Connecticut Photography
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This blue hour photograph of Gardens by the Bay and Marina Bay Sands (MBS) with drifting clouds was taken from the building roof of Marina Barrage. The lit natural and super-trees in the Garden, domes and distinctive boat-like roof top design of MBS, are some of the attractive features of Marina Bay. The floating pontoon in the right foreground provides space for small vessels to be moored.
Best wishes for a great weekend!
Wadi Rum Collection - Raw Tiff 3 Stith Nk T Biclr ad dn df psdR sk Webb TIFF 157.80 MB.
Panoramic view of desert against the blue sky.
Wadi Rum is a protected desert wilderness in southern Jordan almost 300 Km South of Amman city (Capital of Jordan). It features dramatic sandstone mountains and Natural Arches. Many prehistoric inscriptions and carvings line rocky caverns and steep chasms. The natural water source of Lawrence’s Spring is named after British Lieutenant Lawrence of Arabia, who allegedly washed there.
Wadi Rum in Jordan was used for filming the external scenes as the surface of Planet Mars in the Hollywood movie (The Martian) and many other movies.
The largest sphere of the Pearl of the Orient Tower.
The tower features in total 11 spheres in various sizes. The biggest sphere is 50 meters in diameter with an open air observation deck 90 meters above ground level.
© All Rights Reserved - you may not use this image in any form without my prior permission.
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Thruscross is a hamlet in the Harrogate district of North Yorkshire, England. It lies in the Washburn Valley, 11 miles west of Harrogate. The parish includes Thruscross Reservoir and a large area of moorland west of the reservoir
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Photo Taken at Crisp Kringle
Features
Its appearance when viewed from the south-west, i.e. from the direction of Porthmadog, has earned it the sobriquet the "Matterhorn of Wales", albeit being 3,789 metres lower. In reality Cnicht is a long ridge and, at 689 m, is the fifth-highest peak in the Moelwynion mountain range. It can be easily ascended from Croesor, the village at its foot, or, with more difficulty, from Nant Gwynant to the north-west.
Although regarded by some as a mountain in its own right, Cnicht does not have the required 150m of topographic prominence to be classed as a Marilyn.
Snowdonia is a region in northwest Wales concentrated around the mountains and glacial landforms of massive Snowdonia National Park. The park's historic Snowdon Mountain Railway climbs to the summit of Wales's highest mountain, Mount Snowdon, offering views across the sea to Ireland. The park is also home to an extensive network of trails, over 100 lakes and craggy peaks like Cader Idris and Tryfan.
In a scene that features almost every color that a Winter Sunrise can offer from deep purple to bright orange. – A Wisconsin & Southern freight is just out of Iron Ridge, Wisconsin and heading towards Horicon the morning of January 25th, 2018. ~~ A Jeff Hampton Photograph ©
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The robin features prominently in British folklore and that of northwestern France, but much less so in other parts of Europe. It was held to be a storm-cloud bird and sacred to Thor, the god of thunder, in Norse mythology. But this one was quietly waiting for me in the Jardins de Bagatelle.
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The fumaroles at Steamboat Point are the first major thermal features a visitor will encounter when entering Yellowstone National Park from the East Entrance. Fumaroles are vents or openings at the surface where volcanic gases and vapors are emitted. Faint to loud roars and hissing can be heard as the gas escapes the vent. Most of the vapor emitted by fumaroles is steam, formed as groundwater circulates deeply through heated rock. The water vapor mixes with volcanic gases given off by magma deep below in Yellowstone’s caldera. These volcanic gases include sulfur compounds, such as various sulfur oxides and hydrogen sulfide which accounts for the sulfur or “rotten egg smell” visitors may notice. There are no geysers that erupt water here. The fumaroles at Steamboat Point are some of the thermal features associated with the Marys Bay hydrothermal explosion crater that forms this rounded bay on the northeast side of Yellowstone Lake. There are several such hydrothermal explosion craters scattered across Yellowstone National Park in Wyoming. They range from tens of feet to more than a mile across. This one at Marys Bay is not only the largest hydrothermal explosion crater documented in Yellowstone but it is also the largest in the world. It measures 1.5 miles (2.6 km) in diameter and forms an embayment on the north side of Lake Yellowstone. The crater, which formed 13,800 years ago, may have been the result of several separate explosions over a short period of time. The cause or trigger for these hydrothermal explosions are not fully understood but pressure release due to glacial melting, earthquakes, or rapid changes in lake levels could be significant factors. Geological studies have found that these large, violent hydrothermal events are independent of associated volcanism. In the past 16,000 years, none of these events have been followed by an eruption of magma. The deeper magma systems seen unaffected by these sometimes spectacular steam explosions in their overlying hydrothermal systems.
Yellowstone National Park
Wyoming
USA
An abstract from the Porcelain Basin in Yellowstone showing a closeup of the orange and brown thermophiles growing in the cooler waters. This image of the themophiles is only about a foot across
Norris Geyser Basin is the hottest, oldest, and most dynamic of Yellowstone's thermal areas. The highest temperature yet recorded in any geothermal area in Yellowstone was measured in a scientific drill hole at Norris: 459°F (237°C) just 1,087 feet (326 meters) below the surface! There are very few thermal features at Norris under the boiling point (199°F at this elevation).
Norris shows evidence of having had thermal features for at least 115,000 years. The features in the basin change daily, with frequent disturbances from seismic activity and water fluctuations. The vast majority of the waters at Norris are acidic, including acid geysers which are very rare. Steamboat Geyser, the tallest geyser in the world at 300–400 feet (91–122 m) and Echinus Geyser (pH 3.5 or so) are the most popular features.
The basin consists of two areas: Porcelain Basin and the Back Basin. Porcelain Basin is barren of trees and provides a sensory experience in sound, color, and smell; a 3/4-mile (1.2-km) bare ground and boardwalk trail accesses this area. Back Basin is more heavily wooded with features scattered throughout the area. A 1.5-mile (2.4-km) trail of boardwalks and bare ground encircles this part of the basin. – Wikipedia
The church is a modest building that reflects the typical features of Romanian architecture: domed domed tower-domed, trilobated plant and porch on the façade. On the front opens the beautiful marble porch with five polychrome arcades supported by columns from the rich capitals resting on a fine travertine balustrade with vegetable and zoomorphic motifs. The arcade module continues, blind, across the entire outline of the building, above it runs a marble cornice with floral motifs that separate it from the top. The latter is decorated by a gouge frescoed with foliage and rhymed by medallions bearing the figures of Saints. It is accessed through a small nook, domed, separated by grooved marble columns.
La iglesia es un edificio modesto que refleja las características típicas de la arquitectura rumana: cúpula de cúpula de torre, planta trilobulada y porche en la fachada. En la parte delantera se abre el hermoso porche de mármol con cinco arcadas policromadas sostenidas por columnas de los ricos capiteles que descansan sobre una fina balaustrada de travertino con motivos vegetales y zoomorfos. El módulo de arcade continúa, ciego, a lo largo de todo el contorno del edificio, encima corre una cornisa de mármol con motivos florales que lo separan de la parte superior. Este último está decorado con una gubia pintada al fresco con follaje y rimada por medallones con las figuras de los santos. Se accede a través de un pequeño rincón, abovedado, separado por columnas de mármol acanaladas.
Bucharest. Romania Europe
Ha Long Bay features over 1,600 limestone karsts and islets rising dramatically from emerald-green waters. These formations, shaped by 500 million years of geological evolution, are dotted with caves, grottoes, and secluded beaches.
The name “Ha Long” translates to “Descending Dragon”, derived from a local legend. According to the tale, a dragon descended from the heavens to protect Vietnam from invaders, creating the bay’s rocky islands by thrashing its tail.
On the roof of the boat you may notice three animated drone operators who are ecstatic over a perfect sunrise. One of the sunrises I will never forget.
WWT Slimbridge Wetland Centre.
What3Words
///trailers.ripen.grownup
The Mandarin Duck (Aix galericulata) is a medium-sized perching duck famous for being widely regarded as the world's most beautiful duck.
Vibrant Appearance
Mandarin ducks display striking sexual dimorphism, meaning the males and females look completely different:
The Male (Drake):
Highly elaborate and colourful. It features distinctive orange feathers that stick up like "sails" on its back, a purple chest with white bars, orange cheek plumes, and a bright red-pink beak. After the spring breeding season, the male sheds these feathers (moults) into a dull "eclipse" plumage that looks like the female, though he keeps his bright beak.
The Female (Hen):
Intentionally dull and grey-brown to blend into surroundings. She has a grey head, a prominent white ring around her eye with a stripe trailing behind it, and a mottled underside.
Habitat and Global Distribution
Native Range:
Densely wooded wetlands, shallow lakes, and marshes across East Asia, including China, Japan, Korea, and parts of Russia.
Introduced Populations:
They were brought to the UK as decorative birds for private collections in the 18th century. Escaped birds formed a thriving, naturalised wild population across Great Britain.
Behavior:
Despite their loud colours, mandarins are shy, timid birds that prefer hiding under overhanging willows and tree cover. They have long claws that allow them to perch on tree branches and fly through dense forests with incredible agility.
Diet
Mandarins are omnivorous foragers. They eat a varied diet consisting of:
Aquatic plants and seeds
Acorns and grains
Insects, land snails, and small fish
Tree Nesting and "Leaping" Chicks
Mandarin ducks have a unique and dramatic nesting ritual:
High Nesting:
Females lay a clutch of 9–12 eggs during the spring in natural tree cavities or holes, sometimes up to 9 metres off the ground.
The Leap of Faith:
Shortly after hatching, the mother flies down to the ground and calls to her ducklings.
Safe Landing:
The tiny, uninjured ducklings leap from the high tree cavity. Their light weight and fluffy down feathers cushion the impact, allowing them to bounce unharmed and follow their mother straight to the nearest water.
Cultural Symbolism
In traditional East Asian cultures—particularly in China and Japan—mandarin ducks are revered as a symbol of lifelong fidelity, love, and wedded bliss. Pairs are frequently depicted in oriental art and given as wedding gifts, even though wild ducks generally only pair up for a single breeding season.
Edwards Gardens in Toronto features a fountain that includes a gold statue. It's located within the larger Toronto Botanical Garden complex. The fountain is a prominent feature, often seen in photos and descriptions of the garden.
Kampong Glam (Singapore's Muslim Quarter) features many early shophouse style architecture (c. 1840s–1900s), characterized by
narrow, two-story, low-ceilinged structures with minimal plaster ornamentation. These conserved buildings often feature five-foot ways with arched walkways, French windows with louvered shutters, and, today, are renowned for vibrant murals, colorful facades, and independent boutique shops.
These are some of the earliest, most intimate shophouses in Singapore, with many just over 4 meters wide.
Gazetted as part of the Kampong Glam Conservation Area in 1989, these buildings maintain their historical structure while being adapted for modern retail, cafes, and restaurants.
Kata Tjuta in the Australian Northern Territory features heavily in the Aboriginal dreamtime stories, "Tjukurpa"- the foundational belief system of the Aboriginal indigenous people.
Kata Tjuta means "many headed" as it is made up of 36 separate domes made up of conglomerate rock. The rocks are also called the Olgas or Mount Olga named by the explorer Ernest Giles after Queen Olga of Wurttemberg. Travel has certainly always been a dream of mine and visiting places like these are top of the list.
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After the grain train clears the block at MP 132, the signal displays "approach medium". This is one of the unique features that will disappear when the new signal system is cut over.
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Sastrugi
Sastrugi, or zastrugi, are features formed by erosion of snow by wind. They are found in polar regions, and in snowy, wind-swept areas of temperate regions, such as frozen lakes or mountain ridges. Sastrugi are distinguished by upwind-facing points, resembling anvils, which move downwind as the surface erodes. These points usually lie along ridges parallel to the prevailing wind; they are steep on the windward side and sloping to the leeward side. Smaller irregularities of this type are known as ripples (small, ~10 mm high) or wind ridges.
Large sastrugi are troublesome to skiers and snowboarders. Traveling on the irregular surface of sastrugi can be very tiring, and can risk breaking equipment—ripples and waves are often undercut and the surface is hard and unforgiving, with constant minor topographic changes between ridge and trough.
Etymology
The words sastrugi and zastrugi are Russian-language plurals; the singular is zastruga. The form sastruga started as the German-language transliteration of the Russian word заструга (plural: заструги).
A Latin-type analogical singular sastrugus is used in various writings on exploration of the South Pole, including Robert Falcon Scott's expedition's diaries and Ernest Shackleton's The Heart of the Antarctic.
Formation mechanism
White and black colors on sastrugi are not lights and shadows, they demonstrate difference in radioreflectivity of snow deposits on the windward and leeward sides of a sastruga.
Under the action of steady wind, free snow particles accumulate and drift like the sand grains in barchan dunes, and the resulting drifting snow shapes are also popularly referred to as barchans. Inuit of Canada call them kalutoqaniq. When winds slacken, the drifted formations consolidate via sublimation and recrystallization. Subsequent winds erode kalutoqaniq into the sculptured forms of sastrugi. Inuit call large sculpturings kaioqlaq and small ripples tumarinyiq. Further erosion may turn kaioqlaq back into drifting kalutoqaniq. An intermediate stage of erosion is mapsuk, an overhanging shape. On the windward side of a ridge, the base erodes faster than the top, producing a shape like an anvil tip pointing upwind.
On sea ice
Sastrugi are more likely to form on first-year sea ice than on multiyear ice. First-year ice is smoother than multiyear ice, which allows the wind to pass uniformly over the surface without topographic obstructions. Except during the melt season, snow is dry and light in climates cold enough for sea ice, allowing the snow to be easily blown and create sastrugi parallel to the wind direction. The locations of sastrugi are fixed by March in the northern hemisphere and may be linked to the formation of melt ponds. Melt ponds are more likely to form in the depressions between sastrugi on first-year ice.
Source: Wikipedia
This view looks across Yellowstone Lake from the shores Sedge Bay along the East Entrance Road In Yellowstone National Park, Wyoming. The hill on the left side of the photo is Steamboat Point. One close inspection of the photo, steam can be seen rising from fumaroles at the base of the hill just above the lake. These fumaroles are some of the first thermal features encountered by visitors who enter the park from the East Entrance. Fumaroles are vents or openings at the surface where volcanic gases and vapors are emitted. Faint to loud roars and hissing can be heard as the gas escapes the vent. Most of the vapor emitted by fumaroles is steam, formed as groundwater circulates deeply through heated rock. The water vapor mixes with volcanic gases given off by magma deep below in Yellowstone’s caldera. These volcanic gases include sulfur compounds, such as various sulfur oxides and hydrogen sulfide which accounts for the sulfur or “rotten egg smell” visitors may notice. There are no geysers that erupt water here. The fumaroles at Steamboat Point are some of the thermal features associated with the Marys Bay hydrothermal explosion crater on the side of Yellowstone Lake. There are several such hydrothermal explosion craters scattered across Yellowstone National Park in Wyoming. They range from tens of feet to more than a mile across. This one at Marys Bay is not only the largest hydrothermal explosion crater documented in Yellowstone but it is also the largest in the world. It measures 1.5 miles (2.6 km) in diameter and forms an embayment on the north side of Lake Yellowstone. The crater, which formed 13,800 years ago, may have been the result of several separate explosions over a short period of time. The cause or trigger for these hydrothermal explosions are not fully understood but pressure release due to glacial melting, earthquakes, or rapid changes in lake levels could be significant factors. Geological studies have found that these large, violent hydrothermal events are independent of associated volcanism. In the past 16,000 years, none of these events have been followed by an eruption of magma. The deeper magma systems seen unaffected by these sometimes spectacular steam explosions in their overlying hydrothermal systems.
The hill across the lake just beyond its western shore is The Elephant Back. Most of the top of this hill lies above 8600 feet above sea level (ASL) with the culmination at 8731 feet ASL. Elephant Back is typical of the topography in the center of the Yellowstone Caldera.
The park features horticultural exhibits with a pond, falls, bridge, trees and flower beds. As you progress deeper into the park, native plants, ferns and trees dominate and create a wilderness escape full of birds, animals, trees and trails.
New Westminster, British Columbia, Canada
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Usagi Society - Barbara Hair
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~Features
86 Colors
3 Rigged Sizes
1 Unrigged Bangs
Toggle Materials
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========================
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Amitie Closet (PBR)
October features work in progress. There will be 6 mini sets of 5 images each......they all are images that will eventually be part of a larger series.......but for now you can see them as they are now..........warts and all.
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Lighting – Annan Adored Realistic Ambient
Pose - *PosESioN* Geometric 3
Stylist, Photographer, Model – Yhishara Cerise
Update: this is actually not a geyser, but a pool at the Black Sand Basin.
From the website: www.yellowstonenationalpark.com/blacksand.htm
Temperature 180°F Dimensions 145x191 feet. Depth 23.5 feet. Sunset Lake is a shallow thermal pool with a soft sinter bottom and yellow and orange bacteria and algae edges. The pool discharges into Iron Creek, and overflows into Rainbow Pool creating a large microbial mat between the two thermal features. The 1959 earthquake triggered an eruption of Sunset Lake and the surge of hot water killed the bacteria and algae in the run-off channels. It has erupted only occasionally since 1959; during eruption it surges three feet high but may reach eight to ten feet. No known underground connection exists between Rainbow Pool or other Black Sand Basin thermal features.
Thank you for taken your time to visit me, comments or faves are always much appreciated!
Excerpt from conservationhamilton.ca:
Phoenix Creek Sink: We can see the water sinking underground here. Scientists have tested the water and know that this is the same stream we saw spring up at Pottruff Spring.
It is difficult to guess the course the water took to get from here to there because it travels underground and we cannot see it flow. But, we can look at the evidences of water on the surface and make hypotheses.
One way scientists can tell if water has flown underground is by checking the water’s temperature. In the summer, the spring water will be colder than water from a surface stream because the sun will not warm it up as it flows underground. In the winter, the spring water will be warmer because the cold air will not have chilled it, as it did the surface water.
“Colors , like features, follow the changes of the emotions.”
▪▫●▫▪
"If you have on red then you heard what I said"
"If you have on blue then you know what to do."
"If you have on white then you know what's right.
"If you have on black then your name must be Jack.
"If you have on gray then it's going to be a wonderful day!
"If you have on brown then you better get down.
"If you have on green then you know what I mean.
"If you have on yellow then you're a nice fellow.
"If you have on pink then you know what I think.
"If you have on purple then you like to eat Slurple.
XP
▪▫●▫▪
i’m getting seriously CRAZY ..!
XD
" انا احب الللون الاصــفر
انتوا اي لون تحبون
XD
كـح
Happy b.day Asoom.. this pic goes to you .. “ colors freak “ =P
Happy b.day Ghayood sweet 17 ya 7elwa ..!
▪▫●▫▪
يمكـن ما تعودتوا على الخبـال في فلكـري
بس يمدحـون التغيـير
..!!
=P
what's your mood color ?!
ممكـن تحطون دعايـة لاخر صوركم بس
في 188 pix مايكـون المقاس اكثر من250
Well here's another image that features in my latest YouTube video that I shared with you all last night. If you have yet to watch it, simply click on the link below to see this image and many more as well as me rambling on in the falling snow. It really was a winter wonderland :D
www.youtube.com/watch?v=gN28MBP3V7Y
Have a great evening and please feel free to SUBSCRIBE and also leave a comment under the video on YouTube if you fancy.
Many thanks and enjoy.
Canon 5D MK4
Canon 70-200mm f4 @ 131mm
f11
1/100 sec
ISO100
Nisi 3 Stop Grad ND Medium filter
Gitzo GT3543XLS carbon fibre tripod
Gitzo GS3121LVL low profile levelling base
Manfrotto 405 geared tripod head
Mindshift Backlight 36L Bag
UK & Iceland Landscape Photography Workshops, 1-2-1 Private Tuition, print sales and camera club lectures available
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Kirk Maughold Church is one of the oldest churches on the island with features dating back to the sixth century.
The church was founded around 447 AD by the Celtic St Maughold who was expelled from Ireland by St Patrick and landed here on the coast towards the end of the 5th century, bringing Christianity with him.
The church is a simple structure typical of traditional Manx churches and contains a large number of historically significant Celtic crosses dating from the early Christian period (6th-13th century)
L'église Kirk Maughold est l'une des plus anciennes églises de l'île avec des éléments remontant au sixième siècle.
L'église a été fondée vers 447 après J.-C. par le celtique St Maughold qui fut expulsé d'Irlande par St Patrick et débarqua ici sur la côte vers la fin du 5ème siècle, apportant avec lui le christianisme.
L'église est une structure simple typique des églises mannoises traditionnelles et contient un grand nombre de croix celtiques d'importance historique datant de la période paléochrétienne (VI-XIII siècle)
Artist Eline Kersten lives and works in Switzerland.
The Timekeepers series (2024-2025) features hand-blown glass objects filled with glacial water from Antarctica and Greenland. The water comes from ice that scientists melt to collect data. In Timekeepers, this water preserves itself as a kind of time capsule. Paper certificates show the age of the ice.
Kunstenaar Eline Kersten, woont en werkt Eline in Zwitserland.
De serie Timekeepers (2024-2025) toont handgeblazen glazen objecten, gevuld met gletcher water uit Antartica en Groenland. Het water komt van ijs dat wetenschappers laten smelten om gegevens te verzamelen.
In Timekeepers bewaart dit water als een soort tijdscapsule.
Op papieren certificaten is te zien hoe oud het ijs is.
Die Künstlerin Eline Kersten lebt und arbeitet in der Schweiz. Das Wasser stammt aus Eis, das Wissenschaftler schmelzen, um Daten zu sammeln. In „Timekeepers“ konserviert sich dieses Wasser wie eine Art Zeitkapsel. Papierzertifikate geben das Alter des Eises an.
La série « Les Gardiens du Temps » (2024-2025) présente des objets en verre soufflé remplis d'eau glaciaire provenant de l'Antarctique et du Groenland. Cette eau provient de la glace que les scientifiques font fondre pour collecter des données. Dans « Les Gardiens du Temps », cette eau se conserve comme une capsule temporelle. Des certificats en papier indiquent l'âge de la glace.
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