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Bunnet Stane
The Bunnet Stane (or ''bonnet stone'') is a rock formation near the hamlet of Gateside in Fife, at the foot of West Lomond. It sits upon one of the calciferous sandstone outcrops of the Old Red Sandstone suie that exist around the base of the Lomond Hills The Lomond Hills (meaning either beacon hills or bare hills), also known outside the locality as the Paps of Fife, are a range of hills in central Scotland. They lie in western central Fife and Perth and Kinross, Scotland. At West Lomond is the .... The Bunnet Stane itself consists of an elevated table of rock, about ten feet by twenty feet across, which sits upon a thin column of rock like a giant mushroom. There are several romantic explanations for the stone's shape, but it was formed entirely by the natural weathering of the exposed outcrop. Maiden's Bower There is a small man-made cave carved into the outcrop beneath the Bunnet Stane called Maiden's Bower. Originally termed ''Maiden-bore'', the term was also applied t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bunnet Stane2
A flat cap is a rounded cap with a small stiff brim in front, originating in Britain and Ireland. The hat is known in Ireland as a paddy cap; in Scotland as a bunnet; in Wales as a Dai cap; and in the United States as an English cap, Irish cap, or flat cap. Various other terms exist (cabbie cap, driver cap, longshoreman cap, ivy cap, train engineer cap,etc.). Cloths used to make the cap include wool, tweed (most common), and cotton. Less common materials may include leather, linen, or corduroy. The inside of the cap is commonly lined for comfort and warmth. History The style can be traced back to the 14th century in Northern England, when it was more likely to be called a " bonnet". This term was replaced by "cap" before about 1700, except in Scotland, where it continues to be referred to as a ''bunnet'' in Scots. A 1571 Act of the English Parliament was enacted to stimulate domestic wool consumption and general trade. It decreed that on Sundays and holidays, al ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gateside (Fife)
Gateside is a small village in the north east of Fife, Scotland. It is inhabited by around 200 people. It also comprises a school (which is currently closed due to lack of primary aged pupils to attend), a park, seven-a-side football pitch, there used to be a village shop, and a pub (The Gateside Inn) which has now been converted into a private residence, the Gateside Memorial Hall and a garage (the Minimart). Gateside won a Tesco Magazine competition in 2012 and was named the "Friendliest Street in the UK." The River Eden runs through the village, which flows to Guardbridge and then into the North Sea. The nearest city is Perth Perth is the capital and largest city of the Australian state of Western Australia. It is the fourth most populous city in Australia and Oceania, with a population of 2.1 million (80% of the state) living in Greater Perth in 2020. Perth i .... External links Gateside and District Association Villages in Fife {{Fife-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fife
Fife (, ; gd, Fìobha, ; sco, Fife) is a council area, historic county, registration county and lieutenancy area of Scotland. It is situated between the Firth of Tay and the Firth of Forth, with inland boundaries with Perth and Kinross (i.e. the historic counties of Perthshire and Kinross-shire) and Clackmannanshire. By custom it is widely held to have been one of the major Pictish kingdoms, known as ''Fib'', and is still commonly known as the Kingdom of Fife within Scotland. A person from Fife is known as a ''Fifer''. In older documents the county was very occasionally known by the anglicisation Fifeshire. Fife is Scotland's third largest local authority area by population. It has a resident population of just under 367,000, over a third of whom live in the three principal towns, Dunfermline, Kirkcaldy and Glenrothes. The historic town of St Andrews is located on the northeast coast of Fife. It is well known for the University of St Andrews, the most ancient univers ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Lomond
West Lomond is the highest point in the county of Fife, Scotland and the highest peak in the Lomond Hills. Its cone-shaped summit, which is the remains of a volcanic plug, rises above an escarpment of Carboniferous sandstone and limestone layers, capped with a quartz-microgabbro sill. The conspicuous peaks of West Lomond, and its neighbour East Lomond, are visible for many miles around, which explains one suggested origin of their name, the 'Lomond' or 'beacon' hills. On the summit are the remains of an Iron Age hill fort. West Lomond is usually climbed from Craigmead car park on the Falkland-Leslie road which is at a height of almost 300 metres. Another route of ascent leaves from the Bunnet Stane and climbs diagonally up the steep north slopes of the escarpment to a gap in the cliffs, gaining the plateau a short distance from the summit cone. This route is steeper and begins at a much lower altitude than the Craigmead car park. Geodesy Until 1891 West Lomond was the meridi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calciferous Sandstone
Calciferous sandstone is a geological term relating to strata at the base of the Carboniferous formation, below the entire sequence of coal measures. This term may be unique to the UK. Typically this part of the geological sequence, as in the Touch Hills and Fintry Hills to the west of Stirling tends to contain a mixture of lavas and sedimentary rocks, including sandstone Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates ... and mudstone, and lies unconformably on top of older Devonian strata. Carboniferous geology {{UK-geologic-formation-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lomond Hills
The Lomond Hills (meaning either beacon hills or bare hills), also known outside the locality as the Paps of Fife, are a range of hills in central Scotland. They lie in western central Fife and Perth and Kinross, Scotland. At West Lomond is the highest point in the county of Fife. Etymology The name ''Lomond Hills'' was first recorded ''Lomondys'' in 1315, and may derive from a Pictish cognate of Welsh ''llumon'', meaning "beacon", an element found for example in the hill-name Pumlumon in Wales. Also suggested is derivation from Gaelic ''lom monadh'', "bare hill", perhaps adapted from an earlier Pictish name containing cognate elements. Physical geography The Lomond Hills contain two prominent peaks, West Lomond and East Lomond (or Falkland Hill) (), which sit just under apart above a long north and west-facing escarpment over in length. The escarpment, made from beds of sandstone, limestone and a quartz-dolerite sill, rises steeply from the low ground to the north and w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Fife
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tourist Attractions In Fife
Tourism is travel for pleasure or business; also the theory and practice of touring (other), touring, the business of attracting, accommodating, and entertaining tourists, and the business of operating tour (other), tours. The World Tourism Organization defines tourism more generally, in terms which go "beyond the common perception of tourism as being limited to holiday activity only", as people "travelling to and staying in places outside their usual environment for not more than one consecutive year for leisure and not less than 24 hours, business and other purposes". Tourism can be Domestic tourism, domestic (within the traveller's own country) or International tourism, international, and international tourism has both incoming and outgoing implications on a country's balance of payments. Tourism numbers declined as a result of a strong economic slowdown (the late-2000s recession) between the second half of 2008 and the end of 2009, and in consequence of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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