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LONDON, ENGLAND - MAY 07: Moon "Oner" Hyeon-joon of T1 at the League of Legends - Mid-Season Invitational Features Day on May 7, 2023 in London, England. (Photo by Colin Young-Wolff/Riot Games)
"Ichabod" is based on the ghost story by Washington Irving; "Mr. Toad" is a free adaptation of Kenneth Grahame's classic, THE WIND IN THE WILLOWS.
This enjoyable 1949 release marked the end of Disney's anthology features of the 1940s and paved the way for CINDERELLA. ALICE IN WONDERLAND, PETER PAN, and other '50s features.
The Headless Horseman chase is brilliantly animated!
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ISTANBUL, TURKEY - AUGUST 27: Koji "Laz" Ushida of Zeta Division poses at VALORANT Champions 2022 Istanbul Features Day on August 27, 2022 in Istanbul, Turkey. (Photo by Lance Skundrich/Riot Games)
Inamorata Tumaini features the young and adorably grumpy Akech sculpt in Chocolate resin and M bust 4.0 athletic body. Her custom hard cap wig is needle felted mohair wool over poseable copper frame. The inspiration of her fashion was a African quilted dress, but miniaturise it we went for a printed quilt pattern instead (miniature quilting seams would be quite stiff and bulky). To make the traditional look more young and trendy, I reinterpreted the empire waist dress as a crop top and skirt.
* Commissioned art doll and not for sale.
•Set includes a spring-loaded Spell Launcher with fiery shots, disguised as a craggy rock
•Push the button on the Frost Dragon’s back and make her head strike downward
The photo features a striking nighttime panorama of Shanghai's Lujiazui area, highlighting the city's architectural prowess with towering skyscrapers adorned in colorful lights. Prominent structures such as the Oriental Pearl Tower and the Jin Mao Tower stand out against the dark sky, while the red Monument to the People's Heroes adds a splash of color to the urban landscape. The steel truss of Waibaidu bridge in the foreground provides a sense of scale and depth, leading the viewer's eye across the water towards the cityscape. The overall mood is one of awe-inspiring modernity and cultural significance, encapsulating the dynamic energy of China's financial hub.
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REYKJAVIK, ICELAND - APRIL 7: Team ZETA DIVISION poses for the VALORANT Masters Features Day on April 7, 2022 in Reykjavik, Iceland. (Photo by Lance Skundrich/Riot Games)
• Features a sleek satin mini dress with a smooth, glossy finish
• Designed with delicate spaghetti straps and a flattering draped neckline
• Showcases an elegant cowl neck for a soft, luxurious silhouette
• Crafted with a figure-hugging fit that accentuates the body
• Available in 7 color options, sold separately
• Fatpack available at a discounted price
• Rigged for Reborn, Legacy & MaitreyaX
• Copy / Modify / No Transfer
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•Fly the War Bee onto its landing platform
•Drop rocks on enemies below the causeway
•Fire the Ustokal’s spring-loaded siege crossbow
Russian postcard, no. 134.
Vera Kholodnaya (1893-1919) was the first star of the Russian silent cinema. Only 26, the ‘Queen of Screen’ died of the Spanish flu during the pandemic of 1919. Although she worked only three years for the cinema, she must have made between fifty and a hundred short films. The Soviet authorities ordered to destroy many of the Kholodnaya features in 1924, and only five of her films still exist.
Vera Kholodnaya (Russian: Вера Холодная, and also romanized as Vera Kholodnaia and Vira Kholodna) was originally named Vera Vasilyevna Levchenko. She was born into a respectable well-to-do family in Poltava, Russian Empire (now Ukraine) in 1893. Her whole family enjoyed acting in plays. At the age of ten, she was sent to Moscow to live with her widowed grandmother. There she attended the elite Perepelkina Grammar school. The girl dreamed of a career in classical ballet and even enrolled at the Bolshoi Theatre ballet school. That changed in 1908, when Vera attended a performance of the film Francesca da Rimini, with ballerina Vera Komissarzhevskaya in the title role. She was deeply impressed with Komissarzhevskaya's artistry and now was set on becoming an actress. In 1910, the 17-years old married student Vladimir Kholodny, one of the first Russian car racers. Later he became the editor of the magazine AVTO. 1915. Vera would often accompany him in races which resulted in road accidents. She also adopted his surname, which translates as ‘the cold one’ Their daughter, Eugenia Kholodnaya, was born in 1912, and they adopted another daughter, Nonna Kholodnaya, a year later. After her husband was drafted to fight in World War I, she decided to venture into film acting. She first approached Vladimir Gardin, a leading Russian film director, who cast her in a minor role in his grand production of Anna Karenina (Vladimir Gardin, 1914) with Mariya Germanova in the title role. Then director Yevgeni Bauer was looking for a woman of outstanding beauty for a new film. When Kholodnaya was introduced to him, Bauer reportedly was spellbound of the small, intense woman with her commanding grey eyes and mop of black hair. Bauer at once approved her for the part, the lead role in the Ivan Turgenev adaptation Pesn torzhestvuyushchey lyubvi/The Song of the Triumphant Love (Yevgeni Bauer, 1915). This mystical love drama was a major box-office hit, and she signed a three-year contract with the Khanzhonkov studio. The impatient Bauer immediately made another film with his new discovery, Plamya Neba/Flame of the Sky (Yevgeni Bauer, 1915). It was a typical melodrama about the guilty love of a young woman married off to an old widower and his son. In the end, the lovers perish from a thunderbolt. Her next picture was Deti veka/The Children of the Age (Yevgeni Bauer, 1915), a drama with pretensions to reveal social problems. Bauer’s death in 1917 robbed the Russian cinema of one of its great talents, and Kholodnaya of her discoverer. Soon followed more films for her made by other directors. At first, Kholodnaya imitated the acting of Asta Nielsen, but gradually she developed her own style. Another tremendous success was the tragic melodrama Mirazhi/The Mirages (Pyotr Chardynin, 1915). Her extravagant costumes and large grey eyes made her an enigmatic screen presence which fascinated audiences all over Russia.
The melodrama Zhizn za zhizn/A Life for a Life (Yevgeni Bauer, 1916) became one of the most popular films in Vera Kholodnaya’s career. After this film, she was called ‘the Queen of Screen’. The author of this title was the famous singer Alexander Vertinsky who venerated the actress and frequented her house. In 1916 Khanzhonkov’s company started making the film Pierrot with Vertinsky and Kholodnaya playing the leads. Unfortunately, the film was never completed. By the time of the Russian Revolution, a new Kholodnaya film was released every third week. U kamina/By the Fireplace (1917), based on a popular romance, was another resounding commercial success. The film ran in cinemas until 1924 when the Soviet authorities ordered to destroy many of the Kholodnaya features. During the Russian Civil War, the Bolshevik authorities requested film companies to produce less melodrama and more adaptations of classics. Accordingly, Kholodnaya was cast in a screen version of Tolstoy's Zhivoy trup/The Living Corpse (Cheslav Sabinsky, 1917). Her acting abilities in this film were applauded by Stanislavsky, who welcomed Vera to join the troupe of the Moscow Art Theatre. Her last box-office sensation was Molchi, grust... molchi/Be Silent, My Sorrow, Be Silent (Pyotr Chardynin, Cheslav Sabinsky, 1918). Like many of her films, it was based on a Russian traditional love song. By that time, Kholodnaya turned from just a popular and admired actress into a legend of the Russian cinema. She decided to move with her film company to Odessa. There she died at the age of 25 in the 1918 flu pandemic. A director with whom she had worked for several years filmed her grand funeral. Ironically, this seems to be her best known film today. The other five extant films with Vera Kholodnaya are: Deti veka/The Children of the Age (1915), Mirazhi/The Mirages (1915), Zhizn za zhizn/A Life for a Life (1916), Zhivoy trup/The Living Corpse (1918), and Molchi, grust... molchi/Be Silent, My Sorrow, Be Silent (1918). Official Russian records state that Vera Kholodnaya died of the Spanish flu. While that seems quite likely, there is much speculation around her death. Оther stories claim she was poisoned by the French ambassador with whom she reportedly had an affair and who believed that she was a spy for the Bolsheviks. Her husband, Vladimir Kholodny, died 2 months after her. Her mother, Yekaterina Sleptsova, also died shortly after her. Her life was dramatized in Nikita Mikhalkov's film Raba lyubvi/A Slave of Love (1975), and in director, Oleg Kovalov made a documentary on her life, Ostrov Myortvykh/Island of the Dead (1992). A year later, her image was depicted on a postage stamp and in 2003 a life-size bronze statue of her was erected in Odessa, Ukraine; created by the artist Alexander P. Tokarev.
Sources: Jessica Keaton (Silence is platinum), KinoTV.com (German), Russia-IC, Wikipedia and IMDb.
And, please check out our blog European Film Star Postcards.
The Econ features so prominently in my photostream and has its own dedicated gallery because its such a fun river to hike and photograph. The fact that its course remains unaltered and relatively wild (unlike spoiled treasures like the Kissimmee River) make it a rarity in Central Florida.
This view features the old Kirkby South signal box and signals 28/29 which were shown on the opposite side of the Branch line on the Signal Box track diagram. Also of interest is the infamous Up passenger train 1O42, which we always knew as the "York-Bournemouth" That train continued to run right up to the final through working on Saturday 3 September 1966.
Now, a bit about the possible date and loco identity:
I have a contact who has amassed quite a bit of data about 1O42 (and the return working 1N83) trains. Also he has a lot of info on the Brush Type 2 diesels.
It transpires that the Brush Type 2 in the photo has English Electric exhaust ports in the roof. D5677 was the prototype for the engine replacement, in April 1964, with no others being done until February 1965. By that time Doncaster was also doing another modification, the little shields over the windscreen washer nozzles. As far as it is known D5677 was the only loco from GC times that combined English Electric exhaust ports with no shields over the windscreen washer nozzles. (There's one other known exception, D5500, which was one of the last to be re-engined and somehow never got the shields over the windscreen washer nozzles; it is still without them in the NRM).
So it is strongly believed that the photo is of D5677. However, I having a nagging feeling that the 3rd digit of the loco number doesn't look like a '7'. So if anyone else has evidence to identify the date and loco number I'd be pleased to hear their views.
Therefore, unless proved otherwise, I am saying:
D5677 was a Finsbury Park loco when first re-engined but reallocated to Tinsley in November 1964 so the photo was probably taken after that.
There are no leaves on the branches in the left of the shot. so the time would be around winter.
D5677 is known to have worked 1N83 on Saturday 21 November 1964. It is plausible this Kirkby Bentinck picture could be on this date as the 1O42 stock in the picture is the SR rake.
The only other known working for D5677 on 1O42/1N83 is an unidentified date in the week 10-14 May 1965 from a photo of 1N83 in the RCTS photo archive, but the Kirkby Bentinck photo is not that date.
In both instances there's also known workings of D5677 on Cleethorpes-Kings Cross trains around the same time. This suggests in both periods Tinsley were using D5677 as a Type 3 loco.
And it could, of course, be that the photo is of a loco working that is not known about at this moment. There are suspicions that D5677 probably did 1O42/1N83 more than once in November-December 1964, so we can't say for certain that the photo is Saturday 21 November 1964.
Finally, as things stand at present, there's no known workings on 1O42/1N83 of English Electric powered Brush T2s, apart from the 2 known D5677 workings. Finding another one would be an interesting development ........ Over to you !!!!!
BUSAN, SOUTH KOREA - MAY 18: Ryu "Keria" Min-seok of T1 poses at the League of Legends - Mid-Season Invitational Rumble Features Day on May 18, 2022 in Busan, South Korea. (Photo by Lee Aiksoon/Riot Games)
Features red, aqua, grey prints from Sherbet Pips jelly roll, 10 1/2" blocks, sashed in white, backed with DS Quilts argyle from Picnics and Fairgrounds. Measures 42" x 42".
... features a half-million twinkling lights on Illuminated trees, organ sing-a-longs, and carolers throughout the gardens. More than 50 enchanting Christmas trees and more than 16,000 seasonal plants.
-- Longwood Gardens. Org, Kennett Square, Pennsylvania
This image features a Mute Swan (Cygnus olor), characterized by its prominent orange bill with a black base and a graceful, long neck often held in an "S" curve. The species is known for its heavy body, dense white plumage, and generally silent nature compared to other swan species. Mute Swans are often found swimming in pairs or small groups on lakes, ponds, and slow-moving rivers.
ATLANTA, GEORGIA - OCTOBER 26: Choi "Zeus" Woo-je of T1 poses at the League of Legends World Championship Semifinals Features Day on October 26, 2022 in Atlanta, GA. (Photo by Fernando Decillis/Riot Games)
Features Ex LACMTA Neoplan 1189 Ex Tri Met 351Flxible Newlook Ex Pierce Transit 364 Ex San Diego 401 Gm Newlook
SAN FRANCISCO, CALIFORNIA - NOVEMBER 01: Kim "Deft" Hyuk-kyu of DRX poses at the League of Legends World Championship Finals Features Day on November 1, 2022 in San Francisco, CA. (Photo by Lance Skundrich/Riot Games)
The city of Vaison-la-Romaine was, unsurprisingly, built by the Romans, but only in part. In fact, it features two very different built-up areas: one leisurely laid out on flat land, and the other holding on tight to a tall and dominating rocky outcrop, on the other bank of River Ouvèze, which is spanned by a Roman bridge. And the history of Vaison is largely that of a going back and forth between those two areas.
The very first inhabitants of Vaison, pre-Roman conquest, prudently settled on the mountain. Traces of Neolithic occupation were found on its steep slopes. Confident in the Pax Romana they were bringing with them, the Romans settled comfortably in the plain, by the banks of the Ouvèze, and began building a lovely and remarkable city, of which many famous ruins remain. Then the invasions of Barbarians from the East, and Saracens from the South, drove the people back onto the mountain, where they took many of the Roman cut stones of the lower city to fortify, defend and build ramparts, homes and churches. It is not really until the 19th century that they deemed safe to go back down again and re-settle the Antique part of the city, building frenetically over Roman ruins. This being before the time of “pre-emptive archæological digs”, many such ruins are undoubtedly forever buried under the elegant homes of the 1800s Vaison.
The Château comtal (i.e., “Castle of the Counts”) we will visit today and over the following days is a symbol of the centuries-long feud between the sacred and the secular —the former, we must admit, being largely the main culprit: while it is true that secular powers oftentimes tried to encroach upon the religious (for example by trying to usurp and appropriate the right to appoint bishops, abbots or abbesses), the clerical powers-that-be were equally, if not more often liable to try and meddle in, and establish their rule over, profane affairs and management of what we would call today “civilian” life.
In Vaison, bishop Bertrand de Mornas was guilty of such an appropriation and was consequently driven away by force in 1160 by Raymond V of Toulouse, the Toulouse family being the local overlords at the time. The next bishop, Bertrand de Lambesc, re-took the town in 1178 but let Raymond’s troops station on the mountaintop. There, true to form, they built a wooden fort in 1183 to symbolize their domination; it is the ancestor of the castle we still see today. In 1185, the then-bishop, Bérenger de Reillanne, burned that fort. Count Raymond sent his troops back right away, once again driving the bishop away. Between 1190 and 1193, they built a stone castle impervious to fire. :o)
The castle is not open to the public, as there are some spaces that are dangerous. The municipality, which owns the monument, has been working for quite a while in the perspective of opening it one day. Securing the ways to access is also a big challenge, as the whole mountaintop, including the bedrock, is listed as a Historic Landmark. Therefore, nothing can be touched unless declassified —an administrative nightmare— and I verified for myself that getting there can be very tricky, slippery and risky. The way cannot be publicly endorsed as is, oit would bring a slew of law suits against the town. I was permitted access inside in my capacity as pro bono photographer for the Fondation du Patrimoine.
Inside the courtyard, there are buildings on three sides. The sheet wall collapsed or was dismantled on the fourth side, opening directly onto the vertical rock face, hence the need to put a metal fence in place.
Selfie features the iconic Selfridges store and the metal discs match the roundels on the Selfridges façade. The head and feet of the owl are painted chrome to reflect the surroundings, while the name is inspired by the store and the trend of taking ‘selfies’ – what better than a selfie with Selfie!
Artist: Martin Band
Martin Band is an enthusiastic artist and director of Environmental Associates, an urban design and landscape architects business, based in Cheshire.
Martin regularly gets involved in the design of streetscape, civic spaces and gardens – always aiming to bring something new, creative and invigorating to the designs that his practice produces.
Website: www.environmentalassociates.net
Sponsor: LDC
Auction Price: £11,000
The Big Hoot captured the imagination of everyone in Birmingham and beyond, with hundreds of thousands of people taking to the streets with their Big Hoot Trail maps to explore the colourful invasion of individually designed owls. Taking in the city’s 10 districts, tourists and residents alike enjoyed their owl adventure, discovering and celebrating the extraordinary creativity produced by many of Birmingham’s artistic community and over 25,000 young people.
The Big Hoot owls went under the hammer on 15 October 2015 at The Big Hoot auction sponsored by Vodafone and we are thrilled to have smashed our target by raising the incredible sum of £508,035!
The money raised from the auction will support Birmingham Children’s Hospital Charity’s £3.65m Star Appeal. This appeal will enable us to create a first of its kind, a Rare Diseases Centre in the UK specifically for children. It will provide co-ordinated care, treatment, support and most importantly hope to children and families living with a rare or undiagnosed condition.
In addition the auction raised £15,000 for G’owl’d by Temper with proceeds going to Edward’s Trust, and £7,800 for Fleet and Free with proceeds going to Birchfield Harriers.
So thank you - we simply couldn’t have done it without you.
Artists have played a major role in The Big Hoot, creating almost 100 owl sculptures. We would like to thank all the artists for their incredible creativity and hard work.
Professional artists from Birmingham, the wider Midlands region and further afield have created extraordinary giant owls that are all unique in style and character and represent the city’s creativity, history and heritage, music, fashion, architecture and attractions.
Birmingham is home to a wealth of artistic and creative individuals and communities and many award-winning and nationally and internationally acclaimed artists. We are delighted with the response from Birmingham’s creative community and are thrilled to work in collaboration with them to transform the streets, squares and parks of the city.
For five months artists have been creating owls in their studios, at home and in The Big Hoot Artists’ Studio at the Custard Factory in Digbeth. Their inspiring and innovative designs have been realised in genres including graffiti, illustration, fine art, graphics, typography, mosaic and new media. They have worked with both community groups and with corporates to realise ideas and create their stunning designs.
The Big Hoot not only provides a high quality and ambitious free public event for families but also supports the creativity of artists and celebrates talent and diversity. The Big Hoot has provided an inspiring relationship between the city and the arts.
The artists have also reached out to communities enabling more people to participate in the arts, to experience working with professional artists and to be inspiring and inspired. From the north to the south of the city residents groups, youth groups and older peoples’ groups have been collaborating with artists to generate ideas, design and create owls for The Big Hoot.
Creativity is everywhere but the opportunity to participate is not. A range of activities have been programmed within Birmingham’s diverse communities and people from the age of 3 – 97 and from wards within the city boundaries have contributed to The Big Hoot and helped make the event extraordinary. Our projects have seen artists working with hundreds of residents and community members including children in looked after care, older peoples’ clubs, young people and residents organisations to design and decorate the owls displayed as part of the 10 week public event.
ISTANBUL, TURKEY - AUGUST 27: Tomoaki "crow" Maruoka (L) and Koji "Laz" Ushida of Zeta Division pose at VALORANT Champions 2022 Istanbul Features Day on August 27, 2022 in Istanbul, Turkey. (Photo by Lance Skundrich/Riot Games)
This features my version of the Veyman Genesis by Dark Syntax. Instead of posting just the build this time around, I figured I'd show how it compares to my usual measuring sticks. As is my normal, I made a couple of changes to the original build to reflect my design choices and parts availability.
This collection features photographic images generated with artificial intelligence using Midjourney V7, specifically designed to stand out on Flickr Explore. The series explores the most popular colors identified on the platform: red, green, blue, yellow, orange, monochrome and black and white.
Each image has been created with technically precise prompts that simulate professional photographic equipment (Canon, Nikon, Sony, Fujifilm, Leica) and specialized techniques such as macro, architecture, portrait, landscape and documentary photography. The collection spans from cinematic portraits to Mediterranean landscapes, contemporary architecture, nature, Andalusian culture and urban art.
All images use optimized parameters (--style raw --v 7) for maximum photographic realism, with 2:3 and 3:2 formats ideal for social media and digital gallery presentation. This series demonstrates the creative potential of generative AI applied to artistic and commercial photography.
Esta colección presenta imágenes fotográficas generadas con inteligencia artificial utilizando Midjourney V7, específicamente diseñadas para destacar en Flickr Explore. La serie explora los colores más populares identificados en la plataforma: rojo, verde, azul, amarillo, naranja, monocromo y blanco y negro.
Cada imagen ha sido creada con prompts técnicamente precisos que simulan equipamiento fotográfico profesional (Canon, Nikon, Sony, Fujifilm, Leica) y técnicas especializadas como macro, arquitectura, retrato, paisaje y fotografía documental. La colección abarca desde retratos cinematográficos hasta paisajes mediterráneos, arquitectura contemporánea, naturaleza, cultura andaluza y arte urbano.
Todas las imágenes utilizan parámetros optimizados (--style raw --v 7) para máximo realismo fotográfico, con formatos 2:3 y 3:2 ideales para la presentación en redes sociales y galerías digitales. Esta serie demuestra el potencial creativo de la IA generativa aplicada a la fotografía artística y comercial.
ISTANBUL, TURKEY - AUGUST 27: Yuma "Dep" Hashimoto of Zeta Division poses at VALORANT Champions 2022 Istanbul Features Day on August 27, 2022 in Istanbul, Turkey. (Photo by Lance Skundrich/Riot Games)
Structures that show his power, and a mouth in his torso.
This is the first main antagonist of my story. He's nearly complete, but just missing his fingers on his left hand and the white peice on his thigh needs to be changed to black.
The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1,283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them.
The various geyser basins are located where rainwater and snowmelt can percolate into the ground, get indirectly superheated by the underlying Yellowstone hotspot, and then erupt at the surface as geysers, hot springs, and fumaroles. Thus flat-bottomed valleys between ancient lava flows and glacial moraines are where most of the large geothermal areas are located. Smaller geothermal areas can be found where fault lines reach the surface, in places along the circular fracture zone around the caldera, and at the base of slopes that collect excess groundwater. Due to the Yellowstone Plateau's high elevation the average boiling temperature at Yellowstone's geyser basins is 199 °F (93 °C). When properly confined and close to the surface it can periodically release some of the built-up pressure in eruptions of hot water and steam that can reach up to 390 feet (120 m) into the air (see Steamboat Geyser, the world's tallest geyser). Water erupting from Yellowstone's geysers is superheated above that boiling point to an average of 204 °F (95.5 °C) as it leaves the vent. The water cools significantly while airborne and is no longer scalding hot by the time it strikes the ground, nearby boardwalks, or even spectators. Because of the high temperatures of the water in the features it is important that spectators remain on the boardwalks and designated trails. Several deaths have occurred in the park as a result of falls into hot springs.
Prehistoric Native American artifacts have been found at Mammoth Hot Springs and other geothermal areas in Yellowstone. Some accounts state that the early people used hot water from the geothermal features for bathing and cooking. In the 19th century Father Pierre-Jean De Smet reported that natives he interviewed thought that geyser eruptions were "the result of combat between the infernal spirits". The Lewis and Clark Expedition traveled north of the Yellowstone area in 1806. Local natives that they came upon seldom dared to enter what we now know is the caldera because of frequent loud noises that sounded like thunder and the belief that the spirits that possessed the area did not like human intrusion into their realm. The first white man known to travel into the caldera and see the geothermal features was John Colter, who had left the Lewis and Clark Expedition. He described what he saw as "hot spring brimstone". Beaver trapper Joseph Meek recounted in 1830 that the steam rising from the various geyser basins reminded him of smoke coming from industrial smokestacks on a cold winter morning in Pittsburgh, Pennsylvania. In the 1850s famed trapper Jim Bridger called it "the place where Hell bubbled up".
The heat that drives geothermal activity in the Yellowstone area comes from brine (salty water) that is 1.5–3 miles (7,900–15,800 ft; 2,400–4,800 m) below the surface. This is actually below the solid volcanic rock and sediment that extends to a depth of 3,000 to 6,000 feet (900 to 1,800 m) and is inside the hot but mostly solid part of the pluton that contains Yellowstone's magma chamber. At that depth the brine is superheated to temperatures that exceed 400 °F (204 °C) but is able to remain a liquid because it is under great pressure (like a huge pressure cooker).
Convection of the churning brine and conduction from surrounding rock transfers heat to an overlaying layer of fresh groundwater. Movement of the two liquids is facilitated by the highly fractured and porous nature of the rocks under the Yellowstone Plateau. Some silica is dissolved from the fractured rhyolite into the hot water as it travels through the fractured rock. Part of this hard mineral is later redeposited on the walls of the cracks and fissures to make a nearly pressure-tight system. Silica precipitates at the surface to form either geyserite or sinter, creating the massive geyser cones, the scalloped edges of hot springs, and the seemingly barren landscape of geyser basins.
There are at least five types of geothermal features found at Yellowstone:
Fumaroles: Fumaroles, or steam vents, are the hottest hydrothermal features in the park. They have so little water that it all flashes into steam before reaching the surface. At places like Roaring Mountain, the result is loud hissing of steam and gases.
Geysers: Geysers such as Old Faithful are a type of geothermal feature that periodically erupt scalding hot water. Increased pressure exerted by the enormous weight of the overlying rock and water prevents deeper water from boiling. As the hot water rises it is under less pressure and steam bubbles form. They, in turn, expand on their ascent until the bubbles are too big and numerous to pass freely through constrictions. At a critical point the confined bubbles actually lift the water above, causing the geyser to splash or overflow. This decreases the pressure of the system and violent boiling results. Large quantities of water flash into tremendous amounts of steam that force a jet of water out of the vent: an eruption begins. Water (and heat) is expelled faster than the geyser's recharge rate, gradually decreasing the system's pressure and eventually ending the eruption.
Hot springs: Hot springs such as Grand Prismatic Spring are the most common hydrothermal features in the park. Their plumbing has no constrictions. Superheated water cools as it reaches the surface, sinks, and is replaced by hotter water from below. This circulation, called convection, prevents water from reaching the temperature needed to set off an eruption. Many hot springs give rise to streams of heated water.
Mudpots: Mudpots such as Fountain Paint Pots are acidic hot springs with a limited water supply. Some microorganisms use hydrogen sulfide (rotten egg smell), which rises from deep within the earth, as an energy source. They convert the gas into sulfuric acid, which breaks down rock into clay.
Travertine terraces: Travertine terraces, found at Mammoth Hot Springs, are formed from limestone (a rock type made of calcium carbonate). Thermal waters rise through the limestone, carrying high amounts of dissolved carbonate. Carbon dioxide is released at the surface and calcium carbonate deposited as travertine, the chalky white rock of the terraces. These features constantly and quickly change due to the rapid rate of deposition.
Geyser basins
The Norris Geyser Basin 44°43′43″N 110°42′16″W is the hottest geyser basin in the park and is located near the northwest edge of Yellowstone Caldera near Norris Junction and on the intersection of three major faults. The Norris-Mammoth Corridor is a fault that runs from Norris north through Mammoth to the Gardiner, Montana, area. The Hebgen Lake fault runs from northwest of West Yellowstone, Montana, to Norris. This fault experienced an earthquake in 1959 that measured 7.4 on the Richter scale (sources vary on exact magnitude between 7.1 and 7.8; see 1959 Hebgen Lake earthquake). Norris Geyser Basin is so hot and dynamic because these two faults intersect with the ring fracture zone that resulted from the creation of the Yellowstone Caldera of 640,000 years ago.
The Basin consists of three main areas: Porcelain Basin, Back Basin, and One Hundred Springs Plain. Unlike most of other geyser basins in the park, the waters from Norris are acidic rather than alkaline (for example, Echinus Geyser has a pH of ~3.5). The difference in pH allows for a different class of bacterial thermophiles to live at Norris, creating different color patterns in and around the Norris Basin waters.
The Ragged Hills that lie between Back Basin and One Hundred Springs Plain are thermally altered glacial kames. As glaciers receded the underlying thermal features began to express themselves once again, melting remnants of the ice and causing masses of debris to be dumped. These debris piles were then altered by steam and hot water flowing through them. Madison lies within the eroded stream channels cut through lava flows formed after the caldera eruption. The Gibbon Falls lies on the caldera boundary as does Virginia Cascades.
Algae on left bacteria on right at the intersection of flows from the Constant & Whirlgig Geysers at Norris Geyser Basin
The tallest active geyser in the world, Steamboat Geyser,[11] is located in Norris Basin. Unlike the slightly smaller but much more famous Old Faithful Geyser located in Upper Geyser Basin, Steamboat has an erratic and lengthy timetable between major eruptions. During major eruptions, which may be separated by intervals of more than a year (the longest recorded span between major eruptions was 50 years), Steamboat erupts over 300 feet (90 m) into the air. Steamboat does not lie dormant between eruptions, instead displaying minor eruptions of approximately 40 feet (12 m).
Norris Geyser Basin periodically undergoes a large-scale, basin-wide thermal disturbance lasting a few weeks. Water levels fluctuate, and temperatures, pH, colors, and eruptive patterns change throughout the basin. During a disturbance in 1985, Porkchop Geyser continually jetted steam and water; in 1989, the same geyser apparently clogged with silica and blew up, throwing rocks more than 200 feet (61 m). In 2003 a park ranger observed it bubbling heavily, the first such activity seen since 1991. Activity increased dramatically in mid-2003. Because of high ground temperatures and new features beside the trail much of Back Basin was closed until October. In 2004 the boardwalk was routed around the dangerous area and now leads behind Porkchop Geyser.
North of Norris, Roaring Mountain is a large, acidic hydrothermal area (solfatara) with many fumaroles. In the late 19th and early 20th centuries, the number, size, and power of the fumaroles were much greater than today. The fumaroles are most easily seen in the cooler, low-light conditions of morning and evening.
The Gibbon Geyser Basin 44°41′58″N 110°44′34″W includes several thermal areas in the vicinity of the Gibbon River between Gibbon Falls and Norris. The most accessible feature in the basin is Beryl Spring, with a small boardwalk right along the Grand Loop Road. Artists' Paintpots is a small hydrothermal area south of Norris Junction that includes colorful hot springs and two large mudpots.
The Monument Geyser Basin 44°41′03″N 110°45′14″W has no active geysers, but its 'monuments' are siliceous sinter deposits similar to the siliceous spires discovered on the floor of Yellowstone Lake. Scientists hypothesize that this basin's structures formed from a hot water system in a glacially dammed lake during the waning stages of the Pinedale Glaciation. The basin is on a ridge reached by a very steep one-mile (1.6 km) trail south of Artists' Paint Pots. Other areas of thermal activity in Gibbon Geyser Basin lie off-trail.
South of Norris along the rim of the caldera is the Upper Geyser Basin 44°27′52″N 110°49′45″W, which has the highest concentration of geothermal features in the park. This complement of features includes the most famous geyser in the park, Old Faithful Geyser, as well as four other predictable large geysers. One of these large geysers in the area is Castle Geyser which is about 1,400 feet (430 m) northwest of Old Faithful. Castle Geyser has an interval of approximately 13 hours between major eruptions, but is unpredictable after minor eruptions. The other three predictable geysers are Grand Geyser, Daisy Geyser, and Riverside Geyser. Biscuit Basin and Black Sand Basin are also within the boundaries of Upper Geyser Basin.
The hills surrounding Old Faithful and the Upper Geyser Basin are reminders of Quaternary rhyolitic lava flows. These flows, occurring long after the catastrophic eruption of 640,000 years ago, flowed across the landscape like stiff mounds of bread dough due to their high silica content.
Evidence of glacial activity is common, and it is one of the keys that allows geysers to exist. Glacier till deposits underlie the geyser basins providing storage areas for the water used in eruptions. Many landforms, such as Porcupine Hills north of Fountain Flats, are made up of glacial gravel and are reminders that 70,000 to 14,000 years ago, this area was buried under ice.
Signs of the forces of erosion can be seen everywhere, from runoff channels carved across the sinter in the geyser basins to the drainage created by the Firehole River. Mountain building is evident on the drive south of Old Faithful, toward Craig Pass. Here the Rocky Mountains reach a height of 8,262 feet (2,518 m), dividing the country into two distinct watersheds.
Midway Geyser Basin 44°31′04″N 110°49′56″W is much smaller than the other basins found alongside the Firehole River. Despite its small size, it contains two large features, the 200-by-300-foot-wide (60 by 90 m) Excelsior Geyser which pours over 4,000 U.S. gallons (15,000 L; 3,300 imp gal) per minute into the Firehole River. The largest hot spring in Yellowstone, the 370-foot-wide (110 m) and 121-foot-deep (37 m) Grand Prismatic Spring is found here. Also in the basin is Turquoise Pool and Opal Pool.
Lower Geyser Basin
Blue spring with steam rising from it; irregular blotches of red and orange residue are on the banks, along with dead tree trunks.
Silex Spring at Fountain Paint Pot
Farther north is the Lower Geyser Basin 44°32′58″N 110°50′09″W, which is the largest geyser basin in area, covering approximately 11 square miles. Due to its large size, it has a much less concentrated set of geothermal features, including Fountain Paint Pots. Fountain Paint Pots are mud pots, that is, a hot spring that contains boiling mud instead of water. The mud is produced by a higher acidity in the water which enables the spring to dissolve surrounding minerals to create an opaque, usually grey, mud. Also there is Firehole Spring, Celestine Pool, Leather Pool, Red Spouter, Jelly spring, and a number of fumaroles.
Geysers in Lower Geyser Basin include Great Fountain Geyser, whose eruptions reach 100 to 200 feet (30–61 m) in the air, while waves of water cascade down its sinter terraces., the Fountain group of Geysers (Clepsydra Geyser which erupts nearly continuously to heights of 45 feet (14 m), Fountain Geyser, Jelly Geyser, Jet Geyser, Morning Geyser, and Spasm Geyser), the Pink Cone group of geysers (Dilemma Geyser, Labial Geyser, Narcissus Geyser, Pink Geyser, and Pink Cone Geyser), the White Dome group of geysers (Crack Geyser, Gemini Geyser, Pebble Geyser, Rejuvenated Geyser, and White Dome Geyser), as well as Sizzler Geyser.
Clepsydra Geyser erupting. July 2019
Fountain Paint Pots
White Dome Geyser
West Thumb Geyser Basin
Several pools of blue water in ashen rock basin.
West Thumb Geyser Basin
Blackened basin with orange streaks; steam is rising from it with fir trees in the background.
Overflow areas of Silex springs
The West Thumb Geyser Basin 44°25′07″N 110°34′23″W, including Potts Basin to the north, is the largest geyser basin on the shores of Yellowstone Lake. The heat source of the thermal features in this location is thought to be relatively close to the surface, only 10,000 feet (3,000 m) down. West Thumb is about the same size as another famous volcanic caldera, Crater Lake in Oregon, but much smaller than the great Yellowstone Caldera which last erupted about 640,000 years ago. West Thumb is a caldera within a caldera.
West Thumb was created approximately 162,000 years ago when a magma chamber bulged up under the surface of the earth and subsequently cracked it along ring fracture zones. This in turn released the enclosed magma as lava and caused the surface above the emptied magma chamber to collapse. Water later filled the collapsed area of the caldera, forming an extension of Yellowstone Lake. This created the source of heat and water that feed the West Thumb Geyser Basin today.
The thermal features at West Thumb are not only found on the lake shore, but extend under the surface of the lake as well. Several underwater hydrothermal features were discovered in the early 1990s and can be seen as slick spots or slight bulges in the summer. During the winter, the underwater thermal features are visible as melt holes in the icy surface of the lake. The surrounding ice can reach three feet (one yard) in thickness.
Perhaps the most famous hydrothermal feature at West Thumb is a geyser on the lake shore known as Fishing Cone. Walter Trumbull of the 1870 Washburn-Langford-Doane Expedition described a unique event while a man was fishing adjacent to the cone: "...in swinging a trout ashore, it accidentally got off the hook and fell into the spring. For a moment it darted about with wonderful rapidity, as if seeking an outlet. Then it came to the top, dead, and literally boiled." Fishing Cone erupted frequently to the height of 40 feet (12 m) in 1919 and to lesser heights in 1939. One fisherman was badly burned in Fishing Cone in 1921. Fishing at the geyser is now prohibited.
Early visitors would arrive at West Thumb via stagecoach from the Old Faithful area. They had a choice of continuing on the stagecoach or boarding the steamship Zillah to continue the journey by water to Lake Hotel. The boat dock was located near the south end of the geyser basin near Lakeside Spring.
Backcountry Geyser Basins
The Heart Lake 44°18′00″N 110°30′56″W, Lone Star 44°24′50″N 110°49′04″W, and Shoshone Geyser Basins 44°21′16″N 110°47′57″W are located away from the road and require at least several miles of hiking to reach. These areas lack the boardwalks and other safety features of the developed areas. As falling into geothermal features can be fatal, it is usually advisable to visit these areas with an experienced guide or at the very least, travelers need to ensure they remain on well-marked trails.
The Heart Lake Geyser Basin contains several groups of geysers and deep blue hot springs near Heart Lake in the south-central portion of Yellowstone, southeast of most of the main geyser basins. Lying in the Snake River watershed east of Lewis Lake and south of Yellowstone Lake, Heart Lake was named sometime before 1871 for Hart Hunney, a hunter. Other explorers in the region incorrectly assumed that the lake's name was spelled 'heart' because of its shape. The Heart Lake Geyser Basin begins a couple miles from the lake and descends along Witch Creek to the lakeshore. Five groups of hydrothermal features comprise the basin, and all of them contain geysers, although some are dormant.
Between Shoshone Lake and Old Faithful is the Lone Star Geyser Basin, of which the primary feature is Lone Star Geyser, named for its isolation from the nearby geysers of the Upper Geyser Basin. The basin is reachable on foot or bicycle via a 3 mile road that is closed to vehicles.
The Shoshone Geyser Basin, reached by hiking or by boat, contains one of the highest concentrations of geysers in the world – more than 80 in an area 1,600 by 800 feet (490 by 240 m). Hot springs and mudpots dot the landscape between the geyser basin and Shoshone Lake.
Hot Spring Basin is located 15 miles (24 km) north-northeast of Fishing Bridge and has one of Yellowstone's largest collections of hot springs and fumaroles. The geothermal features there release large amounts of sulfur. This makes water from the springs so acidic that it has dissolved holes in the pants of people who sit on wet ground and causes mounds of sulfur three feet (1 m) high to develop around fumaroles. The very hot acidic water and steam have also created voids in the ground that are only covered by a thin crust.
Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate (over two tons flow into Mammoth each day in a solution). Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas.
The thermal features at Mud Volcano and Sulphur Caldron are primarily mud pots and fumaroles because the area is situated on a perched water system with little water available. Fumaroles or "steam vents" occur when the ground water boils away faster than it can be recharged. Also, the vapors are rich in sulfuric acid that leaches the rock, breaking it down into clay. Because no water washes away the acid or leached rock, it remains as sticky clay to form a mud pot. Hydrogen sulfide gas is present deep in the earth at Mud Volcano and is oxidized to sulfuric acid by microbial activity, which dissolves the surface soils to create pools and cones of clay and mud. Along with hydrogen sulfide, steam, carbon dioxide, and other gases explode through the layers of mud.
A series of shallow earthquakes associated with the volcanic activity in Yellowstone struck this area in 1978. Soil temperatures increased to nearly 200 °F (93 °C). The slope between Sizzling Basin and Mud Geyser, once covered with green grass and trees, became a barren landscape of fallen trees known as "the cooking hillside".
Yellowstone National Park is a national park located in the western United States, largely in the northwest corner of Wyoming and extending into Montana and Idaho. It was established by the 42nd U.S. Congress with the Yellowstone National Park Protection Act and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone was the first national park in the U.S. and is also widely held to be the first national park in the world. The park is known for its wildlife and its many geothermal features, especially the Old Faithful geyser, one of its most popular. While it represents many types of biomes, the subalpine forest is the most abundant. It is part of the South Central Rockies forests ecoregion.
While Native Americans have lived in the Yellowstone region for at least 11,000 years, aside from visits by mountain men during the early-to-mid-19th century, organized exploration did not begin until the late 1860s. Management and control of the park originally fell under the jurisdiction of the U.S. Department of the Interior, the first Secretary of the Interior to supervise the park being Columbus Delano. However, the U.S. Army was eventually commissioned to oversee the management of Yellowstone for 30 years between 1886 and 1916. In 1917, the administration of the park was transferred to the National Park Service, which had been created the previous year. Hundreds of structures have been built and are protected for their architectural and historical significance, and researchers have examined more than a thousand archaeological sites.
Yellowstone National Park spans an area of 3,468.4 sq mi (8,983 km2), comprising lakes, canyons, rivers, and mountain ranges. Yellowstone Lake is one of the largest high-elevation lakes in North America and is centered over the Yellowstone Caldera, the largest super volcano on the continent. The caldera is considered a dormant volcano. It has erupted with tremendous force several times in the last two million years. Well over half of the world's geysers and hydrothermal features are in Yellowstone, fueled by this ongoing volcanism. Lava flows and rocks from volcanic eruptions cover most of the land area of Yellowstone. The park is the centerpiece of the Greater Yellowstone Ecosystem, the largest remaining nearly intact ecosystem in the Earth's northern temperate zone. In 1978, Yellowstone was named a UNESCO World Heritage Site.
Hundreds of species of mammals, birds, fish, reptiles, and amphibians have been documented, including several that are either endangered or threatened. The vast forests and grasslands also include unique species of plants. Yellowstone Park is the largest and most famous megafauna location in the contiguous United States. Grizzly bears, cougars, wolves, and free-ranging herds of bison and elk live in this park. The Yellowstone Park bison herd is the oldest and largest public bison herd in the United States. Forest fires occur in the park each year; in the large forest fires of 1988, nearly one-third of the park was burnt. Yellowstone has numerous recreational opportunities, including hiking, camping, boating, fishing, and sightseeing. Paved roads provide close access to the major geothermal areas as well as some of the lakes and waterfalls. During the winter, visitors often access the park by way of guided tours that use either snow coaches or snowmobiles.
Teton County is a county in the U.S. state of Wyoming. As of the 2020 United States Census, the population was 23,331. Its county seat is Jackson. Its west boundary line is also the Wyoming state boundary shared with Idaho and the southern tip of Montana. Teton County is part of the Jackson, WY-ID Micropolitan Statistical Area.
Teton County contains the Jackson Hole ski area, all of Grand Teton National Park, and 40.4% of Yellowstone National Park's total area, including over 96.6% of its water area (largely in Yellowstone Lake).
Wyoming is a state in the Mountain West subregion of the Western United States. It borders Montana to the north and northwest, South Dakota and Nebraska to the east, Idaho to the west, Utah to the southwest, and Colorado to the south. With a population of 576,851 in 2020, Wyoming is the least populous state despite being the 10th largest by area, with the second-lowest population density after Alaska. The state capital and most populous city is Cheyenne, which had an estimated population of 63,957 in 2018.
Wyoming's western half consists mostly of the ranges and rangelands of the Rocky Mountains; its eastern half consists of high-elevation prairie, and is referred to as the High Plains. Wyoming's climate is semi-arid in some parts and continental in others, making it drier and windier overall than other states, with greater temperature extremes. The federal government owns just under half of Wyoming's land, generally protecting it for public uses. The state ranks sixth in the amount of land—-and fifth in the proportion of its land—-that is owned by the federal government. Its federal lands include two national parks (Grand Teton and Yellowstone), two national recreation areas, two national monuments, and several national forests, as well as historic sites, fish hatcheries, and wildlife refuges.
Indigenous peoples inhabited the region for thousands of years. Historic and currently federally recognized tribes include the Arapaho, Crow, Lakota, and Shoshone. Part of the land that is now Wyoming came under American sovereignty via the Louisiana Purchase, part via the Oregon Treaty, and, lastly, via the Mexican Cession. With the opening of the Oregon Trail, the Mormon Trail, and the California Trail, vast numbers of pioneers travelled through parts of the state that had once been traversed mainly by fur trappers, and this spurred the establishment of forts, such as Fort Laramie, that today serve as population centers. The Transcontinental Railroad supplanted the wagon trails in 1867 with a route through southern Wyoming, bringing new settlers and the establishment of founding towns, including the state capital of Cheyenne. On March 27, 1890, Wyoming became the union's 44th state.
Farming and ranching, and the attendant range wars, feature prominently in the state's history. Today, Wyoming's economy is largely based on tourism and the extraction of minerals such as coal, natural gas, oil, and trona. Its agricultural commodities include barley, hay, livestock, sugar beets, wheat, and wool.
Wyoming was the first state to allow women the right to vote (not counting New Jersey, which had allowed it until 1807), and the right to assume elected office, as well as the first state to elect a female governor. In honor of this part of its history, its most common nickname is "The Equality State" and its official state motto is "Equal Rights". It is among the least religious states in the country, and is known for having a political culture that leans towards libertarian conservatism. The Republican presidential nominee has carried the state in every election since 1968.
Earlier this week I posted a picture of the plants in our diningroom window and thought I’d show you a cool thing. The screen on that window developed a hole (don’t remember why) and when casting around for solutions to repair, I found this butterfly. It is a clear sticky patch and two magnets (one for inside and one for outside), so it covers the hole and stays in place. Cool- huh? Some creative problem solvers out there!
This is from a group of work created on instant film and shot through a pinhole camera. Exposed on Worldwide Pinhole Photography Day 2020.
Le Bambole Mk. V, The Colorpack Pinhole Camera. Fujifilm FP-3000B film (very expired, cooked) and negative reclamation (goop). Solarization and sabattier effect in printing process.
Built in 1960, Birch Tower is a 16-story high-rise in the heart of Fort Lauderdale Beach. Birch Tower has a community pool, entertainment room, workout room and storage for bikes. From the roof top terrace, you can watch the boat parades & air shows or fireworks. The Birch Tower HOA fee includes AC, hot water, water, basic cable and 24 hours security. Small pets are allowed.
Key Features and History:
Architect: Charles McKirahan, who was influenced by European architects like Le Corbusier and Oscar Niemeyer.
Year Built: 1960.
Stories: 16.
Units: 120.
Style: Mid-century modern, specifically the International Style.
Location: Central Beach neighborhood, near the intersection of Breakers Avenue and Terramar Street.
Unique Architectural Elements: The building is elevated on pylons, allowing vehicles to pass underneath, a design element inspired by Oscar Niemeyer's work in Brazil. It also features a floating, neon-backed sign stretching seven stories.
Significance: Birch Tower is a landmark in Fort Lauderdale's architectural history, representing the city's embrace of modern design in the 1950s and 60s.
Credit for the data above is given to the following websites:
www.highrises.com/buildings/fort-lauderdale_fl/birch-towe...
www.google.com/search?q=birch+tower+fort+lauderdale+histo...
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One of the less endearing features of British coaches, particularly longer Plaxtons of the late 60s, '70s and early '80s was the tendency to break their backs. In my experience the most resilient of them all were the early Supremes which usually survived quite well. 12m Elites and late '70s Supremes were the worst. The Elite was not aided by the re-location of the Emergency door from behind the driver to the position of what would ordinarily be the penultimate window bay on the 'off side'. The lightweight steel box section bearers of the later Supremes simply rotted out. Of course 'coach' bodies, unlike their 'bus' sisters required luggage accomodation, and in a mid engined standard low deck coach of the era, had to be at the rear. To facilitate maximum space, the option to have chassis extensions was seldom taken up, thereby leaving the rear overhang (perhaps nearly 11 feet) of the body to support itself plus all passengers and potentially their luggage.
Here, ex Castleways Leyland Leopard Plaxton Elite EDG 250L demostrates the issue. Note what should be a straight waist-rail from around the area of the rear wheels. Sadly this preserved coach didn't survive long after this picture was taken, though I'm not sure whether it was this body issue which finally put paid to it. Ironically, the often slated Duple Dominant equivalent ... renowned for body rot, didn't usually suffer in this manner and I can only ever recall seeing one actually broken ... against dozens of Plaxtons.
The special features of the West and East Matukituki Valleys Region were recognised nationally in 1964 when the Mount Aspiring National Park was created, and internationally in 1990 with the establishment of Te Wāhipounamu—South West New Zealand World Heritage Area.
The West and East Matukituki Valleys are part of the Southern Alps, a mountain range extending along much of the length of New Zealand's South Island. Most of the Southern Alps (Kā Tiritiri o te Moana in Maori) started over 220 million years ago as sediment and rock on top of volcanic rocks on the seafloor. Intense heat and pressure consolidated the rock, which was then uplifted to form the Main Divide. During the Ice Ages huge glaciers filled and scoured out the valleys to give the modern landscape.
Beech is the dominant forest in the Matukituki Valley. Red beech (tawhairaunui) prefers warm valley sites, mountain beech (tawhairauriki) dominates the drier, eastern end of the valley, while silver beech/tawhai increases towards the wetter, western end. Ferns and mosses are a feature of the usually open forest. Above the timberline at about 1,100 metres, in the often more frigid zones, stunted subalpine shrub land gives way to alpine tussock grasslands, fell fields (rock-strewn area dominated by low plants or by grasses and sedges) and snow fields.
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Features include opening cockpit, rotating engines, moving gun/landing thingies, and a containment cell for your bad-guy.
The third Ida Rentoul Outhwaite Children's Library Stained Glass Window features the excerpt from a poem; "While underneath in phantom shells, the fairy sailors go, and shining o'er the silent dells, the fairy beacons glow". It, and the painted panel above come from "Fairy Islands" from "Elves and Fairies" published by Thomas Lothian in Melbourne in 1910. The book illustration, much more Art Nouveau in influence than any of the others, is rich with night time blues. Yet the stained glass panel featuring six faeries riding down a river in nautilus shells beneath a silvery full moon, has highlights of pink and golden yellow. The girl faeries all wear Edwardian empire line dancing dresses, such as Isadora Duncan and Anna Pavlova wore, with belts of trailing yellow flowers. Whilst the water looks tranquil enough, the faeries are obviously moving swiftly down the river as their hair and dresses blow in the breeze, and the pink heath sprigs they carry all bend to the wind. The silhouettes of narrow gum trees stand against a full moon glimpsed between two steep banks.
In 1923 with Fitzroy still very much a working class area of Melbourne with pockets of poverty, the parish of St. Mark the Evangelist decided to address the need of the poor in the inner Melbourne suburb. Architects Gawler and Drummond were commissioned to design a two storey red brick Social Settlement Building. It was opened in 1926 by the Vicar of St. Mark the Evangelist, the Reverend Robert G. Nichols (known affectionately amongst the parish as Brother Bill). Known today as the Community Centre, the St. Mark the Evangelist Social Settlements Building looks out onto George Street and also across the St. Mark the Evangelist's forecourt. When it opened, the Social Settlement Building's facilities included a gymnasium, club rooms and children's library.
Opened in 1926, the children's library, which was situated in the corner room of the Social Settlements Building, is believed to be the first known free dedicated children's library in Victoria. The library was given to the children of Fitzroy by Mrs. T. Hackett, in memory of her late husband. The library contained over 3,000 books, as well as children's magazines and even comics. The Social Settlements Building was only erected because Brother Bill organised the commitment of £1,000.00 each from various wealthy businessmen and philanthropists around Melbourne. Mrs Hackett's contribution was the library of £1,000.00 worth of books. Another internationally famous resident of the neighbourhood, Australian children's book illustrator Ida Rentoul Outhwaite, then at the zenith of her career, was engaged by the relentless Brother Bill to create something for the library. Ida donated four stained glass windows each with a hand-painted panel executed by her, based upon illustrations from her books, most notably "Elves and Fairies" which was published to great acclaim in Australia and sold internationally in 1916 and "Fairyland" which had been published earlier that year. These four hand painted stained glass windows were equated to the value of £1,000.00, but are priceless today, as they are the only public works of Ida Rentoul Outhwaite ever commissioned that have been executed in this medium. Ida Rentoul Outhwaite was only ever commissioned to create one other public work; a series of four panels executed in watercolour with pencil underdrawing in 1910 for the Prince Henry Hospital's children's wards in Melbourne (now demolished). Of her panels, only two are believed still to be in existence, buried within the hospital archives. The four Ida Rentoul Outhwaite stained glass windows each depict faeries, pixies, Australian native animals and children, taken from her book illustrations. At the time of photographing, the windows - three overlooking George Street and one St. Mark the Evangelist's forecourt - were located in the community lounge, which served as a drop-in lounge and kitchen for Fitzroy's homeless and marginalised citizens. Today the space has been re-purposed as offices for the Anglicare staff who run the St. Mark's Community Centre, possibly as a way to protect the precious windows from coming to any harm. The only down-side to this is that they are not as easily accessed or viewed as when I photographed them, making my original visit to St. Mark the Evangalist in 2009 extremely fortuitous.
The Ida Rentoul Outhwaite Children's Library Stained Glass Windows are one of Australia's greatest hidden treasures, which seems apt when you consider that the pixies and faeries they depict are also often in hiding when we read about them in children's books and the faerie tales of our childhood. The fact that they are hidden, because it is necessary to enter a little-known and undistinguished building in order to see them, ensures their protection and survival. The windows are unique, not only because they are the only stained glass windows designed and hand-painted by Ida Rentoul Outhwaite, but because they are the earliest and only examples of stained glass art in Australia that deals with theme of childhood.
I am indebted to Peter Bourke who ran the St. Mark's Community Centre in 2009 for giving me the privilege of seeing these beautiful and rare windows created by one of my favourite children's book artists on a hot November afternoon, without me having made prior arrangements. I also appreciate him allowing me the opportunity to photograph them in great detail. I will always be grateful to him for such a wonderful and moving experience.
Ida Sherbourne Outhwaite (1888 - 1960) was an Australian children's book illustrator. She was born on the 9th of June 1888 in the inner Melbourne suburb of Carlton. She was the daughter of the of Presbyterian Reverend John Laurence Rentoul and his wife Annie Isobel. Her family was both literary and artistic, and as such, gifted Ida was encouraged from an early age to embrace her talent of drawing. Her elder sister, Annie Rattray Rentoul (1882 - 1978), was likewise encouraged to write, and both would later form a successful partnership. In 1903 six fairy stories written by Annie and illustrated by Ida were published in the ladies' journal "New Idea". The following year the Rentoul sisters collaborated on a book called "Mollie's Bunyip" which was received with instant success because it combined the idea of European faeries, witches and elves and the Australian bush. "Mollie's Staircase" followed in 1906. In 1908 the Rentoul sisters published their first substantial story book, "The Lady of the Blue Beads". On 9 December 1909 Ida married Arthur Grenbry Outhwaite (1875-1938), manager of the Perpetual Executors and Trustees Association of Australia Ltd. (Annie remained unmarried her entire life). After her marriage, Ida was known as Ida Rentoul Outhwaite, but did not publish anything substantial as she established her family and household until part way through the Great War. In 1916 she brought out her first coloured work; "Elves and Fairies", a de luxe edition produced entirely in Australia by Thomas Lothian. The success of the book, with its delicate watercolour plates, was due both to Ida's artistic talent and to the business acumen of her husband, who provided a £400.00 subsidy to ensure a high-quality production and consigned royalties to the Red Cross, thereby encouraging vice-regal patronage. "Elves and Fairies" is still her best known and loved work. Encouraged by her latest success, Ida travelled to Europe after hostilities ended and in 1920 exhibited in Paris and London. The critics compared her to other artists of the golden years of children's illustration such as Arthur Rackham and Edmund Dulac, thus sealing her international success. She signed a contract with British book publishers A. & C. Black who published five books for her over the next decade, including "The Enchanted Forest" (1921), with text by her husband, and, probably the most popular of all the Rentoul sisters' collaborations, "The Little Green Road to Fairyland" (1922). "The Fairyland of Ida Rentoul Outhwaite" (1926), another sumptuous volume, with text by her husband and sister, was less successful. A. & C. Black also produced a number of postcard series using her illustrations from "Elves and Fairies" as well as her other books published by them. In 1930 the last of her books published by A. & C. Black was released, but already times were changing, and the interest in Ida's work was rapidly fading. Angus & Robertson brought out two more books in 1933 and 1935 but they received relatively little attention. Her last two exhibitions, which between 1916 and 1928 were almost annual events, were held in 1933. The Second World War changed the world, and Ida and Annie's work was relegated to a bygone era, shunned and forgotten. Ida suffered the loss of both of her sons during the war, and she spent her last years sharing a flat in Caulfield with her sister, where, survived by her two daughters, she died on 25 June 1960. She did not live to see the resurgence of interest in her work some twenty-five years later, when in 1985, her picture of "The Little Witch" from "Elves and Fairies" was published on an Australian stamp, opening the fairy world of Ida Rentoul Outhwaite to a whole new generation of children and adults alike.
Today's throwback airbrushed style pinup photo features Kayla in this awkward moment of perfect aim! Some would say the knife thrower missed his mark or that he got too close and endangered his assistant... but in this case perhaps the knife thrower had perfect aim much to Kayla's dismay!
Did you know you can order many of the pinups you see posted on here? Check out the Dietz Dolls online store where you can find military pinups, classic pinups, the propaganda pinup poster series, and lots more in sizes ranging from 8x10 prints to 24x36 posters! www.dietzdolls.com/catalog
Model: Kayla
Photographer: Britt Dietz
Online Pinup Print and Poster Store: www.dietzdolls.com/catalog
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Features working brakes!...yeah I know there is not really any point, but I could so I did :) 2x 9v motors wheel-spin behind this when the brakes are clicked "on"
Also has a lightbrick in the firebox, actuated by pushing the main boiler slightly backwards. This light also serves as a "through" light to the rear tail lamp. Plus a "quick release" cab to be able to access the click hinge brake lever.
Had to sit on this for 8 months or so, but now able to show some of the pictures as "teasers".....designed and made exclusively for "The Lego Adventure" book: www.flickr.com/groups/2021445@N23/ which includes a full 18 page feature on how to build this, starting from chassis to end result.
Was an honour and a privilige to be chosen for this line up of "inspirational" builders throughout the world :)
Several interesting atmospheric features appear in this GOES East satellite image of the western Atlantic Ocean, captured July 9, 2018. The small eye of Tropical Storm Chris is visible off the coast of the Carolinas, while in the eastern Caribbean Sea, we can see the remnants of former Hurricane Beryl, around which a thick plume of Saharan dust is wrapping north and east of the storm. Chris, which formed on July 8, is the third named storm of the 2018 Atlantic hurricane season. In its latest update, the National Hurricane Center reported the storm had sustained winds near 60 mph and remains stalled a few hundred miles off the coast of North Carolina. The storm is expected to strengthen to a hurricane before weakening again as it tracks northeastward toward Newfoundland later this week.
Meanwhile, in the Caribbean, the disorganized remants of Beryl can be seen east of the island of Hispaniola. The storm is currently bringing heavy rain to Puerto Rico and the Virgin Islands, and has a 40 percent chance of re-strengthening to a tropical storm or depression over the next five days. North and east of the storm, a hazy cloud of Saharan dust is visible in the lower-right portion of this image. Known as the Saharan Air Layer, this dry, dusty air mass has been a persistent feature over the tropical Atlantic Ocean in recent weeks.
This geocolor enhanced imagery was created by NOAA's partners at the Cooperative Institute for Research in the Atmosphere. The GOES East geostationary satellite, also known as GOES-16, provides coverage of the Western Hemisphere, including the United States, the Atlantic Ocean and the Gulf of Mexico. The satellite's high-resolution imagery provides optimal viewing of severe weather, such as hurricanes and tropical storms, as well as atmospheric aerosols such as dust and sand.
Credit: NOAA