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Fitness instructor, Steff Owens, jumps elegantly from the railings of a London landmark at London Tower bridge.

 

Lighting: 2 SB28 units from either side - one bare from behind left, creating the rim (on a low power), the other from the right through a white brolley. Both flashes triggered with pocket wizards.

  

Jon and Tina | Portfolio | Travel Portfolio | Follow our Work

Rommerskirchen, Field

Volcanic formed rocks - Daepo Jusangjeolli Cliff (주상절리(대포동지삿개) - juju Island, South Korea

It now contains a day care.

Veig, veig...que veus?...unes formes...de quins colors?...groc, blau, vermell..

The Reversible Brave Plush Toy - 13'' H is a depiction of one of the triplets cubs and Princes from the upcoming Disney/Pixar animated movie Brave. It sells for $19.50, or 2 for $30. It was released on May 14, 2012 in the US and Canada, both online and in stores.

 

This doll can transform from being a bear cub to being one of the triplet Princes, with kilt and boots. There is a velcro closure in the back that allows for the plush toy to be turned inside out, then closed back up neatly. Since the doll is reversible, their arms and legs are not fully formed. In the bear cub form, the arms are sewn into the body, the legs are merely stumps at the bottom of the body, so he cannot stand on his own. In the Prince form, he has a full head of orange velvet hair formed into large curls, embroidered face with a smirking grin, arms that are sewn to the body, a belted kilt and brown boots. He has very short, skimpily stuffed legs, but his feet are well stuffed, and can be turned to the sides or to the front.

 

It is great fun to reverse the doll. It was surprisingly easy to figure out how to stuff one side of the doll inside the other, and close up the back neatly. It is very well made, and quite soft and cuddly, and both the cub and the Prince sides are very cute.

IMG_1402c 2023 08 17 file

Skippy in the ExtraTerrorRestrial Alien Encounter attraction, taken during the Fab2K trip with Peter Schouten. February 4, 2000

James -

 

Here are photos of the tornado forming, along with a description of each.

 

My friend, Nick Lee, is a storm spotter. He and I were out taking these

photos that day. He is the copyright owner and has given me permission to

share them with you.

 

Dirk

 

P.S.: Please use the descriptions somehow in your description of the photos.

 

Description of photos:

 

Tornado-1: shows the storm coming around the corner into view.

Tornado-2: Inflow notch seen - this is where the air feeding the updraft was

located at.

Tornado-3 & 4: Tornado on ground getting closer to City of Cullman. At this

point it was passing Good Hope and going through Cullman County.

Tornado-5: Here you can see another vortex forming. What we were witnessing

was a rapid intensification of this storm from an EF2 to a multi-vortex EF4.

Tornado-6: Even though the funnel is hard to see, the tornado was still on

the ground. Here you can see the multiple vortexes spinning around the one

in the middle that looks like it is invisible.

Another art class ink sketch

For Mosaic Montage Monday theme of Fluid Forms is this montage of the young curled fern frond at the Dale Chihuly Exhibit at the Adelaide Botanic garden and an overlay of flowing lines and dots. Many of Dale Chihuly pieces exhibit flowing curls and curves too indicating fluidity. HMMM

© All rights reserved.

Reproduction or redistribution in any form without prior written permission is strictly prohibited.

Prohibida la reproducción total y parcial de las fotografías expuestas salvo autorización expresa de su autor.

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Blue form of White-lipped Island Pitviper, from Komodo Islands

Beautiful snake in the world?

www.matthieu-berroneau.fr

 

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@Fotosöndag: Form kan vara vad som helst. Därför kom jag att fundera på, vilken form som kan vara avgörande för att fylla en funktion. Det första som dök upp var en "gammaldags" blyertspenna som måste formas med hjälp av en pennvässare för att fungera.

formato A4, schizzo a china con pennino e pennelli, su carta liscia riciclata. da mie fotografie

The lake was formed due to a massive landslide at Attabad village in Gilgit-Baltistan, 9 miles (14 km) upstream (east) of Karimabad that occurred on January 4, 2010. All type of traffic on KKH to and from China was disconnected. In next few days, Attabad Lake was converted into a dam with 130-200 m depth and 22 km length. If this dam was left to be further filled, it would have resulted into a “Dam burst scenario” and would have been the worst disaster of the world. In case of the dam burst, the flow of water downhill towards Gilgit would have been so massive that most of the bridges and villages astride river Hunza would have been completely washed away.

 

Shehzaad Maroof Photography

43046 brings up the rear of The Blue Pullman, back on the Midland in the form of LSL’s HST version heading up the Erewash Valley at Long Eaton working 1Z43, 09:10 St Pancras – Crewe on a wet 12th December 2020.

 

Locomotive History

43046 was built at Crewe Works as part of HST set 253023 for Western Region London – Bristol/South Wales services and entered traffic in December 1976. 253023 was one of five Western Region HST sets transferred to Midland Main Line duties in 1982 and 43046 has been pounding up and down to London St Pancras from the East Midlands and South Yorkshire for last thirty seven years until acquired by LSL in 2020. It has been fitted with a Paxman VP185 engine in lieu of its original Paxman Valenta.

  

Hanging tapering pieces of ice formed by the freezing of dripping water on a Colorado license plate.

 

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formato A4, schizzo a inchiostro e pennelli vari, ispirato alla bellissima fotografia di Fabio Prosperi

He can hold the carvers too =D Had to add those minifig hands in the fingers for it though. Look proper of a scrapbot, which fits him, but also a bit evilish. Tsk.

Sony A7R IV and Aposummicron M 50mm asph

J'ai pris ces photos un matin, à 5h40, lorsque le soleil se levait..

 

I took these pictures a morning at 5:40am, during the sunrise

 

Julien Delfort ©

Norwegen / Nordland - Helgelandskysten

 

Ågskardet

 

Helgeland is the most southerly district in Northern Norway. Generally speaking, Helgeland refers to the part of Nordland county that is located south of the Arctic Circle. It is bordered in the north by the Saltfjellet mountains and Svartisen glacier, which form a natural border with the Salten district. In the south, Helgeland borders Trøndelag county.

 

The district covers an area of about 18,832 square kilometres (7,271 sq mi), with nearly 79,000 inhabitants. There are four towns in the district: from south to north these are Brønnøysund, Mosjøen, Sandnessjøen, and Mo i Rana.

 

Name

 

The Old Norse form of the name was Hálogaland (see Hålogaland).

 

Geography

 

Helgeland is commonly divided into three or four sections:

 

Southern Helgeland (actually southwest), which consists of the municipalities Bindal, Sømna, Brønnøy, Vega and Vevelstad.

Central Helgeland, which is sometimes further divided into the regions:

 

Inner Helgeland, which consists of the municipalities Grane, Hattfjelldal and Vefsn.

 

Outer Helgeland, which consists of the municipalities Leirfjord, Alstahaug, Herøy and Dønna.

 

Northern Helgeland, which consists of the municipalities Hemnes, Rana, Nesna, Lurøy, Træna and Rødøy.

 

Helgeland is characterized by pointed mountains and Strandflaten, a shallow lowland area, sometimes just above the sea surface, and sometimes just below the surface. People living on the coast have settled on this lowland (while inland towns, such as Mo and Mosjøen, are situated in valleys). A consequence of the Strandflaten is thousands of islands, and shallow waters going far into the sea. This has provided some shelter from stormy weather, which might occur in winter. Some islands are fairly large, often with unique mountains, such as Torghatten, De syv søstre (The Seven Sisters), Hestmannen, Rødøyløva (in Rødøy), Dønnamannen (picture), and Træna. There are several sea bird colonies, such as Lovund with thousands of puffins. The Solvær Islands (Solværøyene) in Lurøy consists of about 300 small and flat islands and has the highest densities of Eurasian eagle-owls in Europe.

 

The highest mountains, are located inland, where Oksskolten is the highest mountain in Northern Norway. There are many valleys inland, such as the Dunderland Valley, Vefsndalen, and Hattfjelldal. Røssvatnet is the second largest lake in Norway. There are three large national parks in Helgeland: Saltfjellet–Svartisen National Park (partly), Børgefjell National Park (partly), and Lomsdal–Visten National Park (created in May 2009).

 

Cultural references

 

Helgeland is the scene for Henrik Ibsen's 1857 historical play "The Vikings at Helgeland" (Hærmændene paa Helgeland), whose plot takes place at this region during the time of Erik Blood-axe (c. 930–934).

 

Helgeland Kammerkor, a mixed choir with members from all parts of Helgeland, have recorded an album of folk music from Helgeland (Folketoner fra Helgeland, 2005). The album contains 27 folk tunes from Helgeland, recorded in collaboration with folk musicians from the area. The album was recorded in Alstahaug Church, a 900-year-old stone church located near Sandnessjøen.

 

(Wikipedia)

 

Ågskardet is a village in Meløy Municipality in Nordland county, Norway. It is located on the southern side of the Holandsfjorden, about 3.5 kilometres (2.2 mi) north of the village of Tjong (in neighboring Rødøy Municipality). There were 127 inhabitants in 2008.

 

The village lies along Norwegian County Road 17, with a ferry connection to a port, just west of the village of Halsa. The ferry is the only connection to the rest of Meløy Municipality to the north. The village is situated just north of the border with Rødøy Municipality. The village has its own school, chapel/community centre, and some private companies.

 

(Wikipedia)

 

Helgeland (im Mittelalter Hålogaland) ist eine Landschaft im Norden Norwegens, die heute den südlichen Teil des Fylkes Nordland bis zum Saltfjellet umfasst. Die Region hat 78.400 Einwohner und eine Fläche von 17.936 km². Die Region hat ungefähr 15.000 Inseln.

 

Im Mittelalter bezeichnete Hålogaland das gesamte Territorium nördlich von Trøndelag und war vor der Christianisierung Norwegens ein selbständiges Königreich, das auch den größten Teil von Troms umfasste und sich zeitweilig bis in das von Samen dominierte Gebiet (Finnmark, Schwedisch-Lappland, Nord-Finnland und Nordwest-Russland) erstreckte. Hålogaland nimmt einen hervorragenden Platz in den Sagas ein. Die Göttinnen Þorgerðr Hölgabrúðr und Irpa der Jómsvíkinga saga stammen wahrscheinlich aus Hálogaland und wurden wohl vor allem dort verehrt. Der vermutlich bekannteste Einwohner Hålogalands war der Seefahrer und Kaufmann Ottar, dessen Bericht über seine Heimat einen Platz in Alfreds des Großen Übersetzung der Weltgeschichte des Orosius fand.

 

Der Name stammt nicht von derselben Wurzel wie heilig, wie es schon Adam von Bremen behauptete, sondern von einer Volksbezeichnung háleygir. In Snorri Sturlusons Jüngerer Edda wird er von einem mythischen König Holgi abgeleitet. Holgi wiederum soll ein Nachfolger von Odins Sohn Sæming (Säming) gewesen sein.

 

Die jüngere Form des Namens findet sich ab 1380, die ältere besteht weiter in den Namen der Bistümer Sør-Hålogaland (Nordland) und Nord-Hålogaland (Troms und Finnmark) und im Namen des Obergerichtes (Hålogaland lagmannsrett), das für die drei nördlichen Provinzen Nordland, Troms und Finnmark sowie für Spitzbergen zuständig ist.

 

In Helgeland befand sich bei Bratland und der Insel Aldra ein Sender des Omega-Funknavigationssystems. In der Nähe von Bratland befindet sich auch der Marinesender JXN, der wie einst der Omegasender eine Drahtantenne verwendet, die über einen Fjord gespannt wurde.

 

(Wikipedia)

It's always a fun time when form and light hang out together.

 

Copyright © 2013 by Craig Paup. All rights reserved.

Any use, printed or digital, in whole or edited, requires my written permission.

 

Honda Prelude in Delmenhorst.

www.tourduvalat.org/en/newsletter/la_reserve_naturelle_re...

  

A remarkable site for temporary ponds

  

The Tour du Valat Foundation is the owner of a 2560 ha estate made up of natural and agricultural lands, grazed by some 450 Camargue cattle and 80 Camargue horses. The natural zones form a mosaic of the emblematic and now rare habitats of the fluviolacustrine Camargue, the area at the interface between riverine and maritime influences.

 

These relatively non-saline habitats were largely destroyed in the past for the development of agriculture. The result is a natural heritage of exceptional value, adapted to the particular conditions of the area. Since July 2008, 1845 ha of the Estate (i.e., 72% of its total surface area) have been granted the protection status Réserve naturelle régionale or Regional Natural Reserve (RNR).

 

Of the many natural habitats that make up the site, the temporary ponds are among the most remarkable. Some of them (the least saline) are examples of a habitat of priority community interest under the European Habitats Directive, which are in sharp decline around the Mediterranean basin, Mediterranean Temporary Ponds (MTP)1. Such ponds cover a total surface area of 18.3 ha on the Tour du Valat Estate, i.e. 65% of all the MTPs in the Camargue.

 

In all, there are 65 ponds of various kinds on the Estate covering a total surface area of about 60 ha (their size is highly variable in function of water level). They vary considerably in size, shape, depth, level of isolation, and salinity, with consequent influences on the plant and animal communities that live in and around them.

  

In particular, there is a wide diversity of plant species, certain of which are highly threatened. Among the eleven protected species (four at national level, and seven at regional level) found in the Tour du Valat RNR, two are of major importance for conservation:

 

The Starfruit or Water star (Damasonium polyspermum) is an attractive little white-flowered annual plant, a member of the Alismataceae family. This Western Mediterranean endemic is typical of Mediterranean temporary ponds. Its world conservation status is listed as Vulnerable by the International Union for the Conservation of Nature (IUCN), and it is protected by ministerial decree in France, where it is present at some ten sites, including the Tour du Valat. In the RNR, it is found, sometimes in populations of several thousands, in six oligosaline (very slightly salty) ponds with a sunny exposition and scattered emergent vegetation; it emerges only when flooding conditions are favourable, i.e. when there is enough water in early spring.

Riella helicophylla is a small aquatic liverwort just a few centimetres in height. Endemic to the Mediterranean basin, it is listed in Annex II of the Habitats Directive, and is currently being added to the list of French protected species. It is fond of distinctly saline, shallow, clear, temporary flood water, with limited plant cover. It was only recently discovered at the Tour du Valat (March 2012) in saline borrow pits and some low depressions in the flooded sansouïres bordering the Baisse Salée and the Saline ponds, covering at least 1.2 ha. Until then, it had only been found at one (former) site in the Hérault Department, and at Salin du Caban, east of

  

In terms of animals, the temporary ponds are also of primordial interest, for branchiopod crustaceans, odonates (dragonflies and damselflies), and amphibians. In wet springs, they literally teem with animals of kinds: from Triops cancriformis, a real living fossil, to the impressive tadpoles of the Common parsley frog or the Mediterranean/stripeless tree frog, and larvae of Zygoptera (damselflies, close relatives of the dragonflies). In this category, one of the commonest species in the Tour du Valat ponds, although highly threatened in France, is the Dark emerald damselfly or Dark spreadwing (Lestes macrostigma). This attractive damselfly, listed as Vulnerable in Europe by the IUCN, is only found in a few sites in France, along the Atlantic coast, in Corsica, and in the Camargue.

 

To conserve this natural heritage, it is necessary to maintain the natural hydrological regime of these ponds, characterised by their isolation and long completely parched periods in the summer. Their appearance thus varies immensely in function of precipitation level, ranging from bare cracked soil in late summer to vast flooded areas in wet springs, verdant and teeming with life.

 

*Habitat type 3170 in the Habitats Directive n° 3170.

 

Find out more:

Bigot L. 1999 Sur la réponse de Damasonium polyspermum Cosson (Alismataceae) aux variations des conditions édaphoclimatiques, d'après un suivi de 43 ans (1954-1996) dans une mare temporaire de la Tour-du- Valat (Camargue, Bouches-du-Rhône, France). Bull Soc Linn Provence 50 : 83-88 (in French)

formato A5, schizzo a china con pennino e pennello , dalla bella fotografia di Fabio Prosperi

A still from the video I posted recently. RAW to render. No processing. This one struck me as some kind of sea creature. But it's just ice.

00807947

Machines-outils à la Fosse Arenberg à Wallers dans les Hauts-de-France

The Racetrack is a playa--a dry lakebed--best known for its strange moving rocks. Located in a remote area of California's Death Valley National Park, the heavy stones appear to move across the dried lake bed known as Racetrack Playa, leaving a trail behind them in the cracked mud.

 

In years past, the apparent movement was blamed on everything from space aliens and magnetic fields to pranksters. But until recently no one had actually seen the rocks move, which only added to the mystery.

 

As noted on the National Park Service website, the mystery was finally solved in 2014 when in a paper published in the August 27, PLOS ONE, a team led by Scripps Institution of Oceanography, UC San Diego, paleobiologist Richard Norris reported on first-hand observations of the phenomenon. Because the stones can sit for a decade or more without moving, the researchers did not originally expect to see motion in person. Instead, they decided to monitor the rocks remotely by installing a high-resolution weather station capable of measuring gusts to 1 second intervals and fitting 15 rocks with custom-built, motion-activated GPS units. The experiment was set up in Winter 2011 with permission of the National Park Service. Then –in what Ralph Lorenz of the Applied Physics Laboratory at the Johns Hopkins University, one of the paper's authors, suspected would be "the most boring experiment ever" –they waited for something to happen.

 

But in December 2013, Norris and co-author James Norris (of Interwoof and Richard's cousin) arrived in Death Valley to discover that the playa was covered with a shallow pond no more than seven centimeters (three inches) deep. Shortly after, the rocks began moving.

 

Their observations show that moving the rocks requires a rare combination of events. First, the playa fills with water, which must be deep enough to allow formation of floating ice during cold winter nights but shallow enough to expose the rocks. As nighttime temperatures plummet, the pond freezes to form sheets of "windowpane" ice, which must be thin enough to move freely but thick enough to maintain strength. On sunny days, the ice begins to melt and break up into large floating panels, which light winds drive across the playa pool. The ice sheets shove rocks in front of them and the moving stones leave trails in the soft mud bed below the pool surface.

 

I don't know...I am still going with the space alien theory!

line drawing art form color content print

Taken this very evening at a fantastic Christmas market that I visited with friends. We bought beautiful handmade gifts & some yummy Indian food to take back to eat at their house; my first time trying dosa. For Saturday Self Challenge theme “light”.

  

76/100 : My 100x photos this year will all feature benches or chairs.

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