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Para el Reto de noviembre de Beads Perles tenemos que elaborar tres componentes sueltos, que posteriormente pudieran ser montados para formar una joya.
Como todavía no me he olvidado de los pendientes de la reina, he hecho estas tres piezas de aire renacentista, con cabus de 8, rocalla y perlas.
Haré otro trío si alguna idea más termina de tomar cuerpo.
The three components for a proper country village are the church, a good pub and the village shop (the order is interchangeable)
This was the village shop at Tanworth-in-Arden, the main shop faced the village green and at the side was a small Off Licence, the shop and licence holder were displayed on the board as B.O. Tibbles.
The building is listed and has been maintained in good order today. In keeping with the gentrification of a modern "village" the village shop is an Ocado van, the stores are now Ivy House and provides beauty treatments.
Next door is a very tatty and run-down cottage, this has been transformed into a pretty Olde Worlde home of the kind which those with rose-tinted glasses believe had always been there. The reality was very different.
Copyright Geoff Dowling December 1959: All rights reserved
Argh, finally a chance to get some people in my pictures and then I point my camera too high..
Guessed right: it's (pseudo single raw) HDR. The difference between the shadow and sunlit part of the street was far too great.
Photo captured via Minolta MD Zoom Rokkor-X 75-200mm F/4.5 lens. Second Beach. Part of the Quillayute Needles, a consortium of battered islands and sea stacks. Quillayute Needles National Wildlife Refuge. Olympic National Park. Coast Range. Olympic Peninsula. Clallam County, Washington. Late May 2016.
Exposure Time: 1/800 sec. * ISO Speed: ISO-200 * Aperture: F/8 * Bracketing: None
BNS Louise-Marie (F931) is a Karel Doorman-class frigate of the Marine Component of the Belgian Armed Forces that was commissioned in 2008. It is the second of the two frigates of this class that were purchased from the Royal Netherlands Navy on 22 December 2005.
Pictured here departing Portsmouth Naval Base, Hampshire UK after a weekend visit.
The warship is being assisted by SERCO marine tugs SD Tempest
An MoD Police RiB is providing security
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♦️Outfit:{Feral Youth}– Feral Youth–Panda Pals Gacha –Daydream Kid Event
myBro –PandaPals / PandaLove silly hat / PandaPal Blue hoodie/shirt
My dad came up with a way to make my bridge as high or as low as I want it to be. (within some limits) It's not done yet, as we haven't designed the bottom most segment, but it's looking good so far. Just got done making 18 pier components for the bridge, with three sections for each half pier, (soon to be four, if you count the bottom section as yet undesigned.)
Any thoughts?
Oh, almost forget to say: the three bridge pieces in the foreground make up the nearly finished pier in the background.
en.wikipedia.org/wiki/Atlantic_Ocean
The Atlantic Ocean is the second-largest of the world's oceanic divisions. With a total area of about 106,400,000 square kilometres (41,100,000 sq mi),[1] it covers approximately 20% of the Earth's surface and about 26% of its water surface area. The first part of its name refers to Atlas of Greek mythology, making the Atlantic the "Sea of Atlas".
The oldest known mention of "Atlantic" is in The Histories of Herodotus around 450 BC (Hdt. 1.202.4): Atlantis thalassa (Greek: Ἀτλαντὶς θάλασσα; English: Sea of Atlas); see also: Atlas Mountains. The term Ethiopic Ocean, derived from Ethiopia, was applied to the southern Atlantic ocean as late as the mid-19th century.[2] Before Europeans discovered other oceans, the term "ocean" itself was synonymous with the waters beyond the Strait of Gibraltar that we now know as the Atlantic. The early Greeks believed this ocean to be a gigantic river encircling the world.
The Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Eurasia and Africa to the east, and the Americas to the west. As one component of the interconnected global ocean, it is connected in the north to the Arctic Ocean (which is sometimes considered a sea of the Atlantic), to the Pacific Ocean in the southwest, the Indian Ocean in the southeast, and the Southern Ocean in the south. (Other definitions describe the Atlantic as extending southward to Antarctica.) The equator subdivides it into the North Atlantic Ocean and South Atlantic Ocean.
Geography
The Atlantic Ocean is bounded on the west by North and South America. It connects to the Arctic Ocean through the Denmark Strait, Greenland Sea, Norwegian Sea and Barents Sea. To the east, the boundaries of the ocean proper are Europe; the Strait of Gibraltar (where it connects with the Mediterranean Sea–one of its marginal seas–and, in turn, the Black Sea, both of which also touch upon Asia) and Africa.
In the southeast, the Atlantic merges into the Indian Ocean. The 20° East meridian, running south from Cape Agulhas to Antarctica defines its border. Some authorities show it extending south to Antarctica, while others show it bounded at the 60° parallel by the Southern Ocean.[3]
In the southwest, the Drake Passage connects it to the Pacific Ocean. The man-made Panama Canal links the Atlantic and Pacific. Besides those mentioned, other large bodies of water adjacent to the Atlantic are the Caribbean Sea; the Gulf of Mexico; Hudson Bay; the Arctic Ocean; the Mediterranean Sea; the North Sea; the Baltic Sea and the Celtic Sea.
Covering approximately 22% of Earth's surface, the Atlantic is second in size to the Pacific. With its adjacent seas, it occupies an area of about 106,400,000 square kilometres (41,100,000 sq mi);[1] without them, it has an area of 82,400,000 square kilometres (31,800,000 sq mi). The land that drains into the Atlantic covers four times that of either the Pacific or Indian oceans. The volume of the Atlantic with its adjacent seas is 354,700,000 cubic kilometers (85,100,000 cu mi) and without them 323,600,000 cubic kilometres (77,640,000 cu mi).
The average depth of the Atlantic, with its adjacent seas, is 3,339 metres (1,826 fathoms; 10,950 ft); without them it is 3,926 metres (2,147 fathoms; 12,880 ft). The greatest depth, Milwaukee Deep with 8,380 metres (4,580 fathoms; 27,500 ft), is in the Puerto Rico Trench. The Atlantic's width varies from 1,538 nautical miles (2,848 km; 1,770 mi) between Brazil and Sierra Leone to over 3,450 nautical miles (6,400 km; 4,000 mi) in the south
Cultural significance
Transatlantic travel played a major role in the expansion of Western civilization into the Americas. It is the Atlantic that separates the "Old World" from the "New World". In modern times, some idioms refer to the ocean in a humorously diminutive way as the Pond, describing both the geographical and cultural divide between North America and Europe, in particular between the English-speaking nations of both continents. Many British people refer to the United States and Canada as "across the pond", and vice versa
Ocean bottom
The principal feature of the bathymetry (bottom topography) is a submarine mountain range called the Mid-Atlantic Ridge.[5] It extends from Iceland in the north to approximately 58° South latitude, reaching a maximum width of about 860 nautical miles (1,590 km; 990 mi). A great rift valley also extends along the ridge over most of its length. The depth of water at the apex of the ridge is less than 2,700 metres (1,500 fathoms; 8,900 ft) in most places, while the bottom of the ridge is three times as deep. Several peaks rise above the water and form islands.[6] The South Atlantic Ocean has an additional submarine ridge, the Walvis Ridge.[7]
The Mid-Atlantic Ridge separates the Atlantic Ocean into two large troughs with depths from 3,700–5,500 metres (2,000–3,000 fathoms; 12,000–18,000 ft). Transverse ridges running between the continents and the Mid-Atlantic Ridge divide the ocean floor into numerous basins. Some of the larger basins are the Blake, Guiana, North American, Cape Verde, and Canaries basins in the North Atlantic. The largest South Atlantic basins are the Angola, Cape, Argentina, and Brazil basins.
The deep ocean floor is thought to be fairly flat with occasional deeps, abyssal plains, trenches, seamounts, basins, plateaus, canyons, and some guyots. Various shelves along the margins of the continents constitute about 11% of the bottom topography with few deep channels cut across the continental rise.
Ocean floor trenches and seamounts:
•Puerto Rico Trench, in the North Atlantic, is the deepest trench at 8,605 metres (4,705 fathoms; 28,230 ft)[8]
•Laurentian Abyss is found off the eastern coast of Canada
•South Sandwich Trench reaches a depth of 8,428 metres (4,608 fathoms; 27,650 ft)
•Romanche Trench is located near the equator and reaches a depth of about 7,454 metres (4,076 fathoms; 24,460 ft).
Ocean sediments are composed of:
•Terrigenous deposits with land origins, consisting of sand, mud, and rock particles formed by erosion, weathering, and volcanic activity on land washed to sea. These materials are found mostly on the continental shelves and are thickest near large river mouths or off desert coasts.
•Pelagic deposits, which contain the remains of organisms that sink to the ocean floor, include red clays and Globigerina, pteropod, and siliceous oozes. Covering most of the ocean floor and ranging in thickness from 60–3,300 metres (33–1,800 fathoms; 200–11,000 ft) they are thickest in the convergence belts, notably at the Hamilton Ridge and in upwelling zones.
•Authigenic deposits consist of such materials as manganese nodules. They occur where sedimentation proceeds slowly or where currents sort the deposits, such as in the Hewett Curve.
Water characteristics
On average, the Atlantic is the saltiest major ocean; surface water salinity in the open ocean ranges from 33 to 37 parts per thousand (3.3 – 3.7%) by mass and varies with latitude and season. Evaporation, precipitation, river inflow and sea ice melting influence surface salinity values. Although the lowest salinity values are just north of the equator (because of heavy tropical rainfall), in general the lowest values are in the high latitudes and along coasts where large rivers enter. Maximum salinity values occur at about 25° north and south, in subtropical regions with low rainfall and high evaporation.
Surface water temperatures, which vary with latitude, current systems, and season and reflect the latitudinal distribution of solar energy, range from below −2 °C (28 °F). Maximum temperatures occur north of the equator, and minimum values are found in the polar regions. In the middle latitudes, the area of maximum temperature variations, values may vary by 7–8 °C (12–15 °F).
The Atlantic Ocean consists of four major water masses. The North and South Atlantic central waters make up the surface. The sub-Antarctic intermediate water extends to depths of 1,000 metres (550 fathoms; 3,300 ft). The North Atlantic Deep Water reaches depths of as much as 4,000 metres (2,200 fathoms; 13,000 ft). The Antarctic Bottom Water occupies ocean basins at depths greater than 4,000 metres.
Within the North Atlantic, ocean currents isolate the Sargasso Sea, a large elongated body of water, with above average salinity. The Sargasso Sea contains large amounts of seaweed and is also the spawning ground for both the European eel and the American eel.
The Coriolis effect circulates North Atlantic water in a clockwise direction, whereas South Atlantic water circulates counter-clockwise. The south tides in the Atlantic Ocean are semi-diurnal; that is, two high tides occur during each 24 lunar hours. In latitudes above 40° North some east-west oscillation occurs.
Climate
Climate is influenced by the temperatures of the surface waters and water currents as well as winds. Because of the ocean's great capacity to store and release heat, maritime climates are more moderate and have less extreme seasonal variations than inland climates. Precipitation can be approximated from coastal weather data and air temperature from water temperatures.
The oceans are the major source of the atmospheric moisture that is obtained through evaporation. Climatic zones vary with latitude; the warmest zones stretch across the Atlantic north of the equator. The coldest zones are in high latitudes, with the coldest regions corresponding to the areas covered by sea ice. Ocean currents influence climate by transporting warm and cold waters to other regions. The winds that are cooled or warmed when blowing over these currents influence adjacent land areas.
The Gulf Stream and its northern extension towards Europe, the North Atlantic Drift, for example, warms the atmosphere of the British Isles and north-western Europe and influences weather and climate as far south as the northern Mediterranean. The cold water currents contribute to heavy fog off the coast of eastern Canada (the Grand Banks of Newfoundland area) and Africa's north-western coast. In general, winds transport moisture and air over land areas. Hurricanes develop in the southern part of the North Atlantic Ocean. More local particular weather examples could be found in examples such as the; Azores High, Benguela Current, Nor'easter.
History
The Atlantic Ocean appears to be the second youngest of the five oceans. It did not exist prior to 130 million years ago, when the continents that formed from the breakup of the ancestral super continent Pangaea were drifting apart from seafloor spreading. The Atlantic has been extensively explored since the earliest settlements along its shores.
The Vikings, the Portuguese, and the Spaniards were the most famous among early explorers. After Columbus, European exploration rapidly accelerated, and many new trade routes were established.
As a result, the Atlantic became and remains the major artery between Europe and the Americas (known as transatlantic trade). Scientific explorations include the Challenger expedition, the German Meteor expedition, Columbia University's Lamont-Doherty Earth Observatory and the United States Navy Hydrographic Office.
Notable crossings
Ra II, a ship built from papyrus, was successfully sailed across the Atlantic by Thor Heyerdahl proving that it was possible to cross the Atlantic from Africa using such boats in early epochs of history.
•Around 980 – 982, Eric the Red discovered Greenland, geographically and geologically a part of the Americas.
•In 985 or 986, Bjarni Herjólfsson was the first European to sight the Americas. He did not go ashore, though.
•In the year 1000, the Icelander Leif Ericson was the first European to set foot on North American soil, corresponding to today's Eastern coast of Canada, i. e. the province of Newfoundland and Labrador, including the area of land named "Vinland" by Ericson. The Norse discovery was documented in the 13th century Icelandic Sagas and was corroborated by recent L'Anse aux Meadows archeological evidence.
•Around 1010, Thorfinnr Karlsefni led an attempted Viking settlement in North America with 160 settlers, but was later driven off by the natives. His son Snorri Thorfinnsson was the first American born (somewhere between 1010 and 1013) to European (Icelandic) immigrant parents.
•In 1419 and 1427, Portuguese navigators reached Madeira and Azores, respectively.
•From 1415 to 1488, Portuguese navigators sailed along the Western African coast, reaching the Cape of Good Hope.
•In 1492, Christopher Columbus landed on the island of San Salvador in The Bahamas.
•In 1497, John Cabot landed at Bonavista Newfoundland and Labrador.
•In 1500, Pedro Álvares Cabral reached Brazil.
•In 1524, Italian explorer Giovanni da Verrazzano discovered the United States of America's east coast.
•In 1534, Jacques Cartier entered the Gulf of St. Lawrence and reached the mouth of the St. Lawrence River.
•In 1583, Sir Humphrey Gilbert claimed Newfoundland for the English Crown.
•In 1764 William Harrison (the son of John Harrison) sailed aboard the HMS Tartar, with the H-4 time piece. The voyage became the basis for the invention of the global system of Longitude.
•In 1858, Cyrus West Field laid the first transatlantic telegraph cable (it quickly failed).
•In 1865 Brunel's ship the SS Great Eastern laid the first successful transatlantic telegraph cable .
•In 1870 the small City of Ragusa (Dubrovnik) became the first small Lifeboat to cross the Atlantic from Cork to Boston with two men crew, John Charles Buckley and Nikola Primorac (di Costa), only.[9]
•In 1896 Frank Samuelsen and George Harbo from Norway became the first people to ever row across the Atlantic Ocean.
•On April 15, 1912 the RMS Titanic sank after hitting an iceberg with a loss of more than 1,500 lives.[10]
•1914–1918, the First Battle of the Atlantic took place.
•In 1919, the American NC-4 became the first seaplane to cross the Atlantic (though it made a couple of landings on islands and the sea along the way, and taxied several hundred miles).
•Later in 1919, a British aeroplane piloted by Alcock and Brown made the first non-stop transatlantic flight, from Newfoundland to Ireland.
•In 1921, the British were the first to cross the North Atlantic in an airship.
•In 1922, Sacadura Cabral and Gago Coutinho were the first to cross the South Atlantic in an airship.
•In 1927, Charles Lindbergh made the first solo non-stop transatlantic flight in an aircraft (between New York City and Paris).
•In 1931, Bert Hinkler made the first solo non-stop transatlantic flight across the South Atlantic in an aircraft.
•In 1932, Amelia Earhart became the first female to make a solo flight across the Atlantic
•1939–1945, the Second Battle of the Atlantic. Nearly 3,700 Allied ships were sunk at a cost of 783 German U-boats.[11]
•In 1952, Ann Davison was the first woman to single-handedly sail the Atlantic Ocean.
•In 1965, Robert Manry crossed the Atlantic from the U.S. to England non-stop in a 13.5 foot (4.05 meters) sailboat named "Tinkerbell".[12] Several others also crossed the Atlantic in very small sailboats in the 1960s, none of them non-stop, though.
•In 1969 and 1970 Thor Heyerdahl launched expeditions to cross the Atlantic in boats built from papyrus. He succeeded in crossing the Atlantic from Morocco to Barbados after a two-month voyage of 6,100 km with Ra II in 1970, thus conclusively proving that boats such as the Ra could have sailed with the Canary Current across the Atlantic in prehistoric times.[13]
•In 1975, Fons Oerlemans crossed the Atlantic in 82 days, starting from Safi (Morocco) to Trinidad and Tobago, on a selfmade raft.
•In 1980, Gérard d'Aboville was the first man to cross the Atlantic Ocean rowing solo.
•In 1984, Five Argentines sail in a 10-meter-long raft made from tree trunks named Atlantis from Canary Islands and after 52 days 3,000 miles (4,800 km) journey arrived to Venezuela in an attempt to prove travelers from Africa may have crossed the Atlantic before Christopher Columbus.[14][15]
•In 1994, Guy Delage was the first man to allegedly swim across the Atlantic Ocean (with the help of a kick board, from Cape Verde to Barbados).
•In 1998, Benoît Lecomte was the first man to swim across the northern Atlantic Ocean without a kick board, stopping for only one week in the Azores.
•In 1999, after rowing for 81 days and 4,767 kilometres (2,962 mi), Tori Murden became the first woman to cross the Atlantic Ocean by rowboat alone when she reached Guadeloupe from the Canary Islands.
Ethiopic Ocean
The Aethiopian Sea, Ethiopic Ocean or Ethiopian Ocean (Okeanos Aithiopos), is an old name for what is now called the South Atlantic Ocean, which is separated from the North Atlantic Ocean by a narrow region between Natal, Brazil and Monrovia, Liberia. The use of this term illustrates a past trend towards referring to the whole continent of Africa by the name Aethiopia. The modern nation of Ethiopia, in northeast Africa, is nowhere near the Ethiopic Ocean, which would be said to lie off the west coast of Africa. The term Ethiopian Ocean sometimes appeared until the mid-19th century.[
Economy
The Atlantic has contributed significantly to the development and economy of surrounding countries. Besides major transatlantic transportation and communication routes, the Atlantic offers abundant petroleum deposits in the sedimentary rocks of the continental shelves. The Atlantic hosts the world's richest fishing resources, especially in the waters covering the shelves. The major fish are cod, haddock, hake, herring, and mackerel.
The most productive areas include Newfoundland's Grand Banks, the Nova Scotia shelf, Georges Bank off Cape Cod, the Bahama Banks, the waters around Iceland, the Irish Sea, the Dogger Bank of the North Sea, and the Falkland Banks. Eel, lobster, and whales appear in great quantities. Various international treaties attempt to reduce pollution caused by environmental threats such as oil spills, marine debris, and the incineration of toxic wastes at sea.
Terrain
From October to June the surface is usually covered with sea ice in the Labrador Sea, Denmark Strait, and Baltic Sea. A clockwise warm-water gyre occupies the northern Atlantic, and a counter-clockwise warm-water gyre appears in the southern Atlantic. The Mid-Atlantic Ridge, a rugged north-south centerline for the entire Atlantic basin, first discovered by the Challenger Expedition dominates the ocean floor. This was formed by the vulcanism that also formed the ocean floor and the islands rising from it.
The Atlantic has irregular coasts indented by numerous bays, gulfs, and seas. These include the Norwegian Sea, Baltic Sea, North Sea, Labrador Sea, Black Sea, Gulf of Saint Lawrence, Bay of Fundy, Gulf of Maine, Mediterranean Sea, Gulf of Mexico, and Caribbean Sea.
Islands include Newfoundland (including hundreds of surrounding islands), Greenland, Iceland, Faroe Islands, Great Britain (including numerous surrounding islands), Ireland, Rockall, Sable Island, Azores, St. Pierre and Miquelon, Madeira, Bermuda, Canary Islands, Caribbean, Cape Verde, São Tomé and Príncipe, Annobón Province, Fernando de Noronha, Rocas Atoll, Ascension Island, Saint Helena, Trindade and Martim Vaz, Tristan da Cunha, Gough Island (Also known as Diego Alvarez), Falkland Islands, Tierra del Fuego, South Georgia Island, South Sandwich Islands, and Bouvet Island.
Natural resources
The Atlantic harbors petroleum and gas fields, fish, marine mammals (seals and whales), sand and gravel aggregates, placer deposits, polymetallic nodules, and precious stones.
Natural hazards
Icebergs are common from February to August in the Davis Strait, Denmark Strait, and the northwestern Atlantic and have been spotted as far south as Bermuda and Madeira. Ships are subject to superstructure icing in the extreme north from October to May. Persistent fog can be a maritime hazard from May to September, as can hurricanes north of the equator (May to December).
The United States' southeast coast has a long history of shipwrecks due to its many shoals and reefs. The Virginia and North Carolina coasts were particularly dangerous.
The Bermuda Triangle is popularly believed to be the site of numerous aviation and shipping incidents because of unexplained and supposedly mysterious causes, but Coast Guard records do not support this belief.
Hurricanes are also a natural hazard in the Atlantic, but mainly in the northern part of the ocean, rarely tropical cyclones form in the southern parts. Hurricanes usually form between June 1 and November 30 of every year. The most notable hurricane in the Atlantic would be Hurricane Katrina in the 2005 season
Current environmental issues
Endangered marine species include the manatee, seals, sea lions, turtles, and whales. Drift net fishing can kill dolphins, albatrosses and other seabirds (petrels, auks), hastening the fish stock decline and contributing to international disputes.[16] Municipal pollution comes from the eastern United States, southern Brazil, and eastern Argentina; oil pollution in the Caribbean Sea, Gulf of Mexico, Lake Maracaibo, Mediterranean Sea, and North Sea; and industrial waste and municipal sewage pollution in the Baltic Sea, North Sea, and Mediterranean Sea.
In 2005, there was some concern that warm northern European currents were slowing down, but no scientific consensus formed from that evidence.[17]
On June 7, 2006, Florida's wildlife commission voted to take the manatee off the state's endangered species list. Some environmentalists worry that this could erode safeguards for the popular sea creature.
Marine pollution
Marine pollution is a generic term for the entry into the ocean of potentially hazardous chemicals or particles. The biggest culprits are rivers and with them many agriculture fertilizer chemicals as well as livestock and human waste. The excess of oxygen-depleting chemicals leads to hypoxia and the creation of a dead zone.[18]
Marine debris, which is also known as marine litter, describes human-created waste floating in a body of water. Oceanic debris tends to accumulate at the center of gyres and coastlines, frequently washing aground where it is known as beach litter
Bordering countries and territories
The states (territories in italics) with a coastline on the Atlantic Ocean (excluding the Baltic and Mediterranean Seas) are:
Europe
• Belgium
• Denmark
• Germany
• Spain
• France
• Faroe Islands
• Guernsey
• Isle of Man
• Ireland
• Iceland
• Jersey
• Netherlands
• Norway
• Portugal
• Sweden
• United Kingdom
Africa
• Morocco
• Angola
• Benin
• Bouvet Island
• Côte d'Ivoire
• Cameroon
• Democratic Republic of the Congo
• Republic of the Congo
• Cape Verde
• Western Sahara (claimed by Morocco)
• Spain (Canary Islands)
• Gabon
• Ghana
• Guinea
• Gambia
• Guinea-Bissau
• Equatorial Guinea
• Liberia
• Mauritania
• Namibia
• Nigeria
• Senegal
• Saint Helena, Ascension and Tristan da Cunha
• Sierra Leone
• São Tomé and Príncipe
•
South America
• Argentina
• Brazil
• Chile
• Colombia
• Falkland Islands
• France (French Guiana)
• Guyana
• South Georgia and the South Sandwich Islands
• Suriname
• Uruguay
• Venezuela
Caribbean
• Aruba
• Anguilla
• Antigua and Barbuda
• Bahamas
• Saint Barthélemy
• Barbados
• Cuba
• Curaçao
• Cayman Islands
• Dominica
• Dominican Republic
• France (Martinique and Guadeloupe)
• Grenada
• Haiti
• Jamaica
• Saint Lucia
• Saint Martin
• Montserrat
• Netherlands (Caribbean Netherlands)
• Puerto Rico
• Saint Kitts and Nevis
• Sint Maarten
• Turks and Caicos Islands
• Trinidad and Tobago
• Saint Vincent and the Grenadines
• British Virgin Islands
• United States Virgin Islands
Central and North America
• Belize
• Bermuda
• Canada
• Costa Rica
• Greenland
• Guatemala
• Honduras
• Mexico
• Nicaragua
• Panama
• Saint Pierre and Miquelon
• United States
Should have some kind of voltage/warning sticker but I don't have any so these yellow/black stripes should do.
Multiple integrated circuits at the heart of Europe’s space missions, etched together onto a single piece of silicon.
This 20 cm-diameter wafer contains 35 replicas of five different space chips, each incorporating up to about 10 million transistors or basic circuit switches.
Laid down within a microchip, these designs endow a space mission with the ability to perform various specialised tasks such as data handling, communications processing or attitude control.
To save money on the high cost of fabrication, various chips designed by different companies and destined for multiple ESA projects are crammed onto the same silicon wafers, etched into place at specialised semiconductor manufacturing plants.
Once tested for functionality, the chips on the wafer are chopped up and packaged for use, then mounted on printed circuit boards for connection with other microelectronic components aboard a satellite.
Since 2002, ESA’s Microelectronics section has maintained a catalogue of ‘building blocks’ for chip designs, known as Intellectual Property cores, available to European industry through ESA licence.
More information: www.esa.int/Our_Activities/Space_Engineering_Technology/M...
Credit: ESA-Guus Schoonewille
Ngorongoro Conservation Area.
Un piccolo gruppo di zebre componenti una mandria di alcune decine di capi.
Ngorongoro Conservation Area.
A small group of zebras forming a herd of several dozen animals.
IMG_9414m
Odeon: The Odeon is located to the Northwest of the Stadium. It had a capacity to accommodate 800 spectators and archaeologists are of the opinion that the Odeon was used for musical performances or for conducting classes in rhetoric.
Stadium: The Stadium is located to the Southeastern part of the hill and was excavated by the Italians during their rule of the island of Rhodes. The stadium was all of 600 feet in length. At present the only original components are the Sphendone, Proedries and a few rows of seats in the auditorium. Also preserved is The starting apparatus used in athletic events too is well preserved.
Acropolis of Rhodes (Greece)
Thank you to all who view, favorite, and comment...
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Imagine Peace
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peace takes work
war takes lives
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If everyone demanded peace instead of another television set, then there'd be peace.
- John Lennon
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Peace is always beautiful
- Walt Whitman
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Some cool turning parts images:
Pont Alexandre III
Image by David McA Photographs
A long exposure shot of the Seine at the Pont Alexandre III, a wonderfully ornate bridge more than the Seine by the Grand Palais in Paris.
I liked the way that the low evening sun lit up the gilded parts of the...
Read more about Cool Turning Components photos
(Posted by a Precision Machining China Manufacturer)
Taken with Polaroid SX-70 | Polaroid Time Zero (exp. 12/06) | Jun18 | If you could stretch a given minute what would you find between its unstuck components? ―Don DeLillo, Great Jones Street, 121 | New York City, NY
Olympus OM-2N, Zuiko 50 mm f/1.8, KODAK Color Plus 200 ASA
Scanner EPSON V600 - 2400 dpi
1877 Santo Saccomanno fece
Il monumento, datato 1877, fu eretto per disposizione di Giovanni Battista Noli Da Costa, alla memoria del patrizio portoghese Faustino Antonio Da Costa che, morendo a Genova ottuagenario, lasciò erede il figlio adottivo. Non presenta complesse allegorie, ma una scena di compianto d’intonazione realista. L’erede è rappresentato intento a contemplare per un’ultima volta, con espressione di memore affetto, la salma del vecchio che, deposta sul sarcofago, a breve sarà chiusa nel sepolcro.
SANTO SACCOMANNO (Genova 1833 - 1914)
Dopo avere seguito i corsi di Varni all'Accademia Ligustica, Saccomanno intraprese l'attività di scultore, alternando ritrattistica e scultura funeraria. Partito da un sobrio realismo di ascendenza romantica (Tomba Chiarella, 1872), ne radicalizzò la componente analitica, sortendo talvolta effetti di crudo verismo (Tomba De Costa, 1877) e arrivando addirittura a definire le lacrime della figura dolente nella Tomba Nicolò Lavarello (1890). Quest'ultima è una variante sul tema del "Sonno Eterno"- già proposto nella Tomba Carlo Erba (1883) e nella Tomba Acquarone (1899) - uno dei più adatti ad esprimere la pessimistica concezione della morte di Saccomanno.
www2.comune.genova.it/portal/template/viewTemplate?templa...
it.wikipedia.org/wiki/Cimitero_monumentale_di_Staglieno
genovacultura.org/evento/cimitero-di-staglieno-il-realism...
The green toenail of the statue, the names in gold, the Belgian blue stone and the liberation photo: the pieces of a puzzle of historic reality, now long gone.
Just like astronauts themselves, each and every part to be used in a spacecraft goes through exhaustive testing, guided by ESA-backed standards - just ask Circuit the Component...
Credit: ESA – Ed Grace
Belgian Air Component F-16 'Fighting Falcon' at RAF Waddington during Exercise Cobra Warrior 2023.
Long range fuel tanks, 2 x AIM-120 missiles on the wingtips, 2 x AIM-9 'Sidewinder' missiles under the wingtips, and a 'Sniper' targeting pod under the fuselage.
Also note the 20mm gun port just above the port wing strake.
Componente del Grupo "Avant Garde Dance", que con el espectáculo de variedades "The Silver Tree" nos cautivaron en el Festival Internacional de Teatro y Artes de Calle de Valladolid (2010).
en.wikibooks.org/wiki/Quantum_theory_of_observation/Quant...
Quantum theory of observation - Thierry Dugnolle
Quantum physics for dummies
Fundamental principles and concepts
Examples of measurements
Entanglement
General theory of measurement
The forest of destinies
The appearance of relative classical worlds in the quantum Universe
Quantum entanglement is the fundamental concept to explain the reality of observation.
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Wave-particle duality
Is light a flow of particles or a wave phenomenon ? Light rays could be particle paths and they were regarded thus by Newton in his Optics. Light reflection in a mirror is then naturally interpreted with the hypothesis that particles of light, or photons, are like bouncing balls. Nevertheless Huygens argued that this phenomenon and others were better interpreted with the hypothesis that light rays are perpendicular lines to wave fronts.
Photography gives an evidence of the existence of particles of light, for traces left by light are always like impacts of particles.
But if light is made of particles how can we explain interference patterns such as those found by Young and Fresnel ? Interference is always interference between waves. It seems there can not be any interference with particles. An interference pattern is an experimental evidence that light is a wave phenomenon. It is confirmed by Maxwell's theory of electomagnetism, which defines light as an electromagnetic wave.
That light be made of particles is not contradicted by the existence of interference patterns. Here is what we can see if we look at how an interference pattern appears on a photographic plate (see photo - animated in original publication)
The wave phenomenon, interference, results from impacts of particles.
The superposition principle gives a very direct explanation of wave-particle duality. Any physical system is a particle or a system of particles, but these behave sometimes like waves because they can be in many places at the same time. The wave of a particle or of a system of particles determines its diffuse presence.
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Stanford Encyclopedia of Philosophy
seop.illc.uva.nl/entries/qt-entangle/
1. Quantum Entanglement
In 1935 and 1936, Schrödinger published a two-part article in the Proceedings of the Cambridge Philosophical Society in which he discussed and extended an argument by Einstein, Podolsky, and Rosen. The Einstein-Podolsky-Rosen (EPR) argument was, in many ways, the culmination of Einstein’s critique of the orthodox Copenhagen interpretation of quantum mechanics and was designed to show that the theory is incomplete. (See the entries on the Einstein-Podolsky-Rosen argument in quantum theory and the Copenhagen interpretation of quantum mechanics.)
In classical mechanics the state of a system is essentially a list of the system’s properties — more precisely, it is the specification of a set of parameters from which the list of properties can be reconstructed: the positions and momenta of all the particles comprising the system (or similar parameters in the case of fields).
The dynamics of the theory specifies how properties change in terms of a law of evolution for the state. In a letter to Max Born, Wolfgang Pauli characterized this mode of description of physical systems as a ‘detached observer’ idealization (see The Born-Einstein Letters, Born, 1992; p. 218).
On the Copenhagen interpretation, such a description is not possible for quantum systems. Instead, the quantum state of a system should be understood as a catalogue of what an observer has done to the system and what has been observed, and the import of the state then lies in the probabilities that can be inferred (in terms of the theory) for the outcomes of possible future observations on the system.
Einstein rejected this view and proposed a series of arguments to show that the quantum state is simply an incomplete characterization of a quantum system. The missing parameters are sometimes referred to as ‘hidden parameters’ or ‘hidden variables.’
It should not be supposed that Einstein’s notion of a complete theory included the requirement that the theory should be deterministic. Rather, he required certain conditions of separability and locality for composite systems consisting of separated component systems: each component system separately should be characterized by its own properties (its own ‘being-thus,’ as Einstein put it — ‘So-sein’ in German), and it should be impossible to alter the properties of a distant system instantaneously (or the probabilities of these properties) by acting on a local system.
In later analyses, notably in Bell’s argument for the nonlocality of quantum correlations, it became apparent that these conditions, suitably formulated as probability constraints, are equivalent to the requirement that statistical correlations between separated systems should be reducible to probability distributions over common causes (deterministic or stochastic) in the sense of Reichenbach. (See the entries on Bell’s theorem and Reichenbach’s common cause principle.)
Copyright © 2021 by Craig Paup. All rights reserved.
Any use, printed or digital, in whole or edited, requires my written permission.
In this photo I have the units broken into groups, Armoured, Artillery, Engineers, Transport, SF, Historical and RAEME
These are the patterns I made with the skinner blend roll to use in making my purple kaleidoscope cane.
Holden Torana SL/R, probably a LH fitted with some LX components and trim then modified to represent a LX SL/R 5000 A9X
Various dots grabbed today as follows:
Main:
Caught South of Gatwick at 41,000 feet, Singapore Airlines Cargo Boeing 747-412F(SCD) 9V-SFP slips by as SIA7973 on her way from LA to Brussels
Top left:
Air Malta's Airbus A320-251N 9H-NEB climbing through 21,000 feet as AMC7101 on route Luqa from Heathrow
Top right:
UAE9962 aka Emirates Sky Cargo Boeing 777-F1H A6-EFK trails East over Sussex at 37,000 feet all the way from Houston, Texas towards her Belgian, destination of Maastricht
And lastly, seen streaking across Sussex at 35,000 feet was Belgian Air Component's Dassault Falcon 7X call-sign 'BAF76' aka OO-LUM, one of two civilian examples leased for their 'white fleet' use. This one was out of St. Mawgan and presumably still crew training and on her way back to Belgium. See:
www.aviation24.be/military-aircraft/belgian-air-component...
276A1760, 276A763, 276A764 & 276A766
On 1 July 1933 the vast majority of the ownership and operation of public transport in London was transferred to the newly formed London Passenger Transport Board, better known as London Transport. For the city's tram network this at last saw a common ownership and operation of services that had previously been under multiple undertakings, both municipally and privately owned.
The largest component was that of the London County Council whose tramways operation was highly developed and well run. The LCCT services, that used conduit as well as overhead operation, had several inter-running agreements with both other municipalities (mostly in east London) as well as the three operators owned by the Underground group. These were the Metropolitan Elelectric, the London United and the South Metropolitan Elecric Tramways & Lighting Co Ltd. In summer of 1933 the variously issued maps and guides of the pre-amalgamation concerns appear to have been issued simply overstamped with the details of the new organisation and this November 1933 is, I think, the first attempt at a single map to cover all the merged routes.
It is wholly based on the old LCC map and guide that has been modified to an extent. On the map the old concept of showing the LCC services in a thick red line and connecting or inter-running routes in a thin red line has been perpetuated, the main difference being that in the key the previous distnctions ahve vanished to be replaced by a single line referring to fare sections and route numbers. The map now has the TramwayS logo of the old Underground group now adapted to show London Transport in the semi-circles. It also has an inset to show the ex-Croydon Corporation network. However the LCC evening classes advert survives! The cover also follows the pattern of LCC covers showing a work of art or illustration derived from an advert or poster. This illustration, of the old Waterloo Bridge than trams ran under, along the Subway and Embankment, rather than over is from a series of 1932/33 press adverts issued by the Underground and General companies on London's river crossings and is by, I am sure, R Austin whose "A" can just be made out.
The route guide and timetables now has all London's tram routes shown, no longer with the old LCC convention of north or south of the Thames. The list also shows, as well as night trams, the "unnumbered services" inherited from the various east and south-east London operators that had never been given such information. The other interesting panel is the appearance of the relavtively new trolleybus routes in the Kingston area. The LUT had started in 1931 to look at conversion of tram operations not to motor bus but electric trolleybus to utilise the heavy capital investment in electricity generation and distribution that had continued value unlike the depreciated first generation tramcars. The trolleybus soon became the 'way forward' for the new London Transport and over the next few years the tram map steadily became the trolleybus and tram map - a distinction that continued until the final war delayed abandonment of the 'last tram' in 1952. The trolleybus routes here carry their original route numbers before the addition of 6** (or 5**) numbers to the tram routes they replaced in later conversions and when Kingston's routes were re-numbered in the new sequence.
In 1934 LT's cartographers had got to work and a completely new version of the tram/trolleybus map, in the same style as motor bus, Country bus and Green Line operations was issued.
Dissociative identity disorder (DID), previously known as multiple personality disorder (MPD), is an extremely rare mental disorder characterized by at least two distinct and relatively enduring identities or dissociated personality states that alternately control a person's behavior, and is accompanied by memory impairment for important information not explained by ordinary forgetfulness. These symptoms are not accounted for by substance abuse, seizures, other medical conditions, nor by imaginative play in children. Diagnosis is often difficult as there is considerable comorbidity with other mental disorders. Malingering should be considered if there is possible financial or forensic gain, as well as factitious disorder if help-seeking behavior is prominent.
DID is one of the most controversial psychiatric disorders with no clear consensus regarding its diagnosis or treatment. Research on treatment effectiveness still focuses mainly on clinical approaches and case studies. Dissociative symptoms range from common lapses in attention, becoming distracted by something else, and daydreaming, to pathological dissociative disorders.[6] No systematic, empirically-supported definition of "dissociation" exists.
Although neither epidemiological surveys nor longitudinal studies have been done, it is thought DID rarely resolves spontaneously. Symptoms are said to vary over time.In general, the prognosis is poor, especially for those with co-morbid disorders. There are few systematic data on the prevalence of DID. The International Society for the Study of Trauma and Dissociation states that the prevalence is between 1 and 3% in the general population, and between 1 and 5% in inpatient groups in Europe and North America.[5] DID is diagnosed more frequently in North America than in the rest of the world, and is diagnosed three to nine times more often in females than in males. The prevalence of DID increased greatly in the latter half of the 20th century, along with the number of identities (often referred to as "alters") claimed by patients (increasing from an average of two or three to approximately.DID is also controversial within the legal system[3] where it has been used as a rarely-successful form of the insanity defense.The 1990s showed a parallel increase in the number of court cases involving the diagnosis.
Dissociative disorders including DID have been attributed to disruptions in memory caused by trauma and other forms of stress, but research on this hypothesis has been characterized by poor methodology. So far, scientific studies, usually focusing on memory, have been few and the results have been inconclusive. An alternative hypothesis for the etiology of DID is as a product of techniques employed by some therapists, especially those using hypnosis, and disagreement between the two positions is characterized by intense debate.DID became a popular diagnosis in the 1970s, 80s and 90s but it is unclear if the actual incidence of the disorder increased, if it was more recognized by clinicians, or if sociocultural factors caused an increase in iatrogenic presentations. The unusual number of diagnoses after 1980, clustered around a small number of clinicians and the suggestibility characteristic of those with DID, support the hypothesis that DID is therapist-induced.[15] The unusual clustering of diagnoses has also been explained as due to a lack of awareness and training among clinicians to recognize cases of DID
Signs and symptoms]
According to the fifth Diagnostic and Statistical Manual of Mental Disorders (DSM), DID includes "the presence of two or more distinct identities or personality states" that alternate control of the individual's behavior, accompanied by the inability to recall personal information beyond what is expected through normal forgetfulness. In each individual, the clinical presentation varies and the level of functioning can change from severely impaired to adequate. The symptoms of dissociative amnesia, dissociative fugue and depersonalization disorder are subsumed under the DID diagnosis and are not diagnosed separately. Individuals with DID may experience distress from both the symptoms of DID (intrusive thoughts or emotions) as well as the consequences of the accompanying symptoms (dissociation rendering them unable to remember specific information). The majority of patients with DID report childhood sexual and/or physical abuse, though the accuracy of these reports is controversial. Identities may be unaware of each other and compartmentalize knowledge and memories, resulting in chaotic personal lives.Individuals with DID may be reluctant to discuss symptoms due to associations with abuse, shame and fear. DID patients may also frequently and intensely experience time disturbances.
The number of alters varies widely, with most patients identifying fewer than ten, though as many as 4,500 have been reported. The average number of alters has increased over the past few decades, from two or three to now an average of approximately 16. However it is unclear whether this is due to an actual increase in alters, or simply that the psychiatric community has become more accepting of a high number of alters.The primary identity, which often has the patient's given name, tends to be "passive, dependent, guilty and depressed" with other personalities or "alters" being more active, aggressive or hostile, and often containing more complete memories. Most identities are of ordinary people, though fictional, mythical, celebrity and animal alters have also been reported.
Developmental trauma]
People diagnosed with DID often report that they have experienced severe physical and sexual abuse, especially during early to mid-childhood, (although the accuracy of these reports has been disputed and others report an early loss, serious medical illness or other traumatic event. They also report more historical psychological trauma than those diagnosed with any other mental illness.[not in citation given]Severe sexual, physical, or psychological trauma in childhood has been proposed as an explanation for its development; awareness, memories and emotions of harmful actions or events caused by the trauma are removed from consciousness, and alternate personalities or subpersonalities form with differing memories, emotions and behavior. DID is attributed to extremes of stress or disorders of attachment. What may be expressed as post-traumatic stress disorder in adults may become DID when occurring in children, possibly due to their greater use of imagination as a form of coping. Possibly due to developmental changes and a more coherent sense of self past the age of six, the experience of extreme trauma may result in different, though also complex, dissociative symptoms and identity disturbances. A specific relationship between childhood abuse, disorganized attachment, and lack of social support are thought to be a necessary component of DID. Other suggested explanations include insufficient childhood nurturing combined with the innate ability of children in general to dissociate memories or experiences from consciousness.
Delinking early trauma from the etiology of dissociation has been explicitly rejected by those supporting the early trauma model. However, a 2012 review article supports the hypothesis that current or recent trauma may affect an individual's assessment of the more distant past, changing the experience of the past and resulting in dissociative states. Giesbrecht et al. have suggested there is no actual empirical evidence linking early trauma to dissociation, and instead suggest that problems with neuropsychological functioning, such as increased distractibility in response to certain emotions and contexts, account for dissociative features. A middle position hypothesizes that trauma, in some situations, alters neuronal mechanisms related to memory. Evidence is increasing that dissociative disorders are related both to a trauma history and to "specific neural mechanisms". It has also been suggested that there may be a genuine but more modest link between trauma and DID, with early trauma causing increased fantasy-proneness, which may in turn render individuals more vulnerable to socio-cognitive influences surrounding the development of DID.
dédoublement de personnalité
Il est important de différencier deux termes : le dédoublement de la personnalité et la personnalité multiple.
En effet, la définition donnée est celle de la , qui fait qu'une personne possède deux (voire plus) personnalités complètement différentes, chacune ayant une vie sociale et professionelle distinctes, parfois un nom propre à chacune d'entre elles et étant parfaitement adaptées à leur(s) milieu(x). Ce n'est pas vraiment un trouble, mais une surconstruction personnelle donnant naissance à plusieurs personnalités au lieu d'une seule.
Le dédoublement de personnalité, en revanche, est un trouble de la personnalité provoqué par le subconscient, qui impose occasionnellement à la personnalité "normale" un comportement incohérent, parfois violent, incontrôlé. Il arrive que la personnalité première ne se rende plus compte de ce qu'elle fait (elle est "déconnectée") ce qui donne l'impression d'une autre personnalité, inadaptée socialement , sentimentalement et intellectuelement.
Ce sujet prète à polémique, car certains se contentent du terme troubles dissociatifs de l'identité (Dissociative Identity Disorder) pour englober les deux cas. La différence est de taille : avec cette notion, il n'y aurait pas plusieurs personnalités égales, mais une majeure à laquelle on doit redonner pleine maîtrise de son corps. Comme expliqué plus haut, ce serait dans un cas de dédoublement que l'on peut envisager cette façon de voir les personnalités, et non dans un cas de multiples personnalités. En effet, comment décider qu'une personnalité a plus de droit qu'une autre sur un corps, lorsqu'il n'y en a pas d'originelle ?
Je pense que le sens donné est le sens courant, non ? On peut rajouter des précisions ou mises en garde sur le sens technique du point de vue médical. Lmaltier 18 décembre 2007 à 17:05 (UTC)
En fait, les deux sont liées pour la plupart des gens, c'est pour cela qu'il faut les différencier : on a tendance à croire que les personnes ayant des personnalités multiples sont dangeureuses, peuvent avoir des accès de violence incontrolée dirigés par une personnalité instable. Ce n'est souvent pas le cas (même si c'est possible, comme pour n'importe quelle personnalité dite "normale"). Ce n'est donc pas sur un plan médical qu'il est important de les différencier, mais sur un plan humain : les personnalité multiples sont des personnalités tout ce qu'il y a de plus banales, mais sont persécutées à cause de la mauvaise image que l'on a d'elles, dûe aux dédoublement de personnalités qui, eux, sont des cas de dissociation de personnalités potentiellement dangereux car instables. S Vidal 20 décembre 2007 à 13:20 (UTC)
Peut-être, mais on étudie le mot, pas la maladie (faut voir Wikipédia pour ça). On peut mettre en garde sur les différents sens utilisés, mais c'est tout. Lmaltier 20 décembre 2007 à 17:21 (UTC)
mais justement, le problème est là ! on utilise un même mot pour deux choses différentes... si la définition du mot est faussée, l'étude de ce mot n'a pas lieu d'être, pas sans précisions...
PRECISION:
Il n'y a pas de différence entre ces deux troubles, ils n'en forment en vérité qu'un seul. Le trouble de la personnalité multiple était le nom donné auparavent à cet état, et maintenant il s'appelle Trouble dissociatif de l'identité. Dans les deux cas (puisque ça n'est en fait qu'une maladie) des traumas subits de façon répétitifs ont poussé la personnalité de l'enfant à se dissocier, pour pouvoir supporter les chocs traumatiques, le manque d'attention, etc. Les personnalités apparaissent à différents moments, et peuvent même restées complètement cachées jusqu'assez tard dans la vie d'un individu, avant les premières vraies crises, souvent dues à un stress ou un choc émotionnel important. Elles ont différent degrés de constructions émotionnelles, intellectuelles et sociales, ce qui peut penser à une structure de multiples personnalités toutes égales. Il n'en est en fait rien. même quand on parle de personnalité hote qui doit rester alors que les autres doivent disparaitre, ce n'est pas encore tout à fait juste. Toutes les peronnalités doivent, petit à petit à petit et au long d'une thérapie qui apprendra au patient multiple à se construire et trouver le moyen d'affronter autrement ses traumas passés et à venir, fusionner et ne redevenir qu'une seule et même entité, plus stable, et capable de vivre pleinement sa vie.
dédoublement de la personnalité[modifier]
Ma soeur jumelle souffre de ce trouble depuis l'âge de 16 ans mais ne le reconnait que depuis peu,depuis sa première grosse crise. Elle peut changer de comportement d'une minute à l'autre,laissant place à une femme extravertie et sans limites..alcool,hommes,jeux.. Souvent il lui arrive de se réveiller sans souvenirs de la veille et découvre que son compte en banque a fondu p.ex. Elle devient également plus brusque,plus mauvaise.quand l'alcool s'en mêle elle n'a plus de limites et se bagarre violement(en général avec des hommes)et fini parfois à l'hôpital après avoir brutalisé le personnel infirmier.La plupart du temps perd connaissance. Mais reste persuadée que rien de tout ça ne s'est produit.. Qu'y a-t-il à faire pour atténuer cette maladie?Existe-t-il un moyens de guérison?
Ma plus grande question,pouvons-nous faire confiance aux personnes atteintes de ce trouble?
Il existe un moyen. Il faut emmener la personne a l'hopital, et les medecins vous donnerons un planing a respecter. (ex: ce coucher a une heure exacte et ne pas manger n'importe quoi). mais attention il faut emmener la personne au plus vite a l'hopital car elle peut passer a l'acte.