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Tyne, Trent And Tors Gas Fields
The Tyne, Trent and Tors gas fields are depleted natural gas reservoirs and former gas production facilities in the southern North Sea, centred around the Trent installation about 115 km east of Flamborough Head, Yorkshire. The fields produced gas from 1996 to 2020. The fields The Tyne, Trent and Tors (Kilmar and Garrow) gas fields are located in UK Offshore Blocks 44/18a, 43/24, 43/22a, 42/25a and 43/21a. Tyne and Trent are named after English rivers that flow into the North Sea. Kilmar and Garrow are named after Tors in Cornwall, and together were referred to as the Tors development. The gas reservoirs have the following characteristics. Development The Tyne, Trent, Kilmar and Garrow gas fields were developed over the period 1996 to 2008. Gas was produced by five offshore installations, detailed in the table. Gas export from Trent reused the 24” Esmond to Bacton pipeline (Esmond Transmission System) to the Bacton gas terminal, also known as EAGLES East Anglia Ga ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Gas
Natural gas (also called fossil gas or simply gas) is a naturally occurring mixture of gaseous hydrocarbons consisting primarily of methane in addition to various smaller amounts of other higher alkanes. Low levels of trace gases like carbon dioxide, nitrogen, hydrogen sulfide, and helium are also usually present. Natural gas is colorless and odorless, so odorizers such as mercaptan (which smells like sulfur or rotten eggs) are commonly added to natural gas supplies for safety so that leaks can be readily detected. Natural gas is a fossil fuel and non-renewable resource that is formed when layers of organic matter (primarily marine microorganisms) decompose under anaerobic conditions and are subjected to intense heat and pressure underground over millions of years. The energy that the decayed organisms originally obtained from the sun via photosynthesis is stored as chemical energy within the molecules of methane and other hydrocarbons. Natural gas can be burned fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Sea
The North Sea lies between Great Britain, Norway, Denmark, Germany, the Netherlands and Belgium. An epeiric sea on the European continental shelf, it connects to the Atlantic Ocean through the English Channel in the south and the Norwegian Sea in the north. It is more than long and wide, covering . It hosts key north European shipping lanes and is a major fishery. The coast is a popular destination for recreation and tourism in bordering countries, and a rich source of energy resources, including wind and wave power. The North Sea has featured prominently in geopolitical and military affairs, particularly in Northern Europe, from the Middle Ages to the modern era. It was also important globally through the power northern Europeans projected worldwide during much of the Middle Ages and into the modern era. The North Sea was the centre of the Vikings' rise. The Hanseatic League, the Dutch Republic, and the British each sought to gain command of the North Sea and access t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flamborough Head
Flamborough Head () is a promontory, long on the Yorkshire coast of England, between the Filey and Bridlington bays of the North Sea. It is a chalk headland, with sheer white cliffs. The cliff top has two standing lighthouse towers, the oldest dating from 1669 and Flamborough Head Lighthouse built in 1806. The older lighthouse was designated a Grade II* listed building in 1952 and is now recorded in the National Heritage List for England, maintained by Historic England. The cliffs provide nesting sites for many thousands of seabirds, and are of international significance for their geology. Special Area of Conservation Flamborough Head has been designated a Special Area of Conservation (SAC) by the British Government's Joint Nature Conservation Committee (JNCC). (Special Areas of Conservation are strictly protected sites designated under the European Community Habitats Directive, which requires the establishment of a European network of important high-quality conservation sit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tyne
The River Tyne is a river in North East England. Its length (excluding tributaries) is . It is formed by the North Tyne and the South Tyne, which converge at Warden Rock near Hexham in Northumberland at a place dubbed 'The Meeting of the Waters'. The Tyne Rivers Trust measure the whole Tyne catchment as , containing of waterways. Course North Tyne The North Tyne rises on the Scottish border, north of Kielder Water. It flows through Kielder Forest, and in and out of the border. It then passes through the village of Bellingham before reaching Hexham. South Tyne The South Tyne rises on Alston Moor, Cumbria and flows through the towns of Haltwhistle and Haydon Bridge, in a valley often called the Tyne Gap. Hadrian's Wall lies to the north of the Tyne Gap. Coincidentally, the source of the South Tyne is very close to those of the Tees and the Wear. The South Tyne Valley falls within the North Pennines Area of Outstanding Natural Beauty (AONB) – the second largest of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Trent
The Trent is the Longest rivers of the United Kingdom, third-longest river in the United Kingdom. Its Source (river or stream), source is in Staffordshire, on the southern edge of Biddulph Moor. It flows through and drains the North Midlands. The river is known for dramatic flooding after storms and spring snowmelt, which in the past often caused the river to change course. The river passes through Stoke-on-Trent, Stone, Staffordshire , Stone, Rugeley, Burton upon Trent and Nottingham before joining the River Ouse, Yorkshire, River Ouse at Trent Falls to form the Humber Estuary, which empties into the North Sea between Kingston upon Hull, Hull in Yorkshire and Immingham in Lincolnshire. The wide Humber estuary has often been described as the boundary between the Midlands and the north of England. Name The name "Trent" is possibly from a Romano-British word meaning "strongly flooding". More specifically, the name may be a contraction of two Romano-British words, ''tros'' (" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kilmar Tor
Kilmar Tor (''Cornish: Kil Margh'') is an elongated hill, high and running from SW to NE, on Bodmin Moor in the county of Cornwall, England.Ordnance Survey 1:25,000 ''Explorer'' map series, No. 109 Its prominence of 118 metres qualifies it as a HuMP. Kilmar Tor is located on the eastern side of Bodmin Moor, about 2½ kilometres WSW of the hamlet of North Hill and 3½ kilometres north of Cornwall's highest village, Minions. It is surmounted by granite tors. There is trig point at the summit as well as a cairn and cist. The course of a dismantled railway runs around the hill to the south, evidence of the mining that used to be carried out in the area. On Kilmar Tor's northern flank is Twelve Men's Moor with Trewortha Tor and Hawk's Tor beyond the saddle. To the southeast is Bearah Tor and, to the south, Langstone Downs. Withy Brook runs roughly north to south past the western end of the hill and, to the east, open moorland descends to the valley of the River Lynher. Po ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Garrow Tor
Garrow Tor is a bare, tor-crowned hill, high, located on Garrow Downs in the northwest of Bodmin Moor in the county of Cornwall, England, UK.Ordnance Survey 1:25,000 ''Explorer'' map series, No. 109 At the summit of Garrow Tor are granite rock outcrops and the hill also bears extensive evidence of early settlement, including a massive stone hedge, Bronze Age settlements and hut circles and Medieval settlements. Panoramic views from the summit include Caradon Hill to the south, Rough Tor and Brown Willy to the north, Butter's Tor to the east, clay country to the west and the Atlantic Ocean The Atlantic Ocean is the second-largest of the world's five oceans, with an area of about . It covers approximately 20% of Earth's surface and about 29% of its water surface area. It is known to separate the " Old World" of Africa, Europe ... to the northwest. . [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rotliegend
The Rotliegend, Rotliegend Group or Rotliegendes (german: the underlying red) is a lithostratigraphy, lithostratigraphic unit (a sequence of rock strata) of latest Carboniferous to Guadalupian (middle Permian) age that is found in the subsurface of large areas in western and central Europe. The Rotliegend mainly consists of sandstone layers. It is usually covered by the Zechstein and lies on top of regionally different formation (stratigraphy), formations of late Carboniferous age. The name Rotliegend has in the past not only been used to address the rock strata themselves, but also the time span in which they were formed (in which case the Rotliegend was considered a series (stratigraphy), series or subsystem of the Permian). This time span corresponds roughly with the length of the Cisuralian Epoch (reference date), epoch. Facies and formation In large parts of Pangaea, the last tectonic phase, phases of the Hercynian orogeny were still ongoing during the start of the Permian. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Perenco
Perenco is an independent Anglo-French oil and gas company with a headquarters in London and Paris. It conducts exploration and production activities in 16 countries around the globe (the North Sea, Cameroon, Gabon, Republic of Congo, Democratic Republic of Congo, Guatemala, Ecuador, Colombia, Peru, Venezuela, Brazil, Belize, Tunisia, Egypt, Turkey, Iraq, Vietnam, Trinidad and Tobago). Perenco is involved in operations both onshore and offshore with production equal to approximately of oil equivalent per day. History The company was established in 1975 by Hubert Perrodo as a marine services company based in Singapore. In 1980 the Group founded the Techfor drilling company and built a fleet of drilling rigs, jack-ups, swamp barges and land rigs. In 1982, the Group acquired the French drilling company Cosifor. In 1985, Perenco began its expansion into the upstream business, acquiring several proven onshore oil and gas fields in the United States, applying secondary-recovery te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bacton Gas Terminal
The Bacton Gas Terminal is a complex of six gas terminals within four sites located on the North Sea coast of North Norfolk in the United Kingdom. The sites are near Paston and between Bacton and Mundesley; the nearest town is North Walsham. The other main UK gas terminals which receive gas from the UK continental shelf are at St Fergus, Aberdeenshire; Easington, East Riding of Yorkshire; Theddlethorpe, Lincolnshire; CATS Terminal, Teesside; and Rampside gas terminal, Barrow, Cumbria. History The Bacton complex which covers an area of about 180 acres (73 ha) opened during 1968. It has a frontage of 1 km (3200 feet) along the cliff top. It was initially built by Shell-Esso, Phillips Petroleum-Arpet Group, Amoco-Gas Council. Planning permission had been given on 16 June 1967 by Anthony Greenwood, Baron Greenwood of Rossendale. The Leman field began production on 13 August 1968 (joint Shell-Esso and joint Amoco-Gas Council), the Hewett field (Phillips Petroleum-Arpet Group) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cygnus Gas Field
The Cygnus gas field is a natural gas reservoir and gas production facilities in the UK sector of the southern North Sea. It is about 150 km of east of the Lincolnshire coast and started gas production in 2016. The field The Cygnus field extends over UK offshore Blocks 44/11a and 44/12a. The field was discovered in 1988 by Marathon Oil. The reservoirs are Permian Leman sandstone and Carboniferous sandstone formations and have recoverable reserves of 760 billion cubic feet. In 2019 the Cygnus gas field was jointly owned by Spirit Energy (61.25 %) and Neptune Energy (38.75 %), Neptune E&P UK Ltd operates the infrastructure. Development Production from the field has been developed in stages. In the first stage gas was produced by wells on the Cygnus Alpha platform and then routed by pipeline to the Bacton Gas Terminal via the Esmond Transmission System. The next stage entailed development of the north west part of the field produced from the Cygnus Bravo platform which was rout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
