East Frisia in the context of "Frisians"

The Low Countries (Dutch: de Lage Landen; French: les Pays-Bas), historically also known as the Netherlands (Dutch: de Nederlanden), is a historical and geographically coastal lowland region in Northwestern Europe forming the lower basin of the Rhine–Meuse–Scheldt delta and consisting today of the three modern "Benelux" countries: Belgium, Luxembourg, and the Netherlands (Dutch: Nederland, which is singular). Also sometimes included are parts of France (such as Nord and Pas-de-Calais) and the German regions of East Frisia, Guelders and Cleves. Since the creation of the Holy Roman Empire, the region has been divided into numerous different entities.

Historically, the regions without access to the sea linked themselves politically and economically to those with access to form various unions of ports and hinterland, stretching inland as far as parts of the German Rhineland. Not only physically-low-altitude areas but also some hilly or elevated regions are now therefore considered part of the Low Countries, including Luxembourg and southern Belgium. Within the European Union, the region's political grouping is still referred to as the Benelux (short for Belgium-Netherlands-Luxembourg).

The Frisian languages (/ˈfriːʒən/ FREE-zhən or /ˈfrɪziən/ FRIZ-ee-ən) are a closely related group of West Germanic languages, spoken by about 400,000 Frisian people, who live on the southern fringes of the North Sea in the Netherlands and Germany. The Frisian languages are the closest living language group to the Anglic languages; the two groups make up the Anglo-Frisian languages group and together with the Low German dialects these form the North Sea Germanic languages. Despite the close genetic relationship between English and Frisian, the modern languages are not mutually intelligible. Geographical and historical circumstances have caused the two languages to drift apart linguistically.

Frisian is traditionally divided into three branches often labeled distinct Frisian languages even though the dialects within each branch are not necessarily mutually intelligible. West Frisian is by far the most spoken of the three and is an official language in the Dutch province of Friesland, where it is spoken on the mainland and on two of the West Frisian Islands: Terschelling and Schiermonnikoog. It is also spoken in four villages in the Westerkwartier of the neighbouring province of Groningen. North Frisian, the second branch, is spoken in the northernmost German district of Nordfriesland in the state of Schleswig-Holstein, on the North Frisian mainland and on the North Frisian Islands of Sylt, Föhr, Amrum, and the Halligs. It is also spoken on the islands of Heligoland and Düne in the North Sea. The third Frisian branch, East Frisian, has only one remaining variant, Sater Frisian, spoken in the municipality of Saterland in the Lower Saxon district of Cloppenburg. Surrounded by bogs, the four Saterlandic villages lie just outside the borders of East Frisia, in the Oldenburg Münsterland region. In East Frisia proper, East Frisian Low Saxon is spoken today, which is not a Frisian language, but a variant of Low German/Low Saxon.

The Kingdom of Holland (Dutch: Koningrijk Holland (contemporary), Koninkrijk Holland (modern); French: Royaume de Hollande) was the successor state of the Batavian Republic. It was created by Napoleon Bonaparte in March 1806 in order to strengthen control over the Netherlands by replacing the republican government with a monarchy. Since becoming emperor in 1804, Napoleon sought to extirpate republican tendencies in territories France controlled, and placed his third brother, Louis Bonaparte, on the throne of the puppet kingdom. In 1807, the adjacent German regions of East Frisia and Jever were added to the kingdom.

In 1809, after the Walcheren Campaign, Holland had to surrender all territories south of the River Rhine to France. Also in 1809, Dutch forces fighting on the French side participated in defeating the anti-Bonapartist German rebellion led by Ferdinand von Schill, at the Battle of Stralsund.

Peat is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. 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 or stagnant water obstructs the flow of oxygen from the atmosphere, slowing the rate of decomposition. Peat properties such as organic matter content and saturated hydraulic conductivity can exhibit high spatial heterogeneity.

Peatlands, particularly bogs, are the primary source of peat; although less common, other wetlands, including fens, pocosins and peat swamp forests, also deposit peat. Landscapes covered in peat are home to specific kinds of plants, including Sphagnum moss, ericaceous shrubs and 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 the reconstruction of past environments and the study of land-use changes.

A terp, also known as a wierde, woerd, warf, warft, werf, werve, wurt or værft, is an artificial dwelling mound found on the North European Plain that has been created to provide safe ground during storm surges, high tides and sea or river flooding. The various terms used reflect the regional dialects of the North European region.

Terps are found in the coastal regions of the Netherlands, particularly in the provinces of Zeeland, Friesland and Groningen, as well as in southern Denmark and northwestern Germany. Before the construction of dykes, these mounds provided protection against floodwaters that regularly disrupted daily life. They are especially common in East Frisia (Ostfriesland) and Nordfriesland in Germany. On the Halligen islands in Kries Norfriesland, people continue to live on terps without the protection of dykes. Terps are also present in the Rhine and Meuse river plains in central Netherlands. Further examples occur in North Holland, such as Avendorp near Schagen, and in the towns of Bredene and Leffinge near Oostende in Belgium. Additional terps are located at mouth of the IJssel River, including at Kampereiland in the province of Overijssel, as well as on the former island of Schokland in the Zuiderzee, now part of the reclaimed Noordoostpolder. An old terp, known as Het Torp is also located beneath the town of Den Helder in North Holland.

Bernhard Lauardus Duhm (October 10, 1847 – November 1, 1928) was a German Lutheran theologian, born in Bingum, today part of Leer, East Frisia. He was a member of the history of religions school.