Cuisine Of Gower
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Cuisine Of Gower
The cuisine of Gower, a peninsula in south Wales, is based on ingredients grown, raised or collected on or around the peninsula. The cuisine is based on fresh ingredients with recipes based around a fish or meat dish. Until the twentieth century, the peninsula was virtually cut off from other markets due to poor roads, and no rail connection. The result was that Gower became self-sufficient in food. Gower people also developed their own dialect of English, known as the Gower dialect, and their own traditions, which have since died out. The population of the peninsula was employed in agriculture, fishing, labour on the farms and larger country estates, weaving and, in the north, coal mining and cockling. With the expansion of motorized transport and road improvements, Gower became a popular tourist destination. Many residents now travel from Gower to work in the nearby city of Swansea. Much of the agricultural produce is now sold at Swansea Market, local farmers' markets, and furt ...
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Gower Peninsula
Gower ( cy, Gŵyr) or the Gower Peninsula () in southwest Wales, projects towards the Bristol Channel. It is the most westerly part of the historic county of Glamorgan. In 1956, the majority of Gower became the first area in the United Kingdom to be designated an Area of Outstanding Natural Beauty. Until 1974, Gower was administered as a rural district. It was then merged with the county borough of Swansea. From 1974 to 1996, it formed the Swansea district. Since 1996, Gower has been administered as part of the unitary authority of the City and County of Swansea. Since its establishment in 1999, the Gower Senedd constituency has only elected Labour members. The Gower constituency in Westminster had previously also elected only Labour Members of Parliament (MPs) since 1908; the longest run (with Normanton and Makerfield) of any UK constituency. This ended in 2015 when the Conservatives took the seat. In 2017, it returned to Labour. The area of both constituencies covers the ...
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Enclosure Acts
The Inclosure Acts, which use an archaic spelling of the word now usually spelt "enclosure", cover enclosure of open fields and common land in England and Wales, creating legal property rights to land previously held in common. Between 1604 and 1914, over 5,200 individual enclosure acts were passed, affecting 28,000 km2. History Before the enclosures in England, a portion of the land was categorized as "common" or "waste". "Common" land was under the control of the lord of the manor, but certain rights on the land such as pasture, pannage, or estovers were held variously by certain nearby properties, or (occasionally) ''in gross'' by all manorial tenants. "Waste" was land without value as a farm strip – often very narrow areas (typically less than a yard wide) in awkward locations (such as cliff edges, or inconveniently shaped manorial borders), but also bare rock, and so forth. "Waste" was not officially used by anyone, and so was often farmed by landless peasants. The r ...
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Larva
A larva (; plural larvae ) is a distinct juvenile form many animals undergo before metamorphosis into adults. Animals with indirect development such as insects, amphibians, or cnidarians typically have a larval phase of their life cycle. The larva's appearance is generally very different from the adult form (''e.g.'' caterpillars and butterflies) including different unique structures and organs that do not occur in the adult form. Their diet may also be considerably different. Larvae are frequently adapted to different environments than adults. For example, some larvae such as tadpoles live almost exclusively in aquatic environments, but can live outside water as adult frogs. By living in a distinct environment, larvae may be given shelter from predators and reduce competition for resources with the adult population. Animals in the larval stage will consume food to fuel their transition into the adult form. In some organisms like polychaetes and barnacles, adults are immobil ...
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Marl
Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part of the cliffs of Dover, and the Channel Tunnel follows these marl layers between France and the United Kingdom. Marl is also a common sediment in post-glacial lakes, such as the marl ponds of the northeastern United States. Marl has been used as a soil conditioner and neutralizing agent for acid soil and in the manufacture of cement. Description Marl or marlstone is a carbonate-rich mud or mudstone which contains variable amounts of clays and silt. The term was originally loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions. These typically contain 35–65% clay and 65–35% carbonate. The te ...
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General View Of Agriculture County Surveys
The ''General View'' series of county surveys was an initiative of the Board of Agriculture of Great Britain, of the early 1790s. Many of these works had second editions, in the 1810s. The Board, set up by Sir John Sinclair, was generally a proponent of enclosure Enclosure or Inclosure is a term, used in English landownership, that refers to the appropriation of "waste" or " common land" enclosing it and by doing so depriving commoners of their rights of access and privilege. Agreements to enclose land ...s. England Ireland Scotland Wales Other General William Marshall, who had written the Central Highlands survey, was a rival of Arthur Young, and at odds with him over the surveys. He wrote at length about the reports in 1808 to 1817, producing a five-volume ''Review'', generally critical of the reports. William Lester's ''History of British Implements and Machinery applicable to Agriculture'' (1811) drew heavily on extracts from the surveys, where those covere ...
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Board Of Agriculture (1793–1822)
Board or Boards may refer to: Flat surface * Lumber, or other rigid material, milled or sawn flat ** Plank (wood) ** Cutting board ** Sounding board, of a musical instrument * Cardboard (paper product) * Paperboard * Fiberboard ** Hardboard, a type of fiberboard * Particle board, also known as ''chipboard'' ** Oriented strand board * Printed circuit board, in computing and electronics ** Motherboard, the main printed circuit board of a computer * A reusable writing surface ** Chalkboard ** Whiteboard Recreation * Board game **Chessboard **Checkerboard * Board (bridge), a device used in playing duplicate bridge * Board, colloquial term for the rebound statistic in basketball * Board track racing, a type of motorsport popular in the United States during the 1910s and 1920s * Boards, the wall around a bandy field or ice hockey rink * Boardsports * Diving board (other) Companies * Board International, a Swiss software vendor known for its business intelligence software tool ...
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Old Red Sandstone
The Old Red Sandstone is an assemblage of rocks in the North Atlantic region largely of Devonian age. It extends in the east across Great Britain, Ireland and Norway, and in the west along the northeastern seaboard of North America. It also extends northwards into Greenland and Svalbard. These areas were a part of the ancient continent of Euramerica, Euramerica/Laurussia. In Britain it is a lithostratigraphy, lithostratigraphic unit (a sequence of rock strata) to which Stratigraphy, stratigraphers accord Geological unit#Lithostratigraphic units, supergroup status and which is of considerable importance to early paleontology. For convenience the short version of the term, ORS is often used in literature on the subject. The term was coined to distinguish the sequence from the younger New Red Sandstone which also occurs widely throughout Britain. Sedimentology The Old Red Sandstone describes a suite of sedimentary rocks deposited in a variety of environments during the Devonian ...
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Coal Measures
In lithostratigraphy, the coal measures are the coal-bearing part of the Upper Carboniferous System. In the United Kingdom, the Coal Measures Group consists of the Upper Coal Measures Formation, the Middle Coal Measures Formation and the Lower Coal Measures Formation. The group records the deposition of fluvio-deltaic sediments which consists mainly of clastic rocks (claystones, shales, siltstones, sandstones, conglomerates) interstratified with the beds of coal. In most places, the coal measures are underlain by coarser clastic sequences known as Millstone Grit, of Namurian age. The top of the coal measures may be marked by an unconformity, the overlying rocks being Permian or later in age. In some parts of Britain, however, the coal measures grade up into mainly coal-barren red beds of late Westphalian and possibly Stephanian age. Within the Pennine Basin these barren measures are now referred to as the Warwickshire Group, from the district where they achieve their thickest d ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Geology Of The Gower Peninsula
Geology () is a branch of natural science concerned with Earth and other astronomical objects, the features or rocks of which it is composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology, and so is treated as one major aspect of integrated Earth system science and planetary science. Geology describes the structure of the Earth on and beneath its surface, and the processes that have shaped that structure. It also provides tools to determine the relative and absolute ages of rocks found in a given location, and also to describe the histories of those rocks. By combining these tools, geologists are able to chronicle the geological history of the Earth as a whole, and also to demonstrate the age of the Earth. Geology provides the primary evidence for plate tectonics, the evolutionary history of life, and the Earth's past climates. Geologists broadly study the properties and processes of Earth ...
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