The streets of the city centre were filled with the intoxicating smells of international foods in May and now the traders will be coming back next month. But those who fancy a Greek gyros, a Spanish paella or a pad Thai meal can rejoice with the prospect of an even bigger line-up to tempt the taste buds. A continental market in Stoke. The event will be from 10am to 6pm Wednesday to Saturday October 3 to 6, and set in the heart of the city centre on Eastgate Street. Read More This is how much a shopping basket will cost at Tesco’s new Jack’s store compared with Aldi and Lidl A wide array of products will be on offer, from unusual craft items, to food traders offering the best hot and cold produce from their native countries. Expect the area to be brought to life with the sights, sounds and smells of the continent and beyond. The event is operated by RR Events, a Liverpool-based Event Management company specialising in special event and themed markets. Jason Smith, chief executive at Marketing Gloucester , said: Like us on Facebook.
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Card Member must travel on itinerary booked to be eligible for benefits described. Noon check-in and room upgrade are based on availability and are provided at check-in. Breakfast amenity varies by property, but will be, at a minimum, a continental breakfast. In this instance, complimentary Wi-Fi will be provided in a common space on property.
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Most of the time, the tin will not have a date marked anywhere on it, and that’s where some detective work on your part is required. Dating tins isn’t difficult to do, though it may involve some of your time. This process can turn out to be both fun and personally rewarding. The following information can be used to help document the age of your tins.
You will be fortunate to date your tin right away, most of them will require you to carefully study their appearance both from a structure stand-point and how they are decorated or finished. Some very obvious clues may not be sufficient, may be misleading, or have to be combined with other knowns to arrive at an accurate or close approximate date. Let’s start off with some general things that apply to most 20th century tins and to some 19th.
Addresses on tins can often be linked to a time period, even down to the exact year, if you use an old city directory or telephone book. By looking up the business in the directory you can determine when they moved to a new location or the address simply changed because of changes in the city’s addressing system. By tying in certain company events and changes, the graphics and text on your tin may be able to determine the time period it was introduced and used.
Many companies have gone through name changes ownership, brands, logos, trademarks, mergers because of growth or merging. Knowing when these events took place and matching them to the name on the tin can help. Other point-of-sale POS advertising, particularly die-cut cardboard, may also provide dates. Another source of information could be a merchandise catalog.
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See Article History Dating, in geology , determining a chronology or calendar of events in the history of Earth , using to a large degree the evidence of organic evolution in the sedimentary rocks accumulated through geologic time in marine and continental environments. To date past events, processes, formations, and fossil organisms, geologists employ a variety of techniques. These include some that establish a relative chronology in which occurrences can be placed in the correct sequence relative to one another or to some known succession of events.
Radiometric dating and certain other approaches are used to provide absolute chronologies in terms of years before the present. The two approaches are often complementary, as when a sequence of occurrences in one context can be correlated with an absolute chronlogy elsewhere. Ankyman General considerations Distinctions between relative-age and absolute-age measurements Local relationships on a single outcrop or archaeological site can often be interpreted to deduce the sequence in which the materials were assembled.
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Continental Drift, Sea Floor Spreading and Plate Tectonics Plate Tectonics is a theory developed in the late s, to explain how the outer layers of the Earth move and deform. The theory has caused a revolution in the way we think about the Earth. Since the development of the theory, geologists have had to reexamine almost every aspect of Geology.
Plate tectonics has proven to be so useful that it can predict geologic events and explain almost all aspects of what we see on the Earth. Tectonic Theories Tectonic theories attempt to explain why mountains, earthquakes, and volcanoes occur where they do, the ages of deformational events, and the ages and shapes of continents and ocean basins. Late 19th Century Theories Contraction of the Earth due to cooling.
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These include the breadth of the territorial sea; the seaward limits of the contiguous zone, the exclusive economic zone and, in some cases, the continental shelf. The territorial sea baseline may be of various types depending upon the shape of the coastline in any given locality: The Normal baseline corresponds with the low water line along the coast, including the coasts of islands. Under the Convention, normal baseline can be drawn around low tide elevations which are defined as naturally formed areas of land surrounded by and above water at low tide but submerged at high tide, provided they are wholly or partly within 12 nautical miles of the coast.
Straight baselines are a system of straight lines joining specified or discrete points on the low-water line, usually known as straight baseline end points. These may be used in localities where the coastline is deeply indented and cut into, or where there is a fringe of islands along the coast in its immediate vicinity. Bay or river closing lines are straight lines drawn between the respective low-water marks of the natural entrance points of bays or rivers.
Waters on the landward side of the baseline are internal waters for the purposes of international law.
Chronology and dating As most genealogists know, dating conventions in English documents can cause problems even as late as the 18th century. These problems can become quite complicated in medieval documents. For example, medieval charters are commonly dated by specifying the week day, a nearby religious feast day, and the year of the monarch’s reign – a convention which clearly has little in common with the modern system of day, month and calendar year.
Although the process of dating medieval documents can seem off-putting, fortunately most of the necessary resources are available on the internet.
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The head tubes look as if they were fillet brazed , but they weren’t. The head tube and the tapered segments that lead into the the top tube and down tube were actually made from two special forgings that were “electro-forged” welded together down the centerline, then ground smooth, so the seam is not usually visible. There are necked-down parts that fit into the top tube and down tube, like internal lugs.
Muller has a very detailed explanation of this process, in his superb article: Inside the Varsity , which is now on this site. Mike Rother has an excellent overview of the fillet-brazed lightweights , also on this site. The flat-bladed forks were also forged. The Typhoon probably dates from the late ’50’s or ’60’s.
If I recall, it was what Schwinn called a ” cantilever ” frame, where the seat stays pass by the seat cluster and continue on in a graceful curve to join the bottom of the head tube. Older Schwinn ” cruisers “, such as the Excelsior that was the inspiration of the first mountain bikes, used a straight lower top tube from the bottom of the head tube to the seat tube.
They also manufactured their own rims in the Chicago factory, the “Schwinn Tubular Rim”. These rims, like the Chicago frames, were among the sturdiest ever built.
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Set forth in by Alfred Wegener, a geophysicist and meteorologist, continental drift also explained why look-alike animal and plant fossils, and similar rock formations, are found on different continents. The theory of continental drift Wegener thought all the continents were once joined together in an “Urkontinent” before breaking up and drifting to their current positions.
But geologists soundly denounced Wegener’s theory of continental drift after he published the details in a book called ” The Origin of Continents and Oceans. Though most of Wegener’s observations about fossils and rocks were correct, he was outlandishly wrong on a couple of key points. For instance, Wegener thought the continents might have plowed through the ocean crust like icebreakers smashing through ice. Although Wegener’s “continental drift” theory was discarded, it did introduce the idea of moving continents to geoscience.
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Coinage in western continental Europe , Africa , and the Byzantine Empire The fall of Roman power in the West left the gold currency of the Byzantine Empire undisturbed; it was to become the most dominant single influence in European coinage for 1, years, competing at first with the gold of the Arab caliphates and later with that of the great Italian commercial republics as well.
Byzantine coinage, in its continuity , contrasted strongly with the often erratic monetary systems from the 5th to the 7th century in western Europe, where Germanic invaders inherited the apparatus, money included, of the Roman Empire. In general, they took over the main features of late Roman coinage. The types of the gold coins for some time reflected Byzantine prestige , showing a formalized portrait obverse and titles of the reigning Byzantine emperor, toward whom widespread respect was paid even when Western kings began to add their personal monograms to the normal Victory reverses.
Imperial prerogative , so powerful an influence on western gold, had less effect on silver, the types of which in the West became more flexible; in bronze, where obvious efforts were at times made to link with traditional Roman design, flexibility was greater still. In technique these coinages varied widely: