower station was partially destroyed in a landslide. This drastically reduced power production and put tens of thousands of manufacturing jobs at stake. In 1957, Congress passed the Niagara Redevelopment Act, which granted the New York Power Authority the right to fully develop the United States' share of the Niagara River's hydroelectric potential.
In 1961, when the Niagara Falls hydroelectric project went online, it was the largest hydropower facility in the Western world. Today, Niagara is still the largest electricity producer in New York state, with a generating capacity of 2.4 GW. Up to 1,420 cubic metres (380,000 US gal) of water per second is diverted from the Niagara River through conduits under the city of Niagara Falls to the Lewiston and Robert Moses power plants. Currently between 50% and 75% of the Niagara River's flow is diverted via four huge tunnels that arise far upstream from the waterfalls. The water then passes through hydroelectric turbines that supply power to nearby areas of Canada and the United States before returning to the river well past the falls. When electrical demand is low, the Lewiston units can operate as pumps to transport water from the lower bay back up to the plant's reservoir, allowing this water to be used again during the daytime when electricity use peaks. During peak electrical demand, the same Lewiston pumps are reversed and become generators.
To preserve Niagara Falls' natural beauty, a 1950 treaty signed by the U.S. and Canada limited water usage by the power plants. The treaty allows higher summertime diversion at night when tourists are fewer and during the winter months when there are even fewer tourists. This treaty, designed to ensure an "unbroken curtain of water" flowing over the falls, states that during daylight time during the tourist season (April 1 to October 31) there must be 100,000 cubic feet per second (2,800 m3/s) of water flowing over the falls, and during the night and off-tourist season there must be 50,000 cubic feet per second (1,400 m3/s) of water flowing over the falls. This treaty is monitored by the International Niagara Board of Control, using a NOAA gauging station above the falls. During winter, the Power Authority of New York works with Ontario Power Generation to prevent ice on the Niagara River from interfering with power production or causing flooding of shoreline property. One of their joint efforts is an 8,800-foot-long (2,700 m) ice boom, which prevents the buildup of ice, yet allows water to continue flowing downstream. In addition to minimum water volume, the crest of Horseshoe falls was reduced to maintain an uninterrupted "curtain of water".
In August 2005, Ontario Power Generation, which is responsible for the Sir Adam Beck stations, started a major civil engineering project, called the Niagara Tunnel Project, to increase power production by building a new 12.7-metre (42 ft) diameter, 10.2-kilometre-long (6.3 mi) water diversion tunnel. It was officially placed into service in March 2013, helping to increase the generating complex's nameplate capacity by 150 megawatts. It did so by tapping water from farther up the Niagara River than was possible with the preexisting arrangement. The tunnel provided new hydroelectricity for approximately 160,000 homes.
Transport
Ships can bypass Niagara Falls by means of the Welland Canal, which was improved and incorporated into the Saint Lawrence Seaway in the mid-1950s. While the seaway diverted water traffic from nearby Buffalo and led to the demise of its steel and grain mills, other industries in the Niagara River valley flourished with the help of the electric power produced by the river. However, since the 1970s the region has declined economically.
The cities of Niagara Falls, Ontario, Canada, and Niagara Falls, New York, United States, are connected by two international bridges. The Rainbow Bridge, just downriver from the falls, affords the closest view of the falls and is open to non-commercial vehicle traffic and pedestrians. The Whirlpool Rapids Bridge lies one mile (1.6 km) north of the Rainbow Bridge and is the oldest bridge over the Niagara River. Nearby Niagara Falls International Airport and Buffalo Niagara International Airport were named after the waterfall, as were Niagara University, countless local businesses, and even an asteroid.
Over the falls
The first recorded publicity stunt using the Falls was the wreck of the schooner Michigan in 1827. Local hotel owners acquired a former Lake Erie freighter, loaded it with animals and effigies of people, towed it to a spot above the falls and let it plunge over the brink. Admission of fifty cents was charged.
In October 1829, Sam Patch, who called himself "the Yankee Leapster", jumped from a high tower into the gorge below the falls and survived; this began a long tradition of daredevils trying to go over the falls. Englishman Captain Matthew Webb, the first man to swim the English Channel, drowned in 1883 trying to swim the rapids downriver from the falls.
On October 24, 1901, 63-year-old Michigan school teacher Annie Edson Taylor became the first person to go over the falls in a barrel as a publicity stunt; she survived, bleeding, but otherwise unharmed. Soon after exiting the barrel, she said, "No one ought ever do that again." Days before Taylor's attempt, her domestic cat was sent over the falls in her barrel to test its strength. The cat survived the plunge unharmed and later posed with Taylor in photographs. Since Taylor's historic ride, over a dozen people have intentionally gone over the falls in or on a device, despite her advice. Some have survived unharmed, but others have drowned or been severely injured. Survivors face charges and stiff fines, as it is now illegal, on both sides of the border, to attempt to go over the falls. Charles Stephens, a 58-year-old barber from Bristol, England, went over the falls in a wooden barrel in July 1920 and was the first person to die in an endeavor of this type. Bobby Leach went over Horseshoe Falls in a crude steel barrel in 1911 and needed rescuing by William "Red" Hill Sr. Hill again came to the rescue of Leach following his failed attempt to swim the Niagara Gorge in 1920. In 1928, "Smiling Jean" Lussier tried an entirely different concept, going over the falls in a large rubber ball; he was successful and survived the ordeal.
Annie Edson Taylor posing with her wooden barrel (1901)
In the "Miracle at Niagara", on July 9, 1960, Roger Woodward, a seven-year-old American boy, was swept over Horseshoe Falls after the boat in which he was cruising lost power; two tourists pulled his 17-year-old sister Deanne from the river only 20 ft (6.1 m) from the lip of the Horseshoe Falls at Goat Island. Minutes later, Woodward was plucked from the roiling plunge pool beneath Horseshoe Falls after grabbing a life ring thrown to him by the crew of the Maid of the Mist boat. The children's uncle, Jim Honeycutt, who had been steering the boat, was swept over the edge to his death.
On July 2, 1984, Canadian Karel Soucek from Hamilton, Ontario, plunged over Horseshoe Falls in a barrel with only minor injuries. Soucek was fined $500 for performing the stunt without a license. In 1985, he was fatally injured while attempting to re-create the Niagara drop at the Houston Astrodome. His aim was to climb into a barrel hoisted to the rafters of the Astrodome and to drop 180 ft (55 m) into a water tank on the floor. After his barrel released prematurely, it hit the side of the tank, and he died the next day from his injuries.
In August 1985, Steve Trotter, an aspiring stuntman from Rhode Island, became the youngest person ever (age 22) and the first American in 25 years to go over the falls in a barrel. Ten years later, Trotter went over the falls again, becoming the second person to go over the falls twice and survive. It was also the second "duo"; Lori Martin joined Trotter for the barrel ride over the falls. They survived the fall, but their barrel became stuck at the bottom of the falls, requiring a rescue.
On September 28, 1989, Niagara natives Peter DeBernardi and Jeffery James Petkovich became the first "team" to make it over the falls in a two-person barrel. The stunt was conceived by DeBenardi, who wanted to discourage youth from following in his path of addictive drug use. The pair emerged shortly after going over with minor injuries and were charged with performing an illegal stunt under the Niagara Parks Act.
On June 5, 1990, Jesse Sharp, a whitewater canoeist from Tennessee paddled over the falls in a closed deck canoe. He chose not to wear a helmet to make his face more visible for photographs of the event. He also did not wear a life vest because he believed it would hinder his escape from the hydraulics at the base of the falls. His boat flushed out of the falls, but his body was never found. On September 27, 1993, John "David" Munday, of Caistor Centre, Ontario, completed his second journey over the falls. On October 1, 1995, Robert Douglas "Firecracker" Overacker went over the falls on a Jet Ski to raise awareness for the homeless. His rocket-propelled parachute failed to open and he plunged to his death. Overacker's body was recovered before he was pronounced dead at Niagara General Hospital.
Kirk Jones of Canton, Michigan, became the first known person to survive a plunge over Horseshoe Falls without a flotation device on October 20, 2003. According to some reports, Jones had attempted to commit suicide, but he survived the fall with only battered ribs, scrapes, and bruises. Jones tried going over the falls again in 2017, using a large inflatable ball, but died in the process. Later reports revealed that Jones had arranged for a friend to shoot video clips of his stunt.
On March 11, 2009, a man survived an unprotected trip over Horseshoe Falls. When rescued from the river he suffered from severe hypothermia and a large wound to his head. His identity was never released. Eyewitnesses reported seeing the man intentionally enter the water. On May 21, 2012, an unidentified man became the fourth person to survive an unprotected trip over Horseshoe Falls. Eyewitness reports show he "deliberately jumped" into the Niagara River after climbing over a railing. On July 8, 2019, at roughly 4 am, officers responded to a report of a person in crisis at the brink of the Canadian side of the falls. Once officers got to the scene, the man climbed the retaining wall, jumped into the river and went over Horseshoe Falls. Authorities subsequently began to search the lower Niagara River basin, where the man was found alive but injured sitting on the rocks at the water's edge.
Tightrope walkers
Tightrope walkers drew huge crowds to witness their exploits. Their wires ran across the gorge, near the current Rainbow Bridge, not over the waterfall. Jean François "Blondin" Gravelet was the first to cross Niagara Gorge on June 30, 1859, and did so again eight times that year. His most difficult crossing occurred on August 14, when he carried his manager, Harry Colcord, on his back.[114] His final crossing, on September 8, 1860, was witnessed by the Prince of Wales. Author Ginger Strand argues that these performances may have had symbolic meanings at the time relating to slavery and abolition.
Between 1859 and 1896 a wire-walking craze emerged, resulting in frequent feats over the river below the falls. One inexperienced walker slid down his safety rope. Only one man fell to his death, at night and under mysterious circumstances, at the anchoring place for his wire.
Maria Spelterini, a 23-year-old Italian was the first and only woman to cross the Niagara River gorge; she did so on a tightrope on July 8, 1876. She repeated the stunt several times during the same month. During one crossing she was blindfolded and during another, her ankles and wrists were handcuffed.
Among the many competitors was Ontario's William Hunt, who billed himself as "The Great Farini"; his first crossing was in 1860. Farini competed with Blondin in performing outrageous stunts over the gorge. On August 8, 1864, however, an attempt failed and he needed to be rescued.
On June 15, 2012, high wire artist Nik Wallenda became the first person to walk across the falls area in 116 years, after receiving special permission from both governments. The full length of his tightrope was 1,800 feet (550 m). Wallenda crossed near the brink of Horseshoe Falls, unlike walkers who had crossed farther downstream. According to Wallenda, it was the longest unsupported tightrope walk in history. He carried his passport on the trip and was required to present it upon arrival on the Canadian side of the falls.
Tourism
A ring-billed gull flies by a rainbow over the Horseshoe Falls
Peak visitor traffic occurs in the summertime, when Niagara Falls is both a daytime and evening attraction. From the Canadian side, floodlights illuminate both sides of the falls for several hours after dark (until midnight). The number of visitors in 2007 was expected to total 20 million, and by 2009 the annual rate was expected to top 28 million tourists.
The oldest and best known tourist attraction at Niagara Falls is the Maid of the Mist boat cruise, named for an alleged ancient Ongiara Indian mythical character, which has carried passengers into the rapids immediately below the falls since 1846. Cruise boats operate from boat docks on both sides of the falls, with the Maid of the Mist operating from the American side and Hornblower Cruises (originally Maid of the Mist until 2014) from the Canadian side. In 1996, Native American groups threatened to boycott the boat companies if they would not stop playing what they said was a fake story on their boats. The Maid of the Mist dropped the audio.
From the U.S. side, American Falls can be viewed from walkways along Prospect Point Park, which also features the Prospect Point Observation Tower and a boat dock for the Maid of the Mist. Goat Island offers more views of the falls and is accessible by foot and automobile traffic by bridge above American Falls. From Goat Island, the Cave of the Winds is accessible by elevator and leads hikers to a point beneath Bridal Veil Falls. Also on Goat Island are the Three Sisters Islands, the Power Portal where a statue of Nikola Tesla (the inventor whose patents for the AC induction motor and other devices for AC power transmission helped make the harnessing of the falls possible) can be seen, and a walking path that enables views of the rapids, the Niagara River, the gorge, and all of the falls. Most of these attractions lie within the Niagara Falls State Park.
The Niagara Scenic Trolley offers guided trips along American Falls and around Goat Island. Panoramic and aerial views of the falls can also be viewed by helicopter. The Niagara Gorge Discovery Center showcases the natural and local history of Niagara Falls and the Niagara Gorge. A casino and luxury hotel was opened in Niagara Falls, New York, by the Seneca Indian tribe. The Seneca Niagara Casino & Hotel occupies the former Niagara Falls Convention Center. The new hotel is the first addition to the city's skyline since completion of the United Office Building in the 1920s.
On the Canadian side, Queen Victoria Park features manicured gardens, platforms offering views of American, Bridal Veil, and Horseshoe Falls, and underground walkways leading into observation rooms that yield the illusion of being within the falling waters. Along the Niagara River, the Niagara River Recreational Trail runs 35 mi (56 km) from Fort Erie to Fort George, and includes many historical sites from the War of 1812.
The observation deck of the nearby Skylon Tower offers the highest view of the falls, and in the opposite direction gives views as far as Toronto. Along with the Tower Hotel (built as the Seagrams Tower, later renamed the Heritage Tower, the Royal Inn Tower, the Royal Center Tower, the Panasonic Tower, the Minolta Tower, and most recently the Konica Minolta Tower before receiving its current name in 2010), it is one of two towers in Canada with a view of the falls. The Whirlpool Aero Car, built in 1916 from a design by Spanish engineer Leonardo Torres Quevedo, is a cable car that takes passengers over the Niagara Whirlpool on the Canadian side. The Journey Behind the Falls consists of an observation platform and series of tunnels near the bottom of the Horseshoe Falls on the Canadian side. There are two casinos on the Canadian side of Niagara Falls, the Niagara Fallsview Casino Resort and Casino Niagara.
Touring by helicopter over the falls, from both the US and the Canadian side, was described by The New York Times as still popular a year after a serious crash. Although The New York Times had long before described attempting to tour the falls as "bent on suicide" and despite a number of fatal crashes, the "as many as 100 eight-minute rides each day" are hard to regulate; two countries and various government agencies would have to coordinate. These flights have been available "since the early 1960s."
FV133 Abbott SPG (Self Propelled Gun) (1965-mid 90s) Rolls-Royce K60 Mk 4G multi-fuel opposed piston engine
Civilian Registration Number TRX 157 D (Berkshire)
FV433, Abbott SPG was built by Vickers as a Sexton replacement, the Abbott name continued the Second World War style of naming self-propelled artillery after ecclesiastical titles.
A completely new ammunition family, comprising shells, fuzes and cartridges, was designed for Abbot's L13 gun, designated 105 mm Field (105 mm Fd). Compared to US 105 mm M1 type ammunition, it uses electrical instead of percussion primers, and has longer shells.
The Mark 2 adopted a new projectile design including an improved lethality HE shell (heavier with more HE) and full charge cartridges. Maximum range with 105 mm Fd Mk 1 ammunition was 15 km, the Mk 2 gave 17.4 km. Maximum rate of fire was 6–8 rounds per minute.
The Abbot was able to swim across water, having a flotation screen fixed around the hull that was raised to provide buoyancy. The action of the tracks was sufficient to drive it forward at about 3 knots . Each Abbot was supported by a fully amphibious Stalwart Mk 2 High Mobility Load Carrier that carried additional ammunition.
Thankyou for a massive 54,204,915 views
Shot 29.08.2016 at Shrewesbury Steam Rally, Onslow Park, Shrewesbury REF 119-379
Top 200 of 2017 @ deepskyobject
Места и теги условны, забытые персоны в бесконечном процессе добавления!
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#shoegaze #dreampop
01. Slowdive - Slowdive
02. Ride - Weather Diaries
03. Black Nite Crash - Nevergreen
04. Loomer - Deserter
05. Palm Haze - Tangy Dream
06. Maw - Maw
07. Plant Cell - Flowergaze? (Rebuild)
08. The Cult Of Lip - Your Feedback EP
09. Roma - Ficciones EP
10. Airiel - Molten Young Lovers
11. The Cherry Wave - Inhale, Exhale
12. June Parker - We're Exactly Where We Are
13. Coloresantos - Tercer Paisaje
14. Weed - Born Wrong Love
15. Kindling - Hush
16. Weed Hounds - Double Life EP
17. Fun With Ether - Tanned Skin, Light Eyes
18. Deafcult - Auras
19. Taffy - Nyctophilia
20. Brief Candles - Retreater
...
#dreampop #ethereal
01. Ozean - Ozean EP (1992 / 2017)
02. Pia Fraus - Field Ceremony
03. The Morelings - Same Century
04. Spirit Valley - Negatives
05. Glass - Lure
06. The Luxembourg Signal - Blue Field
07. Secret Shine - There Is Only Now
08. Blonde Tongues - Safe Like Silk In Polyester Sheets
09. Trementina - 810
10. Whimsical - Sleep To Dream
11. Spc Eco - Calm
12. Electro Group - Ranger
13. Autumn's Grey Solace - Celestial Realms
14. Fawns Of Love - Who Cares About Tomorrow
15. Panda Riot - Infinity Maps
16. Slow Glows - Star Trail EP
17. Soon, She Said - The First Casualty Of Love Is Innocence
18. The History Of Colour TV - Something Like Eternity
19. Tangible Rays - Seance
20. The Stargazer Lilies - Lost
...
#indiepop #slowcore #noisepop
01. Cigarettes After Sex - Cigarettes After Sex
02. Agent Blå - Agent Blå
03. Dayzed - Haze EP
04. Johnny Jewel – Windswept
05. The Bv's - Speaking From A Distance
06. Novella - Change of State
07. Fazerdaze - Morningside
08. Japanese Breakfast - Soft Sounds From Another Planet
09. Girl Ray - Earl Grey
10. Drab Majesty - The Demonstration
11. Lau Nau - Poseidon
12. Burning Hearts - Battlefields
13. Beach Fossils - Somersault
14. Pale Honey - Devotion
15. Hoops - Routines
16. Say Sue Me - Say Sue Me
17. Star Tropics - Lost World
18. Alvvays - Antisocialites
19. BMX Bandits - Forever
20. Flotation Toy Warning - The Machine That Made Us
...
#rock #postpunk #psychedelic
01. Wolf Alice - Visions Of A Life
02. LCD Soundsystem - American Dream
03. Kælan Mikla - Mánadans (2013–2014)
04. Idles - Brutalism
05. Thurston Moore - Rock N Roll Consciousness
06. Overlake - Fall
07. Ty Segall - Fried Shallots
08. Wire - Silver/Lead
09. The Horrors - V
10. The Jesus and Mary Chain - Damage and Joy
11. Morrissey - Low in High School
12. Oh Sees - Orc
13. The I.L.Y's - Bodyguard
14. Crash City Saints - Are You Free
15. At the Drive-In - in•ter a•li•a
16. Pond - The Weather
17. L.A. Witch - L.A. Witch
18. UV-TV - Glass
19. Ulrika Spacek - Modern English Decoration
20. Monster Movie - Keep the Voices Distant
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#artpop #lofi #synthwave
01. Hazel English - Just Give In / Never Going Home
02. Midwife - Like Author, Like Daughter
03. Circuit Des Yeux - Reaching for Indigo
04. Susanne Sundfør - Music for People in Trouble
05. Julien Baker - Turn Out the Lights
06. Beaches - Second Of Spring
07. Marika Hackman - I'm Not Your Man
08. Ariel Pink - Dedicated to Bobby Jameson
09. Molly Nilsson - Imaginations
10. Chastity Belt - I Used to Spend So Much Time Alone
11. Priests - Nothing Feels Natural
12. Jane Weaver - Modern Kosmology
13. Future Islands - The Far Field
14. Arcade Fire - Everything Now
15. London Grammar - Truth Is A Beautiful Thing
16. Goldfrapp - Silver Eye
17. Mammút - Kinder Versions
18. St. Vincent - Masseduction
19. The New Pornographers - Whiteout Conditions
20. Shelling - Waiting For Mint Shower
...
#psychedelic #kraut #jazz
01. Kairon; IRSE! – Ruination
02. Kamasi Washington - Harmony Of Difference
03. Videodrones - Nattens Hævn
04. Ulver - The Assassination of Julius Caesar
05. Bardo Pond - Under The Pines
06. Moon Duo - Occult Architecture Vol. 1,2
07. New Candys - Bleeding Magenta
08. Zimpel/Ziołek - Zimpel/Ziołek
09. Dollkraut - Holy Ghost People
10. Kielov - Elektronische EP
11. Mogwai - Every Country's Sun
12. Swans - Deliquescence (live)
13. Godspeed You! Black Emperor - Undoing A Luciferian Towers
14. The Black Heart Death Cult - Black Rainbow EP
15. Electric Moon - Stardust Rituals
16. The Black Angels - Death Song
17. Horte - Horte
18. Fujiya & Miyagi - Different Blades From The Same
19. Lætitia Sadier Source Ensemble - Find Me Finding You
20. Aidan Baker & Claire Brentnall - Delirious Things
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#postmetal #doom #postindustrial #atmosphericblack
01. Elder - Reflections of a Floating World
02. Wolves in the Throne Room + Anna von Hausswolff - Thrice Woven
03. Chelsea Wolfe - Hiss Spun
04. Planning For Burial - Below the House
05. Blanck Mass - World Eater
06. Palehorse/Palerider - Burial Songs
07. Richard H. Kirk - Dasein
08. Converge – The Dusk In Us
09. Auðn - Farvegir Fyrndar
10. Tchornobog - Tchornobog
11. Amenra - Mass VI
12. Couch Slut – Contempt
13. Hell - Hell
14. Rope Sect – Personae Ingratae
15. Avatarium - Hurricanes and Halos
16. Bell Witch – Mirror Reaper
17. Merkabah - Million Miles
18. Paradise Lost - Medusa
19. Enslaved - E
20. Violet Cold – Anomie
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#ambient #drone #noise
01. Angelo Badalamenti - Twin Peaks: Limited Event Series Soundtrack
02. Demen - Nektyr
03. Kaitlyn Aurelia Smith - The Kid
04. Dean Hurley - Anthology Resource Vol. 1: △△
05. The Bug & Earth - Concrete Desert
06. Jefre Cantu-Ledesma - On the Echoing Green
07. William Basinski - A Shadow in Time
08. Kara-Lis Coverdale - Grafts
09. Ryuichi Sakamoto - async
10. Trent Reznor and Atticus Ross - The Vietnam War OST
11. Brian Eno - Sisters
12. Ben Frost - The Centre Cannot Hold
13. Windy & Carl - Blues For A UFO
14. Kaukolampi - 1
15. Sarah Davachi - All My Circles Run
16. Prurient - Rainbow Mirror
17. Hammock - Mysterium
18. Iona Fortune – Tao Of I
19. The Necks - Unfold
20. Chihei Hatakeyama - Mirage
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#electronic #techno #idm
01. Kelly Lee Owens - Kelly Lee Owens
02. John Maus - Screen Memories
03. Actress - AZD
04. Bicep - Bicep
05. Fever Ray - Plunge
06. Dopplereffekt - Cellular Automata
07. James Holden & The Animal Spirits - The Animal Spirits
08. Eye (Laurène Exposito) — Cocktail Mexico EP
09. Carla dal Forno - The Garden EP
10. Colleen - A Flame My Love, A Frequency
11. Tzusing - 東方不敗
12. Karen Gwyer - Rembo
13. Daniel O'Sullivan - Veld
14. JASSS - Weightless
15. Lost Horizons - Ojala
16. Kalax - Kalax
17. Félicia Atkinson - Hand In Hand
18. Wanderwelle - Lost in a Sea of Trees
19. Hidden Orchestra - Dawn Chorus
20. Laurel Halo - Dust
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#Russia
01. Blankenberge - Radiogaze
02. Kedr Livanskiy - Ariadna
03. Спасибо - Навсегда
04. Архитектурный Оркестр Благодетели - АОБ
05. Рука Дочери - Скрежет
06. Aerofall - Forms
07. Лиловые Тюльпаны - 20 [Мы взрослеем позже, чем все] EP
08. Life on Venus - Encounters
09. Твои друзья полимеры - В чужой стране EP
10. Nika boginya - 12 заповедей богичности
11. Commis Voyageur - Le Passé Du Commis Voyageur
12. Sonic Death - Space Goth
13. Утро - Третий альбом
14. Bananafish - VIV
15. Supernova 1006 - Unique World
16. Antethic - Ghost Shirt Society
17. Буерак - Скромные апартаменты
18. Gnoomes - Tschak!
19. Shimmerance - Bright EP
20. Katya Yonder - Winter Skins
21. Chkbns - This Time EP
22. Fleece Flower - Что ты видишь
23. Cherry Candy - Singles
24. Rosemary Loves A Blackberry - Heart
25. Kittypants - Rest In Peace, baby
26. Dee Grinski (Manunkind) - Subspace EP
27. Ил - Нечисть
28. Park17 - Проснуться молодым
29. Краснознаменная Дивизия Имени Моей Бабушки - Посмертные приключения
30. Электрофорез - Quo vadis?
31. Блааӂь - Etudes Of Decay EP
32. Громыка - Нашатырь
33. Jassa - Incarnation of the Higher Gnosis
34. Ploho - Бумажные бомбы
35. Группа Женского Айкидо - Туры Выходного Дня EP
36. Малыш Камю - Никто не хочет играть со мной
37. Atariame - Fear is the World
38. Please Tokyo, Please This Is Tokyo - Карусель
39. Cosmic Triggers - Homo Fractaliens
40. Πлачь Ʒемля - Древние EP
41. Sewage Sour - OTMENA
42. Юлия Накарякова - Здравствуй!
43. Mercurium - Любовь Это Спецэффекты
44. Kirov - Тем, кого это касается EP
45. Iron Driver - Crack Of The Whip EP
46. Reverbcore - Diffusion EP
47. Fraunhofer Diffraction - Star Trails
48. Сруб - Восход
49. Фонтан - Обещание подростка EP
50. Пасош - Каждый раз самый важный раз
honorable mentions:
Pinkshinyultrablast - In The Hanging Gardens, 10" (2017), ждём альбом в мае 2018
Bearsinclouds - Antiparty (2017)
...
Best Concerts of 2017
01. Anna von Hausswolff & Kristof Hahn (Swans), Fennesz & Lillevan, Maarja Nuut & Hendrik Kaljujärv, Dollkraut, Fogh Depot, Anika, Rosemary Loves A Blackberry, Громыка, VHK @ SKIF, St Petersburg, RU, 30.09.2017
02. Auðn, True Widow, Amenra, Chelsea Wolfe, Magma, Oathbreaker, Subrosa (Subdued), Naðra, Perturbator, Zhrine, Telepathy @ Roadburn, Tilburg, NL, 21.04.2017
03. Ulver, Emma Ruth Rundle, Come To Grief, Inter Arma, Radar Men From The Moon, Jaye Jayle, Les Discrets, Oxbow, Pillorian (Agalloch) @ Roadburn, Tilburg, NL, 23.04.2017
04. The Radio Dept., Chelsea Wolfe, Kairon; IRSE!, Death Hawks, Röyksopp feat Jonna Lee, The Coathangers, Ilpo Väisänen & Jimi Tenor: Mika Vainio-tribuutti, Dinosaur Jr., Sanni @ Sideways, Helsinki, FI, 10.06.2017
05. Oranssi Pazuzu, Mysticum, Wolvennest, Aluk Todolo, The Bug vs Dylan Carlson of Earth, Trans Am, Misþyrming, My Dying Bride, Disfear @ Roadburn, Tilburg, NL, 22.04.2017
06. Clock DVA, Actress, Dopplereffekt @ PPF Artplay, St Petersburg, RU, 28.07.2017
07. The Thurston Moore Group, Huoratron, Kaleidobolt, Kynnet, Editors, Mikko Joensuu: Amen 3, Demdike Stare, DJ Shadow, Tommy Cash, Iisa @ Sideways, Helsinki, FI, 09.06.2017
08. At the Drive-In, Franz Ferdinand, The Jesus & Mary Chain, Black Lips, Allah-Las, MØ @ Rock En Seine, Paris, FR, 25.08.2017
09. Slowdive, Ty Segall, Clara Luciaini, Arnaud Rebotini, The Lemon Twigs, The xx, George Ezra @ Rock En Seine, Paris, FR, 27.08.2017
10. Римский-Корсаков - Снегурочка @ Mariinsky Theatre, St Petersburg, RU, 29.01.2017
11. The Jesus & Mary Chain, Cold Cave @ Tavastia, Helsinki, FI 10.10.2017
12. PJ Harvey, Frustration, Ulrika Spacek, Lysistrata, Fakear, Girls In Hawaii, Karoline Rose @ Rock En Seine, Paris, FR, 26.08.2017
13. Daniel Avery, Silver Apples, Unit Moebius, Das Ding, Love Cult, Juju & Jordash, Planetary Assault Systems, Simple Symmetry, Module Werk, Утро, Kausto, Inga Mauer @ PPF, St Petersburg, RU, 29.07.2017
14. Esben and The Witch, Deafheaven, Coven, Subrosa, Suma, Rome, Wolves In The Throne Room, Lycus, Alaric, Bongzilla @ Roadburn, Tilburg, NL, 20.04.2017
15. Legowelt, Silent Servant, Inga Mauer @ Artplay, St Petersburg, RU, 23.02.2017
16. Wardruna, Forndom, Nytt Land @ Kosmonavt, St Petersburg, Russia, 05.02.2017
17. Cigarettes After Sex @ Hi-Hat, St Petersburg, RU, 12.07.2017
18. Blankenberge, Wreck and Reference @ Les Villa, St Petersburg, RU, 21.07.2017
19. Oscar Powell, Alessandro Adriani, David Vunk, An-I (Douglas Lee), DJ Haus (Rupert Cogan), Module Werk, Nocow @ Artplay, St Petersburg, Russia, 23.09.2017
20. Jaakko Eino Kalevi, Teksti-TV 666, K-X-P, Sonic Death, Сплин, Uncle @ Stereoleto, St Petersburg, RU, 09.07.2017
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Top Films of 2017
01. Молодой Годар / Le Redoutable @ Michel Hazanavicius, 10/10
02. Ван Гог. С любовью, Винсент / Loving Vincent @ Hugh Welchman, Dorota Kobiela, 9/10
03. На игле 2 / T2 Trainspotting @ Danny Boyle, 8/10
04. Дюнкерк / Dunkirk @ Christopher Nolan, 8/10
05. Бегущий по лезвию 2049 / Blade Runner 2049 @ Denis Villeneuve, 8/10
06. Валериан и город тысячи планет / Valerian and the City of a Thousand Planets @ Luc Besson, 8/10
07. Ветреная река / Wind river @ Taylor Sheridan, 8/10
08. Джуманджи: Зов джунглей / Jumanji: Welcome to the Jungle @ Jake Kasdan, 8/10
09. Дикарь / Gauguin - Voyage de Tahiti @ Edouard Deluc, 7/10
10. Взрывная блондинка / Atomic Blonde @ David Leitch, 7/10
11. Оно / It @ Andy Muschietti, 7/10
12. Живое / Life @ Daniel Espinosa, 7/10
13. Призрак в доспехах / Ghost in the Shell @ Rupert Sanders, 7/10
14. Убийство священного оленя / The Killing of a Sacred Deer @ Yorgos Lanthimos, 6/10
15. Звёздные войны: Последние джедаи / Star Wars: Episode VIII - The Last Jedi @ Rian Johnson, 6/10
16. За пропастью во ржи / Rebel in the Rye @ Danny Strong, 6/10
17. Субурбикон / Suburbicon @ George Clooney, 6/10
18. Стражи Галактики 2 / Guardians of the Galaxy 2 @ James Gunn, 5/10
19. Двуличный любовник / L'amant double @ François Ozon, 5/10
20. Джон Уик 2 / John Wick: Chapter Two @ Chad Stahelski, 5/10
...
TOTAL RECALL:
2022 | 2021 | 2020 | 2019 | 2018 | 2017 | 2016 | 2015 | 2014
2013 | 2012 | 2011 | 2010 | 2009 | 2008 | 2007 | 2006
...
...
The End.
#bestalbumsof2017 #totp2017 #best_of_2017 #top2017 #top2017 #deepskyobject
Rusting Froth Flotation Skimmer at Geevor tin mine. This used chemicals to separate out the unwanted minerals such as arsenic from the tin ore, and replaced the calciners that roasted out the impurities.
Thanks to John Luxton for identifying the machinery.
Three boys, donning their flotation vests, wave to the camera as they enjoy a day on the lake.
[Ektachrome slide scanned and restored]
Preparing for a solo float on the Willamette River, I place in the back of my pickup my bicycle (to be locked at the downstream site for the ride back to the upstream starting point) and my "River Rat" flotation device.
Historical Context: Copper Mining in BC in the 1950s
British Columbia has a rich history of copper mining, with major operations in areas like the Highland Valley, Vancouver Island (including Quatsino Sound), and the Boundary District. The 1950s saw a post-World War II boom in mining due to demand for copper in industrial and electrical applications. Mills in this era relied on mechanical and chemical processes, with technology that was advanced for the time but still labor-intensive compared to modern methods. The goal of milling was to separate valuable copper minerals from waste rock (gangue) and produce a concentrate for smelting.
How a Copper Ore Mill Worked in the 1950s
A copper ore mill in BC during the 1950s typically followed these steps:
1. Ore Delivery and Initial Crushing
Process: Raw ore was transported from the mine to the mill via tramlines, railcars, or trucks. In regions like Quatsino Sound, tramlines often descended from mountaintop mines to mills near the shoreline.
Equipment: The ore first went through a primary crusher (often a jaw crusher or gyratory crusher) to break large rocks into smaller chunks, typically less than 6 inches in diameter. This made the ore easier to handle in subsequent steps.
Purpose: Reducing the size of the ore allowed for more efficient grinding and mineral liberation.
2. Grinding (Pulverization)
Process: The crushed ore was fed into grinding mills, such as ball mills or rod mills, which were large rotating cylinders filled with steel balls or rods. These mills ground the ore into a fine powder, often to the consistency of sand or finer (less than 0.5 mm).
Equipment: Ball mills were common in the 1950s, powered by electric motors or diesel engines. Water was often added to create a slurry, which helped with grinding and transport through the mill.
Purpose: Grinding liberated the copper-bearing minerals (like chalcopyrite, bornite, or chalcocite, common in BC) from the surrounding waste rock by breaking down the ore into tiny particles.
3. Classification and Separation of Particle Sizes
Process: The slurry from grinding was passed through classifiers (like spiral classifiers or hydrocyclones) to separate finer particles from coarser ones. Coarser particles were sent back to the grinding mill for further processing.
Purpose: This ensured that only particles of the right size moved to the next stage, optimizing the efficiency of mineral separation.
4. Flotation (Concentration of Copper Minerals)
Process: The fine slurry was sent to flotation cells—large tanks where chemicals (reagents) were added to help separate copper minerals from waste rock. Air was blown into the tanks, creating bubbles. The copper minerals, made hydrophobic (water-repelling) by the reagents, attached to the bubbles and floated to the surface as a froth, while the waste rock sank.
Equipment: Flotation machines in the 1950s were mechanical or pneumatic, often arranged in series for multiple stages of separation (rougher, scavenger, and cleaner circuits) to maximize recovery.
Chemicals: Common reagents included collectors (like xanthates) to bind to copper minerals, frothers to stabilize bubbles, and depressants to prevent unwanted minerals from floating.
Purpose: Flotation concentrated the copper content from a low percentage (often 1-2% in raw ore) to 20-30% or higher in the froth concentrate.
BC Specifics: Many BC copper deposits contained sulfide minerals, so sulfide flotation was the dominant method. Mills often dealt with complex ores containing other metals like molybdenum or gold, requiring tailored flotation processes.
5. Thickening and Filtering (Dewatering)
Process: The copper concentrate (froth) was sent to thickeners—large settling tanks where water was removed as the solids settled. The thickened concentrate was then filtered using rotary drum filters or disc filters to produce a damp, cake-like material.
Purpose: Dewatering reduced moisture content, making the concentrate easier and cheaper to transport to a smelter. Excess water was recycled back into the mill process to conserve resources.
BC Specifics: In remote areas like Quatsino Sound, water conservation was critical due to limited infrastructure, and tailings (waste slurry) were often disposed of in nearby ponds or streams (a practice later regulated due to environmental concerns).
6. Tailings Disposal
Process: The waste material (tailings) left after flotation—mostly ground-up rock with little to no copper—was pumped as slurry to a tailings pond or dam near the mill.
Purpose: This separated waste from the valuable concentrate, though in the 1950s, environmental regulations were minimal, and tailings often caused pollution in nearby water bodies.
BC Specifics: In coastal areas like Quatsino Sound, tailings disposal was sometimes directly into the ocean or sound, a practice that became controversial and was later restricted.
7. Shipment of Concentrate
Process: The final copper concentrate was loaded into railcars, trucks, or ships for transport to a smelter, where it would be heated to extract pure copper metal.
BC Specifics: Mills near Quatsino Sound often shipped concentrate via docks to smelters in places like Trail, BC (home of the Teck Cominco smelter), or to international markets. Small steamships or barges were common for coastal transport in the 1950s.
Key Features of 1950s Mills in BC
Technology: While earlier mills (e.g., 1920s) relied heavily on manual labor and basic machinery, by the 1950s, mills in BC used electric power, more efficient grinding equipment, and improved flotation chemicals. Automation was beginning but still limited-much of the process required human oversight.
Scale: Mills varied in size depending on the mine. Large operations like Britannia Mine (near Howe Sound) processed thousands of tons of ore daily, while smaller mills near Quatsino Sound might handle hundreds of tons.
Workforce: Mill workers in the 1950s included operators for crushers and mills, chemists to manage flotation reagents, and laborers for maintenance and transport. Conditions were often noisy, dusty, and hazardous, with limited safety regulations compared to today.
Environmental Impact: In the 1950s, environmental awareness was low. Tailings often contaminated local waterways, and mills produced significant air pollution from dust and smokestacks (if drying or roasting was done onsite).
Example: A Mill Near Quatsino Sound
For a mill near Quatsino Sound in the 1950s, imagine a facility on the shoreline processing ore from a nearby mountain mine (as described in your earlier query). Ore arrived via tramline, was crushed and ground in a mill building with towering ball mills, then moved to flotation cells housed in a separate section. Workers monitored the froth, adjusting chemicals to maximize copper recovery. The concentrate was filtered, loaded onto ships at a nearby dock, and sent to a smelter, while tailings were pumped into a nearby pond or the sound itself. The mill likely operated 24/7, with shifts of workers living in a small company town nearby.
Limitations and Advances
Challenges: Mills in remote BC areas faced logistical issues like limited power supply, difficult terrain, and harsh weather. Breakdowns in equipment were common, requiring onsite repairs.
Innovations: By the late 1950s, some BC mills began adopting early automation for grinding and flotation control, and better reagents improved recovery rates. However, full modernization didn’t occur until later decades.
See more in my Sustainable Energy and Hydrogen economy Set
www.flickr.com/photos/kevinmoore001/sets/72157623631942524/
In this illustration we have my concept for a four-story building, atop a mobile platform. Construction of this concept would take place on land in the form of modules. Then the modules would be transported to deep water for final assembly. The platform consists of two deep draft keels . From the water line down to the bottom of the keel would be approximately 400 feet. The keels would be constructed with chambers that are called "Baffles". The baffles will be flooded with sea water, for ballast or with compressed air for flotation. This system will be controlled by a computer, which will enable the platform to remain stable in all weather conditions. Each keel will house a 5000 hp electric motor and stabilizers that will have full control over pitch, roll and yaw, adding further control and stability to the platform. Although the platform is mobile, the main role of the electric motors would be to enable a computer to keep the platform on a stationary point on the ocean surface, regardless of wind and water currents. The main design of this platform is to remain level on all axes at sea, in all weather. And will not rise and fall with wave action, like conventional ships. So the main deck referred to as the "Weather Deck", would be open to the elements. And if the waves are high enough to breach the gunnels, 20' + it would simply wash over the deck and drain away. Access to the electric motors in the bottom of the keel would be achieved by watertight tubes and a spiral staircase. Above the weather deck is an oval shaped structure that is, 600' x 250', 8' clearance each floor, 4 watertight floors, , 45,000 square feet floor space in total, supported by pillars. A building such as this, could be used as a research laboratory, mobile hospital, support and engineering for the maintenance of a sea-based windfarm, or perhaps a completely self supported "Home on the sea" that would contain: Hydroponic Gardens, Water Desalinization Distillery, Biomass Digester, and Fishing Boats to harvest the catch of the day, from floating off shore Fish Farms. The power for this platform and building would be supplied by a 700 foot diameter, 30 MW wind turbine. The majority off electricity generated by the turbine would convert seawater into liquid hydrogen. The hydrogen would be stored in surplus to provide fuel for internal combustion engines for boats, generators and planes, so this concept would not rely completely on perpetual wind. Any remaining surplus of electricity could be used to power grow lights in the hydroponic gardens, providing them with 24-hour lighting. To be a realist, this concept would be expensive to build, but unlike conventional sea going vessels of this size, once deployed it would be self-sufficient, and unhampered by the cost of food, water and fuel.
"This is not science fiction, the technology is here today! My goal here and in life, is to be part of the solution, not a spectator!".
Kevin R. Moore
2010
The National Renewable Energy Laboratory (NREL), found that a kilogram of hydrogen (roughly equivalent to a gallon of gasoline) could be produced by wind powered electrolysis for between $5.55 in the near term and $2.27 in the long term. Using conventional wind turbines.
Timeline of hydrogen technologies
en.wikipedia.org/wiki/Timeline_of_hydrogen_technologies
Hydrogen economy
en.wikipedia.org/wiki/Category:Hydrogen_economy
High pressure electrolysis
en.wikipedia.org/wiki/High_pressure_electrolysis
More interesting reading: Wind-to-Hydrogen Project
www.nrel.gov/hydrogen/proj_wind_hydrogen.html
Protect Nantucket Sound
This guy left not long after I got down by his car. I was able to get 4 pictures of the car...
2019 Route 66 Car Show
Oak Park Avenue & Ogden Avenue
Berwyn, Illinois.
Cook County, USA.
August 24, 2019
From Wikipedia
The Amphicar Model 770 is an amphibious automobile which was launched at the 1961 New York Auto Show, manufactured in West Germany and marketed from 1961 to 1968. Production stopped in 1965.
Designed by Hans Trippel, the amphibious vehicle was manufactured by the Quandt Group at Lübeck and at Berlin-Borsigwalde, with a total of 3,878 manufactured in a single generation. Engine: Triumph four-cylinder engine of 1147 cc, 8:1 compression ratio, rated at 38.3 bhp
A descendant of the Volkswagen Schwimmwagen, the Amphicar offered only modest performance compared to most contemporary boats or cars, featured navigation lights and flag as mandated by the US Coast Guard — and after operation in water, required greasing at 13 points, one of which required removal of the rear seat.
The Amphicar name is a portmanteau of "amphibious" and "car".
Appearance
Front undersurface is slightly pointed and sharply cut away below. The wheels are set low, so that the vehicle stands well above ground level when on dry land. Front and rear bumpers are placed low on the body panels (but fairly high in relation to dry ground). The one-piece windshield is curved. The foldable top causes the body style to be classified as cabriolet. Its water propulsion is provided by twin propellers mounted under the rear bumper. The Amphicar is made of mild steel.
Powertrain
The Amphicar's engine was mounted at the rear of the craft, driving the rear wheels through a 4-speed manual transmission. For use in the water, the same engine drove a pair of reversible propellers at the rear, with a second gear lever engaging forward or reverse drive. Once in the water, the main gear lever would normally be left in neutral. By engaging first gear as well as drive to the propellers when approaching a boat ramp, the Amphicar could drive itself out of the water. .
Performance
The powerplant was the 1147 cc (69 in³) Standard SC engine from the British Triumph Herald 1200. Many engines were tried in prototypes, but the Triumph engine was "state of the art" in 1961 and it had the necessary combination of performance, weight, cool running, and reliability. Updated versions of this engine remained in production in the Triumph Spitfire until 1980.
The Amphicar engine had a power output of 43 hp (32 kW) at 4750 rpm, slightly more than the Triumph Herald due to a shorter exhaust.[7] Designated the "Model 770",[5] the Amphicar could achieve speeds of 7 knots in the water and 70 mph (110 km/h) on land. Later versions of the engine displaced 1296 cc and 1493 cc and produced up to 75 bhp (56 kW).
One owner was quoted "It's not a good car and it's not a good boat, but it does just fine" largely because of modest performance in and out of water. Another added, "We like to think of it as the fastest car on the water and fastest boat on the road."
Amphicar 1962.
In water as well as on land, the Amphicar steered with the front wheels, making it less maneuverable than a conventional boat. Time’s Dan Neil called it "a vehicle that promised to revolutionize drowning", explaining, "Its flotation was entirely dependent on whether the bilge pump could keep up with the leakage." In reality, a well maintained Amphicar does not leak at all and can be left in water, parked at a dock side, for many hours
History
Production started in late 1960. By the end of 1963 complete production was stopped.[15] From 1963-65 cars were assembled from shells and parts inventory built up in anticipation of sales of 25,000 units, with the last new build units assembled in 1965. Cars were titled in the year they actually sold rather than when they were produced, e.g. an unsold Amphicar assembled in 1963 or 1965 could be titled as 1967 or 1968 if that was when it was first sold, though the inventory could not be sold in the U.S. in the 1968 model year or later due to new environmental and USDOT emissions and safety equipment standards, they were available in other countries into 1968. The remaining inventory of unused parts was eventually purchased by Hugh Gordon of Santa Fe Springs, California.
Most Amphicars were sold in the United States. Cars were sold in the United Kingdom from 1964. Total production was 3,878 vehicles. 99 right-hand drives were converted from left-hand drives. Some were used in the Berlin police department and others were fitted for rescue operations.
Amphicar shows and rides
Amphicar owners regularly convene during the spring, summer and fall months at various locations nationwide for "swim-ins", the largest of which is held at Grand Lake St. Marys State Park, Ohio.
In 2015, the Boathouse at Walt Disney World's Disney Springs in Orlando, Florida began offering public Amphicar rides to visitors, charging $125 per ride for groups of up to three. Disney heavily re-engineered and enhanced the eight Amphicars of various original colors in its fleet for safety, reliability, and comfort.
An aerial photograph of the Froth Flotation Plant and Tailings Treatment Plant at Bolsover Colliery, Derbyshire
This is a scanned image from the SimonACCO company brochure "Achievements in Coal Preparation", printed in 1982.
The aerial photograph illustrates the colliery plant in 1978/79 after the completion of the Froth & Tailings plant.
The colliery closed in 1983
The Peterbilt looks to be a Model 337 complete with urea tank (between gas tank and battery box). The first Kenworth is probably a T440 based on its heavy steel bumper and flotation tires while the two trucks toward the back look like T270′s.
The Mount Elliott Mining Complex is an aggregation of the remnants of copper mining and smelting operations from the early 20th century and the associated former mining township of Selwyn. The earliest copper mining at Mount Elliott was in 1906 with smelting operations commencing shortly after. Significant upgrades to the mining and smelting operations occurred under the management of W.R. Corbould during 1909 - 1910. Following these upgrades and increases in production, the Selwyn Township grew quickly and had 1500 residents by 1918. The Mount Elliott Company took over other companies on the Cloncurry field in the 1920s, including the Mount Cuthbert and Kuridala smelters. Mount Elliott operations were taken over by Mount Isa Mines in 1943 to ensure the supply of copper during World War Two. The Mount Elliott Company was eventually liquidated in 1953.
The Mount Elliott Smelter:
The existence of copper in the Leichhardt River area of north western Queensland had been known since Ernest Henry discovered the Great Australia Mine in 1867 at Cloncurry. In 1899 James Elliott discovered copper on the conical hill that became Mount Elliott, but having no capital to develop the mine, he sold an interest to James Morphett, a pastoralist of Fort Constantine station near Cloncurry. Morphett, being drought stricken, in turn sold out to John Moffat of Irvinebank, the most successful mining promoter in Queensland at the time.
Plentiful capital and cheap transport were prerequisites for developing the Cloncurry field, which had stagnated for forty years. Without capital it was impossible to explore and prove ore-bodies; without proof of large reserves of wealth it was futile to build a railway; and without a railway it was hazardous to invest capital in finding large reserves of ore. The mining investor or the railway builder had to break the impasse.
In 1906 - 1907 copper averaged £87 a ton on the London market, the highest price for thirty years, and the Cloncurry field grew. The railway was extended west of Richmond in 1905 - 1906 by the Government and mines were floated on the Melbourne Stock Exchange. At Mount Elliott a prospecting shaft had been sunk and on the 1st of August 1906 a Cornish boiler and winding plant were installed on the site.
Mount Elliott Limited was floated in Melbourne on the 13th of July 1906. In 1907 it was taken over by British and French interests and restructured. Combining with its competitor, Hampden Cloncurry Copper Mines Limited, Mount Elliott formed a special company to finance and construct the railway from Cloncurry to Malbon, Kuridala (then Friezeland) and Mount Elliott (later Selwyn). This new company then entered into an agreement with the Queensland Railways Department in July 1908.
The railway, which was known as the 'Syndicate Railway', aroused opposition in 1908 from the trade unions and Labor movement generally, who contended that railways should be State-owned. However, the Hampden-Mount Elliott Railway Bill was passed by the Queensland Parliament and assented to on the 21st of April 1908; construction finished in December 1910. The railway terminated at the Mount Elliott smelter.
By 1907 the main underlie shaft had been sunk and construction of the smelters was underway using a second-hand water-jacket blast furnace and converters. At this time, W.H. Corbould was appointed general manager of Mount Elliott Limited.
The second-hand blast furnace and converters were commissioned or 'blown in' in May 1909, but were problematic causing hold-ups. Corbould referred to the equipment in use as being the 'worst collection of worn-out junk he had ever come across'. Corbould soon convinced his directors to scrap the plant and let him design new works.
Corbould was a metallurgist and geologist as well as mine/smelter manager. He foresaw a need to obtain control and thereby ensure a reliable supply of ore from a cross-section of mines in the region. He also saw a need to implement an effective strategy to manage the economies of smelting low-grade ore. Smelting operations in the region were made difficult by the technical and economic problems posed by the deterioration in the grade of ore. Corbould resolved the issue by a process of blending ores with different chemical properties, increasing the throughput capacity of the smelter and by championing the unification of smelting operations in the region. In 1912, Corbould acquired Hampden Consols Mine at Kuridala for Mount Elliott Limited, followed with the purchases of other small mines in the district.
Walkers Limited of Maryborough was commissioned to manufacture a new 200 ton water jacket furnace for the smelters. An air compressor and blower for the smelters were constructed in the powerhouse and an electric motor and dynamo provided power for the crane and lighting for the smelter and mine.
The new smelter was blown in September 1910, a month after the first train arrived, and it ran well, producing 2040 tons of blister copper by the end of the year. The new smelting plant made it possible to cope with low-grade sulphide ores at Mount Elliott. The use of 1000 tons of low-grade sulphide ores bought from the Hampden Consols Mine in 1911 made it clear that if a supply of higher sulphur ore could be obtained and blended, performance, and economy would improve. Accordingly, the company bought a number of smaller mines in the district in 1912.
Corbould mined with cut and fill stoping but a young Mines Inspector condemned the system, ordered it dismantled and replaced with square set timbering. In 1911, after gradual movement in stopes on the No. 3 level, the smelter was closed for two months. Nevertheless, 5447 tons of blister copper was produced in 1911, rising to 6690 tons in 1912 - the company's best year. Many of the surviving structures at the site were built at this time.
Troubles for Mount Elliott started in 1913. In February, a fire at the Consols Mine closed it for months. In June, a thirteen week strike closed the whole operation, severely depleting the workforce. The year 1913 was also bad for industrial accidents in the area, possibly due to inexperienced people replacing the strikers. Nevertheless, the company paid generous dividends that year.
At the end of 1914 smelting ceased for more than a year due to shortage of ore. Although 3200 tons of blister copper was produced in 1913, production fell to 1840 tons in 1914 and the workforce dwindled to only 40 men. For the second half of 1915 and early 1916 the smelter treated ore railed south from Mount Cuthbert. At the end of July 1916 the smelting plant at Selwyn was dismantled except for the flue chambers and stacks. A new furnace with a capacity of 500 tons per day was built, a large amount of second-hand equipment was obtained and the converters were increased in size.
After the enlarged furnace was commissioned in June 1917, continuing industrial unrest retarded production which amounted to only 1000 tons of copper that year. The point of contention was the efficiency of the new smelter which processed twice as much ore while employing fewer men. The company decided to close down the smelter in October and reduce the size of the furnace, the largest in Australia, from 6.5m to 5.5m. In the meantime the price of copper had almost doubled from 1916 due to wartime consumption of munitions.
The new furnace commenced on the 16th of January 1918 and 77,482 tons of ore were smelted yielding 3580 tons of blister copper which were sent to the Bowen refinery before export to Britain. Local coal and coke supply was a problem and materials were being sourced from the distant Bowen Colliery. The smelter had a good run for almost a year except for a strike in July and another in December, which caused Corbould to close down the plant until New Year. In 1919, following relaxation of wartime controls by the British Metal Corporation, the copper price plunged from about £110 per ton at the start of the year to £75 per ton in April, dashing the company's optimism regarding treatment of low grade ores. The smelter finally closed after two months operation and most employees were laid off.
For much of the period 1919 to 1922, Corbould was in England trying to raise capital to reorganise the company's operations but he failed and resigned from the company in 1922. The Mount Elliott Company took over the assets of the other companies on the Cloncurry field in the 1920s - Mount Cuthbert in 1925 and Kuridala in 1926. Mount Isa Mines bought the Mount Elliott plant and machinery, including the three smelters, in 1943 for £2,300, enabling them to start copper production in the middle of the Second World War. The Mount Elliott Company was finally liquidated in 1953.
In 1950 A.E. Powell took up the Mount Elliott Reward Claim at Selwyn and worked close to the old smelter buildings. An open cut mine commenced at Starra, south of Mount Elliott and Selwyn, in 1988 and is Australia's third largest copper producer producing copper-gold concentrates from flotation and gold bullion from carbon-in-leach processing.
Profitable copper-gold ore bodies were recently proved at depth beneath the Mount Elliott smelter and old underground workings by Cyprus Gold Australia Pty Ltd. These deposits were subsequently acquired by Arimco Mining Pty Ltd for underground development which commenced in July 1993. A decline tunnel portal, ore and overburden dumps now occupy a large area of the Maggie Creek valley south-west of the smelter which was formerly the site of early miner's camps.
The Old Selwyn Township:
In 1907, the first hotel, run by H. Williams, was opened at the site. The township was surveyed later, around 1910, by the Mines Department. The town was to be situated north of the mine and smelter operations adjacent the railway, about 1.5km distant. It took its name from the nearby Selwyn Ranges which were named, during Burke's expedition, after the Victorian Government Geologist, A.R. Selwyn. The town has also been known by the name of Mount Elliott, after the nearby mines and smelter.
Many of the residents either worked at the Mount Elliott Mine and Smelter or worked in the service industries which grew around the mining and smelting operations. Little documentation exists about the everyday life of the town's residents. Surrounding sheep and cattle stations, however, meant that meat was available cheaply and vegetables grown in the area were delivered to the township by horse and cart. Imported commodities were, however, expensive.
By 1910 the town had four hotels. There was also an aerated water manufacturer, three stores, four fruiterers, a butcher, baker, saddler, garage, police, hospital, banks, post office (officially from 1906 to 1928, then unofficially until 1975) and a railway station. There was even an orchestra of ten players in 1912. The population of Selwyn rose from 1000 in 1911 to 1500 in 1918, before gradually declining.
Source: Queensland Heritage Register.
Bank of Thrift, North Terrace, taken in April, 1919. It was erected in front of Government House gates in order to facilitate the flotation of the War loans. It was demolished before July 1920.
Visit the State Library of South Australia to view more photos of South Australia
The Mount Elliott Mining Complex is an aggregation of the remnants of copper mining and smelting operations from the early 20th century and the associated former mining township of Selwyn. The earliest copper mining at Mount Elliott was in 1906 with smelting operations commencing shortly after. Significant upgrades to the mining and smelting operations occurred under the management of W.R. Corbould during 1909 - 1910. Following these upgrades and increases in production, the Selwyn Township grew quickly and had 1500 residents by 1918. The Mount Elliott Company took over other companies on the Cloncurry field in the 1920s, including the Mount Cuthbert and Kuridala smelters. Mount Elliott operations were taken over by Mount Isa Mines in 1943 to ensure the supply of copper during World War Two. The Mount Elliott Company was eventually liquidated in 1953.
The Mount Elliott Smelter:
The existence of copper in the Leichhardt River area of north western Queensland had been known since Ernest Henry discovered the Great Australia Mine in 1867 at Cloncurry. In 1899 James Elliott discovered copper on the conical hill that became Mount Elliott, but having no capital to develop the mine, he sold an interest to James Morphett, a pastoralist of Fort Constantine station near Cloncurry. Morphett, being drought stricken, in turn sold out to John Moffat of Irvinebank, the most successful mining promoter in Queensland at the time.
Plentiful capital and cheap transport were prerequisites for developing the Cloncurry field, which had stagnated for forty years. Without capital it was impossible to explore and prove ore-bodies; without proof of large reserves of wealth it was futile to build a railway; and without a railway it was hazardous to invest capital in finding large reserves of ore. The mining investor or the railway builder had to break the impasse.
In 1906 - 1907 copper averaged £87 a ton on the London market, the highest price for thirty years, and the Cloncurry field grew. The railway was extended west of Richmond in 1905 - 1906 by the Government and mines were floated on the Melbourne Stock Exchange. At Mount Elliott a prospecting shaft had been sunk and on the 1st of August 1906 a Cornish boiler and winding plant were installed on the site.
Mount Elliott Limited was floated in Melbourne on the 13th of July 1906. In 1907 it was taken over by British and French interests and restructured. Combining with its competitor, Hampden Cloncurry Copper Mines Limited, Mount Elliott formed a special company to finance and construct the railway from Cloncurry to Malbon, Kuridala (then Friezeland) and Mount Elliott (later Selwyn). This new company then entered into an agreement with the Queensland Railways Department in July 1908.
The railway, which was known as the 'Syndicate Railway', aroused opposition in 1908 from the trade unions and Labor movement generally, who contended that railways should be State-owned. However, the Hampden-Mount Elliott Railway Bill was passed by the Queensland Parliament and assented to on the 21st of April 1908; construction finished in December 1910. The railway terminated at the Mount Elliott smelter.
By 1907 the main underlie shaft had been sunk and construction of the smelters was underway using a second-hand water-jacket blast furnace and converters. At this time, W.H. Corbould was appointed general manager of Mount Elliott Limited.
The second-hand blast furnace and converters were commissioned or 'blown in' in May 1909, but were problematic causing hold-ups. Corbould referred to the equipment in use as being the 'worst collection of worn-out junk he had ever come across'. Corbould soon convinced his directors to scrap the plant and let him design new works.
Corbould was a metallurgist and geologist as well as mine/smelter manager. He foresaw a need to obtain control and thereby ensure a reliable supply of ore from a cross-section of mines in the region. He also saw a need to implement an effective strategy to manage the economies of smelting low-grade ore. Smelting operations in the region were made difficult by the technical and economic problems posed by the deterioration in the grade of ore. Corbould resolved the issue by a process of blending ores with different chemical properties, increasing the throughput capacity of the smelter and by championing the unification of smelting operations in the region. In 1912, Corbould acquired Hampden Consols Mine at Kuridala for Mount Elliott Limited, followed with the purchases of other small mines in the district.
Walkers Limited of Maryborough was commissioned to manufacture a new 200 ton water jacket furnace for the smelters. An air compressor and blower for the smelters were constructed in the powerhouse and an electric motor and dynamo provided power for the crane and lighting for the smelter and mine.
The new smelter was blown in September 1910, a month after the first train arrived, and it ran well, producing 2040 tons of blister copper by the end of the year. The new smelting plant made it possible to cope with low-grade sulphide ores at Mount Elliott. The use of 1000 tons of low-grade sulphide ores bought from the Hampden Consols Mine in 1911 made it clear that if a supply of higher sulphur ore could be obtained and blended, performance, and economy would improve. Accordingly, the company bought a number of smaller mines in the district in 1912.
Corbould mined with cut and fill stoping but a young Mines Inspector condemned the system, ordered it dismantled and replaced with square set timbering. In 1911, after gradual movement in stopes on the No. 3 level, the smelter was closed for two months. Nevertheless, 5447 tons of blister copper was produced in 1911, rising to 6690 tons in 1912 - the company's best year. Many of the surviving structures at the site were built at this time.
Troubles for Mount Elliott started in 1913. In February, a fire at the Consols Mine closed it for months. In June, a thirteen week strike closed the whole operation, severely depleting the workforce. The year 1913 was also bad for industrial accidents in the area, possibly due to inexperienced people replacing the strikers. Nevertheless, the company paid generous dividends that year.
At the end of 1914 smelting ceased for more than a year due to shortage of ore. Although 3200 tons of blister copper was produced in 1913, production fell to 1840 tons in 1914 and the workforce dwindled to only 40 men. For the second half of 1915 and early 1916 the smelter treated ore railed south from Mount Cuthbert. At the end of July 1916 the smelting plant at Selwyn was dismantled except for the flue chambers and stacks. A new furnace with a capacity of 500 tons per day was built, a large amount of second-hand equipment was obtained and the converters were increased in size.
After the enlarged furnace was commissioned in June 1917, continuing industrial unrest retarded production which amounted to only 1000 tons of copper that year. The point of contention was the efficiency of the new smelter which processed twice as much ore while employing fewer men. The company decided to close down the smelter in October and reduce the size of the furnace, the largest in Australia, from 6.5m to 5.5m. In the meantime the price of copper had almost doubled from 1916 due to wartime consumption of munitions.
The new furnace commenced on the 16th of January 1918 and 77,482 tons of ore were smelted yielding 3580 tons of blister copper which were sent to the Bowen refinery before export to Britain. Local coal and coke supply was a problem and materials were being sourced from the distant Bowen Colliery. The smelter had a good run for almost a year except for a strike in July and another in December, which caused Corbould to close down the plant until New Year. In 1919, following relaxation of wartime controls by the British Metal Corporation, the copper price plunged from about £110 per ton at the start of the year to £75 per ton in April, dashing the company's optimism regarding treatment of low grade ores. The smelter finally closed after two months operation and most employees were laid off.
For much of the period 1919 to 1922, Corbould was in England trying to raise capital to reorganise the company's operations but he failed and resigned from the company in 1922. The Mount Elliott Company took over the assets of the other companies on the Cloncurry field in the 1920s - Mount Cuthbert in 1925 and Kuridala in 1926. Mount Isa Mines bought the Mount Elliott plant and machinery, including the three smelters, in 1943 for £2,300, enabling them to start copper production in the middle of the Second World War. The Mount Elliott Company was finally liquidated in 1953.
In 1950 A.E. Powell took up the Mount Elliott Reward Claim at Selwyn and worked close to the old smelter buildings. An open cut mine commenced at Starra, south of Mount Elliott and Selwyn, in 1988 and is Australia's third largest copper producer producing copper-gold concentrates from flotation and gold bullion from carbon-in-leach processing.
Profitable copper-gold ore bodies were recently proved at depth beneath the Mount Elliott smelter and old underground workings by Cyprus Gold Australia Pty Ltd. These deposits were subsequently acquired by Arimco Mining Pty Ltd for underground development which commenced in July 1993. A decline tunnel portal, ore and overburden dumps now occupy a large area of the Maggie Creek valley south-west of the smelter which was formerly the site of early miner's camps.
The Old Selwyn Township:
In 1907, the first hotel, run by H. Williams, was opened at the site. The township was surveyed later, around 1910, by the Mines Department. The town was to be situated north of the mine and smelter operations adjacent the railway, about 1.5km distant. It took its name from the nearby Selwyn Ranges which were named, during Burke's expedition, after the Victorian Government Geologist, A.R. Selwyn. The town has also been known by the name of Mount Elliott, after the nearby mines and smelter.
Many of the residents either worked at the Mount Elliott Mine and Smelter or worked in the service industries which grew around the mining and smelting operations. Little documentation exists about the everyday life of the town's residents. Surrounding sheep and cattle stations, however, meant that meat was available cheaply and vegetables grown in the area were delivered to the township by horse and cart. Imported commodities were, however, expensive.
By 1910 the town had four hotels. There was also an aerated water manufacturer, three stores, four fruiterers, a butcher, baker, saddler, garage, police, hospital, banks, post office (officially from 1906 to 1928, then unofficially until 1975) and a railway station. There was even an orchestra of ten players in 1912. The population of Selwyn rose from 1000 in 1911 to 1500 in 1918, before gradually declining.
Source: Queensland Heritage Register.
Smithsonian National Air and Space Museum annex.
For my video; youtu.be/hbK99xonFRM
The Udvar-Hazy Center in Chantilly, Virginia is a companion facility to the Museum on the National Mall in Washington, DC, USA.
When an Apollo command module landed in the ocean, it could settle into one of two stable positions: nose up or nose down. Landing nose down left its recovery antennas underwater and increased the possibility that the spacecraft might fill with sea water. To turn the command module upright, three inflatable bags were installed in the Command Module's forward (nose) compartment. Astronauts could right the spacecraft by activating air compressors in the aft (blunt) end of the spacecraft. The compressors were connected to the bags with tubing.
This is one of three flotation bags used on Apollo 11 at the end of its historic lunar landing mission on July 24, 1969. The astronauts deployed it after the command module settled nose down, enabling the spacecraft to right itself about six and half minutes after splashdown.
This artifact was transferred from NASA to the Smithsonian in 1973.
“APOLLO 13 RECOVERY--A water-level view of the Apollo 13 recovery operations in the South Pacific. The three astronauts have egressed their spacecraft, and Astronaut Fred W. Haise Jr., lunar module pilot, has already ascended to the helicopter. The other two crewmen await the return of the “Billy Pugh” net. Astronaut James A. Lovell Jr. (center), commander, will remain in the life raft until Astronaut John L. Swigert Jr., command module pilot, has boarded the helicopter. A U.S. Navy underwater demolition team swimmer assists with the recovery operations. The three Apollo 13 crewmen were flown to the USS Iwo Jima, primer recovery ship. Apollo 13 splashed down at 12:0:44 p.m. (CST), April 17, 1970, to safely conclude a perilous space flight.”
Mike Carroll, a wonderful photographer from Port Townsend, Washington. took this photo of me in my 4th KSR Race of the 2006 season, October . The flotation was yet evolving, but it was buoyant enough & stable.. 2025, BFG has raced 45 times, Still has its original front tire, the rear tire replaced ten or so years back from wear ofbraking & acceleration. I have kinetic raced 91 times since 2000.
Brand new Caymen Islands registered Airbus Helicopters H145 VP-CLP, equipped with a flotation system on the skids, at Cotswold Airport, Kemble, on 18th February 2025.
Recovery efforts included having a barge with a large crane hold the loaded tank car in place, along with the flotation bags, in order to carefully empty it's contents.
Sunnyside
Home Port: North Bend, WA
Year Built: 2019
LOA: 14
Owner: Joe Grez
Designer: Grez Yachts
Design: Unknown
Type: Power
Sunnyside was a COVID project built in the spring of 2020. 14 ft in length, 6 ft beam, cruising displacement is 1,000 lb. While her topside, cabin, and coach construction is stitch and glue plywood, her hull is based on a Uffa Fox International 14 but, wider and flatter midships. She has 300 lb of cement ballast to assure stability with adequate closed-cell flotation.
She has demonstrated very good seakeeping performance in normal summertime inland conditions.
Her complete propulsion system includes 300W of solar on the coach roof, an EP Carry propulsion system including motor and battery, and a Victron solar controller.
Her complete propulsion system costs $2400, weighs 30 lb., and is renewably powered by the sun. On a rainy, cloudy day, Sunnyside can still travel over 20 nm on solar alone. The longest day trip on the water was a meandering circumnavigation of Vashon Island last year, a total distance of nearly 40 nm. Solar propulsion arranged in this manner is suitable for long-range pleasure cruises because the sunlight (or cloud light) scales with the propulsion needs of a displacement hull very well.
(view from mine vehicle, en route from the office to the working floor)
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This waste rock pile is at the Continental Mine (= Continental Pit) in Butte, Montana. The town is known as the “Richest Hill on Earth” and "The Mining City". The Butte Mining District has produced gold, silver, copper, molybdenum, manganese, and other metals.
The area's bedrock consists of the Butte Quartz Monzonite (a.k.a. Butte Pluton), which is part of the Boulder Batholith. The Butte Quartz Monzonite ("BQM") formed 76.3 million years ago, during the mid-Campanian Stage in the Late Cretaceous. BQM rocks have been intruded and altered by hydrothermal veins containing valuable metallic minerals - principally sulfides. The copper mineralization has been dated to 62-66 million years ago, during the latest Maastrichtian Stage (latest Cretaceous) and Danian Stage (Early Paleocene). In the supergene enrichment zone of the area, the original sulfide mineralogy has been altered.
The Continental Mine was started in 1980 by the Anaconda Copper Mining Company - it is currently owned by Montana Resources. The mine targets a low-grade copper and molybdenum deposit on the eastern side of the Continental Fault, a major Basin & Range normal fault in the Butte area with about 3500 feet of offset. The mine's rocks consist of BQM with disseminated copper sulfides, plus copper- and molybdenum-bearing hydrothermal veins that intrude the BQM. Minerals at the site include chalcopyrite, molybdenite, malachite, azurite, tenorite, and cuprite. The latter four minerals are secondary copper minerals, produced by alteration of the primary copper sulfides.
When I visited in 2010, the Continental Mine was making 50,000 to 52,000 tons of ore each day. This mine can operate down to an ore grade of 0.1% copper. Most of the mineralization is disseminated copper, but veins are also present. Two stages of mineralization occurred in the Butte area - a porphyry copper system and a main stage system with large veins. The bottom of the porphyry copper system is ~ less than 12,800 feet below the surface. Veins peter out at 5600 to 5800 feet below the surface. At the Continental Mine, veins are small - they're veinlets less than 6 inches wide.
Mining is done 24 hours a day, 365 to 366 days per year. There's 1 to 2 days of down time at the mill. During those days, mining stops and waste material is moved. The ore:waste ratio is 8:10 (= strip ratio). The alluvial overburden consists of 7 paleosol horizons, including some caliches - the lime content results in an average pH of 8. The caliche material can be used to treat acidic materials.
This mine has 14 shovels and 15 trucks. A large Bucyrus shovel can load a 240-ton truck in three passes. The mine's benches are forty feet tall. Blasting is done with ANFO - ammonium nitrate and fuel oil. 0.65 pounds of explosives are used per ton of rock. The mine uses ~45 megawatts of power per day, which is about the same as the city of Butte itself.
Continental Mine ores are crushed in two stages. The crushed ores are then sent to the mill, where they are ground down to the fineness of talcum powder. Flotation and lime are used in procesing. Sulfides are collected. 1% of the mined material goes to the concentrator. 99% of mined material becomes tailings. The tailings powder is wet (33% solid and the rest is water) and piped uphill to a pond. The tailings pond water has a pH of 10. Water from the pond is recycled to make tailings slurry. 27 million gallons a day enters the pond. An earthen dam around the pond is designed to withstand a powerful earthquake.
Copper and molybdenum concentrates produced at the Continental Mine are not smelted locally - they are not even smelted in America. Concentrates are sold around the world, where material is smelted and the metals are produced. America shipping rocks overseas and buying back the finished product is the behavior of an underdeveloped country - America is not interested in smelting anymore - a sad reality.
"An ore deposit is a mine if it can stand total mismanagement and still make money."
Fish Quay, North Shields, Tyne and Wear, England, UK
Fish Quay The Fish Quay dates back to the 13th century, boasting a fascinating history. In 1225, a village of shielings - or fishermen's huts - formed where the Fish Quay stands today. North Shields took its name from these shielings and its location on the north bank of the River Tyne.
Traditional seafood businesses coexist with newer players, such as those in marketing and public relations. The Fish Quay buzzes with social life. There are plenty of places to eat, from classic fish restaurants to trendy brasseries. You can even enjoy fish and chips while overlooking the river and watching the ships pass by.
Mooring Buoys Anchors secured these large flotation devices to the riverbed. They rose and fell with the tide. Boats could moor to these buoys without risk. This keeps the quayside berths free for unloading fish.
Photographic Information
Taken on 28th April, 2025 at 1206hrs with a Pentax Spotmatic F 35mm film camera, through a Super Takumar 55mm ƒ/2 lens, on Kodak Ektar 100 ASA negative stock, scanned on an Epson 4490 Photo with SilverFast 9, post processed with Adobe Photoshop CS5.
© Timothy Pickford-Jones 2025
The Block 10 mine, one of the original BHP leases, was floated as the BHP Block 10 Co. Ltd in 1888. A concentration mill was erected at the mine in the 1890s to treat sulphide ore. Underground subsidence seriously affected the mill and, as a result, a new mill was erected on this hill in 1903, about 600 metres from the mine.
An aerial ropeway, the first at Broken Hill, was completed in 1904. This transported broken ore from the mine to a large storage bin above the mill. The mill cost £50 000 and could treat 3500 tons of ore per week.
The mine produced 2.5 million tons of ore and paid £1.5 million in dividends up to 1923 when it and the mill closed and were purchased by BHP. The mine was reworked by Broken Hill South Ltd between 1946 and 1960. Much of the mine site is now covered by overburden dumps from modern open-cut operations.
The concrete foundations on site are the remnants of the Block 10 concentration mill erected in 1903. The mill, designed by Captain John Warren and containing many of his inventions, was the first all electric mill in Broken Hill.
The aerial ropeway delivered broken ore from the mine to a storage bin above the mill. Broken ore was fed to crushing rolls and then passed to cylindrical trommels and hydraulic classifiers for sizing. Subsequent treatment consisted of wet concentration by jigs, Wilfley tables and vanners. These relied on specific gravity to separate the heavier lead and silver minerals from the zinc minerals. The resultant concentrate contained about two-thirds of the lead and one-half of the silver in the original ore, but very little zinc.
Flotation units were added to the mill in 1910 to produce a zinc concentrate from the tailings. Combined gravity-flotation concentration mills were standard at Broken Hill until after 1930 when the first all-flotation plants were installed.
Source: City Of Broken Hill.
The beach buns are here again.... waiting to make a splash. This set includes a new flamingo floatie. After two weeks of swimming lessons, I see a close resemblance to the bunnies and terrified kids at the pool. The black one is obviously being forced by his mommy to participate. Trust your flotation devices friends and remember to blow your bubbles.