Gowdall, ENG - Postcode - DN14 0AQ - Post Codes & Zip Codes List
|City/County/District||East Riding of Yorkshire|
|States or Territories||England|
|States or Territories Abbrieviation||ENG|
MAPS & LOCATION
East Riding of Yorkshire
Located in the ceremonial county of Yorkshire and the unitary authority area of Yorkshire and the Humber, East Riding of Yorkshire (or simply East Riding or East Yorkshire) is a part of England. North Yorkshire and South Yorkshire are to its north and west, and Lincolnshire is to its south.
Bridlington, Hornsea, and Withernsea are all prominent seaside resorts; Howden is home to the historic Howden Minster; Market Weighton, Pocklington, Brough, Hedon, and Driffield have regular markets; and Hessle and Goole serve as the county's two major ports. Kingston upon Hull is a major hub for trade, transportation, and tourism, and it also serves as a major port for cargo shipping around the world. After the former County of Humberside was abolished in 1996, the present-day East Riding of Yorkshire was formed. Beverley, a historical marketplace, is where county government is located. Yorkshire Wolds is primarily rural, with a smattering of tiny towns and villages dotting the landscape. Kingston upon Hull, Beverley, Bridlington, and Goole are all significant cities in the area. There were 334,179 people living there as of the 2011 census in the United Kingdom.
The name comes from the fact that it is the most easterly of the three traditional administrative divisions (known as Thrydings or Ridings) of the historic county of Yorkshire. Historical cultural and legal practices recognized the East Riding, North Riding, and West Riding as three distinct areas delineated by their respective boundaries. Due to its enormous size, the county of Yorkshire was divided into three administrative county councils in 1889 under the provisions of the Local Government Act of 1888. These councils followed the ancient boundaries of the county's three Ridings. For eighty-six years, until new administrative tiers were put in place, the East Riding County Council served as the area's administrative local government and ceremonial county (Lieutenancy) area (with its seat in Beverley).
This was followed by a reclassification of the region's political status. In spite of their similarities in name, the boundaries of the successor local council regions are not the same. Although the current ceremonial area and the current local government administrative area councils cover more territory than the traditional geographic and historic cultural East Riding of Yorkshire, the latter does not include the entire region.
The scenery consists of the low chalk hills of the Yorkshire Wolds in the center, with the low-lying fertile plains of Holderness and the Vale of York on each side. It is bounded to the south by the Humber Estuary and to the east by the North Sea. Since the last ice age, archaeologists have uncovered artifacts and buildings from every era in human history. There are no major cities or manufacturing hubs in the area. Beverley, a historical marketplace and religious center, serves as the region's administrative center. The predominant faith in the region is Christianity, and there is a larger-than-average elderly population
The Riding's historic buildings, natural reserves, and the Yorkshire Wolds Way long-distance footpath all attract tourists, and the economy is largely focused on agriculture and tourism. High amounts of renewable energy generation can be attributed in large part to the region's open, coastal nature and lack of significant urbanization.
There is a college for agriculture at Bishop Burton, and the only university in the area is in Hull. A15 connects Hessle and Barton-upon-Humber in North Lincolnshire across the Humber Bridge in the county's southern border region, close to Hull.
The East Riding region can be roughly divided into three geological zones. The Humberhead Levels to the south and the eastern portion of the Vale of York make up the western region. There is a band of sandstones here, overlain by glacial and lake deposits that were left over after the end of the last ice age. The middle section consists of the Yorkshire Wolds, a chalk formation that stretches from North Ferriby on the Humber to Flamborough Head on the coast. The low-lying Holderness coastal plain is located in the southeast of the district; it faces east toward the North Sea and drains south into the Humber Estuary. Several beaches may be found at Bridlington, which is located to the south of Flamborough Head, and the Spurn peninsula can be found to the district's extreme southeast.
East of the Yorkshire Wolds, where traces of beaches were unearthed, was the area's coast before the last ice age. After the North Sea ice sheet retreated, it left behind a massive boulder clay deposit, which eventually turned into the damp and swampy plain of Holderness. Simultaneously, an ice sheet in the Vale of York withdrew, leaving behind heavy glacial deposits and two notable moraines to the west of the Wolds. The marshes in the Vale of York were formed in part by the deposits from this area. In and of themselves, the Wolds were mostly ice-free, well-drained, chalk uplands. As the ice withdrew, tundra conditions gradually gave way to vegetation that could support grazing species. Due to the fact that a lot of water was still frozen in the northern ice sheets, sea level was significantly lower than it is today, and a land mass extended eastward to the low countries.
The East Riding features moderate winters and mild summers. The climate changes from day to day and season to season. Winds from the west, together with any accompanying depressions and fronts, can cause blustery conditions throughout the winter months due to the area's latitude. There are typically brief intervals of good weather brought on by small, mobile anticyclones in between depressions. Anticyclones are the cause of the chilly, dry weather that characterizes winter. Drought is a real possibility on the Wolds in the summer due to the anticyclones' dry steady weather. The Gulf Stream in the northern Atlantic Ocean provides unusually mild winters and cold summers at this latitude. Depending on the time of day and the season, the air might feel very different. Nighttime lows are often cooler, and January is consistently the year's chilliest month. The Pennines give protection from the most severe of the wet, westward winds, and the closeness to the North Sea also plays a significant role in shaping the local climate.
There aren't other cities in the area as sizable as Hull, so most of the region is rural. Beverley, Driffield, Goole, Market Weighton, and Pocklington are some of the market towns in the area, while Bridlington, Hornsea, and Withernsea are some of the coastal towns. Parts of the district, like Hessle in the south, are outside of Hull itself but yet within the city's greater metropolitan region. In general, the number of enterprises per square mile is higher in rural areas than in urban ones, which is indicative of the prevalence of agricultural businesses and small firms in the rural sector. Despite a 40% decline between 1997 and 2003, 20% of all VAT-registered enterprises in the East Riding are in agricultural and allied sectors.  The coastal town of Easington is home to four separate gas terminals run by BP and Centrica, as well as the natural gas terminal Easington Gas Terminal utilized by the Langeled pipeline.
England, UK Description
England is the UK's largest constituent unit, occupying more than half of the island. Despite its political, economic, and cultural legacy, England is no longer a governmental or political unit.
With its rich soil and crisscrossing network of rivers and streams, England has been and remains a thriving agricultural economy. England became the epicenter of the global Industrial Revolution in the early 1800s, quickly rising to the top of the global industrialization rankings. Manufacturing industries in Manchester, Birmingham, and Liverpool turned raw materials into finished goods for export. London, the country's capital, became one of the world's most important cities, a hub for a global political economy. The London metropolitan area continues to be Europe's financial center and a hotbed of innovation, particularly in the fields of popular culture.
One of the most fundamental features of the English language is its diversity within a limited compass. Even England's most remote regions are accessible by car or train within a day's drive or train ride of London. Many English people identify with the regions or shires from which they are descended—for example, Yorkshire, the West Country, or the Midlands—and maintain strong ties to those regions even if they live in other parts of the country. Some differences exist, but many more, especially as England transitioned from a rural to an urban society, began to fade after 1945. The country's island location has shaped the English character, which values social harmony, social harmony, and good manners that ensure orderly relations in a densely populated landscape, among other characteristics.
During the dismantling of Britain's vast overseas empire in the mid-20th century, England suffered an identity crisis, and much attention has been paid to discussions of "Englishness"—that is, what it means to be English in a country that now has large immigrant populations from many former colonies and is far more cosmopolitan than insular. Although influenced by other cultures, English culture is distinct and difficult to define. The Lion and the Unicorn by George Orwell, a self-described "revolutionary patriot" who chronicled politics and society in the 1930s and 1940s, makes this observation.
Geographical Description of England
Except for Yorkshire and Nottinghamshire in the east, England's topography is low-lying but rarely flat. The area has many rolling hillsides, with the highest elevations in the north, north-west, and southwest. Intricate underlying structures have resulted in intricate patterns in the landscape. The oldest sedimentary rocks and some igneous rocks (found in isolated granite hills) are found in Cornwall and Devon, while the most recent alluvial soils are found in the Fens of Cambridgeshire, Lincolnshire, and Norfolk. Both the sandstone and limestone bands that separate these two regions date from prehistoric times when large sections of central and southern England were submerged under warm seas. Geological forces lifted and folded some of these rocks, forming northern England's spine. Scafell Pike, England's highest point, stands at 3,210 feet (978 metres) and is part of the world's highest mountain range. The northern mountains are mostly slate, while the southern mountains are mostly lava flows. Mountain ranges have developed from the North Downs at 965 feet (294 meters) to the Cotswolds at 1,083 feet (330 meters).
The Chiltern Hills, North Yorkshire Moors, Yorkshire and Lincolnshire Wolds, and Yorkshire and Lincolnshire Wolds were rounded into distinctive plateaus with west-facing escarpments during the Pleistocene Epoch (about 2,600,000 to 11,700 years ago). A land bridge connecting Britain to the rest of Europe was engulfed as the last glacial sheet melted. The retreating glaciers left behind gravel, sand, and glacial mud, further altering the land surface. Rain, rivers, and tides, as well as subsidence, have shaped the hills and coastline of eastern England. Limestone, gritstone, and carboniferous strata plateaus are associated with major coalfields, some visible as surface outcrops.
A great example of England's geologic complexity is its cliff structure. The chalk cliffs of Dover are made up of a series of sedimentary rocks of varying ages that start at Land's End in the far southwest and end at the Isle of Wight. The English coastline is dotted with cliffs, bays, and river estuaries that add to the overall beauty of the landscape.
England's weather is as varied as its topography. The average temperature in England, like other temperate maritime zones, is moderate, ranging from around 35 degrees Fahrenheit (2 degrees Celsius) in January to 72 degrees Fahrenheit (22 degrees Celsius) in July in the Thames river valley (32 degrees Celsius). Tacitus, the Roman historian, described it as "unpleasant" with "frequent rains and mists but no extreme cold." However, the higher elevations of England receive snow for roughly 50 days out of the year. In fact, the northwest and southwest of England are particularly "wet". These areas receive less than 30 inches (750 mm) of rain per year and are frequently subject to severe drought. Rainfall averages only 20 inches in parts of the southeast (500 mm). The weather has influenced English art and literature not only seasonally but also day-to-day and even hour-to-hour. The bumbershoot's moniker as the stereotypical English gentleman's walking stick is not accidental.
The Economy of England
In the 18th and 19th centuries, England's economy was primarily agricultural until the Industrial Revolution transformed it into a highly urbanized and industrialized region as a result of the Industrial Revolution. A result of the close proximity of coal and iron ore deposits, heavy industries (iron and steel, textiles, and shipbuilding) sprang up in the north-eastern counties, and they continue to thrive today. During the 1930s, the Great Depression and foreign competition both contributed to a decline in manufactured goods production and an increase in unemployment in the industrial north, which contributed to the Great Depression. Residents of these northern counties who were out of work were forced to relocate south to London and its environs. Because of urbanization and industrialization, the southeast has become dominated by industries such as automotive, chemical, electrical, and machine tool manufacturing. Despite the fact that population growth and urbanization significantly reduced farmland in England during the twentieth century, the geographical counties of Cornwall, Devon, Kent, Lincolnshire, Somerset, and North Yorkshire have retained a significant proportion of their agricultural land.
Another period of industrial decline occurred in the late twentieth century, during which coal mining was virtually phased out and job losses in industries such as iron and steel production, shipbuilding, and textile manufacturing were particularly severe. The decline of these industries had a disproportionately negative impact on the economies of the north and the Midlands, while the economies of the south remained relatively prosperous. By the turn of the twenty-first century, the service sector had taken over as the dominant sector of the English economy, with banking and other financial services, retail, distribution, media and entertainment, education, health care, and hotels and restaurants among the leading sectors.