Staithes Viaduct, WR
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Staithes Viaduct, WR
Staithes is a seaside village in the borough of Scarborough in North Yorkshire, England. Easington and Roxby Becks, two brooks that run into Staithes Beck, form the border between the Borough of Scarborough and Redcar and Cleveland. The area located on the Redcar and Cleveland side is called Cowbar. Formerly one of the many fishing centres in England, Staithes is now largely a tourist destination within the North York Moors National Park. History The name Staithes derives from Old English and means 'landing-place'. It has been suggested that it is so named after being the port for the nearby Seaton Hall and Hinderwell. The spelling ''Steeas'' is sometimes used to indicate the traditional local dialect pronunciation . At the turn of the 20th century, there were 80 full-time fishing boats putting out from Staithes. A hundred years later there are still a few part-time fisher men. There is a long tradition of using the coble (a traditional fishing vessel) in Staithes. Staithes ...
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Coble
The coble is a type of open traditional fishing boat which developed on the North East coast of England. The southernmost examples occur around Hull (although Cooke drew examples at Yarmouth, see his ''Shipping and Craft'' series of drawings of 1829); the type extends to Burnmouth just across the Scottish border. The distinctive shape of the boat — flat-bottomed and high- bowed — arose to cope with the particular conditions prevalent in this area. Flat bottoms allowed launching from and landing upon shallow, sandy beaches; an advantage in this part of the coast where the wide bays and inlets provided little shelter from stormy weather. However, fishermen required high bows to sail in the dangerous North Sea and in particular to launch into the surf and to land on the beaches. The design contains relics of Norse influence, though in the main it shows Dutch origin. A Scottish version of the coble, much shallower and beamier than the English type, serves for salmon-fishing ...
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Cleveland Way
The Cleveland Way is a National Trail in the historic area of Cleveland in North Yorkshire, northern England. It runs between Helmsley and the Brigg at Filey, skirting the North York Moors National Park. History Development of the Cleveland Way began in the 1930s when the Teesside Ramblers' Association pressed for the creation of a long-distance path in the north-east of Yorkshire linking the Hambleton Drove Road, the Cleveland escarpment and footpaths on the Yorkshire coast. Subsequently, in 1953, a formal proposal to create the route was submitted to the North Riding of Yorkshire Council by the National Parks Commission. The trail was officially opened in 1969. It was the second official National Trail to be opened. Route The trail can be walked in either direction linking the trailheads of Helmsley () and Filey () in a horseshoe configuration. The trail is waymarked along its length using the standard National Trail acorn symbol. The trail falls into two roughly equa ...
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Bonnet (headgear)
Bonnet has been used as the name for a wide variety of headgear for both sexes—more often female—from the Middle Ages to the present. As with "hat" and "cap", it is impossible to generalize as to the styles for which the word has been used, but there is for both sexes a tendency to use the word for pop styles in soft material and lacking a brim, or at least one all the way round, rather than just at the front. Yet the term has also been used, for example, for steel helmets. This was from Scotland (in 1505), where the term has long been especially popular.''OED'', "Bonnet" Headgear tied under the chin with a string was especially likely to be called a bonnet. Other features associated with bonnets as opposed to hats was that the forehead was not covered, and the back of the head often was. The outdoor headgear of female servants and workers was more likely to be called a bonnet. It was often worn outside over a thinner everyday head covering, which was worn at all times. In ...
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Thornaby-on-Tees
Thornaby-on-Tees, commonly referred to as Thornaby, is a town and civil parish on the River Tees's southern bank. It is in the Borough of Stockton-on-Tees, North Yorkshire, England. The parish had a population of 24,741 at the 2011 census, in the Teesside built-up area. The town had a royal charter enacted to form a municipal borough in 1892, during the Victorian era, before merging into the County Borough of Teesside in 1968. A borough no longer defines a specific settlement's status as a town in England since the Local Government Act 1972 reforms. The modern centre was built on the north eastern part of Thornaby airfield and lies south-west of Stockton-on-Tees and south-west of Middlesbrough. History Prehistoric There are other signs of Thornaby being a much older settlement. Traces of prehistoric man have been found, the earliest being a stone axe, 8 inches long, dating back to the Mesolithic Period (about 3000 BC). In 1926, a dugout canoe said to date from ...
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A174 Road
The A174 is a major road in North Yorkshire, England. It runs from the A19 road at Thornaby-on-Tees, across South Teesside and down the Yorkshire Coast to Whitby. The A174 is the coastal route between Teesside and Whitby; the alternative road, the A171, is described as being the moorland route. Settlements on the route From West to east; *Thornaby-on-Tees *Coulby Newham *Tollesby * Marton *Ormesby * Normanby *Eston * Grangetown *Lazenby * Wilton *Yearby * Longbeck *New Marske *Skelton-in-Cleveland *North Skelton *Brotton *Carlin How * Loftus * Easington *Boulby *Hinderwell * Ellerby *Lythe *Sandsend *Whitby Route description The route starts at Thornaby Road with a junction on the A1044 road going eastwards towards the A19 road. This section was single carriageway, but it was upgraded as part of the long-term plans for the area. After the junction with the A19, the route cuts across South Teesside taking an east/west cut past Normanby, Ormesby and Eston to a junction with ...
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Whitby, Redcar And Middlesbrough Union Railway
The Whitby, Redcar and Middlesbrough Union Railway (WRMU), the Whitby–Loftus Line, was a railway line in North Yorkshire, England, built between 1871 and 1886, running from Loftus on the Yorkshire coast to the Esk at Whitby, and connecting Middlesbrough to Whitby along the coast. For much of its journey the line hugged the cliffs, and had a troubled build due to the proximity to the sea and poor quality of the construction on many of its original bridges and viaducts. The line was closed to passengers in May 1958, but the northern section to Boulby Potash Mine re-opened in the 1970s. History Background Whitby had been connected to the national rail system by the Whitby and Pickering Railway since the 1830s. Loftus was connected to the rail system by the 1870s via an extension of the Cleveland Railway: both the Cleveland Railway and the Middlesbrough and Guisborough Railway were constructed in the 1860s connecting Middlesbrough to Guisborough. Loftus to Whitby The ext ...
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Staithes Railway Station
Staithes railway station was a railway station on the Whitby Redcar and Middlesbrough Union Railway, serving the villages of Staithes and Dalehouse in North Yorkshire, England. It was opened on 3 December 1883. History The line through Staithes had proposals dating back to the late 1860s, but the station did not open until December 1883 after a protracted building process which saw the viaducts on the line strengthened, financial ruin of the contractor and a diversion through the cliffs between and . The station was north of railway station, and south of . The station was host to a LNER camping coach from 1935 to 1939 and may have had a coach visiting in 1934 and 1935. A coach was also positioned here by the North Eastern Region of British Railways from 1954 to 1958. A goods shed, steam crane and sidings were located on the west side of the station, with a south facing connection. The steam crane was capable of handling up to . Like other locations on the Yorkshire coast, ...
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Ammonite
Ammonoids are a group of extinct marine mollusc animals in the subclass Ammonoidea of the class Cephalopoda. These molluscs, commonly referred to as ammonites, are more closely related to living coleoids (i.e., octopuses, squid and cuttlefish) than they are to shelled nautiloids such as the living ''Nautilus'' species. The earliest ammonites appeared during the Devonian, with the last species vanishing during the Cretaceous–Paleogene extinction event. Ammonites are excellent index fossils, and linking the rock layer in which a particular species or genus is found to specific geologic time periods is often possible. Their fossil shells usually take the form of planispirals, although some helically spiraled and nonspiraled forms (known as heteromorphs) have been found. The name "ammonite", from which the scientific term is derived, was inspired by the spiral shape of their fossilized shells, which somewhat resemble tightly coiled rams' horns. Pliny the Elder ( 79 AD near Pomp ...
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Port Mulgrave, North Yorkshire
Port Mulgrave is a derelict former ironstone exporting port on the North Yorkshire coast midway between Staithes and Runswick Bay in the civil parish of Hinderwell. Rows of domestic properties and individual houses exist on the top of the cliff. Historically the locality was known as Rosedale, but to avoid confusion with the ironstone mines and iron works at Rosedale in the middle of the North York Moors the area was renamed Port Mulgrave for the local landowner the Earl of Mulgrave. History In the 1850s Sir Charles Palmer opened an ironstone mine at Rosedale Wyke, Port Mulgrave with ironstone loaded onto small vessels from a wooden jetty. The barges were moved in and out using a paddle steamer. A nearby harbour was constructed by Sir Charles Palmer in 1856-57 at a cost of £45,000. Initially the harbour exported ironstone to Jarrow on Tyneside to supply Palmers Shipbuilding and Iron Company Limited founded by Sir Charles Palmer. Later ironst ...
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Dinosaur
Dinosaurs are a diverse group of reptiles of the clade Dinosauria. They first appeared during the Triassic period, between 243 and 233.23 million years ago (mya), although the exact origin and timing of the evolution of dinosaurs is the subject of active research. They became the dominant terrestrial vertebrates after the Triassic–Jurassic extinction event 201.3 mya; their dominance continued throughout the Jurassic and Cretaceous periods. The fossil record shows that birds are feathered dinosaurs, having evolved from earlier theropods during the Late Jurassic epoch, and are the only dinosaur lineage known to have survived the Cretaceous–Paleogene extinction event approximately 66 mya. Dinosaurs can therefore be divided into avian dinosaurs—birds—and the extinct non-avian dinosaurs, which are all dinosaurs other than birds. Dinosaurs are varied from taxonomic, morphological and ecological standpoints. Birds, at over 10,700 living species, are among ...
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Fossil
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the ...
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Lias Group
The Lias Group or Lias is a lithostratigraphic unit (a sequence of rock strata) found in a large area of western Europe, including the British Isles, the North Sea, the Low Countries and the north of Germany. It consists of marine limestones, shales, marls and clays. ''Lias'' is a Middle English term for hard limestone, used in this specific sense by geologists since 1833. In the past, geologists used ''Lias'' not only for the sequence of rock layers, but also for the timespan during which they were formed. It was thus an alternative name for the Early Jurassic epoch of the geologic timescale. It is now more specifically known that the Lias is Rhaetian to Toarcian in age (over a period of 20 million years between ) and thus also includes a part of the Triassic. The use of the name "Lias" for a unit of time is therefore slowly disappearing. Subdivisions In southern England, the Lias Group is often divided into Lower, Middle and Upper subgroups. In Southern England the Lias is d ...
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