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Another shot from higher up of Bow Locks in East London. The River Lea Navigation (in reality a canal) rejoins the natural river here after the two have run roughly parallel since Hertford Castle Weir in Hertfordshire, north of Greater London. However the canal section continues to the right as The Limehouse Cut, which provides a straight route to Limehouse Basin and The River Thames, avoiding the bendy and tidal lower reaches of the main river which joins The Thames at Trinity Buoy Wharf.
A closer look at the confluence of Glacier Los Leones south, center and north glaciers where they descend from the icefields of Parque Nacional Laguna San Rafael (upper left) and terminate in the beautiful glacial green Lago Leones, Patagonia. Several avalanche tracks can be seen on the steep cliffs to the right of the image.
19/02/2021 www.allenfotowild.com
J’ai pris cette photo sous le bâtiment du musée des confluences à Lyon. Les personnes en silhouettes sur le bord opposé du bassin étaient toutes dans des postures expressives. Deux secondes avant ou deux secondes après, la photo aurait forcément été différente …
Sadhus singing holy songs for god, while modern sports facilities await people to enjoy those....a typical display of Indian confluent culture on the bank of ancient river Betwa in Memorial campus of Orchha, Madhyapradesh, India
Cañón de Añisclo, Sobrarbe, Huesca, Aragón, España.
El cañón de Añisclo o del río Bellos se sitúa en el Pirineo de Huesca, comunidad autónoma de Aragón, España, al sur del macizo de Monte Perdido, discurriendo rectilíneamente en dirección Sur durante más de 10 km, desde el Circo de Añisclo a los pies del mismo Monte Perdido, hasta la confluencia con el valle del río Aso.
El cañón de Añisclo forma parte del parque nacional de Ordesa y Monte Perdido, junto con el macizo de Monte Perdido, Valle de Ordesa, las Gargantas de Escuaín y la cabecera del valle de Pineta.
Al norte, el Circo de Añisclo está cerrado por el Collado de Añisclo, entre el Monte Perdido y la Sierra de las Sucas, paso a 2500 metros de altitud que comunica con el Valle de Pineta. Al Oeste, la Sierra Custodia y el Mondicieto separan a este valle del Valle de Ordesa, mientras que al Este, tras otra cresta, se encuentran las Gargantas de Escuaín.
Se trata de un impresionante valle, que en su cabecera tiene un circo glaciar, pero que posteriormente se encajona en un profundo cañón, fruto de la acción kárstica del agua del río sobre la roca caliza, en una sucesión de bellos toboganes y cascadas, entre los que hay que reseñar la Fuen Blanca o Fon Blanca, un nacimiento en la pared vertical del Pico de Añisclo (o Soum de Ramond) que se desploma verticalmente sobre el valle. En los sitios en los que el terreno y la altura permiten el crecimiento de vegetación, la gran humedad y la casi permanente sombra del profundo cañón, producen tupidos bosques como la Selva Plana.
A la altura de la ermita de San Úrbez, el cañón del Bellos se encajona más si cabe y toma dirección NW-SE hasta la localidad de Escalona.
The Añisclo canyon or the Bellos river is located in the Pyrenees of Huesca, autonomous community of Aragon, Spain, south of the Monte Perdido massif, running straight south for more than 10 km, from the Circo de Añisclo at the foot from Monte Perdido itself, up to the confluence with the Aso river valley.
The Añisclo canyon is part of the Ordesa y Monte Perdido National Park, together with the Monte Perdido massif, Ordesa Valley, the Escuaín Gorges and the head of the Pineta Valley.
To the north, the Circo de Añisclo is closed by the Collado de Añisclo, between the Monte Perdido and the Sierra de las Sucas, a pass at an altitude of 2500 meters that communicates with the Pineta Valley. To the west, the Sierra Custodia and the Mondicieto separate this valley from the Ordesa Valley, while to the east, behind another ridge, are the Escuaín Gorges.
It is an impressive valley, which has a glacial cirque at its head, but which is later encased in a deep canyon, the result of the karst action of the river water on the limestone rock, in a succession of beautiful slides and waterfalls, between The ones to be highlighted are the Fuen Blanca or Fon Blanca, a source in the vertical wall of Pico de Añisclo (or Soum de Ramond) that falls vertically over the valley. In places where the terrain and height allow the growth of vegetation, the high humidity and the almost permanent shadow of the deep canyon, they produce dense forests such as the Flat Jungle.
At the height of the hermitage of San Úrbez, the Bellos canyon becomes more confined if possible and takes a NW-SE direction to the town of Escalona.
2,000 feet down two rivers meet where the Green offers up it’s current to the Colorado. Their headwaters distant and in differing states, yet join here in these depths for a dance through the Grand to empty with all the others flowing, to begin again as rain.
I created this piece in Adobe Fresco. It is a meditation on the confluence of the Green and Colorado Rivers and the rock formations that line the river's flow. A print of this and other artwork will be on display in the Datura Deli in Moonflower Market in Moab, Utah for July and August.
Im hinteren Lenninger Tal, direkt unterhalb von Gutenberg, fließen zwei Quellflüsse der Lauter ineinander.
I call this Confluence because there are a number of factors coming together in this sunset/early twilight vista looking east: Earth Shadow, Belt of Venus colors, a singular broad anti-crepuscular ray fading into the vanishing point, and the moon.
Senge Tsangpo སེང་གེ་གཙང་པོ་ county
Senge Tsangpo སེང་གེ་གཙང་པོ་ county, formerly known as Gar, straddles the confluences of the Senge Tsangpo སེང་གཙང་པོ་ (Indus River) and two of its tributaries: the Langchu Tsangpo, which converges at the town of Senge Khabab, and the Gar Tsangpo, which converges south of Tashigang. Senge Khabab, which is both the prefectural and county capital, is located at Senge Tsangpo Area: 11.802 sq km. www.footprinttravelguides.com/c/2848/tibet/&Action=pr... སྒར། > sgar > Gar The name sGar is said to have come from the many military camps (sgar) that dGa’ ldan tshe dbang set up in this area as reinforcements for the government of Tibet. After that the area came to be called sGar. The rdzong was created in 1959. The region of sGar is populated by semi-nomads. There are many livestock animals, such as yaks, goats and sheep, oxen, bulls, mdzo and mdzo mo, horses and mules. There is also a considerable amount of wheat, barley and beans harvested. The rdzong is rich in minerals, including coal, white salt, gold, lead and salt. It is, moreover, the habitat of a great many animals, such as wild yaks, yellow leopards, wild asses, black bears, Tibetan lynxes, antelopes, Tibetan antelopes, foxes and wolves. There are also many unique characteristics of sGar rdzong to be seen in the popular old legends, myths, music, dances and other facets of the culture. sGar rdzong possesses a number of sites of historical interest, including the monasteries of Dri bda’ spos ri, Gyam smyug lha khang, mDun chu Monastery and Gu ru gyam, the Bonpo monastery. Many of the important Bonpo monasteries can still be visited. www.thlib.org/places/monasteries/list/nyingma/#iframe=htt...
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Sunrise at the place where the East and West Branches of the DuPage River come together to form a single waterway.
Not managing to get out much at the moment, partly due to a dodgy knee and rubbish weather, so another one from last year
Old friends will recognize one of my favorite "theme" topics (see the SET to the right)--this falls on Sugar River which is truly a well kept secret. Even on the sunniest weekend summer day there will be only one or 2 groups of people enjoying the view and the misty air; most often I'm there alone when I shoot. I went out to do a test of the new 80-400mm and had a terrible time :) Mist on the lens (forgot the lens hood), more water coming over the falls than I've ever seen, so the water blur effect was anything but subtle. Also, I didn't dare cross over the stream, which had turned into a rushing torrent that seemed a foot or 2 higher than I've seen--covering most of the stepping stones I usually use. No way the new lens was going to be trusted to my footing under those conditions. And the best shots are from the other side !! I also found out that the default setting for the remote timer on the D90 can really work against a tripod shooter in adverse conditions. It kept timing out on me while I played with shutter speeds and zoom settings, and wiping the lens, requiring enough resets that I was forced to read the manual (later) to find which menu item holds the longer settings. Oh my. Anyhow, this one looked OK after all the bother, so here you are.