Half-foot

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Half-foot (Scottish Gaelic : leth-chois, Scots : hauf-fit) was a kind of land tenure peculiar to northern and western Scotland.

Scots language Germanic language

Scots is the Germanic language variety spoken in Lowland Scotland and parts of Ulster in Ireland. It is sometimes called Lowland Scots to distinguish it from Scottish Gaelic, the Celtic language which was historically restricted to most of the Highlands, the Hebrides and Galloway after the 16th century. The Scots language developed during the Middle English period as a distinct entity.

In common law systems, land tenure is the legal regime in which land is owned by an individual, who is said to "hold" the land. It determines who can use land, for how long, and under what conditions. Tenure may be based both on official laws and policies, and on informal customs. The French verb "tenir" means "to hold" and "tenant" is the present participle of "tenir". The sovereign monarch, known as The Crown, held land in its own right. All private owners are either its tenants or sub-tenants. Tenure signifies the relationship between tenant and lord, not the relationship between tenant and land. Over history, many different forms of land ownership, i.e., ways of owning land, have been established.

Scotland Country in Europe, part of the United Kingdom

Scotland is a country that is part of the United Kingdom. Sharing a border with England to the southeast, Scotland is otherwise surrounded by the Atlantic Ocean to the north and west, by the North Sea to the northeast and by the Irish Sea to the south. In addition to the mainland, situated on the northern third of the island of Great Britain, Scotland has over 790 islands, including the Northern Isles and the Hebrides.

The possessor, generally impoverished, or without facilities for working the land, often furnished the land and seed corn, and the tenant cultivated it, the produce being equally divided between them. There have been instances of it in the 20th century.

Other uses:

Peat accumulation of partially decayed vegetation

Peat, also known as turf, is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem is the most efficient carbon sink on the planet, because peatland plants capture CO2 naturally 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 [4.9 to 7.5 ft], which is the average depth of the boreal [northern] peatlands". Sphagnum moss, also 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 primarily 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.

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References

Edward Dwelly British lexicographer

Edward Dwelly (1864–1939) was an English lexicographer and genealogist. He created the authoritative dictionary of Scottish Gaelic, and his work has had an influence on Irish Gaelic lexicography. He also practised as a professional genealogist and published transcripts of many original documents relating to Somerset.