View allAll Photos Tagged fee
12 septembre 2014, Ca' Marcantonio.
—MN1561 © alain-michel boley 2014
————————
The Website | Second Flickr | The Blog | Facing Beauty
—————————
© alain-michel boley 2014 | All rights reserved
My images are not to be used, copied, edited, or blogged without my written permission.
"The University Church of St Mary the Virgin (St Mary's or SMV for short) is an Oxford church situated on the north side of the High Street. It is the centre from which the University of Oxford grew and its parish consists almost exclusively of university and college buildings.
St Mary's possesses an eccentric baroque porch, designed by Nicholas Stone, facing High Street, and a spire which is claimed by some church historians to be one of the most beautiful in England. Radcliffe Square lies to the north and to the east is Catte Street. The 13th-century tower is open to the public for a fee and provides good views across the heart of the historic university city, especially Radcliffe Square, the Radcliffe Camera, Brasenose College, Oxford and All Souls College.
Oxford is a university city in Oxfordshire, England, with a population of 155,000. It is 56 miles (90 km) northwest of London, 64 miles (103 km) from Birmingham and 24 miles (39 km) from Reading by road.
The city is home to the University of Oxford, the oldest in the English-speaking world, and has buildings in every style of English architecture from late Anglo-Saxon. Oxford's industries include motor manufacturing, education, publishing, information technology and science." - info from Wikipedia.
Summer 2019 I did a solo cycling tour across Europe through 12 countries over the course of 3 months. I began my adventure in Edinburgh, Scotland and finished in Florence, Italy cycling 8,816 km. During my trip I took 47,000 photos.
Now on Instagram.
PERFORMANCE IN RED.
Continuo a postare le immagini scattate in occasione del concerto che i Tubes hanno fatto ad Udine nel lontano 1981.
Si tratta di diapositive riversate in digitale e mi soddisfano due cose.....la mia posizione scelta proprio sotto il palco e l'ottima qualità di conservazione delle dia nonostante il tempo trascorso.
-------------------------------------------------------
PERFORMANCE IN RED.
I continue to post the images taken on the occasion of the concert that the Tubes did in Udine way back in 1981.
These are digitally transferred slides and two things satisfy me..... my chosen position right under the stage and the excellent quality of conservation of the slides despite the time that has passed.
Riversamento da dia a digitale
books, photo's, calendars, oracle cards and postcards available at my website: geertweggen.com/
If you like my work and want to support me and the squirrels on Patreon with daily photos, videos, e-books, educational work, coupons etc. for a small monthly fee. www.patreon.com/geertweggen?fan_landing=true
A beach is a geological landform along the shoreline of an ocean, sea. It usually consists of loose particles which are often composed of rock, such as sand, gravel, shingle, pebbles or cobblestones. The particles of which the beach is composed can sometimes instead primarily be of biological origins, such as whole or fragmentary mollusc shells or fragments of coralline algae.
Wild beaches are beaches which do not have lifeguards or trappings of modernity nearby, such as resorts and hotels. They are sometimes called undeclared, undeveloped or undiscovered beaches. Wild beaches can be valued for their untouched beauty and preserved nature. They are most commonly found in less developed areas including, for example, parts of Puerto Rico, Thailand, the Philippines, and Indonesia.
Beaches often occur along coastal areas where wave or current action deposits and reworks sediments.
Although the seashore is most commonly associated with the word beach, beaches are found by lakes and alongside large rivers, as well as by the sea or oceans.
Beach may refer to:
small systems where rock material moves onshore, offshore, or alongshore by the forces of waves and currents; or geological units of considerable size.
The former are described in detail below; the larger geological units are discussed elsewhere under bars.
There are several conspicuous parts to a beach which relate to the processes that form and shape it. The part mostly above water (depending upon tide), and more or less actively influenced by the waves at some point in the tide, is termed the beach berm. The berm is the deposit of material comprising the active shoreline. The berm has a crest (top) and a face — the latter being the slope leading down towards the water from the crest. At the very bottom of the face, there may be a trough, and further seaward one or more long shore bars: slightly raised, underwater embankments formed where the waves first start to break.
The sand deposit may extend well inland from the berm crest, where there may be evidence of one or more older crests (the storm beach) resulting from very large storm waves and beyond the influence of the normal waves. At some point the influence of the waves (even storm waves) on the material comprising the beach stops, and if the particles are small enough (sand size or smaller) , winds shape the feature. Where wind is the force distributing the grains inland, the deposit behind the beach becomes a dune.
These geomorphic features compose what is called the beach profile. The beach profile changes seasonally due to the change in wave energy experienced during summer and winter months. The beach profile is higher during the summer due to the gentle wave action during this season. The lower energy waves deposit sediment on the beach berm and dune, adding to the beach profile. Conversely, the beach profile is lower in the winter due to the increased wave energy associated with storms. Higher energy waves erode sediment from the beach berm and dune, and deposit it off shore, forming longshore bars. The removal of sediment from the beach berm and dune decreases the beach profile.
The line between beach and dune is difficult to define in the field. Over any significant period of time, sand is always being exchanged between them. The drift line (the high point of material deposited by waves) is one potential demarcation. This would be the point at which significant wind movement of sand could occur, since the normal waves do not wet the sand beyond this area. However, the drift line is likely to move inland under assault by storm waves.
Beach formation
Beaches are the result of wave action by which waves or currents move sand or other loose sediments of which the beach is made as these particles are held in suspension. Alternatively, sand may be moved by saltation (a bouncing movement of large particles). Beach materials come from erosion of rocks offshore, as well as from headland erosion and slumping producing deposits of scree. Some of the whitest sand in the world, along Florida's Emerald Coast, comes from the erosion of quartz in the Appalachian Mountains. A coral reef offshore is a significant source of sand particles.
The shape of a beach depends on whether or not the waves are constructive or destructive, and whether the material is sand or shingle. Constructive waves move material up the beach while destructive waves move the material down the beach. On sandy beaches, the backwash of the waves removes material forming a gently sloping beach. On shingle beaches the swash is dissipated because the large particle size allows percolation, so the backwash is not very powerful, and the beach remains steep. Cusps and horns form where incoming waves divide, depositing sand as horns and scouring out sand to form cusps. This forms the uneven face on some sand shorelines.
There are several beaches which are claimed to be the "World's longest", including Cox's Bazar, Bangladesh (120 km unbroken), Praia do Cassino, Fraser Island beach, 90 Mile Beach in Australia and 90 Mile Beach in New Zealand (88 km), Troia-Sines Beach (63 km) in Portugal and Long Beach, Washington (which is about 40 km).
Beaches and recreation
Many beaches are very popular on warm sunny days. In the Victorian era, many popular beach resorts were equipped with bathing machines because even the all-covering beachwear of the period was considered immodest. This social standard still prevails in many Muslim countries. At the other end of the spectrum are topfree beaches and nude beaches where clothing is optional or not allowed. In most countries social norms are significantly different on a beach in hot weather, compared to adjacent areas where similar behaviour might not be tolerated and might even be prosecuted.
Usually beach wear consists of a bikini, short shorts, and beach sandals for women. For men it is usually swim trunks and beach sandals.
In more than thirty countries in Europe, South Africa, New Zealand, Canada, Costa Rica, South America and the Caribbean, the best recreational beaches are awarded Blue Flag status, based on such criteria as water quality and safety provision. Subsequent loss of this status can have a severe effect on tourism revenues.
Due to intense use by the expanding human population, beaches are often dumping grounds for waste and litter, necessitating the use of beach cleaners and other cleanup projects. More significantly, many beaches are a discharge zone for untreated sewage in most underdeveloped countries; even in developed countries beach closure is an occasional circumstance due to sanitary sewer overflow. In these cases of marine discharge, waterborne disease from fecal pathogens and contamination of certain marine species is a frequent outcome.
Beach tokens
"Beach tokens", a form of season pass admission ticket, may be required for entrance, for people and even pets. They are made of metal etc. durable material, to enable them to withstand swimming, so the bearer can just carry them around his neck or on his swimsuit. Goals may be:
-restricting to only community members
-user fees for lifeguards, clean up
Artificial beaches
Some beaches are artificial; they are either permanent or temporary (For examples see Monaco, Paris, Copenhagen, Rotterdam, Toronto, Hong Kong and Singapore).
The soothing qualities of a beach and the pleasant environment offered to the beachgoer are replicated in artificial beaches, such as "beach style" pools with zero-depth entry and wave pools that recreate the natural waves pounding upon a beach. In a zero-depth entry pool, the bottom surface slopes gradually from above water down to depth. Another approach involves so-called urban beaches, a form of public park becoming common in large cities. Urban beaches attempt to mimic natural beaches with fountains that imitate surf and mask city noises, and in some cases can be used as a play park.
Beach nourishment involves pumping sand onto beaches to improve their health. Beach nourishment is common for major beach cities around the world; however the beaches that have been nourished can still appear quite natural and often many visitors are unaware of the works undertaken to support the health of the beach. Such beaches are often not recognized (by consumers) as artificial.
A concept of IENCE has been devised to describe investment into the capacity of natural environments. IENCE is Investment to Enhance the Natural Capacity of the Environment and includes things like beach nourishment of natural beaches to enhance recreational enjoyment and snow machines that extend ski seasons for areas with an existing snow economy developed upon a natural snowy mountain. As the name implies IENCE is not quite mainstream natural science as its goal is to artificially invest into an environment's capacity to support anthropogenic economic activity. An artificial reef designed to enhance wave quality for surfing is another example of IENCE. The Surfrider Foundation has debated the merits of artificial reefs with members torn between their desire to support natural coastal environments and opportunities to enhance the quality of surfing waves. Similar debates surround Beach nourishment and Snow cannon in sensitive environments.
Beaches as habitat
A beach is an unstable environment which exposes plants and animals to changeable and potentially harsh conditions. Some small animals burrow into the sand and feed on material deposited by the waves. Crabs, insects and shorebirds feed on these beach dwellers. The endangered Piping Plover and some tern species rely on beaches for nesting. Sea turtles also lay their eggs on ocean beaches. Seagrasses and other beach plants grow on undisturbed areas of the beach and dunes.
Ocean beaches are habitats with organisms adapted to salt spray, tidal overwash, and shifting sands. Some of these organisms are found only on beaches. Examples of these beach organisms in the southeast US include plants like sea oats, sea rocket, beach elder, beach morning glory aka Ipomoea pes-caprae, and beach peanut, and animals such as mole crabs aka Hippoidea, coquina clams aka Donax, ghost crabs, and white beach tiger beetles.
Fee was a stray. He wandered into our yard as about a 4 month old pup one summer day in 1991. I had always figured someone dumped him because we did everything we could to find his people. But maybe I hoped we wouldn’t find them because when Lenore came home from work that day I greeted her with Fee (although he was unnamed) bundled up in my arms and I said, “look what came today, a little package,” then I paused…. “can we keep him?” From the beginning then he had the nickname “Little Package” and he kept it his entire life. We named him Fee Waybill, after the lead singer of the band “The Tubes.” He could sing, was a total showman, and a real character.
He was a fantastic dog, full of sass and personality. He liked Weasel and he was a pretty good puller. So now we had a very unlikely four-dog team.
On October 12, 2007 at nearly 17 years of age Fee walked away and we never saw him or any trace of him again. Although I looked and looked. I have not suffered from a lack of closure, his departure as much a mystery as his arrival and there are some things I don't need to, or perhaps am not meant to know.
There are a few more pics and words about him in his set.
www.facebook.com/DarylChapmanAutomotivePhotography
Purchase photos via PayMe / FPS
Large file, NO Watermark.
All photos INDIVIDUALLY edited with pride
**No monthly fees**
54,935,236 views!!!
German postcard by Ross Verlag, no. 3463/1, 1928-1929. Photo: Atelier Kiesel, Berlin.
Pretty Fee Malten (1911-2005) was a popular German film star in the late 1920s and early 1930s. She portrayed uncomplicated, gay girls in several silent and early sound films until her budding career was broken off by the rise of Adolph Hitler.