Eckfelder Maar

The House of Manderscheid was the name of the most powerful family in the Eifel region of Germany for a considerable period of time in the 15th century. In 1457, Dietrich III von Manderscheid was made a Reichsgraf (Imperial count) by the Emperor (probably Frederick III). When Dietrich died on 20 February 1498, he had appointed his sons Johann, Konrad and Wilhelm as new rulers – the family property had been distributed in 1488. Each of the sons founded a powerful lineage: Johann started the Manderscheid-Blankenheim-Gerolstein line, William the Manderscheid-Kail line, and Konrad (Cuno) the Manderscheid-Schleiden line. Augusta von Manderscheid-Blankenheim was the last countess. She was married to a member of the Bohemian nobility, Count Philipp Christian von Sternberg (1732–1811).

Manderscheid is a former Verbandsgemeinde ("collective municipality") in the district Bernkastel-Wittlich, in Rhineland-Palatinate, Germany. Its seat of administration was in Manderscheid. On 1 July 2014 it merged into the Verbandsgemeinde Wittlich-Land. The Verbandsgemeinde Manderscheid consisted of the following Ortsgemeinden ("local municipalities"):

Near the Eifel town of Manderscheid are the ruins of two castles, the castles of Manderschied, whose history and location reflect the mediaeval conflict of interest between the Electorate of Trier and the Duchy of Luxembourg.

Manderscheid (in Eifel dialect: Maanischd) is a town in the Bernkastel-Wittlich district in Rhineland-Palatinate, Germany, and also both a climatic spa and a Kneipp spa. Until 1 July 2014, when it became part of the Verbandsgemeinde Wittlich-Land, it was the seat of the former Verbandsgemeinde Manderscheid.

Eckfeld is an Ortsgemeinde – a municipality belonging to a Verbandsgemeinde, a kind of collective municipality – in the Bernkastel-Wittlich district in Rhineland-Palatinate, Germany.

Brockscheid is an Ortsgemeinde – a municipality belonging to a Verbandsgemeinde, a kind of collective municipality – in the Vulkaneifel district in Rhineland-Palatinate, Germany. It belongs to the Verbandsgemeinde of Daun, whose seat is in the like-named town.

Pantenburg (in Eifel dialect: Pahntebuasch) is an Ortsgemeinde – a municipality belonging to a Verbandsgemeinde, a kind of collective municipality – in the Bernkastel-Wittlich district in Rhineland-Palatinate, Germany.

Windsborn Crater Lake (German: Windsborn-Kratersee) is a water-filled volcanic crater in the Eifel mountains in Germany. It is located near Bettenfeld in the county of Bernkastel-Wittlich and in the state of Rhineland-Palatinate, and belongs to a group of four craters known as the Mosenberg Crater Row (Reihenkrater Mosenberg), named after the village of Mosenberg.

The Hitsche Maar lies in the Eifel Mountains between Bitburg and Ulmen. The maar has a diameter of 60 metres and a crater depth of 5 metres. Known as the "smallest maar in the Eifel", the Hitsche has silted up to form a sedge marsh.

The Dürres Maar is a maar located in the vicinity of the village of Gillenfeld, Germany in the West Eifel mountains about 400 metres northwest of the Holzmaar. The Dürres Maar ist a dry maar, the original maar lake has silted up. It is surrounded by an embankment of lapilli-tuff which has only been gently eroded and has a diameter of about 290 metres. The Dürres Maar was formed more than 25,000 years ago. In the hollow formed by the maar is a transitional bog, which is made of sphagnum and brown moss peats. The peat body is about 3,000 to 4,000 years old and has a thickness of about 12 metres. Below the peat are heavily disintegrated limnic deposits that date to the late late glacial period. The bog is not only fed by precipitation, but also be springs that are found at the northeastern end. The Dürres Maar is protected as a nature reserve.

Laufeld is an Ortsgemeinde – a municipality belonging to a Verbandsgemeinde, a kind of collective municipality – in the Bernkastel-Wittlich district in Rhineland-Palatinate, Germany.

The Holzmaar lies in the Volcanic Eifel in the German state of Rhineland-Palatinate almost halfway between Gillenfeld (2.5 km away to the southwest) and Eckfeld. The maar has an area of about 6.8 hectares (17 acres), a diameter of 325 metres (1,066 ft) and a depth of 21 metres (69 ft) and lies within a nature reserve, almost completely surrounded by woods. It is one of the two maars making up the Gillenfeld Maars, the other being the Pulvermaar. The Holzmaar is fed by a headstream of the Sammetbach which crosses the maar. In the immediate vicinity is another maar, the Dürres Maar. On its south and southwest shores, the maar has silted up with sediments, core samples from which give a comprehensive picture of the climate going back to the last cold period. The sediments of the Holzmaar go back 23,200 years. This assessment was made possible by comparing the sequence and radiometric dating obtained in the maar basin with that of the Meerfelder Maar. The time of the maximum of the last glaciation derived from varve chronology is in close agreement with data from the Greenland Ice Sheet Project (GISP2), but are somewhat at odds with those of the Greenland Ice Core Project (GRIP). In the sequence of sediments three zones of strata were found, when the most dust was deposited in the crater lake. If these dust-laden layers correspond to the ice advances of the northern German inland ice sheet, by comparing them with the exact chronological sequence of the dust layers in the Maar sediments an equally accurate age for local terminal moraines may be possible at suitable locations in northern Germany.