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Tunbridge Wells Sand
The Tunbridge Wells Sand Formation is a geological unit which forms part of the Wealden Group and the uppermost and youngest part of the unofficial Hastings Beds. These geological units make up the core of the geology of the Weald in the English counties of West Sussex, East Sussex and Kent. The other component formations of the Hastings Beds are the underlying Wadhurst Clay Formation and the Ashdown Formation. The Hastings Beds in turn form part of the Wealden Group which underlies much of southeast England. The sediments of the Weald, including the Tunbridge Wells Sand Formation, were deposited during the Early Cretaceous Period, which lasted for approximately 40 million years from 140 to 100 million years ago. The Tunbridge Wells Sands are of Late Valanginian age.Hopson, P.M., Wilkinson, I.P. and Woods, M.A. (2010) ''A stratigraphical framework for the Lower Cretaceous of England''. Research Report RR/08/03. British Geological Survey, Keyworth. The Formation takes its ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bexhill-on-Sea
Bexhill-on-Sea (often shortened to Bexhill) is a seaside town and civil parish situated in the county of East Sussex in South East England. An ancient town and part of the local government district of Rother, Bexhill is home to a number of archaeological sites, a Manor House in the Old Town, an abundance of Edwardian and Victorian architecture, and the famous De La Warr Pavilion: today a centre for contemporary art – which has featured the work of Andy Warhol, Cerith Wyn Evans and Richard Wilson among others – and an auditorium, where Bob Marley had his first UK appearance and has since seen performances by Elvis Costello, Goldfrapp, Marti Caine, Ray Davies, Years & Years, Patti Smith and Laurie Anderson. History The first reference to Bexhill, or Bexelei as it was originally called, was in a charter granted by King Offa of Mercia in 772 AD. It is recorded that King Offa had "defeated the men of Hastings" in 771 AD. At this time, the term Hastings would have re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kent
Kent is a county in South East England and one of the home counties. It borders Greater London to the north-west, Surrey to the west and East Sussex to the south-west, and Essex to the north across the estuary of the River Thames; it faces the French department of Pas-de-Calais across the Strait of Dover. The county town is Maidstone. It is the fifth most populous county in England, the most populous non-Metropolitan county and the most populous of the home counties. Kent was one of the first British territories to be settled by Germanic tribes, most notably the Jutes, following the withdrawal of the Romans. Canterbury Cathedral in Kent, the oldest cathedral in England, has been the seat of the Archbishops of Canterbury since the conversion of England to Christianity that began in the 6th century with Saint Augustine. Rochester Cathedral in Medway is England's second-oldest cathedral. Located between London and the Strait of Dover, which separates England from mainla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Sandstone
Southern Sandstone is a local name for the Ardingly Sandstone of southeast England, a soft sandstone of Cretaceous age separating the Tunbridge Wells Sands from the overlying Grinstead Clay. The outcrops in the Weald of Kent are the rock climbing crags closest to London and are probably the most heavily climbed in the UK. Geology The horizon of thick, cross-bedded, fine-to-medium grained quartz sandstone separating the Tunbridge Wells Sands from the overlying Grinstead Clay is known as Ardingly Sandstone. It is particularly well exposed throughout the region between East Grinstead, West Sussex, and Tunbridge Wells, Kent. Climbing Stone Farm and Harrisons Rocks are managed by the British Mountaineering Council (BMC). The rock is particularly soft and care needs to be taken to prevent erosion. It is climbed either solo or on a top-rope. Many bolts have been placed at the top of the crags. Soloing requires no more equipment than bouldering. Locations Southern Sandstone is outcr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Climbers
Rock climbing is a sport in which participants climb up, across, or down natural rock formations. The goal is to reach the summit of a formation or the endpoint of a usually pre-defined route without falling. Rock climbing is a physically and mentally demanding sport, one that often tests a climber's strength, endurance, agility and balance along with mental control. Knowledge of proper climbing techniques and the use of specialized climbing equipment is crucial for the safe completion of routes. Because of the wide range and variety of rock formations around the world, rock climbing has been separated into several different styles and sub-disciplines, such as scrambling, bouldering, sport climbing, and trad (traditional) climbing another activity involving the scaling of hills and similar formations, differentiated by the rock climber's sustained use of hands to support their body weight as well as to provide balance. Rock climbing competitions have the objectives of either ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Rocks
High Rocks is a geological Site of Special Scientific Interest west of Tunbridge Wells in East Sussex and Kent. It is a Geological Conservation Review site. Prehistory The location was formed when a melting ice sheet at the end of the last ice age uncovered hardened silt deposited when the area was part of the Wealden Lake. There are traces of Middle Stone Age and Iron Age residents, including a 1st-century A.D. fort guarding against the Roman invasion. Recent history After King James II visited Tunbridge Wells and made the woodland a resort in the 17th century, High Rocks became a tourist attraction which also offered a maze, a bowling green, gambling rooms and cold baths. The ''Aerial Walk'', a series of bridges linking the tops of the crags, was built in the 19th century. A halt served by the local railway was established in 1907, and was used until 1952. The Spa Valley Railway, a heritage railway, now connects the High Rocks pub beyond the High Rocks turnstiles to Tunbr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harrisons Rocks
Harrison's Rocks is a series of sandstone crags approximately south of the village of Groombridge in the county of East Sussex. The site is a notable example of a periglacial tor landform developed in rocks of the Ardingly Sandstone Member of the Tunbridge Wells Sand Formation. It is popular with rock climbers, and is the largest of the cluster of local outcrops known by climbers as Southern Sandstone. Harrison's Rocks is owned by climbers and is managed on their behalf by the British Mountaineering Council with funding from the English Sports Council. Geology Harrison's Rocks are a notable example of a periglacial tor landform, developed in rocks of the Tunbridge Wells Sand Formation of the Wealden Supergroup of early Cretaceous age. Harrison's Rocks is composed of a soft sandstone, which is prone to being worn away. Climbing Harrison's Rocks has been owned by the British Mountaineering Council since 2009, and is managed by a local group of volunteers known as the Harri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Hoathly
West Hoathly is a village and civil parish in the Mid Sussex District, Mid Sussex District of West Sussex, England, located south west of East Grinstead. In the 2001 census 2,121 people, of whom 1,150 were economically active, lived in 813 households. At the 2011 Census the population increased to 2,181. The parish, which has a land area of , includes the Hamlet (place), hamlets of Highbrook, Selsfield Common and Sharpthorne. The mostly rural parish is centred on West Hoathly village, an ancient hilltop settlement in the Weald, High Weald between the North Downs, North and South Downs. History The area was already settled by the 11th century, when St Margaret's Church, West Hoathly, St Margaret's Church was founded. Names recorded at that time include ''Hadlega'' and ''Hodlega''—later standardised to ''Hodlegh'' and ''Hothelegh'', then (West) Hoathly. This Anglo-Saxons, Anglo-Saxon word signifies a heath-covered clearing. The parish lay on the edge of the dense woodland of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Grinstead
East Grinstead is a town in West Sussex, England, near the East Sussex, Surrey, and Kent borders, south of London, northeast of Brighton, and northeast of the county town of Chichester. Situated in the extreme northeast of the county, the civil parish has an area of . The population at the 2011 Census was 26,383. Nearby towns include Crawley and Horley to the west, Tunbridge Wells to the east and Redhill and Reigate to the northwest. The town is contiguous with the village of Felbridge to the northwest. Until 1974 East Grinstead was in East Sussex, before joining together with Haywards Heath and Burgess Hill as the Mid-Sussex district of West Sussex. The town is on the Greenwich Meridian. It has many historic buildings, and the Weald and Ashdown Forest lie to the south-east. Places of interest The High Street contains one of the longest continuous runs of 14th-century timber-framed buildings in England. Other notable buildings in the town include Sackville College, the san ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bowles Rocks
Bowles Rocks is a sandstone crag in the county of East Sussex, on the border with Kent, approximately south of the town of Royal Tunbridge Wells. It is popular with rock climbers due to the excellent, south-facing, quick-drying rock, the range of climbs and the ease of access. It is one of the cluster of local outcrops known as Southern Sandstone. History Bowles Rocks was cleared in the early 1960s by John Walters, who was inspired to set up a 'rock climbing gymnasium'. Previously the site had been used as a firing range during the Second World War and to house pigs – hence the climb named Pig's Nose and area called Range Wall. The bullet holes in the rock and larger square holes lower down, which once supported the wooden beams of the pig sties, can still be clearly seen. Climbing There are approximately 230 climbs or variants at Bowles Rocks, ranging widely in difficulty. A good list can be found here. Type of rock Bowles Rocks is made of a relatively soft sandst ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haywards Heath
Haywards Heath is a town in West Sussex, England, south of London, north of Brighton, south of Gatwick Airport and northeast of the county town, Chichester. Nearby towns include Burgess Hill to the southwest, Horsham to the northwest, Crawley northwest and East Grinstead northeast. With only a relatively small number of jobs available in the immediate vicinity, mostly in the agricultural or service sector, many residents work "remotely" or commute daily via road or rail to London, Brighton, Crawley or Gatwick Airport for work. Etymology The first element of the place-name Haywards Heath is derived from the Old English ''hege'' + ''worð'', meaning hedge enclosure, with the later addition of ''hǣð''. The place-name was first recorded in 1261 as ''Heyworth'', then in 1359 as ''Hayworthe'', in 1544 as ''Haywards Hoth'' (i.e. 'heath by the enclosure with a hedge'), and in 1607 as ''Hayworths Hethe''. There is a local legend that the name comes from a highwayman who went under ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tunbridge Wells
Royal Tunbridge Wells is a town in Kent, England, southeast of central London. It lies close to the border with East Sussex on the northern edge of the Weald, High Weald, whose sandstone geology is exemplified by the rock formation High Rocks. The town was a spa in the Restoration (England), Restoration and a fashionable resort in the mid-1700s under Richard (Beau) Nash, Beau Nash when the Pantiles, and its chalybeate spring, attracted visitors who wished to take the waters. Though its popularity as a spa town waned with the advent of sea bathing, the town still derives much of its income from tourism. The town has a population of around 56,500, and is the administrative centre of Tunbridge Wells (borough), Tunbridge Wells Borough and in the parliamentary constituency of Tunbridge Wells (UK Parliament constituency), Tunbridge Wells. History Iron Age Evidence suggests that Iron Age people farmed the fields and mined the iron-rich rocks in the Tunbridge Wells area, and excava ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valanginian
In the geologic timescale, the Valanginian is an age or stage of the Early or Lower Cretaceous. It spans between 139.8 ± 3.0 Ma and 132.9 ± 2.0 Ma (million years ago). The Valanginian Stage succeeds the Berriasian Stage of the Lower Cretaceous and precedes the Hauterivian Stage of the Lower Cretaceous. Stratigraphic definitions The Valanginian was first described and named by Édouard Desor in 1853. It is named after Valangin Valangin () is a former municipality in the district of Val-de-Ruz in the canton of Neuchâtel in Switzerland. On 1 January 2021 the former municipalities of Corcelles-Cormondrèche, Peseux and Valangin merged into the municipality of Neuchâ ..., a small town north of Neuchâtel in the Jura Mountains of Switzerland. The base of the Valanginian is at the first appearance of Calpionellidae, calpionellid species ''Calpionellites darderi'' in the stratigraphic column. A global reference section (a GSSP) had in 2009 not yet been appointed. The top o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
