Knockaird is a village on the Isle of Lewis in the parish of Ness, in the Outer Hebrides, Scotland. It is the highest point in Port of Ness and is home to Dùn Èistean an ancient ruined fort on a small island, joined by a bridge. Knockaird is within the parish of Barvas; the B8014 travels between Port of Ness and Eoropie. The Clach Stein standing stones are situated between Port of Ness. Galson Estate - Knockaird Canmore - Lewis, Knockaird site record Canmore - Lewis, Clach Stein site record
Fivepenny is one of the many villages in the Lewis district of Ness and part of the Isle of Lewis, Outer Hebrides, Scotland. Fivepenny is within the parish of Barvas, is situated on the B8014, between Port of Ness and Eoropie. There are two separate places with this name, both in the north-west of Lewis. Furthest north in Ness the full name of the village there is Còig Peighinnean Nis, in the Borve area further south of the village there is Còig Peighinnean Bhuirgh. Both are known locally as Na Còig Peighinnean, the full name only being used to distinguish one from the other; the name refers to the fact. Visitor's guide for the Island of Lewis Website of the Western Isles Council with links to other resources Disabled access to Lewis for residents and visitors "Lewis-with-Harris". Encyclopædia Britannica. 16. 1911. Pp. 525–526. A Guide to living in the Outer Hebrides, with most information pertaining to Lewis
North Tolsta is a village in the Scottish Outer Hebrides, on the east side of the Isle of Lewis. North Tolsta is within the parish of Stornoway. Tolsta is notable for its long sandy beach, popular with surfers; the village of Bail' Ùr Tholastaidh is to Gleann Tholastaidh to the south. At the end of Tolsta's long sandy beach there are 5 caves only visitable during low tide, these Caves are locally known as "The Caves of Life." The village has a Primary School, two Churches and a Post office and community shop "Buth Tholastaidh". Formed in 2005, Tolsta Community Development Limited is a community interest company based in the village; the company operates a wind turbine at Glen Tolsta with the profits being used to benefit the Tolsta community. Wildlife in the area includes the kittiwake and the herring gull. Seals, dolphins and whales can be seen offshore. Lewis and Harris History of the Outer Hebrides North Tolsta Historical Society Visitor's guide for the Island of Lewis Website of the Western Isles Council with links to other resources Disabled access to Lewis for residents and visitors "Lewis-with-Harris".
Encyclopædia Britannica. 16. 1911. Pp. 525–526
Cross is a township on the Isle of Lewis in the community of Ness, in the Outer Hebrides, Scotland. Cross is within the parish of Barvas. Cross is situated on the A857, between Stornoway and Port of Ness. Cross had a school, now the Community Museum; the settlement has a food store, a hotel-inn, war memorial, post office, two churches and Croileagan. Cross is home to around 100 people. Canmore - Lewis, Cross site record Canmore - Lewis, Church of Scotland site record Canmore - Lewis, Free Church site record Canmore - Lewis, North Lewis War Memorial site record
The Scottish Parliament is the devolved unicameral legislature of Scotland. Located in the Holyrood area of the capital city, Edinburgh, it is referred to by the metonym Holyrood; the Parliament is a democratically elected body comprising 129 members known as Members of the Scottish Parliament, elected for four-year terms under the additional member system: 73 MSPs represent individual geographical constituencies elected by the plurality system, while a further 56 are returned from eight additional member regions, each electing seven MSPs. The most recent general election to the Parliament was held on 5 May 2016, with the Scottish National Party winning a plurality; the original Parliament of Scotland was the national legislature of the independent Kingdom of Scotland, existed from the early 13th century until the Kingdom of Scotland merged with the Kingdom of England under the Acts of Union 1707 to form the Kingdom of Great Britain. As a consequence, both the Parliament of Scotland and the Parliament of England ceased to exist, the Parliament of Great Britain, which sat at Westminster in London was formed.
Following a referendum in 1997, in which the Scottish electorate voted for devolution, the powers of the devolved legislature were specified by the Scotland Act 1998. The Act delineates the legislative competence of the Parliament – the areas in which it can make laws – by explicitly specifying powers that are "reserved" to the Parliament of the United Kingdom; the Scottish Parliament has the power to legislate in all areas that are not explicitly reserved to Westminster. The British Parliament retains the ability to amend the terms of reference of the Scottish Parliament, can extend or reduce the areas in which it can make laws; the first meeting of the new Parliament took place on 12 May 1999. The competence of the Scottish Parliament has been amended numerous times since most notably by the Scotland Act 2012 and Scotland Act 2016, with some of the most significant changes being the expansion of the Parliament's powers over taxation and welfare. Before the Treaty of Union 1707 united the Kingdom of Scotland and the Kingdom of England into a new state called "Great Britain", Scotland had an independent parliament known as the Parliament of Scotland.
Initial Scottish proposals in the negotiation over the Union suggested a devolved Parliament be retained in Scotland, but this was not accepted by the English negotiators. For the next three hundred years, Scotland was directly governed by the Parliament of Great Britain and the subsequent Parliament of the United Kingdom, both seated at Westminster, the lack of a Parliament of Scotland remained an important element in Scottish national identity. Suggestions for a'devolved' Parliament were made before 1914, but were shelved due to the outbreak of the First World War. A sharp rise in nationalism in Scotland during the late 1960s fuelled demands for some form of home rule or complete independence, in 1969 prompted the incumbent Labour government of Harold Wilson to set up the Kilbrandon Commission to consider the British constitution. One of the principal objectives of the commission was to examine ways of enabling more self-government for Scotland, within the unitary state of the United Kingdom.
Kilbrandon published his report in 1973 recommending the establishment of a directly elected Scottish Assembly to legislate for the majority of domestic Scottish affairs. During this time, the discovery of oil in the North Sea and the following "It's Scotland's oil" campaign of the Scottish National Party resulted in rising support for Scottish independence, as well as the SNP; the party argued that the revenues from the oil were not benefitting Scotland as much as they should. The combined effect of these events led to Prime Minister Wilson committing his government to some form of devolved legislature in 1974. However, it was not until 1978 that final legislative proposals for a Scottish Assembly were passed by the United Kingdom Parliament. Under the terms of the Scotland Act 1978, an elected assembly would be set up in Edinburgh provided that a referendum be held on 1 March 1979, with at least 40% of the total electorate voting in favour of the proposal; the 1979 Scottish devolution referendum failed: although the vote was 51.6% in favour of a Scottish Assembly, with a turnout of 63.6%, the majority represented only 32.9% of the eligible voting population.
Throughout the 1980s and 1990s, demand for a Scottish Parliament grew, in part because the government of the United Kingdom was controlled by the Conservative Party, while Scotland itself elected few Conservative MPs. In the aftermath of the 1979 referendum defeat, the Campaign for a Scottish Assembly was initiated as a pressure group, leading to the 1989 Scottish Constitutional Convention with various organisations such as Scottish churches, political parties and representatives of industry taking part. Publishing its blueprint for devolution in 1995, the Convention provided much of the basis for the structure of the Parliament. Devolution continued to be part of the platform of the Labour Party which, in May 1997, took power under Tony Blair. In September 1997, the Scottish devolution referendum was put to the Scottish electorate and secured a majority in favour of the establishment of a new devolved Scottish Parliament, with tax-varying powers, in Edinburgh. An election was held on 6 May 1999, on 1 July of that year power was transferred from Westminster to the new Parliament.
Since September 2004, the official home of the Scottish Parliament has been a new Scottish Parliament Building, in the Holyrood area of Edinburgh. The Scottish Parliament building was designed by Spanish architect Enric Miralles in partnership with local Ed
Peat known as turf, is an accumulation of decayed vegetation or organic matter. It is unique to natural areas called peatlands, mires, moors, or muskegs; the peatland ecosystem is the most efficient carbon sink on the planet, because peatland plants capture CO2 released from the peat, maintaining an equilibrium. In natural peatlands, the "annual rate of biomass production is greater than the rate of decomposition", but it takes "thousands of years for peatlands to develop the deposits of 1.5 to 2.3 m, the average depth of the boreal peatlands". Sphagnum moss called peat moss, is one of the most common components in peat, although many other plants can contribute; the biological features of Sphagnum mosses act to create a habitat aiding peat formation, a phenomenon termed'habitat manipulation'. Soils consisting of peat are known as histosols. Peat forms in wetland conditions, where flooding obstructs the flow of oxygen from the atmosphere, slowing the rate of decomposition. Peatlands bogs, are the primary source of peat, although less-common wetlands including fens and peat swamp forests deposit peat.
Landscapes covered in peat are home to specific kinds of plants including Sphagnum moss, ericaceous shrubs, sedges. Because organic matter accumulates over thousands of years, peat deposits provide records of past vegetation and climate by preserving plant remains, such as pollen; this allows humans to reconstruct past environments and study changes in human land use. Peat is harvested as an important source of fuel in certain parts of the world. By volume, there are about 4 trillion cubic metres of peat in the world, covering a total of around 2% of the global land area, containing about 8 billion terajoules of energy. Over time, the formation of peat is the first step in the geological formation of other fossil fuels such as coal low-grade coal such as lignite. Depending on the agency, peat is not regarded as a renewable source of energy, due to its extraction rate in industrialized countries far exceeding its slow regrowth rate of 1 mm per year, as it is reported that peat regrowth takes place only in 30-40% of peatlands.
Because of this, the UNFCCC, another organization affiliated with the United Nations classified peat as a fossil fuel. However, the Intergovernmental Panel on Climate Change has begun to classify peat as a "slowly renewable" fuel; this is the classification used by many in the peat industry. At 106 g CO2/MJ, the carbon dioxide emission intensity of peat is higher than that of coal and natural gas. Peat forms when plant material does not decay in acidic and anaerobic conditions, it is composed of wetland vegetation: principally bog plants including mosses and shrubs. As it accumulates, the peat holds water; this creates wetter conditions that allow the area of wetland to expand. Peatland features can include ponds and raised bogs. Most modern peat bogs formed 12,000 years ago in high latitudes after the glaciers retreated at the end of the last ice age. Peat accumulates at the rate of about a millimetre per year. Peat material is either hemic, or sapric. Fibric peats are the least consist of intact fibre.
Hemic peats are decomposed and sapric are the most decomposed. Phragmites peat are composed of reed grass, Phragmites australis, other grasses, it is denser than many other types of peat. Engineers may describe a soil as peat which has a high percentage of organic material; this soil is problematic because it exhibits poor consolidation properties – it cannot be compacted to serve as a stable foundation to support loads, such as roads or buildings. In a cited article and Clarke defined peatlands or mires as...the most widespread of all wetland types in the world, representing 50 to 70% of global wetlands. They cover over 3 % of the land and freshwater surface of the planet. In these ecosystems are found one third of the world’s soil carbon and 10% of global freshwater resources; these ecosystems are characterized by the unique ability to accumulate and store dead organic matter from Sphagnum and many other non-moss species, as peat, under conditions of permanent water saturation. Peatlands are adapted to the extreme conditions of high water and low oxygen content, of toxic elements and low availability of plant nutrients.
Their water chemistry varies from alkaline to acidic. Peatlands occur on all continents, from the tropical to boreal and Arctic zones from sea level to high alpine conditions. Peatlands are areas of land with formed layers of peat, they can cover around 4 million square kilometres. In Europe, peatlands extend to about 515,000 km2. About 60% of the world's wetlands are made of peat. Peat deposits are found in many places around the world, including northern Europe and North America; the North American peat deposits are principally found in the Northern United States. Some of the world's largest peatlands include the West Siberian Lowland, the Hudson Bay Lowlands, the Mackenzie River Valley. There is less peat in part because there is less land; that said, the vast Magellanic Moorland in South America is an extensive peat-dominated landscape. Peat can be found in New Zealand
Eoropie is the most northerly village on the Isle of Lewis in the parish of Ness, in the Outer Hebrides, Scotland. Eoropie is within the parish of Barvas; the Teampull Mholuaidh is to be found here. Eoropie is situated at the end of the B8013 and B8014 roads, from Lionel and Port of Ness, respectively, it contains the Eoropie Dunes Park. It is beside a beautiful beach at Traigh Shanndaigh. Cannmore - Lewis, Eoropie site record