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Humber Gap
The Humber Gap is a term for the geographic gap between the roughly north–south running line of hills formed by the Yorkshire Wolds and the Lincolnshire Wolds, formed by the west–east running Humber Estuary. In the geological past the gap has formed part of an ice barrier due to glaciers during the ice age resulting in damming and formation of a 'Humber Lake', and also forms a geological division. In modern times the gap has formed a natural choice for transport routes, such as the railways. The Humber Bridge also crosses the Humber close to the gap. See also *Humberhead Levels: very heavily silted area formed west of the gap as a result of the damming of the gap, and subsequent lake formation *North Ferriby and South Ferriby South Ferriby is a village in North Lincolnshire, England. It is situated on the south bank of the Humber Estuary and west from the Humber Bridge. North Ferriby is directly opposite on the Estuary's north bank. Village population was 651 in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordnance Survey Quarter-inch Sheet 11 North Midlands And Yorkshire, Published 1964
Ordnance may refer to: Military and defense *Materiel in military logistics, including weapons, ammunition, vehicles, and maintenance tools and equipment. **The military branch responsible for supplying and developing these items, e.g., the United States Army Ordnance Corps *Artillery, often in a formal name, e.g., "Ordnance Survey". *Artillery Shell (projectile), shells, specifically unexploded ordnance. *Aircraft ordnance, weapons carried by and used by an aircraft. Places *Ordnance, Oregon, a former community near the Umatilla Chemical Depot *Ordnance Island, formerly a Royal Army Ordnance Corps Supply depot, depot, in St. George's, Bermuda, St. George's Town, Bermuda Maps-related *Ordnance datum (from use in ballistics), a vertical datum used as the basis for deriving altitudes on maps *Ordnance Survey, the national mapping agency for Great Britain See also *Ordnance Corps (other) {{disambiguation, geo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yorkshire Wolds
The Yorkshire Wolds are low hills in the counties of the East Riding of Yorkshire and North Yorkshire in north-eastern England. The name also applies to the district in which the hills lie. On the western edge, the Wolds rise to an escarpment which then drops sharply to the Vale of York. The highest point on the escarpment is Bishop Wilton Wold (also known as Garrowby Hill), which is above sea level. To the north, on the other side of the Vale of Pickering, lie the North York Moors, and to the east the hills flatten into the plain of Holderness. The largest town in the Wolds is Driffield, with other places including Pocklington, Thixendale and Kilham, the original 'capital' of the Wolds. The highest village on the Yorkshire Wolds is Fridaythorpe at above sea level. The market town of Beverley lies on the eastern slopes, along with the civil parish of Molescroft. Geology The hills are formed from a series of pure marine limestones formed during the Cretaceous period, kno ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lincolnshire Wolds
The Lincolnshire Wolds are a range of low hills in the county of Lincolnshire, England which run roughly parallel with the North Sea coast, from the Humber Estuary in the north-west to the edge of the Lincolnshire Fens in the south-east. They are a designated Area of Outstanding Natural Beauty (AONB), and the highest area of land in eastern England between Yorkshire and Kent.Ordnance Survey maps: Geology The Wolds are formed largely from a series of pure marine limestones formed during the Cretaceous period, known collectively as the Chalk Group. The chalk overlies a series of other sedimentary strata of late Jurassic/early Cretaceous age. The strata dip gently to the east and form a scarp which runs southeast from Barton upon Humber via Caistor before it loses its identity north of Spilsby. To the north of the Humber Gap, the same formations continue as the Yorkshire Wolds. The rock succession in stratigraphic order i.e. youngest/uppermost first, is this: *White Chalk Subgro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humber Estuary
The Humber is a large tidal estuary on the east coast of Northern England. It is formed at Trent Falls, Faxfleet, by the confluence of the tidal rivers Ouse and Trent. From there to the North Sea, it forms part of the boundary between the East Riding of Yorkshire on the north bank and North Lincolnshire on the south bank. Although the Humber is an estuary from the point at which it is formed, many maps show it as the River Humber. Below Trent Falls, the Humber passes the junction with the Market Weighton Canal on the north shore, the confluence of the River Ancholme on the south shore; between North Ferriby and South Ferriby and under the Humber Bridge; between Barton-upon-Humber on the south bank and Kingston upon Hull on the north bank (where the River Hull joins), then meets the North Sea between Cleethorpes on the Lincolnshire side and the long and thin headland of Spurn Head to the north. Ports on the Humber include the Port of Hull, the Port of Grimsby and the Port ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humberhead Levels
The Humberhead Levels is a national character area covering a large expanse of flat, low-lying land towards the western end of the Humber estuary in northern England. The levels occupy the former Glacial Lake Humber, an area bounded to the east by the Yorkshire Wolds and the northern Lincolnshire Edge, a limestone escarpment, and to the west by the southern part of the Yorkshire magnesian limestone ridge. In the north the levels merge into the slightly more undulating Vale of York close to the Escrick glacial moraine, and to the south merge into the Trent Vale. Glacial Lake Humber During the last ice age, a glacier extended across this area almost to where Doncaster now is. The main glacial front was at Escrick where the Escrick moraine marks its furthest extension. This was the northern limit of an extensive lake which was impounded by the blocking of the Humber Gap by another ice front. The lake bottom gradually filled with clay sediments which are up to 20 metres thick. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Ferriby
North Ferriby is a village and civil parish in the Haltemprice area of the East Riding of Yorkshire, England. History Humber Estuary "The archaeology of the intertidal wetlands of the Humber Estuary is of international importance, and includes prehistoric boats, trackways, fishtraps and platforms, Roman settlements and ports and Post-Medieval fishweirs." The foreshore of North Ferriby, within the Humber Estuary, is the site of the earliest sewn plank boats known outside Egypt. In 1931, wooden planks belonging to an ancient boat were discovered by local man Ted Wright on the shore of the Humber. Two further boats have since been discovered. Estimates using radiocarbon dating have placed the origin of the boats to the Bronze Age, between 2030 and 1680 BC. The Ferriby Boats are the earliest known boats found in Europe. In addition, Bronze Age round barrows were found near North Ferriby by archaeologists excavating the land on which the A63 junction was built. There was als ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Ferriby
South Ferriby is a village in North Lincolnshire, England. It is situated on the south bank of the Humber Estuary and west from the Humber Bridge. North Ferriby is directly opposite on the Estuary's north bank. Village population was 651 in 2011. History South Ferriby dates back at least to Roman times when there was a major settlement. It is known locally as one of the 'Low Villages' at the bottom of a chalk escarpment, where the chalk meets the clay to give, before piped water, (the village was one of the first to have piped water with houses plumbing into the supply which was put down to supply steam ships) to the a plentiful water supply. It also marks the point where the Lincolnshire Wolds meet the Humber Estuary and was, as the name suggests, the southern end of an ancient ferry over the Humber to North Ferriby. The entry in the ''Domesday Book'' of 1086 records a church, a mill and two ferries. To sustain two ferries suggests that a prosperous trading community must h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of The East Riding Of Yorkshire
Geography (from Greek: , ''geographia''. Combination of Greek words ‘Geo’ (The Earth) and ‘Graphien’ (to describe), literally "earth description") is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of Earth. The first recorded use of the word γεωγραφία was as a title of a book by Greek scholar Eratosthenes (276–194 BC). Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be. While geography is specific to Earth, many concepts can be applied more broadly to other celestial bodies in the field of planetary science. One such concept, the first law of geography, proposed by Waldo Tobler, is "everything is related to everything else, but near things are more related than distant things." Geography has been called "the world discipline" and "the bridge between the human and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Lincolnshire
The ceremonial county of Lincolnshire (composed of the shire county of Lincolnshire, plus the unitary authorities of North Lincolnshire and North-East Lincolnshire) is the second largest of the English counties and one that is predominantly agricultural in character. Despite its relatively large physical area, it has a comparatively small population (of less than 1 million people). The unusually low population density that arises gives the county a very different character from the much more densely populated an urbanised counties of south-east and northern England, and is, in many ways, key to understanding the nature of the county (and perhaps even its people). Classification For the purposed of a general geographical classification the county can be broken down into a number of sub-regions: *The Lincolnshire coast. *Lincolnshire Fens: a region of flat, marshy land (much of it reclaimed from the sea) that predominates in the southern and south-eastern areas of the county (most ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humber
The Humber is a large tidal estuary on the east coast of Northern England. It is formed at Trent Falls, Faxfleet, by the confluence of the tidal rivers Ouse and Trent. From there to the North Sea, it forms part of the boundary between the East Riding of Yorkshire on the north bank and North Lincolnshire on the south bank. Although the Humber is an estuary from the point at which it is formed, many maps show it as the River Humber. Below Trent Falls, the Humber passes the junction with the Market Weighton Canal on the north shore, the confluence of the River Ancholme on the south shore; between North Ferriby and South Ferriby and under the Humber Bridge; between Barton-upon-Humber on the south bank and Kingston upon Hull on the north bank (where the River Hull joins), then meets the North Sea between Cleethorpes on the Lincolnshire side and the long and thin headland of Spurn Head to the north. Ports on the Humber include the Port of Hull, the Port of Grimsby and the P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Apr2006.jpg "Click for more on -> Yorkshire Wolds")
