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Fairy Falls, Trefriw
The Fairy Falls (Welsh language, Welsh: Rhaeadr y Tylwyth Teg) are a waterfall in the village of Trefriw, north Wales. The falls are on the river Crafnant which has its source at Llyn Crafnant, being joined upstream by a tributary, the river Geirionydd. Below the falls the river Crafnant flows on to itself become a tributary of the river Conwy. The main falls are about 25 feet high, the water falling down an angled rockface, and they were formed during the Last Glacial Period, last ice age some 20,000 years ago. As the main glacier passed down the Conwy Valley, it truncated the Crafnant valley, leaving a hanging valley and this series of falls.''The Conwy Valley'', K. Mortimer Hart, 1987 Not all of the water from the river Crafnant passes over the falls, as a little upstream some is diverted through a pipeline to provide hydro-electric power for the woollen mill. During drier periods this can leave the falls with little or even no water, but most of the year there is a go ...
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Fairy Falls Trefriw After Heavy Rainfall
A fairy (also called fay, fae, fae folk, fey, fair folk, or faerie) is a type of mythical being or legendary creature, generally described as anthropomorphism, anthropomorphic, found in the folklore of multiple European cultures (including Celtic mythology, Celtic, Slavic paganism, Slavic, Germanic folklore, Germanic, and French folklore, French folklore), a form of Supernatural#Spirit, spirit, often with metaphysical, supernatural, or preternatural qualities. Myths and stories about fairies do not have a single origin but are rather a collection of folk beliefs from disparate sources. Various folk theories about the origins of fairies include casting them as either demoted angels or demons in a Christian mythology, Christian tradition, as deities in Paganism, Pagan belief systems, as Spirit (supernatural entity), spirits of the dead, as Prehistory, prehistoric precursors to humans, or as spirits of nature. The label of ''fairy'' has at times applied only to specific Magic (su ...
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Hanging Valley
A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. Forma ...
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Waterfalls Of Conwy County Borough
A waterfall is any point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling onto softer rock, which erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls since prehistory, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century, they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is g ...
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List Of Waterfalls In Wales
Wales is a mountainous country with a wet climate and hence home to many hundreds of waterfalls. Some are popular visitor attractions, many are celebrated in legend whilst others are relatively unknown. Naming of falls As might be expected in this bilingual country, many waterfalls are known by both English and Welsh names. The terms 'rhaeadr', 'sgwd', 'pistyll' and 'ffrwd' all feature in the Welsh names of waterfalls. 'Sgwd' (plural 'sgydau') is restricted to the southern part of mid Wales, notably Brecknockshire whilst 'pistyll' is common in the northern parts of mid Wales. Alphabetical table of named waterfalls A, B, C D, E, F G, H, I, J, K, L M, N, O P, Q R S T, U, V, W, X, Y, Z See also * List of waterfalls * Waterfall Country References Ordnance Survey 1:25,000 scale Explorer map series, sheets 151-266 {{Geography of Wales Wales Wales ( ) is a Countries of the United Kingdom, country that is part of the United Kingdom. It is bordered by t ...
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List Of Waterfalls
This list of notable waterfalls of the world is sorted by continent, then country, then province, state or territory. A waterfall is included if it is at least tall and has an existing Wikipedia article, or it is considered historically significant based on multiple reliable references. There is no standard way to measure the height or width of a waterfall. No ranking of waterfalls should be assumed because of the heights or widths provided in the list. Many numbers are estimated and measurements may be imprecise. See additional lists of waterfalls by List of waterfalls by height, height, List of waterfalls by flow rate, flow rate and List of waterfalls by type, type. Africa Angola * Kalandula Falls – high Burundi * Kagera waterfalls, Kagera Falls * Rusumo Falls Central African Republic * Boali, Boali Falls Chad * Gauthiot Falls Democratic Republic of the Congo * Boyoma Falls – formerly known as Stanley Falls; highest flow rate in the world * Inga ...
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Llyn Geirionydd
Llyn Geirionydd lies in a valley in North Wales where the northern edge of the Gwydyr Forest meets the lower slopes of the Carneddau mountains. The lake is almost a mile long and covers an area of , but is never any deeper than according to Jehu's survey. The lake can be reached by car from Trefriw or Llanrwst in the Conwy valley, the lane passing through the hamlet of Llanrhychwyn, or from the road through the Gwydir Forest. Access is not particularly easy by either route, but this has not stopped the lake being the only one designated in Snowdonia to permit power boats and water skiing. Many visitors also walk to the lake from the village of Trefriw (it is on one of the Trefriw Trail routes) or from the neighbouring lake of Llyn Crafnant, which runs parallel to it, but a mile distant, the two being separated by Mynydd Deulyn, “mountain of the two lakes”. The lake has a car park (with toilets) and the location is very popular in the summer. This car park was once a was ...
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British Goblins
''British Goblins: Welsh Folk-Lore, Fairy Mythology, Legends and Traditions'' is an 1880 book on Welsh folklore and mythology by American journalist Wirt Sikes. Background and publication William Wirt Sikes was an American journalist and author who served as the United States Consul in Cardiff from 1876 until his death in 1883. In his early career, Sikes wrote various short-stories and poems for American magazines and newspapers, some of which were compiled into the ''Book for the Winter-Evening Fireside'' in 1858. He published two novels in the late 1860s, partially drawn from his experiences as a reporter for the '' Chicago Evening Journal''. Before taking his post as Consul, Sikes unsuccessfully searched for coverage of southern Wales in various bookstores, noting that he was only able to find an obsolete 18th century account of the region in the Library of Congress. Seeing American knowledge of Wales as insufficient, he published a number of articles on the country in Americ ...
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Wirt Sikes
William Wirt Sikes (November 23, 1836 – August 18, 1883) was an American journalist and writer, perhaps best known today for his writings on Welsh folklore and customs. Early life William Wirt Sikes was born in Watertown, New York, the son of William Johnson Sikes, a prominent local physician. He was the seventh of eleven children, of whom only six survived to adulthood. Sikes himself was seriously ill as a child and almost lost his hearing, so he was largely educated at home. At fourteen he went to work for a printer and learned how to set type. He supported himself thereafter by typesetting, contributing to local newspapers, and giving temperance lectures. At the age of nineteen, on August 28, 1855, he married Jeannette Annie Wilcox (1837–1889); they had two children, George Preston Sikes (1856–1957) and Clara Jeanette Sikes (1858–1956). Career in America In 1856 he was working at the ''Utica Morning Herald'' as a typesetter and contributor. He published a book of sto ...
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Edwardian
In the United Kingdom, the Edwardian era was a period in the early 20th century that spanned the reign of King Edward VII from 1901 to 1910. It is commonly extended to the start of the First World War in 1914, during the early reign of King George V. The era is dated from the Death and state funeral of Queen Victoria, death of Queen Victoria in January 1901, which marked the end of the Victorian era. Her son and successor, Edward VII, was already the leader of a fashionable elite that set a style influenced by the art and fashions of continental Europe. Samuel Hynes described the Edwardian era as a "leisurely time when women wore picture hats and did not vote, when the rich were not ashamed to live conspicuously, and The empire on which the sun never sets, the sun never set on the British flag." The Liberals returned to power in 1906 United Kingdom general election, 1906 and made Liberal welfare reforms, significant reforms. Below the upper class, the era was marked by signifi ...
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Waterwheel
A water wheel is a machine for converting the kinetic energy of flowing or falling water into useful forms of power, often in a watermill. A water wheel consists of a large wheel (usually constructed from wood or metal), with numerous blades or buckets attached to the outer rim forming the drive mechanism. Water wheels were still in commercial use well into the 20th century, although they are no longer in common use today. Water wheels are used for milling flour in gristmills, grinding wood into pulp for papermaking, hammering wrought iron, machining, ore crushing and pounding fibre for use in the manufacture of cloth. Some water wheels are fed by water from a mill pond, which is formed when a flowing stream is dammed. A channel for the water flowing to or from a water wheel is called a mill race. The race bringing water from the mill pond to the water wheel is a headrace; the one carrying water after it has left the wheel is commonly referred to as a tailrace. Waterwheel ...
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Hydro-electric Power
Hydroelectricity, or hydroelectric power, is electricity generated from hydropower (water power). Hydropower supplies 15% of the world's electricity, almost 4,210 TWh in 2023, which is more than all other renewable sources combined and also more than nuclear power. Hydropower can provide large amounts of low-carbon electricity on demand, making it a key element for creating secure and clean electricity supply systems. A hydroelectric power station that has a dam and reservoir is a flexible source, since the amount of electricity produced can be increased or decreased in seconds or minutes in response to varying electricity demand. Once a hydroelectric complex is constructed, it produces no direct waste, and almost always emits considerably less greenhouse gas than fossil fuel-powered energy plants.
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Conwy Valley
The River Conwy (; ) is a river in north Wales. From its source to its discharge in Conwy Bay it is long and drains an area of 678 square km. "Conwy" was formerly anglicised as "Conway." The name 'Conwy' derives from the old Welsh words ''cyn'' (chief) and ''gwy'' (water), the river being originally called the 'Cynwy'. It rises on the Migneint moor where a number of small streams flow into Llyn Conwy, then flows in a generally northern direction, being joined by the tributaries of the rivers Machno and Afon Lledr before reaching Betws-y-coed, where it is also joined by Llugwy. From Betws-y-coed the river continues to flow north through Llanrwst, Trefriw (where it is joined by the Afon Crafnant) and Dolgarrog (where it is joined by Afon Porth-llwyd and Afon Ddu) before reaching Conwy Bay at Conwy. A local quay, Cei Cae Gwyn, is located on its bank. During spring tides the river is tidal as far as Tan-lan, near Llanrwst. Tributaries of the River Conwy This is a l ...
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